The carbon cycle describes the continuous biogeochemical movement of carbon between the atmosphere, biosphere, geosphere, and hydrosphere. Carbon dioxide is sequestered from the atmosphere by producers via photosynthesis to synthesize complex organic molecules such as glucose, starch, and proteins. This carbon is returned to the atmosphere through aerobic respiration in plants, animals, and decomposers, and via the combustion of fossil fuels. The cycle relies heavily on microorganisms (bacteria and fungi) for decomposition, ensuring that essential materials are recycled to support new life.
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