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Stepwise oxygenation of the Paleozoic atmosphere

By Alexander J. Krause, Benjamin J. W. Mills, Shuang Zhang, Noah J. Planavsky, Timothy M. Lenton and Simon W. Poulton

Abstract

The GEOCARBSULF model provides the most detailed reconstructions of Phanerozoic O2, but its predictions are not supported by geochemical data. Here, a GEOCARBSULF model rebuilt from first principles, with the addition of an amended sulphur cycle and the latest isotope records, supports a Paleozoic Oxygenation Event

Topics: Science, Q
Publisher: Nature Publishing Group
Year: 2018
DOI identifier: 10.1038/s41467-018-06383-y
OAI identifier: oai:doaj.org/article:b79392405e8e4f27b4bdc7f6c38c0679
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