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Chapter 2 - Change and Stability in Ecosystems
Section 21 - Cycling of Matter in Ecosystems
Types of Matter
bull ORGANIC MATTER containsbull Carbonbull Hydrogenbull Sometimes Oxygenbull Sometimes Nitrogenbull Examples include proteins sugars and fats
bull INORGANIC MATTER does not containbull carbon and hydrogenbull Examples include carbon dioxide (CO2) water (H2O) and ammonia (NH3)
Cycling of Organic Matter
Organic Matter is continuously being recycled
Living organisms are made up of organic matter There is a limited amount on the Earth so it must be recycled for life to continue
Example Carbon molecules are recycled over and over This means that it is possible that your body contains a carbon molecule which was part of a dinosaur from 70 million years ago
Food is organic matter that was once part of a living thing
Digestion breaks down organic molecules which areused by your cells
Decay is when decomposer organisms breakdown organic materials (dead bodies and feces) and make it available to other living organisms
Fruit and Vegetable Decay
Sample Food Chain
Plant
Rabbit
Fox (feces)
Soil Bacteria (Decomposers)
Inorganic Molecules
Inorganic nutrients
Plant
Assignment
read pages 50-51 and do questions 1 2 5 amp 6 on page 51
Section 25-The Carbon Cycle
Carbon is the key element for living things
Carbon can be found in
1 The atmosphere (CO2)
2 Ocean (dissolved)
3 Plants (sugar C6H12O6)
4 Animals (protein)
5 Soil and rocks
The Carbon Cycle As carbon moves through the ecosystem it is
changed from one form to another
In Plants PHOTOSYNTHESISsunlight
CO2 + H2O C6H12O6 + O2
(Carbon dioxide + water glucose + oxygen)
In Animals CELLULAR RESPIRATION
C6H12O6 + O2 CO2 + H2O
The relationship between photosynthesis and cellular respiration is called the carbon cycle
Photosynthesis is the process in which plants use solar energy carbon dioxide from the atmosphere and water from the soil to make sugar
Cellular Respiration uses sugar and oxygen for energy and releases carbon dioxide back into the environment
The Carbon Cycle
Carbon ReservoirsReservoirs of Inorganic Carbon When carbon is not in organic form it can be found in three
types of storage (reservoirs)
Atmosphere (smallest ~ 003) Oceans (largest) Earthrsquos crust
Reservoirs for Organic Carbon Organic carbon is held in the bodies of living organisms
All living things eventually die and return their carbon in an inorganic form The only exception to this are bogs which have large quantities of organic carbon which may be stored for years in the peat (dead plant matter)
Humans have modified the carbon cycle by releasing large quantities of organic carbon
Example mining coal burning fossil fuels and burning forests
Assignment
read pages 62-65 and do the assigned questions for the Carbon Cycle(handout)
Play the Carbon Cycle Game httpwwwwindowsucareduearthclimatecarbon_cyclehtml
Section 26-The Nitrogen and Phosphorus Cycles
The Nitrogen Cycle
Life depends on the cycling of nitrogen used by cells to make protein in plants and
animals
used to make DNA in plant and animal cells
used as fertilizer to make plants grow
The atmosphere is 79 nitrogen all of which is unusable by plants and animals
Nitrogen is changed into nitrates (usable form) by
lightning
nitrogen fixing bacteria
Nitrogen Fixation Through Lightning energy from the lightning causes nitrogen gas to
react with oxygen gas to produce nitrates
the nitrates dissolve in rain or surface water enter the soil and then move into plants through their roots
Nitrogen Fixation by Bacteria bacteria found in the soil provide the vast majority
of nitrates in the ecosystem Some bacteria may also be found in small lumps called nodules on the roots of some plants
called nitrogen fixing bacteria
Denitrification involves the decay process in which denitrifying bacteria break down nitrates into nitrites and then into nitrogen gas which goes up into the air
This process ensures the balance between soil nitrates nitrites and nitrogen gas
Denitrifying bacteria grow well in areas of low oxygen like lawns By aerating your lawn (adding more oxygen) the breakdown of nitrates into nitrogen gas is reduced and your lawn will stay green longer (nitrates stay in your lawn)
Nitrogen Cycle Animation
Assignment
Read pages 66-67 and complete the assigned questions for the Nitrogen Cycle(handout)
Play the Nitrogen Cycle Game httpwwwwindowsucaredutourlink=teach
er_resourcesteach_nitrogenhtml
The Phosphorus CyclePhosphorous cycles in two ways
Long term in rocks in the Earthrsquos crust phosphates eroded from rock are carried away by rivers and
lakes and end up in the ocean animals use the phosphates to make bones and shells when these animal die they end up at the bottom of the
ocean where over time they may become rock again Plants also absorb phosphates from the water
Short term in living organisms phosphates in dead organisms are recycled by
decomposers which break them down and release the phosphates back into the ecosystem
Phosphorus Cycle
Assignment
bullRead page 68 and complete the questions on the Phosphorus Cycle (handout)
Phosphorus Cycle Animation
Phosphorus Cycle
Section 22-Pesticides
Pesticides are chemicals used to kill insects weeds and microorganisms that might damage crops
Why Use Pesticides Up to 30 of crops in Canada are destroyed by pests This impacts the farmerrsquos income and the price that we pay for the produce
First Generation Pesticides
Pest control dates back to 500 BCE Toxic chemicals were frequently used until we discovered they were more dangerous to us than to the pests
Second Generation Pesticidesbull chemicals made in a lab
bull Can be grouped into four categories
Type Target Examples Persistence
Insecticide Insects DDT 2 - 15 years
Herbicide Weeds Roundup Days to weeks
Fungicide Moulds
and fungi Captan Days
Bactericides Bacteria Penicillin Days
Assignment
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Complete the sheet on histograms (handout)
Play the ldquoOh Deer Gamerdquohttpwwwriverventureorgcharlestonresourcespdfpopulation20study20gamepdf
Bioamplification
When water insoluble pesticides enter food chains the animals that eat them canrsquot break them down so they stay in their bodies The pesticides stay in the fatty tissue The pesticides then built up in a process called bioamplification
DDTbullDDT was the first modern pesticide developed to kill mosquitoes that spread malaria and typhus
bullIn 1962 an American activist named Rachel Carson published a book which alleged that DDT caused cancer and harmed bird reproduction This information led to the pesticide being banned in 1971
bullAlthough it is not being used in North America it is still being used in other countries and can be transmitted through bioamplification
DDT Video
Modern Chemical PesticidesNew pesticides are now water soluble and do not
build up in the tissues of animals They are safer but still have negative effects such as1 They break down quickly so they have to be spread
more often (cost more)
2 They are not selective so they can also kill birds reptiles amphibians and fish
3 Animals that do not die immediately may still put others at risk through bioamplification
4 They have a shelf life meaning that they become ineffective after a while
The Pests Fight Back Pests that reproduce often start to become
resistant to pesticides The first time using a chemical you will probably
kill 90 of the insects and the 10 that are left alive will reproduce
The 10 that survived probably had a natural resistance to the chemical Many of their offspring will also have the resistance After several generations the chemical is not as effective
New pesticides must be developed to take their place
Assignment
Read pages 52-57 and do questions 1-7 on page 58
Read pages 81-82 andmake a list of 4 pros and 4 cons for pesticide usage in controlling tentcaterpillars
Section 29-Monitoring Changes in Population
During the last three centuries global population has risen at an exponential rate
500 million in 16501 billion in 18502 billion in 19304 billion in 1975estimated at 8 billion in 2013
Population Growth Patterns Changes in population size occur when people
are added or removed from the population The four factors involved in population growth
are
1 Natality the number of offspring born in one year
2 Mortality the number of individuals that die in one year
3 Immigration the number of individuals moving into a population
4 Emigration the number of individuals moving out of a population
Population Growth = ( Births + Immigration) - ( Deaths + Emigration)
Open and Closed Populations
An open population occurs when all four factors are acting on the population
(Ex The population of Charlottetown)
A closed population occurs when only natality and mortality affect the population size
(Ex Population of the Earth)
Population Histogramsbulluseful when studying population of long-lived organisms such as humans
bullThe shape of pyramid allows you to predict changes in the populations
bullA wide base indicates that the population is rapidly growing
bull When the base is narrower than the middle section fewer offspring are produced and population will decline
Questions
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Section 210-Limits on Populations
Mice populations can change drastically in 6 months 20 mice can become 5120 mice
Why donrsquot we see billionsof mice when we lookout the window
The reason is that there are limitations on all populations including mice
Carrying Capacity
Populations fluctuate but tend to be fairly stable Stabilityhappens when the population does not exceed the carryingcapacity
Carrying Capacity - The maximum number of individual species that can be supported by an ecosystem
Law of Minimum - The nutrient in least supply is the one that limits growth
Law of Tolerance - An organism can survive within a certain range of abiotic factors Going above or below this range will cause death
Biotic potential is the maximum number of offspring that a species can produce if resources were unlimited
It is regulated by four factors
1) Birth potential maximum number of offspring per birth
2) Capacity of survival number of offspring that reach reproductive age
3) Procreation number of times a species reproduces each year
4) Length of reproductive life the age of sexual maturity and the number of years the individual can reproduce
Limiting Factors
The environment provides factors that prevent populations from attaining their biotic potential Environmental Factor Population Changes
Abiotic light temperaturechemical environment
Biotic Amount of foodnumber or effectiveness of predatorsdiseases and parasitesability to compete for resources
Some factors that control population can depend on the size or density of the population
A population is dense when a large number of organisms live in one area
Density IndependentFactors
Density DependentFactors
Flood Food shortage
Fire Competition for mates or habitat
Pesticides Diseases
Change in climate or temperature
Introduction of exotic species
Destruction of habitat Increased predation
Drought Competition for water and other resources
Questions
Read pages 77-80 and do questions 1 2 amp 3 (abc) on page 80
Chapter 3Sustaining Terrestrial Ecosystems
Section 31 Canadian Biomes
Jigsaw Activity
bull In groups you will be using pages 88-93 to complete the sheets on ldquoThe Canadian Biomesrdquo
bull Video Response Biomes (Earth at Risk Series)
Canadian Biomes Biome ndash a collection of ecosystems that are
similar or related to each other usually in the type of plants they support
Four Canadian Biomes
The Tundra The Boreal Forest The Temperate Deciduous
Forest The Grassland
Tundra
Boreal Forest
Grassland
Temperate Deciduous Forest
The Tundra- Canadarsquos northernmost biome
Biotic FactorsAbiotic Factors
very low temp for most
of the year
short growing season
Permafrost layer beneath the soil
low precipitation
poor soil quality
rapid-growing plants
mosses and lichens
caribou
ptarmigan
lemmings
arctic foxes
wolverines
Similar to a desert low precipitation (10-12 cmyear) supports a low number of species
Two layers of soil Permafrost ndash layer of soil that never thaws Active Layer ndash above permafrost thaws in summer allowing
roots to take in water and minerals
Decomposition of Organic Matter extremely slow in cold temp because cold keeps the
bacteria and fungi from reproducing This leaves only a small amount of organic material in the soil
Nitrogen and Carbon Cycles slows the rates of the cycles slow decomposition with surface water causes the
formation of bogs These store carbon for long periods of time and decrease denitrification
The Boreal Forest- Immediately south of the Tundra
Biotic FactorsAbiotic Factors
warmer than the Tundra
no permafrost
changeable weather
soils contains some water and is acidic
precipitation 40 cmyear or more
coniferous trees
seed-eating birds
squirrels
voles
snowshoe hare
deer
pine martens
grey wolves
Climate harsh with rapid changes in temp mixing warm and cool air results in
more precipitation
Soil warmer temp allows the soil to thaw every season higher organic matter from faster rates of decomposition soil is more acidic as coniferous needles produce acid when they decay
ndash this can limit the number of plants that can grow
What are conifers Trees with needle shaped leaves ndash evergreens
4 Reasons why conifers are dominant Thin needles have a small surface area so they lose little water during
winter Thick cuticle of wax covers the needles to reduce water loss and
protect from frost damage Pyramid shape of tree and flexible branches allow the tree to support
heavy snowfall Shed their leaves slowly throughout the year so they can begin
photosynthesis when the growing season begins (advantage in a short growing season)
The Temperate Deciduous Forest- South of the Boreal Forest in EasternCentral Canada
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp then Tundra or Boreal Forest
fertile soil
precipitation up to
100 cmyear
deciduous trees
many ferns and shrubs
tree and ground squirrels
many insects
shrews and mice
deer
woodpeckers
weasels black bears wolves
What are the dominant trees in
this biome Deciduous trees (maples oaks poplars
beech and birch)
What features about deciduous trees allow them to complete with conifers
The broad leaves maximize light capture for photosynthesis
Soil and Decomposition
higher temperatures allow for faster decomposition resulting in richer
soil
Understory and Canopy Understory ndash the lower branches of a trees
Canopy ndash the upper levels of the trees
What factors allow for high biodiversity in this biome
The presence of so many different kinds of plants supports many
animals
The thick litter layer is ideal for different insects
Many insects support amphibians lizards birds and insect-eating animals
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
Section 21 - Cycling of Matter in Ecosystems
Types of Matter
bull ORGANIC MATTER containsbull Carbonbull Hydrogenbull Sometimes Oxygenbull Sometimes Nitrogenbull Examples include proteins sugars and fats
bull INORGANIC MATTER does not containbull carbon and hydrogenbull Examples include carbon dioxide (CO2) water (H2O) and ammonia (NH3)
Cycling of Organic Matter
Organic Matter is continuously being recycled
Living organisms are made up of organic matter There is a limited amount on the Earth so it must be recycled for life to continue
Example Carbon molecules are recycled over and over This means that it is possible that your body contains a carbon molecule which was part of a dinosaur from 70 million years ago
Food is organic matter that was once part of a living thing
Digestion breaks down organic molecules which areused by your cells
Decay is when decomposer organisms breakdown organic materials (dead bodies and feces) and make it available to other living organisms
Fruit and Vegetable Decay
Sample Food Chain
Plant
Rabbit
Fox (feces)
Soil Bacteria (Decomposers)
Inorganic Molecules
Inorganic nutrients
Plant
Assignment
read pages 50-51 and do questions 1 2 5 amp 6 on page 51
Section 25-The Carbon Cycle
Carbon is the key element for living things
Carbon can be found in
1 The atmosphere (CO2)
2 Ocean (dissolved)
3 Plants (sugar C6H12O6)
4 Animals (protein)
5 Soil and rocks
The Carbon Cycle As carbon moves through the ecosystem it is
changed from one form to another
In Plants PHOTOSYNTHESISsunlight
CO2 + H2O C6H12O6 + O2
(Carbon dioxide + water glucose + oxygen)
In Animals CELLULAR RESPIRATION
C6H12O6 + O2 CO2 + H2O
The relationship between photosynthesis and cellular respiration is called the carbon cycle
Photosynthesis is the process in which plants use solar energy carbon dioxide from the atmosphere and water from the soil to make sugar
Cellular Respiration uses sugar and oxygen for energy and releases carbon dioxide back into the environment
The Carbon Cycle
Carbon ReservoirsReservoirs of Inorganic Carbon When carbon is not in organic form it can be found in three
types of storage (reservoirs)
Atmosphere (smallest ~ 003) Oceans (largest) Earthrsquos crust
Reservoirs for Organic Carbon Organic carbon is held in the bodies of living organisms
All living things eventually die and return their carbon in an inorganic form The only exception to this are bogs which have large quantities of organic carbon which may be stored for years in the peat (dead plant matter)
Humans have modified the carbon cycle by releasing large quantities of organic carbon
Example mining coal burning fossil fuels and burning forests
Assignment
read pages 62-65 and do the assigned questions for the Carbon Cycle(handout)
Play the Carbon Cycle Game httpwwwwindowsucareduearthclimatecarbon_cyclehtml
Section 26-The Nitrogen and Phosphorus Cycles
The Nitrogen Cycle
Life depends on the cycling of nitrogen used by cells to make protein in plants and
animals
used to make DNA in plant and animal cells
used as fertilizer to make plants grow
The atmosphere is 79 nitrogen all of which is unusable by plants and animals
Nitrogen is changed into nitrates (usable form) by
lightning
nitrogen fixing bacteria
Nitrogen Fixation Through Lightning energy from the lightning causes nitrogen gas to
react with oxygen gas to produce nitrates
the nitrates dissolve in rain or surface water enter the soil and then move into plants through their roots
Nitrogen Fixation by Bacteria bacteria found in the soil provide the vast majority
of nitrates in the ecosystem Some bacteria may also be found in small lumps called nodules on the roots of some plants
called nitrogen fixing bacteria
Denitrification involves the decay process in which denitrifying bacteria break down nitrates into nitrites and then into nitrogen gas which goes up into the air
This process ensures the balance between soil nitrates nitrites and nitrogen gas
Denitrifying bacteria grow well in areas of low oxygen like lawns By aerating your lawn (adding more oxygen) the breakdown of nitrates into nitrogen gas is reduced and your lawn will stay green longer (nitrates stay in your lawn)
Nitrogen Cycle Animation
Assignment
Read pages 66-67 and complete the assigned questions for the Nitrogen Cycle(handout)
Play the Nitrogen Cycle Game httpwwwwindowsucaredutourlink=teach
er_resourcesteach_nitrogenhtml
The Phosphorus CyclePhosphorous cycles in two ways
Long term in rocks in the Earthrsquos crust phosphates eroded from rock are carried away by rivers and
lakes and end up in the ocean animals use the phosphates to make bones and shells when these animal die they end up at the bottom of the
ocean where over time they may become rock again Plants also absorb phosphates from the water
Short term in living organisms phosphates in dead organisms are recycled by
decomposers which break them down and release the phosphates back into the ecosystem
Phosphorus Cycle
Assignment
bullRead page 68 and complete the questions on the Phosphorus Cycle (handout)
Phosphorus Cycle Animation
Phosphorus Cycle
Section 22-Pesticides
Pesticides are chemicals used to kill insects weeds and microorganisms that might damage crops
Why Use Pesticides Up to 30 of crops in Canada are destroyed by pests This impacts the farmerrsquos income and the price that we pay for the produce
First Generation Pesticides
Pest control dates back to 500 BCE Toxic chemicals were frequently used until we discovered they were more dangerous to us than to the pests
Second Generation Pesticidesbull chemicals made in a lab
bull Can be grouped into four categories
Type Target Examples Persistence
Insecticide Insects DDT 2 - 15 years
Herbicide Weeds Roundup Days to weeks
Fungicide Moulds
and fungi Captan Days
Bactericides Bacteria Penicillin Days
Assignment
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Complete the sheet on histograms (handout)
Play the ldquoOh Deer Gamerdquohttpwwwriverventureorgcharlestonresourcespdfpopulation20study20gamepdf
Bioamplification
When water insoluble pesticides enter food chains the animals that eat them canrsquot break them down so they stay in their bodies The pesticides stay in the fatty tissue The pesticides then built up in a process called bioamplification
DDTbullDDT was the first modern pesticide developed to kill mosquitoes that spread malaria and typhus
bullIn 1962 an American activist named Rachel Carson published a book which alleged that DDT caused cancer and harmed bird reproduction This information led to the pesticide being banned in 1971
bullAlthough it is not being used in North America it is still being used in other countries and can be transmitted through bioamplification
DDT Video
Modern Chemical PesticidesNew pesticides are now water soluble and do not
build up in the tissues of animals They are safer but still have negative effects such as1 They break down quickly so they have to be spread
more often (cost more)
2 They are not selective so they can also kill birds reptiles amphibians and fish
3 Animals that do not die immediately may still put others at risk through bioamplification
4 They have a shelf life meaning that they become ineffective after a while
The Pests Fight Back Pests that reproduce often start to become
resistant to pesticides The first time using a chemical you will probably
kill 90 of the insects and the 10 that are left alive will reproduce
The 10 that survived probably had a natural resistance to the chemical Many of their offspring will also have the resistance After several generations the chemical is not as effective
New pesticides must be developed to take their place
Assignment
Read pages 52-57 and do questions 1-7 on page 58
Read pages 81-82 andmake a list of 4 pros and 4 cons for pesticide usage in controlling tentcaterpillars
Section 29-Monitoring Changes in Population
During the last three centuries global population has risen at an exponential rate
500 million in 16501 billion in 18502 billion in 19304 billion in 1975estimated at 8 billion in 2013
Population Growth Patterns Changes in population size occur when people
are added or removed from the population The four factors involved in population growth
are
1 Natality the number of offspring born in one year
2 Mortality the number of individuals that die in one year
3 Immigration the number of individuals moving into a population
4 Emigration the number of individuals moving out of a population
Population Growth = ( Births + Immigration) - ( Deaths + Emigration)
Open and Closed Populations
An open population occurs when all four factors are acting on the population
(Ex The population of Charlottetown)
A closed population occurs when only natality and mortality affect the population size
(Ex Population of the Earth)
Population Histogramsbulluseful when studying population of long-lived organisms such as humans
bullThe shape of pyramid allows you to predict changes in the populations
bullA wide base indicates that the population is rapidly growing
bull When the base is narrower than the middle section fewer offspring are produced and population will decline
Questions
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Section 210-Limits on Populations
Mice populations can change drastically in 6 months 20 mice can become 5120 mice
Why donrsquot we see billionsof mice when we lookout the window
The reason is that there are limitations on all populations including mice
Carrying Capacity
Populations fluctuate but tend to be fairly stable Stabilityhappens when the population does not exceed the carryingcapacity
Carrying Capacity - The maximum number of individual species that can be supported by an ecosystem
Law of Minimum - The nutrient in least supply is the one that limits growth
Law of Tolerance - An organism can survive within a certain range of abiotic factors Going above or below this range will cause death
Biotic potential is the maximum number of offspring that a species can produce if resources were unlimited
It is regulated by four factors
1) Birth potential maximum number of offspring per birth
2) Capacity of survival number of offspring that reach reproductive age
3) Procreation number of times a species reproduces each year
4) Length of reproductive life the age of sexual maturity and the number of years the individual can reproduce
Limiting Factors
The environment provides factors that prevent populations from attaining their biotic potential Environmental Factor Population Changes
Abiotic light temperaturechemical environment
Biotic Amount of foodnumber or effectiveness of predatorsdiseases and parasitesability to compete for resources
Some factors that control population can depend on the size or density of the population
A population is dense when a large number of organisms live in one area
Density IndependentFactors
Density DependentFactors
Flood Food shortage
Fire Competition for mates or habitat
Pesticides Diseases
Change in climate or temperature
Introduction of exotic species
Destruction of habitat Increased predation
Drought Competition for water and other resources
Questions
Read pages 77-80 and do questions 1 2 amp 3 (abc) on page 80
Chapter 3Sustaining Terrestrial Ecosystems
Section 31 Canadian Biomes
Jigsaw Activity
bull In groups you will be using pages 88-93 to complete the sheets on ldquoThe Canadian Biomesrdquo
bull Video Response Biomes (Earth at Risk Series)
Canadian Biomes Biome ndash a collection of ecosystems that are
similar or related to each other usually in the type of plants they support
Four Canadian Biomes
The Tundra The Boreal Forest The Temperate Deciduous
Forest The Grassland
Tundra
Boreal Forest
Grassland
Temperate Deciduous Forest
The Tundra- Canadarsquos northernmost biome
Biotic FactorsAbiotic Factors
very low temp for most
of the year
short growing season
Permafrost layer beneath the soil
low precipitation
poor soil quality
rapid-growing plants
mosses and lichens
caribou
ptarmigan
lemmings
arctic foxes
wolverines
Similar to a desert low precipitation (10-12 cmyear) supports a low number of species
Two layers of soil Permafrost ndash layer of soil that never thaws Active Layer ndash above permafrost thaws in summer allowing
roots to take in water and minerals
Decomposition of Organic Matter extremely slow in cold temp because cold keeps the
bacteria and fungi from reproducing This leaves only a small amount of organic material in the soil
Nitrogen and Carbon Cycles slows the rates of the cycles slow decomposition with surface water causes the
formation of bogs These store carbon for long periods of time and decrease denitrification
The Boreal Forest- Immediately south of the Tundra
Biotic FactorsAbiotic Factors
warmer than the Tundra
no permafrost
changeable weather
soils contains some water and is acidic
precipitation 40 cmyear or more
coniferous trees
seed-eating birds
squirrels
voles
snowshoe hare
deer
pine martens
grey wolves
Climate harsh with rapid changes in temp mixing warm and cool air results in
more precipitation
Soil warmer temp allows the soil to thaw every season higher organic matter from faster rates of decomposition soil is more acidic as coniferous needles produce acid when they decay
ndash this can limit the number of plants that can grow
What are conifers Trees with needle shaped leaves ndash evergreens
4 Reasons why conifers are dominant Thin needles have a small surface area so they lose little water during
winter Thick cuticle of wax covers the needles to reduce water loss and
protect from frost damage Pyramid shape of tree and flexible branches allow the tree to support
heavy snowfall Shed their leaves slowly throughout the year so they can begin
photosynthesis when the growing season begins (advantage in a short growing season)
The Temperate Deciduous Forest- South of the Boreal Forest in EasternCentral Canada
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp then Tundra or Boreal Forest
fertile soil
precipitation up to
100 cmyear
deciduous trees
many ferns and shrubs
tree and ground squirrels
many insects
shrews and mice
deer
woodpeckers
weasels black bears wolves
What are the dominant trees in
this biome Deciduous trees (maples oaks poplars
beech and birch)
What features about deciduous trees allow them to complete with conifers
The broad leaves maximize light capture for photosynthesis
Soil and Decomposition
higher temperatures allow for faster decomposition resulting in richer
soil
Understory and Canopy Understory ndash the lower branches of a trees
Canopy ndash the upper levels of the trees
What factors allow for high biodiversity in this biome
The presence of so many different kinds of plants supports many
animals
The thick litter layer is ideal for different insects
Many insects support amphibians lizards birds and insect-eating animals
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
Cycling of Organic Matter
Organic Matter is continuously being recycled
Living organisms are made up of organic matter There is a limited amount on the Earth so it must be recycled for life to continue
Example Carbon molecules are recycled over and over This means that it is possible that your body contains a carbon molecule which was part of a dinosaur from 70 million years ago
Food is organic matter that was once part of a living thing
Digestion breaks down organic molecules which areused by your cells
Decay is when decomposer organisms breakdown organic materials (dead bodies and feces) and make it available to other living organisms
Fruit and Vegetable Decay
Sample Food Chain
Plant
Rabbit
Fox (feces)
Soil Bacteria (Decomposers)
Inorganic Molecules
Inorganic nutrients
Plant
Assignment
read pages 50-51 and do questions 1 2 5 amp 6 on page 51
Section 25-The Carbon Cycle
Carbon is the key element for living things
Carbon can be found in
1 The atmosphere (CO2)
2 Ocean (dissolved)
3 Plants (sugar C6H12O6)
4 Animals (protein)
5 Soil and rocks
The Carbon Cycle As carbon moves through the ecosystem it is
changed from one form to another
In Plants PHOTOSYNTHESISsunlight
CO2 + H2O C6H12O6 + O2
(Carbon dioxide + water glucose + oxygen)
In Animals CELLULAR RESPIRATION
C6H12O6 + O2 CO2 + H2O
The relationship between photosynthesis and cellular respiration is called the carbon cycle
Photosynthesis is the process in which plants use solar energy carbon dioxide from the atmosphere and water from the soil to make sugar
Cellular Respiration uses sugar and oxygen for energy and releases carbon dioxide back into the environment
The Carbon Cycle
Carbon ReservoirsReservoirs of Inorganic Carbon When carbon is not in organic form it can be found in three
types of storage (reservoirs)
Atmosphere (smallest ~ 003) Oceans (largest) Earthrsquos crust
Reservoirs for Organic Carbon Organic carbon is held in the bodies of living organisms
All living things eventually die and return their carbon in an inorganic form The only exception to this are bogs which have large quantities of organic carbon which may be stored for years in the peat (dead plant matter)
Humans have modified the carbon cycle by releasing large quantities of organic carbon
Example mining coal burning fossil fuels and burning forests
Assignment
read pages 62-65 and do the assigned questions for the Carbon Cycle(handout)
Play the Carbon Cycle Game httpwwwwindowsucareduearthclimatecarbon_cyclehtml
Section 26-The Nitrogen and Phosphorus Cycles
The Nitrogen Cycle
Life depends on the cycling of nitrogen used by cells to make protein in plants and
animals
used to make DNA in plant and animal cells
used as fertilizer to make plants grow
The atmosphere is 79 nitrogen all of which is unusable by plants and animals
Nitrogen is changed into nitrates (usable form) by
lightning
nitrogen fixing bacteria
Nitrogen Fixation Through Lightning energy from the lightning causes nitrogen gas to
react with oxygen gas to produce nitrates
the nitrates dissolve in rain or surface water enter the soil and then move into plants through their roots
Nitrogen Fixation by Bacteria bacteria found in the soil provide the vast majority
of nitrates in the ecosystem Some bacteria may also be found in small lumps called nodules on the roots of some plants
called nitrogen fixing bacteria
Denitrification involves the decay process in which denitrifying bacteria break down nitrates into nitrites and then into nitrogen gas which goes up into the air
This process ensures the balance between soil nitrates nitrites and nitrogen gas
Denitrifying bacteria grow well in areas of low oxygen like lawns By aerating your lawn (adding more oxygen) the breakdown of nitrates into nitrogen gas is reduced and your lawn will stay green longer (nitrates stay in your lawn)
Nitrogen Cycle Animation
Assignment
Read pages 66-67 and complete the assigned questions for the Nitrogen Cycle(handout)
Play the Nitrogen Cycle Game httpwwwwindowsucaredutourlink=teach
er_resourcesteach_nitrogenhtml
The Phosphorus CyclePhosphorous cycles in two ways
Long term in rocks in the Earthrsquos crust phosphates eroded from rock are carried away by rivers and
lakes and end up in the ocean animals use the phosphates to make bones and shells when these animal die they end up at the bottom of the
ocean where over time they may become rock again Plants also absorb phosphates from the water
Short term in living organisms phosphates in dead organisms are recycled by
decomposers which break them down and release the phosphates back into the ecosystem
Phosphorus Cycle
Assignment
bullRead page 68 and complete the questions on the Phosphorus Cycle (handout)
Phosphorus Cycle Animation
Phosphorus Cycle
Section 22-Pesticides
Pesticides are chemicals used to kill insects weeds and microorganisms that might damage crops
Why Use Pesticides Up to 30 of crops in Canada are destroyed by pests This impacts the farmerrsquos income and the price that we pay for the produce
First Generation Pesticides
Pest control dates back to 500 BCE Toxic chemicals were frequently used until we discovered they were more dangerous to us than to the pests
Second Generation Pesticidesbull chemicals made in a lab
bull Can be grouped into four categories
Type Target Examples Persistence
Insecticide Insects DDT 2 - 15 years
Herbicide Weeds Roundup Days to weeks
Fungicide Moulds
and fungi Captan Days
Bactericides Bacteria Penicillin Days
Assignment
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Complete the sheet on histograms (handout)
Play the ldquoOh Deer Gamerdquohttpwwwriverventureorgcharlestonresourcespdfpopulation20study20gamepdf
Bioamplification
When water insoluble pesticides enter food chains the animals that eat them canrsquot break them down so they stay in their bodies The pesticides stay in the fatty tissue The pesticides then built up in a process called bioamplification
DDTbullDDT was the first modern pesticide developed to kill mosquitoes that spread malaria and typhus
bullIn 1962 an American activist named Rachel Carson published a book which alleged that DDT caused cancer and harmed bird reproduction This information led to the pesticide being banned in 1971
bullAlthough it is not being used in North America it is still being used in other countries and can be transmitted through bioamplification
DDT Video
Modern Chemical PesticidesNew pesticides are now water soluble and do not
build up in the tissues of animals They are safer but still have negative effects such as1 They break down quickly so they have to be spread
more often (cost more)
2 They are not selective so they can also kill birds reptiles amphibians and fish
3 Animals that do not die immediately may still put others at risk through bioamplification
4 They have a shelf life meaning that they become ineffective after a while
The Pests Fight Back Pests that reproduce often start to become
resistant to pesticides The first time using a chemical you will probably
kill 90 of the insects and the 10 that are left alive will reproduce
The 10 that survived probably had a natural resistance to the chemical Many of their offspring will also have the resistance After several generations the chemical is not as effective
New pesticides must be developed to take their place
Assignment
Read pages 52-57 and do questions 1-7 on page 58
Read pages 81-82 andmake a list of 4 pros and 4 cons for pesticide usage in controlling tentcaterpillars
Section 29-Monitoring Changes in Population
During the last three centuries global population has risen at an exponential rate
500 million in 16501 billion in 18502 billion in 19304 billion in 1975estimated at 8 billion in 2013
Population Growth Patterns Changes in population size occur when people
are added or removed from the population The four factors involved in population growth
are
1 Natality the number of offspring born in one year
2 Mortality the number of individuals that die in one year
3 Immigration the number of individuals moving into a population
4 Emigration the number of individuals moving out of a population
Population Growth = ( Births + Immigration) - ( Deaths + Emigration)
Open and Closed Populations
An open population occurs when all four factors are acting on the population
(Ex The population of Charlottetown)
A closed population occurs when only natality and mortality affect the population size
(Ex Population of the Earth)
Population Histogramsbulluseful when studying population of long-lived organisms such as humans
bullThe shape of pyramid allows you to predict changes in the populations
bullA wide base indicates that the population is rapidly growing
bull When the base is narrower than the middle section fewer offspring are produced and population will decline
Questions
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Section 210-Limits on Populations
Mice populations can change drastically in 6 months 20 mice can become 5120 mice
Why donrsquot we see billionsof mice when we lookout the window
The reason is that there are limitations on all populations including mice
Carrying Capacity
Populations fluctuate but tend to be fairly stable Stabilityhappens when the population does not exceed the carryingcapacity
Carrying Capacity - The maximum number of individual species that can be supported by an ecosystem
Law of Minimum - The nutrient in least supply is the one that limits growth
Law of Tolerance - An organism can survive within a certain range of abiotic factors Going above or below this range will cause death
Biotic potential is the maximum number of offspring that a species can produce if resources were unlimited
It is regulated by four factors
1) Birth potential maximum number of offspring per birth
2) Capacity of survival number of offspring that reach reproductive age
3) Procreation number of times a species reproduces each year
4) Length of reproductive life the age of sexual maturity and the number of years the individual can reproduce
Limiting Factors
The environment provides factors that prevent populations from attaining their biotic potential Environmental Factor Population Changes
Abiotic light temperaturechemical environment
Biotic Amount of foodnumber or effectiveness of predatorsdiseases and parasitesability to compete for resources
Some factors that control population can depend on the size or density of the population
A population is dense when a large number of organisms live in one area
Density IndependentFactors
Density DependentFactors
Flood Food shortage
Fire Competition for mates or habitat
Pesticides Diseases
Change in climate or temperature
Introduction of exotic species
Destruction of habitat Increased predation
Drought Competition for water and other resources
Questions
Read pages 77-80 and do questions 1 2 amp 3 (abc) on page 80
Chapter 3Sustaining Terrestrial Ecosystems
Section 31 Canadian Biomes
Jigsaw Activity
bull In groups you will be using pages 88-93 to complete the sheets on ldquoThe Canadian Biomesrdquo
bull Video Response Biomes (Earth at Risk Series)
Canadian Biomes Biome ndash a collection of ecosystems that are
similar or related to each other usually in the type of plants they support
Four Canadian Biomes
The Tundra The Boreal Forest The Temperate Deciduous
Forest The Grassland
Tundra
Boreal Forest
Grassland
Temperate Deciduous Forest
The Tundra- Canadarsquos northernmost biome
Biotic FactorsAbiotic Factors
very low temp for most
of the year
short growing season
Permafrost layer beneath the soil
low precipitation
poor soil quality
rapid-growing plants
mosses and lichens
caribou
ptarmigan
lemmings
arctic foxes
wolverines
Similar to a desert low precipitation (10-12 cmyear) supports a low number of species
Two layers of soil Permafrost ndash layer of soil that never thaws Active Layer ndash above permafrost thaws in summer allowing
roots to take in water and minerals
Decomposition of Organic Matter extremely slow in cold temp because cold keeps the
bacteria and fungi from reproducing This leaves only a small amount of organic material in the soil
Nitrogen and Carbon Cycles slows the rates of the cycles slow decomposition with surface water causes the
formation of bogs These store carbon for long periods of time and decrease denitrification
The Boreal Forest- Immediately south of the Tundra
Biotic FactorsAbiotic Factors
warmer than the Tundra
no permafrost
changeable weather
soils contains some water and is acidic
precipitation 40 cmyear or more
coniferous trees
seed-eating birds
squirrels
voles
snowshoe hare
deer
pine martens
grey wolves
Climate harsh with rapid changes in temp mixing warm and cool air results in
more precipitation
Soil warmer temp allows the soil to thaw every season higher organic matter from faster rates of decomposition soil is more acidic as coniferous needles produce acid when they decay
ndash this can limit the number of plants that can grow
What are conifers Trees with needle shaped leaves ndash evergreens
4 Reasons why conifers are dominant Thin needles have a small surface area so they lose little water during
winter Thick cuticle of wax covers the needles to reduce water loss and
protect from frost damage Pyramid shape of tree and flexible branches allow the tree to support
heavy snowfall Shed their leaves slowly throughout the year so they can begin
photosynthesis when the growing season begins (advantage in a short growing season)
The Temperate Deciduous Forest- South of the Boreal Forest in EasternCentral Canada
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp then Tundra or Boreal Forest
fertile soil
precipitation up to
100 cmyear
deciduous trees
many ferns and shrubs
tree and ground squirrels
many insects
shrews and mice
deer
woodpeckers
weasels black bears wolves
What are the dominant trees in
this biome Deciduous trees (maples oaks poplars
beech and birch)
What features about deciduous trees allow them to complete with conifers
The broad leaves maximize light capture for photosynthesis
Soil and Decomposition
higher temperatures allow for faster decomposition resulting in richer
soil
Understory and Canopy Understory ndash the lower branches of a trees
Canopy ndash the upper levels of the trees
What factors allow for high biodiversity in this biome
The presence of so many different kinds of plants supports many
animals
The thick litter layer is ideal for different insects
Many insects support amphibians lizards birds and insect-eating animals
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
Food is organic matter that was once part of a living thing
Digestion breaks down organic molecules which areused by your cells
Decay is when decomposer organisms breakdown organic materials (dead bodies and feces) and make it available to other living organisms
Fruit and Vegetable Decay
Sample Food Chain
Plant
Rabbit
Fox (feces)
Soil Bacteria (Decomposers)
Inorganic Molecules
Inorganic nutrients
Plant
Assignment
read pages 50-51 and do questions 1 2 5 amp 6 on page 51
Section 25-The Carbon Cycle
Carbon is the key element for living things
Carbon can be found in
1 The atmosphere (CO2)
2 Ocean (dissolved)
3 Plants (sugar C6H12O6)
4 Animals (protein)
5 Soil and rocks
The Carbon Cycle As carbon moves through the ecosystem it is
changed from one form to another
In Plants PHOTOSYNTHESISsunlight
CO2 + H2O C6H12O6 + O2
(Carbon dioxide + water glucose + oxygen)
In Animals CELLULAR RESPIRATION
C6H12O6 + O2 CO2 + H2O
The relationship between photosynthesis and cellular respiration is called the carbon cycle
Photosynthesis is the process in which plants use solar energy carbon dioxide from the atmosphere and water from the soil to make sugar
Cellular Respiration uses sugar and oxygen for energy and releases carbon dioxide back into the environment
The Carbon Cycle
Carbon ReservoirsReservoirs of Inorganic Carbon When carbon is not in organic form it can be found in three
types of storage (reservoirs)
Atmosphere (smallest ~ 003) Oceans (largest) Earthrsquos crust
Reservoirs for Organic Carbon Organic carbon is held in the bodies of living organisms
All living things eventually die and return their carbon in an inorganic form The only exception to this are bogs which have large quantities of organic carbon which may be stored for years in the peat (dead plant matter)
Humans have modified the carbon cycle by releasing large quantities of organic carbon
Example mining coal burning fossil fuels and burning forests
Assignment
read pages 62-65 and do the assigned questions for the Carbon Cycle(handout)
Play the Carbon Cycle Game httpwwwwindowsucareduearthclimatecarbon_cyclehtml
Section 26-The Nitrogen and Phosphorus Cycles
The Nitrogen Cycle
Life depends on the cycling of nitrogen used by cells to make protein in plants and
animals
used to make DNA in plant and animal cells
used as fertilizer to make plants grow
The atmosphere is 79 nitrogen all of which is unusable by plants and animals
Nitrogen is changed into nitrates (usable form) by
lightning
nitrogen fixing bacteria
Nitrogen Fixation Through Lightning energy from the lightning causes nitrogen gas to
react with oxygen gas to produce nitrates
the nitrates dissolve in rain or surface water enter the soil and then move into plants through their roots
Nitrogen Fixation by Bacteria bacteria found in the soil provide the vast majority
of nitrates in the ecosystem Some bacteria may also be found in small lumps called nodules on the roots of some plants
called nitrogen fixing bacteria
Denitrification involves the decay process in which denitrifying bacteria break down nitrates into nitrites and then into nitrogen gas which goes up into the air
This process ensures the balance between soil nitrates nitrites and nitrogen gas
Denitrifying bacteria grow well in areas of low oxygen like lawns By aerating your lawn (adding more oxygen) the breakdown of nitrates into nitrogen gas is reduced and your lawn will stay green longer (nitrates stay in your lawn)
Nitrogen Cycle Animation
Assignment
Read pages 66-67 and complete the assigned questions for the Nitrogen Cycle(handout)
Play the Nitrogen Cycle Game httpwwwwindowsucaredutourlink=teach
er_resourcesteach_nitrogenhtml
The Phosphorus CyclePhosphorous cycles in two ways
Long term in rocks in the Earthrsquos crust phosphates eroded from rock are carried away by rivers and
lakes and end up in the ocean animals use the phosphates to make bones and shells when these animal die they end up at the bottom of the
ocean where over time they may become rock again Plants also absorb phosphates from the water
Short term in living organisms phosphates in dead organisms are recycled by
decomposers which break them down and release the phosphates back into the ecosystem
Phosphorus Cycle
Assignment
bullRead page 68 and complete the questions on the Phosphorus Cycle (handout)
Phosphorus Cycle Animation
Phosphorus Cycle
Section 22-Pesticides
Pesticides are chemicals used to kill insects weeds and microorganisms that might damage crops
Why Use Pesticides Up to 30 of crops in Canada are destroyed by pests This impacts the farmerrsquos income and the price that we pay for the produce
First Generation Pesticides
Pest control dates back to 500 BCE Toxic chemicals were frequently used until we discovered they were more dangerous to us than to the pests
Second Generation Pesticidesbull chemicals made in a lab
bull Can be grouped into four categories
Type Target Examples Persistence
Insecticide Insects DDT 2 - 15 years
Herbicide Weeds Roundup Days to weeks
Fungicide Moulds
and fungi Captan Days
Bactericides Bacteria Penicillin Days
Assignment
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Complete the sheet on histograms (handout)
Play the ldquoOh Deer Gamerdquohttpwwwriverventureorgcharlestonresourcespdfpopulation20study20gamepdf
Bioamplification
When water insoluble pesticides enter food chains the animals that eat them canrsquot break them down so they stay in their bodies The pesticides stay in the fatty tissue The pesticides then built up in a process called bioamplification
DDTbullDDT was the first modern pesticide developed to kill mosquitoes that spread malaria and typhus
bullIn 1962 an American activist named Rachel Carson published a book which alleged that DDT caused cancer and harmed bird reproduction This information led to the pesticide being banned in 1971
bullAlthough it is not being used in North America it is still being used in other countries and can be transmitted through bioamplification
DDT Video
Modern Chemical PesticidesNew pesticides are now water soluble and do not
build up in the tissues of animals They are safer but still have negative effects such as1 They break down quickly so they have to be spread
more often (cost more)
2 They are not selective so they can also kill birds reptiles amphibians and fish
3 Animals that do not die immediately may still put others at risk through bioamplification
4 They have a shelf life meaning that they become ineffective after a while
The Pests Fight Back Pests that reproduce often start to become
resistant to pesticides The first time using a chemical you will probably
kill 90 of the insects and the 10 that are left alive will reproduce
The 10 that survived probably had a natural resistance to the chemical Many of their offspring will also have the resistance After several generations the chemical is not as effective
New pesticides must be developed to take their place
Assignment
Read pages 52-57 and do questions 1-7 on page 58
Read pages 81-82 andmake a list of 4 pros and 4 cons for pesticide usage in controlling tentcaterpillars
Section 29-Monitoring Changes in Population
During the last three centuries global population has risen at an exponential rate
500 million in 16501 billion in 18502 billion in 19304 billion in 1975estimated at 8 billion in 2013
Population Growth Patterns Changes in population size occur when people
are added or removed from the population The four factors involved in population growth
are
1 Natality the number of offspring born in one year
2 Mortality the number of individuals that die in one year
3 Immigration the number of individuals moving into a population
4 Emigration the number of individuals moving out of a population
Population Growth = ( Births + Immigration) - ( Deaths + Emigration)
Open and Closed Populations
An open population occurs when all four factors are acting on the population
(Ex The population of Charlottetown)
A closed population occurs when only natality and mortality affect the population size
(Ex Population of the Earth)
Population Histogramsbulluseful when studying population of long-lived organisms such as humans
bullThe shape of pyramid allows you to predict changes in the populations
bullA wide base indicates that the population is rapidly growing
bull When the base is narrower than the middle section fewer offspring are produced and population will decline
Questions
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Section 210-Limits on Populations
Mice populations can change drastically in 6 months 20 mice can become 5120 mice
Why donrsquot we see billionsof mice when we lookout the window
The reason is that there are limitations on all populations including mice
Carrying Capacity
Populations fluctuate but tend to be fairly stable Stabilityhappens when the population does not exceed the carryingcapacity
Carrying Capacity - The maximum number of individual species that can be supported by an ecosystem
Law of Minimum - The nutrient in least supply is the one that limits growth
