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The Carbon Cycle
The carbon cycle is the movement of atoms and molecules containing the element carbon between sources and sinks
Some cycling of carbon happens quickly… other types of cycling take millions of years
The carbon cycle is a biogeochemical cycle, which is a self-regulating, naturally-occuring movement of chemical molecules through various sources and sinks (reservoirs)
These cycles help stabilize and regulate the flow of matter through ecosystems
Biogeochemical Cycles can be disturbed by human activity
Photosynthesis takes in carbon and puts it into the soil
On the other hand, microbial respiration and decomposition releases carbon into the air (soil carbon)
There is also fossil carbon, which is fossil fuel that is released from human emmisions

Fast Carbon Cycling
Fast carbon cycling is largely the movement of carbon compounds through the biosphere — the living organisms on Earth
This type of cycling is driven by the cellular metabolism of producers in ecosystems
The main biological processes involved in fast carbon cycling are photosynthesis and cellular respiration
For fast carbon cycling, the primary carbon reservoir is the atmosphere
The length of time a carbon compound spends in the atmosphere is relatively brief
Other Processes
During the process of decomposition of organic material, decomposer organisms help
Return of CO2 to the atmosphere through cellular respiration
Return of carbon to soil or water through breakdown of sugars in the bodies they are decomposing
Sedimentation and burial: Organic material can result in a much longer sequestration of carbon compounds. Once the carbon is buried, it is essentially removed from the fast carbon cycle
Remember, the deep ocean sediments and fossil carbon (coal, oil, natural gas) are the largest reservoirs of carbon … and those are the result of sedimentation and burial
Long-term carbon reservoirs can return to cycling via…
Fossil fuel extraction and combustion (quick return to cycling)
Uplift and weathering of limestone (slow return to cycling)
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