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• W2012028156 abstract "Research Article| May 01, 2013 Anoxia in the terrestrial environment during the late Mesoproterozoic Vivien M. Cumming; Vivien M. Cumming * 1Department of Earth Sciences, Durham University, South Road, Durham DH1 3LE, UK *E-mail: v.m.cumming@durham.ac.uk. Search for other works by this author on: GSW Google Scholar Simon W. Poulton; Simon W. Poulton 2School of Earth and Environment, University of Leeds, Leeds LS2 9JT, UK Search for other works by this author on: GSW Google Scholar Alan D. Rooney; Alan D. Rooney 3Department of Earth and Planetary Sciences, Harvard University, Cambridge, Massachusetts 02138, USA Search for other works by this author on: GSW Google Scholar David Selby David Selby 1Department of Earth Sciences, Durham University, South Road, Durham DH1 3LE, UK Search for other works by this author on: GSW Google Scholar Author and Article Information Vivien M. Cumming * 1Department of Earth Sciences, Durham University, South Road, Durham DH1 3LE, UK Simon W. Poulton 2School of Earth and Environment, University of Leeds, Leeds LS2 9JT, UK Alan D. Rooney 3Department of Earth and Planetary Sciences, Harvard University, Cambridge, Massachusetts 02138, USA David Selby 1Department of Earth Sciences, Durham University, South Road, Durham DH1 3LE, UK *E-mail: v.m.cumming@durham.ac.uk. Publisher: Geological Society of America Received: 09 Oct 2012 Revision Received: 10 Dec 2012 Accepted: 11 Dec 2012 First Online: 09 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 © 2013 Geological Society of America Geology (2013) 41 (5): 583–586. https://doi.org/10.1130/G34299.1 Article history Received: 09 Oct 2012 Revision Received: 10 Dec 2012 Accepted: 11 Dec 2012 First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Vivien M. Cumming, Simon W. Poulton, Alan D. Rooney, David Selby; Anoxia in the terrestrial environment during the late Mesoproterozoic. Geology 2013;; 41 (5): 583–586. doi: https://doi.org/10.1130/G34299.1 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 A significant body of evidence suggests that the marine environment remained largely anoxic throughout most of the Precambrian. In contrast, the oxygenation history of terrestrial aquatic environments has received little attention, despite the significance of such settings for early eukaryote evolution. To address this, we provide here a geochemical and isotopic assessment of sediments from the late Mesoproterozoic Nonesuch Formation of central North America. We utilize rhenium-osmium (Re-Os) geochronology to yield a depositional age of 1078 ± 24 Ma, while Os isotope compositions support existing evidence for a lacustrine setting. Fe-S-C systematics suggest that the Nonesuch Formation was deposited from an anoxic Fe-rich (ferruginous) water column. Thus, similar to the marine realm, anoxia persisted in terrestrial aquatic environments in the Middle to Late Proterozoic, but sulfidic water column conditions were not ubiquitous. Our data suggest that oxygenation of the terrestrial realm was not pervasive at this time and may not have preceded oxygenation of the marine environment, signifying a major requirement for further investigation of links between the oxygenation state of terrestrial aquatic environments and eukaryote evolution. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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• W2012028156 title "Anoxia in the terrestrial environment during the late Mesoproterozoic" @default.
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