Law of Tolerance - An organism can survive within a certain range of abiotic factors Going above or below this range will cause death
Biotic potential is the maximum number of offspring that a species can produce if resources were unlimited
It is regulated by four factors
1) Birth potential maximum number of offspring per birth
2) Capacity of survival number of offspring that reach reproductive age
3) Procreation number of times a species reproduces each year
4) Length of reproductive life the age of sexual maturity and the number of years the individual can reproduce
Limiting Factors
The environment provides factors that prevent populations from attaining their biotic potential Environmental Factor Population Changes
Abiotic light temperaturechemical environment
Biotic Amount of foodnumber or effectiveness of predatorsdiseases and parasitesability to compete for resources
Some factors that control population can depend on the size or density of the population
A population is dense when a large number of organisms live in one area
Density IndependentFactors
Density DependentFactors
Flood Food shortage
Fire Competition for mates or habitat
Pesticides Diseases
Change in climate or temperature
Introduction of exotic species
Destruction of habitat Increased predation
Drought Competition for water and other resources
Questions
Read pages 77-80 and do questions 1 2 amp 3 (abc) on page 80
Chapter 3Sustaining Terrestrial Ecosystems
Section 31 Canadian Biomes
Jigsaw Activity
bull In groups you will be using pages 88-93 to complete the sheets on ldquoThe Canadian Biomesrdquo
bull Video Response Biomes (Earth at Risk Series)
Canadian Biomes Biome ndash a collection of ecosystems that are
similar or related to each other usually in the type of plants they support
Four Canadian Biomes
The Tundra The Boreal Forest The Temperate Deciduous
Forest The Grassland
Tundra
Boreal Forest
Grassland
Temperate Deciduous Forest
The Tundra- Canadarsquos northernmost biome
Biotic FactorsAbiotic Factors
very low temp for most
of the year
short growing season
Permafrost layer beneath the soil
low precipitation
poor soil quality
rapid-growing plants
mosses and lichens
caribou
ptarmigan
lemmings
arctic foxes
wolverines
Similar to a desert low precipitation (10-12 cmyear) supports a low number of species
Two layers of soil Permafrost ndash layer of soil that never thaws Active Layer ndash above permafrost thaws in summer allowing
roots to take in water and minerals
Decomposition of Organic Matter extremely slow in cold temp because cold keeps the
bacteria and fungi from reproducing This leaves only a small amount of organic material in the soil
Nitrogen and Carbon Cycles slows the rates of the cycles slow decomposition with surface water causes the
formation of bogs These store carbon for long periods of time and decrease denitrification
The Boreal Forest- Immediately south of the Tundra
Biotic FactorsAbiotic Factors
warmer than the Tundra
no permafrost
changeable weather
soils contains some water and is acidic
precipitation 40 cmyear or more
coniferous trees
seed-eating birds
squirrels
voles
snowshoe hare
deer
pine martens
grey wolves
Climate harsh with rapid changes in temp mixing warm and cool air results in
more precipitation
Soil warmer temp allows the soil to thaw every season higher organic matter from faster rates of decomposition soil is more acidic as coniferous needles produce acid when they decay
ndash this can limit the number of plants that can grow
What are conifers Trees with needle shaped leaves ndash evergreens
4 Reasons why conifers are dominant Thin needles have a small surface area so they lose little water during
winter Thick cuticle of wax covers the needles to reduce water loss and
protect from frost damage Pyramid shape of tree and flexible branches allow the tree to support
heavy snowfall Shed their leaves slowly throughout the year so they can begin
photosynthesis when the growing season begins (advantage in a short growing season)
The Temperate Deciduous Forest- South of the Boreal Forest in EasternCentral Canada
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp then Tundra or Boreal Forest
fertile soil
precipitation up to
100 cmyear
deciduous trees
many ferns and shrubs
tree and ground squirrels
many insects
shrews and mice
deer
woodpeckers
weasels black bears wolves
What are the dominant trees in
this biome Deciduous trees (maples oaks poplars
beech and birch)
What features about deciduous trees allow them to complete with conifers
The broad leaves maximize light capture for photosynthesis
Soil and Decomposition
higher temperatures allow for faster decomposition resulting in richer
soil
Understory and Canopy Understory ndash the lower branches of a trees
Canopy ndash the upper levels of the trees
What factors allow for high biodiversity in this biome
The presence of so many different kinds of plants supports many
animals
The thick litter layer is ideal for different insects
Many insects support amphibians lizards birds and insect-eating animals
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
Sample Food Chain
Plant
Rabbit
Fox (feces)
Soil Bacteria (Decomposers)
Inorganic Molecules
Inorganic nutrients
Plant
Assignment
read pages 50-51 and do questions 1 2 5 amp 6 on page 51
Section 25-The Carbon Cycle
Carbon is the key element for living things
Carbon can be found in
1 The atmosphere (CO2)
2 Ocean (dissolved)
3 Plants (sugar C6H12O6)
4 Animals (protein)
5 Soil and rocks
The Carbon Cycle As carbon moves through the ecosystem it is
changed from one form to another
In Plants PHOTOSYNTHESISsunlight
CO2 + H2O C6H12O6 + O2
(Carbon dioxide + water glucose + oxygen)
In Animals CELLULAR RESPIRATION
C6H12O6 + O2 CO2 + H2O
The relationship between photosynthesis and cellular respiration is called the carbon cycle
Photosynthesis is the process in which plants use solar energy carbon dioxide from the atmosphere and water from the soil to make sugar
Cellular Respiration uses sugar and oxygen for energy and releases carbon dioxide back into the environment
The Carbon Cycle
Carbon ReservoirsReservoirs of Inorganic Carbon When carbon is not in organic form it can be found in three
types of storage (reservoirs)
Atmosphere (smallest ~ 003) Oceans (largest) Earthrsquos crust
Reservoirs for Organic Carbon Organic carbon is held in the bodies of living organisms
All living things eventually die and return their carbon in an inorganic form The only exception to this are bogs which have large quantities of organic carbon which may be stored for years in the peat (dead plant matter)
Humans have modified the carbon cycle by releasing large quantities of organic carbon
Example mining coal burning fossil fuels and burning forests
Assignment
read pages 62-65 and do the assigned questions for the Carbon Cycle(handout)
Play the Carbon Cycle Game httpwwwwindowsucareduearthclimatecarbon_cyclehtml
Section 26-The Nitrogen and Phosphorus Cycles
The Nitrogen Cycle
Life depends on the cycling of nitrogen used by cells to make protein in plants and
animals
used to make DNA in plant and animal cells
used as fertilizer to make plants grow
The atmosphere is 79 nitrogen all of which is unusable by plants and animals
Nitrogen is changed into nitrates (usable form) by
lightning
nitrogen fixing bacteria
Nitrogen Fixation Through Lightning energy from the lightning causes nitrogen gas to
react with oxygen gas to produce nitrates
the nitrates dissolve in rain or surface water enter the soil and then move into plants through their roots
Nitrogen Fixation by Bacteria bacteria found in the soil provide the vast majority
of nitrates in the ecosystem Some bacteria may also be found in small lumps called nodules on the roots of some plants
called nitrogen fixing bacteria
Denitrification involves the decay process in which denitrifying bacteria break down nitrates into nitrites and then into nitrogen gas which goes up into the air
This process ensures the balance between soil nitrates nitrites and nitrogen gas
Denitrifying bacteria grow well in areas of low oxygen like lawns By aerating your lawn (adding more oxygen) the breakdown of nitrates into nitrogen gas is reduced and your lawn will stay green longer (nitrates stay in your lawn)
Nitrogen Cycle Animation
Assignment
Read pages 66-67 and complete the assigned questions for the Nitrogen Cycle(handout)
Play the Nitrogen Cycle Game httpwwwwindowsucaredutourlink=teach
er_resourcesteach_nitrogenhtml
The Phosphorus CyclePhosphorous cycles in two ways
Long term in rocks in the Earthrsquos crust phosphates eroded from rock are carried away by rivers and
lakes and end up in the ocean animals use the phosphates to make bones and shells when these animal die they end up at the bottom of the
ocean where over time they may become rock again Plants also absorb phosphates from the water
Short term in living organisms phosphates in dead organisms are recycled by
decomposers which break them down and release the phosphates back into the ecosystem
Phosphorus Cycle
Assignment
bullRead page 68 and complete the questions on the Phosphorus Cycle (handout)
Phosphorus Cycle Animation
Phosphorus Cycle
Section 22-Pesticides
Pesticides are chemicals used to kill insects weeds and microorganisms that might damage crops
Why Use Pesticides Up to 30 of crops in Canada are destroyed by pests This impacts the farmerrsquos income and the price that we pay for the produce
First Generation Pesticides
Pest control dates back to 500 BCE Toxic chemicals were frequently used until we discovered they were more dangerous to us than to the pests
Second Generation Pesticidesbull chemicals made in a lab
bull Can be grouped into four categories
Type Target Examples Persistence
Insecticide Insects DDT 2 - 15 years
Herbicide Weeds Roundup Days to weeks
Fungicide Moulds
and fungi Captan Days
Bactericides Bacteria Penicillin Days
Assignment
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Complete the sheet on histograms (handout)
Play the ldquoOh Deer Gamerdquohttpwwwriverventureorgcharlestonresourcespdfpopulation20study20gamepdf
Bioamplification
When water insoluble pesticides enter food chains the animals that eat them canrsquot break them down so they stay in their bodies The pesticides stay in the fatty tissue The pesticides then built up in a process called bioamplification
DDTbullDDT was the first modern pesticide developed to kill mosquitoes that spread malaria and typhus
bullIn 1962 an American activist named Rachel Carson published a book which alleged that DDT caused cancer and harmed bird reproduction This information led to the pesticide being banned in 1971
bullAlthough it is not being used in North America it is still being used in other countries and can be transmitted through bioamplification
DDT Video
Modern Chemical PesticidesNew pesticides are now water soluble and do not
build up in the tissues of animals They are safer but still have negative effects such as1 They break down quickly so they have to be spread
more often (cost more)
2 They are not selective so they can also kill birds reptiles amphibians and fish
3 Animals that do not die immediately may still put others at risk through bioamplification
4 They have a shelf life meaning that they become ineffective after a while
The Pests Fight Back Pests that reproduce often start to become
resistant to pesticides The first time using a chemical you will probably
kill 90 of the insects and the 10 that are left alive will reproduce
The 10 that survived probably had a natural resistance to the chemical Many of their offspring will also have the resistance After several generations the chemical is not as effective
New pesticides must be developed to take their place
Assignment
Read pages 52-57 and do questions 1-7 on page 58
Read pages 81-82 andmake a list of 4 pros and 4 cons for pesticide usage in controlling tentcaterpillars
Section 29-Monitoring Changes in Population
During the last three centuries global population has risen at an exponential rate
500 million in 16501 billion in 18502 billion in 19304 billion in 1975estimated at 8 billion in 2013
Population Growth Patterns Changes in population size occur when people
are added or removed from the population The four factors involved in population growth
are
1 Natality the number of offspring born in one year
2 Mortality the number of individuals that die in one year
3 Immigration the number of individuals moving into a population
4 Emigration the number of individuals moving out of a population
Population Growth = ( Births + Immigration) - ( Deaths + Emigration)
Open and Closed Populations
An open population occurs when all four factors are acting on the population
(Ex The population of Charlottetown)
A closed population occurs when only natality and mortality affect the population size
(Ex Population of the Earth)
Population Histogramsbulluseful when studying population of long-lived organisms such as humans
bullThe shape of pyramid allows you to predict changes in the populations
bullA wide base indicates that the population is rapidly growing
bull When the base is narrower than the middle section fewer offspring are produced and population will decline
Questions
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Section 210-Limits on Populations
Mice populations can change drastically in 6 months 20 mice can become 5120 mice
Why donrsquot we see billionsof mice when we lookout the window
The reason is that there are limitations on all populations including mice
Carrying Capacity
Populations fluctuate but tend to be fairly stable Stabilityhappens when the population does not exceed the carryingcapacity
Carrying Capacity - The maximum number of individual species that can be supported by an ecosystem
Law of Minimum - The nutrient in least supply is the one that limits growth
Law of Tolerance - An organism can survive within a certain range of abiotic factors Going above or below this range will cause death
Biotic potential is the maximum number of offspring that a species can produce if resources were unlimited
It is regulated by four factors
1) Birth potential maximum number of offspring per birth
2) Capacity of survival number of offspring that reach reproductive age
3) Procreation number of times a species reproduces each year
4) Length of reproductive life the age of sexual maturity and the number of years the individual can reproduce
Limiting Factors
The environment provides factors that prevent populations from attaining their biotic potential Environmental Factor Population Changes
Abiotic light temperaturechemical environment
Biotic Amount of foodnumber or effectiveness of predatorsdiseases and parasitesability to compete for resources
Some factors that control population can depend on the size or density of the population
A population is dense when a large number of organisms live in one area
Density IndependentFactors
Density DependentFactors
Flood Food shortage
Fire Competition for mates or habitat
Pesticides Diseases
Change in climate or temperature
Introduction of exotic species
Destruction of habitat Increased predation
Drought Competition for water and other resources
Questions
Read pages 77-80 and do questions 1 2 amp 3 (abc) on page 80
Chapter 3Sustaining Terrestrial Ecosystems
Section 31 Canadian Biomes
Jigsaw Activity
bull In groups you will be using pages 88-93 to complete the sheets on ldquoThe Canadian Biomesrdquo
bull Video Response Biomes (Earth at Risk Series)
Canadian Biomes Biome ndash a collection of ecosystems that are
similar or related to each other usually in the type of plants they support
Four Canadian Biomes
The Tundra The Boreal Forest The Temperate Deciduous
Forest The Grassland
Tundra
Boreal Forest
Grassland
Temperate Deciduous Forest
The Tundra- Canadarsquos northernmost biome
Biotic FactorsAbiotic Factors
very low temp for most
of the year
short growing season
Permafrost layer beneath the soil
low precipitation
poor soil quality
rapid-growing plants
mosses and lichens
caribou
ptarmigan
lemmings
arctic foxes
wolverines
Similar to a desert low precipitation (10-12 cmyear) supports a low number of species
Two layers of soil Permafrost ndash layer of soil that never thaws Active Layer ndash above permafrost thaws in summer allowing
roots to take in water and minerals
Decomposition of Organic Matter extremely slow in cold temp because cold keeps the
bacteria and fungi from reproducing This leaves only a small amount of organic material in the soil
Nitrogen and Carbon Cycles slows the rates of the cycles slow decomposition with surface water causes the
formation of bogs These store carbon for long periods of time and decrease denitrification
The Boreal Forest- Immediately south of the Tundra
Biotic FactorsAbiotic Factors
warmer than the Tundra
no permafrost
changeable weather
soils contains some water and is acidic
precipitation 40 cmyear or more
coniferous trees
seed-eating birds
squirrels
voles
snowshoe hare
deer
pine martens
grey wolves
Climate harsh with rapid changes in temp mixing warm and cool air results in
more precipitation
Soil warmer temp allows the soil to thaw every season higher organic matter from faster rates of decomposition soil is more acidic as coniferous needles produce acid when they decay
ndash this can limit the number of plants that can grow
What are conifers Trees with needle shaped leaves ndash evergreens
4 Reasons why conifers are dominant Thin needles have a small surface area so they lose little water during
winter Thick cuticle of wax covers the needles to reduce water loss and
protect from frost damage Pyramid shape of tree and flexible branches allow the tree to support
heavy snowfall Shed their leaves slowly throughout the year so they can begin
photosynthesis when the growing season begins (advantage in a short growing season)
The Temperate Deciduous Forest- South of the Boreal Forest in EasternCentral Canada
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp then Tundra or Boreal Forest
fertile soil
precipitation up to
100 cmyear
deciduous trees
many ferns and shrubs
tree and ground squirrels
many insects
shrews and mice
deer
woodpeckers
weasels black bears wolves
What are the dominant trees in
this biome Deciduous trees (maples oaks poplars
beech and birch)
What features about deciduous trees allow them to complete with conifers
The broad leaves maximize light capture for photosynthesis
Soil and Decomposition
higher temperatures allow for faster decomposition resulting in richer
soil
Understory and Canopy Understory ndash the lower branches of a trees
Canopy ndash the upper levels of the trees
What factors allow for high biodiversity in this biome
The presence of so many different kinds of plants supports many
animals
The thick litter layer is ideal for different insects
Many insects support amphibians lizards birds and insect-eating animals
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
Assignment
read pages 50-51 and do questions 1 2 5 amp 6 on page 51
Section 25-The Carbon Cycle
Carbon is the key element for living things
Carbon can be found in
1 The atmosphere (CO2)
2 Ocean (dissolved)
3 Plants (sugar C6H12O6)
4 Animals (protein)
5 Soil and rocks
The Carbon Cycle As carbon moves through the ecosystem it is
changed from one form to another
In Plants PHOTOSYNTHESISsunlight
CO2 + H2O C6H12O6 + O2
(Carbon dioxide + water glucose + oxygen)
In Animals CELLULAR RESPIRATION
C6H12O6 + O2 CO2 + H2O
The relationship between photosynthesis and cellular respiration is called the carbon cycle
Photosynthesis is the process in which plants use solar energy carbon dioxide from the atmosphere and water from the soil to make sugar
Cellular Respiration uses sugar and oxygen for energy and releases carbon dioxide back into the environment
The Carbon Cycle
Carbon ReservoirsReservoirs of Inorganic Carbon When carbon is not in organic form it can be found in three
types of storage (reservoirs)
Atmosphere (smallest ~ 003) Oceans (largest) Earthrsquos crust
Reservoirs for Organic Carbon Organic carbon is held in the bodies of living organisms
All living things eventually die and return their carbon in an inorganic form The only exception to this are bogs which have large quantities of organic carbon which may be stored for years in the peat (dead plant matter)
Humans have modified the carbon cycle by releasing large quantities of organic carbon
Example mining coal burning fossil fuels and burning forests
Assignment
read pages 62-65 and do the assigned questions for the Carbon Cycle(handout)
Play the Carbon Cycle Game httpwwwwindowsucareduearthclimatecarbon_cyclehtml
Section 26-The Nitrogen and Phosphorus Cycles
The Nitrogen Cycle
Life depends on the cycling of nitrogen used by cells to make protein in plants and
animals
used to make DNA in plant and animal cells
used as fertilizer to make plants grow
The atmosphere is 79 nitrogen all of which is unusable by plants and animals
Nitrogen is changed into nitrates (usable form) by
lightning
nitrogen fixing bacteria
Nitrogen Fixation Through Lightning energy from the lightning causes nitrogen gas to
react with oxygen gas to produce nitrates
the nitrates dissolve in rain or surface water enter the soil and then move into plants through their roots
Nitrogen Fixation by Bacteria bacteria found in the soil provide the vast majority
of nitrates in the ecosystem Some bacteria may also be found in small lumps called nodules on the roots of some plants
called nitrogen fixing bacteria
Denitrification involves the decay process in which denitrifying bacteria break down nitrates into nitrites and then into nitrogen gas which goes up into the air
This process ensures the balance between soil nitrates nitrites and nitrogen gas
Denitrifying bacteria grow well in areas of low oxygen like lawns By aerating your lawn (adding more oxygen) the breakdown of nitrates into nitrogen gas is reduced and your lawn will stay green longer (nitrates stay in your lawn)
Nitrogen Cycle Animation
Assignment
Read pages 66-67 and complete the assigned questions for the Nitrogen Cycle(handout)
Play the Nitrogen Cycle Game httpwwwwindowsucaredutourlink=teach
er_resourcesteach_nitrogenhtml
The Phosphorus CyclePhosphorous cycles in two ways
Long term in rocks in the Earthrsquos crust phosphates eroded from rock are carried away by rivers and
lakes and end up in the ocean animals use the phosphates to make bones and shells when these animal die they end up at the bottom of the
ocean where over time they may become rock again Plants also absorb phosphates from the water
Short term in living organisms phosphates in dead organisms are recycled by
decomposers which break them down and release the phosphates back into the ecosystem
Phosphorus Cycle
Assignment
bullRead page 68 and complete the questions on the Phosphorus Cycle (handout)
Phosphorus Cycle Animation
Phosphorus Cycle
Section 22-Pesticides
Pesticides are chemicals used to kill insects weeds and microorganisms that might damage crops
Why Use Pesticides Up to 30 of crops in Canada are destroyed by pests This impacts the farmerrsquos income and the price that we pay for the produce
First Generation Pesticides
Pest control dates back to 500 BCE Toxic chemicals were frequently used until we discovered they were more dangerous to us than to the pests
Second Generation Pesticidesbull chemicals made in a lab
bull Can be grouped into four categories
Type Target Examples Persistence
Insecticide Insects DDT 2 - 15 years
Herbicide Weeds Roundup Days to weeks
Fungicide Moulds
and fungi Captan Days
Bactericides Bacteria Penicillin Days
Assignment
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Complete the sheet on histograms (handout)
Play the ldquoOh Deer Gamerdquohttpwwwriverventureorgcharlestonresourcespdfpopulation20study20gamepdf
Bioamplification
When water insoluble pesticides enter food chains the animals that eat them canrsquot break them down so they stay in their bodies The pesticides stay in the fatty tissue The pesticides then built up in a process called bioamplification
DDTbullDDT was the first modern pesticide developed to kill mosquitoes that spread malaria and typhus
bullIn 1962 an American activist named Rachel Carson published a book which alleged that DDT caused cancer and harmed bird reproduction This information led to the pesticide being banned in 1971
bullAlthough it is not being used in North America it is still being used in other countries and can be transmitted through bioamplification
DDT Video
Modern Chemical PesticidesNew pesticides are now water soluble and do not
build up in the tissues of animals They are safer but still have negative effects such as1 They break down quickly so they have to be spread
more often (cost more)
2 They are not selective so they can also kill birds reptiles amphibians and fish
3 Animals that do not die immediately may still put others at risk through bioamplification
4 They have a shelf life meaning that they become ineffective after a while
The Pests Fight Back Pests that reproduce often start to become
resistant to pesticides The first time using a chemical you will probably
kill 90 of the insects and the 10 that are left alive will reproduce
The 10 that survived probably had a natural resistance to the chemical Many of their offspring will also have the resistance After several generations the chemical is not as effective
New pesticides must be developed to take their place
Assignment
Read pages 52-57 and do questions 1-7 on page 58
Read pages 81-82 andmake a list of 4 pros and 4 cons for pesticide usage in controlling tentcaterpillars
Section 29-Monitoring Changes in Population
During the last three centuries global population has risen at an exponential rate
500 million in 16501 billion in 18502 billion in 19304 billion in 1975estimated at 8 billion in 2013
Population Growth Patterns Changes in population size occur when people
are added or removed from the population The four factors involved in population growth
are
1 Natality the number of offspring born in one year
2 Mortality the number of individuals that die in one year
3 Immigration the number of individuals moving into a population
4 Emigration the number of individuals moving out of a population
Population Growth = ( Births + Immigration) - ( Deaths + Emigration)
Open and Closed Populations
An open population occurs when all four factors are acting on the population
(Ex The population of Charlottetown)
A closed population occurs when only natality and mortality affect the population size
(Ex Population of the Earth)
Population Histogramsbulluseful when studying population of long-lived organisms such as humans
bullThe shape of pyramid allows you to predict changes in the populations
bullA wide base indicates that the population is rapidly growing
bull When the base is narrower than the middle section fewer offspring are produced and population will decline
Questions
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Section 210-Limits on Populations
Mice populations can change drastically in 6 months 20 mice can become 5120 mice
Why donrsquot we see billionsof mice when we lookout the window
The reason is that there are limitations on all populations including mice
Carrying Capacity
Populations fluctuate but tend to be fairly stable Stabilityhappens when the population does not exceed the carryingcapacity
Carrying Capacity - The maximum number of individual species that can be supported by an ecosystem
Law of Minimum - The nutrient in least supply is the one that limits growth
Law of Tolerance - An organism can survive within a certain range of abiotic factors Going above or below this range will cause death
Biotic potential is the maximum number of offspring that a species can produce if resources were unlimited
It is regulated by four factors
1) Birth potential maximum number of offspring per birth
2) Capacity of survival number of offspring that reach reproductive age
3) Procreation number of times a species reproduces each year
4) Length of reproductive life the age of sexual maturity and the number of years the individual can reproduce
Limiting Factors
The environment provides factors that prevent populations from attaining their biotic potential Environmental Factor Population Changes
Abiotic light temperaturechemical environment
Biotic Amount of foodnumber or effectiveness of predatorsdiseases and parasitesability to compete for resources
Some factors that control population can depend on the size or density of the population
A population is dense when a large number of organisms live in one area
Density IndependentFactors
Density DependentFactors
Flood Food shortage
Fire Competition for mates or habitat
Pesticides Diseases
Change in climate or temperature
Introduction of exotic species
Destruction of habitat Increased predation
Drought Competition for water and other resources
Questions
Read pages 77-80 and do questions 1 2 amp 3 (abc) on page 80
Chapter 3Sustaining Terrestrial Ecosystems
Section 31 Canadian Biomes
Jigsaw Activity
bull In groups you will be using pages 88-93 to complete the sheets on ldquoThe Canadian Biomesrdquo
bull Video Response Biomes (Earth at Risk Series)
Canadian Biomes Biome ndash a collection of ecosystems that are
similar or related to each other usually in the type of plants they support
Four Canadian Biomes
The Tundra The Boreal Forest The Temperate Deciduous
Forest The Grassland
Tundra
Boreal Forest
Grassland
Temperate Deciduous Forest
The Tundra- Canadarsquos northernmost biome
Biotic FactorsAbiotic Factors
very low temp for most
of the year
short growing season
Permafrost layer beneath the soil
low precipitation
poor soil quality
rapid-growing plants
mosses and lichens
caribou
ptarmigan
lemmings
arctic foxes
wolverines
Similar to a desert low precipitation (10-12 cmyear) supports a low number of species
Two layers of soil Permafrost ndash layer of soil that never thaws Active Layer ndash above permafrost thaws in summer allowing
roots to take in water and minerals
Decomposition of Organic Matter extremely slow in cold temp because cold keeps the
bacteria and fungi from reproducing This leaves only a small amount of organic material in the soil
Nitrogen and Carbon Cycles slows the rates of the cycles slow decomposition with surface water causes the
formation of bogs These store carbon for long periods of time and decrease denitrification
The Boreal Forest- Immediately south of the Tundra
Biotic FactorsAbiotic Factors
warmer than the Tundra
no permafrost
changeable weather
soils contains some water and is acidic
precipitation 40 cmyear or more
coniferous trees
seed-eating birds
squirrels
voles
snowshoe hare
deer
pine martens
grey wolves
Climate harsh with rapid changes in temp mixing warm and cool air results in
more precipitation
Soil warmer temp allows the soil to thaw every season higher organic matter from faster rates of decomposition soil is more acidic as coniferous needles produce acid when they decay
ndash this can limit the number of plants that can grow
What are conifers Trees with needle shaped leaves ndash evergreens
4 Reasons why conifers are dominant Thin needles have a small surface area so they lose little water during
winter Thick cuticle of wax covers the needles to reduce water loss and
protect from frost damage Pyramid shape of tree and flexible branches allow the tree to support
heavy snowfall Shed their leaves slowly throughout the year so they can begin
photosynthesis when the growing season begins (advantage in a short growing season)
The Temperate Deciduous Forest- South of the Boreal Forest in EasternCentral Canada
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp then Tundra or Boreal Forest
fertile soil
precipitation up to
100 cmyear
deciduous trees
many ferns and shrubs
tree and ground squirrels
many insects
shrews and mice
deer
woodpeckers
weasels black bears wolves
What are the dominant trees in
this biome Deciduous trees (maples oaks poplars
beech and birch)
What features about deciduous trees allow them to complete with conifers
The broad leaves maximize light capture for photosynthesis
Soil and Decomposition
higher temperatures allow for faster decomposition resulting in richer
soil
Understory and Canopy Understory ndash the lower branches of a trees
Canopy ndash the upper levels of the trees
What factors allow for high biodiversity in this biome
The presence of so many different kinds of plants supports many
animals
The thick litter layer is ideal for different insects
Many insects support amphibians lizards birds and insect-eating animals
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
Section 25-The Carbon Cycle
Carbon is the key element for living things
Carbon can be found in
1 The atmosphere (CO2)
2 Ocean (dissolved)
3 Plants (sugar C6H12O6)
4 Animals (protein)
5 Soil and rocks
The Carbon Cycle As carbon moves through the ecosystem it is
changed from one form to another
In Plants PHOTOSYNTHESISsunlight
CO2 + H2O C6H12O6 + O2
(Carbon dioxide + water glucose + oxygen)
In Animals CELLULAR RESPIRATION
C6H12O6 + O2 CO2 + H2O
The relationship between photosynthesis and cellular respiration is called the carbon cycle
Photosynthesis is the process in which plants use solar energy carbon dioxide from the atmosphere and water from the soil to make sugar
Cellular Respiration uses sugar and oxygen for energy and releases carbon dioxide back into the environment
The Carbon Cycle
Carbon ReservoirsReservoirs of Inorganic Carbon When carbon is not in organic form it can be found in three
types of storage (reservoirs)
Atmosphere (smallest ~ 003) Oceans (largest) Earthrsquos crust
Reservoirs for Organic Carbon Organic carbon is held in the bodies of living organisms
All living things eventually die and return their carbon in an inorganic form The only exception to this are bogs which have large quantities of organic carbon which may be stored for years in the peat (dead plant matter)
Humans have modified the carbon cycle by releasing large quantities of organic carbon
Example mining coal burning fossil fuels and burning forests
Assignment
read pages 62-65 and do the assigned questions for the Carbon Cycle(handout)
Play the Carbon Cycle Game httpwwwwindowsucareduearthclimatecarbon_cyclehtml
Section 26-The Nitrogen and Phosphorus Cycles
The Nitrogen Cycle
Life depends on the cycling of nitrogen used by cells to make protein in plants and
animals
used to make DNA in plant and animal cells
used as fertilizer to make plants grow
The atmosphere is 79 nitrogen all of which is unusable by plants and animals
Nitrogen is changed into nitrates (usable form) by
lightning
nitrogen fixing bacteria
Nitrogen Fixation Through Lightning energy from the lightning causes nitrogen gas to
react with oxygen gas to produce nitrates
the nitrates dissolve in rain or surface water enter the soil and then move into plants through their roots
Nitrogen Fixation by Bacteria bacteria found in the soil provide the vast majority
of nitrates in the ecosystem Some bacteria may also be found in small lumps called nodules on the roots of some plants
called nitrogen fixing bacteria
Denitrification involves the decay process in which denitrifying bacteria break down nitrates into nitrites and then into nitrogen gas which goes up into the air
This process ensures the balance between soil nitrates nitrites and nitrogen gas
Denitrifying bacteria grow well in areas of low oxygen like lawns By aerating your lawn (adding more oxygen) the breakdown of nitrates into nitrogen gas is reduced and your lawn will stay green longer (nitrates stay in your lawn)
Nitrogen Cycle Animation
Assignment
Read pages 66-67 and complete the assigned questions for the Nitrogen Cycle(handout)
Play the Nitrogen Cycle Game httpwwwwindowsucaredutourlink=teach
er_resourcesteach_nitrogenhtml
The Phosphorus CyclePhosphorous cycles in two ways
Long term in rocks in the Earthrsquos crust phosphates eroded from rock are carried away by rivers and
lakes and end up in the ocean animals use the phosphates to make bones and shells when these animal die they end up at the bottom of the
ocean where over time they may become rock again Plants also absorb phosphates from the water
Short term in living organisms phosphates in dead organisms are recycled by
decomposers which break them down and release the phosphates back into the ecosystem
Phosphorus Cycle
Assignment
bullRead page 68 and complete the questions on the Phosphorus Cycle (handout)
Phosphorus Cycle Animation
Phosphorus Cycle
Section 22-Pesticides
Pesticides are chemicals used to kill insects weeds and microorganisms that might damage crops
Why Use Pesticides Up to 30 of crops in Canada are destroyed by pests This impacts the farmerrsquos income and the price that we pay for the produce
First Generation Pesticides
Pest control dates back to 500 BCE Toxic chemicals were frequently used until we discovered they were more dangerous to us than to the pests
Second Generation Pesticidesbull chemicals made in a lab
bull Can be grouped into four categories
Type Target Examples Persistence
Insecticide Insects DDT 2 - 15 years
Herbicide Weeds Roundup Days to weeks
Fungicide Moulds
and fungi Captan Days
Bactericides Bacteria Penicillin Days
Assignment
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Complete the sheet on histograms (handout)
Play the ldquoOh Deer Gamerdquohttpwwwriverventureorgcharlestonresourcespdfpopulation20study20gamepdf
Bioamplification
When water insoluble pesticides enter food chains the animals that eat them canrsquot break them down so they stay in their bodies The pesticides stay in the fatty tissue The pesticides then built up in a process called bioamplification
DDTbullDDT was the first modern pesticide developed to kill mosquitoes that spread malaria and typhus
bullIn 1962 an American activist named Rachel Carson published a book which alleged that DDT caused cancer and harmed bird reproduction This information led to the pesticide being banned in 1971
bullAlthough it is not being used in North America it is still being used in other countries and can be transmitted through bioamplification
DDT Video
Modern Chemical PesticidesNew pesticides are now water soluble and do not
build up in the tissues of animals They are safer but still have negative effects such as1 They break down quickly so they have to be spread
more often (cost more)
2 They are not selective so they can also kill birds reptiles amphibians and fish
3 Animals that do not die immediately may still put others at risk through bioamplification
4 They have a shelf life meaning that they become ineffective after a while
The Pests Fight Back Pests that reproduce often start to become
resistant to pesticides The first time using a chemical you will probably
kill 90 of the insects and the 10 that are left alive will reproduce
The 10 that survived probably had a natural resistance to the chemical Many of their offspring will also have the resistance After several generations the chemical is not as effective
New pesticides must be developed to take their place
Assignment
Read pages 52-57 and do questions 1-7 on page 58
Read pages 81-82 andmake a list of 4 pros and 4 cons for pesticide usage in controlling tentcaterpillars
Section 29-Monitoring Changes in Population
During the last three centuries global population has risen at an exponential rate
500 million in 16501 billion in 18502 billion in 19304 billion in 1975estimated at 8 billion in 2013
Population Growth Patterns Changes in population size occur when people
are added or removed from the population The four factors involved in population growth
are
1 Natality the number of offspring born in one year
2 Mortality the number of individuals that die in one year
3 Immigration the number of individuals moving into a population
4 Emigration the number of individuals moving out of a population
Population Growth = ( Births + Immigration) - ( Deaths + Emigration)
Open and Closed Populations
An open population occurs when all four factors are acting on the population
(Ex The population of Charlottetown)
A closed population occurs when only natality and mortality affect the population size
(Ex Population of the Earth)
Population Histogramsbulluseful when studying population of long-lived organisms such as humans
bullThe shape of pyramid allows you to predict changes in the populations
bullA wide base indicates that the population is rapidly growing
bull When the base is narrower than the middle section fewer offspring are produced and population will decline
Questions
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Section 210-Limits on Populations
Mice populations can change drastically in 6 months 20 mice can become 5120 mice
Why donrsquot we see billionsof mice when we lookout the window
The reason is that there are limitations on all populations including mice
Carrying Capacity
Populations fluctuate but tend to be fairly stable Stabilityhappens when the population does not exceed the carryingcapacity
Carrying Capacity - The maximum number of individual species that can be supported by an ecosystem
Law of Minimum - The nutrient in least supply is the one that limits growth
Law of Tolerance - An organism can survive within a certain range of abiotic factors Going above or below this range will cause death
Biotic potential is the maximum number of offspring that a species can produce if resources were unlimited
It is regulated by four factors
1) Birth potential maximum number of offspring per birth
2) Capacity of survival number of offspring that reach reproductive age
3) Procreation number of times a species reproduces each year
4) Length of reproductive life the age of sexual maturity and the number of years the individual can reproduce
Limiting Factors
The environment provides factors that prevent populations from attaining their biotic potential Environmental Factor Population Changes
Abiotic light temperaturechemical environment
Biotic Amount of foodnumber or effectiveness of predatorsdiseases and parasitesability to compete for resources
Some factors that control population can depend on the size or density of the population
A population is dense when a large number of organisms live in one area
Density IndependentFactors
Density DependentFactors
Flood Food shortage
Fire Competition for mates or habitat
Pesticides Diseases
Change in climate or temperature
Introduction of exotic species
Destruction of habitat Increased predation
Drought Competition for water and other resources
Questions
Read pages 77-80 and do questions 1 2 amp 3 (abc) on page 80
Chapter 3Sustaining Terrestrial Ecosystems
Section 31 Canadian Biomes
Jigsaw Activity
bull In groups you will be using pages 88-93 to complete the sheets on ldquoThe Canadian Biomesrdquo
bull Video Response Biomes (Earth at Risk Series)
Canadian Biomes Biome ndash a collection of ecosystems that are
similar or related to each other usually in the type of plants they support
Four Canadian Biomes
The Tundra The Boreal Forest The Temperate Deciduous
Forest The Grassland
Tundra
Boreal Forest
Grassland
Temperate Deciduous Forest
The Tundra- Canadarsquos northernmost biome
Biotic FactorsAbiotic Factors
very low temp for most
of the year
short growing season
Permafrost layer beneath the soil
low precipitation
poor soil quality
rapid-growing plants
mosses and lichens
caribou
ptarmigan
lemmings
arctic foxes
wolverines
Similar to a desert low precipitation (10-12 cmyear) supports a low number of species
Two layers of soil Permafrost ndash layer of soil that never thaws Active Layer ndash above permafrost thaws in summer allowing
roots to take in water and minerals
Decomposition of Organic Matter extremely slow in cold temp because cold keeps the
bacteria and fungi from reproducing This leaves only a small amount of organic material in the soil
Nitrogen and Carbon Cycles slows the rates of the cycles slow decomposition with surface water causes the
formation of bogs These store carbon for long periods of time and decrease denitrification
The Boreal Forest- Immediately south of the Tundra
Biotic FactorsAbiotic Factors
warmer than the Tundra
no permafrost
changeable weather
soils contains some water and is acidic
precipitation 40 cmyear or more
coniferous trees
seed-eating birds
squirrels
voles
snowshoe hare
deer
pine martens
grey wolves
Climate harsh with rapid changes in temp mixing warm and cool air results in
more precipitation
Soil warmer temp allows the soil to thaw every season higher organic matter from faster rates of decomposition soil is more acidic as coniferous needles produce acid when they decay
ndash this can limit the number of plants that can grow
What are conifers Trees with needle shaped leaves ndash evergreens
4 Reasons why conifers are dominant Thin needles have a small surface area so they lose little water during
winter Thick cuticle of wax covers the needles to reduce water loss and
protect from frost damage Pyramid shape of tree and flexible branches allow the tree to support
heavy snowfall Shed their leaves slowly throughout the year so they can begin
photosynthesis when the growing season begins (advantage in a short growing season)
The Temperate Deciduous Forest- South of the Boreal Forest in EasternCentral Canada
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp then Tundra or Boreal Forest
fertile soil
precipitation up to
100 cmyear
deciduous trees
many ferns and shrubs
tree and ground squirrels
many insects
shrews and mice
deer
woodpeckers
weasels black bears wolves
What are the dominant trees in
this biome Deciduous trees (maples oaks poplars
beech and birch)
What features about deciduous trees allow them to complete with conifers
The broad leaves maximize light capture for photosynthesis
Soil and Decomposition
higher temperatures allow for faster decomposition resulting in richer
soil
Understory and Canopy Understory ndash the lower branches of a trees
Canopy ndash the upper levels of the trees
What factors allow for high biodiversity in this biome
The presence of so many different kinds of plants supports many
animals
The thick litter layer is ideal for different insects
Many insects support amphibians lizards birds and insect-eating animals
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
The Carbon Cycle As carbon moves through the ecosystem it is
changed from one form to another
In Plants PHOTOSYNTHESISsunlight
CO2 + H2O C6H12O6 + O2
(Carbon dioxide + water glucose + oxygen)
In Animals CELLULAR RESPIRATION
C6H12O6 + O2 CO2 + H2O
The relationship between photosynthesis and cellular respiration is called the carbon cycle
Photosynthesis is the process in which plants use solar energy carbon dioxide from the atmosphere and water from the soil to make sugar
Cellular Respiration uses sugar and oxygen for energy and releases carbon dioxide back into the environment
The Carbon Cycle
Carbon ReservoirsReservoirs of Inorganic Carbon When carbon is not in organic form it can be found in three
types of storage (reservoirs)
Atmosphere (smallest ~ 003) Oceans (largest) Earthrsquos crust
Reservoirs for Organic Carbon Organic carbon is held in the bodies of living organisms
All living things eventually die and return their carbon in an inorganic form The only exception to this are bogs which have large quantities of organic carbon which may be stored for years in the peat (dead plant matter)
Humans have modified the carbon cycle by releasing large quantities of organic carbon
Example mining coal burning fossil fuels and burning forests
Assignment
read pages 62-65 and do the assigned questions for the Carbon Cycle(handout)
Play the Carbon Cycle Game httpwwwwindowsucareduearthclimatecarbon_cyclehtml
Section 26-The Nitrogen and Phosphorus Cycles
The Nitrogen Cycle
Life depends on the cycling of nitrogen used by cells to make protein in plants and
animals
used to make DNA in plant and animal cells
used as fertilizer to make plants grow
The atmosphere is 79 nitrogen all of which is unusable by plants and animals
Nitrogen is changed into nitrates (usable form) by
lightning
nitrogen fixing bacteria
Nitrogen Fixation Through Lightning energy from the lightning causes nitrogen gas to
react with oxygen gas to produce nitrates
the nitrates dissolve in rain or surface water enter the soil and then move into plants through their roots
Nitrogen Fixation by Bacteria bacteria found in the soil provide the vast majority
of nitrates in the ecosystem Some bacteria may also be found in small lumps called nodules on the roots of some plants
called nitrogen fixing bacteria
Denitrification involves the decay process in which denitrifying bacteria break down nitrates into nitrites and then into nitrogen gas which goes up into the air
This process ensures the balance between soil nitrates nitrites and nitrogen gas
Denitrifying bacteria grow well in areas of low oxygen like lawns By aerating your lawn (adding more oxygen) the breakdown of nitrates into nitrogen gas is reduced and your lawn will stay green longer (nitrates stay in your lawn)
Nitrogen Cycle Animation
Assignment
Read pages 66-67 and complete the assigned questions for the Nitrogen Cycle(handout)
Play the Nitrogen Cycle Game httpwwwwindowsucaredutourlink=teach
er_resourcesteach_nitrogenhtml
The Phosphorus CyclePhosphorous cycles in two ways
Long term in rocks in the Earthrsquos crust phosphates eroded from rock are carried away by rivers and
lakes and end up in the ocean animals use the phosphates to make bones and shells when these animal die they end up at the bottom of the
ocean where over time they may become rock again Plants also absorb phosphates from the water
Short term in living organisms phosphates in dead organisms are recycled by
decomposers which break them down and release the phosphates back into the ecosystem
Phosphorus Cycle
Assignment
bullRead page 68 and complete the questions on the Phosphorus Cycle (handout)
Phosphorus Cycle Animation
Phosphorus Cycle
Section 22-Pesticides
Pesticides are chemicals used to kill insects weeds and microorganisms that might damage crops
Why Use Pesticides Up to 30 of crops in Canada are destroyed by pests This impacts the farmerrsquos income and the price that we pay for the produce
First Generation Pesticides
Pest control dates back to 500 BCE Toxic chemicals were frequently used until we discovered they were more dangerous to us than to the pests
Second Generation Pesticidesbull chemicals made in a lab
bull Can be grouped into four categories
Type Target Examples Persistence
Insecticide Insects DDT 2 - 15 years
Herbicide Weeds Roundup Days to weeks
Fungicide Moulds
and fungi Captan Days
Bactericides Bacteria Penicillin Days
Assignment
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Complete the sheet on histograms (handout)
Play the ldquoOh Deer Gamerdquohttpwwwriverventureorgcharlestonresourcespdfpopulation20study20gamepdf
Bioamplification
When water insoluble pesticides enter food chains the animals that eat them canrsquot break them down so they stay in their bodies The pesticides stay in the fatty tissue The pesticides then built up in a process called bioamplification
DDTbullDDT was the first modern pesticide developed to kill mosquitoes that spread malaria and typhus
bullIn 1962 an American activist named Rachel Carson published a book which alleged that DDT caused cancer and harmed bird reproduction This information led to the pesticide being banned in 1971
bullAlthough it is not being used in North America it is still being used in other countries and can be transmitted through bioamplification
DDT Video
Modern Chemical PesticidesNew pesticides are now water soluble and do not
build up in the tissues of animals They are safer but still have negative effects such as1 They break down quickly so they have to be spread
more often (cost more)
2 They are not selective so they can also kill birds reptiles amphibians and fish
3 Animals that do not die immediately may still put others at risk through bioamplification
4 They have a shelf life meaning that they become ineffective after a while
The Pests Fight Back Pests that reproduce often start to become
resistant to pesticides The first time using a chemical you will probably
kill 90 of the insects and the 10 that are left alive will reproduce
The 10 that survived probably had a natural resistance to the chemical Many of their offspring will also have the resistance After several generations the chemical is not as effective
New pesticides must be developed to take their place
Assignment
Read pages 52-57 and do questions 1-7 on page 58
Read pages 81-82 andmake a list of 4 pros and 4 cons for pesticide usage in controlling tentcaterpillars
Section 29-Monitoring Changes in Population
During the last three centuries global population has risen at an exponential rate
500 million in 16501 billion in 18502 billion in 19304 billion in 1975estimated at 8 billion in 2013
Population Growth Patterns Changes in population size occur when people
are added or removed from the population The four factors involved in population growth
are
1 Natality the number of offspring born in one year
2 Mortality the number of individuals that die in one year
3 Immigration the number of individuals moving into a population
