Ocean chemistry and deep-sea sediments
Ocean chemistry and deep-sea sediments
Ocean chemistry and deep-sea sediments
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Summary:• Organic matter produced by primary productionin surface waters is a major regulator of <strong>sea</strong>watercomposition of minor <strong>and</strong> major constituents.• Major constituents - the nutrients are phophate,nitrate <strong>and</strong> silica.• They are depleted in surface waters <strong>and</strong>enriched in intermediate <strong>and</strong> <strong>deep</strong> waters.• Maximum oxygen depletion occurs inintermediate waters due to decomposition oforganic material at about 1 km water depth.• Oxygen is brought to the <strong>deep</strong> ocean bydownwelling (convergence) in polar regions.