Primary production

Global oceanic and terrestrial photoautotroph abundance, from September 1997 to August 2000. As an estimate of autotroph biomass, it is only a rough indicator of primary-production potential. From the SeaWiFS Project, NASA/Goddard Space Flight Center and ORBIMAGE.

Primary production is the synthesis of organic compounds from carbon dioxide. It occurs by photosynthesis. Light is its source of energy. It also occurs through chemosynthesis, which uses the oxidation or reduction of inorganic chemical compounds as its source of energy.

Almost all life on Earth relies directly or indirectly on primary production. The organisms responsible for primary production are known as primary producers or autotrophs. They form the base of the food chain. On land, these are mainly plants; in the sea (or lakes) algae do this role. Also, there are shallow water oxygen primary producers like sea grass.

By photosynthesis or chemosynthesis, energy is used to make complex organic molecules from simpler inorganic compounds (such as carbon dioxide (CO₂) and water (H₂O). The following are simplified equations of photosynthesis (top) and (one form of) chemosynthesis (bottom):

CO₂ + H₂O + light → CH₂O + O₂

CO₂ + O₂ + 4 H₂S → CH₂O + 4 S + 3 H₂O

Primary Production Media

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  Overview of the Calvin cycle pathway. Original work by Mike Jones en:User:Adenosine*Also see C4 Carbon Fixation here.*This image was copied from wikipedia:en. The original description was:*Modified version of

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  Marine diatoms; an example of planktonic microalgae

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  Differences in relative photosynthesis between plankton species under different irradiance

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  A kelp forest; an example of attached macroalgae

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  An oak tree; a typical modern, terrestrial autotroph

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  The Konza tallgrass prairie in the Flint Hills of northeastern Kansas