Plankton cooled a greenhouse

Birger Schmitz ()
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Birger Schmitz: Department of Earth Sciences University of Göteborg

Nature, 2000, vol. 407, issue 6801, 143-144

Abstract: At the Palaeocene/Eocene boundary, 55 million years ago, temperatures and atmospheric concentrations of CO2were especially high. New data, which track the response of the oceans' biosphere, point to a plausible mechanism by which such an episode of greenhouse warming may end.

Date: 2000
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DOI: 10.1038/35025173

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