4 Emigration the number of individuals moving out of a population
Population Growth = ( Births + Immigration) - ( Deaths + Emigration)
Open and Closed Populations
An open population occurs when all four factors are acting on the population
(Ex The population of Charlottetown)
A closed population occurs when only natality and mortality affect the population size
(Ex Population of the Earth)
Population Histogramsbulluseful when studying population of long-lived organisms such as humans
bullThe shape of pyramid allows you to predict changes in the populations
bullA wide base indicates that the population is rapidly growing
bull When the base is narrower than the middle section fewer offspring are produced and population will decline
Questions
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Section 210-Limits on Populations
Mice populations can change drastically in 6 months 20 mice can become 5120 mice
Why donrsquot we see billionsof mice when we lookout the window
The reason is that there are limitations on all populations including mice
Carrying Capacity
Populations fluctuate but tend to be fairly stable Stabilityhappens when the population does not exceed the carryingcapacity
Carrying Capacity - The maximum number of individual species that can be supported by an ecosystem
Law of Minimum - The nutrient in least supply is the one that limits growth
Law of Tolerance - An organism can survive within a certain range of abiotic factors Going above or below this range will cause death
Biotic potential is the maximum number of offspring that a species can produce if resources were unlimited
It is regulated by four factors
1) Birth potential maximum number of offspring per birth
2) Capacity of survival number of offspring that reach reproductive age
3) Procreation number of times a species reproduces each year
4) Length of reproductive life the age of sexual maturity and the number of years the individual can reproduce
Limiting Factors
The environment provides factors that prevent populations from attaining their biotic potential Environmental Factor Population Changes
Abiotic light temperaturechemical environment
Biotic Amount of foodnumber or effectiveness of predatorsdiseases and parasitesability to compete for resources
Some factors that control population can depend on the size or density of the population
A population is dense when a large number of organisms live in one area
Density IndependentFactors
Density DependentFactors
Flood Food shortage
Fire Competition for mates or habitat
Pesticides Diseases
Change in climate or temperature
Introduction of exotic species
Destruction of habitat Increased predation
Drought Competition for water and other resources
Questions
Read pages 77-80 and do questions 1 2 amp 3 (abc) on page 80
Chapter 3Sustaining Terrestrial Ecosystems
Section 31 Canadian Biomes
Jigsaw Activity
bull In groups you will be using pages 88-93 to complete the sheets on ldquoThe Canadian Biomesrdquo
bull Video Response Biomes (Earth at Risk Series)
Canadian Biomes Biome ndash a collection of ecosystems that are
similar or related to each other usually in the type of plants they support
Four Canadian Biomes
The Tundra The Boreal Forest The Temperate Deciduous
Forest The Grassland
Tundra
Boreal Forest
Grassland
Temperate Deciduous Forest
The Tundra- Canadarsquos northernmost biome
Biotic FactorsAbiotic Factors
very low temp for most
of the year
short growing season
Permafrost layer beneath the soil
low precipitation
poor soil quality
rapid-growing plants
mosses and lichens
caribou
ptarmigan
lemmings
arctic foxes
wolverines
Similar to a desert low precipitation (10-12 cmyear) supports a low number of species
Two layers of soil Permafrost ndash layer of soil that never thaws Active Layer ndash above permafrost thaws in summer allowing
roots to take in water and minerals
Decomposition of Organic Matter extremely slow in cold temp because cold keeps the
bacteria and fungi from reproducing This leaves only a small amount of organic material in the soil
Nitrogen and Carbon Cycles slows the rates of the cycles slow decomposition with surface water causes the
formation of bogs These store carbon for long periods of time and decrease denitrification
The Boreal Forest- Immediately south of the Tundra
Biotic FactorsAbiotic Factors
warmer than the Tundra
no permafrost
changeable weather
soils contains some water and is acidic
precipitation 40 cmyear or more
coniferous trees
seed-eating birds
squirrels
voles
snowshoe hare
deer
pine martens
grey wolves
Climate harsh with rapid changes in temp mixing warm and cool air results in
more precipitation
Soil warmer temp allows the soil to thaw every season higher organic matter from faster rates of decomposition soil is more acidic as coniferous needles produce acid when they decay
ndash this can limit the number of plants that can grow
What are conifers Trees with needle shaped leaves ndash evergreens
4 Reasons why conifers are dominant Thin needles have a small surface area so they lose little water during
winter Thick cuticle of wax covers the needles to reduce water loss and
protect from frost damage Pyramid shape of tree and flexible branches allow the tree to support
heavy snowfall Shed their leaves slowly throughout the year so they can begin
photosynthesis when the growing season begins (advantage in a short growing season)
The Temperate Deciduous Forest- South of the Boreal Forest in EasternCentral Canada
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp then Tundra or Boreal Forest
fertile soil
precipitation up to
100 cmyear
deciduous trees
many ferns and shrubs
tree and ground squirrels
many insects
shrews and mice
deer
woodpeckers
weasels black bears wolves
What are the dominant trees in
this biome Deciduous trees (maples oaks poplars
beech and birch)
What features about deciduous trees allow them to complete with conifers
The broad leaves maximize light capture for photosynthesis
Soil and Decomposition
higher temperatures allow for faster decomposition resulting in richer
soil
Understory and Canopy Understory ndash the lower branches of a trees
Canopy ndash the upper levels of the trees
What factors allow for high biodiversity in this biome
The presence of so many different kinds of plants supports many
animals
The thick litter layer is ideal for different insects
Many insects support amphibians lizards birds and insect-eating animals
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
The relationship between photosynthesis and cellular respiration is called the carbon cycle
Photosynthesis is the process in which plants use solar energy carbon dioxide from the atmosphere and water from the soil to make sugar
Cellular Respiration uses sugar and oxygen for energy and releases carbon dioxide back into the environment
The Carbon Cycle
Carbon ReservoirsReservoirs of Inorganic Carbon When carbon is not in organic form it can be found in three
types of storage (reservoirs)
Atmosphere (smallest ~ 003) Oceans (largest) Earthrsquos crust
Reservoirs for Organic Carbon Organic carbon is held in the bodies of living organisms
All living things eventually die and return their carbon in an inorganic form The only exception to this are bogs which have large quantities of organic carbon which may be stored for years in the peat (dead plant matter)
Humans have modified the carbon cycle by releasing large quantities of organic carbon
Example mining coal burning fossil fuels and burning forests
Assignment
read pages 62-65 and do the assigned questions for the Carbon Cycle(handout)
Play the Carbon Cycle Game httpwwwwindowsucareduearthclimatecarbon_cyclehtml
Section 26-The Nitrogen and Phosphorus Cycles
The Nitrogen Cycle
Life depends on the cycling of nitrogen used by cells to make protein in plants and
animals
used to make DNA in plant and animal cells
used as fertilizer to make plants grow
The atmosphere is 79 nitrogen all of which is unusable by plants and animals
Nitrogen is changed into nitrates (usable form) by
lightning
nitrogen fixing bacteria
Nitrogen Fixation Through Lightning energy from the lightning causes nitrogen gas to
react with oxygen gas to produce nitrates
the nitrates dissolve in rain or surface water enter the soil and then move into plants through their roots
Nitrogen Fixation by Bacteria bacteria found in the soil provide the vast majority
of nitrates in the ecosystem Some bacteria may also be found in small lumps called nodules on the roots of some plants
called nitrogen fixing bacteria
Denitrification involves the decay process in which denitrifying bacteria break down nitrates into nitrites and then into nitrogen gas which goes up into the air
This process ensures the balance between soil nitrates nitrites and nitrogen gas
Denitrifying bacteria grow well in areas of low oxygen like lawns By aerating your lawn (adding more oxygen) the breakdown of nitrates into nitrogen gas is reduced and your lawn will stay green longer (nitrates stay in your lawn)
Nitrogen Cycle Animation
Assignment
Read pages 66-67 and complete the assigned questions for the Nitrogen Cycle(handout)
Play the Nitrogen Cycle Game httpwwwwindowsucaredutourlink=teach
er_resourcesteach_nitrogenhtml
The Phosphorus CyclePhosphorous cycles in two ways
Long term in rocks in the Earthrsquos crust phosphates eroded from rock are carried away by rivers and
lakes and end up in the ocean animals use the phosphates to make bones and shells when these animal die they end up at the bottom of the
ocean where over time they may become rock again Plants also absorb phosphates from the water
Short term in living organisms phosphates in dead organisms are recycled by
decomposers which break them down and release the phosphates back into the ecosystem
Phosphorus Cycle
Assignment
bullRead page 68 and complete the questions on the Phosphorus Cycle (handout)
Phosphorus Cycle Animation
Phosphorus Cycle
Section 22-Pesticides
Pesticides are chemicals used to kill insects weeds and microorganisms that might damage crops
Why Use Pesticides Up to 30 of crops in Canada are destroyed by pests This impacts the farmerrsquos income and the price that we pay for the produce
First Generation Pesticides
Pest control dates back to 500 BCE Toxic chemicals were frequently used until we discovered they were more dangerous to us than to the pests
Second Generation Pesticidesbull chemicals made in a lab
bull Can be grouped into four categories
Type Target Examples Persistence
Insecticide Insects DDT 2 - 15 years
Herbicide Weeds Roundup Days to weeks
Fungicide Moulds
and fungi Captan Days
Bactericides Bacteria Penicillin Days
Assignment
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Complete the sheet on histograms (handout)
Play the ldquoOh Deer Gamerdquohttpwwwriverventureorgcharlestonresourcespdfpopulation20study20gamepdf
Bioamplification
When water insoluble pesticides enter food chains the animals that eat them canrsquot break them down so they stay in their bodies The pesticides stay in the fatty tissue The pesticides then built up in a process called bioamplification
DDTbullDDT was the first modern pesticide developed to kill mosquitoes that spread malaria and typhus
bullIn 1962 an American activist named Rachel Carson published a book which alleged that DDT caused cancer and harmed bird reproduction This information led to the pesticide being banned in 1971
bullAlthough it is not being used in North America it is still being used in other countries and can be transmitted through bioamplification
DDT Video
Modern Chemical PesticidesNew pesticides are now water soluble and do not
build up in the tissues of animals They are safer but still have negative effects such as1 They break down quickly so they have to be spread
more often (cost more)
2 They are not selective so they can also kill birds reptiles amphibians and fish
3 Animals that do not die immediately may still put others at risk through bioamplification
4 They have a shelf life meaning that they become ineffective after a while
The Pests Fight Back Pests that reproduce often start to become
resistant to pesticides The first time using a chemical you will probably
kill 90 of the insects and the 10 that are left alive will reproduce
The 10 that survived probably had a natural resistance to the chemical Many of their offspring will also have the resistance After several generations the chemical is not as effective
New pesticides must be developed to take their place
Assignment
Read pages 52-57 and do questions 1-7 on page 58
Read pages 81-82 andmake a list of 4 pros and 4 cons for pesticide usage in controlling tentcaterpillars
Section 29-Monitoring Changes in Population
During the last three centuries global population has risen at an exponential rate
500 million in 16501 billion in 18502 billion in 19304 billion in 1975estimated at 8 billion in 2013
Population Growth Patterns Changes in population size occur when people
are added or removed from the population The four factors involved in population growth
are
1 Natality the number of offspring born in one year
2 Mortality the number of individuals that die in one year
3 Immigration the number of individuals moving into a population
4 Emigration the number of individuals moving out of a population
Population Growth = ( Births + Immigration) - ( Deaths + Emigration)
Open and Closed Populations
An open population occurs when all four factors are acting on the population
(Ex The population of Charlottetown)
A closed population occurs when only natality and mortality affect the population size
(Ex Population of the Earth)
Population Histogramsbulluseful when studying population of long-lived organisms such as humans
bullThe shape of pyramid allows you to predict changes in the populations
bullA wide base indicates that the population is rapidly growing
bull When the base is narrower than the middle section fewer offspring are produced and population will decline
Questions
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Section 210-Limits on Populations
Mice populations can change drastically in 6 months 20 mice can become 5120 mice
Why donrsquot we see billionsof mice when we lookout the window
The reason is that there are limitations on all populations including mice
Carrying Capacity
Populations fluctuate but tend to be fairly stable Stabilityhappens when the population does not exceed the carryingcapacity
Carrying Capacity - The maximum number of individual species that can be supported by an ecosystem
Law of Minimum - The nutrient in least supply is the one that limits growth
Law of Tolerance - An organism can survive within a certain range of abiotic factors Going above or below this range will cause death
Biotic potential is the maximum number of offspring that a species can produce if resources were unlimited
It is regulated by four factors
1) Birth potential maximum number of offspring per birth
2) Capacity of survival number of offspring that reach reproductive age
3) Procreation number of times a species reproduces each year
4) Length of reproductive life the age of sexual maturity and the number of years the individual can reproduce
Limiting Factors
The environment provides factors that prevent populations from attaining their biotic potential Environmental Factor Population Changes
Abiotic light temperaturechemical environment
Biotic Amount of foodnumber or effectiveness of predatorsdiseases and parasitesability to compete for resources
Some factors that control population can depend on the size or density of the population
A population is dense when a large number of organisms live in one area
Density IndependentFactors
Density DependentFactors
Flood Food shortage
Fire Competition for mates or habitat
Pesticides Diseases
Change in climate or temperature
Introduction of exotic species
Destruction of habitat Increased predation
Drought Competition for water and other resources
Questions
Read pages 77-80 and do questions 1 2 amp 3 (abc) on page 80
Chapter 3Sustaining Terrestrial Ecosystems
Section 31 Canadian Biomes
Jigsaw Activity
bull In groups you will be using pages 88-93 to complete the sheets on ldquoThe Canadian Biomesrdquo
bull Video Response Biomes (Earth at Risk Series)
Canadian Biomes Biome ndash a collection of ecosystems that are
similar or related to each other usually in the type of plants they support
Four Canadian Biomes
The Tundra The Boreal Forest The Temperate Deciduous
Forest The Grassland
Tundra
Boreal Forest
Grassland
Temperate Deciduous Forest
The Tundra- Canadarsquos northernmost biome
Biotic FactorsAbiotic Factors
very low temp for most
of the year
short growing season
Permafrost layer beneath the soil
low precipitation
poor soil quality
rapid-growing plants
mosses and lichens
caribou
ptarmigan
lemmings
arctic foxes
wolverines
Similar to a desert low precipitation (10-12 cmyear) supports a low number of species
Two layers of soil Permafrost ndash layer of soil that never thaws Active Layer ndash above permafrost thaws in summer allowing
roots to take in water and minerals
Decomposition of Organic Matter extremely slow in cold temp because cold keeps the
bacteria and fungi from reproducing This leaves only a small amount of organic material in the soil
Nitrogen and Carbon Cycles slows the rates of the cycles slow decomposition with surface water causes the
formation of bogs These store carbon for long periods of time and decrease denitrification
The Boreal Forest- Immediately south of the Tundra
Biotic FactorsAbiotic Factors
warmer than the Tundra
no permafrost
changeable weather
soils contains some water and is acidic
precipitation 40 cmyear or more
coniferous trees
seed-eating birds
squirrels
voles
snowshoe hare
deer
pine martens
grey wolves
Climate harsh with rapid changes in temp mixing warm and cool air results in
more precipitation
Soil warmer temp allows the soil to thaw every season higher organic matter from faster rates of decomposition soil is more acidic as coniferous needles produce acid when they decay
ndash this can limit the number of plants that can grow
What are conifers Trees with needle shaped leaves ndash evergreens
4 Reasons why conifers are dominant Thin needles have a small surface area so they lose little water during
winter Thick cuticle of wax covers the needles to reduce water loss and
protect from frost damage Pyramid shape of tree and flexible branches allow the tree to support
heavy snowfall Shed their leaves slowly throughout the year so they can begin
photosynthesis when the growing season begins (advantage in a short growing season)
The Temperate Deciduous Forest- South of the Boreal Forest in EasternCentral Canada
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp then Tundra or Boreal Forest
fertile soil
precipitation up to
100 cmyear
deciduous trees
many ferns and shrubs
tree and ground squirrels
many insects
shrews and mice
deer
woodpeckers
weasels black bears wolves
What are the dominant trees in
this biome Deciduous trees (maples oaks poplars
beech and birch)
What features about deciduous trees allow them to complete with conifers
The broad leaves maximize light capture for photosynthesis
Soil and Decomposition
higher temperatures allow for faster decomposition resulting in richer
soil
Understory and Canopy Understory ndash the lower branches of a trees
Canopy ndash the upper levels of the trees
What factors allow for high biodiversity in this biome
The presence of so many different kinds of plants supports many
animals
The thick litter layer is ideal for different insects
Many insects support amphibians lizards birds and insect-eating animals
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
The Carbon Cycle
Carbon ReservoirsReservoirs of Inorganic Carbon When carbon is not in organic form it can be found in three
types of storage (reservoirs)
Atmosphere (smallest ~ 003) Oceans (largest) Earthrsquos crust
Reservoirs for Organic Carbon Organic carbon is held in the bodies of living organisms
All living things eventually die and return their carbon in an inorganic form The only exception to this are bogs which have large quantities of organic carbon which may be stored for years in the peat (dead plant matter)
Humans have modified the carbon cycle by releasing large quantities of organic carbon
Example mining coal burning fossil fuels and burning forests
Assignment
read pages 62-65 and do the assigned questions for the Carbon Cycle(handout)
Play the Carbon Cycle Game httpwwwwindowsucareduearthclimatecarbon_cyclehtml
Section 26-The Nitrogen and Phosphorus Cycles
The Nitrogen Cycle
Life depends on the cycling of nitrogen used by cells to make protein in plants and
animals
used to make DNA in plant and animal cells
used as fertilizer to make plants grow
The atmosphere is 79 nitrogen all of which is unusable by plants and animals
Nitrogen is changed into nitrates (usable form) by
lightning
nitrogen fixing bacteria
Nitrogen Fixation Through Lightning energy from the lightning causes nitrogen gas to
react with oxygen gas to produce nitrates
the nitrates dissolve in rain or surface water enter the soil and then move into plants through their roots
Nitrogen Fixation by Bacteria bacteria found in the soil provide the vast majority
of nitrates in the ecosystem Some bacteria may also be found in small lumps called nodules on the roots of some plants
called nitrogen fixing bacteria
Denitrification involves the decay process in which denitrifying bacteria break down nitrates into nitrites and then into nitrogen gas which goes up into the air
This process ensures the balance between soil nitrates nitrites and nitrogen gas
Denitrifying bacteria grow well in areas of low oxygen like lawns By aerating your lawn (adding more oxygen) the breakdown of nitrates into nitrogen gas is reduced and your lawn will stay green longer (nitrates stay in your lawn)
Nitrogen Cycle Animation
Assignment
Read pages 66-67 and complete the assigned questions for the Nitrogen Cycle(handout)
Play the Nitrogen Cycle Game httpwwwwindowsucaredutourlink=teach
er_resourcesteach_nitrogenhtml
The Phosphorus CyclePhosphorous cycles in two ways
Long term in rocks in the Earthrsquos crust phosphates eroded from rock are carried away by rivers and
lakes and end up in the ocean animals use the phosphates to make bones and shells when these animal die they end up at the bottom of the
ocean where over time they may become rock again Plants also absorb phosphates from the water
Short term in living organisms phosphates in dead organisms are recycled by
decomposers which break them down and release the phosphates back into the ecosystem
Phosphorus Cycle
Assignment
bullRead page 68 and complete the questions on the Phosphorus Cycle (handout)
Phosphorus Cycle Animation
Phosphorus Cycle
Section 22-Pesticides
Pesticides are chemicals used to kill insects weeds and microorganisms that might damage crops
Why Use Pesticides Up to 30 of crops in Canada are destroyed by pests This impacts the farmerrsquos income and the price that we pay for the produce
First Generation Pesticides
Pest control dates back to 500 BCE Toxic chemicals were frequently used until we discovered they were more dangerous to us than to the pests
Second Generation Pesticidesbull chemicals made in a lab
bull Can be grouped into four categories
Type Target Examples Persistence
Insecticide Insects DDT 2 - 15 years
Herbicide Weeds Roundup Days to weeks
Fungicide Moulds
and fungi Captan Days
Bactericides Bacteria Penicillin Days
Assignment
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Complete the sheet on histograms (handout)
Play the ldquoOh Deer Gamerdquohttpwwwriverventureorgcharlestonresourcespdfpopulation20study20gamepdf
Bioamplification
When water insoluble pesticides enter food chains the animals that eat them canrsquot break them down so they stay in their bodies The pesticides stay in the fatty tissue The pesticides then built up in a process called bioamplification
DDTbullDDT was the first modern pesticide developed to kill mosquitoes that spread malaria and typhus
bullIn 1962 an American activist named Rachel Carson published a book which alleged that DDT caused cancer and harmed bird reproduction This information led to the pesticide being banned in 1971
bullAlthough it is not being used in North America it is still being used in other countries and can be transmitted through bioamplification
DDT Video
Modern Chemical PesticidesNew pesticides are now water soluble and do not
build up in the tissues of animals They are safer but still have negative effects such as1 They break down quickly so they have to be spread
more often (cost more)
2 They are not selective so they can also kill birds reptiles amphibians and fish
3 Animals that do not die immediately may still put others at risk through bioamplification
4 They have a shelf life meaning that they become ineffective after a while
The Pests Fight Back Pests that reproduce often start to become
resistant to pesticides The first time using a chemical you will probably
kill 90 of the insects and the 10 that are left alive will reproduce
The 10 that survived probably had a natural resistance to the chemical Many of their offspring will also have the resistance After several generations the chemical is not as effective
New pesticides must be developed to take their place
Assignment
Read pages 52-57 and do questions 1-7 on page 58
Read pages 81-82 andmake a list of 4 pros and 4 cons for pesticide usage in controlling tentcaterpillars
Section 29-Monitoring Changes in Population
During the last three centuries global population has risen at an exponential rate
500 million in 16501 billion in 18502 billion in 19304 billion in 1975estimated at 8 billion in 2013
Population Growth Patterns Changes in population size occur when people
are added or removed from the population The four factors involved in population growth
are
1 Natality the number of offspring born in one year
2 Mortality the number of individuals that die in one year
3 Immigration the number of individuals moving into a population
4 Emigration the number of individuals moving out of a population
Population Growth = ( Births + Immigration) - ( Deaths + Emigration)
Open and Closed Populations
An open population occurs when all four factors are acting on the population
(Ex The population of Charlottetown)
A closed population occurs when only natality and mortality affect the population size
(Ex Population of the Earth)
Population Histogramsbulluseful when studying population of long-lived organisms such as humans
bullThe shape of pyramid allows you to predict changes in the populations
bullA wide base indicates that the population is rapidly growing
bull When the base is narrower than the middle section fewer offspring are produced and population will decline
Questions
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Section 210-Limits on Populations
Mice populations can change drastically in 6 months 20 mice can become 5120 mice
Why donrsquot we see billionsof mice when we lookout the window
The reason is that there are limitations on all populations including mice
Carrying Capacity
Populations fluctuate but tend to be fairly stable Stabilityhappens when the population does not exceed the carryingcapacity
Carrying Capacity - The maximum number of individual species that can be supported by an ecosystem
Law of Minimum - The nutrient in least supply is the one that limits growth
Law of Tolerance - An organism can survive within a certain range of abiotic factors Going above or below this range will cause death
Biotic potential is the maximum number of offspring that a species can produce if resources were unlimited
It is regulated by four factors
1) Birth potential maximum number of offspring per birth
2) Capacity of survival number of offspring that reach reproductive age
3) Procreation number of times a species reproduces each year
4) Length of reproductive life the age of sexual maturity and the number of years the individual can reproduce
Limiting Factors
The environment provides factors that prevent populations from attaining their biotic potential Environmental Factor Population Changes
Abiotic light temperaturechemical environment
Biotic Amount of foodnumber or effectiveness of predatorsdiseases and parasitesability to compete for resources
Some factors that control population can depend on the size or density of the population
A population is dense when a large number of organisms live in one area
Density IndependentFactors
Density DependentFactors
Flood Food shortage
Fire Competition for mates or habitat
Pesticides Diseases
Change in climate or temperature
Introduction of exotic species
Destruction of habitat Increased predation
Drought Competition for water and other resources
Questions
Read pages 77-80 and do questions 1 2 amp 3 (abc) on page 80
Chapter 3Sustaining Terrestrial Ecosystems
Section 31 Canadian Biomes
Jigsaw Activity
bull In groups you will be using pages 88-93 to complete the sheets on ldquoThe Canadian Biomesrdquo
bull Video Response Biomes (Earth at Risk Series)
Canadian Biomes Biome ndash a collection of ecosystems that are
similar or related to each other usually in the type of plants they support
Four Canadian Biomes
The Tundra The Boreal Forest The Temperate Deciduous
Forest The Grassland
Tundra
Boreal Forest
Grassland
Temperate Deciduous Forest
The Tundra- Canadarsquos northernmost biome
Biotic FactorsAbiotic Factors
very low temp for most
of the year
short growing season
Permafrost layer beneath the soil
low precipitation
poor soil quality
rapid-growing plants
mosses and lichens
caribou
ptarmigan
lemmings
arctic foxes
wolverines
Similar to a desert low precipitation (10-12 cmyear) supports a low number of species
Two layers of soil Permafrost ndash layer of soil that never thaws Active Layer ndash above permafrost thaws in summer allowing
roots to take in water and minerals
Decomposition of Organic Matter extremely slow in cold temp because cold keeps the
bacteria and fungi from reproducing This leaves only a small amount of organic material in the soil
Nitrogen and Carbon Cycles slows the rates of the cycles slow decomposition with surface water causes the
formation of bogs These store carbon for long periods of time and decrease denitrification
The Boreal Forest- Immediately south of the Tundra
Biotic FactorsAbiotic Factors
warmer than the Tundra
no permafrost
changeable weather
soils contains some water and is acidic
precipitation 40 cmyear or more
coniferous trees
seed-eating birds
squirrels
voles
snowshoe hare
deer
pine martens
grey wolves
Climate harsh with rapid changes in temp mixing warm and cool air results in
more precipitation
Soil warmer temp allows the soil to thaw every season higher organic matter from faster rates of decomposition soil is more acidic as coniferous needles produce acid when they decay
ndash this can limit the number of plants that can grow
What are conifers Trees with needle shaped leaves ndash evergreens
4 Reasons why conifers are dominant Thin needles have a small surface area so they lose little water during
winter Thick cuticle of wax covers the needles to reduce water loss and
protect from frost damage Pyramid shape of tree and flexible branches allow the tree to support
heavy snowfall Shed their leaves slowly throughout the year so they can begin
photosynthesis when the growing season begins (advantage in a short growing season)
The Temperate Deciduous Forest- South of the Boreal Forest in EasternCentral Canada
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp then Tundra or Boreal Forest
fertile soil
precipitation up to
100 cmyear
deciduous trees
many ferns and shrubs
tree and ground squirrels
many insects
shrews and mice
deer
woodpeckers
weasels black bears wolves
What are the dominant trees in
this biome Deciduous trees (maples oaks poplars
beech and birch)
What features about deciduous trees allow them to complete with conifers
The broad leaves maximize light capture for photosynthesis
Soil and Decomposition
higher temperatures allow for faster decomposition resulting in richer
soil
Understory and Canopy Understory ndash the lower branches of a trees
Canopy ndash the upper levels of the trees
What factors allow for high biodiversity in this biome
The presence of so many different kinds of plants supports many
animals
The thick litter layer is ideal for different insects
Many insects support amphibians lizards birds and insect-eating animals
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
Carbon ReservoirsReservoirs of Inorganic Carbon When carbon is not in organic form it can be found in three
types of storage (reservoirs)
Atmosphere (smallest ~ 003) Oceans (largest) Earthrsquos crust
Reservoirs for Organic Carbon Organic carbon is held in the bodies of living organisms
All living things eventually die and return their carbon in an inorganic form The only exception to this are bogs which have large quantities of organic carbon which may be stored for years in the peat (dead plant matter)
Humans have modified the carbon cycle by releasing large quantities of organic carbon
Example mining coal burning fossil fuels and burning forests
Assignment
read pages 62-65 and do the assigned questions for the Carbon Cycle(handout)
Play the Carbon Cycle Game httpwwwwindowsucareduearthclimatecarbon_cyclehtml
Section 26-The Nitrogen and Phosphorus Cycles
The Nitrogen Cycle
Life depends on the cycling of nitrogen used by cells to make protein in plants and
animals
used to make DNA in plant and animal cells
used as fertilizer to make plants grow
The atmosphere is 79 nitrogen all of which is unusable by plants and animals
Nitrogen is changed into nitrates (usable form) by
lightning
nitrogen fixing bacteria
Nitrogen Fixation Through Lightning energy from the lightning causes nitrogen gas to
react with oxygen gas to produce nitrates
the nitrates dissolve in rain or surface water enter the soil and then move into plants through their roots
Nitrogen Fixation by Bacteria bacteria found in the soil provide the vast majority
of nitrates in the ecosystem Some bacteria may also be found in small lumps called nodules on the roots of some plants
called nitrogen fixing bacteria
Denitrification involves the decay process in which denitrifying bacteria break down nitrates into nitrites and then into nitrogen gas which goes up into the air
This process ensures the balance between soil nitrates nitrites and nitrogen gas
Denitrifying bacteria grow well in areas of low oxygen like lawns By aerating your lawn (adding more oxygen) the breakdown of nitrates into nitrogen gas is reduced and your lawn will stay green longer (nitrates stay in your lawn)
Nitrogen Cycle Animation
Assignment
Read pages 66-67 and complete the assigned questions for the Nitrogen Cycle(handout)
Play the Nitrogen Cycle Game httpwwwwindowsucaredutourlink=teach
er_resourcesteach_nitrogenhtml
The Phosphorus CyclePhosphorous cycles in two ways
Long term in rocks in the Earthrsquos crust phosphates eroded from rock are carried away by rivers and
lakes and end up in the ocean animals use the phosphates to make bones and shells when these animal die they end up at the bottom of the
ocean where over time they may become rock again Plants also absorb phosphates from the water
Short term in living organisms phosphates in dead organisms are recycled by
decomposers which break them down and release the phosphates back into the ecosystem
Phosphorus Cycle
Assignment
bullRead page 68 and complete the questions on the Phosphorus Cycle (handout)
Phosphorus Cycle Animation
Phosphorus Cycle
Section 22-Pesticides
Pesticides are chemicals used to kill insects weeds and microorganisms that might damage crops
Why Use Pesticides Up to 30 of crops in Canada are destroyed by pests This impacts the farmerrsquos income and the price that we pay for the produce
First Generation Pesticides
Pest control dates back to 500 BCE Toxic chemicals were frequently used until we discovered they were more dangerous to us than to the pests
Second Generation Pesticidesbull chemicals made in a lab
bull Can be grouped into four categories
Type Target Examples Persistence
Insecticide Insects DDT 2 - 15 years
Herbicide Weeds Roundup Days to weeks
Fungicide Moulds
and fungi Captan Days
Bactericides Bacteria Penicillin Days
Assignment
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Complete the sheet on histograms (handout)
Play the ldquoOh Deer Gamerdquohttpwwwriverventureorgcharlestonresourcespdfpopulation20study20gamepdf
Bioamplification
When water insoluble pesticides enter food chains the animals that eat them canrsquot break them down so they stay in their bodies The pesticides stay in the fatty tissue The pesticides then built up in a process called bioamplification
DDTbullDDT was the first modern pesticide developed to kill mosquitoes that spread malaria and typhus
bullIn 1962 an American activist named Rachel Carson published a book which alleged that DDT caused cancer and harmed bird reproduction This information led to the pesticide being banned in 1971
bullAlthough it is not being used in North America it is still being used in other countries and can be transmitted through bioamplification
DDT Video
Modern Chemical PesticidesNew pesticides are now water soluble and do not
build up in the tissues of animals They are safer but still have negative effects such as1 They break down quickly so they have to be spread
more often (cost more)
2 They are not selective so they can also kill birds reptiles amphibians and fish
3 Animals that do not die immediately may still put others at risk through bioamplification
4 They have a shelf life meaning that they become ineffective after a while
The Pests Fight Back Pests that reproduce often start to become
resistant to pesticides The first time using a chemical you will probably
kill 90 of the insects and the 10 that are left alive will reproduce
The 10 that survived probably had a natural resistance to the chemical Many of their offspring will also have the resistance After several generations the chemical is not as effective
New pesticides must be developed to take their place
Assignment
Read pages 52-57 and do questions 1-7 on page 58
Read pages 81-82 andmake a list of 4 pros and 4 cons for pesticide usage in controlling tentcaterpillars
Section 29-Monitoring Changes in Population
During the last three centuries global population has risen at an exponential rate
500 million in 16501 billion in 18502 billion in 19304 billion in 1975estimated at 8 billion in 2013
Population Growth Patterns Changes in population size occur when people
are added or removed from the population The four factors involved in population growth
are
1 Natality the number of offspring born in one year
2 Mortality the number of individuals that die in one year
3 Immigration the number of individuals moving into a population
4 Emigration the number of individuals moving out of a population
Population Growth = ( Births + Immigration) - ( Deaths + Emigration)
Open and Closed Populations
An open population occurs when all four factors are acting on the population
(Ex The population of Charlottetown)
A closed population occurs when only natality and mortality affect the population size
(Ex Population of the Earth)
Population Histogramsbulluseful when studying population of long-lived organisms such as humans
bullThe shape of pyramid allows you to predict changes in the populations
bullA wide base indicates that the population is rapidly growing
bull When the base is narrower than the middle section fewer offspring are produced and population will decline
Questions
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Section 210-Limits on Populations
Mice populations can change drastically in 6 months 20 mice can become 5120 mice
Why donrsquot we see billionsof mice when we lookout the window
The reason is that there are limitations on all populations including mice
Carrying Capacity
Populations fluctuate but tend to be fairly stable Stabilityhappens when the population does not exceed the carryingcapacity
Carrying Capacity - The maximum number of individual species that can be supported by an ecosystem
Law of Minimum - The nutrient in least supply is the one that limits growth
Law of Tolerance - An organism can survive within a certain range of abiotic factors Going above or below this range will cause death
Biotic potential is the maximum number of offspring that a species can produce if resources were unlimited
It is regulated by four factors
1) Birth potential maximum number of offspring per birth
2) Capacity of survival number of offspring that reach reproductive age
3) Procreation number of times a species reproduces each year
4) Length of reproductive life the age of sexual maturity and the number of years the individual can reproduce
Limiting Factors
The environment provides factors that prevent populations from attaining their biotic potential Environmental Factor Population Changes
Abiotic light temperaturechemical environment
Biotic Amount of foodnumber or effectiveness of predatorsdiseases and parasitesability to compete for resources
Some factors that control population can depend on the size or density of the population
A population is dense when a large number of organisms live in one area
Density IndependentFactors
Density DependentFactors
Flood Food shortage
Fire Competition for mates or habitat
Pesticides Diseases
Change in climate or temperature
Introduction of exotic species
Destruction of habitat Increased predation
Drought Competition for water and other resources
Questions
Read pages 77-80 and do questions 1 2 amp 3 (abc) on page 80
Chapter 3Sustaining Terrestrial Ecosystems
Section 31 Canadian Biomes
Jigsaw Activity
bull In groups you will be using pages 88-93 to complete the sheets on ldquoThe Canadian Biomesrdquo
bull Video Response Biomes (Earth at Risk Series)
Canadian Biomes Biome ndash a collection of ecosystems that are
similar or related to each other usually in the type of plants they support
Four Canadian Biomes
The Tundra The Boreal Forest The Temperate Deciduous
Forest The Grassland
Tundra
Boreal Forest
Grassland
Temperate Deciduous Forest
The Tundra- Canadarsquos northernmost biome
Biotic FactorsAbiotic Factors
very low temp for most
of the year
short growing season
Permafrost layer beneath the soil
low precipitation
poor soil quality
rapid-growing plants
mosses and lichens
caribou
ptarmigan
lemmings
arctic foxes
wolverines
Similar to a desert low precipitation (10-12 cmyear) supports a low number of species
Two layers of soil Permafrost ndash layer of soil that never thaws Active Layer ndash above permafrost thaws in summer allowing
roots to take in water and minerals
Decomposition of Organic Matter extremely slow in cold temp because cold keeps the
bacteria and fungi from reproducing This leaves only a small amount of organic material in the soil
Nitrogen and Carbon Cycles slows the rates of the cycles slow decomposition with surface water causes the
formation of bogs These store carbon for long periods of time and decrease denitrification
The Boreal Forest- Immediately south of the Tundra
Biotic FactorsAbiotic Factors
warmer than the Tundra
no permafrost
changeable weather
soils contains some water and is acidic
precipitation 40 cmyear or more
coniferous trees
seed-eating birds
squirrels
voles
snowshoe hare
deer
pine martens
grey wolves
Climate harsh with rapid changes in temp mixing warm and cool air results in
more precipitation
Soil warmer temp allows the soil to thaw every season higher organic matter from faster rates of decomposition soil is more acidic as coniferous needles produce acid when they decay
ndash this can limit the number of plants that can grow
What are conifers Trees with needle shaped leaves ndash evergreens
4 Reasons why conifers are dominant Thin needles have a small surface area so they lose little water during
winter Thick cuticle of wax covers the needles to reduce water loss and
protect from frost damage Pyramid shape of tree and flexible branches allow the tree to support
heavy snowfall Shed their leaves slowly throughout the year so they can begin
photosynthesis when the growing season begins (advantage in a short growing season)
The Temperate Deciduous Forest- South of the Boreal Forest in EasternCentral Canada
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp then Tundra or Boreal Forest
fertile soil
precipitation up to
100 cmyear
deciduous trees
many ferns and shrubs
tree and ground squirrels
many insects
shrews and mice
deer
woodpeckers
weasels black bears wolves
What are the dominant trees in
this biome Deciduous trees (maples oaks poplars
beech and birch)
What features about deciduous trees allow them to complete with conifers
The broad leaves maximize light capture for photosynthesis
Soil and Decomposition
higher temperatures allow for faster decomposition resulting in richer
soil
Understory and Canopy Understory ndash the lower branches of a trees
Canopy ndash the upper levels of the trees
What factors allow for high biodiversity in this biome
The presence of so many different kinds of plants supports many
animals
The thick litter layer is ideal for different insects
Many insects support amphibians lizards birds and insect-eating animals
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
Humans have modified the carbon cycle by releasing large quantities of organic carbon
Example mining coal burning fossil fuels and burning forests
Assignment
read pages 62-65 and do the assigned questions for the Carbon Cycle(handout)
Play the Carbon Cycle Game httpwwwwindowsucareduearthclimatecarbon_cyclehtml
Section 26-The Nitrogen and Phosphorus Cycles
The Nitrogen Cycle
Life depends on the cycling of nitrogen used by cells to make protein in plants and
animals
used to make DNA in plant and animal cells
used as fertilizer to make plants grow
The atmosphere is 79 nitrogen all of which is unusable by plants and animals
Nitrogen is changed into nitrates (usable form) by
lightning
nitrogen fixing bacteria
Nitrogen Fixation Through Lightning energy from the lightning causes nitrogen gas to
react with oxygen gas to produce nitrates
the nitrates dissolve in rain or surface water enter the soil and then move into plants through their roots
Nitrogen Fixation by Bacteria bacteria found in the soil provide the vast majority
of nitrates in the ecosystem Some bacteria may also be found in small lumps called nodules on the roots of some plants
called nitrogen fixing bacteria
Denitrification involves the decay process in which denitrifying bacteria break down nitrates into nitrites and then into nitrogen gas which goes up into the air
This process ensures the balance between soil nitrates nitrites and nitrogen gas
Denitrifying bacteria grow well in areas of low oxygen like lawns By aerating your lawn (adding more oxygen) the breakdown of nitrates into nitrogen gas is reduced and your lawn will stay green longer (nitrates stay in your lawn)
Nitrogen Cycle Animation
Assignment
Read pages 66-67 and complete the assigned questions for the Nitrogen Cycle(handout)
Play the Nitrogen Cycle Game httpwwwwindowsucaredutourlink=teach
er_resourcesteach_nitrogenhtml
The Phosphorus CyclePhosphorous cycles in two ways
Long term in rocks in the Earthrsquos crust phosphates eroded from rock are carried away by rivers and
lakes and end up in the ocean animals use the phosphates to make bones and shells when these animal die they end up at the bottom of the
ocean where over time they may become rock again Plants also absorb phosphates from the water
Short term in living organisms phosphates in dead organisms are recycled by
decomposers which break them down and release the phosphates back into the ecosystem
Phosphorus Cycle
Assignment
bullRead page 68 and complete the questions on the Phosphorus Cycle (handout)
Phosphorus Cycle Animation
Phosphorus Cycle
Section 22-Pesticides
Pesticides are chemicals used to kill insects weeds and microorganisms that might damage crops
Why Use Pesticides Up to 30 of crops in Canada are destroyed by pests This impacts the farmerrsquos income and the price that we pay for the produce
First Generation Pesticides
Pest control dates back to 500 BCE Toxic chemicals were frequently used until we discovered they were more dangerous to us than to the pests
Second Generation Pesticidesbull chemicals made in a lab
bull Can be grouped into four categories
Type Target Examples Persistence
Insecticide Insects DDT 2 - 15 years
Herbicide Weeds Roundup Days to weeks
Fungicide Moulds
and fungi Captan Days
Bactericides Bacteria Penicillin Days
Assignment
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Complete the sheet on histograms (handout)
Play the ldquoOh Deer Gamerdquohttpwwwriverventureorgcharlestonresourcespdfpopulation20study20gamepdf
Bioamplification
When water insoluble pesticides enter food chains the animals that eat them canrsquot break them down so they stay in their bodies The pesticides stay in the fatty tissue The pesticides then built up in a process called bioamplification
DDTbullDDT was the first modern pesticide developed to kill mosquitoes that spread malaria and typhus
bullIn 1962 an American activist named Rachel Carson published a book which alleged that DDT caused cancer and harmed bird reproduction This information led to the pesticide being banned in 1971
bullAlthough it is not being used in North America it is still being used in other countries and can be transmitted through bioamplification
DDT Video
Modern Chemical PesticidesNew pesticides are now water soluble and do not
build up in the tissues of animals They are safer but still have negative effects such as1 They break down quickly so they have to be spread
more often (cost more)
2 They are not selective so they can also kill birds reptiles amphibians and fish
3 Animals that do not die immediately may still put others at risk through bioamplification
4 They have a shelf life meaning that they become ineffective after a while
The Pests Fight Back Pests that reproduce often start to become
resistant to pesticides The first time using a chemical you will probably
kill 90 of the insects and the 10 that are left alive will reproduce
The 10 that survived probably had a natural resistance to the chemical Many of their offspring will also have the resistance After several generations the chemical is not as effective
New pesticides must be developed to take their place
Assignment
Read pages 52-57 and do questions 1-7 on page 58
Read pages 81-82 andmake a list of 4 pros and 4 cons for pesticide usage in controlling tentcaterpillars
Section 29-Monitoring Changes in Population
During the last three centuries global population has risen at an exponential rate
500 million in 16501 billion in 18502 billion in 19304 billion in 1975estimated at 8 billion in 2013
Population Growth Patterns Changes in population size occur when people
are added or removed from the population The four factors involved in population growth
are
1 Natality the number of offspring born in one year
2 Mortality the number of individuals that die in one year
3 Immigration the number of individuals moving into a population
4 Emigration the number of individuals moving out of a population
Population Growth = ( Births + Immigration) - ( Deaths + Emigration)
Open and Closed Populations
An open population occurs when all four factors are acting on the population
(Ex The population of Charlottetown)
A closed population occurs when only natality and mortality affect the population size
(Ex Population of the Earth)
Population Histogramsbulluseful when studying population of long-lived organisms such as humans
bullThe shape of pyramid allows you to predict changes in the populations
bullA wide base indicates that the population is rapidly growing
bull When the base is narrower than the middle section fewer offspring are produced and population will decline
Questions
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Section 210-Limits on Populations
Mice populations can change drastically in 6 months 20 mice can become 5120 mice
Why donrsquot we see billionsof mice when we lookout the window
The reason is that there are limitations on all populations including mice
Carrying Capacity
Populations fluctuate but tend to be fairly stable Stabilityhappens when the population does not exceed the carryingcapacity
Carrying Capacity - The maximum number of individual species that can be supported by an ecosystem
Law of Minimum - The nutrient in least supply is the one that limits growth
Law of Tolerance - An organism can survive within a certain range of abiotic factors Going above or below this range will cause death
Biotic potential is the maximum number of offspring that a species can produce if resources were unlimited
It is regulated by four factors
1) Birth potential maximum number of offspring per birth
2) Capacity of survival number of offspring that reach reproductive age
3) Procreation number of times a species reproduces each year
4) Length of reproductive life the age of sexual maturity and the number of years the individual can reproduce
Limiting Factors
The environment provides factors that prevent populations from attaining their biotic potential Environmental Factor Population Changes
