A Model for the Oceanic Mass Balance of Rhenium and Implications for the Extent of Proterozoic Ocean Anoxia
UC Riverside UC Riverside Previously Published Works Title A model for the oceanic mass balance of rhenium and implications for the extent of Proterozoic ocean anoxia Permalink https://escholarship.org/uc/item/1gh1h920 Journal GEOCHIMICA ET COSMOCHIMICA ACTA, 227 ISSN 0016-7037 Authors Sheen, Alex I Kendall, Brian Reinhard, Christopher T et al. Publication Date 2018-04-15 DOI 10.1016/j.gca.2018.01.036 Peer reviewed eScholarship.org Powered by the California Digital Library University of California Available online at www.sciencedirect.com ScienceDirect Geochimica et Cosmochimica Acta 227 (2018) 75–95 www.elsevier.com/locate/gca A model for the oceanic mass balance of rhenium and implications for the extent of Proterozoic ocean anoxia Alex I. Sheen a,b,⇑, Brian Kendall a, Christopher T. Reinhard c, Robert A. Creaser b, Timothy W. Lyons d, Andrey Bekker d, Simon W. Poulton e, Ariel D. Anbar f,g a Department of Earth and Environmental Sciences, University of Waterloo, 200 University Avenue West, Waterloo, Ontario N2L 3G1, Canada b Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, Alberta T6G 2E3, Canada c School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, GA 30332, USA d Department of Earth Sciences, University of California, Riverside, CA 92521, USA e School of Earth and Environment, University of Leeds, Leeds LS2 9JT, UK f School of Earth and Space Exploration, Arizona State University, Tempe, AZ 85287, USA g School of Molecular Sciences, Arizona State University, Tempe, AZ 85287, USA Received 13 July 2017; accepted in revised form 30 January 2018; available online 8 February 2018 Abstract Emerging geochemical evidence suggests that the atmosphere-ocean system underwent a significant decrease in O2 content following the Great Oxidation Event (GOE), leading to a mid-Proterozoic ocean (ca.
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