2010 Lecture _ 2 Structure & Diversity of Ecosystems

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    (Physical) Structure&

    Diversity(biological structure)

    ofEcosystems

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    Apopulation :

    a group ofindividualsofthesamespecies

    inhabiting thesame area atthesametime.

    Important characteristics:

    Population Size

    Population Density Genetic Diversity

    Autecology & Population Ecology

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    Kirkwood Lake Pr

    plantation planted

    in 1928 :notebiological &

    physical structure

    ofmonoculture

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    Communities :

    populationsofmanyspecies

    living & interacting together

    inthesame location

    atthesametime.

    Similar communitiesoccur undersimilarenvironmental conditions; but

    Composition & structure canvary

    considerablyfromone locationto another.

    Ecotones : Transitions between communities.

    Community Ecologyor Synecology

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    Physical STRUCTURETerrestrial Ecosystems based primarilyongrowth habitofplants

    ground layer (bryophytes & herbs +

    dead,downedtrees)

    shrubby layer understory canopy

    (sometrees suppressed)

    overstory canopy

    (dominanttrees;may bemorethanone) climbing vines & epiphytes

    may beonlyone layer (?)

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    Rich understory species &

    downed logs / coarse woody

    debris

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    Greenwood Lake White Pine Stand Diversity

    Foreststructure & compositionOverstory: 100% Pw (composition)

    Lower canopy: white & black spruce, balsam

    fir, white & yellow birch,sugarmapleShrub layer:mountainmaple and beakedhazel

    Herbaceous layer

    Standing snags and downed logs(coarse woody debris)

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    Physical STRUCTURE

    Aquatic Ecosystems

    (standing orflowing water)

    based 1 on chemical propertiesofwater:1. salinity(saltwater,freshwater, brackish)

    2. temperature

    3. dissolvedoxygen4. Clarity(colour & how well sunlightistransmitted)

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    FreshwaterAquatic Ecosystem

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    Changesoverspace & time

    Ecological succession (time)

    & zonation (space)

    (See E&FBCh.21; SternCh.25)

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    Succession

    During succession plantspecies (& otherorganisms) graduallychangetheirenvironment

    sothatotherspecies are better adaptedtonew environment;

    New specieseventually becomethedominant

    plantformsinthat area. Species composition (& communitystructure)

    has changed.

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    Succession

    Primary Succession - Soil Formation

    Secondary Succession - Disturbed areas

    Pioneering, Transitional & Climaxspecies:

    seres

    Climax Vegetation - Stable plant associations

    (structure & diversityinequilibrium)

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    Primary Succession

    Xerosere :Primarysuccessionthat begins with bare rocks

    and lava thathave beenexposedthrough

    glacial orvolcanic activity,orthroughlandslides

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    Primary Succession

    Hydrosere :Successionin wethabitats.

    May be accelerated byeutrophication:

    duetoenrichmentfromsedimentorother runoffcomponents

    (ie. phosphorousfoundin

    fertilizers & detergents)

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    Secondary Succession:Fire Ecology

    Natural fires,started primarily by lightning,have played a roleinecosystemsfor

    thousandsofyears

    ie. Western US, growth ringsofPonderosaPinesfire cycle wasofevery 6-7years;

    aroundhere, 60-120 typical

    specieshavespecific adaptationsto regular

    fires;trying toeliminatefiresdisruptsnatural

    cycles & ecosystems; can leadto

    catastrophic fires.

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    Fire Ecology

    Fires also play a roleinforestspeciescomposition:

    Manytreespecies repeatedly replace

    themselves afterfires (fire climax) Firesmaintain grasslands by recycling

    deadorganic material, and byeliminating

    shrubs and woodyspecies.

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    EdaphicClimax

    Somesiteshavespecific soil typesthat restrictthespeciesthat can grow there:

    dry, acidic & nutrient-poor: jack pine

    wet, acidic & nutrient-poor: black spruce

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    Diversity

    Number & proportionofspecies can beassessed atdifferent levels

    plant communityor association

    eg.foreststand,meadow watershedor landscape

    forest region

    biome(E&FBCh. 28 & 29; SternCh. 26)

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    Tundra

    Primarily abovethe arctic circle Abovetreeline

    Precipitation averages < 25 cm annually

    Permafrostholds water atornearthesurface

    Short growing seasonof2-3months

    Hightemperatures rangeto about 27oC Veryfragile

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    Taiga

    NorthernConifer (Boreal)ForestAdjacentto andsouthofarctic tundra

    Dominated by Spruce,Fir, and Pine

    Disturbance-drivenecosystems (1 fire) ExtremeClimate:

    Temperate Range-50oCto30oC

    Annual precipitation rangesfrom 25-100cm,mostlyinthesummer

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    Temperate DeciduousForest

    Composedofmostly broad-leaved (fall)deciduoustreespecies

    Mostlyin continental interiorsofNorthern

    Hemisphere

    Longer growing season:

    Temperatures rangefrom4oCto 20oC

    Annual precipitation rangesfrom 50-165 cm;mostlyoccursinsummer

    During summer,solid canopy keepsdirect

    sunlightfrom reaching theforestfloor

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    Algonquin Park

    Forest

    Authority

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    Grassland

    Foundininteriorofcontinental massesoftendueto rainshadow effect

    Broadleaftrees,butonly around water courses

    Mostlyone layerto communitystructure

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    Grassland

    Warmsummertemperaturesincreasesevaporationrates

    Annual precipitation rangesfrom 25-100 cm

    Temperatures rangefrom-45oCto45oC

    NorthAmerican grasslands (prairies) grew onfertilesoilssupporting largeherdsofmigratory grazingbuffalo

    Mediterranean climate receivesmost

    precipitationinthe winter,thus grassesdonotgrow astall asthoseofMidwestern prairies

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    Desert

    Manyofthe worldsmajordeserts are located at30o N and30o S latitude

    Plant adaptationsincludethick cuticles, water-

    storagetissuesinstems and leaves, andthick

    leaves and / or reducedinsize Verydry:

    Most receive < 12.5 cm annual precipitation

    Low humidity Widedailytemperaturefluctuations

    15oC- 35oCon a hotsummerday

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    WesternCoastal Forest

    TemperateConiferous Rainforests Pacific Northwest

    w slopeofmountainous spineinNA

    orographic precipitation

    -10 Cto +10 Ctemperature range

    long growing season

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    MountainForests

    SubalpineForests portionsofthe RockyMountains andthe

    Sierra Nevada Mountains

    SimilartoBoreal Forest

    Conspicuous altitudinal zonationofspecies

    Relativelydrysummers Frequentforestfire regime

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    Tropical RainForest

    Closeto Equator

    Verydiverse communitiesdominated by broad-leavedevergreentrees

    Densemulti-layered canopy

    Shallow rootsystems

    Poorsoils;Nutrientseither uptaken by plantsorleached byheavy rainfall

    Annual precipitation rangesfrom 200-400 cm.

    Nodryordormantseason Humidity usually > 80%.

    Temperatures range between 25oC and35oC.

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