Carbon Cycle
Carbon stores
what is it ?
Geological carbon cycle
Importance of phytoplankton
- A biochemical cycle in which carbon is stored and moved between different stores through fluxes
- If the carbon source is also the sink the cycle is in equilibrium
- Water
- Rocks
- Organisms
- Lithosphere
- Oceanic
- Biomass
- Atmospheric
- Geological processes control the geological carbon cycle through processes such as volcanic outgassing and chemical weathering (carbonic acid)
- Has a slow reservoir turnover rate of at least 100,000 years
- Carbon sequestration is the process in which carbon is captured and stored long term
- Carbon is stored in sedimentary rocks such as limestone
- Sequesters atmospheric carbon during photosynthesis on the surface of the ocean as part of the biological pump
- Changes in phytoplankton can impact biodiversity, global warming and fisheries
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Oceanic stores
- Warm water releases C02
- Cold water stores C02
- In areas where deep currents meet suface currents, the C02 sources flux is greater
Biological pump
- Driven by organisms that live in the ocean
- Involves processes such as photosynthesis
- Moves carbon down to the sea floor
Carbonate pump
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