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  1. Article

    Open Access

    Mantle data imply a decline of oxidizable volcanic gases could have triggered the Great Oxidation

    Aerobic lifeforms, including humans, thrive because of abundant atmospheric O2, but for much of Earth history O2 levels were low. Even after evidence for oxygenic photosynthesis appeared, the atmosphere remained ...

    Shintaro Kadoya, David C. Catling, Robert W. Nicklas in Nature Communications (2020)