Abiotic light temperaturechemical environment
Biotic Amount of foodnumber or effectiveness of predatorsdiseases and parasitesability to compete for resources
Some factors that control population can depend on the size or density of the population
A population is dense when a large number of organisms live in one area
Density IndependentFactors
Density DependentFactors
Flood Food shortage
Fire Competition for mates or habitat
Pesticides Diseases
Change in climate or temperature
Introduction of exotic species
Destruction of habitat Increased predation
Drought Competition for water and other resources
Questions
Read pages 77-80 and do questions 1 2 amp 3 (abc) on page 80
Chapter 3Sustaining Terrestrial Ecosystems
Section 31 Canadian Biomes
Jigsaw Activity
bull In groups you will be using pages 88-93 to complete the sheets on ldquoThe Canadian Biomesrdquo
bull Video Response Biomes (Earth at Risk Series)
Canadian Biomes Biome ndash a collection of ecosystems that are
similar or related to each other usually in the type of plants they support
Four Canadian Biomes
The Tundra The Boreal Forest The Temperate Deciduous
Forest The Grassland
Tundra
Boreal Forest
Grassland
Temperate Deciduous Forest
The Tundra- Canadarsquos northernmost biome
Biotic FactorsAbiotic Factors
very low temp for most
of the year
short growing season
Permafrost layer beneath the soil
low precipitation
poor soil quality
rapid-growing plants
mosses and lichens
caribou
ptarmigan
lemmings
arctic foxes
wolverines
Similar to a desert low precipitation (10-12 cmyear) supports a low number of species
Two layers of soil Permafrost ndash layer of soil that never thaws Active Layer ndash above permafrost thaws in summer allowing
roots to take in water and minerals
Decomposition of Organic Matter extremely slow in cold temp because cold keeps the
bacteria and fungi from reproducing This leaves only a small amount of organic material in the soil
Nitrogen and Carbon Cycles slows the rates of the cycles slow decomposition with surface water causes the
formation of bogs These store carbon for long periods of time and decrease denitrification
The Boreal Forest- Immediately south of the Tundra
Biotic FactorsAbiotic Factors
warmer than the Tundra
no permafrost
changeable weather
soils contains some water and is acidic
precipitation 40 cmyear or more
coniferous trees
seed-eating birds
squirrels
voles
snowshoe hare
deer
pine martens
grey wolves
Climate harsh with rapid changes in temp mixing warm and cool air results in
more precipitation
Soil warmer temp allows the soil to thaw every season higher organic matter from faster rates of decomposition soil is more acidic as coniferous needles produce acid when they decay
ndash this can limit the number of plants that can grow
What are conifers Trees with needle shaped leaves ndash evergreens
4 Reasons why conifers are dominant Thin needles have a small surface area so they lose little water during
winter Thick cuticle of wax covers the needles to reduce water loss and
protect from frost damage Pyramid shape of tree and flexible branches allow the tree to support
heavy snowfall Shed their leaves slowly throughout the year so they can begin
photosynthesis when the growing season begins (advantage in a short growing season)
The Temperate Deciduous Forest- South of the Boreal Forest in EasternCentral Canada
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp then Tundra or Boreal Forest
fertile soil
precipitation up to
100 cmyear
deciduous trees
many ferns and shrubs
tree and ground squirrels
many insects
shrews and mice
deer
woodpeckers
weasels black bears wolves
What are the dominant trees in
this biome Deciduous trees (maples oaks poplars
beech and birch)
What features about deciduous trees allow them to complete with conifers
The broad leaves maximize light capture for photosynthesis
Soil and Decomposition
higher temperatures allow for faster decomposition resulting in richer
soil
Understory and Canopy Understory ndash the lower branches of a trees
Canopy ndash the upper levels of the trees
What factors allow for high biodiversity in this biome
The presence of so many different kinds of plants supports many
animals
The thick litter layer is ideal for different insects
Many insects support amphibians lizards birds and insect-eating animals
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
Assignment
read pages 62-65 and do the assigned questions for the Carbon Cycle(handout)
Play the Carbon Cycle Game httpwwwwindowsucareduearthclimatecarbon_cyclehtml
Section 26-The Nitrogen and Phosphorus Cycles
The Nitrogen Cycle
Life depends on the cycling of nitrogen used by cells to make protein in plants and
animals
used to make DNA in plant and animal cells
used as fertilizer to make plants grow
The atmosphere is 79 nitrogen all of which is unusable by plants and animals
Nitrogen is changed into nitrates (usable form) by
lightning
nitrogen fixing bacteria
Nitrogen Fixation Through Lightning energy from the lightning causes nitrogen gas to
react with oxygen gas to produce nitrates
the nitrates dissolve in rain or surface water enter the soil and then move into plants through their roots
Nitrogen Fixation by Bacteria bacteria found in the soil provide the vast majority
of nitrates in the ecosystem Some bacteria may also be found in small lumps called nodules on the roots of some plants
called nitrogen fixing bacteria
Denitrification involves the decay process in which denitrifying bacteria break down nitrates into nitrites and then into nitrogen gas which goes up into the air
This process ensures the balance between soil nitrates nitrites and nitrogen gas
Denitrifying bacteria grow well in areas of low oxygen like lawns By aerating your lawn (adding more oxygen) the breakdown of nitrates into nitrogen gas is reduced and your lawn will stay green longer (nitrates stay in your lawn)
Nitrogen Cycle Animation
Assignment
Read pages 66-67 and complete the assigned questions for the Nitrogen Cycle(handout)
Play the Nitrogen Cycle Game httpwwwwindowsucaredutourlink=teach
er_resourcesteach_nitrogenhtml
The Phosphorus CyclePhosphorous cycles in two ways
Long term in rocks in the Earthrsquos crust phosphates eroded from rock are carried away by rivers and
lakes and end up in the ocean animals use the phosphates to make bones and shells when these animal die they end up at the bottom of the
ocean where over time they may become rock again Plants also absorb phosphates from the water
Short term in living organisms phosphates in dead organisms are recycled by
decomposers which break them down and release the phosphates back into the ecosystem
Phosphorus Cycle
Assignment
bullRead page 68 and complete the questions on the Phosphorus Cycle (handout)
Phosphorus Cycle Animation
Phosphorus Cycle
Section 22-Pesticides
Pesticides are chemicals used to kill insects weeds and microorganisms that might damage crops
Why Use Pesticides Up to 30 of crops in Canada are destroyed by pests This impacts the farmerrsquos income and the price that we pay for the produce
First Generation Pesticides
Pest control dates back to 500 BCE Toxic chemicals were frequently used until we discovered they were more dangerous to us than to the pests
Second Generation Pesticidesbull chemicals made in a lab
bull Can be grouped into four categories
Type Target Examples Persistence
Insecticide Insects DDT 2 - 15 years
Herbicide Weeds Roundup Days to weeks
Fungicide Moulds
and fungi Captan Days
Bactericides Bacteria Penicillin Days
Assignment
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Complete the sheet on histograms (handout)
Play the ldquoOh Deer Gamerdquohttpwwwriverventureorgcharlestonresourcespdfpopulation20study20gamepdf
Bioamplification
When water insoluble pesticides enter food chains the animals that eat them canrsquot break them down so they stay in their bodies The pesticides stay in the fatty tissue The pesticides then built up in a process called bioamplification
DDTbullDDT was the first modern pesticide developed to kill mosquitoes that spread malaria and typhus
bullIn 1962 an American activist named Rachel Carson published a book which alleged that DDT caused cancer and harmed bird reproduction This information led to the pesticide being banned in 1971
bullAlthough it is not being used in North America it is still being used in other countries and can be transmitted through bioamplification
DDT Video
Modern Chemical PesticidesNew pesticides are now water soluble and do not
build up in the tissues of animals They are safer but still have negative effects such as1 They break down quickly so they have to be spread
more often (cost more)
2 They are not selective so they can also kill birds reptiles amphibians and fish
3 Animals that do not die immediately may still put others at risk through bioamplification
4 They have a shelf life meaning that they become ineffective after a while
The Pests Fight Back Pests that reproduce often start to become
resistant to pesticides The first time using a chemical you will probably
kill 90 of the insects and the 10 that are left alive will reproduce
The 10 that survived probably had a natural resistance to the chemical Many of their offspring will also have the resistance After several generations the chemical is not as effective
New pesticides must be developed to take their place
Assignment
Read pages 52-57 and do questions 1-7 on page 58
Read pages 81-82 andmake a list of 4 pros and 4 cons for pesticide usage in controlling tentcaterpillars
Section 29-Monitoring Changes in Population
During the last three centuries global population has risen at an exponential rate
500 million in 16501 billion in 18502 billion in 19304 billion in 1975estimated at 8 billion in 2013
Population Growth Patterns Changes in population size occur when people
are added or removed from the population The four factors involved in population growth
are
1 Natality the number of offspring born in one year
2 Mortality the number of individuals that die in one year
3 Immigration the number of individuals moving into a population
4 Emigration the number of individuals moving out of a population
Population Growth = ( Births + Immigration) - ( Deaths + Emigration)
Open and Closed Populations
An open population occurs when all four factors are acting on the population
(Ex The population of Charlottetown)
A closed population occurs when only natality and mortality affect the population size
(Ex Population of the Earth)
Population Histogramsbulluseful when studying population of long-lived organisms such as humans
bullThe shape of pyramid allows you to predict changes in the populations
bullA wide base indicates that the population is rapidly growing
bull When the base is narrower than the middle section fewer offspring are produced and population will decline
Questions
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Section 210-Limits on Populations
Mice populations can change drastically in 6 months 20 mice can become 5120 mice
Why donrsquot we see billionsof mice when we lookout the window
The reason is that there are limitations on all populations including mice
Carrying Capacity
Populations fluctuate but tend to be fairly stable Stabilityhappens when the population does not exceed the carryingcapacity
Carrying Capacity - The maximum number of individual species that can be supported by an ecosystem
Law of Minimum - The nutrient in least supply is the one that limits growth
Law of Tolerance - An organism can survive within a certain range of abiotic factors Going above or below this range will cause death
Biotic potential is the maximum number of offspring that a species can produce if resources were unlimited
It is regulated by four factors
1) Birth potential maximum number of offspring per birth
2) Capacity of survival number of offspring that reach reproductive age
3) Procreation number of times a species reproduces each year
4) Length of reproductive life the age of sexual maturity and the number of years the individual can reproduce
Limiting Factors
The environment provides factors that prevent populations from attaining their biotic potential Environmental Factor Population Changes
Abiotic light temperaturechemical environment
Biotic Amount of foodnumber or effectiveness of predatorsdiseases and parasitesability to compete for resources
Some factors that control population can depend on the size or density of the population
A population is dense when a large number of organisms live in one area
Density IndependentFactors
Density DependentFactors
Flood Food shortage
Fire Competition for mates or habitat
Pesticides Diseases
Change in climate or temperature
Introduction of exotic species
Destruction of habitat Increased predation
Drought Competition for water and other resources
Questions
Read pages 77-80 and do questions 1 2 amp 3 (abc) on page 80
Chapter 3Sustaining Terrestrial Ecosystems
Section 31 Canadian Biomes
Jigsaw Activity
bull In groups you will be using pages 88-93 to complete the sheets on ldquoThe Canadian Biomesrdquo
bull Video Response Biomes (Earth at Risk Series)
Canadian Biomes Biome ndash a collection of ecosystems that are
similar or related to each other usually in the type of plants they support
Four Canadian Biomes
The Tundra The Boreal Forest The Temperate Deciduous
Forest The Grassland
Tundra
Boreal Forest
Grassland
Temperate Deciduous Forest
The Tundra- Canadarsquos northernmost biome
Biotic FactorsAbiotic Factors
very low temp for most
of the year
short growing season
Permafrost layer beneath the soil
low precipitation
poor soil quality
rapid-growing plants
mosses and lichens
caribou
ptarmigan
lemmings
arctic foxes
wolverines
Similar to a desert low precipitation (10-12 cmyear) supports a low number of species
Two layers of soil Permafrost ndash layer of soil that never thaws Active Layer ndash above permafrost thaws in summer allowing
roots to take in water and minerals
Decomposition of Organic Matter extremely slow in cold temp because cold keeps the
bacteria and fungi from reproducing This leaves only a small amount of organic material in the soil
Nitrogen and Carbon Cycles slows the rates of the cycles slow decomposition with surface water causes the
formation of bogs These store carbon for long periods of time and decrease denitrification
The Boreal Forest- Immediately south of the Tundra
Biotic FactorsAbiotic Factors
warmer than the Tundra
no permafrost
changeable weather
soils contains some water and is acidic
precipitation 40 cmyear or more
coniferous trees
seed-eating birds
squirrels
voles
snowshoe hare
deer
pine martens
grey wolves
Climate harsh with rapid changes in temp mixing warm and cool air results in
more precipitation
Soil warmer temp allows the soil to thaw every season higher organic matter from faster rates of decomposition soil is more acidic as coniferous needles produce acid when they decay
ndash this can limit the number of plants that can grow
What are conifers Trees with needle shaped leaves ndash evergreens
4 Reasons why conifers are dominant Thin needles have a small surface area so they lose little water during
winter Thick cuticle of wax covers the needles to reduce water loss and
protect from frost damage Pyramid shape of tree and flexible branches allow the tree to support
heavy snowfall Shed their leaves slowly throughout the year so they can begin
photosynthesis when the growing season begins (advantage in a short growing season)
The Temperate Deciduous Forest- South of the Boreal Forest in EasternCentral Canada
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp then Tundra or Boreal Forest
fertile soil
precipitation up to
100 cmyear
deciduous trees
many ferns and shrubs
tree and ground squirrels
many insects
shrews and mice
deer
woodpeckers
weasels black bears wolves
What are the dominant trees in
this biome Deciduous trees (maples oaks poplars
beech and birch)
What features about deciduous trees allow them to complete with conifers
The broad leaves maximize light capture for photosynthesis
Soil and Decomposition
higher temperatures allow for faster decomposition resulting in richer
soil
Understory and Canopy Understory ndash the lower branches of a trees
Canopy ndash the upper levels of the trees
What factors allow for high biodiversity in this biome
The presence of so many different kinds of plants supports many
animals
The thick litter layer is ideal for different insects
Many insects support amphibians lizards birds and insect-eating animals
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
Section 26-The Nitrogen and Phosphorus Cycles
The Nitrogen Cycle
Life depends on the cycling of nitrogen used by cells to make protein in plants and
animals
used to make DNA in plant and animal cells
used as fertilizer to make plants grow
The atmosphere is 79 nitrogen all of which is unusable by plants and animals
Nitrogen is changed into nitrates (usable form) by
lightning
nitrogen fixing bacteria
Nitrogen Fixation Through Lightning energy from the lightning causes nitrogen gas to
react with oxygen gas to produce nitrates
the nitrates dissolve in rain or surface water enter the soil and then move into plants through their roots
Nitrogen Fixation by Bacteria bacteria found in the soil provide the vast majority
of nitrates in the ecosystem Some bacteria may also be found in small lumps called nodules on the roots of some plants
called nitrogen fixing bacteria
Denitrification involves the decay process in which denitrifying bacteria break down nitrates into nitrites and then into nitrogen gas which goes up into the air
This process ensures the balance between soil nitrates nitrites and nitrogen gas
Denitrifying bacteria grow well in areas of low oxygen like lawns By aerating your lawn (adding more oxygen) the breakdown of nitrates into nitrogen gas is reduced and your lawn will stay green longer (nitrates stay in your lawn)
Nitrogen Cycle Animation
Assignment
Read pages 66-67 and complete the assigned questions for the Nitrogen Cycle(handout)
Play the Nitrogen Cycle Game httpwwwwindowsucaredutourlink=teach
er_resourcesteach_nitrogenhtml
The Phosphorus CyclePhosphorous cycles in two ways
Long term in rocks in the Earthrsquos crust phosphates eroded from rock are carried away by rivers and
lakes and end up in the ocean animals use the phosphates to make bones and shells when these animal die they end up at the bottom of the
ocean where over time they may become rock again Plants also absorb phosphates from the water
Short term in living organisms phosphates in dead organisms are recycled by
decomposers which break them down and release the phosphates back into the ecosystem
Phosphorus Cycle
Assignment
bullRead page 68 and complete the questions on the Phosphorus Cycle (handout)
Phosphorus Cycle Animation
Phosphorus Cycle
Section 22-Pesticides
Pesticides are chemicals used to kill insects weeds and microorganisms that might damage crops
Why Use Pesticides Up to 30 of crops in Canada are destroyed by pests This impacts the farmerrsquos income and the price that we pay for the produce
First Generation Pesticides
Pest control dates back to 500 BCE Toxic chemicals were frequently used until we discovered they were more dangerous to us than to the pests
Second Generation Pesticidesbull chemicals made in a lab
bull Can be grouped into four categories
Type Target Examples Persistence
Insecticide Insects DDT 2 - 15 years
Herbicide Weeds Roundup Days to weeks
Fungicide Moulds
and fungi Captan Days
Bactericides Bacteria Penicillin Days
Assignment
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Complete the sheet on histograms (handout)
Play the ldquoOh Deer Gamerdquohttpwwwriverventureorgcharlestonresourcespdfpopulation20study20gamepdf
Bioamplification
When water insoluble pesticides enter food chains the animals that eat them canrsquot break them down so they stay in their bodies The pesticides stay in the fatty tissue The pesticides then built up in a process called bioamplification
DDTbullDDT was the first modern pesticide developed to kill mosquitoes that spread malaria and typhus
bullIn 1962 an American activist named Rachel Carson published a book which alleged that DDT caused cancer and harmed bird reproduction This information led to the pesticide being banned in 1971
bullAlthough it is not being used in North America it is still being used in other countries and can be transmitted through bioamplification
DDT Video
Modern Chemical PesticidesNew pesticides are now water soluble and do not
build up in the tissues of animals They are safer but still have negative effects such as1 They break down quickly so they have to be spread
more often (cost more)
2 They are not selective so they can also kill birds reptiles amphibians and fish
3 Animals that do not die immediately may still put others at risk through bioamplification
4 They have a shelf life meaning that they become ineffective after a while
The Pests Fight Back Pests that reproduce often start to become
resistant to pesticides The first time using a chemical you will probably
kill 90 of the insects and the 10 that are left alive will reproduce
The 10 that survived probably had a natural resistance to the chemical Many of their offspring will also have the resistance After several generations the chemical is not as effective
New pesticides must be developed to take their place
Assignment
Read pages 52-57 and do questions 1-7 on page 58
Read pages 81-82 andmake a list of 4 pros and 4 cons for pesticide usage in controlling tentcaterpillars
Section 29-Monitoring Changes in Population
During the last three centuries global population has risen at an exponential rate
500 million in 16501 billion in 18502 billion in 19304 billion in 1975estimated at 8 billion in 2013
Population Growth Patterns Changes in population size occur when people
are added or removed from the population The four factors involved in population growth
are
1 Natality the number of offspring born in one year
2 Mortality the number of individuals that die in one year
3 Immigration the number of individuals moving into a population
4 Emigration the number of individuals moving out of a population
Population Growth = ( Births + Immigration) - ( Deaths + Emigration)
Open and Closed Populations
An open population occurs when all four factors are acting on the population
(Ex The population of Charlottetown)
A closed population occurs when only natality and mortality affect the population size
(Ex Population of the Earth)
Population Histogramsbulluseful when studying population of long-lived organisms such as humans
bullThe shape of pyramid allows you to predict changes in the populations
bullA wide base indicates that the population is rapidly growing
bull When the base is narrower than the middle section fewer offspring are produced and population will decline
Questions
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Section 210-Limits on Populations
Mice populations can change drastically in 6 months 20 mice can become 5120 mice
Why donrsquot we see billionsof mice when we lookout the window
The reason is that there are limitations on all populations including mice
Carrying Capacity
Populations fluctuate but tend to be fairly stable Stabilityhappens when the population does not exceed the carryingcapacity
Carrying Capacity - The maximum number of individual species that can be supported by an ecosystem
Law of Minimum - The nutrient in least supply is the one that limits growth
Law of Tolerance - An organism can survive within a certain range of abiotic factors Going above or below this range will cause death
Biotic potential is the maximum number of offspring that a species can produce if resources were unlimited
It is regulated by four factors
1) Birth potential maximum number of offspring per birth
2) Capacity of survival number of offspring that reach reproductive age
3) Procreation number of times a species reproduces each year
4) Length of reproductive life the age of sexual maturity and the number of years the individual can reproduce
Limiting Factors
The environment provides factors that prevent populations from attaining their biotic potential Environmental Factor Population Changes
Abiotic light temperaturechemical environment
Biotic Amount of foodnumber or effectiveness of predatorsdiseases and parasitesability to compete for resources
Some factors that control population can depend on the size or density of the population
A population is dense when a large number of organisms live in one area
Density IndependentFactors
Density DependentFactors
Flood Food shortage
Fire Competition for mates or habitat
Pesticides Diseases
Change in climate or temperature
Introduction of exotic species
Destruction of habitat Increased predation
Drought Competition for water and other resources
Questions
Read pages 77-80 and do questions 1 2 amp 3 (abc) on page 80
Chapter 3Sustaining Terrestrial Ecosystems
Section 31 Canadian Biomes
Jigsaw Activity
bull In groups you will be using pages 88-93 to complete the sheets on ldquoThe Canadian Biomesrdquo
bull Video Response Biomes (Earth at Risk Series)
Canadian Biomes Biome ndash a collection of ecosystems that are
similar or related to each other usually in the type of plants they support
Four Canadian Biomes
The Tundra The Boreal Forest The Temperate Deciduous
Forest The Grassland
Tundra
Boreal Forest
Grassland
Temperate Deciduous Forest
The Tundra- Canadarsquos northernmost biome
Biotic FactorsAbiotic Factors
very low temp for most
of the year
short growing season
Permafrost layer beneath the soil
low precipitation
poor soil quality
rapid-growing plants
mosses and lichens
caribou
ptarmigan
lemmings
arctic foxes
wolverines
Similar to a desert low precipitation (10-12 cmyear) supports a low number of species
Two layers of soil Permafrost ndash layer of soil that never thaws Active Layer ndash above permafrost thaws in summer allowing
roots to take in water and minerals
Decomposition of Organic Matter extremely slow in cold temp because cold keeps the
bacteria and fungi from reproducing This leaves only a small amount of organic material in the soil
Nitrogen and Carbon Cycles slows the rates of the cycles slow decomposition with surface water causes the
formation of bogs These store carbon for long periods of time and decrease denitrification
The Boreal Forest- Immediately south of the Tundra
Biotic FactorsAbiotic Factors
warmer than the Tundra
no permafrost
changeable weather
soils contains some water and is acidic
precipitation 40 cmyear or more
coniferous trees
seed-eating birds
squirrels
voles
snowshoe hare
deer
pine martens
grey wolves
Climate harsh with rapid changes in temp mixing warm and cool air results in
more precipitation
Soil warmer temp allows the soil to thaw every season higher organic matter from faster rates of decomposition soil is more acidic as coniferous needles produce acid when they decay
ndash this can limit the number of plants that can grow
What are conifers Trees with needle shaped leaves ndash evergreens
4 Reasons why conifers are dominant Thin needles have a small surface area so they lose little water during
winter Thick cuticle of wax covers the needles to reduce water loss and
protect from frost damage Pyramid shape of tree and flexible branches allow the tree to support
heavy snowfall Shed their leaves slowly throughout the year so they can begin
photosynthesis when the growing season begins (advantage in a short growing season)
The Temperate Deciduous Forest- South of the Boreal Forest in EasternCentral Canada
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp then Tundra or Boreal Forest
fertile soil
precipitation up to
100 cmyear
deciduous trees
many ferns and shrubs
tree and ground squirrels
many insects
shrews and mice
deer
woodpeckers
weasels black bears wolves
What are the dominant trees in
this biome Deciduous trees (maples oaks poplars
beech and birch)
What features about deciduous trees allow them to complete with conifers
The broad leaves maximize light capture for photosynthesis
Soil and Decomposition
higher temperatures allow for faster decomposition resulting in richer
soil
Understory and Canopy Understory ndash the lower branches of a trees
Canopy ndash the upper levels of the trees
What factors allow for high biodiversity in this biome
The presence of so many different kinds of plants supports many
animals
The thick litter layer is ideal for different insects
Many insects support amphibians lizards birds and insect-eating animals
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
The atmosphere is 79 nitrogen all of which is unusable by plants and animals
Nitrogen is changed into nitrates (usable form) by
lightning
nitrogen fixing bacteria
Nitrogen Fixation Through Lightning energy from the lightning causes nitrogen gas to
react with oxygen gas to produce nitrates
the nitrates dissolve in rain or surface water enter the soil and then move into plants through their roots
Nitrogen Fixation by Bacteria bacteria found in the soil provide the vast majority
of nitrates in the ecosystem Some bacteria may also be found in small lumps called nodules on the roots of some plants
called nitrogen fixing bacteria
Denitrification involves the decay process in which denitrifying bacteria break down nitrates into nitrites and then into nitrogen gas which goes up into the air
This process ensures the balance between soil nitrates nitrites and nitrogen gas
Denitrifying bacteria grow well in areas of low oxygen like lawns By aerating your lawn (adding more oxygen) the breakdown of nitrates into nitrogen gas is reduced and your lawn will stay green longer (nitrates stay in your lawn)
Nitrogen Cycle Animation
Assignment
Read pages 66-67 and complete the assigned questions for the Nitrogen Cycle(handout)
Play the Nitrogen Cycle Game httpwwwwindowsucaredutourlink=teach
er_resourcesteach_nitrogenhtml
The Phosphorus CyclePhosphorous cycles in two ways
Long term in rocks in the Earthrsquos crust phosphates eroded from rock are carried away by rivers and
lakes and end up in the ocean animals use the phosphates to make bones and shells when these animal die they end up at the bottom of the
ocean where over time they may become rock again Plants also absorb phosphates from the water
Short term in living organisms phosphates in dead organisms are recycled by
decomposers which break them down and release the phosphates back into the ecosystem
Phosphorus Cycle
Assignment
bullRead page 68 and complete the questions on the Phosphorus Cycle (handout)
Phosphorus Cycle Animation
Phosphorus Cycle
Section 22-Pesticides
Pesticides are chemicals used to kill insects weeds and microorganisms that might damage crops
Why Use Pesticides Up to 30 of crops in Canada are destroyed by pests This impacts the farmerrsquos income and the price that we pay for the produce
First Generation Pesticides
Pest control dates back to 500 BCE Toxic chemicals were frequently used until we discovered they were more dangerous to us than to the pests
Second Generation Pesticidesbull chemicals made in a lab
bull Can be grouped into four categories
Type Target Examples Persistence
Insecticide Insects DDT 2 - 15 years
Herbicide Weeds Roundup Days to weeks
Fungicide Moulds
and fungi Captan Days
Bactericides Bacteria Penicillin Days
Assignment
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Complete the sheet on histograms (handout)
Play the ldquoOh Deer Gamerdquohttpwwwriverventureorgcharlestonresourcespdfpopulation20study20gamepdf
Bioamplification
When water insoluble pesticides enter food chains the animals that eat them canrsquot break them down so they stay in their bodies The pesticides stay in the fatty tissue The pesticides then built up in a process called bioamplification
DDTbullDDT was the first modern pesticide developed to kill mosquitoes that spread malaria and typhus
bullIn 1962 an American activist named Rachel Carson published a book which alleged that DDT caused cancer and harmed bird reproduction This information led to the pesticide being banned in 1971
bullAlthough it is not being used in North America it is still being used in other countries and can be transmitted through bioamplification
DDT Video
Modern Chemical PesticidesNew pesticides are now water soluble and do not
build up in the tissues of animals They are safer but still have negative effects such as1 They break down quickly so they have to be spread
more often (cost more)
2 They are not selective so they can also kill birds reptiles amphibians and fish
3 Animals that do not die immediately may still put others at risk through bioamplification
4 They have a shelf life meaning that they become ineffective after a while
The Pests Fight Back Pests that reproduce often start to become
resistant to pesticides The first time using a chemical you will probably
kill 90 of the insects and the 10 that are left alive will reproduce
The 10 that survived probably had a natural resistance to the chemical Many of their offspring will also have the resistance After several generations the chemical is not as effective
New pesticides must be developed to take their place
Assignment
Read pages 52-57 and do questions 1-7 on page 58
Read pages 81-82 andmake a list of 4 pros and 4 cons for pesticide usage in controlling tentcaterpillars
Section 29-Monitoring Changes in Population
During the last three centuries global population has risen at an exponential rate
500 million in 16501 billion in 18502 billion in 19304 billion in 1975estimated at 8 billion in 2013
Population Growth Patterns Changes in population size occur when people
are added or removed from the population The four factors involved in population growth
are
1 Natality the number of offspring born in one year
2 Mortality the number of individuals that die in one year
3 Immigration the number of individuals moving into a population
4 Emigration the number of individuals moving out of a population
Population Growth = ( Births + Immigration) - ( Deaths + Emigration)
Open and Closed Populations
An open population occurs when all four factors are acting on the population
(Ex The population of Charlottetown)
A closed population occurs when only natality and mortality affect the population size
(Ex Population of the Earth)
Population Histogramsbulluseful when studying population of long-lived organisms such as humans
bullThe shape of pyramid allows you to predict changes in the populations
bullA wide base indicates that the population is rapidly growing
bull When the base is narrower than the middle section fewer offspring are produced and population will decline
Questions
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Section 210-Limits on Populations
Mice populations can change drastically in 6 months 20 mice can become 5120 mice
Why donrsquot we see billionsof mice when we lookout the window
The reason is that there are limitations on all populations including mice
Carrying Capacity
Populations fluctuate but tend to be fairly stable Stabilityhappens when the population does not exceed the carryingcapacity
Carrying Capacity - The maximum number of individual species that can be supported by an ecosystem
Law of Minimum - The nutrient in least supply is the one that limits growth
Law of Tolerance - An organism can survive within a certain range of abiotic factors Going above or below this range will cause death
Biotic potential is the maximum number of offspring that a species can produce if resources were unlimited
It is regulated by four factors
1) Birth potential maximum number of offspring per birth
2) Capacity of survival number of offspring that reach reproductive age
3) Procreation number of times a species reproduces each year
4) Length of reproductive life the age of sexual maturity and the number of years the individual can reproduce
Limiting Factors
The environment provides factors that prevent populations from attaining their biotic potential Environmental Factor Population Changes
Abiotic light temperaturechemical environment
Biotic Amount of foodnumber or effectiveness of predatorsdiseases and parasitesability to compete for resources
Some factors that control population can depend on the size or density of the population
A population is dense when a large number of organisms live in one area
Density IndependentFactors
Density DependentFactors
Flood Food shortage
Fire Competition for mates or habitat
Pesticides Diseases
Change in climate or temperature
Introduction of exotic species
Destruction of habitat Increased predation
Drought Competition for water and other resources
Questions
Read pages 77-80 and do questions 1 2 amp 3 (abc) on page 80
Chapter 3Sustaining Terrestrial Ecosystems
Section 31 Canadian Biomes
Jigsaw Activity
bull In groups you will be using pages 88-93 to complete the sheets on ldquoThe Canadian Biomesrdquo
bull Video Response Biomes (Earth at Risk Series)
Canadian Biomes Biome ndash a collection of ecosystems that are
similar or related to each other usually in the type of plants they support
Four Canadian Biomes
The Tundra The Boreal Forest The Temperate Deciduous
Forest The Grassland
Tundra
Boreal Forest
Grassland
Temperate Deciduous Forest
The Tundra- Canadarsquos northernmost biome
Biotic FactorsAbiotic Factors
very low temp for most
of the year
short growing season
Permafrost layer beneath the soil
low precipitation
poor soil quality
rapid-growing plants
mosses and lichens
caribou
ptarmigan
lemmings
arctic foxes
wolverines
Similar to a desert low precipitation (10-12 cmyear) supports a low number of species
Two layers of soil Permafrost ndash layer of soil that never thaws Active Layer ndash above permafrost thaws in summer allowing
roots to take in water and minerals
Decomposition of Organic Matter extremely slow in cold temp because cold keeps the
bacteria and fungi from reproducing This leaves only a small amount of organic material in the soil
Nitrogen and Carbon Cycles slows the rates of the cycles slow decomposition with surface water causes the
formation of bogs These store carbon for long periods of time and decrease denitrification
The Boreal Forest- Immediately south of the Tundra
Biotic FactorsAbiotic Factors
warmer than the Tundra
no permafrost
changeable weather
soils contains some water and is acidic
precipitation 40 cmyear or more
coniferous trees
seed-eating birds
squirrels
voles
snowshoe hare
deer
pine martens
grey wolves
Climate harsh with rapid changes in temp mixing warm and cool air results in
more precipitation
Soil warmer temp allows the soil to thaw every season higher organic matter from faster rates of decomposition soil is more acidic as coniferous needles produce acid when they decay
ndash this can limit the number of plants that can grow
What are conifers Trees with needle shaped leaves ndash evergreens
4 Reasons why conifers are dominant Thin needles have a small surface area so they lose little water during
winter Thick cuticle of wax covers the needles to reduce water loss and
protect from frost damage Pyramid shape of tree and flexible branches allow the tree to support
heavy snowfall Shed their leaves slowly throughout the year so they can begin
photosynthesis when the growing season begins (advantage in a short growing season)
The Temperate Deciduous Forest- South of the Boreal Forest in EasternCentral Canada
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp then Tundra or Boreal Forest
fertile soil
precipitation up to
100 cmyear
deciduous trees
many ferns and shrubs
tree and ground squirrels
many insects
shrews and mice
deer
woodpeckers
weasels black bears wolves
What are the dominant trees in
this biome Deciduous trees (maples oaks poplars
beech and birch)
What features about deciduous trees allow them to complete with conifers
The broad leaves maximize light capture for photosynthesis
Soil and Decomposition
higher temperatures allow for faster decomposition resulting in richer
soil
Understory and Canopy Understory ndash the lower branches of a trees
Canopy ndash the upper levels of the trees
What factors allow for high biodiversity in this biome
The presence of so many different kinds of plants supports many
animals
The thick litter layer is ideal for different insects
Many insects support amphibians lizards birds and insect-eating animals
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
Nitrogen Fixation Through Lightning energy from the lightning causes nitrogen gas to
react with oxygen gas to produce nitrates
the nitrates dissolve in rain or surface water enter the soil and then move into plants through their roots
Nitrogen Fixation by Bacteria bacteria found in the soil provide the vast majority
of nitrates in the ecosystem Some bacteria may also be found in small lumps called nodules on the roots of some plants
called nitrogen fixing bacteria
Denitrification involves the decay process in which denitrifying bacteria break down nitrates into nitrites and then into nitrogen gas which goes up into the air
This process ensures the balance between soil nitrates nitrites and nitrogen gas
Denitrifying bacteria grow well in areas of low oxygen like lawns By aerating your lawn (adding more oxygen) the breakdown of nitrates into nitrogen gas is reduced and your lawn will stay green longer (nitrates stay in your lawn)
Nitrogen Cycle Animation
Assignment
Read pages 66-67 and complete the assigned questions for the Nitrogen Cycle(handout)
Play the Nitrogen Cycle Game httpwwwwindowsucaredutourlink=teach
er_resourcesteach_nitrogenhtml
The Phosphorus CyclePhosphorous cycles in two ways
Long term in rocks in the Earthrsquos crust phosphates eroded from rock are carried away by rivers and
lakes and end up in the ocean animals use the phosphates to make bones and shells when these animal die they end up at the bottom of the
ocean where over time they may become rock again Plants also absorb phosphates from the water
Short term in living organisms phosphates in dead organisms are recycled by
decomposers which break them down and release the phosphates back into the ecosystem
Phosphorus Cycle
Assignment
bullRead page 68 and complete the questions on the Phosphorus Cycle (handout)
Phosphorus Cycle Animation
Phosphorus Cycle
Section 22-Pesticides
Pesticides are chemicals used to kill insects weeds and microorganisms that might damage crops
Why Use Pesticides Up to 30 of crops in Canada are destroyed by pests This impacts the farmerrsquos income and the price that we pay for the produce
First Generation Pesticides
Pest control dates back to 500 BCE Toxic chemicals were frequently used until we discovered they were more dangerous to us than to the pests
Second Generation Pesticidesbull chemicals made in a lab
bull Can be grouped into four categories
Type Target Examples Persistence
Insecticide Insects DDT 2 - 15 years
Herbicide Weeds Roundup Days to weeks
Fungicide Moulds
and fungi Captan Days
Bactericides Bacteria Penicillin Days
Assignment
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Complete the sheet on histograms (handout)
Play the ldquoOh Deer Gamerdquohttpwwwriverventureorgcharlestonresourcespdfpopulation20study20gamepdf
Bioamplification
When water insoluble pesticides enter food chains the animals that eat them canrsquot break them down so they stay in their bodies The pesticides stay in the fatty tissue The pesticides then built up in a process called bioamplification
DDTbullDDT was the first modern pesticide developed to kill mosquitoes that spread malaria and typhus
bullIn 1962 an American activist named Rachel Carson published a book which alleged that DDT caused cancer and harmed bird reproduction This information led to the pesticide being banned in 1971
bullAlthough it is not being used in North America it is still being used in other countries and can be transmitted through bioamplification
DDT Video
Modern Chemical PesticidesNew pesticides are now water soluble and do not
build up in the tissues of animals They are safer but still have negative effects such as1 They break down quickly so they have to be spread
more often (cost more)
2 They are not selective so they can also kill birds reptiles amphibians and fish
3 Animals that do not die immediately may still put others at risk through bioamplification
4 They have a shelf life meaning that they become ineffective after a while
The Pests Fight Back Pests that reproduce often start to become
resistant to pesticides The first time using a chemical you will probably
kill 90 of the insects and the 10 that are left alive will reproduce
The 10 that survived probably had a natural resistance to the chemical Many of their offspring will also have the resistance After several generations the chemical is not as effective
New pesticides must be developed to take their place
Assignment
Read pages 52-57 and do questions 1-7 on page 58
Read pages 81-82 andmake a list of 4 pros and 4 cons for pesticide usage in controlling tentcaterpillars
Section 29-Monitoring Changes in Population
During the last three centuries global population has risen at an exponential rate
500 million in 16501 billion in 18502 billion in 19304 billion in 1975estimated at 8 billion in 2013
Population Growth Patterns Changes in population size occur when people
are added or removed from the population The four factors involved in population growth
are
1 Natality the number of offspring born in one year
2 Mortality the number of individuals that die in one year
3 Immigration the number of individuals moving into a population
4 Emigration the number of individuals moving out of a population
Population Growth = ( Births + Immigration) - ( Deaths + Emigration)
Open and Closed Populations
An open population occurs when all four factors are acting on the population
(Ex The population of Charlottetown)
A closed population occurs when only natality and mortality affect the population size
(Ex Population of the Earth)
Population Histogramsbulluseful when studying population of long-lived organisms such as humans
bullThe shape of pyramid allows you to predict changes in the populations
bullA wide base indicates that the population is rapidly growing
bull When the base is narrower than the middle section fewer offspring are produced and population will decline
Questions
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Section 210-Limits on Populations
Mice populations can change drastically in 6 months 20 mice can become 5120 mice
Why donrsquot we see billionsof mice when we lookout the window
The reason is that there are limitations on all populations including mice
Carrying Capacity
Populations fluctuate but tend to be fairly stable Stabilityhappens when the population does not exceed the carryingcapacity
Carrying Capacity - The maximum number of individual species that can be supported by an ecosystem
Law of Minimum - The nutrient in least supply is the one that limits growth
Law of Tolerance - An organism can survive within a certain range of abiotic factors Going above or below this range will cause death
Biotic potential is the maximum number of offspring that a species can produce if resources were unlimited
It is regulated by four factors
1) Birth potential maximum number of offspring per birth
2) Capacity of survival number of offspring that reach reproductive age
3) Procreation number of times a species reproduces each year
4) Length of reproductive life the age of sexual maturity and the number of years the individual can reproduce
Limiting Factors
The environment provides factors that prevent populations from attaining their biotic potential Environmental Factor Population Changes
Abiotic light temperaturechemical environment
Biotic Amount of foodnumber or effectiveness of predatorsdiseases and parasitesability to compete for resources
Some factors that control population can depend on the size or density of the population
A population is dense when a large number of organisms live in one area
Density IndependentFactors
Density DependentFactors
Flood Food shortage
Fire Competition for mates or habitat
Pesticides Diseases
Change in climate or temperature
Introduction of exotic species
Destruction of habitat Increased predation
Drought Competition for water and other resources
Questions
Read pages 77-80 and do questions 1 2 amp 3 (abc) on page 80
Chapter 3Sustaining Terrestrial Ecosystems
Section 31 Canadian Biomes
Jigsaw Activity
bull In groups you will be using pages 88-93 to complete the sheets on ldquoThe Canadian Biomesrdquo
bull Video Response Biomes (Earth at Risk Series)
Canadian Biomes Biome ndash a collection of ecosystems that are
similar or related to each other usually in the type of plants they support
Four Canadian Biomes
The Tundra The Boreal Forest The Temperate Deciduous
Forest The Grassland
Tundra
Boreal Forest
Grassland
Temperate Deciduous Forest
The Tundra- Canadarsquos northernmost biome
Biotic FactorsAbiotic Factors
very low temp for most
of the year
short growing season
Permafrost layer beneath the soil
low precipitation
poor soil quality
rapid-growing plants
mosses and lichens
caribou
ptarmigan
lemmings
arctic foxes
wolverines
Similar to a desert low precipitation (10-12 cmyear) supports a low number of species
Two layers of soil Permafrost ndash layer of soil that never thaws Active Layer ndash above permafrost thaws in summer allowing
roots to take in water and minerals
Decomposition of Organic Matter extremely slow in cold temp because cold keeps the
bacteria and fungi from reproducing This leaves only a small amount of organic material in the soil
Nitrogen and Carbon Cycles slows the rates of the cycles slow decomposition with surface water causes the
formation of bogs These store carbon for long periods of time and decrease denitrification
The Boreal Forest- Immediately south of the Tundra
Biotic FactorsAbiotic Factors
warmer than the Tundra
no permafrost
changeable weather
soils contains some water and is acidic
precipitation 40 cmyear or more
coniferous trees
seed-eating birds
squirrels
voles
snowshoe hare
deer
pine martens
grey wolves
Climate harsh with rapid changes in temp mixing warm and cool air results in
more precipitation
Soil warmer temp allows the soil to thaw every season higher organic matter from faster rates of decomposition soil is more acidic as coniferous needles produce acid when they decay
ndash this can limit the number of plants that can grow
What are conifers Trees with needle shaped leaves ndash evergreens
4 Reasons why conifers are dominant Thin needles have a small surface area so they lose little water during
winter Thick cuticle of wax covers the needles to reduce water loss and
protect from frost damage Pyramid shape of tree and flexible branches allow the tree to support
heavy snowfall Shed their leaves slowly throughout the year so they can begin
photosynthesis when the growing season begins (advantage in a short growing season)
The Temperate Deciduous Forest- South of the Boreal Forest in EasternCentral Canada
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp then Tundra or Boreal Forest
fertile soil
precipitation up to
100 cmyear
deciduous trees
many ferns and shrubs
tree and ground squirrels
many insects
shrews and mice
deer
woodpeckers
weasels black bears wolves
What are the dominant trees in
this biome Deciduous trees (maples oaks poplars
beech and birch)
What features about deciduous trees allow them to complete with conifers
The broad leaves maximize light capture for photosynthesis
Soil and Decomposition
higher temperatures allow for faster decomposition resulting in richer
soil
Understory and Canopy Understory ndash the lower branches of a trees
Canopy ndash the upper levels of the trees
What factors allow for high biodiversity in this biome
The presence of so many different kinds of plants supports many
animals
The thick litter layer is ideal for different insects
Many insects support amphibians lizards birds and insect-eating animals
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
Denitrification involves the decay process in which denitrifying bacteria break down nitrates into nitrites and then into nitrogen gas which goes up into the air
This process ensures the balance between soil nitrates nitrites and nitrogen gas
Denitrifying bacteria grow well in areas of low oxygen like lawns By aerating your lawn (adding more oxygen) the breakdown of nitrates into nitrogen gas is reduced and your lawn will stay green longer (nitrates stay in your lawn)
Nitrogen Cycle Animation
Assignment
Read pages 66-67 and complete the assigned questions for the Nitrogen Cycle(handout)
Play the Nitrogen Cycle Game httpwwwwindowsucaredutourlink=teach
er_resourcesteach_nitrogenhtml
The Phosphorus CyclePhosphorous cycles in two ways
Long term in rocks in the Earthrsquos crust phosphates eroded from rock are carried away by rivers and
lakes and end up in the ocean animals use the phosphates to make bones and shells when these animal die they end up at the bottom of the
ocean where over time they may become rock again Plants also absorb phosphates from the water
Short term in living organisms phosphates in dead organisms are recycled by
decomposers which break them down and release the phosphates back into the ecosystem
