The biological carbon pump revisited: feedback mechanisms between climate and the redfield ratio.

A.W. Omta, J. Bruggeman, S.A.L.M. Kooijman, H.A. Dijkstra

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Abstract

Biological activity gives rise to a difference in carbon concentration between the ocean surface and the deep waters. This difference is determined by the carbon:nutrient ratio of the sinking organic material and it is crucial in determining the distribution of CO
Original languageEnglish
Article numberL14613
Number of pages4
JournalGeophysical Research Letters
Volume33
DOIs
Publication statusPublished - 2006

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