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Plankton refer to marine organisms that cannot swim against the current. They are generally free-floating, and many have physical structures that help them either move up and down the water column or remain buoyant (i.e. suspended) near the surface. Plankton can be microscopic, like diatoms and radiolarians, or stretch up to 130 ft in length, like some colonial siphonophores. In this investigation, it is the microscopic plankton that is of importance. Microscopic plankton are the base of the food webs in the marine environment. Therefore, their presence and availability influences the abundance of countless other marine organisms. |
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Plankton that can carry out photosynthesis to produce their own food are known as phytoplankton. These are the "plants" in the ocean. They produce most of the oxygen in the air that we breathe, and form the base of almost all food chains in the ocean. Their abundance is influenced by the availability of nitrogen and phosphorous. |
Almost all organisms in the ocean start out their life as a microscopic zooplankton. These are the egg and larval stages of their lives. Some zooplankton eventually grow into a large adult stage, like anchovies, blue crabs, corals, sea urchins, etc. Other animals remain small their entire life, such as copepods and krill. | |||||||
(www.chesapeakebay.net/info/plankton.cfm) |
(www.cnas.smsu.edu/zooplankton/epischura.htm) |
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The high availability of nitrogen and phosphorous along Peru's coast makes it a rich environment to support an abundance of anchovies.
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This web site was created by Lynn Tran at the North Carolina State University, Department of Mathematics, Science, and Technology Education on 7/12/03. Faculty advisor Dr. David Eggleston, NCSU, Department of Marine, Earth, & Atmospheric Sciences. Last updated December 29, 2003 . |