Marine

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Ecosystem
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[edit] Marine ecosystems

Marine ecosystems cover approximately 71% of the Earth's surface and contain approximately 97% of the planet's water. They generate 32% of the world's net primary production [1]. They are distinguished from freshwater ecosystems by the presence of dissolved compounds, especially salts, in the water. Approximately 85% of the dissolved materials in seawater are sodium and chlorine. Seawater has an average salinity of 35 parts per thousand (ppt) of water. Actual salinity varies among different marine ecosystems. [2]

Marine ecosystems can be divided into the following zones: oceanic (the relatively shallow part of the ocean that lies over the continental shelf); profundal (bottom or deep water); benthic (bottom substrates); intertidal (the area between high and low tides); estuaries; salt marshes; coral reefs; and hydrothermal vents (where chemosynthetic sulphur bacteria form the food base). [1]

In the Cenozoic, Classes of organisms found in marine ecosystems include brown algae, dinoflagellates, corals, cephalopods, echinoderms, bony fish, and sharks. [1]

[edit] References

[1] Alexander, David E. (1999-05-01). Encyclopedia of Environmental Science. Springer. ISBN 0412740508.

[2] United States Environmental Protection Agency (2006-03-02). Marine Ecosystems. Retrieved on 2006-08-25.

[edit] Credits

This page incorporates material from Wikipedia which is available under the terms of the GNU Free Documentation License. Wikipedia url for material on this page:
http://en.wikipedia.org/wiki/Aquatic_ecosystem
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