A record of deep-ocean dissolved O2 from the oxidation state of iron in submarine basalts

Daniel A. Stolper () and C. Brenhin Keller
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Daniel A. Stolper: University of California
C. Brenhin Keller: University of California

Nature, 2018, vol. 553, issue 7688, 323-327

Abstract: Deep-ocean O2 concentrations over the past 3.5 billion years are estimated using the oxidation state of iron in submarine basalts and indicate that deep-ocean oxygenation occurred in the Phanerozoic.

Date: 2018
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DOI: 10.1038/nature25009

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