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

Author

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  • Daniel A. Stolper

    (University of California)

  • C. Brenhin Keller

    (University of California
    Berkeley Geochronology Center)

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.

Suggested Citation

  • Daniel A. Stolper & C. Brenhin Keller, 2018. "A record of deep-ocean dissolved O2 from the oxidation state of iron in submarine basalts," Nature, Nature, vol. 553(7688), pages 323-327, January.
    • Handle: RePEc:nat:nature:v:553:y:2018:i:7688:d:10.1038_nature25009
    DOI: 10.1038/nature25009
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    Cited by:

    1. Mojtaba Fakhraee & Noah Planavsky, 2024. "Insights from a dynamical system approach into the history of atmospheric oxygenation," Nature Communications, Nature, vol. 15(1), pages 1-10, December.

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