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Research Article| May 01, 2009 Reconstructing Earth's surface oxidation across the Archean-Proterozoic transition Qingjun Guo; Qingjun Guo 11State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China 22Geologisch-Paläontologisches Institut der Westfälischen Wilhelms-Universität Münster, Corrensstraße 24, 48149 Münster, Germany *E-mail: guoqingjun@vip.skleg.cn. Search for other works by this author on: GSW Google Scholar Harald Strauss; Harald Strauss 22Geologisch-Paläontologisches Institut der Westfälischen Wilhelms-Universität Münster, Corrensstraße 24, 48149 Münster, Germany Search for other works by this author on: GSW Google Scholar Alan J. Kaufman; Alan J. Kaufman 22Geologisch-Paläontologisches Institut der Westfälischen Wilhelms-Universität Münster, Corrensstraße 24, 48149 Münster, Germany 33Department of Geology and Earth System Science Interdisciplinary Center, University of Maryland, College Park, Maryland 20742, USA Search for other works by this author on: GSW Google Scholar Stefan Schröder; Stefan Schröder 44Paleoproterozoic Mineralization Research Group, Department of Geology, University of Johannesburg, Auckland Park, 2006 Johannesburg, South Africa 55Total E Jens Gutzmer 44Paleoproterozoic Mineralization Research Group, Department of Geology, University of Johannesburg, Auckland Park, 2006 Johannesburg, South Africa 66Institut für Mineralogie, TU Bergakademie Freiberg, 09596 Freiberg, Germany Search for other works by this author on: GSW Google Scholar Boswell Wing; Boswell Wing 77Department of Earth and Planetary Sciences and GEOTOP UQAM-McGill, McGill University, Montreal, Quebec H3A 2A7, Canada Search for other works by this author on: GSW Google Scholar Margaret A. Baker; Margaret A. Baker 88Department of Geology, University of Maryland, College Park, Maryland 20742, USA Search for other works by this author on: GSW Google Scholar Andrey Bekker; Andrey Bekker 99Department of Geological Sciences, University of Manitoba, Winnipeg, MB R3T 2N2, Canada Search for other works by this author on: GSW Google Scholar Qusheng Jin; Qusheng Jin 1010Department of Geological Sciences, University of Oregon, Eugene, Oregon 97403, USA Search for other works by this author on: GSW Google Scholar Sang-Tae Kim; Sang-Tae Kim 88Department of Geology, University of Maryland, College Park, Maryland 20742, USA Search for other works by this author on: GSW Google Scholar James Farquhar James Farquhar 33Department of Geology and Earth System Science Interdisciplinary Center, University of Maryland, College Park, Maryland 20742, USA Search for other works by this author on: GSW Google Scholar Author and Article Information Qingjun Guo 11State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China 22Geologisch-Paläontologisches Institut der Westfälischen Wilhelms-Universität Münster, Corrensstraße 24, 48149 Münster, Germany Harald Strauss 22Geologisch-Paläontologisches Institut der Westfälischen Wilhelms-Universität Münster, Corrensstraße 24, 48149 Münster, Germany Alan J. Kaufman 22Geologisch-Paläontologisches Institut der Westfälischen Wilhelms-Universität Münster, Corrensstraße 24, 48149 Münster, Germany 33Department of Geology and Earth System Science Interdisciplinary Center, University of Maryland, College Park, Maryland 20742, USA Stefan Schröder 44Paleoproterozoic Mineralization Research Group, Department of Geology, University of Johannesburg, Auckland Park, 2006 Johannesburg, South Africa 55Total E Reconstructing Earth's surface oxidation across the Archean-Proterozoic transition. Geology 2009;; 37 (5): 399–402. doi: https://doi.org/10.1130/G25423A.1 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract The Archean-Proterozoic transition is characterized by the widespread deposition of organic-rich shale, sedimentary iron formation, glacial diamictite, and marine carbonates recording profound carbon isotope anomalies, but notably lacks bedded evaporites. All deposits reflect environmental changes in oceanic and atmospheric redox states, in part associated with Earth's earliest ice ages. Time-series data for multiple sulfur isotopes from carbonate-associated sulfate as well as sulfides in sediments of the Transvaal Supergroup, South Africa, capture the concomitant buildup of sulfate in the ocean and the loss of atmospheric mass-independent sulfur isotope fractionation. In phase with sulfur is the earliest recorded positive carbon isotope anomaly, convincingly linking these environmental perturbations to the Great Oxidation Event (ca. 2.3 Ga). You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
Guo et al. (Fri,) studied this question.
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