Ocean chemistry and deep-sea sediments
Ocean chemistry and deep-sea sediments
Ocean chemistry and deep-sea sediments
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• In the photic zone thephytoplankton is grazedby the zooplankton.• The dead particles aremainly decomposed by,for example bacteria.• The organic matter isrecycled to the photiczone.• The organic matterconsists of oxygen,hydrogen, carbon,nitrogen, phosphorus.• Some particles sinkthrough the water column<strong>and</strong> reach the <strong>sea</strong>bed.