Article on Carbon cycle about 400 words
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Answer:
In fact, it usually takes millions of years for carbon to cycle through the geological pathway. Carbon may be stored for long periods of time in the atmosphere, bodies of liquid water—mostly oceans— ocean sediment, soil, rocks, fossil fuels, and Earth's interior.
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Answer:
The carbon cycle is most easily studied as two interconnected subcycles:
One dealing with rapid carbon exchange among living organisms
One dealing with long-term cycling of carbon through geologic processes
Although we will look at them separately, it's important to realize these cycles are linked. For instance, the same pools of atmospheric and oceanic \text{CO}_2CO
2
C, O, start subscript, 2, end subscript that are utilized by organisms are also fed and depleted by geological processes.
As a brief overview, carbon exists in the air largely as carbon dioxide—\text{CO}_2CO
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C, O, start subscript, 2, end subscript—gas, which dissolves in water and reacts with water molecules to produce bicarbonate—\text{HCO}_3^-HCO
3
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H, C, O, start subscript, 3, end subscript, start superscript, minus, end superscript. Photosynthesis by land plants, bacteria, and algae converts carbon dioxide or bicarbonate into organic molecules. Organic molecules made by photosynthesizers are passed through food chains, and cellular respiration converts the organic carbon back into carbon dioxide gas.
Longterm storage of organic carbon occurs when matter from living organisms is buried deep underground or sinks to the bottom of the ocean and forms sedimentary rock. Volcanic activity and, more recently, human burning of fossil fuels bring this stored carbon back into the carbon cycle. Although the formation of fossil fuels happens on a slow, geologic timescale, human release of the carbon they contain—as \text{CO}_2CO
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C, O, start subscript, 2, end subscript—is on a very fast timescale.