The Continuing Puzzle of the Great Oxidation Event

The rise of atmospheric O[subscript 2] was a milestone in the history of life. Although O[subscript 2] itself is not a climate-active gas, its appearance would have removed a methane greenhouse present on the early Earth and potentially led to dramatic cooling. Moreover, by fundamentally altering th...

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Bibliographic Details
Main Authors: Sessions, Alex L. (Author), Doughty, David M. (Contributor), Welander, Paula V. (Contributor), Summons, Roger E. (Author), Newman, Dianne K (Author)
Other Authors: Massachusetts Institute of Technology. Department of Biology (Contributor), Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences (Contributor), Newman, Dianne K. (Contributor)
Format: Article
Language:English
Published: Elsevier, 2015-03-25T17:46:35Z.
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Summary:The rise of atmospheric O[subscript 2] was a milestone in the history of life. Although O[subscript 2] itself is not a climate-active gas, its appearance would have removed a methane greenhouse present on the early Earth and potentially led to dramatic cooling. Moreover, by fundamentally altering the biogeochemical cycles of C, N, S and Fe, its rise first in the atmosphere and later in the oceans would also have had important indirect effects on Earth's climate. Here, we summarize major lines of evidence from the geological literature that pertain to when and how O[subscript 2] first appeared in significant amounts in the atmosphere. On the early Earth, atmospheric O[subscript 2] would initially have been very low, probably <10−5 of the present atmospheric level. Around 2.45 billion years ago, atmospheric O[subscript 2] rose suddenly in what is now termed the Great Oxidation Event. While the rise of oxygen has been the subject of considerable attention by Earth scientists, several important aspects of this problem remain unresolved. Our goal in this review is to provide a short summary of the current state of the field, and make the case that future progress towards solving the riddle of oxygen will benefit greatly from the involvement of molecular biologists.
Howard Hughes Medical Institute
National Science Foundation (U.S.)
United States. National Aeronautics and Space Administration (Astrobiology Program)
United States. National Aeronautics and Space Administration (Exobiology Program)