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4.3. Carbon cycling Miltiadis-Spyridon Kitsos Platon IB Diploma http://scied.ucar.edu/sites/default/files/images/large_image_for_image_content/carbon_cycle_diagram_ipcc_900x543.jpg http://scied.ucar.edu/sites/default/files/images/large_image_for_image_content/carbon_cycle_diagram_ipcc_900x543.jpg

4.3 Carbon cycling

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Page 1: 4.3 Carbon cycling

4.3. Carbon cycling

Miltiadis-Spyridon Kitsos Platon IB Diploma

http://scied.ucar.edu/sites/default/files/images/large_image_for_image_content/carbon_cycle_diagram_ipcc_900x543.jpg

http://scied.ucar.edu/sites/default/files/images/large_image_for_image_content/carbon_cycle_diagram_ipcc_900x543.jpg

Page 2: 4.3 Carbon cycling

The official IB Diploma Biology guideEssential idea: Continued availability of carbon in ecosystems depends on carbon cycling.

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Biogeochemical cycles

Slide from

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Unlike energy, nutrients are constantly recycled within the ecosystems through chemical, biological and geological process

Inorganic reserve Producers

Basic pattern of nutrient cycling

Convert nutrients in organic substances

Chemical and Geological processes

Consumers

Dead organic matter Dead corpses,

excretions, hair, dead skin

Dead plants, leaves or bush and tree trimmings,

Saprotrophs

Decomposition

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Biogeochemical cycles

Slide from

The Earth is essentially a closed system with respect to matter. Thus the availability of matter to organisms is happening through a continuous cycling.

Biogeochemical cycles is the sum of the biological (e.g., cellular respiration in the C cycle), geological (formation of limestone in the C cycle) and chemical processes (formation of hydrogen carbonate ions) related to the cycling of matter on earth

The carbon cyclehttps://upload.wikimedia.org/wikipedia/commons/d/d5/Carbon_cycle.jpg

The nitrogen cyclehttps://upload.wikimedia.org/wikipedia/commons/thumb/f/fe/Nitrogen_Cycle.svg/800px-Nitrogen_Cycle.svg.png

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Carbon input in the ecosystems - FixationAutotrophs convert carbon dioxide into carbohydrates and other carbon compounds – Carbon dioxide diffuses from the atmosphere or water into the autotrophs.

Revision: Outline the process of Carbon fixation and the Calvin cycle in plants.

http://www.cms4schools.com/greenfield/faculty/mvolk/dark%20reactions%20picture.jpg

https://upload.wikimedia.org/wikipedia/commons/thumb/d/d5/Carbon_cycle.jpg/1280px-Carbon_cycle.jpg

Activity: This NASA map demonstrates CO2 concentration in mid-troposphere in 2009. Can you explain this pattern?

http://www.tankonyvtar.hu/en/tartalom/tamop425/0010_1A_Book_angol_01_novenyelettan/images/img40.png

Low CO2 concentration

High CO2 concentration

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Carbon input in the ecosystems – Aquatic ecosystems

http://image.slidesharecdn.com/biok4-150219124749-conversion-gate02/95/bioknowledgy-43-carbon-cycling-11-638.jpg?cb=1424350183

In aquatic habitats carbon dioxide is present as a dissolved gas and hydrogen carbonate ions - Carbon dioxide diffuses from the atmosphere or water into the autotrophs.

http://www.cliparthut.com/clip-arts/234/underwater-clip-art-234466.png

International mindedness

http://www.pmel.noaa.gov/co2/story/Ocean+Acidification

Ocean Acidification: The Other Carbon Dioxide Problem

Hydrogen carbonate ions are absorbed by aquatic plantsDiffuses down the concentration gradient

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Release of CO2 - cell respirationCarbon dioxide is produced by respiration and diffuses out of organisms into water of the atmosphere

Revision: Outline the process of CO2 production during the Krebs cycle

http://www.sivabio.50webs.com/plas036.jpg

Activity: Which arrows represent respiration and why?

Clearing the Air: Livestock’s Contribution to Climate Change

Read more

http://animalscience.ucdavis.edu/faculty/mitloehner/publications/2009%20pitesky%20Clearing%20the%20Air.pdf

http://piedmontib7thscience.weebly.com/uploads/2/4/2/3/24237687/carbon-cycle-diagram-to-label-i1.jpg

Organisms thar contribute in CO2 production via respiration

• Non-photosynthetic cells of plants• Animal cells - consumers, detritivores• Saprotrophs

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Release of CO2 - cell respirationCarbon dioxide is produced by respiration and diffuses out of organisms into water of the atmosphere

Revision: Outline the process of CO2 production during the Krebs cycle

http://www.sivabio.50webs.com/plas036.jpg

Clearing the Air: Livestock’s Contribution to Climate Change

Read more

http://animalscience.ucdavis.edu/faculty/mitloehner/publications/2009%20pitesky%20Clearing%20the%20Air.pdf

http://www.forestry.gov.uk/images/straits_diag02.gif/$FILE/straits_diag02.gif

Graph demonstrating the long term averageNet Ecosystem Productivity) and the average accumulated CO2 removal from the atmosphere at the Alice Holt flux site.