Phosphorus Cycle
Assignment
bullRead page 68 and complete the questions on the Phosphorus Cycle (handout)
Phosphorus Cycle Animation
Phosphorus Cycle
Section 22-Pesticides
Pesticides are chemicals used to kill insects weeds and microorganisms that might damage crops
Why Use Pesticides Up to 30 of crops in Canada are destroyed by pests This impacts the farmerrsquos income and the price that we pay for the produce
First Generation Pesticides
Pest control dates back to 500 BCE Toxic chemicals were frequently used until we discovered they were more dangerous to us than to the pests
Second Generation Pesticidesbull chemicals made in a lab
bull Can be grouped into four categories
Type Target Examples Persistence
Insecticide Insects DDT 2 - 15 years
Herbicide Weeds Roundup Days to weeks
Fungicide Moulds
and fungi Captan Days
Bactericides Bacteria Penicillin Days
Assignment
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Complete the sheet on histograms (handout)
Play the ldquoOh Deer Gamerdquohttpwwwriverventureorgcharlestonresourcespdfpopulation20study20gamepdf
Bioamplification
When water insoluble pesticides enter food chains the animals that eat them canrsquot break them down so they stay in their bodies The pesticides stay in the fatty tissue The pesticides then built up in a process called bioamplification
DDTbullDDT was the first modern pesticide developed to kill mosquitoes that spread malaria and typhus
bullIn 1962 an American activist named Rachel Carson published a book which alleged that DDT caused cancer and harmed bird reproduction This information led to the pesticide being banned in 1971
bullAlthough it is not being used in North America it is still being used in other countries and can be transmitted through bioamplification
DDT Video
Modern Chemical PesticidesNew pesticides are now water soluble and do not
build up in the tissues of animals They are safer but still have negative effects such as1 They break down quickly so they have to be spread
more often (cost more)
2 They are not selective so they can also kill birds reptiles amphibians and fish
3 Animals that do not die immediately may still put others at risk through bioamplification
4 They have a shelf life meaning that they become ineffective after a while
The Pests Fight Back Pests that reproduce often start to become
resistant to pesticides The first time using a chemical you will probably
kill 90 of the insects and the 10 that are left alive will reproduce
The 10 that survived probably had a natural resistance to the chemical Many of their offspring will also have the resistance After several generations the chemical is not as effective
New pesticides must be developed to take their place
Assignment
Read pages 52-57 and do questions 1-7 on page 58
Read pages 81-82 andmake a list of 4 pros and 4 cons for pesticide usage in controlling tentcaterpillars
Section 29-Monitoring Changes in Population
During the last three centuries global population has risen at an exponential rate
500 million in 16501 billion in 18502 billion in 19304 billion in 1975estimated at 8 billion in 2013
Population Growth Patterns Changes in population size occur when people
are added or removed from the population The four factors involved in population growth
are
1 Natality the number of offspring born in one year
2 Mortality the number of individuals that die in one year
3 Immigration the number of individuals moving into a population
4 Emigration the number of individuals moving out of a population
Population Growth = ( Births + Immigration) - ( Deaths + Emigration)
Open and Closed Populations
An open population occurs when all four factors are acting on the population
(Ex The population of Charlottetown)
A closed population occurs when only natality and mortality affect the population size
(Ex Population of the Earth)
Population Histogramsbulluseful when studying population of long-lived organisms such as humans
bullThe shape of pyramid allows you to predict changes in the populations
bullA wide base indicates that the population is rapidly growing
bull When the base is narrower than the middle section fewer offspring are produced and population will decline
Questions
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Section 210-Limits on Populations
Mice populations can change drastically in 6 months 20 mice can become 5120 mice
Why donrsquot we see billionsof mice when we lookout the window
The reason is that there are limitations on all populations including mice
Carrying Capacity
Populations fluctuate but tend to be fairly stable Stabilityhappens when the population does not exceed the carryingcapacity
Carrying Capacity - The maximum number of individual species that can be supported by an ecosystem
Law of Minimum - The nutrient in least supply is the one that limits growth
Law of Tolerance - An organism can survive within a certain range of abiotic factors Going above or below this range will cause death
Biotic potential is the maximum number of offspring that a species can produce if resources were unlimited
It is regulated by four factors
1) Birth potential maximum number of offspring per birth
2) Capacity of survival number of offspring that reach reproductive age
3) Procreation number of times a species reproduces each year
4) Length of reproductive life the age of sexual maturity and the number of years the individual can reproduce
Limiting Factors
The environment provides factors that prevent populations from attaining their biotic potential Environmental Factor Population Changes
Abiotic light temperaturechemical environment
Biotic Amount of foodnumber or effectiveness of predatorsdiseases and parasitesability to compete for resources
Some factors that control population can depend on the size or density of the population
A population is dense when a large number of organisms live in one area
Density IndependentFactors
Density DependentFactors
Flood Food shortage
Fire Competition for mates or habitat
Pesticides Diseases
Change in climate or temperature
Introduction of exotic species
Destruction of habitat Increased predation
Drought Competition for water and other resources
Questions
Read pages 77-80 and do questions 1 2 amp 3 (abc) on page 80
Chapter 3Sustaining Terrestrial Ecosystems
Section 31 Canadian Biomes
Jigsaw Activity
bull In groups you will be using pages 88-93 to complete the sheets on ldquoThe Canadian Biomesrdquo
bull Video Response Biomes (Earth at Risk Series)
Canadian Biomes Biome ndash a collection of ecosystems that are
similar or related to each other usually in the type of plants they support
Four Canadian Biomes
The Tundra The Boreal Forest The Temperate Deciduous
Forest The Grassland
Tundra
Boreal Forest
Grassland
Temperate Deciduous Forest
The Tundra- Canadarsquos northernmost biome
Biotic FactorsAbiotic Factors
very low temp for most
of the year
short growing season
Permafrost layer beneath the soil
low precipitation
poor soil quality
rapid-growing plants
mosses and lichens
caribou
ptarmigan
lemmings
arctic foxes
wolverines
Similar to a desert low precipitation (10-12 cmyear) supports a low number of species
Two layers of soil Permafrost ndash layer of soil that never thaws Active Layer ndash above permafrost thaws in summer allowing
roots to take in water and minerals
Decomposition of Organic Matter extremely slow in cold temp because cold keeps the
bacteria and fungi from reproducing This leaves only a small amount of organic material in the soil
Nitrogen and Carbon Cycles slows the rates of the cycles slow decomposition with surface water causes the
formation of bogs These store carbon for long periods of time and decrease denitrification
The Boreal Forest- Immediately south of the Tundra
Biotic FactorsAbiotic Factors
warmer than the Tundra
no permafrost
changeable weather
soils contains some water and is acidic
precipitation 40 cmyear or more
coniferous trees
seed-eating birds
squirrels
voles
snowshoe hare
deer
pine martens
grey wolves
Climate harsh with rapid changes in temp mixing warm and cool air results in
more precipitation
Soil warmer temp allows the soil to thaw every season higher organic matter from faster rates of decomposition soil is more acidic as coniferous needles produce acid when they decay
ndash this can limit the number of plants that can grow
What are conifers Trees with needle shaped leaves ndash evergreens
4 Reasons why conifers are dominant Thin needles have a small surface area so they lose little water during
winter Thick cuticle of wax covers the needles to reduce water loss and
protect from frost damage Pyramid shape of tree and flexible branches allow the tree to support
heavy snowfall Shed their leaves slowly throughout the year so they can begin
photosynthesis when the growing season begins (advantage in a short growing season)
The Temperate Deciduous Forest- South of the Boreal Forest in EasternCentral Canada
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp then Tundra or Boreal Forest
fertile soil
precipitation up to
100 cmyear
deciduous trees
many ferns and shrubs
tree and ground squirrels
many insects
shrews and mice
deer
woodpeckers
weasels black bears wolves
What are the dominant trees in
this biome Deciduous trees (maples oaks poplars
beech and birch)
What features about deciduous trees allow them to complete with conifers
The broad leaves maximize light capture for photosynthesis
Soil and Decomposition
higher temperatures allow for faster decomposition resulting in richer
soil
Understory and Canopy Understory ndash the lower branches of a trees
Canopy ndash the upper levels of the trees
What factors allow for high biodiversity in this biome
The presence of so many different kinds of plants supports many
animals
The thick litter layer is ideal for different insects
Many insects support amphibians lizards birds and insect-eating animals
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
Nitrogen Cycle Animation
Assignment
Read pages 66-67 and complete the assigned questions for the Nitrogen Cycle(handout)
Play the Nitrogen Cycle Game httpwwwwindowsucaredutourlink=teach
er_resourcesteach_nitrogenhtml
The Phosphorus CyclePhosphorous cycles in two ways
Long term in rocks in the Earthrsquos crust phosphates eroded from rock are carried away by rivers and
lakes and end up in the ocean animals use the phosphates to make bones and shells when these animal die they end up at the bottom of the
ocean where over time they may become rock again Plants also absorb phosphates from the water
Short term in living organisms phosphates in dead organisms are recycled by
decomposers which break them down and release the phosphates back into the ecosystem
Phosphorus Cycle
Assignment
bullRead page 68 and complete the questions on the Phosphorus Cycle (handout)
Phosphorus Cycle Animation
Phosphorus Cycle
Section 22-Pesticides
Pesticides are chemicals used to kill insects weeds and microorganisms that might damage crops
Why Use Pesticides Up to 30 of crops in Canada are destroyed by pests This impacts the farmerrsquos income and the price that we pay for the produce
First Generation Pesticides
Pest control dates back to 500 BCE Toxic chemicals were frequently used until we discovered they were more dangerous to us than to the pests
Second Generation Pesticidesbull chemicals made in a lab
bull Can be grouped into four categories
Type Target Examples Persistence
Insecticide Insects DDT 2 - 15 years
Herbicide Weeds Roundup Days to weeks
Fungicide Moulds
and fungi Captan Days
Bactericides Bacteria Penicillin Days
Assignment
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Complete the sheet on histograms (handout)
Play the ldquoOh Deer Gamerdquohttpwwwriverventureorgcharlestonresourcespdfpopulation20study20gamepdf
Bioamplification
When water insoluble pesticides enter food chains the animals that eat them canrsquot break them down so they stay in their bodies The pesticides stay in the fatty tissue The pesticides then built up in a process called bioamplification
DDTbullDDT was the first modern pesticide developed to kill mosquitoes that spread malaria and typhus
bullIn 1962 an American activist named Rachel Carson published a book which alleged that DDT caused cancer and harmed bird reproduction This information led to the pesticide being banned in 1971
bullAlthough it is not being used in North America it is still being used in other countries and can be transmitted through bioamplification
DDT Video
Modern Chemical PesticidesNew pesticides are now water soluble and do not
build up in the tissues of animals They are safer but still have negative effects such as1 They break down quickly so they have to be spread
more often (cost more)
2 They are not selective so they can also kill birds reptiles amphibians and fish
3 Animals that do not die immediately may still put others at risk through bioamplification
4 They have a shelf life meaning that they become ineffective after a while
The Pests Fight Back Pests that reproduce often start to become
resistant to pesticides The first time using a chemical you will probably
kill 90 of the insects and the 10 that are left alive will reproduce
The 10 that survived probably had a natural resistance to the chemical Many of their offspring will also have the resistance After several generations the chemical is not as effective
New pesticides must be developed to take their place
Assignment
Read pages 52-57 and do questions 1-7 on page 58
Read pages 81-82 andmake a list of 4 pros and 4 cons for pesticide usage in controlling tentcaterpillars
Section 29-Monitoring Changes in Population
During the last three centuries global population has risen at an exponential rate
500 million in 16501 billion in 18502 billion in 19304 billion in 1975estimated at 8 billion in 2013
Population Growth Patterns Changes in population size occur when people
are added or removed from the population The four factors involved in population growth
are
1 Natality the number of offspring born in one year
2 Mortality the number of individuals that die in one year
3 Immigration the number of individuals moving into a population
4 Emigration the number of individuals moving out of a population
Population Growth = ( Births + Immigration) - ( Deaths + Emigration)
Open and Closed Populations
An open population occurs when all four factors are acting on the population
(Ex The population of Charlottetown)
A closed population occurs when only natality and mortality affect the population size
(Ex Population of the Earth)
Population Histogramsbulluseful when studying population of long-lived organisms such as humans
bullThe shape of pyramid allows you to predict changes in the populations
bullA wide base indicates that the population is rapidly growing
bull When the base is narrower than the middle section fewer offspring are produced and population will decline
Questions
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Section 210-Limits on Populations
Mice populations can change drastically in 6 months 20 mice can become 5120 mice
Why donrsquot we see billionsof mice when we lookout the window
The reason is that there are limitations on all populations including mice
Carrying Capacity
Populations fluctuate but tend to be fairly stable Stabilityhappens when the population does not exceed the carryingcapacity
Carrying Capacity - The maximum number of individual species that can be supported by an ecosystem
Law of Minimum - The nutrient in least supply is the one that limits growth
Law of Tolerance - An organism can survive within a certain range of abiotic factors Going above or below this range will cause death
Biotic potential is the maximum number of offspring that a species can produce if resources were unlimited
It is regulated by four factors
1) Birth potential maximum number of offspring per birth
2) Capacity of survival number of offspring that reach reproductive age
3) Procreation number of times a species reproduces each year
4) Length of reproductive life the age of sexual maturity and the number of years the individual can reproduce
Limiting Factors
The environment provides factors that prevent populations from attaining their biotic potential Environmental Factor Population Changes
Abiotic light temperaturechemical environment
Biotic Amount of foodnumber or effectiveness of predatorsdiseases and parasitesability to compete for resources
Some factors that control population can depend on the size or density of the population
A population is dense when a large number of organisms live in one area
Density IndependentFactors
Density DependentFactors
Flood Food shortage
Fire Competition for mates or habitat
Pesticides Diseases
Change in climate or temperature
Introduction of exotic species
Destruction of habitat Increased predation
Drought Competition for water and other resources
Questions
Read pages 77-80 and do questions 1 2 amp 3 (abc) on page 80
Chapter 3Sustaining Terrestrial Ecosystems
Section 31 Canadian Biomes
Jigsaw Activity
bull In groups you will be using pages 88-93 to complete the sheets on ldquoThe Canadian Biomesrdquo
bull Video Response Biomes (Earth at Risk Series)
Canadian Biomes Biome ndash a collection of ecosystems that are
similar or related to each other usually in the type of plants they support
Four Canadian Biomes
The Tundra The Boreal Forest The Temperate Deciduous
Forest The Grassland
Tundra
Boreal Forest
Grassland
Temperate Deciduous Forest
The Tundra- Canadarsquos northernmost biome
Biotic FactorsAbiotic Factors
very low temp for most
of the year
short growing season
Permafrost layer beneath the soil
low precipitation
poor soil quality
rapid-growing plants
mosses and lichens
caribou
ptarmigan
lemmings
arctic foxes
wolverines
Similar to a desert low precipitation (10-12 cmyear) supports a low number of species
Two layers of soil Permafrost ndash layer of soil that never thaws Active Layer ndash above permafrost thaws in summer allowing
roots to take in water and minerals
Decomposition of Organic Matter extremely slow in cold temp because cold keeps the
bacteria and fungi from reproducing This leaves only a small amount of organic material in the soil
Nitrogen and Carbon Cycles slows the rates of the cycles slow decomposition with surface water causes the
formation of bogs These store carbon for long periods of time and decrease denitrification
The Boreal Forest- Immediately south of the Tundra
Biotic FactorsAbiotic Factors
warmer than the Tundra
no permafrost
changeable weather
soils contains some water and is acidic
precipitation 40 cmyear or more
coniferous trees
seed-eating birds
squirrels
voles
snowshoe hare
deer
pine martens
grey wolves
Climate harsh with rapid changes in temp mixing warm and cool air results in
more precipitation
Soil warmer temp allows the soil to thaw every season higher organic matter from faster rates of decomposition soil is more acidic as coniferous needles produce acid when they decay
ndash this can limit the number of plants that can grow
What are conifers Trees with needle shaped leaves ndash evergreens
4 Reasons why conifers are dominant Thin needles have a small surface area so they lose little water during
winter Thick cuticle of wax covers the needles to reduce water loss and
protect from frost damage Pyramid shape of tree and flexible branches allow the tree to support
heavy snowfall Shed their leaves slowly throughout the year so they can begin
photosynthesis when the growing season begins (advantage in a short growing season)
The Temperate Deciduous Forest- South of the Boreal Forest in EasternCentral Canada
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp then Tundra or Boreal Forest
fertile soil
precipitation up to
100 cmyear
deciduous trees
many ferns and shrubs
tree and ground squirrels
many insects
shrews and mice
deer
woodpeckers
weasels black bears wolves
What are the dominant trees in
this biome Deciduous trees (maples oaks poplars
beech and birch)
What features about deciduous trees allow them to complete with conifers
The broad leaves maximize light capture for photosynthesis
Soil and Decomposition
higher temperatures allow for faster decomposition resulting in richer
soil
Understory and Canopy Understory ndash the lower branches of a trees
Canopy ndash the upper levels of the trees
What factors allow for high biodiversity in this biome
The presence of so many different kinds of plants supports many
animals
The thick litter layer is ideal for different insects
Many insects support amphibians lizards birds and insect-eating animals
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
Assignment
Read pages 66-67 and complete the assigned questions for the Nitrogen Cycle(handout)
Play the Nitrogen Cycle Game httpwwwwindowsucaredutourlink=teach
er_resourcesteach_nitrogenhtml
The Phosphorus CyclePhosphorous cycles in two ways
Long term in rocks in the Earthrsquos crust phosphates eroded from rock are carried away by rivers and
lakes and end up in the ocean animals use the phosphates to make bones and shells when these animal die they end up at the bottom of the
ocean where over time they may become rock again Plants also absorb phosphates from the water
Short term in living organisms phosphates in dead organisms are recycled by
decomposers which break them down and release the phosphates back into the ecosystem
Phosphorus Cycle
Assignment
bullRead page 68 and complete the questions on the Phosphorus Cycle (handout)
Phosphorus Cycle Animation
Phosphorus Cycle
Section 22-Pesticides
Pesticides are chemicals used to kill insects weeds and microorganisms that might damage crops
Why Use Pesticides Up to 30 of crops in Canada are destroyed by pests This impacts the farmerrsquos income and the price that we pay for the produce
First Generation Pesticides
Pest control dates back to 500 BCE Toxic chemicals were frequently used until we discovered they were more dangerous to us than to the pests
Second Generation Pesticidesbull chemicals made in a lab
bull Can be grouped into four categories
Type Target Examples Persistence
Insecticide Insects DDT 2 - 15 years
Herbicide Weeds Roundup Days to weeks
Fungicide Moulds
and fungi Captan Days
Bactericides Bacteria Penicillin Days
Assignment
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Complete the sheet on histograms (handout)
Play the ldquoOh Deer Gamerdquohttpwwwriverventureorgcharlestonresourcespdfpopulation20study20gamepdf
Bioamplification
When water insoluble pesticides enter food chains the animals that eat them canrsquot break them down so they stay in their bodies The pesticides stay in the fatty tissue The pesticides then built up in a process called bioamplification
DDTbullDDT was the first modern pesticide developed to kill mosquitoes that spread malaria and typhus
bullIn 1962 an American activist named Rachel Carson published a book which alleged that DDT caused cancer and harmed bird reproduction This information led to the pesticide being banned in 1971
bullAlthough it is not being used in North America it is still being used in other countries and can be transmitted through bioamplification
DDT Video
Modern Chemical PesticidesNew pesticides are now water soluble and do not
build up in the tissues of animals They are safer but still have negative effects such as1 They break down quickly so they have to be spread
more often (cost more)
2 They are not selective so they can also kill birds reptiles amphibians and fish
3 Animals that do not die immediately may still put others at risk through bioamplification
4 They have a shelf life meaning that they become ineffective after a while
The Pests Fight Back Pests that reproduce often start to become
resistant to pesticides The first time using a chemical you will probably
kill 90 of the insects and the 10 that are left alive will reproduce
The 10 that survived probably had a natural resistance to the chemical Many of their offspring will also have the resistance After several generations the chemical is not as effective
New pesticides must be developed to take their place
Assignment
Read pages 52-57 and do questions 1-7 on page 58
Read pages 81-82 andmake a list of 4 pros and 4 cons for pesticide usage in controlling tentcaterpillars
Section 29-Monitoring Changes in Population
During the last three centuries global population has risen at an exponential rate
500 million in 16501 billion in 18502 billion in 19304 billion in 1975estimated at 8 billion in 2013
Population Growth Patterns Changes in population size occur when people
are added or removed from the population The four factors involved in population growth
are
1 Natality the number of offspring born in one year
2 Mortality the number of individuals that die in one year
3 Immigration the number of individuals moving into a population
4 Emigration the number of individuals moving out of a population
Population Growth = ( Births + Immigration) - ( Deaths + Emigration)
Open and Closed Populations
An open population occurs when all four factors are acting on the population
(Ex The population of Charlottetown)
A closed population occurs when only natality and mortality affect the population size
(Ex Population of the Earth)
Population Histogramsbulluseful when studying population of long-lived organisms such as humans
bullThe shape of pyramid allows you to predict changes in the populations
bullA wide base indicates that the population is rapidly growing
bull When the base is narrower than the middle section fewer offspring are produced and population will decline
Questions
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Section 210-Limits on Populations
Mice populations can change drastically in 6 months 20 mice can become 5120 mice
Why donrsquot we see billionsof mice when we lookout the window
The reason is that there are limitations on all populations including mice
Carrying Capacity
Populations fluctuate but tend to be fairly stable Stabilityhappens when the population does not exceed the carryingcapacity
Carrying Capacity - The maximum number of individual species that can be supported by an ecosystem
Law of Minimum - The nutrient in least supply is the one that limits growth
Law of Tolerance - An organism can survive within a certain range of abiotic factors Going above or below this range will cause death
Biotic potential is the maximum number of offspring that a species can produce if resources were unlimited
It is regulated by four factors
1) Birth potential maximum number of offspring per birth
2) Capacity of survival number of offspring that reach reproductive age
3) Procreation number of times a species reproduces each year
4) Length of reproductive life the age of sexual maturity and the number of years the individual can reproduce
Limiting Factors
The environment provides factors that prevent populations from attaining their biotic potential Environmental Factor Population Changes
Abiotic light temperaturechemical environment
Biotic Amount of foodnumber or effectiveness of predatorsdiseases and parasitesability to compete for resources
Some factors that control population can depend on the size or density of the population
A population is dense when a large number of organisms live in one area
Density IndependentFactors
Density DependentFactors
Flood Food shortage
Fire Competition for mates or habitat
Pesticides Diseases
Change in climate or temperature
Introduction of exotic species
Destruction of habitat Increased predation
Drought Competition for water and other resources
Questions
Read pages 77-80 and do questions 1 2 amp 3 (abc) on page 80
Chapter 3Sustaining Terrestrial Ecosystems
Section 31 Canadian Biomes
Jigsaw Activity
bull In groups you will be using pages 88-93 to complete the sheets on ldquoThe Canadian Biomesrdquo
bull Video Response Biomes (Earth at Risk Series)
Canadian Biomes Biome ndash a collection of ecosystems that are
similar or related to each other usually in the type of plants they support
Four Canadian Biomes
The Tundra The Boreal Forest The Temperate Deciduous
Forest The Grassland
Tundra
Boreal Forest
Grassland
Temperate Deciduous Forest
The Tundra- Canadarsquos northernmost biome
Biotic FactorsAbiotic Factors
very low temp for most
of the year
short growing season
Permafrost layer beneath the soil
low precipitation
poor soil quality
rapid-growing plants
mosses and lichens
caribou
ptarmigan
lemmings
arctic foxes
wolverines
Similar to a desert low precipitation (10-12 cmyear) supports a low number of species
Two layers of soil Permafrost ndash layer of soil that never thaws Active Layer ndash above permafrost thaws in summer allowing
roots to take in water and minerals
Decomposition of Organic Matter extremely slow in cold temp because cold keeps the
bacteria and fungi from reproducing This leaves only a small amount of organic material in the soil
Nitrogen and Carbon Cycles slows the rates of the cycles slow decomposition with surface water causes the
formation of bogs These store carbon for long periods of time and decrease denitrification
The Boreal Forest- Immediately south of the Tundra
Biotic FactorsAbiotic Factors
warmer than the Tundra
no permafrost
changeable weather
soils contains some water and is acidic
precipitation 40 cmyear or more
coniferous trees
seed-eating birds
squirrels
voles
snowshoe hare
deer
pine martens
grey wolves
Climate harsh with rapid changes in temp mixing warm and cool air results in
more precipitation
Soil warmer temp allows the soil to thaw every season higher organic matter from faster rates of decomposition soil is more acidic as coniferous needles produce acid when they decay
ndash this can limit the number of plants that can grow
What are conifers Trees with needle shaped leaves ndash evergreens
4 Reasons why conifers are dominant Thin needles have a small surface area so they lose little water during
winter Thick cuticle of wax covers the needles to reduce water loss and
protect from frost damage Pyramid shape of tree and flexible branches allow the tree to support
heavy snowfall Shed their leaves slowly throughout the year so they can begin
photosynthesis when the growing season begins (advantage in a short growing season)
The Temperate Deciduous Forest- South of the Boreal Forest in EasternCentral Canada
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp then Tundra or Boreal Forest
fertile soil
precipitation up to
100 cmyear
deciduous trees
many ferns and shrubs
tree and ground squirrels
many insects
shrews and mice
deer
woodpeckers
weasels black bears wolves
What are the dominant trees in
this biome Deciduous trees (maples oaks poplars
beech and birch)
What features about deciduous trees allow them to complete with conifers
The broad leaves maximize light capture for photosynthesis
Soil and Decomposition
higher temperatures allow for faster decomposition resulting in richer
soil
Understory and Canopy Understory ndash the lower branches of a trees
Canopy ndash the upper levels of the trees
What factors allow for high biodiversity in this biome
The presence of so many different kinds of plants supports many
animals
The thick litter layer is ideal for different insects
Many insects support amphibians lizards birds and insect-eating animals
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
The Phosphorus CyclePhosphorous cycles in two ways
Long term in rocks in the Earthrsquos crust phosphates eroded from rock are carried away by rivers and
lakes and end up in the ocean animals use the phosphates to make bones and shells when these animal die they end up at the bottom of the
ocean where over time they may become rock again Plants also absorb phosphates from the water
Short term in living organisms phosphates in dead organisms are recycled by
decomposers which break them down and release the phosphates back into the ecosystem
Phosphorus Cycle
Assignment
bullRead page 68 and complete the questions on the Phosphorus Cycle (handout)
Phosphorus Cycle Animation
Phosphorus Cycle
Section 22-Pesticides
Pesticides are chemicals used to kill insects weeds and microorganisms that might damage crops
Why Use Pesticides Up to 30 of crops in Canada are destroyed by pests This impacts the farmerrsquos income and the price that we pay for the produce
First Generation Pesticides
Pest control dates back to 500 BCE Toxic chemicals were frequently used until we discovered they were more dangerous to us than to the pests
Second Generation Pesticidesbull chemicals made in a lab
bull Can be grouped into four categories
Type Target Examples Persistence
Insecticide Insects DDT 2 - 15 years
Herbicide Weeds Roundup Days to weeks
Fungicide Moulds
and fungi Captan Days
Bactericides Bacteria Penicillin Days
Assignment
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Complete the sheet on histograms (handout)
Play the ldquoOh Deer Gamerdquohttpwwwriverventureorgcharlestonresourcespdfpopulation20study20gamepdf
Bioamplification
When water insoluble pesticides enter food chains the animals that eat them canrsquot break them down so they stay in their bodies The pesticides stay in the fatty tissue The pesticides then built up in a process called bioamplification
DDTbullDDT was the first modern pesticide developed to kill mosquitoes that spread malaria and typhus
bullIn 1962 an American activist named Rachel Carson published a book which alleged that DDT caused cancer and harmed bird reproduction This information led to the pesticide being banned in 1971
bullAlthough it is not being used in North America it is still being used in other countries and can be transmitted through bioamplification
DDT Video
Modern Chemical PesticidesNew pesticides are now water soluble and do not
build up in the tissues of animals They are safer but still have negative effects such as1 They break down quickly so they have to be spread
more often (cost more)
2 They are not selective so they can also kill birds reptiles amphibians and fish
3 Animals that do not die immediately may still put others at risk through bioamplification
4 They have a shelf life meaning that they become ineffective after a while
The Pests Fight Back Pests that reproduce often start to become
resistant to pesticides The first time using a chemical you will probably
kill 90 of the insects and the 10 that are left alive will reproduce
The 10 that survived probably had a natural resistance to the chemical Many of their offspring will also have the resistance After several generations the chemical is not as effective
New pesticides must be developed to take their place
Assignment
Read pages 52-57 and do questions 1-7 on page 58
Read pages 81-82 andmake a list of 4 pros and 4 cons for pesticide usage in controlling tentcaterpillars
Section 29-Monitoring Changes in Population
During the last three centuries global population has risen at an exponential rate
500 million in 16501 billion in 18502 billion in 19304 billion in 1975estimated at 8 billion in 2013
Population Growth Patterns Changes in population size occur when people
are added or removed from the population The four factors involved in population growth
are
1 Natality the number of offspring born in one year
2 Mortality the number of individuals that die in one year
3 Immigration the number of individuals moving into a population
4 Emigration the number of individuals moving out of a population
Population Growth = ( Births + Immigration) - ( Deaths + Emigration)
Open and Closed Populations
An open population occurs when all four factors are acting on the population
(Ex The population of Charlottetown)
A closed population occurs when only natality and mortality affect the population size
(Ex Population of the Earth)
Population Histogramsbulluseful when studying population of long-lived organisms such as humans
bullThe shape of pyramid allows you to predict changes in the populations
bullA wide base indicates that the population is rapidly growing
bull When the base is narrower than the middle section fewer offspring are produced and population will decline
Questions
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Section 210-Limits on Populations
Mice populations can change drastically in 6 months 20 mice can become 5120 mice
Why donrsquot we see billionsof mice when we lookout the window
The reason is that there are limitations on all populations including mice
Carrying Capacity
Populations fluctuate but tend to be fairly stable Stabilityhappens when the population does not exceed the carryingcapacity
Carrying Capacity - The maximum number of individual species that can be supported by an ecosystem
Law of Minimum - The nutrient in least supply is the one that limits growth
Law of Tolerance - An organism can survive within a certain range of abiotic factors Going above or below this range will cause death
Biotic potential is the maximum number of offspring that a species can produce if resources were unlimited
It is regulated by four factors
1) Birth potential maximum number of offspring per birth
2) Capacity of survival number of offspring that reach reproductive age
3) Procreation number of times a species reproduces each year
4) Length of reproductive life the age of sexual maturity and the number of years the individual can reproduce
Limiting Factors
The environment provides factors that prevent populations from attaining their biotic potential Environmental Factor Population Changes
Abiotic light temperaturechemical environment
Biotic Amount of foodnumber or effectiveness of predatorsdiseases and parasitesability to compete for resources
Some factors that control population can depend on the size or density of the population
A population is dense when a large number of organisms live in one area
Density IndependentFactors
Density DependentFactors
Flood Food shortage
Fire Competition for mates or habitat
Pesticides Diseases
Change in climate or temperature
Introduction of exotic species
Destruction of habitat Increased predation
Drought Competition for water and other resources
Questions
Read pages 77-80 and do questions 1 2 amp 3 (abc) on page 80
Chapter 3Sustaining Terrestrial Ecosystems
Section 31 Canadian Biomes
Jigsaw Activity
bull In groups you will be using pages 88-93 to complete the sheets on ldquoThe Canadian Biomesrdquo
bull Video Response Biomes (Earth at Risk Series)
Canadian Biomes Biome ndash a collection of ecosystems that are
similar or related to each other usually in the type of plants they support
Four Canadian Biomes
The Tundra The Boreal Forest The Temperate Deciduous
Forest The Grassland
Tundra
Boreal Forest
Grassland
Temperate Deciduous Forest
The Tundra- Canadarsquos northernmost biome
Biotic FactorsAbiotic Factors
very low temp for most
of the year
short growing season
Permafrost layer beneath the soil
low precipitation
poor soil quality
rapid-growing plants
mosses and lichens
caribou
ptarmigan
lemmings
arctic foxes
wolverines
Similar to a desert low precipitation (10-12 cmyear) supports a low number of species
Two layers of soil Permafrost ndash layer of soil that never thaws Active Layer ndash above permafrost thaws in summer allowing
roots to take in water and minerals
Decomposition of Organic Matter extremely slow in cold temp because cold keeps the
bacteria and fungi from reproducing This leaves only a small amount of organic material in the soil
Nitrogen and Carbon Cycles slows the rates of the cycles slow decomposition with surface water causes the
formation of bogs These store carbon for long periods of time and decrease denitrification
The Boreal Forest- Immediately south of the Tundra
Biotic FactorsAbiotic Factors
warmer than the Tundra
no permafrost
changeable weather
soils contains some water and is acidic
precipitation 40 cmyear or more
coniferous trees
seed-eating birds
squirrels
voles
snowshoe hare
deer
pine martens
grey wolves
Climate harsh with rapid changes in temp mixing warm and cool air results in
more precipitation
Soil warmer temp allows the soil to thaw every season higher organic matter from faster rates of decomposition soil is more acidic as coniferous needles produce acid when they decay
ndash this can limit the number of plants that can grow
What are conifers Trees with needle shaped leaves ndash evergreens
4 Reasons why conifers are dominant Thin needles have a small surface area so they lose little water during
winter Thick cuticle of wax covers the needles to reduce water loss and
protect from frost damage Pyramid shape of tree and flexible branches allow the tree to support
heavy snowfall Shed their leaves slowly throughout the year so they can begin
photosynthesis when the growing season begins (advantage in a short growing season)
The Temperate Deciduous Forest- South of the Boreal Forest in EasternCentral Canada
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp then Tundra or Boreal Forest
fertile soil
precipitation up to
100 cmyear
deciduous trees
many ferns and shrubs
tree and ground squirrels
many insects
shrews and mice
deer
woodpeckers
weasels black bears wolves
What are the dominant trees in
this biome Deciduous trees (maples oaks poplars
beech and birch)
What features about deciduous trees allow them to complete with conifers
The broad leaves maximize light capture for photosynthesis
Soil and Decomposition
higher temperatures allow for faster decomposition resulting in richer
soil
Understory and Canopy Understory ndash the lower branches of a trees
Canopy ndash the upper levels of the trees
What factors allow for high biodiversity in this biome
The presence of so many different kinds of plants supports many
animals
The thick litter layer is ideal for different insects
Many insects support amphibians lizards birds and insect-eating animals
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
Phosphorus Cycle
Assignment
bullRead page 68 and complete the questions on the Phosphorus Cycle (handout)
Phosphorus Cycle Animation
Phosphorus Cycle
Section 22-Pesticides
Pesticides are chemicals used to kill insects weeds and microorganisms that might damage crops
Why Use Pesticides Up to 30 of crops in Canada are destroyed by pests This impacts the farmerrsquos income and the price that we pay for the produce
First Generation Pesticides
Pest control dates back to 500 BCE Toxic chemicals were frequently used until we discovered they were more dangerous to us than to the pests
Second Generation Pesticidesbull chemicals made in a lab
bull Can be grouped into four categories
Type Target Examples Persistence
Insecticide Insects DDT 2 - 15 years
Herbicide Weeds Roundup Days to weeks
Fungicide Moulds
and fungi Captan Days
Bactericides Bacteria Penicillin Days
Assignment
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Complete the sheet on histograms (handout)
Play the ldquoOh Deer Gamerdquohttpwwwriverventureorgcharlestonresourcespdfpopulation20study20gamepdf
Bioamplification
When water insoluble pesticides enter food chains the animals that eat them canrsquot break them down so they stay in their bodies The pesticides stay in the fatty tissue The pesticides then built up in a process called bioamplification
DDTbullDDT was the first modern pesticide developed to kill mosquitoes that spread malaria and typhus
bullIn 1962 an American activist named Rachel Carson published a book which alleged that DDT caused cancer and harmed bird reproduction This information led to the pesticide being banned in 1971
bullAlthough it is not being used in North America it is still being used in other countries and can be transmitted through bioamplification
DDT Video
Modern Chemical PesticidesNew pesticides are now water soluble and do not
build up in the tissues of animals They are safer but still have negative effects such as1 They break down quickly so they have to be spread
more often (cost more)
2 They are not selective so they can also kill birds reptiles amphibians and fish
3 Animals that do not die immediately may still put others at risk through bioamplification
4 They have a shelf life meaning that they become ineffective after a while
The Pests Fight Back Pests that reproduce often start to become
resistant to pesticides The first time using a chemical you will probably
kill 90 of the insects and the 10 that are left alive will reproduce
The 10 that survived probably had a natural resistance to the chemical Many of their offspring will also have the resistance After several generations the chemical is not as effective
New pesticides must be developed to take their place
Assignment
Read pages 52-57 and do questions 1-7 on page 58
Read pages 81-82 andmake a list of 4 pros and 4 cons for pesticide usage in controlling tentcaterpillars
Section 29-Monitoring Changes in Population
During the last three centuries global population has risen at an exponential rate
500 million in 16501 billion in 18502 billion in 19304 billion in 1975estimated at 8 billion in 2013
Population Growth Patterns Changes in population size occur when people
are added or removed from the population The four factors involved in population growth
are
1 Natality the number of offspring born in one year
2 Mortality the number of individuals that die in one year
3 Immigration the number of individuals moving into a population
4 Emigration the number of individuals moving out of a population
Population Growth = ( Births + Immigration) - ( Deaths + Emigration)
Open and Closed Populations
An open population occurs when all four factors are acting on the population
(Ex The population of Charlottetown)
A closed population occurs when only natality and mortality affect the population size
(Ex Population of the Earth)
Population Histogramsbulluseful when studying population of long-lived organisms such as humans
bullThe shape of pyramid allows you to predict changes in the populations
bullA wide base indicates that the population is rapidly growing
bull When the base is narrower than the middle section fewer offspring are produced and population will decline
Questions
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Section 210-Limits on Populations
Mice populations can change drastically in 6 months 20 mice can become 5120 mice
Why donrsquot we see billionsof mice when we lookout the window
The reason is that there are limitations on all populations including mice
Carrying Capacity
Populations fluctuate but tend to be fairly stable Stabilityhappens when the population does not exceed the carryingcapacity
Carrying Capacity - The maximum number of individual species that can be supported by an ecosystem
Law of Minimum - The nutrient in least supply is the one that limits growth
Law of Tolerance - An organism can survive within a certain range of abiotic factors Going above or below this range will cause death
Biotic potential is the maximum number of offspring that a species can produce if resources were unlimited
It is regulated by four factors
1) Birth potential maximum number of offspring per birth
2) Capacity of survival number of offspring that reach reproductive age
3) Procreation number of times a species reproduces each year
4) Length of reproductive life the age of sexual maturity and the number of years the individual can reproduce
Limiting Factors
The environment provides factors that prevent populations from attaining their biotic potential Environmental Factor Population Changes
Abiotic light temperaturechemical environment
Biotic Amount of foodnumber or effectiveness of predatorsdiseases and parasitesability to compete for resources
Some factors that control population can depend on the size or density of the population
A population is dense when a large number of organisms live in one area
Density IndependentFactors
Density DependentFactors
Flood Food shortage
Fire Competition for mates or habitat
Pesticides Diseases
Change in climate or temperature
Introduction of exotic species
Destruction of habitat Increased predation
Drought Competition for water and other resources
Questions
Read pages 77-80 and do questions 1 2 amp 3 (abc) on page 80
Chapter 3Sustaining Terrestrial Ecosystems
Section 31 Canadian Biomes
Jigsaw Activity
bull In groups you will be using pages 88-93 to complete the sheets on ldquoThe Canadian Biomesrdquo
bull Video Response Biomes (Earth at Risk Series)
Canadian Biomes Biome ndash a collection of ecosystems that are
similar or related to each other usually in the type of plants they support
Four Canadian Biomes
The Tundra The Boreal Forest The Temperate Deciduous
Forest The Grassland
Tundra
Boreal Forest
Grassland
Temperate Deciduous Forest
The Tundra- Canadarsquos northernmost biome
Biotic FactorsAbiotic Factors
very low temp for most
of the year
short growing season
Permafrost layer beneath the soil
low precipitation
poor soil quality
rapid-growing plants
mosses and lichens
caribou
ptarmigan
lemmings
arctic foxes
wolverines
Similar to a desert low precipitation (10-12 cmyear) supports a low number of species
Two layers of soil Permafrost ndash layer of soil that never thaws Active Layer ndash above permafrost thaws in summer allowing
roots to take in water and minerals
Decomposition of Organic Matter extremely slow in cold temp because cold keeps the
bacteria and fungi from reproducing This leaves only a small amount of organic material in the soil
Nitrogen and Carbon Cycles slows the rates of the cycles slow decomposition with surface water causes the
formation of bogs These store carbon for long periods of time and decrease denitrification
The Boreal Forest- Immediately south of the Tundra
Biotic FactorsAbiotic Factors
warmer than the Tundra
no permafrost
changeable weather
soils contains some water and is acidic
precipitation 40 cmyear or more
coniferous trees
seed-eating birds
squirrels
voles
snowshoe hare
deer
pine martens
grey wolves
Climate harsh with rapid changes in temp mixing warm and cool air results in
more precipitation
Soil warmer temp allows the soil to thaw every season higher organic matter from faster rates of decomposition soil is more acidic as coniferous needles produce acid when they decay
ndash this can limit the number of plants that can grow
What are conifers Trees with needle shaped leaves ndash evergreens
4 Reasons why conifers are dominant Thin needles have a small surface area so they lose little water during
winter Thick cuticle of wax covers the needles to reduce water loss and
protect from frost damage Pyramid shape of tree and flexible branches allow the tree to support
heavy snowfall Shed their leaves slowly throughout the year so they can begin
photosynthesis when the growing season begins (advantage in a short growing season)
The Temperate Deciduous Forest- South of the Boreal Forest in EasternCentral Canada
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp then Tundra or Boreal Forest
fertile soil
precipitation up to
100 cmyear
deciduous trees
many ferns and shrubs
tree and ground squirrels
many insects
shrews and mice
deer
woodpeckers
weasels black bears wolves
What are the dominant trees in
this biome Deciduous trees (maples oaks poplars
beech and birch)
What features about deciduous trees allow them to complete with conifers
The broad leaves maximize light capture for photosynthesis
Soil and Decomposition
higher temperatures allow for faster decomposition resulting in richer
soil
Understory and Canopy Understory ndash the lower branches of a trees
Canopy ndash the upper levels of the trees
What factors allow for high biodiversity in this biome
The presence of so many different kinds of plants supports many
animals
The thick litter layer is ideal for different insects
Many insects support amphibians lizards birds and insect-eating animals
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
Section 22-Pesticides
Pesticides are chemicals used to kill insects weeds and microorganisms that might damage crops
Why Use Pesticides Up to 30 of crops in Canada are destroyed by pests This impacts the farmerrsquos income and the price that we pay for the produce
First Generation Pesticides
Pest control dates back to 500 BCE Toxic chemicals were frequently used until we discovered they were more dangerous to us than to the pests
Second Generation Pesticidesbull chemicals made in a lab
bull Can be grouped into four categories
Type Target Examples Persistence
Insecticide Insects DDT 2 - 15 years
Herbicide Weeds Roundup Days to weeks
Fungicide Moulds
and fungi Captan Days
Bactericides Bacteria Penicillin Days
Assignment
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Complete the sheet on histograms (handout)
Play the ldquoOh Deer Gamerdquohttpwwwriverventureorgcharlestonresourcespdfpopulation20study20gamepdf
Bioamplification
When water insoluble pesticides enter food chains the animals that eat them canrsquot break them down so they stay in their bodies The pesticides stay in the fatty tissue The pesticides then built up in a process called bioamplification
DDTbullDDT was the first modern pesticide developed to kill mosquitoes that spread malaria and typhus
bullIn 1962 an American activist named Rachel Carson published a book which alleged that DDT caused cancer and harmed bird reproduction This information led to the pesticide being banned in 1971
bullAlthough it is not being used in North America it is still being used in other countries and can be transmitted through bioamplification
DDT Video
