The carbon cycle describes the storage and exchange of carbon between the Earth's biosphere (living matter), atmosphere (air), hydrosphere (water), and geosphere (earth).
Need to Study the Carbon Cycle?
Carbon is an element that is essential for life as we know it. Living organisms obtain carbon from their environment. When they die, carbon is returned to the non-living environment. However, the concentration of carbon in living matter (18%) is about 100 times higher than the concentration of carbon in the earth (0.19%). The uptake of carbon into living organisms and return of carbon to the non-living environment are not in balance.
Forms of Carbon in the Carbon Cycle
Carbon exists in several forms as it moves through the carbon cycle.
Carbon in the Non-Living Environment
The non-living environment includes substances that never were alive as well as carbon-bearing materials that remain after organisms die. Carbon is found in the non-living part of the hydrosphere, atmosphere, and geosphere as:
carbonate (CaCO3) rocks: limestone and coral
dead organic matter, such as humus in soil
fossil fuels from dead organic matter (coal, oil, natural gas)
carbon dioxide (CO2) in the air
carbon dioxide dissolved in water to form HCO3?
How Carbon Enters Living Matter
Carbon enters living matter through autotrophs, which are organisms capable of making their own nutrients from inorganic materials.
Photoautotrophs are responsible for most of the conversion of carbon into organic nutrients. Photoautotrophs, primarily plants and algae, use light from the sun, carbon dioxide, and water to make organic carbon compounds (e.g., glucose).
Chemoautotrophs are bacteria and archaea that convert carbon from carbon dioxide into an organic form, but they get the energy for the reaction through oxidation of molecules rather than from sunlight.
How Carbon Is Returned to the Non-Living Environment
Carbon returns to the atmosphere and hydrosphere through:
burning (as elemental carbon and several carbon compounds)
respiration by plants and animals (as carbon dioxide, CO2)
decay (as carbon dioxide if oxygen is present or as methane, CH4, if oxygen is not present)