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sedimentation

bicarbonate (HCO

3

-

)

decay

respiration

Soils

dead

organisms

and animal

waste

coal

natural gas

oil

CO

2

in Atmosphere

di usion

Ocean

Land plants

combustion

photosynthesis

destruction of vegetation

Photo by Dave Carr/Flickr RF/Getty Images

Figure 19 

The diagram shows how carbon

and oxygen cycle through the environment.

Describe

how carbon moves from the abiotic

to the biotic parts of the ecosystem.

The carbon and oxygen cycles

Carbon and oxygen often combine to form

molecules essential for life, including carbon

dioxide and simple sugars. The cycles of these

two elements are shown in

Figure 19

.

Photosynthesis and cellular respiration are

important components of the carbon cycle, in

which carbon is exchanged among the bio-

sphere, atmosphere, oceans, and geosphere

through chemical, physical, and biological

processes. During photosynthesis, plants and

algae convert carbon dioxide and water into

carbohydrates and release oxygen back into the

air. Living organisms consume oxygen and

release carbon dioxide during cellular respira-

tion. Carbon dioxide also enters the atmo-

sphere as dead organisms decay, and carbon

enters the soil through the decomposition of

plant and animal matter and animal waste.

Carbon enters a long-term cycle when organic

matter is buried underground and converted to

fossil fuels such as coal, oil, or gas. Carbon

dioxide returns to the atmosphere those fossil

fuels combust (burn).

Carbon and oxygen enter long-term cycles

when they combine with calcium to create

calcium carbonate. When the shells of some sea

creatures fall to the ocean floor, they form vast

deposits of calcium carbonate in limestone

rock, such as those found in the white cliffs

pictured in

Figure 20

. Carbon and oxygen

remain in these deposits until weathering and

erosion release them from the rocks.

Figure 20 

The white cliffs in Dover, England, are com-

posed almost entirely of calcium carbonate, or chalk. The

carbon and oxygen found in these cliffs are in the long-

term part of the cycle for carbon and oxygen.

Lesson 3 • Cycling of Matter 

41