Modern Chemical PesticidesNew pesticides are now water soluble and do not
build up in the tissues of animals They are safer but still have negative effects such as1 They break down quickly so they have to be spread
more often (cost more)
2 They are not selective so they can also kill birds reptiles amphibians and fish
3 Animals that do not die immediately may still put others at risk through bioamplification
4 They have a shelf life meaning that they become ineffective after a while
The Pests Fight Back Pests that reproduce often start to become
resistant to pesticides The first time using a chemical you will probably
kill 90 of the insects and the 10 that are left alive will reproduce
The 10 that survived probably had a natural resistance to the chemical Many of their offspring will also have the resistance After several generations the chemical is not as effective
New pesticides must be developed to take their place
Assignment
Read pages 52-57 and do questions 1-7 on page 58
Read pages 81-82 andmake a list of 4 pros and 4 cons for pesticide usage in controlling tentcaterpillars
Section 29-Monitoring Changes in Population
During the last three centuries global population has risen at an exponential rate
500 million in 16501 billion in 18502 billion in 19304 billion in 1975estimated at 8 billion in 2013
Population Growth Patterns Changes in population size occur when people
are added or removed from the population The four factors involved in population growth
are
1 Natality the number of offspring born in one year
2 Mortality the number of individuals that die in one year
3 Immigration the number of individuals moving into a population
4 Emigration the number of individuals moving out of a population
Population Growth = ( Births + Immigration) - ( Deaths + Emigration)
Open and Closed Populations
An open population occurs when all four factors are acting on the population
(Ex The population of Charlottetown)
A closed population occurs when only natality and mortality affect the population size
(Ex Population of the Earth)
Population Histogramsbulluseful when studying population of long-lived organisms such as humans
bullThe shape of pyramid allows you to predict changes in the populations
bullA wide base indicates that the population is rapidly growing
bull When the base is narrower than the middle section fewer offspring are produced and population will decline
Questions
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Section 210-Limits on Populations
Mice populations can change drastically in 6 months 20 mice can become 5120 mice
Why donrsquot we see billionsof mice when we lookout the window
The reason is that there are limitations on all populations including mice
Carrying Capacity
Populations fluctuate but tend to be fairly stable Stabilityhappens when the population does not exceed the carryingcapacity
Carrying Capacity - The maximum number of individual species that can be supported by an ecosystem
Law of Minimum - The nutrient in least supply is the one that limits growth
Law of Tolerance - An organism can survive within a certain range of abiotic factors Going above or below this range will cause death
Biotic potential is the maximum number of offspring that a species can produce if resources were unlimited
It is regulated by four factors
1) Birth potential maximum number of offspring per birth
2) Capacity of survival number of offspring that reach reproductive age
3) Procreation number of times a species reproduces each year
4) Length of reproductive life the age of sexual maturity and the number of years the individual can reproduce
Limiting Factors
The environment provides factors that prevent populations from attaining their biotic potential Environmental Factor Population Changes
Abiotic light temperaturechemical environment
Biotic Amount of foodnumber or effectiveness of predatorsdiseases and parasitesability to compete for resources
Some factors that control population can depend on the size or density of the population
A population is dense when a large number of organisms live in one area
Density IndependentFactors
Density DependentFactors
Flood Food shortage
Fire Competition for mates or habitat
Pesticides Diseases
Change in climate or temperature
Introduction of exotic species
Destruction of habitat Increased predation
Drought Competition for water and other resources
Questions
Read pages 77-80 and do questions 1 2 amp 3 (abc) on page 80
Chapter 3Sustaining Terrestrial Ecosystems
Section 31 Canadian Biomes
Jigsaw Activity
bull In groups you will be using pages 88-93 to complete the sheets on ldquoThe Canadian Biomesrdquo
bull Video Response Biomes (Earth at Risk Series)
Canadian Biomes Biome ndash a collection of ecosystems that are
similar or related to each other usually in the type of plants they support
Four Canadian Biomes
The Tundra The Boreal Forest The Temperate Deciduous
Forest The Grassland
Tundra
Boreal Forest
Grassland
Temperate Deciduous Forest
The Tundra- Canadarsquos northernmost biome
Biotic FactorsAbiotic Factors
very low temp for most
of the year
short growing season
Permafrost layer beneath the soil
low precipitation
poor soil quality
rapid-growing plants
mosses and lichens
caribou
ptarmigan
lemmings
arctic foxes
wolverines
Similar to a desert low precipitation (10-12 cmyear) supports a low number of species
Two layers of soil Permafrost ndash layer of soil that never thaws Active Layer ndash above permafrost thaws in summer allowing
roots to take in water and minerals
Decomposition of Organic Matter extremely slow in cold temp because cold keeps the
bacteria and fungi from reproducing This leaves only a small amount of organic material in the soil
Nitrogen and Carbon Cycles slows the rates of the cycles slow decomposition with surface water causes the
formation of bogs These store carbon for long periods of time and decrease denitrification
The Boreal Forest- Immediately south of the Tundra
Biotic FactorsAbiotic Factors
warmer than the Tundra
no permafrost
changeable weather
soils contains some water and is acidic
precipitation 40 cmyear or more
coniferous trees
seed-eating birds
squirrels
voles
snowshoe hare
deer
pine martens
grey wolves
Climate harsh with rapid changes in temp mixing warm and cool air results in
more precipitation
Soil warmer temp allows the soil to thaw every season higher organic matter from faster rates of decomposition soil is more acidic as coniferous needles produce acid when they decay
ndash this can limit the number of plants that can grow
What are conifers Trees with needle shaped leaves ndash evergreens
4 Reasons why conifers are dominant Thin needles have a small surface area so they lose little water during
winter Thick cuticle of wax covers the needles to reduce water loss and
protect from frost damage Pyramid shape of tree and flexible branches allow the tree to support
heavy snowfall Shed their leaves slowly throughout the year so they can begin
photosynthesis when the growing season begins (advantage in a short growing season)
The Temperate Deciduous Forest- South of the Boreal Forest in EasternCentral Canada
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp then Tundra or Boreal Forest
fertile soil
precipitation up to
100 cmyear
deciduous trees
many ferns and shrubs
tree and ground squirrels
many insects
shrews and mice
deer
woodpeckers
weasels black bears wolves
What are the dominant trees in
this biome Deciduous trees (maples oaks poplars
beech and birch)
What features about deciduous trees allow them to complete with conifers
The broad leaves maximize light capture for photosynthesis
Soil and Decomposition
higher temperatures allow for faster decomposition resulting in richer
soil
Understory and Canopy Understory ndash the lower branches of a trees
Canopy ndash the upper levels of the trees
What factors allow for high biodiversity in this biome
The presence of so many different kinds of plants supports many
animals
The thick litter layer is ideal for different insects
Many insects support amphibians lizards birds and insect-eating animals
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
First Generation Pesticides
Pest control dates back to 500 BCE Toxic chemicals were frequently used until we discovered they were more dangerous to us than to the pests
Second Generation Pesticidesbull chemicals made in a lab
bull Can be grouped into four categories
Type Target Examples Persistence
Insecticide Insects DDT 2 - 15 years
Herbicide Weeds Roundup Days to weeks
Fungicide Moulds
and fungi Captan Days
Bactericides Bacteria Penicillin Days
Assignment
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Complete the sheet on histograms (handout)
Play the ldquoOh Deer Gamerdquohttpwwwriverventureorgcharlestonresourcespdfpopulation20study20gamepdf
Bioamplification
When water insoluble pesticides enter food chains the animals that eat them canrsquot break them down so they stay in their bodies The pesticides stay in the fatty tissue The pesticides then built up in a process called bioamplification
DDTbullDDT was the first modern pesticide developed to kill mosquitoes that spread malaria and typhus
bullIn 1962 an American activist named Rachel Carson published a book which alleged that DDT caused cancer and harmed bird reproduction This information led to the pesticide being banned in 1971
bullAlthough it is not being used in North America it is still being used in other countries and can be transmitted through bioamplification
DDT Video
Modern Chemical PesticidesNew pesticides are now water soluble and do not
build up in the tissues of animals They are safer but still have negative effects such as1 They break down quickly so they have to be spread
more often (cost more)
2 They are not selective so they can also kill birds reptiles amphibians and fish
3 Animals that do not die immediately may still put others at risk through bioamplification
4 They have a shelf life meaning that they become ineffective after a while
The Pests Fight Back Pests that reproduce often start to become
resistant to pesticides The first time using a chemical you will probably
kill 90 of the insects and the 10 that are left alive will reproduce
The 10 that survived probably had a natural resistance to the chemical Many of their offspring will also have the resistance After several generations the chemical is not as effective
New pesticides must be developed to take their place
Assignment
Read pages 52-57 and do questions 1-7 on page 58
Read pages 81-82 andmake a list of 4 pros and 4 cons for pesticide usage in controlling tentcaterpillars
Section 29-Monitoring Changes in Population
During the last three centuries global population has risen at an exponential rate
500 million in 16501 billion in 18502 billion in 19304 billion in 1975estimated at 8 billion in 2013
Population Growth Patterns Changes in population size occur when people
are added or removed from the population The four factors involved in population growth
are
1 Natality the number of offspring born in one year
2 Mortality the number of individuals that die in one year
3 Immigration the number of individuals moving into a population
4 Emigration the number of individuals moving out of a population
Population Growth = ( Births + Immigration) - ( Deaths + Emigration)
Open and Closed Populations
An open population occurs when all four factors are acting on the population
(Ex The population of Charlottetown)
A closed population occurs when only natality and mortality affect the population size
(Ex Population of the Earth)
Population Histogramsbulluseful when studying population of long-lived organisms such as humans
bullThe shape of pyramid allows you to predict changes in the populations
bullA wide base indicates that the population is rapidly growing
bull When the base is narrower than the middle section fewer offspring are produced and population will decline
Questions
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Section 210-Limits on Populations
Mice populations can change drastically in 6 months 20 mice can become 5120 mice
Why donrsquot we see billionsof mice when we lookout the window
The reason is that there are limitations on all populations including mice
Carrying Capacity
Populations fluctuate but tend to be fairly stable Stabilityhappens when the population does not exceed the carryingcapacity
Carrying Capacity - The maximum number of individual species that can be supported by an ecosystem
Law of Minimum - The nutrient in least supply is the one that limits growth
Law of Tolerance - An organism can survive within a certain range of abiotic factors Going above or below this range will cause death
Biotic potential is the maximum number of offspring that a species can produce if resources were unlimited
It is regulated by four factors
1) Birth potential maximum number of offspring per birth
2) Capacity of survival number of offspring that reach reproductive age
3) Procreation number of times a species reproduces each year
4) Length of reproductive life the age of sexual maturity and the number of years the individual can reproduce
Limiting Factors
The environment provides factors that prevent populations from attaining their biotic potential Environmental Factor Population Changes
Abiotic light temperaturechemical environment
Biotic Amount of foodnumber or effectiveness of predatorsdiseases and parasitesability to compete for resources
Some factors that control population can depend on the size or density of the population
A population is dense when a large number of organisms live in one area
Density IndependentFactors
Density DependentFactors
Flood Food shortage
Fire Competition for mates or habitat
Pesticides Diseases
Change in climate or temperature
Introduction of exotic species
Destruction of habitat Increased predation
Drought Competition for water and other resources
Questions
Read pages 77-80 and do questions 1 2 amp 3 (abc) on page 80
Chapter 3Sustaining Terrestrial Ecosystems
Section 31 Canadian Biomes
Jigsaw Activity
bull In groups you will be using pages 88-93 to complete the sheets on ldquoThe Canadian Biomesrdquo
bull Video Response Biomes (Earth at Risk Series)
Canadian Biomes Biome ndash a collection of ecosystems that are
similar or related to each other usually in the type of plants they support
Four Canadian Biomes
The Tundra The Boreal Forest The Temperate Deciduous
Forest The Grassland
Tundra
Boreal Forest
Grassland
Temperate Deciduous Forest
The Tundra- Canadarsquos northernmost biome
Biotic FactorsAbiotic Factors
very low temp for most
of the year
short growing season
Permafrost layer beneath the soil
low precipitation
poor soil quality
rapid-growing plants
mosses and lichens
caribou
ptarmigan
lemmings
arctic foxes
wolverines
Similar to a desert low precipitation (10-12 cmyear) supports a low number of species
Two layers of soil Permafrost ndash layer of soil that never thaws Active Layer ndash above permafrost thaws in summer allowing
roots to take in water and minerals
Decomposition of Organic Matter extremely slow in cold temp because cold keeps the
bacteria and fungi from reproducing This leaves only a small amount of organic material in the soil
Nitrogen and Carbon Cycles slows the rates of the cycles slow decomposition with surface water causes the
formation of bogs These store carbon for long periods of time and decrease denitrification
The Boreal Forest- Immediately south of the Tundra
Biotic FactorsAbiotic Factors
warmer than the Tundra
no permafrost
changeable weather
soils contains some water and is acidic
precipitation 40 cmyear or more
coniferous trees
seed-eating birds
squirrels
voles
snowshoe hare
deer
pine martens
grey wolves
Climate harsh with rapid changes in temp mixing warm and cool air results in
more precipitation
Soil warmer temp allows the soil to thaw every season higher organic matter from faster rates of decomposition soil is more acidic as coniferous needles produce acid when they decay
ndash this can limit the number of plants that can grow
What are conifers Trees with needle shaped leaves ndash evergreens
4 Reasons why conifers are dominant Thin needles have a small surface area so they lose little water during
winter Thick cuticle of wax covers the needles to reduce water loss and
protect from frost damage Pyramid shape of tree and flexible branches allow the tree to support
heavy snowfall Shed their leaves slowly throughout the year so they can begin
photosynthesis when the growing season begins (advantage in a short growing season)
The Temperate Deciduous Forest- South of the Boreal Forest in EasternCentral Canada
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp then Tundra or Boreal Forest
fertile soil
precipitation up to
100 cmyear
deciduous trees
many ferns and shrubs
tree and ground squirrels
many insects
shrews and mice
deer
woodpeckers
weasels black bears wolves
What are the dominant trees in
this biome Deciduous trees (maples oaks poplars
beech and birch)
What features about deciduous trees allow them to complete with conifers
The broad leaves maximize light capture for photosynthesis
Soil and Decomposition
higher temperatures allow for faster decomposition resulting in richer
soil
Understory and Canopy Understory ndash the lower branches of a trees
Canopy ndash the upper levels of the trees
What factors allow for high biodiversity in this biome
The presence of so many different kinds of plants supports many
animals
The thick litter layer is ideal for different insects
Many insects support amphibians lizards birds and insect-eating animals
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
Second Generation Pesticidesbull chemicals made in a lab
bull Can be grouped into four categories
Type Target Examples Persistence
Insecticide Insects DDT 2 - 15 years
Herbicide Weeds Roundup Days to weeks
Fungicide Moulds
and fungi Captan Days
Bactericides Bacteria Penicillin Days
Assignment
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Complete the sheet on histograms (handout)
Play the ldquoOh Deer Gamerdquohttpwwwriverventureorgcharlestonresourcespdfpopulation20study20gamepdf
Bioamplification
When water insoluble pesticides enter food chains the animals that eat them canrsquot break them down so they stay in their bodies The pesticides stay in the fatty tissue The pesticides then built up in a process called bioamplification
DDTbullDDT was the first modern pesticide developed to kill mosquitoes that spread malaria and typhus
bullIn 1962 an American activist named Rachel Carson published a book which alleged that DDT caused cancer and harmed bird reproduction This information led to the pesticide being banned in 1971
bullAlthough it is not being used in North America it is still being used in other countries and can be transmitted through bioamplification
DDT Video
Modern Chemical PesticidesNew pesticides are now water soluble and do not
build up in the tissues of animals They are safer but still have negative effects such as1 They break down quickly so they have to be spread
more often (cost more)
2 They are not selective so they can also kill birds reptiles amphibians and fish
3 Animals that do not die immediately may still put others at risk through bioamplification
4 They have a shelf life meaning that they become ineffective after a while
The Pests Fight Back Pests that reproduce often start to become
resistant to pesticides The first time using a chemical you will probably
kill 90 of the insects and the 10 that are left alive will reproduce
The 10 that survived probably had a natural resistance to the chemical Many of their offspring will also have the resistance After several generations the chemical is not as effective
New pesticides must be developed to take their place
Assignment
Read pages 52-57 and do questions 1-7 on page 58
Read pages 81-82 andmake a list of 4 pros and 4 cons for pesticide usage in controlling tentcaterpillars
Section 29-Monitoring Changes in Population
During the last three centuries global population has risen at an exponential rate
500 million in 16501 billion in 18502 billion in 19304 billion in 1975estimated at 8 billion in 2013
Population Growth Patterns Changes in population size occur when people
are added or removed from the population The four factors involved in population growth
are
1 Natality the number of offspring born in one year
2 Mortality the number of individuals that die in one year
3 Immigration the number of individuals moving into a population
4 Emigration the number of individuals moving out of a population
Population Growth = ( Births + Immigration) - ( Deaths + Emigration)
Open and Closed Populations
An open population occurs when all four factors are acting on the population
(Ex The population of Charlottetown)
A closed population occurs when only natality and mortality affect the population size
(Ex Population of the Earth)
Population Histogramsbulluseful when studying population of long-lived organisms such as humans
bullThe shape of pyramid allows you to predict changes in the populations
bullA wide base indicates that the population is rapidly growing
bull When the base is narrower than the middle section fewer offspring are produced and population will decline
Questions
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Section 210-Limits on Populations
Mice populations can change drastically in 6 months 20 mice can become 5120 mice
Why donrsquot we see billionsof mice when we lookout the window
The reason is that there are limitations on all populations including mice
Carrying Capacity
Populations fluctuate but tend to be fairly stable Stabilityhappens when the population does not exceed the carryingcapacity
Carrying Capacity - The maximum number of individual species that can be supported by an ecosystem
Law of Minimum - The nutrient in least supply is the one that limits growth
Law of Tolerance - An organism can survive within a certain range of abiotic factors Going above or below this range will cause death
Biotic potential is the maximum number of offspring that a species can produce if resources were unlimited
It is regulated by four factors
1) Birth potential maximum number of offspring per birth
2) Capacity of survival number of offspring that reach reproductive age
3) Procreation number of times a species reproduces each year
4) Length of reproductive life the age of sexual maturity and the number of years the individual can reproduce
Limiting Factors
The environment provides factors that prevent populations from attaining their biotic potential Environmental Factor Population Changes
Abiotic light temperaturechemical environment
Biotic Amount of foodnumber or effectiveness of predatorsdiseases and parasitesability to compete for resources
Some factors that control population can depend on the size or density of the population
A population is dense when a large number of organisms live in one area
Density IndependentFactors
Density DependentFactors
Flood Food shortage
Fire Competition for mates or habitat
Pesticides Diseases
Change in climate or temperature
Introduction of exotic species
Destruction of habitat Increased predation
Drought Competition for water and other resources
Questions
Read pages 77-80 and do questions 1 2 amp 3 (abc) on page 80
Chapter 3Sustaining Terrestrial Ecosystems
Section 31 Canadian Biomes
Jigsaw Activity
bull In groups you will be using pages 88-93 to complete the sheets on ldquoThe Canadian Biomesrdquo
bull Video Response Biomes (Earth at Risk Series)
Canadian Biomes Biome ndash a collection of ecosystems that are
similar or related to each other usually in the type of plants they support
Four Canadian Biomes
The Tundra The Boreal Forest The Temperate Deciduous
Forest The Grassland
Tundra
Boreal Forest
Grassland
Temperate Deciduous Forest
The Tundra- Canadarsquos northernmost biome
Biotic FactorsAbiotic Factors
very low temp for most
of the year
short growing season
Permafrost layer beneath the soil
low precipitation
poor soil quality
rapid-growing plants
mosses and lichens
caribou
ptarmigan
lemmings
arctic foxes
wolverines
Similar to a desert low precipitation (10-12 cmyear) supports a low number of species
Two layers of soil Permafrost ndash layer of soil that never thaws Active Layer ndash above permafrost thaws in summer allowing
roots to take in water and minerals
Decomposition of Organic Matter extremely slow in cold temp because cold keeps the
bacteria and fungi from reproducing This leaves only a small amount of organic material in the soil
Nitrogen and Carbon Cycles slows the rates of the cycles slow decomposition with surface water causes the
formation of bogs These store carbon for long periods of time and decrease denitrification
The Boreal Forest- Immediately south of the Tundra
Biotic FactorsAbiotic Factors
warmer than the Tundra
no permafrost
changeable weather
soils contains some water and is acidic
precipitation 40 cmyear or more
coniferous trees
seed-eating birds
squirrels
voles
snowshoe hare
deer
pine martens
grey wolves
Climate harsh with rapid changes in temp mixing warm and cool air results in
more precipitation
Soil warmer temp allows the soil to thaw every season higher organic matter from faster rates of decomposition soil is more acidic as coniferous needles produce acid when they decay
ndash this can limit the number of plants that can grow
What are conifers Trees with needle shaped leaves ndash evergreens
4 Reasons why conifers are dominant Thin needles have a small surface area so they lose little water during
winter Thick cuticle of wax covers the needles to reduce water loss and
protect from frost damage Pyramid shape of tree and flexible branches allow the tree to support
heavy snowfall Shed their leaves slowly throughout the year so they can begin
photosynthesis when the growing season begins (advantage in a short growing season)
The Temperate Deciduous Forest- South of the Boreal Forest in EasternCentral Canada
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp then Tundra or Boreal Forest
fertile soil
precipitation up to
100 cmyear
deciduous trees
many ferns and shrubs
tree and ground squirrels
many insects
shrews and mice
deer
woodpeckers
weasels black bears wolves
What are the dominant trees in
this biome Deciduous trees (maples oaks poplars
beech and birch)
What features about deciduous trees allow them to complete with conifers
The broad leaves maximize light capture for photosynthesis
Soil and Decomposition
higher temperatures allow for faster decomposition resulting in richer
soil
Understory and Canopy Understory ndash the lower branches of a trees
Canopy ndash the upper levels of the trees
What factors allow for high biodiversity in this biome
The presence of so many different kinds of plants supports many
animals
The thick litter layer is ideal for different insects
Many insects support amphibians lizards birds and insect-eating animals
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
Assignment
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Complete the sheet on histograms (handout)
Play the ldquoOh Deer Gamerdquohttpwwwriverventureorgcharlestonresourcespdfpopulation20study20gamepdf
Bioamplification
When water insoluble pesticides enter food chains the animals that eat them canrsquot break them down so they stay in their bodies The pesticides stay in the fatty tissue The pesticides then built up in a process called bioamplification
DDTbullDDT was the first modern pesticide developed to kill mosquitoes that spread malaria and typhus
bullIn 1962 an American activist named Rachel Carson published a book which alleged that DDT caused cancer and harmed bird reproduction This information led to the pesticide being banned in 1971
bullAlthough it is not being used in North America it is still being used in other countries and can be transmitted through bioamplification
DDT Video
Modern Chemical PesticidesNew pesticides are now water soluble and do not
build up in the tissues of animals They are safer but still have negative effects such as1 They break down quickly so they have to be spread
more often (cost more)
2 They are not selective so they can also kill birds reptiles amphibians and fish
3 Animals that do not die immediately may still put others at risk through bioamplification
4 They have a shelf life meaning that they become ineffective after a while
The Pests Fight Back Pests that reproduce often start to become
resistant to pesticides The first time using a chemical you will probably
kill 90 of the insects and the 10 that are left alive will reproduce
The 10 that survived probably had a natural resistance to the chemical Many of their offspring will also have the resistance After several generations the chemical is not as effective
New pesticides must be developed to take their place
Assignment
Read pages 52-57 and do questions 1-7 on page 58
Read pages 81-82 andmake a list of 4 pros and 4 cons for pesticide usage in controlling tentcaterpillars
Section 29-Monitoring Changes in Population
During the last three centuries global population has risen at an exponential rate
500 million in 16501 billion in 18502 billion in 19304 billion in 1975estimated at 8 billion in 2013
Population Growth Patterns Changes in population size occur when people
are added or removed from the population The four factors involved in population growth
are
1 Natality the number of offspring born in one year
2 Mortality the number of individuals that die in one year
3 Immigration the number of individuals moving into a population
4 Emigration the number of individuals moving out of a population
Population Growth = ( Births + Immigration) - ( Deaths + Emigration)
Open and Closed Populations
An open population occurs when all four factors are acting on the population
(Ex The population of Charlottetown)
A closed population occurs when only natality and mortality affect the population size
(Ex Population of the Earth)
Population Histogramsbulluseful when studying population of long-lived organisms such as humans
bullThe shape of pyramid allows you to predict changes in the populations
bullA wide base indicates that the population is rapidly growing
bull When the base is narrower than the middle section fewer offspring are produced and population will decline
Questions
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Section 210-Limits on Populations
Mice populations can change drastically in 6 months 20 mice can become 5120 mice
Why donrsquot we see billionsof mice when we lookout the window
The reason is that there are limitations on all populations including mice
Carrying Capacity
Populations fluctuate but tend to be fairly stable Stabilityhappens when the population does not exceed the carryingcapacity
Carrying Capacity - The maximum number of individual species that can be supported by an ecosystem
Law of Minimum - The nutrient in least supply is the one that limits growth
Law of Tolerance - An organism can survive within a certain range of abiotic factors Going above or below this range will cause death
Biotic potential is the maximum number of offspring that a species can produce if resources were unlimited
It is regulated by four factors
1) Birth potential maximum number of offspring per birth
2) Capacity of survival number of offspring that reach reproductive age
3) Procreation number of times a species reproduces each year
4) Length of reproductive life the age of sexual maturity and the number of years the individual can reproduce
Limiting Factors
The environment provides factors that prevent populations from attaining their biotic potential Environmental Factor Population Changes
Abiotic light temperaturechemical environment
Biotic Amount of foodnumber or effectiveness of predatorsdiseases and parasitesability to compete for resources
Some factors that control population can depend on the size or density of the population
A population is dense when a large number of organisms live in one area
Density IndependentFactors
Density DependentFactors
Flood Food shortage
Fire Competition for mates or habitat
Pesticides Diseases
Change in climate or temperature
Introduction of exotic species
Destruction of habitat Increased predation
Drought Competition for water and other resources
Questions
Read pages 77-80 and do questions 1 2 amp 3 (abc) on page 80
Chapter 3Sustaining Terrestrial Ecosystems
Section 31 Canadian Biomes
Jigsaw Activity
bull In groups you will be using pages 88-93 to complete the sheets on ldquoThe Canadian Biomesrdquo
bull Video Response Biomes (Earth at Risk Series)
Canadian Biomes Biome ndash a collection of ecosystems that are
similar or related to each other usually in the type of plants they support
Four Canadian Biomes
The Tundra The Boreal Forest The Temperate Deciduous
Forest The Grassland
Tundra
Boreal Forest
Grassland
Temperate Deciduous Forest
The Tundra- Canadarsquos northernmost biome
Biotic FactorsAbiotic Factors
very low temp for most
of the year
short growing season
Permafrost layer beneath the soil
low precipitation
poor soil quality
rapid-growing plants
mosses and lichens
caribou
ptarmigan
lemmings
arctic foxes
wolverines
Similar to a desert low precipitation (10-12 cmyear) supports a low number of species
Two layers of soil Permafrost ndash layer of soil that never thaws Active Layer ndash above permafrost thaws in summer allowing
roots to take in water and minerals
Decomposition of Organic Matter extremely slow in cold temp because cold keeps the
bacteria and fungi from reproducing This leaves only a small amount of organic material in the soil
Nitrogen and Carbon Cycles slows the rates of the cycles slow decomposition with surface water causes the
formation of bogs These store carbon for long periods of time and decrease denitrification
The Boreal Forest- Immediately south of the Tundra
Biotic FactorsAbiotic Factors
warmer than the Tundra
no permafrost
changeable weather
soils contains some water and is acidic
precipitation 40 cmyear or more
coniferous trees
seed-eating birds
squirrels
voles
snowshoe hare
deer
pine martens
grey wolves
Climate harsh with rapid changes in temp mixing warm and cool air results in
more precipitation
Soil warmer temp allows the soil to thaw every season higher organic matter from faster rates of decomposition soil is more acidic as coniferous needles produce acid when they decay
ndash this can limit the number of plants that can grow
What are conifers Trees with needle shaped leaves ndash evergreens
4 Reasons why conifers are dominant Thin needles have a small surface area so they lose little water during
winter Thick cuticle of wax covers the needles to reduce water loss and
protect from frost damage Pyramid shape of tree and flexible branches allow the tree to support
heavy snowfall Shed their leaves slowly throughout the year so they can begin
photosynthesis when the growing season begins (advantage in a short growing season)
The Temperate Deciduous Forest- South of the Boreal Forest in EasternCentral Canada
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp then Tundra or Boreal Forest
fertile soil
precipitation up to
100 cmyear
deciduous trees
many ferns and shrubs
tree and ground squirrels
many insects
shrews and mice
deer
woodpeckers
weasels black bears wolves
What are the dominant trees in
this biome Deciduous trees (maples oaks poplars
beech and birch)
What features about deciduous trees allow them to complete with conifers
The broad leaves maximize light capture for photosynthesis
Soil and Decomposition
higher temperatures allow for faster decomposition resulting in richer
soil
Understory and Canopy Understory ndash the lower branches of a trees
Canopy ndash the upper levels of the trees
What factors allow for high biodiversity in this biome
The presence of so many different kinds of plants supports many
animals
The thick litter layer is ideal for different insects
Many insects support amphibians lizards birds and insect-eating animals
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
Bioamplification
When water insoluble pesticides enter food chains the animals that eat them canrsquot break them down so they stay in their bodies The pesticides stay in the fatty tissue The pesticides then built up in a process called bioamplification
DDTbullDDT was the first modern pesticide developed to kill mosquitoes that spread malaria and typhus
bullIn 1962 an American activist named Rachel Carson published a book which alleged that DDT caused cancer and harmed bird reproduction This information led to the pesticide being banned in 1971
bullAlthough it is not being used in North America it is still being used in other countries and can be transmitted through bioamplification
DDT Video
Modern Chemical PesticidesNew pesticides are now water soluble and do not
build up in the tissues of animals They are safer but still have negative effects such as1 They break down quickly so they have to be spread
more often (cost more)
2 They are not selective so they can also kill birds reptiles amphibians and fish
3 Animals that do not die immediately may still put others at risk through bioamplification
4 They have a shelf life meaning that they become ineffective after a while
The Pests Fight Back Pests that reproduce often start to become
resistant to pesticides The first time using a chemical you will probably
kill 90 of the insects and the 10 that are left alive will reproduce
The 10 that survived probably had a natural resistance to the chemical Many of their offspring will also have the resistance After several generations the chemical is not as effective
New pesticides must be developed to take their place
Assignment
Read pages 52-57 and do questions 1-7 on page 58
Read pages 81-82 andmake a list of 4 pros and 4 cons for pesticide usage in controlling tentcaterpillars
Section 29-Monitoring Changes in Population
During the last three centuries global population has risen at an exponential rate
500 million in 16501 billion in 18502 billion in 19304 billion in 1975estimated at 8 billion in 2013
Population Growth Patterns Changes in population size occur when people
are added or removed from the population The four factors involved in population growth
are
1 Natality the number of offspring born in one year
2 Mortality the number of individuals that die in one year
3 Immigration the number of individuals moving into a population
4 Emigration the number of individuals moving out of a population
Population Growth = ( Births + Immigration) - ( Deaths + Emigration)
Open and Closed Populations
An open population occurs when all four factors are acting on the population
(Ex The population of Charlottetown)
A closed population occurs when only natality and mortality affect the population size
(Ex Population of the Earth)
Population Histogramsbulluseful when studying population of long-lived organisms such as humans
bullThe shape of pyramid allows you to predict changes in the populations
bullA wide base indicates that the population is rapidly growing
bull When the base is narrower than the middle section fewer offspring are produced and population will decline
Questions
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Section 210-Limits on Populations
Mice populations can change drastically in 6 months 20 mice can become 5120 mice
Why donrsquot we see billionsof mice when we lookout the window
The reason is that there are limitations on all populations including mice
Carrying Capacity
Populations fluctuate but tend to be fairly stable Stabilityhappens when the population does not exceed the carryingcapacity
Carrying Capacity - The maximum number of individual species that can be supported by an ecosystem
Law of Minimum - The nutrient in least supply is the one that limits growth
Law of Tolerance - An organism can survive within a certain range of abiotic factors Going above or below this range will cause death
Biotic potential is the maximum number of offspring that a species can produce if resources were unlimited
It is regulated by four factors
1) Birth potential maximum number of offspring per birth
2) Capacity of survival number of offspring that reach reproductive age
3) Procreation number of times a species reproduces each year
4) Length of reproductive life the age of sexual maturity and the number of years the individual can reproduce
Limiting Factors
The environment provides factors that prevent populations from attaining their biotic potential Environmental Factor Population Changes
Abiotic light temperaturechemical environment
Biotic Amount of foodnumber or effectiveness of predatorsdiseases and parasitesability to compete for resources
Some factors that control population can depend on the size or density of the population
A population is dense when a large number of organisms live in one area
Density IndependentFactors
Density DependentFactors
Flood Food shortage
Fire Competition for mates or habitat
Pesticides Diseases
Change in climate or temperature
Introduction of exotic species
Destruction of habitat Increased predation
Drought Competition for water and other resources
Questions
Read pages 77-80 and do questions 1 2 amp 3 (abc) on page 80
Chapter 3Sustaining Terrestrial Ecosystems
Section 31 Canadian Biomes
Jigsaw Activity
bull In groups you will be using pages 88-93 to complete the sheets on ldquoThe Canadian Biomesrdquo
bull Video Response Biomes (Earth at Risk Series)
Canadian Biomes Biome ndash a collection of ecosystems that are
similar or related to each other usually in the type of plants they support
Four Canadian Biomes
The Tundra The Boreal Forest The Temperate Deciduous
Forest The Grassland
Tundra
Boreal Forest
Grassland
Temperate Deciduous Forest
The Tundra- Canadarsquos northernmost biome
Biotic FactorsAbiotic Factors
very low temp for most
of the year
short growing season
Permafrost layer beneath the soil
low precipitation
poor soil quality
rapid-growing plants
mosses and lichens
caribou
ptarmigan
lemmings
arctic foxes
wolverines
Similar to a desert low precipitation (10-12 cmyear) supports a low number of species
Two layers of soil Permafrost ndash layer of soil that never thaws Active Layer ndash above permafrost thaws in summer allowing
roots to take in water and minerals
Decomposition of Organic Matter extremely slow in cold temp because cold keeps the
bacteria and fungi from reproducing This leaves only a small amount of organic material in the soil
Nitrogen and Carbon Cycles slows the rates of the cycles slow decomposition with surface water causes the
formation of bogs These store carbon for long periods of time and decrease denitrification
The Boreal Forest- Immediately south of the Tundra
Biotic FactorsAbiotic Factors
warmer than the Tundra
no permafrost
changeable weather
soils contains some water and is acidic
precipitation 40 cmyear or more
coniferous trees
seed-eating birds
squirrels
voles
snowshoe hare
deer
pine martens
grey wolves
Climate harsh with rapid changes in temp mixing warm and cool air results in
more precipitation
Soil warmer temp allows the soil to thaw every season higher organic matter from faster rates of decomposition soil is more acidic as coniferous needles produce acid when they decay
ndash this can limit the number of plants that can grow
What are conifers Trees with needle shaped leaves ndash evergreens
4 Reasons why conifers are dominant Thin needles have a small surface area so they lose little water during
winter Thick cuticle of wax covers the needles to reduce water loss and
protect from frost damage Pyramid shape of tree and flexible branches allow the tree to support
heavy snowfall Shed their leaves slowly throughout the year so they can begin
photosynthesis when the growing season begins (advantage in a short growing season)
The Temperate Deciduous Forest- South of the Boreal Forest in EasternCentral Canada
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp then Tundra or Boreal Forest
fertile soil
precipitation up to
100 cmyear
deciduous trees
many ferns and shrubs
tree and ground squirrels
many insects
shrews and mice
deer
woodpeckers
weasels black bears wolves
What are the dominant trees in
this biome Deciduous trees (maples oaks poplars
beech and birch)
What features about deciduous trees allow them to complete with conifers
The broad leaves maximize light capture for photosynthesis
Soil and Decomposition
higher temperatures allow for faster decomposition resulting in richer
soil
Understory and Canopy Understory ndash the lower branches of a trees
Canopy ndash the upper levels of the trees
What factors allow for high biodiversity in this biome
The presence of so many different kinds of plants supports many
animals
The thick litter layer is ideal for different insects
Many insects support amphibians lizards birds and insect-eating animals
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
DDTbullDDT was the first modern pesticide developed to kill mosquitoes that spread malaria and typhus
bullIn 1962 an American activist named Rachel Carson published a book which alleged that DDT caused cancer and harmed bird reproduction This information led to the pesticide being banned in 1971
bullAlthough it is not being used in North America it is still being used in other countries and can be transmitted through bioamplification
DDT Video
Modern Chemical PesticidesNew pesticides are now water soluble and do not
build up in the tissues of animals They are safer but still have negative effects such as1 They break down quickly so they have to be spread
more often (cost more)
2 They are not selective so they can also kill birds reptiles amphibians and fish
3 Animals that do not die immediately may still put others at risk through bioamplification
4 They have a shelf life meaning that they become ineffective after a while
The Pests Fight Back Pests that reproduce often start to become
resistant to pesticides The first time using a chemical you will probably
kill 90 of the insects and the 10 that are left alive will reproduce
The 10 that survived probably had a natural resistance to the chemical Many of their offspring will also have the resistance After several generations the chemical is not as effective
New pesticides must be developed to take their place
Assignment
Read pages 52-57 and do questions 1-7 on page 58
Read pages 81-82 andmake a list of 4 pros and 4 cons for pesticide usage in controlling tentcaterpillars
Section 29-Monitoring Changes in Population
During the last three centuries global population has risen at an exponential rate
500 million in 16501 billion in 18502 billion in 19304 billion in 1975estimated at 8 billion in 2013
Population Growth Patterns Changes in population size occur when people
are added or removed from the population The four factors involved in population growth
are
1 Natality the number of offspring born in one year
2 Mortality the number of individuals that die in one year
3 Immigration the number of individuals moving into a population
4 Emigration the number of individuals moving out of a population
Population Growth = ( Births + Immigration) - ( Deaths + Emigration)
Open and Closed Populations
An open population occurs when all four factors are acting on the population
(Ex The population of Charlottetown)
A closed population occurs when only natality and mortality affect the population size
(Ex Population of the Earth)
Population Histogramsbulluseful when studying population of long-lived organisms such as humans
bullThe shape of pyramid allows you to predict changes in the populations
bullA wide base indicates that the population is rapidly growing
bull When the base is narrower than the middle section fewer offspring are produced and population will decline
Questions
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Section 210-Limits on Populations
Mice populations can change drastically in 6 months 20 mice can become 5120 mice
Why donrsquot we see billionsof mice when we lookout the window
The reason is that there are limitations on all populations including mice
Carrying Capacity
Populations fluctuate but tend to be fairly stable Stabilityhappens when the population does not exceed the carryingcapacity
Carrying Capacity - The maximum number of individual species that can be supported by an ecosystem
Law of Minimum - The nutrient in least supply is the one that limits growth
Law of Tolerance - An organism can survive within a certain range of abiotic factors Going above or below this range will cause death
Biotic potential is the maximum number of offspring that a species can produce if resources were unlimited
It is regulated by four factors
1) Birth potential maximum number of offspring per birth
2) Capacity of survival number of offspring that reach reproductive age
3) Procreation number of times a species reproduces each year
4) Length of reproductive life the age of sexual maturity and the number of years the individual can reproduce
Limiting Factors
The environment provides factors that prevent populations from attaining their biotic potential Environmental Factor Population Changes
Abiotic light temperaturechemical environment
Biotic Amount of foodnumber or effectiveness of predatorsdiseases and parasitesability to compete for resources
Some factors that control population can depend on the size or density of the population
A population is dense when a large number of organisms live in one area
Density IndependentFactors
Density DependentFactors
Flood Food shortage
Fire Competition for mates or habitat
Pesticides Diseases
Change in climate or temperature
Introduction of exotic species
Destruction of habitat Increased predation
Drought Competition for water and other resources
Questions
Read pages 77-80 and do questions 1 2 amp 3 (abc) on page 80
Chapter 3Sustaining Terrestrial Ecosystems
Section 31 Canadian Biomes
Jigsaw Activity
bull In groups you will be using pages 88-93 to complete the sheets on ldquoThe Canadian Biomesrdquo
bull Video Response Biomes (Earth at Risk Series)
Canadian Biomes Biome ndash a collection of ecosystems that are
similar or related to each other usually in the type of plants they support
Four Canadian Biomes
The Tundra The Boreal Forest The Temperate Deciduous
Forest The Grassland
Tundra
Boreal Forest
Grassland
Temperate Deciduous Forest
The Tundra- Canadarsquos northernmost biome
Biotic FactorsAbiotic Factors
very low temp for most
of the year
short growing season
Permafrost layer beneath the soil
low precipitation
poor soil quality
rapid-growing plants
mosses and lichens
caribou
ptarmigan
lemmings
arctic foxes
wolverines
Similar to a desert low precipitation (10-12 cmyear) supports a low number of species
Two layers of soil Permafrost ndash layer of soil that never thaws Active Layer ndash above permafrost thaws in summer allowing
roots to take in water and minerals
Decomposition of Organic Matter extremely slow in cold temp because cold keeps the
bacteria and fungi from reproducing This leaves only a small amount of organic material in the soil
Nitrogen and Carbon Cycles slows the rates of the cycles slow decomposition with surface water causes the
formation of bogs These store carbon for long periods of time and decrease denitrification
The Boreal Forest- Immediately south of the Tundra
Biotic FactorsAbiotic Factors
warmer than the Tundra
no permafrost
changeable weather
soils contains some water and is acidic
precipitation 40 cmyear or more
coniferous trees
seed-eating birds
squirrels
voles
snowshoe hare
deer
pine martens
grey wolves
Climate harsh with rapid changes in temp mixing warm and cool air results in
more precipitation
Soil warmer temp allows the soil to thaw every season higher organic matter from faster rates of decomposition soil is more acidic as coniferous needles produce acid when they decay
ndash this can limit the number of plants that can grow
What are conifers Trees with needle shaped leaves ndash evergreens
4 Reasons why conifers are dominant Thin needles have a small surface area so they lose little water during
winter Thick cuticle of wax covers the needles to reduce water loss and
protect from frost damage Pyramid shape of tree and flexible branches allow the tree to support
heavy snowfall Shed their leaves slowly throughout the year so they can begin
photosynthesis when the growing season begins (advantage in a short growing season)
The Temperate Deciduous Forest- South of the Boreal Forest in EasternCentral Canada
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp then Tundra or Boreal Forest
fertile soil
precipitation up to
100 cmyear
deciduous trees
many ferns and shrubs
tree and ground squirrels
many insects
shrews and mice
deer
woodpeckers
weasels black bears wolves
What are the dominant trees in
this biome Deciduous trees (maples oaks poplars
beech and birch)
What features about deciduous trees allow them to complete with conifers
The broad leaves maximize light capture for photosynthesis
Soil and Decomposition
higher temperatures allow for faster decomposition resulting in richer
soil
Understory and Canopy Understory ndash the lower branches of a trees
Canopy ndash the upper levels of the trees
What factors allow for high biodiversity in this biome
The presence of so many different kinds of plants supports many
animals
The thick litter layer is ideal for different insects
