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

doi:10.1029/2006GL026213

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 language	English
Article number	L14613
Number of pages	4
Journal	Geophysical Research Letters
Volume	33
DOIs	https://doi.org/10.1029/2006GL026213
Publication status	Published - 2006

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

Abstract

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