Research Article| March 01, 2015 Two Paleoproterozoic glacio-eustatic cycles in the Turee Creek Group, Western Australia Martin J. Van Kranendonk; Martin J. Van Kranendonk † 1School of Biological, Earth and Environmental Sciences, and Australian Centre for Astrobiology, University of New South Wales, Kensington, NSW 2052, Australia2ARC Centre of Excellence for Core to Crust Fluid Systems, Department of Earth & Planetary Sciences, Macquarie University, NSW 2109, Australia †m.vankranendonk@unsw.edu.au. Search for other works by this author on: GSW Google Scholar Rajat Mazumder Rajat Mazumder 1School of Biological, Earth and Environmental Sciences, and Australian Centre for Astrobiology, University of New South Wales, Kensington, NSW 2052, Australia Search for other works by this author on: GSW Google Scholar Author and Article Information Martin J. Van Kranendonk † 1School of Biological, Earth and Environmental Sciences, and Australian Centre for Astrobiology, University of New South Wales, Kensington, NSW 2052, Australia2ARC Centre of Excellence for Core to Crust Fluid Systems, Department of Earth & Planetary Sciences, Macquarie University, NSW 2109, Australia Rajat Mazumder 1School of Biological, Earth and Environmental Sciences, and Australian Centre for Astrobiology, University of New South Wales, Kensington, NSW 2052, Australia †m.vankranendonk@unsw.edu.au. Publisher: Geological Society of America Received: 28 Oct 2013 Revision Received: 11 Aug 2014 Accepted: 26 Sep 2014 First Online: 08 Mar 2017 Online ISSN: 1943-2674 Print ISSN: 0016-7606 © 2014 Geological Society of America GSA Bulletin (2015) 127 (3-4): 596–607. https://doi.org/10.1130/B31025.1 Article history Received: 28 Oct 2013 Revision Received: 11 Aug 2014 Accepted: 26 Sep 2014 First Online: 08 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Martin J. Van Kranendonk, Rajat Mazumder; Two Paleoproterozoic glacio-eustatic cycles in the Turee Creek Group, Western Australia. GSA Bulletin 2015;; 127 (3-4): 596–607. doi: https://doi.org/10.1130/B31025.1 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 SocietyGSA Bulletin Search Advanced Search Abstract Widespread glaciations in the period 2.42–2.22 Ga have led to the suggestion of a Paleoproterozoic "snowball Earth," yet this hypothesis has been difficult to substantiate. Here, we report the discovery of two Paleoproterozoic glacio-eustatic cycles from a predominantly marine succession in Western Australia, where previously only one had been recorded. Sedimentary facies characteristics reveal that each cycle sharply commenced with a falling stage systems tract and terminated with a transgressive systems tract, consistent with drawdown and subsequent release of large volumes of seawater from, and into, waxing and waning ice sheets, respectively. This discovery provides support for the widespread nature of Paleoproterozoic glaciations and a major climatic change accompanying the rise in atmospheric oxygen. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
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Kranendonk et al. (2014) studied this question.
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