Many insects support amphibians lizards birds and insect-eating animals
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
Modern Chemical PesticidesNew pesticides are now water soluble and do not
build up in the tissues of animals They are safer but still have negative effects such as1 They break down quickly so they have to be spread
more often (cost more)
2 They are not selective so they can also kill birds reptiles amphibians and fish
3 Animals that do not die immediately may still put others at risk through bioamplification
4 They have a shelf life meaning that they become ineffective after a while
The Pests Fight Back Pests that reproduce often start to become
resistant to pesticides The first time using a chemical you will probably
kill 90 of the insects and the 10 that are left alive will reproduce
The 10 that survived probably had a natural resistance to the chemical Many of their offspring will also have the resistance After several generations the chemical is not as effective
New pesticides must be developed to take their place
Assignment
Read pages 52-57 and do questions 1-7 on page 58
Read pages 81-82 andmake a list of 4 pros and 4 cons for pesticide usage in controlling tentcaterpillars
Section 29-Monitoring Changes in Population
During the last three centuries global population has risen at an exponential rate
500 million in 16501 billion in 18502 billion in 19304 billion in 1975estimated at 8 billion in 2013
Population Growth Patterns Changes in population size occur when people
are added or removed from the population The four factors involved in population growth
are
1 Natality the number of offspring born in one year
2 Mortality the number of individuals that die in one year
3 Immigration the number of individuals moving into a population
4 Emigration the number of individuals moving out of a population
Population Growth = ( Births + Immigration) - ( Deaths + Emigration)
Open and Closed Populations
An open population occurs when all four factors are acting on the population
(Ex The population of Charlottetown)
A closed population occurs when only natality and mortality affect the population size
(Ex Population of the Earth)
Population Histogramsbulluseful when studying population of long-lived organisms such as humans
bullThe shape of pyramid allows you to predict changes in the populations
bullA wide base indicates that the population is rapidly growing
bull When the base is narrower than the middle section fewer offspring are produced and population will decline
Questions
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Section 210-Limits on Populations
Mice populations can change drastically in 6 months 20 mice can become 5120 mice
Why donrsquot we see billionsof mice when we lookout the window
The reason is that there are limitations on all populations including mice
Carrying Capacity
Populations fluctuate but tend to be fairly stable Stabilityhappens when the population does not exceed the carryingcapacity
Carrying Capacity - The maximum number of individual species that can be supported by an ecosystem
Law of Minimum - The nutrient in least supply is the one that limits growth
Law of Tolerance - An organism can survive within a certain range of abiotic factors Going above or below this range will cause death
Biotic potential is the maximum number of offspring that a species can produce if resources were unlimited
It is regulated by four factors
1) Birth potential maximum number of offspring per birth
2) Capacity of survival number of offspring that reach reproductive age
3) Procreation number of times a species reproduces each year
4) Length of reproductive life the age of sexual maturity and the number of years the individual can reproduce
Limiting Factors
The environment provides factors that prevent populations from attaining their biotic potential Environmental Factor Population Changes
Abiotic light temperaturechemical environment
Biotic Amount of foodnumber or effectiveness of predatorsdiseases and parasitesability to compete for resources
Some factors that control population can depend on the size or density of the population
A population is dense when a large number of organisms live in one area
Density IndependentFactors
Density DependentFactors
Flood Food shortage
Fire Competition for mates or habitat
Pesticides Diseases
Change in climate or temperature
Introduction of exotic species
Destruction of habitat Increased predation
Drought Competition for water and other resources
Questions
Read pages 77-80 and do questions 1 2 amp 3 (abc) on page 80
Chapter 3Sustaining Terrestrial Ecosystems
Section 31 Canadian Biomes
Jigsaw Activity
bull In groups you will be using pages 88-93 to complete the sheets on ldquoThe Canadian Biomesrdquo
bull Video Response Biomes (Earth at Risk Series)
Canadian Biomes Biome ndash a collection of ecosystems that are
similar or related to each other usually in the type of plants they support
Four Canadian Biomes
The Tundra The Boreal Forest The Temperate Deciduous
Forest The Grassland
Tundra
Boreal Forest
Grassland
Temperate Deciduous Forest
The Tundra- Canadarsquos northernmost biome
Biotic FactorsAbiotic Factors
very low temp for most
of the year
short growing season
Permafrost layer beneath the soil
low precipitation
poor soil quality
rapid-growing plants
mosses and lichens
caribou
ptarmigan
lemmings
arctic foxes
wolverines
Similar to a desert low precipitation (10-12 cmyear) supports a low number of species
Two layers of soil Permafrost ndash layer of soil that never thaws Active Layer ndash above permafrost thaws in summer allowing
roots to take in water and minerals
Decomposition of Organic Matter extremely slow in cold temp because cold keeps the
bacteria and fungi from reproducing This leaves only a small amount of organic material in the soil
Nitrogen and Carbon Cycles slows the rates of the cycles slow decomposition with surface water causes the
formation of bogs These store carbon for long periods of time and decrease denitrification
The Boreal Forest- Immediately south of the Tundra
Biotic FactorsAbiotic Factors
warmer than the Tundra
no permafrost
changeable weather
soils contains some water and is acidic
precipitation 40 cmyear or more
coniferous trees
seed-eating birds
squirrels
voles
snowshoe hare
deer
pine martens
grey wolves
Climate harsh with rapid changes in temp mixing warm and cool air results in
more precipitation
Soil warmer temp allows the soil to thaw every season higher organic matter from faster rates of decomposition soil is more acidic as coniferous needles produce acid when they decay
ndash this can limit the number of plants that can grow
What are conifers Trees with needle shaped leaves ndash evergreens
4 Reasons why conifers are dominant Thin needles have a small surface area so they lose little water during
winter Thick cuticle of wax covers the needles to reduce water loss and
protect from frost damage Pyramid shape of tree and flexible branches allow the tree to support
heavy snowfall Shed their leaves slowly throughout the year so they can begin
photosynthesis when the growing season begins (advantage in a short growing season)
The Temperate Deciduous Forest- South of the Boreal Forest in EasternCentral Canada
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp then Tundra or Boreal Forest
fertile soil
precipitation up to
100 cmyear
deciduous trees
many ferns and shrubs
tree and ground squirrels
many insects
shrews and mice
deer
woodpeckers
weasels black bears wolves
What are the dominant trees in
this biome Deciduous trees (maples oaks poplars
beech and birch)
What features about deciduous trees allow them to complete with conifers
The broad leaves maximize light capture for photosynthesis
Soil and Decomposition
higher temperatures allow for faster decomposition resulting in richer
soil
Understory and Canopy Understory ndash the lower branches of a trees
Canopy ndash the upper levels of the trees
What factors allow for high biodiversity in this biome
The presence of so many different kinds of plants supports many
animals
The thick litter layer is ideal for different insects
Many insects support amphibians lizards birds and insect-eating animals
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
The Pests Fight Back Pests that reproduce often start to become
resistant to pesticides The first time using a chemical you will probably
kill 90 of the insects and the 10 that are left alive will reproduce
The 10 that survived probably had a natural resistance to the chemical Many of their offspring will also have the resistance After several generations the chemical is not as effective
New pesticides must be developed to take their place
Assignment
Read pages 52-57 and do questions 1-7 on page 58
Read pages 81-82 andmake a list of 4 pros and 4 cons for pesticide usage in controlling tentcaterpillars
Section 29-Monitoring Changes in Population
During the last three centuries global population has risen at an exponential rate
500 million in 16501 billion in 18502 billion in 19304 billion in 1975estimated at 8 billion in 2013
Population Growth Patterns Changes in population size occur when people
are added or removed from the population The four factors involved in population growth
are
1 Natality the number of offspring born in one year
2 Mortality the number of individuals that die in one year
3 Immigration the number of individuals moving into a population
4 Emigration the number of individuals moving out of a population
Population Growth = ( Births + Immigration) - ( Deaths + Emigration)
Open and Closed Populations
An open population occurs when all four factors are acting on the population
(Ex The population of Charlottetown)
A closed population occurs when only natality and mortality affect the population size
(Ex Population of the Earth)
Population Histogramsbulluseful when studying population of long-lived organisms such as humans
bullThe shape of pyramid allows you to predict changes in the populations
bullA wide base indicates that the population is rapidly growing
bull When the base is narrower than the middle section fewer offspring are produced and population will decline
Questions
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Section 210-Limits on Populations
Mice populations can change drastically in 6 months 20 mice can become 5120 mice
Why donrsquot we see billionsof mice when we lookout the window
The reason is that there are limitations on all populations including mice
Carrying Capacity
Populations fluctuate but tend to be fairly stable Stabilityhappens when the population does not exceed the carryingcapacity
Carrying Capacity - The maximum number of individual species that can be supported by an ecosystem
Law of Minimum - The nutrient in least supply is the one that limits growth
Law of Tolerance - An organism can survive within a certain range of abiotic factors Going above or below this range will cause death
Biotic potential is the maximum number of offspring that a species can produce if resources were unlimited
It is regulated by four factors
1) Birth potential maximum number of offspring per birth
2) Capacity of survival number of offspring that reach reproductive age
3) Procreation number of times a species reproduces each year
4) Length of reproductive life the age of sexual maturity and the number of years the individual can reproduce
Limiting Factors
The environment provides factors that prevent populations from attaining their biotic potential Environmental Factor Population Changes
Abiotic light temperaturechemical environment
Biotic Amount of foodnumber or effectiveness of predatorsdiseases and parasitesability to compete for resources
Some factors that control population can depend on the size or density of the population
A population is dense when a large number of organisms live in one area
Density IndependentFactors
Density DependentFactors
Flood Food shortage
Fire Competition for mates or habitat
Pesticides Diseases
Change in climate or temperature
Introduction of exotic species
Destruction of habitat Increased predation
Drought Competition for water and other resources
Questions
Read pages 77-80 and do questions 1 2 amp 3 (abc) on page 80
Chapter 3Sustaining Terrestrial Ecosystems
Section 31 Canadian Biomes
Jigsaw Activity
bull In groups you will be using pages 88-93 to complete the sheets on ldquoThe Canadian Biomesrdquo
bull Video Response Biomes (Earth at Risk Series)
Canadian Biomes Biome ndash a collection of ecosystems that are
similar or related to each other usually in the type of plants they support
Four Canadian Biomes
The Tundra The Boreal Forest The Temperate Deciduous
Forest The Grassland
Tundra
Boreal Forest
Grassland
Temperate Deciduous Forest
The Tundra- Canadarsquos northernmost biome
Biotic FactorsAbiotic Factors
very low temp for most
of the year
short growing season
Permafrost layer beneath the soil
low precipitation
poor soil quality
rapid-growing plants
mosses and lichens
caribou
ptarmigan
lemmings
arctic foxes
wolverines
Similar to a desert low precipitation (10-12 cmyear) supports a low number of species
Two layers of soil Permafrost ndash layer of soil that never thaws Active Layer ndash above permafrost thaws in summer allowing
roots to take in water and minerals
Decomposition of Organic Matter extremely slow in cold temp because cold keeps the
bacteria and fungi from reproducing This leaves only a small amount of organic material in the soil
Nitrogen and Carbon Cycles slows the rates of the cycles slow decomposition with surface water causes the
formation of bogs These store carbon for long periods of time and decrease denitrification
The Boreal Forest- Immediately south of the Tundra
Biotic FactorsAbiotic Factors
warmer than the Tundra
no permafrost
changeable weather
soils contains some water and is acidic
precipitation 40 cmyear or more
coniferous trees
seed-eating birds
squirrels
voles
snowshoe hare
deer
pine martens
grey wolves
Climate harsh with rapid changes in temp mixing warm and cool air results in
more precipitation
Soil warmer temp allows the soil to thaw every season higher organic matter from faster rates of decomposition soil is more acidic as coniferous needles produce acid when they decay
ndash this can limit the number of plants that can grow
What are conifers Trees with needle shaped leaves ndash evergreens
4 Reasons why conifers are dominant Thin needles have a small surface area so they lose little water during
winter Thick cuticle of wax covers the needles to reduce water loss and
protect from frost damage Pyramid shape of tree and flexible branches allow the tree to support
heavy snowfall Shed their leaves slowly throughout the year so they can begin
photosynthesis when the growing season begins (advantage in a short growing season)
The Temperate Deciduous Forest- South of the Boreal Forest in EasternCentral Canada
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp then Tundra or Boreal Forest
fertile soil
precipitation up to
100 cmyear
deciduous trees
many ferns and shrubs
tree and ground squirrels
many insects
shrews and mice
deer
woodpeckers
weasels black bears wolves
What are the dominant trees in
this biome Deciduous trees (maples oaks poplars
beech and birch)
What features about deciduous trees allow them to complete with conifers
The broad leaves maximize light capture for photosynthesis
Soil and Decomposition
higher temperatures allow for faster decomposition resulting in richer
soil
Understory and Canopy Understory ndash the lower branches of a trees
Canopy ndash the upper levels of the trees
What factors allow for high biodiversity in this biome
The presence of so many different kinds of plants supports many
animals
The thick litter layer is ideal for different insects
Many insects support amphibians lizards birds and insect-eating animals
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
Assignment
Read pages 52-57 and do questions 1-7 on page 58
Read pages 81-82 andmake a list of 4 pros and 4 cons for pesticide usage in controlling tentcaterpillars
Section 29-Monitoring Changes in Population
During the last three centuries global population has risen at an exponential rate
500 million in 16501 billion in 18502 billion in 19304 billion in 1975estimated at 8 billion in 2013
Population Growth Patterns Changes in population size occur when people
are added or removed from the population The four factors involved in population growth
are
1 Natality the number of offspring born in one year
2 Mortality the number of individuals that die in one year
3 Immigration the number of individuals moving into a population
4 Emigration the number of individuals moving out of a population
Population Growth = ( Births + Immigration) - ( Deaths + Emigration)
Open and Closed Populations
An open population occurs when all four factors are acting on the population
(Ex The population of Charlottetown)
A closed population occurs when only natality and mortality affect the population size
(Ex Population of the Earth)
Population Histogramsbulluseful when studying population of long-lived organisms such as humans
bullThe shape of pyramid allows you to predict changes in the populations
bullA wide base indicates that the population is rapidly growing
bull When the base is narrower than the middle section fewer offspring are produced and population will decline
Questions
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Section 210-Limits on Populations
Mice populations can change drastically in 6 months 20 mice can become 5120 mice
Why donrsquot we see billionsof mice when we lookout the window
The reason is that there are limitations on all populations including mice
Carrying Capacity
Populations fluctuate but tend to be fairly stable Stabilityhappens when the population does not exceed the carryingcapacity
Carrying Capacity - The maximum number of individual species that can be supported by an ecosystem
Law of Minimum - The nutrient in least supply is the one that limits growth
Law of Tolerance - An organism can survive within a certain range of abiotic factors Going above or below this range will cause death
Biotic potential is the maximum number of offspring that a species can produce if resources were unlimited
It is regulated by four factors
1) Birth potential maximum number of offspring per birth
2) Capacity of survival number of offspring that reach reproductive age
3) Procreation number of times a species reproduces each year
4) Length of reproductive life the age of sexual maturity and the number of years the individual can reproduce
Limiting Factors
The environment provides factors that prevent populations from attaining their biotic potential Environmental Factor Population Changes
Abiotic light temperaturechemical environment
Biotic Amount of foodnumber or effectiveness of predatorsdiseases and parasitesability to compete for resources
Some factors that control population can depend on the size or density of the population
A population is dense when a large number of organisms live in one area
Density IndependentFactors
Density DependentFactors
Flood Food shortage
Fire Competition for mates or habitat
Pesticides Diseases
Change in climate or temperature
Introduction of exotic species
Destruction of habitat Increased predation
Drought Competition for water and other resources
Questions
Read pages 77-80 and do questions 1 2 amp 3 (abc) on page 80
Chapter 3Sustaining Terrestrial Ecosystems
Section 31 Canadian Biomes
Jigsaw Activity
bull In groups you will be using pages 88-93 to complete the sheets on ldquoThe Canadian Biomesrdquo
bull Video Response Biomes (Earth at Risk Series)
Canadian Biomes Biome ndash a collection of ecosystems that are
similar or related to each other usually in the type of plants they support
Four Canadian Biomes
The Tundra The Boreal Forest The Temperate Deciduous
Forest The Grassland
Tundra
Boreal Forest
Grassland
Temperate Deciduous Forest
The Tundra- Canadarsquos northernmost biome
Biotic FactorsAbiotic Factors
very low temp for most
of the year
short growing season
Permafrost layer beneath the soil
low precipitation
poor soil quality
rapid-growing plants
mosses and lichens
caribou
ptarmigan
lemmings
arctic foxes
wolverines
Similar to a desert low precipitation (10-12 cmyear) supports a low number of species
Two layers of soil Permafrost ndash layer of soil that never thaws Active Layer ndash above permafrost thaws in summer allowing
roots to take in water and minerals
Decomposition of Organic Matter extremely slow in cold temp because cold keeps the
bacteria and fungi from reproducing This leaves only a small amount of organic material in the soil
Nitrogen and Carbon Cycles slows the rates of the cycles slow decomposition with surface water causes the
formation of bogs These store carbon for long periods of time and decrease denitrification
The Boreal Forest- Immediately south of the Tundra
Biotic FactorsAbiotic Factors
warmer than the Tundra
no permafrost
changeable weather
soils contains some water and is acidic
precipitation 40 cmyear or more
coniferous trees
seed-eating birds
squirrels
voles
snowshoe hare
deer
pine martens
grey wolves
Climate harsh with rapid changes in temp mixing warm and cool air results in
more precipitation
Soil warmer temp allows the soil to thaw every season higher organic matter from faster rates of decomposition soil is more acidic as coniferous needles produce acid when they decay
ndash this can limit the number of plants that can grow
What are conifers Trees with needle shaped leaves ndash evergreens
4 Reasons why conifers are dominant Thin needles have a small surface area so they lose little water during
winter Thick cuticle of wax covers the needles to reduce water loss and
protect from frost damage Pyramid shape of tree and flexible branches allow the tree to support
heavy snowfall Shed their leaves slowly throughout the year so they can begin
photosynthesis when the growing season begins (advantage in a short growing season)
The Temperate Deciduous Forest- South of the Boreal Forest in EasternCentral Canada
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp then Tundra or Boreal Forest
fertile soil
precipitation up to
100 cmyear
deciduous trees
many ferns and shrubs
tree and ground squirrels
many insects
shrews and mice
deer
woodpeckers
weasels black bears wolves
What are the dominant trees in
this biome Deciduous trees (maples oaks poplars
beech and birch)
What features about deciduous trees allow them to complete with conifers
The broad leaves maximize light capture for photosynthesis
Soil and Decomposition
higher temperatures allow for faster decomposition resulting in richer
soil
Understory and Canopy Understory ndash the lower branches of a trees
Canopy ndash the upper levels of the trees
What factors allow for high biodiversity in this biome
The presence of so many different kinds of plants supports many
animals
The thick litter layer is ideal for different insects
Many insects support amphibians lizards birds and insect-eating animals
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
Section 29-Monitoring Changes in Population
During the last three centuries global population has risen at an exponential rate
500 million in 16501 billion in 18502 billion in 19304 billion in 1975estimated at 8 billion in 2013
Population Growth Patterns Changes in population size occur when people
are added or removed from the population The four factors involved in population growth
are
1 Natality the number of offspring born in one year
2 Mortality the number of individuals that die in one year
3 Immigration the number of individuals moving into a population
4 Emigration the number of individuals moving out of a population
Population Growth = ( Births + Immigration) - ( Deaths + Emigration)
Open and Closed Populations
An open population occurs when all four factors are acting on the population
(Ex The population of Charlottetown)
A closed population occurs when only natality and mortality affect the population size
(Ex Population of the Earth)
Population Histogramsbulluseful when studying population of long-lived organisms such as humans
bullThe shape of pyramid allows you to predict changes in the populations
bullA wide base indicates that the population is rapidly growing
bull When the base is narrower than the middle section fewer offspring are produced and population will decline
Questions
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Section 210-Limits on Populations
Mice populations can change drastically in 6 months 20 mice can become 5120 mice
Why donrsquot we see billionsof mice when we lookout the window
The reason is that there are limitations on all populations including mice
Carrying Capacity
Populations fluctuate but tend to be fairly stable Stabilityhappens when the population does not exceed the carryingcapacity
Carrying Capacity - The maximum number of individual species that can be supported by an ecosystem
Law of Minimum - The nutrient in least supply is the one that limits growth
Law of Tolerance - An organism can survive within a certain range of abiotic factors Going above or below this range will cause death
Biotic potential is the maximum number of offspring that a species can produce if resources were unlimited
It is regulated by four factors
1) Birth potential maximum number of offspring per birth
2) Capacity of survival number of offspring that reach reproductive age
3) Procreation number of times a species reproduces each year
4) Length of reproductive life the age of sexual maturity and the number of years the individual can reproduce
Limiting Factors
The environment provides factors that prevent populations from attaining their biotic potential Environmental Factor Population Changes
Abiotic light temperaturechemical environment
Biotic Amount of foodnumber or effectiveness of predatorsdiseases and parasitesability to compete for resources
Some factors that control population can depend on the size or density of the population
A population is dense when a large number of organisms live in one area
Density IndependentFactors
Density DependentFactors
Flood Food shortage
Fire Competition for mates or habitat
Pesticides Diseases
Change in climate or temperature
Introduction of exotic species
Destruction of habitat Increased predation
Drought Competition for water and other resources
Questions
Read pages 77-80 and do questions 1 2 amp 3 (abc) on page 80
Chapter 3Sustaining Terrestrial Ecosystems
Section 31 Canadian Biomes
Jigsaw Activity
bull In groups you will be using pages 88-93 to complete the sheets on ldquoThe Canadian Biomesrdquo
bull Video Response Biomes (Earth at Risk Series)
Canadian Biomes Biome ndash a collection of ecosystems that are
similar or related to each other usually in the type of plants they support
Four Canadian Biomes
The Tundra The Boreal Forest The Temperate Deciduous
Forest The Grassland
Tundra
Boreal Forest
Grassland
Temperate Deciduous Forest
The Tundra- Canadarsquos northernmost biome
Biotic FactorsAbiotic Factors
very low temp for most
of the year
short growing season
Permafrost layer beneath the soil
low precipitation
poor soil quality
rapid-growing plants
mosses and lichens
caribou
ptarmigan
lemmings
arctic foxes
wolverines
Similar to a desert low precipitation (10-12 cmyear) supports a low number of species
Two layers of soil Permafrost ndash layer of soil that never thaws Active Layer ndash above permafrost thaws in summer allowing
roots to take in water and minerals
Decomposition of Organic Matter extremely slow in cold temp because cold keeps the
bacteria and fungi from reproducing This leaves only a small amount of organic material in the soil
Nitrogen and Carbon Cycles slows the rates of the cycles slow decomposition with surface water causes the
formation of bogs These store carbon for long periods of time and decrease denitrification
The Boreal Forest- Immediately south of the Tundra
Biotic FactorsAbiotic Factors
warmer than the Tundra
no permafrost
changeable weather
soils contains some water and is acidic
precipitation 40 cmyear or more
coniferous trees
seed-eating birds
squirrels
voles
snowshoe hare
deer
pine martens
grey wolves
Climate harsh with rapid changes in temp mixing warm and cool air results in
more precipitation
Soil warmer temp allows the soil to thaw every season higher organic matter from faster rates of decomposition soil is more acidic as coniferous needles produce acid when they decay
ndash this can limit the number of plants that can grow
What are conifers Trees with needle shaped leaves ndash evergreens
4 Reasons why conifers are dominant Thin needles have a small surface area so they lose little water during
winter Thick cuticle of wax covers the needles to reduce water loss and
protect from frost damage Pyramid shape of tree and flexible branches allow the tree to support
heavy snowfall Shed their leaves slowly throughout the year so they can begin
photosynthesis when the growing season begins (advantage in a short growing season)
The Temperate Deciduous Forest- South of the Boreal Forest in EasternCentral Canada
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp then Tundra or Boreal Forest
fertile soil
precipitation up to
100 cmyear
deciduous trees
many ferns and shrubs
tree and ground squirrels
many insects
shrews and mice
deer
woodpeckers
weasels black bears wolves
What are the dominant trees in
this biome Deciduous trees (maples oaks poplars
beech and birch)
What features about deciduous trees allow them to complete with conifers
The broad leaves maximize light capture for photosynthesis
Soil and Decomposition
higher temperatures allow for faster decomposition resulting in richer
soil
Understory and Canopy Understory ndash the lower branches of a trees
Canopy ndash the upper levels of the trees
What factors allow for high biodiversity in this biome
The presence of so many different kinds of plants supports many
animals
The thick litter layer is ideal for different insects
Many insects support amphibians lizards birds and insect-eating animals
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
Population Growth Patterns Changes in population size occur when people
are added or removed from the population The four factors involved in population growth
are
1 Natality the number of offspring born in one year
2 Mortality the number of individuals that die in one year
3 Immigration the number of individuals moving into a population
4 Emigration the number of individuals moving out of a population
Population Growth = ( Births + Immigration) - ( Deaths + Emigration)
Open and Closed Populations
An open population occurs when all four factors are acting on the population
(Ex The population of Charlottetown)
A closed population occurs when only natality and mortality affect the population size
(Ex Population of the Earth)
Population Histogramsbulluseful when studying population of long-lived organisms such as humans
bullThe shape of pyramid allows you to predict changes in the populations
bullA wide base indicates that the population is rapidly growing
bull When the base is narrower than the middle section fewer offspring are produced and population will decline
Questions
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Section 210-Limits on Populations
Mice populations can change drastically in 6 months 20 mice can become 5120 mice
Why donrsquot we see billionsof mice when we lookout the window
The reason is that there are limitations on all populations including mice
Carrying Capacity
Populations fluctuate but tend to be fairly stable Stabilityhappens when the population does not exceed the carryingcapacity
Carrying Capacity - The maximum number of individual species that can be supported by an ecosystem
Law of Minimum - The nutrient in least supply is the one that limits growth
Law of Tolerance - An organism can survive within a certain range of abiotic factors Going above or below this range will cause death
Biotic potential is the maximum number of offspring that a species can produce if resources were unlimited
It is regulated by four factors
1) Birth potential maximum number of offspring per birth
2) Capacity of survival number of offspring that reach reproductive age
3) Procreation number of times a species reproduces each year
4) Length of reproductive life the age of sexual maturity and the number of years the individual can reproduce
Limiting Factors
The environment provides factors that prevent populations from attaining their biotic potential Environmental Factor Population Changes
Abiotic light temperaturechemical environment
Biotic Amount of foodnumber or effectiveness of predatorsdiseases and parasitesability to compete for resources
Some factors that control population can depend on the size or density of the population
A population is dense when a large number of organisms live in one area
Density IndependentFactors
Density DependentFactors
Flood Food shortage
Fire Competition for mates or habitat
Pesticides Diseases
Change in climate or temperature
Introduction of exotic species
Destruction of habitat Increased predation
Drought Competition for water and other resources
Questions
Read pages 77-80 and do questions 1 2 amp 3 (abc) on page 80
Chapter 3Sustaining Terrestrial Ecosystems
Section 31 Canadian Biomes
Jigsaw Activity
bull In groups you will be using pages 88-93 to complete the sheets on ldquoThe Canadian Biomesrdquo
bull Video Response Biomes (Earth at Risk Series)
Canadian Biomes Biome ndash a collection of ecosystems that are
similar or related to each other usually in the type of plants they support
Four Canadian Biomes
The Tundra The Boreal Forest The Temperate Deciduous
Forest The Grassland
Tundra
Boreal Forest
Grassland
Temperate Deciduous Forest
The Tundra- Canadarsquos northernmost biome
Biotic FactorsAbiotic Factors
very low temp for most
of the year
short growing season
Permafrost layer beneath the soil
low precipitation
poor soil quality
rapid-growing plants
mosses and lichens
caribou
ptarmigan
lemmings
arctic foxes
wolverines
Similar to a desert low precipitation (10-12 cmyear) supports a low number of species
Two layers of soil Permafrost ndash layer of soil that never thaws Active Layer ndash above permafrost thaws in summer allowing
roots to take in water and minerals
Decomposition of Organic Matter extremely slow in cold temp because cold keeps the
bacteria and fungi from reproducing This leaves only a small amount of organic material in the soil
Nitrogen and Carbon Cycles slows the rates of the cycles slow decomposition with surface water causes the
formation of bogs These store carbon for long periods of time and decrease denitrification
The Boreal Forest- Immediately south of the Tundra
Biotic FactorsAbiotic Factors
warmer than the Tundra
no permafrost
changeable weather
soils contains some water and is acidic
precipitation 40 cmyear or more
coniferous trees
seed-eating birds
squirrels
voles
snowshoe hare
deer
pine martens
grey wolves
Climate harsh with rapid changes in temp mixing warm and cool air results in
more precipitation
Soil warmer temp allows the soil to thaw every season higher organic matter from faster rates of decomposition soil is more acidic as coniferous needles produce acid when they decay
ndash this can limit the number of plants that can grow
What are conifers Trees with needle shaped leaves ndash evergreens
4 Reasons why conifers are dominant Thin needles have a small surface area so they lose little water during
winter Thick cuticle of wax covers the needles to reduce water loss and
protect from frost damage Pyramid shape of tree and flexible branches allow the tree to support
heavy snowfall Shed their leaves slowly throughout the year so they can begin
photosynthesis when the growing season begins (advantage in a short growing season)
The Temperate Deciduous Forest- South of the Boreal Forest in EasternCentral Canada
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp then Tundra or Boreal Forest
fertile soil
precipitation up to
100 cmyear
deciduous trees
many ferns and shrubs
tree and ground squirrels
many insects
shrews and mice
deer
woodpeckers
weasels black bears wolves
What are the dominant trees in
this biome Deciduous trees (maples oaks poplars
beech and birch)
What features about deciduous trees allow them to complete with conifers
The broad leaves maximize light capture for photosynthesis
Soil and Decomposition
higher temperatures allow for faster decomposition resulting in richer
soil
Understory and Canopy Understory ndash the lower branches of a trees
Canopy ndash the upper levels of the trees
What factors allow for high biodiversity in this biome
The presence of so many different kinds of plants supports many
animals
The thick litter layer is ideal for different insects
Many insects support amphibians lizards birds and insect-eating animals
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
Open and Closed Populations
An open population occurs when all four factors are acting on the population
(Ex The population of Charlottetown)
A closed population occurs when only natality and mortality affect the population size
(Ex Population of the Earth)
Population Histogramsbulluseful when studying population of long-lived organisms such as humans
bullThe shape of pyramid allows you to predict changes in the populations
bullA wide base indicates that the population is rapidly growing
bull When the base is narrower than the middle section fewer offspring are produced and population will decline
Questions
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Section 210-Limits on Populations
Mice populations can change drastically in 6 months 20 mice can become 5120 mice
Why donrsquot we see billionsof mice when we lookout the window
The reason is that there are limitations on all populations including mice
Carrying Capacity
Populations fluctuate but tend to be fairly stable Stabilityhappens when the population does not exceed the carryingcapacity
Carrying Capacity - The maximum number of individual species that can be supported by an ecosystem
Law of Minimum - The nutrient in least supply is the one that limits growth
Law of Tolerance - An organism can survive within a certain range of abiotic factors Going above or below this range will cause death
Biotic potential is the maximum number of offspring that a species can produce if resources were unlimited
It is regulated by four factors
1) Birth potential maximum number of offspring per birth
2) Capacity of survival number of offspring that reach reproductive age
3) Procreation number of times a species reproduces each year
4) Length of reproductive life the age of sexual maturity and the number of years the individual can reproduce
Limiting Factors
The environment provides factors that prevent populations from attaining their biotic potential Environmental Factor Population Changes
Abiotic light temperaturechemical environment
Biotic Amount of foodnumber or effectiveness of predatorsdiseases and parasitesability to compete for resources
Some factors that control population can depend on the size or density of the population
A population is dense when a large number of organisms live in one area
Density IndependentFactors
Density DependentFactors
Flood Food shortage
Fire Competition for mates or habitat
Pesticides Diseases
Change in climate or temperature
Introduction of exotic species
Destruction of habitat Increased predation
Drought Competition for water and other resources
Questions
Read pages 77-80 and do questions 1 2 amp 3 (abc) on page 80
Chapter 3Sustaining Terrestrial Ecosystems
Section 31 Canadian Biomes
Jigsaw Activity
bull In groups you will be using pages 88-93 to complete the sheets on ldquoThe Canadian Biomesrdquo
bull Video Response Biomes (Earth at Risk Series)
Canadian Biomes Biome ndash a collection of ecosystems that are
similar or related to each other usually in the type of plants they support
Four Canadian Biomes
The Tundra The Boreal Forest The Temperate Deciduous
Forest The Grassland
Tundra
Boreal Forest
Grassland
Temperate Deciduous Forest
The Tundra- Canadarsquos northernmost biome
Biotic FactorsAbiotic Factors
very low temp for most
of the year
short growing season
Permafrost layer beneath the soil
low precipitation
poor soil quality
rapid-growing plants
mosses and lichens
caribou
ptarmigan
lemmings
arctic foxes
wolverines
Similar to a desert low precipitation (10-12 cmyear) supports a low number of species
Two layers of soil Permafrost ndash layer of soil that never thaws Active Layer ndash above permafrost thaws in summer allowing
roots to take in water and minerals
Decomposition of Organic Matter extremely slow in cold temp because cold keeps the
bacteria and fungi from reproducing This leaves only a small amount of organic material in the soil
Nitrogen and Carbon Cycles slows the rates of the cycles slow decomposition with surface water causes the
formation of bogs These store carbon for long periods of time and decrease denitrification
The Boreal Forest- Immediately south of the Tundra
Biotic FactorsAbiotic Factors
warmer than the Tundra
no permafrost
changeable weather
soils contains some water and is acidic
precipitation 40 cmyear or more
coniferous trees
seed-eating birds
squirrels
voles
snowshoe hare
deer
pine martens
grey wolves
Climate harsh with rapid changes in temp mixing warm and cool air results in
more precipitation
Soil warmer temp allows the soil to thaw every season higher organic matter from faster rates of decomposition soil is more acidic as coniferous needles produce acid when they decay
ndash this can limit the number of plants that can grow
What are conifers Trees with needle shaped leaves ndash evergreens
4 Reasons why conifers are dominant Thin needles have a small surface area so they lose little water during
winter Thick cuticle of wax covers the needles to reduce water loss and
protect from frost damage Pyramid shape of tree and flexible branches allow the tree to support
heavy snowfall Shed their leaves slowly throughout the year so they can begin
photosynthesis when the growing season begins (advantage in a short growing season)
The Temperate Deciduous Forest- South of the Boreal Forest in EasternCentral Canada
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp then Tundra or Boreal Forest
fertile soil
precipitation up to
100 cmyear
deciduous trees
many ferns and shrubs
tree and ground squirrels
many insects
shrews and mice
deer
woodpeckers
weasels black bears wolves
What are the dominant trees in
this biome Deciduous trees (maples oaks poplars
beech and birch)
What features about deciduous trees allow them to complete with conifers
The broad leaves maximize light capture for photosynthesis
Soil and Decomposition
higher temperatures allow for faster decomposition resulting in richer
soil
Understory and Canopy Understory ndash the lower branches of a trees
Canopy ndash the upper levels of the trees
What factors allow for high biodiversity in this biome
The presence of so many different kinds of plants supports many
animals
The thick litter layer is ideal for different insects
Many insects support amphibians lizards birds and insect-eating animals
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
Population Histogramsbulluseful when studying population of long-lived organisms such as humans
bullThe shape of pyramid allows you to predict changes in the populations
bullA wide base indicates that the population is rapidly growing
bull When the base is narrower than the middle section fewer offspring are produced and population will decline
Questions
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Section 210-Limits on Populations
Mice populations can change drastically in 6 months 20 mice can become 5120 mice
Why donrsquot we see billionsof mice when we lookout the window
The reason is that there are limitations on all populations including mice
Carrying Capacity
Populations fluctuate but tend to be fairly stable Stabilityhappens when the population does not exceed the carryingcapacity
Carrying Capacity - The maximum number of individual species that can be supported by an ecosystem
Law of Minimum - The nutrient in least supply is the one that limits growth
Law of Tolerance - An organism can survive within a certain range of abiotic factors Going above or below this range will cause death
Biotic potential is the maximum number of offspring that a species can produce if resources were unlimited
It is regulated by four factors
1) Birth potential maximum number of offspring per birth
2) Capacity of survival number of offspring that reach reproductive age
3) Procreation number of times a species reproduces each year
4) Length of reproductive life the age of sexual maturity and the number of years the individual can reproduce
Limiting Factors
The environment provides factors that prevent populations from attaining their biotic potential Environmental Factor Population Changes
Abiotic light temperaturechemical environment
Biotic Amount of foodnumber or effectiveness of predatorsdiseases and parasitesability to compete for resources
Some factors that control population can depend on the size or density of the population
A population is dense when a large number of organisms live in one area
Density IndependentFactors
Density DependentFactors
Flood Food shortage
Fire Competition for mates or habitat
Pesticides Diseases
Change in climate or temperature
Introduction of exotic species
Destruction of habitat Increased predation
Drought Competition for water and other resources
Questions
Read pages 77-80 and do questions 1 2 amp 3 (abc) on page 80
Chapter 3Sustaining Terrestrial Ecosystems
Section 31 Canadian Biomes
Jigsaw Activity
bull In groups you will be using pages 88-93 to complete the sheets on ldquoThe Canadian Biomesrdquo
bull Video Response Biomes (Earth at Risk Series)
Canadian Biomes Biome ndash a collection of ecosystems that are
similar or related to each other usually in the type of plants they support
Four Canadian Biomes
The Tundra The Boreal Forest The Temperate Deciduous
Forest The Grassland
Tundra
Boreal Forest
Grassland
Temperate Deciduous Forest
The Tundra- Canadarsquos northernmost biome
Biotic FactorsAbiotic Factors
very low temp for most
of the year
short growing season
Permafrost layer beneath the soil
low precipitation
poor soil quality
rapid-growing plants
mosses and lichens
caribou
ptarmigan
lemmings
arctic foxes
wolverines
Similar to a desert low precipitation (10-12 cmyear) supports a low number of species
Two layers of soil Permafrost ndash layer of soil that never thaws Active Layer ndash above permafrost thaws in summer allowing
roots to take in water and minerals
Decomposition of Organic Matter extremely slow in cold temp because cold keeps the
bacteria and fungi from reproducing This leaves only a small amount of organic material in the soil
Nitrogen and Carbon Cycles slows the rates of the cycles slow decomposition with surface water causes the
formation of bogs These store carbon for long periods of time and decrease denitrification
The Boreal Forest- Immediately south of the Tundra
Biotic FactorsAbiotic Factors
warmer than the Tundra
no permafrost
changeable weather
soils contains some water and is acidic
precipitation 40 cmyear or more
coniferous trees
seed-eating birds
squirrels
voles
snowshoe hare
deer
pine martens
grey wolves
Climate harsh with rapid changes in temp mixing warm and cool air results in
more precipitation
Soil warmer temp allows the soil to thaw every season higher organic matter from faster rates of decomposition soil is more acidic as coniferous needles produce acid when they decay
ndash this can limit the number of plants that can grow
What are conifers Trees with needle shaped leaves ndash evergreens
4 Reasons why conifers are dominant Thin needles have a small surface area so they lose little water during
winter Thick cuticle of wax covers the needles to reduce water loss and
protect from frost damage Pyramid shape of tree and flexible branches allow the tree to support
heavy snowfall Shed their leaves slowly throughout the year so they can begin
photosynthesis when the growing season begins (advantage in a short growing season)
The Temperate Deciduous Forest- South of the Boreal Forest in EasternCentral Canada
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp then Tundra or Boreal Forest
fertile soil
precipitation up to
100 cmyear
deciduous trees
many ferns and shrubs
tree and ground squirrels
many insects
shrews and mice
deer
woodpeckers
weasels black bears wolves
What are the dominant trees in
this biome Deciduous trees (maples oaks poplars
beech and birch)
What features about deciduous trees allow them to complete with conifers
The broad leaves maximize light capture for photosynthesis
Soil and Decomposition
higher temperatures allow for faster decomposition resulting in richer
soil
Understory and Canopy Understory ndash the lower branches of a trees
Canopy ndash the upper levels of the trees
What factors allow for high biodiversity in this biome
The presence of so many different kinds of plants supports many
animals
The thick litter layer is ideal for different insects
Many insects support amphibians lizards birds and insect-eating animals
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
Questions
Read pages 74-76 and do questions 1-4 amp 6abc on page 76
Section 210-Limits on Populations
Mice populations can change drastically in 6 months 20 mice can become 5120 mice
Why donrsquot we see billionsof mice when we lookout the window
The reason is that there are limitations on all populations including mice
Carrying Capacity
Populations fluctuate but tend to be fairly stable Stabilityhappens when the population does not exceed the carryingcapacity
Carrying Capacity - The maximum number of individual species that can be supported by an ecosystem
Law of Minimum - The nutrient in least supply is the one that limits growth
Law of Tolerance - An organism can survive within a certain range of abiotic factors Going above or below this range will cause death
Biotic potential is the maximum number of offspring that a species can produce if resources were unlimited
It is regulated by four factors
1) Birth potential maximum number of offspring per birth
2) Capacity of survival number of offspring that reach reproductive age
3) Procreation number of times a species reproduces each year
4) Length of reproductive life the age of sexual maturity and the number of years the individual can reproduce
Limiting Factors
The environment provides factors that prevent populations from attaining their biotic potential Environmental Factor Population Changes
Abiotic light temperaturechemical environment
Biotic Amount of foodnumber or effectiveness of predatorsdiseases and parasitesability to compete for resources
Some factors that control population can depend on the size or density of the population
A population is dense when a large number of organisms live in one area
Density IndependentFactors
Density DependentFactors
Flood Food shortage
Fire Competition for mates or habitat
Pesticides Diseases
Change in climate or temperature
Introduction of exotic species
Destruction of habitat Increased predation
Drought Competition for water and other resources
Questions
Read pages 77-80 and do questions 1 2 amp 3 (abc) on page 80
Chapter 3Sustaining Terrestrial Ecosystems
Section 31 Canadian Biomes
Jigsaw Activity
bull In groups you will be using pages 88-93 to complete the sheets on ldquoThe Canadian Biomesrdquo
bull Video Response Biomes (Earth at Risk Series)
Canadian Biomes Biome ndash a collection of ecosystems that are
similar or related to each other usually in the type of plants they support
Four Canadian Biomes
The Tundra The Boreal Forest The Temperate Deciduous
Forest The Grassland
Tundra
Boreal Forest
Grassland
Temperate Deciduous Forest
The Tundra- Canadarsquos northernmost biome
Biotic FactorsAbiotic Factors
very low temp for most
of the year
short growing season
Permafrost layer beneath the soil
low precipitation
poor soil quality
rapid-growing plants
mosses and lichens
caribou
ptarmigan
lemmings
arctic foxes
wolverines
Similar to a desert low precipitation (10-12 cmyear) supports a low number of species
Two layers of soil Permafrost ndash layer of soil that never thaws Active Layer ndash above permafrost thaws in summer allowing
roots to take in water and minerals
Decomposition of Organic Matter extremely slow in cold temp because cold keeps the
bacteria and fungi from reproducing This leaves only a small amount of organic material in the soil
Nitrogen and Carbon Cycles slows the rates of the cycles slow decomposition with surface water causes the
formation of bogs These store carbon for long periods of time and decrease denitrification
The Boreal Forest- Immediately south of the Tundra
Biotic FactorsAbiotic Factors
warmer than the Tundra
no permafrost
changeable weather
soils contains some water and is acidic
precipitation 40 cmyear or more
coniferous trees
seed-eating birds
squirrels
voles
snowshoe hare
deer
pine martens
grey wolves
Climate harsh with rapid changes in temp mixing warm and cool air results in
more precipitation
