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Sources of Organic Matter to the Deep-Sea Benthos
Gilbert T. Rowe and Nick Staresinic
Ambio Special Report
No. 6, The Deep Sea: Ecology and Exploitation (1979), pp. 19-23
Published by: Springer
Stable URL: http://www.jstor.org/stable/25099603
Page Count: 5
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Particulate organic matter (POM) in the deep sea is derived from five major sources: planktonic material, carcasses of large nekton, marine macrophyte detritus, terrigenous matter and chemoautotrophic production. The direct contribution of terrigenous matter to deep marine sediments is small. Sediment trap measurements show that small planktonic POM adds about 4 g C m⁻²yr⁻¹ to the deep-sea carbon pool. The maximum expected input of pelagic Sargassum to the deep Atlantic is one-tenth of this, 0.4 g C m⁻²yr⁻¹. Calculations suggest the remains of large nekton contribute approximately 50 mg C m⁻²yr⁻¹ while the rate of primary carbon synthesis by chemoautotrophs is estimated to be 0.01 to 0.1 mg C m⁻²yr⁻¹.
Ambio Special Report © 1979 Royal Swedish Academy of Sciences