Evolution of the global phosphorus cycle

Christopher T. Reinhard (), Noah J. Planavsky (), Benjamin C. Gill, Kazumi Ozaki, Leslie J. Robbins, Timothy W. Lyons, Woodward W. Fischer, Chunjiang Wang, Devon B. Cole and Kurt O. Konhauser
Additional contact information
Christopher T. Reinhard: School of Earth and Atmospheric Sciences, Georgia Institute of Technology
Noah J. Planavsky: Yale University
Benjamin C. Gill: Virginia Tech
Kazumi Ozaki: School of Earth and Atmospheric Sciences, Georgia Institute of Technology
Leslie J. Robbins: University of Alberta, Edmonton
Timothy W. Lyons: University of California
Woodward W. Fischer: California Institute of Technology
Chunjiang Wang: State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum
Devon B. Cole: Yale University
Kurt O. Konhauser: University of Alberta, Edmonton

Nature, 2017, vol. 541, issue 7637, 386-389

Abstract: Low phosphorus burial in shallow marine sedimentary rocks before about 750 million years ago implies a change in the global phosphorus cycle, coinciding with the end of what may have been a stable low-oxygen world.

Date: 2017
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DOI: 10.1038/nature20772

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