Acid rain and ozone depletion from pulsed Siberian Traps magmatism

Research Article| January 01, 2014 Acid rain and ozone depletion from pulsed Siberian Traps magmatism Benjamin A. Black; Benjamin A. Black * 1Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, Massachusetts 02139, USA *E-mails: bablack@mit.edu; lamar@ucar.edu; shields@ucar.edu; ltelkins@dtm.ciw.edu; jtkon@ucar.edu. Search for other works by this author on: GSW Google Scholar Jean-François Lamarque; Jean-François Lamarque * 2National Center for Atmospheric Research, Boulder, Colorado 80305, USA *E-mails: bablack@mit.edu; lamar@ucar.edu; shields@ucar.edu; ltelkins@dtm.ciw.edu; jtkon@ucar.edu. Search for other works by this author on: GSW Google Scholar Christine A. Shields; Christine A. Shields * 2National Center for Atmospheric Research, Boulder, Colorado 80305, USA *E-mails: bablack@mit.edu; lamar@ucar.edu; shields@ucar.edu; ltelkins@dtm.ciw.edu; jtkon@ucar.edu. Search for other works by this author on: GSW Google Scholar Linda T. Elkins-Tanton; Linda T. Elkins-Tanton * 3Department of Terrestrial Magnetism, Carnegie Institution for Science, Washington, D.C. 20015, USA *E-mails: bablack@mit.edu; lamar@ucar.edu; shields@ucar.edu; ltelkins@dtm.ciw.edu; jtkon@ucar.edu. Search for other works by this author on: GSW Google Scholar Jeffrey T. Kiehl Jeffrey T. Kiehl * 2National Center for Atmospheric Research, Boulder, Colorado 80305, USA *E-mails: bablack@mit.edu; lamar@ucar.edu; shields@ucar.edu; ltelkins@dtm.ciw.edu; jtkon@ucar.edu. Search for other works by this author on: GSW Google Scholar Author and Article Information Benjamin A. Black * 1Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, Massachusetts 02139, USA Jean-François Lamarque * 2National Center for Atmospheric Research, Boulder, Colorado 80305, USA Christine A. Shields * 2National Center for Atmospheric Research, Boulder, Colorado 80305, USA Linda T. Elkins-Tanton * 3Department of Terrestrial Magnetism, Carnegie Institution for Science, Washington, D.C. 20015, USA Jeffrey T. Kiehl * 2National Center for Atmospheric Research, Boulder, Colorado 80305, USA *E-mails: bablack@mit.edu; lamar@ucar.edu; shields@ucar.edu; ltelkins@dtm.ciw.edu; jtkon@ucar.edu. Publisher: Geological Society of America Received: 25 Jun 2013 Revision Received: 03 Oct 2013 Accepted: 07 Oct 2013 First Online: 09 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 © 2013 Geological Society of America Geology (2014) 42 (1): 67–70. https://doi.org/10.1130/G34875.1 Article history Received: 25 Jun 2013 Revision Received: 03 Oct 2013 Accepted: 07 Oct 2013 First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Benjamin A. Black, Jean-François Lamarque, Christine A. Shields, Linda T. Elkins-Tanton, Jeffrey T. Kiehl; Acid rain and ozone depletion from pulsed Siberian Traps magmatism. Geology 2014;; 42 (1): 67–70. doi: https://doi.org/10.1130/G34875.1 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 Siberian Traps flood basalts have been invoked as a trigger for the catastrophic end-Permian mass extinction. Widespread aberrant plant remains across the Permian-Triassic boundary provide evidence that atmospheric stress contributed to the collapse in terrestrial diversity. We used detailed estimates of magmatic degassing from the Siberian Traps to complete the first three-dimensional global climate modeling of atmospheric chemistry during eruption of a large igneous province. Our results show that both strongly acidic rain and global ozone collapse are possible transient consequences of episodic pyroclastic volcanism and heating of volatile-rich Siberian country rocks. We suggest that in conjunction with abrupt warming from greenhouse gas emissions, these repeated, rapidly applied atmospheric stresses directly linked Siberian magmatism to end-Permian ecological failure on land. Our comprehensive modeling supplies the first picture of the global distribution and severity of acid rain and ozone depletion, providing testable predictions for the geography of end-Permian environmental proxies. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.