Reconstructing Earth's surface oxidation across the Archean-Proterozoic transition
Abstract
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&P, Ave Larribau, F-64018 Pau, France Search for other works by this author on: GSW Google Scholar Jens Gutzmer; 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&P, Ave Larribau, F-64018 Pau, France 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 Boswell Wing 77Department of Earth and Planetary Sciences and GEOTOP UQAM-McGill, McGill University, Montreal, Quebec H3A 2A7, Canada Margaret A. Baker 88Department of Geology, University of Maryland, College Park, Maryland 20742, USA Andrey Bekker 99Department of Geological Sciences, University of Manitoba, Winnipeg, MB R3T 2N2, Canada Qusheng Jin 1010Department of Geological Sciences, University of Oregon, Eugene, Oregon 97403, USA Sang-Tae Kim 88Department of Geology, University of Maryland, College Park, Maryland 20742, USA James Farquhar 33Department of Geology and Earth System Science Interdisciplinary Center, University of Maryland, College Park, Maryland 20742, USA *E-mail: guoqingjun@vip.skleg.cn. Publisher: Geological Society of America Received: 27 Aug 2008 Revision Received: 03 Dec 2008 Accepted: 09 Dec 2008 First Online: 02 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 © 2009 Geological Society of America Geology (2009) 37 (5): 399–402. https://doi.org/10.1130/G25423A.1 Artic
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The Great Oxygenation Event at 2.45-2.22 Ga marks the rapid appearance of free oxygen in Earth's atmosphere.
“The Great Oxygenation Event (GOE) at 2.45-2.22Ga (Bekker et al., 2004;Guo et al., 2009;Gumsley et al., 2017) marks the rapid appearance of free oxygen in the Earth's atmosphere (Anbar et al., 2007;Sessions et al., 2009)”
From Secular change and the onset of plate tectonics on Earth (2020) · cites this paper as Guo et al., 2009
This expected sulfate level is not consistent with models that suggest extremely low seawater sulfate levels before the GOE, possibly as low as 2.5 μM.
“This is not consistent with models that suggest extremely low seawater sulfate levels before the GOE, possibly as low as 2.5 μM (34, 62).”
From Rapid oxygenation of Earth’s atmosphere 2.33 billion years ago (2016) · cites this paper as [34]
An increase in the marine sulfate reservoir at about 2.3 Ga is supported by the large sulfur isotope separation between CAS and pyrite recorded in the topmost Duitschland Formation and the recent finding of gypsum in sabkha-facies evaporites at ~2.31 Ga.
“An increase in the marine sulfate reservoir at about 2.3 Ga is also supported by the large sulfur isotope separation between CAS and pyrite (attributed to microbial sulfate reduction) recorded in the topmost Duitschland Formation (34), as well as the recent finding of gypsum in sabkha-facies evaporites at ~2.31 Ga (41).”
From Rapid oxygenation of Earth’s atmosphere 2.33 billion years ago (2016) · cites this paper as [34]
A much higher sink of seawater sulfate is required to maintain the very low sulfate levels previously suggested.
“Therefore, a much higher sink of seawater sulfate is required to maintain the very low sulfate levels previously suggested (8, 34, 60).”
From Rapid oxygenation of Earth’s atmosphere 2.33 billion years ago (2016) · cites this paper as [34]
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- Authors
- Guo, Q., Strauss, H., Kaufman, A. J., Schröder, S., Gutzmer, J., Wing, B., Baker, M. A., Bekker, A., Jin, Q., Kim, S.-T., & Farquhar, J.
- Affiliations
- Chinese Academy of Sciences (CN)
- University of Münster (DE)
- Total (France) (FR)
- University of Johannesburg (ZA)
- Geotop (CA)
- University of Maryland, College Park (US)
- University of Manitoba (CA)
- University of Oregon (US)
- Earth System Science Interdisciplinary Center (US)
- ORCID
- Venue
- Geology
- Publisher
- Geological Society of America
- Published
- 2009-05
- Volume
- 37
- Issue
- 5
- Pages
- 399-402
- ISSN
- 0091-7613 (ISSN-L)
- 1943-2682
- OpenAlex
- W2130859746
- Cited by
- 284
- References
- 35
- Citations by year
- 2026: 5 · 2025: 14 · 2024: 11 · 2023: 5 · 2022: 14 · 2021: 13 · 2020: 27 · 2019: 20 · 2018: 21 · 2017: 15 · 2016: 10 · 2015: 17 · 2014: 21 · 2013: 33 · 2012: 27
- FWCI
- 15.11
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Geology (publishedVersion)
- Funders
- National Science Foundation
- Deutsche Forschungsgemeinschaft
- National Natural Science Foundation of China
- Chinese Academy of Sciences
- Natural Sciences and Engineering Research Council of Canada
- Topics
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Keywords
- surface oxidation, Archean-Proterozoic transition, atmospheric oxygenation, redox state, iron oxide, banded iron formations, iron oxyhydroxide, paleoredox proxies, paleo-oxygenation, Precambrian atmosphere
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