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In the carbon cycle, carbon atoms travel throughout the ecosystem.
Starting with photosynthesis, autotrophs, such as plants, transform carbon from the atmosphere in the form of carbon dioxide into consumable energy that is ingested by heterotrophs. These organisms can then return the carbon into the atmosphere through respiration or into the soil during decomposition.
Carbon dioxide in the atmosphere is also highly soluble in water so the oceans constitute a major reservoir of carbon.
Carbon dioxide reacts with water to form carbonic acid and then carbonate ions. Calcium carbonate in ocean water is used to build coral skeletons and mollusc shells. Carbon can also be stored for short terms in the bodies of long-lived trees and in the soil or, for a much longer time in the case of fossil fuels, the organic remains of once living organisms.
Finally, carbon stored in sediments and soils of the earth's crust can be melted into magma and vented into the atmosphere during volcanic eruptions, a process called degassing.
Carbon is the basis of all organic matter on Earth, and is recycled through the ecosystem in two primary processes: one in which carbon is exchanged a…
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