ROCKS β limestone (CaCOβ) formed from shells of ancient marine organisms.
Processes in the Carbon Cycle
REMOVING COβ FROM THE ATMOSPHERE:
PHOTOSYNTHESIS β plants and algae absorb COβ and convert it to glucose. Carbon is incorporated into the plant's biomass.
DISSOLUTION IN OCEANS β COβ dissolves in seawater to form carbonic acid. Marine organisms use dissolved carbon to make calcium carbonate (CaCOβ) shells.
RETURNING COβ TO THE ATMOSPHERE:
RESPIRATION β ALL living organisms (plants, animals, fungi, bacteria) respire, releasing COβ as glucose is broken down.
DECOMPOSITION β microorganisms (bacteria and fungi) break down dead organic matter, releasing COβ and returning carbon to the atmosphere and soil.
COMBUSTION β burning of organic material (wood, coal, oil, gas) releases COβ rapidly into the atmosphere.
FOSSILISATION β over millions of years, the remains of organisms become compressed into fossil fuels (coal from ancient forests, oil and gas from marine organisms).
Burning fossil fuels releases this long-term stored carbon rapidly β adding COβ to the atmosphere FASTER than natural processes can remove it β CLIMATE CHANGE.
Human Impact on the Carbon Cycle
Human activities are disrupting the carbon cycle by adding COβ to the atmosphere faster than it can be removed.
BURNING FOSSIL FUELS β coal, oil and natural gas burn to release COβ that has been stored underground for millions of years.
DEFORESTATION:
Felling trees removes photosynthesising plants β less COβ absorbed.
Burning or rotting felled trees releases COβ.
Double negative impact on atmospheric COβ.
CEMENT PRODUCTION β manufacturing cement releases COβ from limestone (CaCOβ β CaO + COβ).
RICE PADDY AGRICULTURE and LIVESTOCK β produce methane (CHβ), another greenhouse gas.
CONSEQUENCES OF RISING COβ:
Enhanced greenhouse effect β global warming β climate change.
Ocean acidification β more COβ dissolves β more carbonic acid β threatens marine ecosystems (especially coral reefs and shell-forming organisms).
β οΈ Common Mistake
PLANTS also respire β they release COβ just like animals. The difference is that during the DAY, photosynthesis removes MORE COβ than respiration releases β so there is net COβ uptake. At night, only respiration occurs. Students often say 'plants absorb COβ, they don't release it' β this is wrong.
π Key Note
COβ removed by: photosynthesis, dissolution in oceans. COβ returned by: respiration (all organisms), decomposition, combustion, volcanic activity. Fossil fuels = long-term carbon store. Burning them releases ancient carbon rapidly β climate change.
Sort each process into removing COβ from or returning COβ to the atmosphere. β drag the symbols on the right to match the component names on the left.
Removes COβ
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Returns COβ
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Returns COβ
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Removes COβ
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Returns COβ
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Returns COβ
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Decomposition β bacteria and fungi release COβ from dead organic matter
Photosynthesis β plants convert COβ into glucose using light energy
Dissolution in oceans β COβ absorbed into seawater
Volcanic activity β releases COβ from underground carbon stores
Combustion β burning wood or fossil fuels releases COβ
Respiration β all living organisms release COβ as they break down glucose
π― Test Yourself
Question 1 of 2
1. Why does burning fossil fuels increase atmospheric COβ more than burning wood?
2. How does deforestation affect atmospheric COβ levels?
β How Well Do You Understand This Topic?
Be honest with yourself β this helps you know what to revise!
Don't get itGetting thereNailed it!
π€ Ask Mr Badmus AI
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