Respiration patterns in the deep ocean

The biological pump affects atmospheric CO2 levels and fuels most heterotrophic activity in the deep ocean. The efficiency of this pump depends on the rate of carbon fixation, export out of the euphotic zone and the depth of respiration. Here we study the depth dependence of respiration patterns, he...

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Bibliographic Details
Published in:Geophysical research letters Vol. 31; no. 3; pp. L03304 - n/a
Main Authors: Andersson, J. Henrik, Wijsman, Jeroen W. M., Herman, Peter M. J., Middelburg, Jack J., Soetaert, Karline, Heip, Carlo
Format: Journal Article
Language:English
Published: American Geophysical Union 01-02-2004
Blackwell Publishing Ltd
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Summary:The biological pump affects atmospheric CO2 levels and fuels most heterotrophic activity in the deep ocean. The efficiency of this pump depends on the rate of carbon fixation, export out of the euphotic zone and the depth of respiration. Here we study the depth dependence of respiration patterns, hence particulate carbon flux, using a compiled data set of sediment oxygen consumption rates. We show that the depth relationship can best be described by a double exponential model. For the upper part of the ocean, our resulting equation is similar to previous flux‐depth relationships but predicted fluxes are significantly larger in deeper waters. This implies a more efficient biological pump. Total oceanic respiration below the shelf break (200 m) is estimated to be 827 Tmol O2 yr−1.
Bibliography:ArticleID:2003GL018756
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ISSN:0094-8276
1944-8007
DOI:10.1029/2003GL018756