Erosional truncation of uppermost Permian shallow-marine carbonates and implications for Permian-Triassic boundary events: Reply

Abstract

Research Article| May 01, 2009 Erosional truncation of uppermost Permian shallow-marine carbonates and implications for Permian-Triassic boundary events: Reply Jonathan L. Payne; Jonathan L. Payne * 1 Department of Geological and Environmental Sciences, Stanford University, 450 Serra Mall, Building 320, Stanford, California 94305, USA *E-mail: [e-mail] Search for other works by this author on: GSW Google Scholar Daniel J. Lehrmann; Daniel J. Lehrmann 2 Department of Geology, University of Wisconsin-Oshkosh, 800 Algoma Boulevard, Oshkosh, Wisconsin 54901, USA Search for other works by this author on: GSW Google Scholar David Follett; David Follett 2 Department of Geology, University of Wisconsin-Oshkosh, 800 Algoma Boulevard, Oshkosh, Wisconsin 54901, USA Search for other works by this author on: GSW Google Scholar Margaret Seibel; Margaret Seibel 2 Department of Geology, University of Wisconsin-Oshkosh, 800 Algoma Boulevard, Oshkosh, Wisconsin 54901, USA Search for other works by this author on: GSW Google Scholar Lee R. Kump; Lee R. Kump 3 Department of Geosciences, 503 Deike Building, The Pennsylvania State University, University Park, Pennsylvania 16802, USA Search for other works by this author on: GSW Google Scholar Anthony Riccardi; Anthony Riccardi 3 Department of Geosciences, 503 Deike Building, The Pennsylvania State University, University Park, Pennsylvania 16802, USA Search for other works by this author on: GSW Google Scholar Demir Altiner; Demir Altiner 4 Department of Geological Engineering, Middle East Technical University, 06531 Ankara, Turkey Search for other works by this author on: GSW Google Scholar Hiroyoshi Sano; Hiroyoshi Sano 5 Department of Earth and Planetary Sciences, Kyushu University, Fukuoka 812–8581, Japan Search for other works by this author on: GSW Google Scholar Jiayong Wei Jiayong Wei 6 Guizhou Geological Survey, Bagongli, 550005 Guiyang, China Search for other works by this author on: GSW Google Scholar Author and Article Information Jonathan L. Payne * 1 Department of Geological and Environmental Sciences, Stanford University, 450 Serra Mall, Building 320, Stanford, California 94305, USA Daniel J. Lehrmann 2 Department of Geology, University of Wisconsin-Oshkosh, 800 Algoma Boulevard, Oshkosh, Wisconsin 54901, USA David Follett 2 Department of Geology, University of Wisconsin-Oshkosh, 800 Algoma Boulevard, Oshkosh, Wisconsin 54901, USA Margaret Seibel 2 Department of Geology, University of Wisconsin-Oshkosh, 800 Algoma Boulevard, Oshkosh, Wisconsin 54901, USA Lee R. Kump 3 Department of Geosciences, 503 Deike Building, The Pennsylvania State University, University Park, Pennsylvania 16802, USA Anthony Riccardi 3 Department of Geosciences, 503 Deike Building, The Pennsylvania State University, University Park, Pennsylvania 16802, USA Demir Altiner 4 Department of Geological Engineering, Middle East Technical University, 06531 Ankara, Turkey Hiroyoshi Sano 5 Department of Earth and Planetary Sciences, Kyushu University, Fukuoka 812–8581, Japan Jiayong Wei 6 Guizhou Geological Survey, Bagongli, 550005 Guiyang, China *E-mail: [e-mail] Publisher: Geological Society of America Received: 08 Jul 2008 Accepted: 11 Jul 2008 First Online: 03 Oct 2017 Online ISSN: 1943-2674 Print ISSN: 0016-7606 © 2009 Geological Society of America GSA Bulletin (2009) 121 (5-6): 957–959. https://doi.org/10.1130/B26588.1 Article history Received: 08 Jul 2008 Accepted: 11 Jul 2008 First Online: 03 Oct 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Jonathan L. Payne, Daniel J. Lehrmann, David Follett, Margaret Seibel, Lee R. Kump, Anthony Riccardi, Demir Altiner, Hiroyoshi Sano, Jiayong Wei; Erosional truncation of uppermost Permian shallow-marine carbonates and implications for Permian-Triassic boundary events: Reply. GSA Bulletin 2009;; 121 (5-6): 957–959. doi: https://doi.org/10.1130/B26588.1 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 Wignall et al. (2009) present two arguments that the erosional surface that we described (Payne et al., 2007) is unrelated to the end-Permian mass-extinction event. First, they prefer to attribute erosion of uppermost Permian strata to subaerial exposure rather than to submarine carbonate erosion and/or dissolution. Second, they suggest that the erosion surface is not demonstrably younger than a sequence boundary within preextinction strata observed at Meishan and elsewhere. We are thankful for the interest in our study and for the opportunity to clarify the reasoning that led us to interpret the erosion surface as a feature developed... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.