Columns below the zero line (day 0 to 140 & 280 to 365) indicate that the forest is acting as a net source for CO2.

For the summer period (day 141 to 279) columns are above the zero line indicating that forest is acting as a net sink. The solid line indicates the average accumulated carbon balance for the site.

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ANAEROBICCONDITIONS

Methane and MethanogenesisMethane is produced from organic mater in anaerobic conditions by methanogenic archaeans (bacteria) and some diffuses into the atmosphere.

https://dl.sciencesocieties.org/images/publications/sh/53/4/12fig6.jpeg

Bacteria

Alcohol, organic acids, CO2

Bacteria

Acetate, CO2, HArchaea

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Methane and MethanogenesisSome of the most well known methane producing environments.

http://m5.i.pbase.com/o6/52/679252/1/115312855.NCZy9Qhl.IMGP0177pb.jpg

Muddy shores – fine sedimentshttp://www.richkni.co.uk/dartmoor/pix/foxmire/mire5.jpg

Swamps - mires

https://upload.wikimedia.org/wikipedia/commons/thumb/7/70/Wysypisko.jpg/1920px-Wysypisko.jpg

Landfillshttps://upload.wikimedia.org/wikipedia/commons/b/b6/Aune_head_mire3.jpg

Other water-logged areas

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Methane and Methanogenesis: Oxidation of methane

http://www.ux1.eiu.edu/~cfjps/1400/TBL01_0T2.JPG

Methane atmospheric concentration is very low in comparison to the amount released in the atmosphere.

Methane is oxidized to carbon dioxide and water in the atmosphere.

Methane is gradually oxidized in the atmosphere. Hydroxyl (OH-) radicals and monatomic oxygen (0-) play an important role.

http://media-3.web.britannica.com/eb-media/22/6022-004-32EBE121.jpg

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Methane and Methanogenesis: Oxidation of methaneMethane is oxidized to carbon dioxide and water in the atmosphere.

Methane persists in the atmosphere for a period of 12 years.

However, atmospheric data from Mauna Loa, Hawaii, and other monitoring stations indicate a gradual increase of the concentration in the atmosphere.

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Formation of PeatPeat forms when organic matter is not fully decomposed because of anaerobic conditions in waterlogged soils

http://media-3.web.britannica.com/eb-media/22/6022-004-32EBE121.jpg

https://upload.wikimedia.org/wikipedia/commons/5/59/Exposed_peat_-_geograph.org.uk_-_1226373.jpg

Waterlogged anaerobic soil

Saprotrophs may not thrive –lack of O2

Organic matter is not fully digested-anaerobic bacteria develop

pH drops, saprotrophs and methanogens are further inhibited

http://i.telegraph.co.uk/multimedia/archive/01879/peat2_1879196c.jpg

Large quantities of undigested organic matter build up forming the peat.

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Peat plant, Irdyn swampland, https://upload.wikimedia.org/wikipedia/commons/thumb/6/64/Peat_plant_1%2C_2006.5.JPG/489px-Peat_plant_1%2C_2006.5.JPG

Peat forms when organic matter is not fully decomposed because of anaerobic conditions in waterlogged soils

https://upload.wikimedia.org/wikipedia/commons/4/43/Peat-bog-Ireland.jpg

Peat may be used as a fuel and is burned in old-fashioned peat plants

Slide from

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Fossilized organic matterPartially decomposed organic matter from past geological eras was converted into oil and gas in porous rocks or into cola.

http://media-3.web.britannica.com/eb-media/22/6022-004-32EBE121.jpg

https://www.uky.edu/KGS/coal/images/coalform.jpg

Formation of coal from peat

Layers from the Carboniferous Pennsylvanian era (circa 320 million years ago)

http://www.ucmp.berkeley.edu/carboniferous/images/measuringlayers.jpg

Oil and natural gas are formed at the bottom of the sea or lakes due to the anaerobic combustion of organic material and the further deposition of additional material. Increased pressure and various chemical processes lead to the formation of crude oil and gas.

