Mercury abundance and isotopic composition indicate subaerial volcanism prior to the end-Archean "whiff" of oxygen.

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第一作者： Jana,Meixnerová

第一单位： Department of Earth and Space Sciences, University of Washington, Seattle, WA 98195-1310.;Astrobiology Program, University of Washington, Seattle, WA 98195-1310.

作者： Jana,Meixnerová ^[1] ; Joel D,Blum ^[2] ; Marcus W,Johnson ^[3] ; Eva E,Stüeken ^[4] ; Michael A,Kipp ^[5] ; Ariel D,Anbar ^[6] ; Roger,Buick ^[1]

作者单位： Department of Earth and Space Sciences, University of Washington, Seattle, WA 98195-1310.;Astrobiology Program, University of Washington, Seattle, WA 98195-1310. ^[1] Department of Earth and Environmental Sciences, University of Michigan, Ann Arbor, MI 48109; jdblum@umich.edu ees4@st-andrews.ac.uk. ^[2] Department of Earth and Environmental Sciences, University of Michigan, Ann Arbor, MI 48109. ^[3] School of Earth and Environmental Sciences, University of St. Andrews, St. Andrews, Scotland KY16 9AL, United Kingdom; jdblum@umich.edu ees4@st-andrews.ac.uk. ^[4] Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125. ^[5] School of Earth and Space Exploration and School of Molecular Sciences, Arizona State University, Tempe, AZ 85287. ^[6]

关键词 Archean atmospheric oxygenation mercury isotopes

DOI 10.1073/pnas.2107511118

PMID 34373333

发布时间 2022-02-10

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