New constraints on the ages of Neoproterozoic glaciations in south China

Research Article| May 01, 2004 New constraints on the ages of Neoproterozoic glaciations in south China Chuanming Zhou; Chuanming Zhou 1Nanjing Institute of Geology and Paleontology, Nanjing 210008, China, and Department of Geosciences, Virginia Polytechnic Institute, Blacksburg, Virginia 24061, USA Search for other works by this author on: GSW Google Scholar Robert Tucker; Robert Tucker 2Department of Earth and Planetary Sciences, Washington University, St. Louis, Missouri 63130, USA Search for other works by this author on: GSW Google Scholar Shuhai Xiao; Shuhai Xiao 3Department of Geosciences, Virginia Polytechnic Institute, Blacksburg, Virginia 24061, USA Search for other works by this author on: GSW Google Scholar Zhanxiong Peng; Zhanxiong Peng 4Department of Earth and Planetary Sciences, Washington University, St. Louis, Missouri 63130, USA Search for other works by this author on: GSW Google Scholar Xunlai Yuan; Xunlai Yuan 5Nanjing Institute of Geology and Paleontology, Nanjing 210008, China Search for other works by this author on: GSW Google Scholar Zhe Chen Zhe Chen 5Nanjing Institute of Geology and Paleontology, Nanjing 210008, China Search for other works by this author on: GSW Google Scholar Author and Article Information Chuanming Zhou 1Nanjing Institute of Geology and Paleontology, Nanjing 210008, China, and Department of Geosciences, Virginia Polytechnic Institute, Blacksburg, Virginia 24061, USA Robert Tucker 2Department of Earth and Planetary Sciences, Washington University, St. Louis, Missouri 63130, USA Shuhai Xiao 3Department of Geosciences, Virginia Polytechnic Institute, Blacksburg, Virginia 24061, USA Zhanxiong Peng 4Department of Earth and Planetary Sciences, Washington University, St. Louis, Missouri 63130, USA Xunlai Yuan 5Nanjing Institute of Geology and Paleontology, Nanjing 210008, China Zhe Chen 5Nanjing Institute of Geology and Paleontology, Nanjing 210008, China Publisher: Geological Society of America Received: 22 Oct 2003 Revision Received: 12 Jan 2004 Accepted: 14 Jan 2004 First Online: 02 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (2004) 32 (5): 437–440. https://doi.org/10.1130/G20286.1 Article history Received: 22 Oct 2003 Revision Received: 12 Jan 2004 Accepted: 14 Jan 2004 First Online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Chuanming Zhou, Robert Tucker, Shuhai Xiao, Zhanxiong Peng, Xunlai Yuan, Zhe Chen; New constraints on the ages of Neoproterozoic glaciations in south China. Geology 2004;; 32 (5): 437–440. doi: https://doi.org/10.1130/G20286.1 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 most complete Neoproterozoic successions in south China contain three diamictite intervals in the Changan, Tiesiao, and Nantuo Formations. The youngest and most widespread Nantuo glacial deposit overlies the Datangpo Formation and underlies the fossil- rich Doushantuo Formation. Previous authors have correlated the Nantuo diamictite to either Sturtian or Marinoan glacial deposits elsewhere. Here we report sedimentary and δ13C chemostratigraphic data of the Doushantuo cap dolostone, which overlies the Nantuo Formation. Facies-dependent variation in δ13C is interpreted as evidence for spatial heterogeneity in δ13C and/or temporal diachroneity in the initiation of cap carbonate sedimentation. Sedimentary and chemostratigraphic data are indicative of a Marinoan age for the Nantuo glaciation. This inference is supported by a new U-Pb zircon age of 663 ± 4 Ma from a tuffaceous bed in the Datangpo Formation. The new date and other isotopic ages from south China constrain the age of the Changan and Tiesiao glaciation(s) as between 761 ± 8 Ma and 663 ± 4 Ma, and the Nantuo glaciation as between 663 ± 4 Ma and 599 ± 4 Ma. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.