Productivity of the Glacial Ocean: Discussion of the Iron Hypothesis

An increase in the productivity of the glacial-age Southern Ocean has been postulated to explain the decrease in $pCO_2$ of the atmosphere observed in ice cores. A plausible mechanism has been proposed elsewhere that productivity is limited by the availability of Fe in this region and that the great...

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Veröffentlicht in:Limnology and oceanography 1991-12, Vol.36 (8), p.1899-1918
Hauptverfasser: Berger, W. H., Wefer, G.
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Sprache:eng
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