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The Epipelagic The pelagic realm of the ocean describes the vast, open ocean. –The epipelagic realm is the upper part of this environment. Depths only to about 200m Corresponds to the depth of the euphotic zone –Euphotic depth the depth below which where there is no longer enough light for organisms to grow. –Divided into coastal, or neritic waters that lie over the continental shelf, and oceanic waters.
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Net Tows
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Plankton by Size Plankton: organisms that can’t swim against a current – Picoplankton (0.2 – 2 m) and Nanoplankton (2 – 20 m) »Mostly bacteria and very small single celled algae –Netplankton (>20 m) »Includes the larger phytoplankton and all of the zooplankton
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Plankton by Size
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Phytoplankton –Responsible for >95% of the photosynthesis in the oceans and over ½ the primary production on earth Most important members are diatoms and dinoflagellates. Cyanobacteria are also important phytoplankton because they are able to fix nitrogen, ie. turn inorganic nitrogen into organic nitrogen that can be used by phytoplankton.
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Figure 15.03
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Epipelagic Food Web
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Copepod
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Figure 15.07b
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Larvacean
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Pteropod
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Figure 15.11b
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Figure 15.11c
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Figure 15.11d
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Figure 15.11e
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Fish Larva
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Chaetognath (Arrow Worm)
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Comb Jelly
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Polychaete Worm
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Copepod
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Figure 15.13b
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Crab Zoea
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Fish Larva
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Figure 15.13e
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Snail and a Jelly
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Nekton
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Diel Vertical Migration
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Neuston
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Nekton
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Staying Afloat
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Camouflage
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Epipelagic Food Web
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Global Productivity
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Figure 15.25b
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Figure 15.26
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Seasonal Productivity-Tropics
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Seasonal Productivity- Temperate
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Seasonal Productivity- Polar
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Wind-Driven Upwelling
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Global Upwelling
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Figure 15.32
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