http://www.planetseed.com/laboratory/how-natural-gas-formed

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Combustion Carbon dioxide is produced by the combustion of biomass and fossilized organic matter

Complete Combustion is a reaction in which organic matter is fully oxidized to CO2 and H2O (in the presence of O2)

Fires

Naturally occurring Human induced

http://news.psu.edu/sites/default/files/styles/threshold-992/public/forest_floor_fire.jpg

http://constantine.typepad.com/.a/6a0120a7fc3be9970b017743aa2cbd970d-pi

http://hardenup.org/media/307462/coal_fire_station_pic.jpg

Combustion of fossil fuels

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Combustion Carbon dioxide is produced by the combustion of biomass and fossilized organic matter

International mindedness: The “slash and burn” practise of the Amazon farmers

For decades the Amazonian farmers are using the “slash and burn” practise to increase the agricultural land area against the rainforest. Can you think of the implications of this activity?

Slash & Burn | Part 1: Why Amazonian farmers use fire

See the series of documentaries to consider the implications of the “slash and burn” process

https://s-media-cache-ak0.pinimg.com/originals/4e/b3/fe/4eb3fe4aa603ae17d31e99e70bd54143.jpg

http://static1.squarespace.com/static/542ce587e4b003527579fd2f/547c1e7ee4b00f7531d1a108/547c1e83e4b019f892a8f903/1417420419951/slashandburn.jpgSlide from

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Limestone formationAnimals such as reef-building corals and molluscs have hard parts that are composed of calcium carbonate and can become fossilized in limestone

http://www.sciencelearn.org.nz/var/sciencelearn/storage/images/contexts/a-fizzy-rock/sci-media/images/mollusc-shell-structure/744044-1-eng-NZ/Mollusc-shell-structure.jpg

http://thumbs.dreamstime.com/x/aquatic-mollusk-shells-11137975.jpg

http://thumbs.dreamstime.com/z/coral-anatomy-vector-diagram-structure-polyp-polyps-tend-to-live-colonies-form-building-blocks-reef-36203292.jpg

https://upload.wikimedia.org/wikipedia/commons/2/2e/Coral_Outcrop_Flynn_Reef.jpg

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Limestone formationAnimals such as reef-building corals and molluscs have hard parts that are composed of calcium carbonate and can become fossilized in limestone

http://jgs.lyellcollection.org/content/165/1/395/F2.large.jpg

Hard shells of dead animals are gradually decomposed. The gradual decompostion of the shells and the precipitation of CaCO3 leads to creation of limestone.

https://d1u1p2xjjiahg3.cloudfront.net/5440f0a7-273a-4823-9344-c48d83e3f685.jpg

https://www2.nau.edu/rcb7/CoquinaRpt.jpg

A rocky shore made of limestone in Mexico

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Analysis of data from air monitoring stations to explain annual fluctuations.

Many field stations globally use the same standardised method. All stations show a clear upward trend with annual cycles.

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http://www.esrl.noaa.gov/gmd/dv/iadv/

The Earth System Research Laboratory contains environmental data sets from many stations around the world.

We will use this data to explore trends in CO2 concentration in the atmosphere.

1. Choose one station2. Open the carbon cycle gases

Analysis of data from air monitoring stations to explain annual fluctuations.

Page 23: 4.3 Carbon cycling

http://www.esrl.noaa.gov/gmd/dv/iadv/

3. Choose time series and select a subset of data of your choice.

4. Copy the data in your excel and draw a scatter graph (remember what we have discussed about graphs)

5. Discuss the trends resulting from the analysis of results

Analysis of data from air monitoring stations to explain annual fluctuations.

Page 24: 4.3 Carbon cycling

Analysis of data from air monitoring stations to explain annual fluctuations.

Page 25: 4.3 Carbon cycling

Analysis of data from air monitoring stations to explain annual fluctuations.

Page 26: 4.3 Carbon cycling

Analysis of data from air monitoring stations to explain annual fluctuations.

Page 27: 4.3 Carbon cycling

https://www.ncdc.noaa.gov/cdo/f?p=518:1:0:::APP:PROXYTOSEARCH:7

Analysis of data from air monitoring stations to explain annual fluctuations.

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Construct a diagram of the carbon cycle.

CO2 in the atmosphere and hydrosphere (oceans)

In order to construct a diagram of the carbon cycles we need to consider

Sinks: organic or inorganic reserves of C.

Carbon compounds in producers (autotrophs)

Carbon compounds in consumers

Carbon compounds in dead organic matter

Key:SinkFlux

n.b. some of the fluxes will need to be used more than once.Original slide from

Carbon compounds in fossil fuels

Page 29: 4.3 Carbon cycling

Construct a diagram of the carbon cycle.

