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Life Science Dictionary

Carbon cycle

Ecology · Botany · Marine Biology

Say it: KAR-bun SY-kul

The carbon cycle is the movement of carbon among the air, oceans, living things, soils and rocks through processes like photosynthesis and respiration.

Definition

What is the carbon cycle?

The carbon cycle is the continuous exchange of carbon among Earth's main reservoirs: the atmosphere, where it is mostly carbon dioxide; the oceans, which hold about 50 times more carbon than the air; living organisms and soils; and rocks and sediments, including limestone and fossil fuels, which store by far the largest amount. Carbon forms the backbone of every organic molecule, so its cycling links all life on the planet.

The cycle has a fast biological part and a slow geological part. In the fast part, plants, algae and other autotrophs take in carbon dioxide during photosynthesis and build it into sugars, and producers, consumers and decomposers release it again through cellular respiration and decay. In the slow part, carbon dioxide dissolves in seawater to form bicarbonate, which marine organisms use to build calcium carbonate shells that settle and, over millions of years, become limestone. Buried remains can turn into coal, oil and gas, and volcanoes return carbon to the air.

Since the Industrial Revolution, people have released carbon stored over millions of years by burning fossil fuels, clearing forests and making cement, raising atmospheric carbon dioxide and warming the climate. The ocean absorbs much of the extra gas, which lowers its pH in a process called ocean acidification.

Word parts

Where does the term “carbon cycle” come from?

carbon
coal, charcoalLatin carbo, via French carbone
cycle
circleGreek kyklos

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