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Atmospheric oxygenation three billion years ago

Sean A. Crowe (), Lasse N. Døssing, Nicolas J. Beukes, Michael Bau, Stephanus J. Kruger, Robert Frei and Donald E. Canfield
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Sean A. Crowe: Institute of Biology, and Nordic Center for Earth Evolution, University of Southern Denmark, Odense 5230, Denmark
Lasse N. Døssing: Institute of Biology, and Nordic Center for Earth Evolution, University of Southern Denmark, Odense 5230, Denmark
Nicolas J. Beukes: University of Johannesburg, Johannesburg 2006, South Africa
Michael Bau: Earth and Space Sciences Program, Jacobs University Bremen, Bremen 28759, Germany
Stephanus J. Kruger: University of Johannesburg, Johannesburg 2006, South Africa
Robert Frei: and Nordic Center for Earth Evolution, University of Copenhagen, Copenhagen 1350, Denmark
Donald E. Canfield: Institute of Biology, and Nordic Center for Earth Evolution, University of Southern Denmark, Odense 5230, Denmark

Nature, 2013, vol. 501, issue 7468, 535-538

Abstract: The distribution of chromium isotopes and redox-sensitive metals in the Nsuze palaeosol and in the Ijzermyn iron formation from the Pongola Supergroup, in South Africa, suggests that there were appreciable levels of atmospheric oxygen about three billion years ago, some 300–400 million years earlier than previous indications for Earth surface oxygenation.

Date: 2013
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DOI: 10.1038/nature12426

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