Soil warmer temp allows the soil to thaw every season higher organic matter from faster rates of decomposition soil is more acidic as coniferous needles produce acid when they decay
ndash this can limit the number of plants that can grow
What are conifers Trees with needle shaped leaves ndash evergreens
4 Reasons why conifers are dominant Thin needles have a small surface area so they lose little water during
winter Thick cuticle of wax covers the needles to reduce water loss and
protect from frost damage Pyramid shape of tree and flexible branches allow the tree to support
heavy snowfall Shed their leaves slowly throughout the year so they can begin
photosynthesis when the growing season begins (advantage in a short growing season)
The Temperate Deciduous Forest- South of the Boreal Forest in EasternCentral Canada
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp then Tundra or Boreal Forest
fertile soil
precipitation up to
100 cmyear
deciduous trees
many ferns and shrubs
tree and ground squirrels
many insects
shrews and mice
deer
woodpeckers
weasels black bears wolves
What are the dominant trees in
this biome Deciduous trees (maples oaks poplars
beech and birch)
What features about deciduous trees allow them to complete with conifers
The broad leaves maximize light capture for photosynthesis
Soil and Decomposition
higher temperatures allow for faster decomposition resulting in richer
soil
Understory and Canopy Understory ndash the lower branches of a trees
Canopy ndash the upper levels of the trees
What factors allow for high biodiversity in this biome
The presence of so many different kinds of plants supports many
animals
The thick litter layer is ideal for different insects
Many insects support amphibians lizards birds and insect-eating animals
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
Section 210-Limits on Populations
Mice populations can change drastically in 6 months 20 mice can become 5120 mice
Why donrsquot we see billionsof mice when we lookout the window
The reason is that there are limitations on all populations including mice
Carrying Capacity
Populations fluctuate but tend to be fairly stable Stabilityhappens when the population does not exceed the carryingcapacity
Carrying Capacity - The maximum number of individual species that can be supported by an ecosystem
Law of Minimum - The nutrient in least supply is the one that limits growth
Law of Tolerance - An organism can survive within a certain range of abiotic factors Going above or below this range will cause death
Biotic potential is the maximum number of offspring that a species can produce if resources were unlimited
It is regulated by four factors
1) Birth potential maximum number of offspring per birth
2) Capacity of survival number of offspring that reach reproductive age
3) Procreation number of times a species reproduces each year
4) Length of reproductive life the age of sexual maturity and the number of years the individual can reproduce
Limiting Factors
The environment provides factors that prevent populations from attaining their biotic potential Environmental Factor Population Changes
Abiotic light temperaturechemical environment
Biotic Amount of foodnumber or effectiveness of predatorsdiseases and parasitesability to compete for resources
Some factors that control population can depend on the size or density of the population
A population is dense when a large number of organisms live in one area
Density IndependentFactors
Density DependentFactors
Flood Food shortage
Fire Competition for mates or habitat
Pesticides Diseases
Change in climate or temperature
Introduction of exotic species
Destruction of habitat Increased predation
Drought Competition for water and other resources
Questions
Read pages 77-80 and do questions 1 2 amp 3 (abc) on page 80
Chapter 3Sustaining Terrestrial Ecosystems
Section 31 Canadian Biomes
Jigsaw Activity
bull In groups you will be using pages 88-93 to complete the sheets on ldquoThe Canadian Biomesrdquo
bull Video Response Biomes (Earth at Risk Series)
Canadian Biomes Biome ndash a collection of ecosystems that are
similar or related to each other usually in the type of plants they support
Four Canadian Biomes
The Tundra The Boreal Forest The Temperate Deciduous
Forest The Grassland
Tundra
Boreal Forest
Grassland
Temperate Deciduous Forest
The Tundra- Canadarsquos northernmost biome
Biotic FactorsAbiotic Factors
very low temp for most
of the year
short growing season
Permafrost layer beneath the soil
low precipitation
poor soil quality
rapid-growing plants
mosses and lichens
caribou
ptarmigan
lemmings
arctic foxes
wolverines
Similar to a desert low precipitation (10-12 cmyear) supports a low number of species
Two layers of soil Permafrost ndash layer of soil that never thaws Active Layer ndash above permafrost thaws in summer allowing
roots to take in water and minerals
Decomposition of Organic Matter extremely slow in cold temp because cold keeps the
bacteria and fungi from reproducing This leaves only a small amount of organic material in the soil
Nitrogen and Carbon Cycles slows the rates of the cycles slow decomposition with surface water causes the
formation of bogs These store carbon for long periods of time and decrease denitrification
The Boreal Forest- Immediately south of the Tundra
Biotic FactorsAbiotic Factors
warmer than the Tundra
no permafrost
changeable weather
soils contains some water and is acidic
precipitation 40 cmyear or more
coniferous trees
seed-eating birds
squirrels
voles
snowshoe hare
deer
pine martens
grey wolves
Climate harsh with rapid changes in temp mixing warm and cool air results in
more precipitation
Soil warmer temp allows the soil to thaw every season higher organic matter from faster rates of decomposition soil is more acidic as coniferous needles produce acid when they decay
ndash this can limit the number of plants that can grow
What are conifers Trees with needle shaped leaves ndash evergreens
4 Reasons why conifers are dominant Thin needles have a small surface area so they lose little water during
winter Thick cuticle of wax covers the needles to reduce water loss and
protect from frost damage Pyramid shape of tree and flexible branches allow the tree to support
heavy snowfall Shed their leaves slowly throughout the year so they can begin
photosynthesis when the growing season begins (advantage in a short growing season)
The Temperate Deciduous Forest- South of the Boreal Forest in EasternCentral Canada
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp then Tundra or Boreal Forest
fertile soil
precipitation up to
100 cmyear
deciduous trees
many ferns and shrubs
tree and ground squirrels
many insects
shrews and mice
deer
woodpeckers
weasels black bears wolves
What are the dominant trees in
this biome Deciduous trees (maples oaks poplars
beech and birch)
What features about deciduous trees allow them to complete with conifers
The broad leaves maximize light capture for photosynthesis
Soil and Decomposition
higher temperatures allow for faster decomposition resulting in richer
soil
Understory and Canopy Understory ndash the lower branches of a trees
Canopy ndash the upper levels of the trees
What factors allow for high biodiversity in this biome
The presence of so many different kinds of plants supports many
animals
The thick litter layer is ideal for different insects
Many insects support amphibians lizards birds and insect-eating animals
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
Carrying Capacity
Populations fluctuate but tend to be fairly stable Stabilityhappens when the population does not exceed the carryingcapacity
Carrying Capacity - The maximum number of individual species that can be supported by an ecosystem
Law of Minimum - The nutrient in least supply is the one that limits growth
Law of Tolerance - An organism can survive within a certain range of abiotic factors Going above or below this range will cause death
Biotic potential is the maximum number of offspring that a species can produce if resources were unlimited
It is regulated by four factors
1) Birth potential maximum number of offspring per birth
2) Capacity of survival number of offspring that reach reproductive age
3) Procreation number of times a species reproduces each year
4) Length of reproductive life the age of sexual maturity and the number of years the individual can reproduce
Limiting Factors
The environment provides factors that prevent populations from attaining their biotic potential Environmental Factor Population Changes
Abiotic light temperaturechemical environment
Biotic Amount of foodnumber or effectiveness of predatorsdiseases and parasitesability to compete for resources
Some factors that control population can depend on the size or density of the population
A population is dense when a large number of organisms live in one area
Density IndependentFactors
Density DependentFactors
Flood Food shortage
Fire Competition for mates or habitat
Pesticides Diseases
Change in climate or temperature
Introduction of exotic species
Destruction of habitat Increased predation
Drought Competition for water and other resources
Questions
Read pages 77-80 and do questions 1 2 amp 3 (abc) on page 80
Chapter 3Sustaining Terrestrial Ecosystems
Section 31 Canadian Biomes
Jigsaw Activity
bull In groups you will be using pages 88-93 to complete the sheets on ldquoThe Canadian Biomesrdquo
bull Video Response Biomes (Earth at Risk Series)
Canadian Biomes Biome ndash a collection of ecosystems that are
similar or related to each other usually in the type of plants they support
Four Canadian Biomes
The Tundra The Boreal Forest The Temperate Deciduous
Forest The Grassland
Tundra
Boreal Forest
Grassland
Temperate Deciduous Forest
The Tundra- Canadarsquos northernmost biome
Biotic FactorsAbiotic Factors
very low temp for most
of the year
short growing season
Permafrost layer beneath the soil
low precipitation
poor soil quality
rapid-growing plants
mosses and lichens
caribou
ptarmigan
lemmings
arctic foxes
wolverines
Similar to a desert low precipitation (10-12 cmyear) supports a low number of species
Two layers of soil Permafrost ndash layer of soil that never thaws Active Layer ndash above permafrost thaws in summer allowing
roots to take in water and minerals
Decomposition of Organic Matter extremely slow in cold temp because cold keeps the
bacteria and fungi from reproducing This leaves only a small amount of organic material in the soil
Nitrogen and Carbon Cycles slows the rates of the cycles slow decomposition with surface water causes the
formation of bogs These store carbon for long periods of time and decrease denitrification
The Boreal Forest- Immediately south of the Tundra
Biotic FactorsAbiotic Factors
warmer than the Tundra
no permafrost
changeable weather
soils contains some water and is acidic
precipitation 40 cmyear or more
coniferous trees
seed-eating birds
squirrels
voles
snowshoe hare
deer
pine martens
grey wolves
Climate harsh with rapid changes in temp mixing warm and cool air results in
more precipitation
Soil warmer temp allows the soil to thaw every season higher organic matter from faster rates of decomposition soil is more acidic as coniferous needles produce acid when they decay
ndash this can limit the number of plants that can grow
What are conifers Trees with needle shaped leaves ndash evergreens
4 Reasons why conifers are dominant Thin needles have a small surface area so they lose little water during
winter Thick cuticle of wax covers the needles to reduce water loss and
protect from frost damage Pyramid shape of tree and flexible branches allow the tree to support
heavy snowfall Shed their leaves slowly throughout the year so they can begin
photosynthesis when the growing season begins (advantage in a short growing season)
The Temperate Deciduous Forest- South of the Boreal Forest in EasternCentral Canada
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp then Tundra or Boreal Forest
fertile soil
precipitation up to
100 cmyear
deciduous trees
many ferns and shrubs
tree and ground squirrels
many insects
shrews and mice
deer
woodpeckers
weasels black bears wolves
What are the dominant trees in
this biome Deciduous trees (maples oaks poplars
beech and birch)
What features about deciduous trees allow them to complete with conifers
The broad leaves maximize light capture for photosynthesis
Soil and Decomposition
higher temperatures allow for faster decomposition resulting in richer
soil
Understory and Canopy Understory ndash the lower branches of a trees
Canopy ndash the upper levels of the trees
What factors allow for high biodiversity in this biome
The presence of so many different kinds of plants supports many
animals
The thick litter layer is ideal for different insects
Many insects support amphibians lizards birds and insect-eating animals
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
Biotic potential is the maximum number of offspring that a species can produce if resources were unlimited
It is regulated by four factors
1) Birth potential maximum number of offspring per birth
2) Capacity of survival number of offspring that reach reproductive age
3) Procreation number of times a species reproduces each year
4) Length of reproductive life the age of sexual maturity and the number of years the individual can reproduce
Limiting Factors
The environment provides factors that prevent populations from attaining their biotic potential Environmental Factor Population Changes
Abiotic light temperaturechemical environment
Biotic Amount of foodnumber or effectiveness of predatorsdiseases and parasitesability to compete for resources
Some factors that control population can depend on the size or density of the population
A population is dense when a large number of organisms live in one area
Density IndependentFactors
Density DependentFactors
Flood Food shortage
Fire Competition for mates or habitat
Pesticides Diseases
Change in climate or temperature
Introduction of exotic species
Destruction of habitat Increased predation
Drought Competition for water and other resources
Questions
Read pages 77-80 and do questions 1 2 amp 3 (abc) on page 80
Chapter 3Sustaining Terrestrial Ecosystems
Section 31 Canadian Biomes
Jigsaw Activity
bull In groups you will be using pages 88-93 to complete the sheets on ldquoThe Canadian Biomesrdquo
bull Video Response Biomes (Earth at Risk Series)
Canadian Biomes Biome ndash a collection of ecosystems that are
similar or related to each other usually in the type of plants they support
Four Canadian Biomes
The Tundra The Boreal Forest The Temperate Deciduous
Forest The Grassland
Tundra
Boreal Forest
Grassland
Temperate Deciduous Forest
The Tundra- Canadarsquos northernmost biome
Biotic FactorsAbiotic Factors
very low temp for most
of the year
short growing season
Permafrost layer beneath the soil
low precipitation
poor soil quality
rapid-growing plants
mosses and lichens
caribou
ptarmigan
lemmings
arctic foxes
wolverines
Similar to a desert low precipitation (10-12 cmyear) supports a low number of species
Two layers of soil Permafrost ndash layer of soil that never thaws Active Layer ndash above permafrost thaws in summer allowing
roots to take in water and minerals
Decomposition of Organic Matter extremely slow in cold temp because cold keeps the
bacteria and fungi from reproducing This leaves only a small amount of organic material in the soil
Nitrogen and Carbon Cycles slows the rates of the cycles slow decomposition with surface water causes the
formation of bogs These store carbon for long periods of time and decrease denitrification
The Boreal Forest- Immediately south of the Tundra
Biotic FactorsAbiotic Factors
warmer than the Tundra
no permafrost
changeable weather
soils contains some water and is acidic
precipitation 40 cmyear or more
coniferous trees
seed-eating birds
squirrels
voles
snowshoe hare
deer
pine martens
grey wolves
Climate harsh with rapid changes in temp mixing warm and cool air results in
more precipitation
Soil warmer temp allows the soil to thaw every season higher organic matter from faster rates of decomposition soil is more acidic as coniferous needles produce acid when they decay
ndash this can limit the number of plants that can grow
What are conifers Trees with needle shaped leaves ndash evergreens
4 Reasons why conifers are dominant Thin needles have a small surface area so they lose little water during
winter Thick cuticle of wax covers the needles to reduce water loss and
protect from frost damage Pyramid shape of tree and flexible branches allow the tree to support
heavy snowfall Shed their leaves slowly throughout the year so they can begin
photosynthesis when the growing season begins (advantage in a short growing season)
The Temperate Deciduous Forest- South of the Boreal Forest in EasternCentral Canada
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp then Tundra or Boreal Forest
fertile soil
precipitation up to
100 cmyear
deciduous trees
many ferns and shrubs
tree and ground squirrels
many insects
shrews and mice
deer
woodpeckers
weasels black bears wolves
What are the dominant trees in
this biome Deciduous trees (maples oaks poplars
beech and birch)
What features about deciduous trees allow them to complete with conifers
The broad leaves maximize light capture for photosynthesis
Soil and Decomposition
higher temperatures allow for faster decomposition resulting in richer
soil
Understory and Canopy Understory ndash the lower branches of a trees
Canopy ndash the upper levels of the trees
What factors allow for high biodiversity in this biome
The presence of so many different kinds of plants supports many
animals
The thick litter layer is ideal for different insects
Many insects support amphibians lizards birds and insect-eating animals
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
Limiting Factors
The environment provides factors that prevent populations from attaining their biotic potential Environmental Factor Population Changes
Abiotic light temperaturechemical environment
Biotic Amount of foodnumber or effectiveness of predatorsdiseases and parasitesability to compete for resources
Some factors that control population can depend on the size or density of the population
A population is dense when a large number of organisms live in one area
Density IndependentFactors
Density DependentFactors
Flood Food shortage
Fire Competition for mates or habitat
Pesticides Diseases
Change in climate or temperature
Introduction of exotic species
Destruction of habitat Increased predation
Drought Competition for water and other resources
Questions
Read pages 77-80 and do questions 1 2 amp 3 (abc) on page 80
Chapter 3Sustaining Terrestrial Ecosystems
Section 31 Canadian Biomes
Jigsaw Activity
bull In groups you will be using pages 88-93 to complete the sheets on ldquoThe Canadian Biomesrdquo
bull Video Response Biomes (Earth at Risk Series)
Canadian Biomes Biome ndash a collection of ecosystems that are
similar or related to each other usually in the type of plants they support
Four Canadian Biomes
The Tundra The Boreal Forest The Temperate Deciduous
Forest The Grassland
Tundra
Boreal Forest
Grassland
Temperate Deciduous Forest
The Tundra- Canadarsquos northernmost biome
Biotic FactorsAbiotic Factors
very low temp for most
of the year
short growing season
Permafrost layer beneath the soil
low precipitation
poor soil quality
rapid-growing plants
mosses and lichens
caribou
ptarmigan
lemmings
arctic foxes
wolverines
Similar to a desert low precipitation (10-12 cmyear) supports a low number of species
Two layers of soil Permafrost ndash layer of soil that never thaws Active Layer ndash above permafrost thaws in summer allowing
roots to take in water and minerals
Decomposition of Organic Matter extremely slow in cold temp because cold keeps the
bacteria and fungi from reproducing This leaves only a small amount of organic material in the soil
Nitrogen and Carbon Cycles slows the rates of the cycles slow decomposition with surface water causes the
formation of bogs These store carbon for long periods of time and decrease denitrification
The Boreal Forest- Immediately south of the Tundra
Biotic FactorsAbiotic Factors
warmer than the Tundra
no permafrost
changeable weather
soils contains some water and is acidic
precipitation 40 cmyear or more
coniferous trees
seed-eating birds
squirrels
voles
snowshoe hare
deer
pine martens
grey wolves
Climate harsh with rapid changes in temp mixing warm and cool air results in
more precipitation
Soil warmer temp allows the soil to thaw every season higher organic matter from faster rates of decomposition soil is more acidic as coniferous needles produce acid when they decay
ndash this can limit the number of plants that can grow
What are conifers Trees with needle shaped leaves ndash evergreens
4 Reasons why conifers are dominant Thin needles have a small surface area so they lose little water during
winter Thick cuticle of wax covers the needles to reduce water loss and
protect from frost damage Pyramid shape of tree and flexible branches allow the tree to support
heavy snowfall Shed their leaves slowly throughout the year so they can begin
photosynthesis when the growing season begins (advantage in a short growing season)
The Temperate Deciduous Forest- South of the Boreal Forest in EasternCentral Canada
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp then Tundra or Boreal Forest
fertile soil
precipitation up to
100 cmyear
deciduous trees
many ferns and shrubs
tree and ground squirrels
many insects
shrews and mice
deer
woodpeckers
weasels black bears wolves
What are the dominant trees in
this biome Deciduous trees (maples oaks poplars
beech and birch)
What features about deciduous trees allow them to complete with conifers
The broad leaves maximize light capture for photosynthesis
Soil and Decomposition
higher temperatures allow for faster decomposition resulting in richer
soil
Understory and Canopy Understory ndash the lower branches of a trees
Canopy ndash the upper levels of the trees
What factors allow for high biodiversity in this biome
The presence of so many different kinds of plants supports many
animals
The thick litter layer is ideal for different insects
Many insects support amphibians lizards birds and insect-eating animals
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
Some factors that control population can depend on the size or density of the population
A population is dense when a large number of organisms live in one area
Density IndependentFactors
Density DependentFactors
Flood Food shortage
Fire Competition for mates or habitat
Pesticides Diseases
Change in climate or temperature
Introduction of exotic species
Destruction of habitat Increased predation
Drought Competition for water and other resources
Questions
Read pages 77-80 and do questions 1 2 amp 3 (abc) on page 80
Chapter 3Sustaining Terrestrial Ecosystems
Section 31 Canadian Biomes
Jigsaw Activity
bull In groups you will be using pages 88-93 to complete the sheets on ldquoThe Canadian Biomesrdquo
bull Video Response Biomes (Earth at Risk Series)
Canadian Biomes Biome ndash a collection of ecosystems that are
similar or related to each other usually in the type of plants they support
Four Canadian Biomes
The Tundra The Boreal Forest The Temperate Deciduous
Forest The Grassland
Tundra
Boreal Forest
Grassland
Temperate Deciduous Forest
The Tundra- Canadarsquos northernmost biome
Biotic FactorsAbiotic Factors
very low temp for most
of the year
short growing season
Permafrost layer beneath the soil
low precipitation
poor soil quality
rapid-growing plants
mosses and lichens
caribou
ptarmigan
lemmings
arctic foxes
wolverines
Similar to a desert low precipitation (10-12 cmyear) supports a low number of species
Two layers of soil Permafrost ndash layer of soil that never thaws Active Layer ndash above permafrost thaws in summer allowing
roots to take in water and minerals
Decomposition of Organic Matter extremely slow in cold temp because cold keeps the
bacteria and fungi from reproducing This leaves only a small amount of organic material in the soil
Nitrogen and Carbon Cycles slows the rates of the cycles slow decomposition with surface water causes the
formation of bogs These store carbon for long periods of time and decrease denitrification
The Boreal Forest- Immediately south of the Tundra
Biotic FactorsAbiotic Factors
warmer than the Tundra
no permafrost
changeable weather
soils contains some water and is acidic
precipitation 40 cmyear or more
coniferous trees
seed-eating birds
squirrels
voles
snowshoe hare
deer
pine martens
grey wolves
Climate harsh with rapid changes in temp mixing warm and cool air results in
more precipitation
Soil warmer temp allows the soil to thaw every season higher organic matter from faster rates of decomposition soil is more acidic as coniferous needles produce acid when they decay
ndash this can limit the number of plants that can grow
What are conifers Trees with needle shaped leaves ndash evergreens
4 Reasons why conifers are dominant Thin needles have a small surface area so they lose little water during
winter Thick cuticle of wax covers the needles to reduce water loss and
protect from frost damage Pyramid shape of tree and flexible branches allow the tree to support
heavy snowfall Shed their leaves slowly throughout the year so they can begin
photosynthesis when the growing season begins (advantage in a short growing season)
The Temperate Deciduous Forest- South of the Boreal Forest in EasternCentral Canada
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp then Tundra or Boreal Forest
fertile soil
precipitation up to
100 cmyear
deciduous trees
many ferns and shrubs
tree and ground squirrels
many insects
shrews and mice
deer
woodpeckers
weasels black bears wolves
What are the dominant trees in
this biome Deciduous trees (maples oaks poplars
beech and birch)
What features about deciduous trees allow them to complete with conifers
The broad leaves maximize light capture for photosynthesis
Soil and Decomposition
higher temperatures allow for faster decomposition resulting in richer
soil
Understory and Canopy Understory ndash the lower branches of a trees
Canopy ndash the upper levels of the trees
What factors allow for high biodiversity in this biome
The presence of so many different kinds of plants supports many
animals
The thick litter layer is ideal for different insects
Many insects support amphibians lizards birds and insect-eating animals
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
Questions
Read pages 77-80 and do questions 1 2 amp 3 (abc) on page 80
Chapter 3Sustaining Terrestrial Ecosystems
Section 31 Canadian Biomes
Jigsaw Activity
bull In groups you will be using pages 88-93 to complete the sheets on ldquoThe Canadian Biomesrdquo
bull Video Response Biomes (Earth at Risk Series)
Canadian Biomes Biome ndash a collection of ecosystems that are
similar or related to each other usually in the type of plants they support
Four Canadian Biomes
The Tundra The Boreal Forest The Temperate Deciduous
Forest The Grassland
Tundra
Boreal Forest
Grassland
Temperate Deciduous Forest
The Tundra- Canadarsquos northernmost biome
Biotic FactorsAbiotic Factors
very low temp for most
of the year
short growing season
Permafrost layer beneath the soil
low precipitation
poor soil quality
rapid-growing plants
mosses and lichens
caribou
ptarmigan
lemmings
arctic foxes
wolverines
Similar to a desert low precipitation (10-12 cmyear) supports a low number of species
Two layers of soil Permafrost ndash layer of soil that never thaws Active Layer ndash above permafrost thaws in summer allowing
roots to take in water and minerals
Decomposition of Organic Matter extremely slow in cold temp because cold keeps the
bacteria and fungi from reproducing This leaves only a small amount of organic material in the soil
Nitrogen and Carbon Cycles slows the rates of the cycles slow decomposition with surface water causes the
formation of bogs These store carbon for long periods of time and decrease denitrification
The Boreal Forest- Immediately south of the Tundra
Biotic FactorsAbiotic Factors
warmer than the Tundra
no permafrost
changeable weather
soils contains some water and is acidic
precipitation 40 cmyear or more
coniferous trees
seed-eating birds
squirrels
voles
snowshoe hare
deer
pine martens
grey wolves
Climate harsh with rapid changes in temp mixing warm and cool air results in
more precipitation
Soil warmer temp allows the soil to thaw every season higher organic matter from faster rates of decomposition soil is more acidic as coniferous needles produce acid when they decay
ndash this can limit the number of plants that can grow
What are conifers Trees with needle shaped leaves ndash evergreens
4 Reasons why conifers are dominant Thin needles have a small surface area so they lose little water during
winter Thick cuticle of wax covers the needles to reduce water loss and
protect from frost damage Pyramid shape of tree and flexible branches allow the tree to support
heavy snowfall Shed their leaves slowly throughout the year so they can begin
photosynthesis when the growing season begins (advantage in a short growing season)
The Temperate Deciduous Forest- South of the Boreal Forest in EasternCentral Canada
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp then Tundra or Boreal Forest
fertile soil
precipitation up to
100 cmyear
deciduous trees
many ferns and shrubs
tree and ground squirrels
many insects
shrews and mice
deer
woodpeckers
weasels black bears wolves
What are the dominant trees in
this biome Deciduous trees (maples oaks poplars
beech and birch)
What features about deciduous trees allow them to complete with conifers
The broad leaves maximize light capture for photosynthesis
Soil and Decomposition
higher temperatures allow for faster decomposition resulting in richer
soil
Understory and Canopy Understory ndash the lower branches of a trees
Canopy ndash the upper levels of the trees
What factors allow for high biodiversity in this biome
The presence of so many different kinds of plants supports many
animals
The thick litter layer is ideal for different insects
Many insects support amphibians lizards birds and insect-eating animals
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
Chapter 3Sustaining Terrestrial Ecosystems
Section 31 Canadian Biomes
Jigsaw Activity
bull In groups you will be using pages 88-93 to complete the sheets on ldquoThe Canadian Biomesrdquo
bull Video Response Biomes (Earth at Risk Series)
Canadian Biomes Biome ndash a collection of ecosystems that are
similar or related to each other usually in the type of plants they support
Four Canadian Biomes
The Tundra The Boreal Forest The Temperate Deciduous
Forest The Grassland
Tundra
Boreal Forest
Grassland
Temperate Deciduous Forest
The Tundra- Canadarsquos northernmost biome
Biotic FactorsAbiotic Factors
very low temp for most
of the year
short growing season
Permafrost layer beneath the soil
low precipitation
poor soil quality
rapid-growing plants
mosses and lichens
caribou
ptarmigan
lemmings
arctic foxes
wolverines
Similar to a desert low precipitation (10-12 cmyear) supports a low number of species
Two layers of soil Permafrost ndash layer of soil that never thaws Active Layer ndash above permafrost thaws in summer allowing
roots to take in water and minerals
Decomposition of Organic Matter extremely slow in cold temp because cold keeps the
bacteria and fungi from reproducing This leaves only a small amount of organic material in the soil
Nitrogen and Carbon Cycles slows the rates of the cycles slow decomposition with surface water causes the
formation of bogs These store carbon for long periods of time and decrease denitrification
The Boreal Forest- Immediately south of the Tundra
Biotic FactorsAbiotic Factors
warmer than the Tundra
no permafrost
changeable weather
soils contains some water and is acidic
precipitation 40 cmyear or more
coniferous trees
seed-eating birds
squirrels
voles
snowshoe hare
deer
pine martens
grey wolves
Climate harsh with rapid changes in temp mixing warm and cool air results in
more precipitation
Soil warmer temp allows the soil to thaw every season higher organic matter from faster rates of decomposition soil is more acidic as coniferous needles produce acid when they decay
ndash this can limit the number of plants that can grow
What are conifers Trees with needle shaped leaves ndash evergreens
4 Reasons why conifers are dominant Thin needles have a small surface area so they lose little water during
winter Thick cuticle of wax covers the needles to reduce water loss and
protect from frost damage Pyramid shape of tree and flexible branches allow the tree to support
heavy snowfall Shed their leaves slowly throughout the year so they can begin
photosynthesis when the growing season begins (advantage in a short growing season)
The Temperate Deciduous Forest- South of the Boreal Forest in EasternCentral Canada
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp then Tundra or Boreal Forest
fertile soil
precipitation up to
100 cmyear
deciduous trees
many ferns and shrubs
tree and ground squirrels
many insects
shrews and mice
deer
woodpeckers
weasels black bears wolves
What are the dominant trees in
this biome Deciduous trees (maples oaks poplars
beech and birch)
What features about deciduous trees allow them to complete with conifers
The broad leaves maximize light capture for photosynthesis
Soil and Decomposition
higher temperatures allow for faster decomposition resulting in richer
soil
Understory and Canopy Understory ndash the lower branches of a trees
Canopy ndash the upper levels of the trees
What factors allow for high biodiversity in this biome
The presence of so many different kinds of plants supports many
animals
The thick litter layer is ideal for different insects
Many insects support amphibians lizards birds and insect-eating animals
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
Canadian Biomes Biome ndash a collection of ecosystems that are
similar or related to each other usually in the type of plants they support
Four Canadian Biomes
The Tundra The Boreal Forest The Temperate Deciduous
Forest The Grassland
Tundra
Boreal Forest
Grassland
Temperate Deciduous Forest
The Tundra- Canadarsquos northernmost biome
Biotic FactorsAbiotic Factors
very low temp for most
of the year
short growing season
Permafrost layer beneath the soil
low precipitation
poor soil quality
rapid-growing plants
mosses and lichens
caribou
ptarmigan
lemmings
arctic foxes
wolverines
Similar to a desert low precipitation (10-12 cmyear) supports a low number of species
Two layers of soil Permafrost ndash layer of soil that never thaws Active Layer ndash above permafrost thaws in summer allowing
roots to take in water and minerals
Decomposition of Organic Matter extremely slow in cold temp because cold keeps the
bacteria and fungi from reproducing This leaves only a small amount of organic material in the soil
Nitrogen and Carbon Cycles slows the rates of the cycles slow decomposition with surface water causes the
formation of bogs These store carbon for long periods of time and decrease denitrification
The Boreal Forest- Immediately south of the Tundra
Biotic FactorsAbiotic Factors
warmer than the Tundra
no permafrost
changeable weather
soils contains some water and is acidic
precipitation 40 cmyear or more
coniferous trees
seed-eating birds
squirrels
voles
snowshoe hare
deer
pine martens
grey wolves
Climate harsh with rapid changes in temp mixing warm and cool air results in
more precipitation
Soil warmer temp allows the soil to thaw every season higher organic matter from faster rates of decomposition soil is more acidic as coniferous needles produce acid when they decay
ndash this can limit the number of plants that can grow
What are conifers Trees with needle shaped leaves ndash evergreens
4 Reasons why conifers are dominant Thin needles have a small surface area so they lose little water during
winter Thick cuticle of wax covers the needles to reduce water loss and
protect from frost damage Pyramid shape of tree and flexible branches allow the tree to support
heavy snowfall Shed their leaves slowly throughout the year so they can begin
photosynthesis when the growing season begins (advantage in a short growing season)
The Temperate Deciduous Forest- South of the Boreal Forest in EasternCentral Canada
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp then Tundra or Boreal Forest
fertile soil
precipitation up to
100 cmyear
deciduous trees
many ferns and shrubs
tree and ground squirrels
many insects
shrews and mice
deer
woodpeckers
weasels black bears wolves
What are the dominant trees in
this biome Deciduous trees (maples oaks poplars
beech and birch)
What features about deciduous trees allow them to complete with conifers
The broad leaves maximize light capture for photosynthesis
Soil and Decomposition
higher temperatures allow for faster decomposition resulting in richer
soil
Understory and Canopy Understory ndash the lower branches of a trees
Canopy ndash the upper levels of the trees
What factors allow for high biodiversity in this biome
The presence of so many different kinds of plants supports many
animals
The thick litter layer is ideal for different insects
Many insects support amphibians lizards birds and insect-eating animals
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
The Tundra- Canadarsquos northernmost biome
Biotic FactorsAbiotic Factors
very low temp for most
of the year
short growing season
Permafrost layer beneath the soil
low precipitation
poor soil quality
rapid-growing plants
mosses and lichens
caribou
ptarmigan
lemmings
arctic foxes
wolverines
Similar to a desert low precipitation (10-12 cmyear) supports a low number of species
Two layers of soil Permafrost ndash layer of soil that never thaws Active Layer ndash above permafrost thaws in summer allowing
roots to take in water and minerals
Decomposition of Organic Matter extremely slow in cold temp because cold keeps the
bacteria and fungi from reproducing This leaves only a small amount of organic material in the soil
Nitrogen and Carbon Cycles slows the rates of the cycles slow decomposition with surface water causes the
formation of bogs These store carbon for long periods of time and decrease denitrification
The Boreal Forest- Immediately south of the Tundra
Biotic FactorsAbiotic Factors
warmer than the Tundra
no permafrost
changeable weather
soils contains some water and is acidic
precipitation 40 cmyear or more
coniferous trees
seed-eating birds
squirrels
voles
snowshoe hare
deer
pine martens
grey wolves
Climate harsh with rapid changes in temp mixing warm and cool air results in
more precipitation
Soil warmer temp allows the soil to thaw every season higher organic matter from faster rates of decomposition soil is more acidic as coniferous needles produce acid when they decay
ndash this can limit the number of plants that can grow
What are conifers Trees with needle shaped leaves ndash evergreens
4 Reasons why conifers are dominant Thin needles have a small surface area so they lose little water during
winter Thick cuticle of wax covers the needles to reduce water loss and
protect from frost damage Pyramid shape of tree and flexible branches allow the tree to support
heavy snowfall Shed their leaves slowly throughout the year so they can begin
photosynthesis when the growing season begins (advantage in a short growing season)
The Temperate Deciduous Forest- South of the Boreal Forest in EasternCentral Canada
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp then Tundra or Boreal Forest
fertile soil
precipitation up to
100 cmyear
deciduous trees
many ferns and shrubs
tree and ground squirrels
many insects
shrews and mice
deer
woodpeckers
weasels black bears wolves
What are the dominant trees in
this biome Deciduous trees (maples oaks poplars
beech and birch)
What features about deciduous trees allow them to complete with conifers
The broad leaves maximize light capture for photosynthesis
Soil and Decomposition
higher temperatures allow for faster decomposition resulting in richer
soil
Understory and Canopy Understory ndash the lower branches of a trees
Canopy ndash the upper levels of the trees
What factors allow for high biodiversity in this biome
The presence of so many different kinds of plants supports many
animals
The thick litter layer is ideal for different insects
Many insects support amphibians lizards birds and insect-eating animals
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
Similar to a desert low precipitation (10-12 cmyear) supports a low number of species
Two layers of soil Permafrost ndash layer of soil that never thaws Active Layer ndash above permafrost thaws in summer allowing
roots to take in water and minerals
Decomposition of Organic Matter extremely slow in cold temp because cold keeps the
bacteria and fungi from reproducing This leaves only a small amount of organic material in the soil
Nitrogen and Carbon Cycles slows the rates of the cycles slow decomposition with surface water causes the
formation of bogs These store carbon for long periods of time and decrease denitrification
The Boreal Forest- Immediately south of the Tundra
Biotic FactorsAbiotic Factors
warmer than the Tundra
no permafrost
changeable weather
soils contains some water and is acidic
precipitation 40 cmyear or more
coniferous trees
seed-eating birds
squirrels
voles
snowshoe hare
deer
pine martens
grey wolves
Climate harsh with rapid changes in temp mixing warm and cool air results in
more precipitation
Soil warmer temp allows the soil to thaw every season higher organic matter from faster rates of decomposition soil is more acidic as coniferous needles produce acid when they decay
ndash this can limit the number of plants that can grow
What are conifers Trees with needle shaped leaves ndash evergreens
4 Reasons why conifers are dominant Thin needles have a small surface area so they lose little water during
winter Thick cuticle of wax covers the needles to reduce water loss and
protect from frost damage Pyramid shape of tree and flexible branches allow the tree to support
heavy snowfall Shed their leaves slowly throughout the year so they can begin
photosynthesis when the growing season begins (advantage in a short growing season)
The Temperate Deciduous Forest- South of the Boreal Forest in EasternCentral Canada
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp then Tundra or Boreal Forest
fertile soil
precipitation up to
100 cmyear
deciduous trees
many ferns and shrubs
tree and ground squirrels
many insects
shrews and mice
deer
woodpeckers
weasels black bears wolves
What are the dominant trees in
this biome Deciduous trees (maples oaks poplars
beech and birch)
What features about deciduous trees allow them to complete with conifers
The broad leaves maximize light capture for photosynthesis
Soil and Decomposition
higher temperatures allow for faster decomposition resulting in richer
soil
Understory and Canopy Understory ndash the lower branches of a trees
Canopy ndash the upper levels of the trees
What factors allow for high biodiversity in this biome
The presence of so many different kinds of plants supports many
animals
The thick litter layer is ideal for different insects
Many insects support amphibians lizards birds and insect-eating animals
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
The Boreal Forest- Immediately south of the Tundra
Biotic FactorsAbiotic Factors
warmer than the Tundra
no permafrost
changeable weather
soils contains some water and is acidic
precipitation 40 cmyear or more
coniferous trees
seed-eating birds
squirrels
voles
snowshoe hare
deer
pine martens
grey wolves
Climate harsh with rapid changes in temp mixing warm and cool air results in
more precipitation
Soil warmer temp allows the soil to thaw every season higher organic matter from faster rates of decomposition soil is more acidic as coniferous needles produce acid when they decay
ndash this can limit the number of plants that can grow
What are conifers Trees with needle shaped leaves ndash evergreens
4 Reasons why conifers are dominant Thin needles have a small surface area so they lose little water during
winter Thick cuticle of wax covers the needles to reduce water loss and
protect from frost damage Pyramid shape of tree and flexible branches allow the tree to support
heavy snowfall Shed their leaves slowly throughout the year so they can begin
photosynthesis when the growing season begins (advantage in a short growing season)
The Temperate Deciduous Forest- South of the Boreal Forest in EasternCentral Canada
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp then Tundra or Boreal Forest
fertile soil
precipitation up to
100 cmyear
deciduous trees
many ferns and shrubs
tree and ground squirrels
many insects
shrews and mice
deer
woodpeckers
weasels black bears wolves
What are the dominant trees in
this biome Deciduous trees (maples oaks poplars
beech and birch)
What features about deciduous trees allow them to complete with conifers
The broad leaves maximize light capture for photosynthesis
Soil and Decomposition
higher temperatures allow for faster decomposition resulting in richer
soil
Understory and Canopy Understory ndash the lower branches of a trees
Canopy ndash the upper levels of the trees
What factors allow for high biodiversity in this biome
The presence of so many different kinds of plants supports many
animals
The thick litter layer is ideal for different insects
Many insects support amphibians lizards birds and insect-eating animals
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
Climate harsh with rapid changes in temp mixing warm and cool air results in
more precipitation
Soil warmer temp allows the soil to thaw every season higher organic matter from faster rates of decomposition soil is more acidic as coniferous needles produce acid when they decay
ndash this can limit the number of plants that can grow
What are conifers Trees with needle shaped leaves ndash evergreens
4 Reasons why conifers are dominant Thin needles have a small surface area so they lose little water during
winter Thick cuticle of wax covers the needles to reduce water loss and
protect from frost damage Pyramid shape of tree and flexible branches allow the tree to support
heavy snowfall Shed their leaves slowly throughout the year so they can begin
photosynthesis when the growing season begins (advantage in a short growing season)
The Temperate Deciduous Forest- South of the Boreal Forest in EasternCentral Canada
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp then Tundra or Boreal Forest
fertile soil
precipitation up to
100 cmyear
deciduous trees
many ferns and shrubs
tree and ground squirrels
many insects
shrews and mice
deer
woodpeckers
weasels black bears wolves
What are the dominant trees in
this biome Deciduous trees (maples oaks poplars
beech and birch)
What features about deciduous trees allow them to complete with conifers
The broad leaves maximize light capture for photosynthesis
Soil and Decomposition
higher temperatures allow for faster decomposition resulting in richer
soil
Understory and Canopy Understory ndash the lower branches of a trees
Canopy ndash the upper levels of the trees
What factors allow for high biodiversity in this biome
The presence of so many different kinds of plants supports many
animals
The thick litter layer is ideal for different insects
Many insects support amphibians lizards birds and insect-eating animals
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
The Temperate Deciduous Forest- South of the Boreal Forest in EasternCentral Canada
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp then Tundra or Boreal Forest
fertile soil
precipitation up to
100 cmyear
deciduous trees
many ferns and shrubs
tree and ground squirrels
many insects
shrews and mice
deer
woodpeckers
weasels black bears wolves
What are the dominant trees in
this biome Deciduous trees (maples oaks poplars
beech and birch)
What features about deciduous trees allow them to complete with conifers
The broad leaves maximize light capture for photosynthesis
Soil and Decomposition
higher temperatures allow for faster decomposition resulting in richer
soil
Understory and Canopy Understory ndash the lower branches of a trees
Canopy ndash the upper levels of the trees
What factors allow for high biodiversity in this biome
The presence of so many different kinds of plants supports many
animals
The thick litter layer is ideal for different insects
Many insects support amphibians lizards birds and insect-eating animals
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
What are the dominant trees in
this biome Deciduous trees (maples oaks poplars
beech and birch)
What features about deciduous trees allow them to complete with conifers
The broad leaves maximize light capture for photosynthesis
Soil and Decomposition
higher temperatures allow for faster decomposition resulting in richer
soil
Understory and Canopy Understory ndash the lower branches of a trees
Canopy ndash the upper levels of the trees
What factors allow for high biodiversity in this biome
The presence of so many different kinds of plants supports many
animals
The thick litter layer is ideal for different insects
Many insects support amphibians lizards birds and insect-eating animals
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
The Grassland- At the same latitude as the deciduous forest
Biotic FactorsAbiotic Factors
longer growing season
than the Boreal Forest
higher temp than Tundra and Boreal Forest
rich fertile soil
precipitation from 25-75 cmyear
fescue grasses
grasshoppers
bison
voles mice
snakes
hawks
wolves
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
What is the main difference between it and the deciduous forest biomes
Grasslands receive less moisture (25-75 cmyear) not enough to support trees except near
ponds lakes and rivers
What abiotic factor played the role of decomposer in this ecosystem fire
Soil and Decomposition most fertile soil (black)in the world Rapid decomposition due
to high summer temp and short lived grasses
Biodiversity Low Grasslands only have one layer to support animals
Deciduous forests have three layers ndash canopy understory and litter layer
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
Section 33 Soil and Itrsquos Formation
Components of Soil Soil is very important in our lives Without healthy soil we
canrsquot grow enough food Soil is in layers each with itrsquos own color and texture
Starting from the top they are
1 Litter - Made up of partly decomposed grass and leaves It acts as a blanket protecting the other layers from temperature changes and water loss
2 Topsoil - Made up of small particles of rock with decaying plant and animal material (humus) Humus is black so topsoil is usually dark and has a rich supply of minerals and nutrients Air and water are also found here to help with decomposition
3 Subsoil - Made up of more stones and less organic material It is lighter in color It may have large amounts of minerals such as iron and aluminum
4 Bedrock - A layer of rock that marks the end of the soil
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
Formation of Soil
Soil starts out as bedrock but over time weather (rain wind frost snow) and living things break it into smaller and smaller pieces This is called weathering
Once there are enough small particles of rock plants can grow When they die they add to the soil and more will grow This process can take hundreds or thousands of years
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
Water Beneath the Soil Surface water is precipitation (rain snow sleet hail) that
is above ground
Ground water is water that has flowed into the soil and rocks
Percolation is the process of water being pulled down through the soil by gravity The larger the particles in the soil the more air there is between them and the water flows down faster
The water table is the boundary between the area where ground water is percolating down and a layer that canrsquot hold any more water (saturated)
Leaching is a serious problem Sometimes when water percolates down through the soil it carries minerals and nutrients with it This removes it from the topsoil and plants canrsquot get to it
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
Soil pH
Soil can be 1 Acidic
2 Neutral
3 Basic (Alkaline)
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
The pH is determined by the type of rock that the soil was formed from and the plants that grow in it (more plants more acidic)
Acid rain and snow also make a difference
The pH of the soil determines what can grow there Mosses are one of the few plants that do very well in acidic soils
Calcium or lime can be added to make the soil more alkaline (basic)
In Canadarsquos grasslands the soil is basic because it is formed from limestone Prairie grasses do very well while most trees donrsquot
Sulfur can be added to the soil to make it more acidic
Assignment
Read pages 97-99 and do questions 1-8 on page 99
Assignment
Read pages 97-99 and do questions 1-8 on page 99