In order to construct a diagram of the carbon cycles we need to consider

Fluxes: Transfer of element from one pool to another

Key:SinkFlux

n.b. some of the fluxes will need to be used more than once.

Cell respiration Photosynthesis

Combustion

FeedingEgestion

Death

Incomplete decomposition & fossilisation

Original slide from

Page 30: 4.3 Carbon cycling

Construct a diagram of the carbon cycle.

Start from the Sinks/Pools you know well Key:SinkFlux

CO2 in the atmosphere and hydrosphere (e.g. oceans)

Carbon compounds in producers (autotrophs)

Carbon compounds in consumers

Carbon compounds in dead organic matter

Original slide from

Page 31: 4.3 Carbon cycling

Construct a diagram of the carbon cycle.

Start from the Sinks/Pools you know well Add the fundamental fluxes

Key:SinkFlux

CO2 in the atmosphere and hydrosphere (e.g. oceans)

Carbon compounds in producers (autotrophs)

Carbon compounds in consumers

Carbon compounds in dead organic matter

Phot

osyn

thes

is

Cell

resp

iratio

n

Feed

ing

Feeding

Cell

respiration

Original slide from

Page 32: 4.3 Carbon cycling

Construct a diagram of the carbon cycle.

Start from the Sinks/Pools you know well Add the fundamental fluxes

Key:SinkFlux

CO2 in the atmosphere and hydrosphere (e.g. oceans)

Carbon compounds in producers (autotrophs)

Carbon compounds in consumers

Carbon compounds in dead organic matter

Phot

osyn

thes

is

Cell

resp

iratio

n

Feed

ing

Feeding

Cell

respiration

Death

Cell respiration

Death

Egestion

Feeding

Original slide from

Page 33: 4.3 Carbon cycling

Construct a diagram of the carbon cycle.

Start from the Sinks/Pools you know well Lets discuss fossilisation and man-made intervention

Key:SinkFlux

CO2 in the atmosphere and hydrosphere (e.g. oceans)

Carbon compounds in producers (autotrophs)

Carbon compounds in consumers

Carbon compounds in dead organic matter

Phot

osyn

thes

is

Cell

resp

iratio

n

Feed

ing

Feeding

Cell

respiration

Death

Cell respiration

Death

Egestion

Feeding

Carbon compounds in fossil fuels

Incomplete decomposition &

fossilisation

Combustion

Com

busti

on

Original slide from

Page 34: 4.3 Carbon cycling

Construct a diagram of the carbon cycle.

Start from the Sinks/Pools you know well Lets discuss fossilisation and man-made intervention

Key:SinkFlux

CO2 in the atmosphere and hydrosphere (e.g. oceans)

Carbon compounds in producers (autotrophs)

Carbon compounds in consumers

Carbon compounds in dead organic matter

Phot

osyn

thes

is

Cell

resp

iratio

n

Feed

ing

Feeding

Cell

respiration

Death

Cell respiration

Death

Egestion

Feeding

Carbon compounds in fossil fuels

Incomplete decomposition &

fossilisation

Combustion

Com

busti

on

Original slide from

http://youtu.be/CitOibRcCcI

Page 35: 4.3 Carbon cycling

Construct a diagram of the carbon cycle.

Start from the Sinks/Pools you know well Lets discuss fossilisation and man-made intervention

Key:SinkFlux

CO2 in the atmosphere and hydrosphere (e.g. oceans)

Carbon compounds in producers (autotrophs)

Carbon compounds in consumers

Carbon compounds in dead organic matter

Phot

osyn

thes

is

Cell

resp

iratio

n

Feed

ing

Feeding

Cell

respiration

Death

Cell respiration

Death

Egestion

Feeding

Carbon compounds in fossil fuels

Incomplete decomposition &

fossilisation

Combustion

Com

busti

on

Original slide from

Extend your understanding:Between which sinks would you add a flux showing volcanoes and the weathering of rocks?What additional sink would you add to show the role of corals and shellfish? What additional flux would be needed?In some environments water is unable to drain out of soils so they become waterlogged and anaerobic. This prevents the decomposition of dead organic matter forming peat deposits [4.3.U7]. Peat can be dried and burnt as a fuel. Suggest how peat could be added to the carbon cycle.Explain why fossil fuels are classified as non-renewable resources when the carbon cycle indicates they are renewed (hint: refer to the pictorial carbon cycle).Diffusion is a flux that moves CO2 from the atmosphere to the hydrosphere and back again. Taken together these fluxes are largest in the cycle suggest why.

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www.stepsinbiology.com