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• W2322179616 abstract "Research Article| October 01, 2014 Microanalyses link sulfur from large igneous provinces and Mesozoic mass extinctions Sara Callegaro; Sara Callegaro 1Department of Geosciences, University of Padua, via Gradenigo 6, 35131 Padua, Italy Search for other works by this author on: GSW Google Scholar Don R. Baker; Don R. Baker 2Department of Earth and Planetary Sciences, McGill University, 3450 University Street, Montreal, Quebec H3A 0G4, Canada Search for other works by this author on: GSW Google Scholar Angelo De Min; Angelo De Min 3Department of Geosciences, University of Trieste, via E. Weiss 8, 34127 Trieste, Italy Search for other works by this author on: GSW Google Scholar Andrea Marzoli; Andrea Marzoli 1Department of Geosciences, University of Padua, via Gradenigo 6, 35131 Padua, Italy Search for other works by this author on: GSW Google Scholar Kalotina Geraki; Kalotina Geraki 4Diamond Light Source, Harwell Science and Innovation Campus, Didcot OX11 0DE, UK Search for other works by this author on: GSW Google Scholar Hervé Bertrand; Hervé Bertrand 5Laboratoire de Géologie de Lyon, UMR CNRS 5276, Université Lyon 1 et Ecole Normale Supérieure de Lyon, 46 Allée d’Italie, 69364 Lyon Cedex 7, France Search for other works by this author on: GSW Google Scholar Cecilia Viti; Cecilia Viti 6Earth Science Section, University of Siena, via Laterina 8, 53100 Siena, Italy Search for other works by this author on: GSW Google Scholar Fabrizio Nestola Fabrizio Nestola 1Department of Geosciences, University of Padua, via Gradenigo 6, 35131 Padua, Italy Search for other works by this author on: GSW Google Scholar Author and Article Information Sara Callegaro 1Department of Geosciences, University of Padua, via Gradenigo 6, 35131 Padua, Italy Don R. Baker 2Department of Earth and Planetary Sciences, McGill University, 3450 University Street, Montreal, Quebec H3A 0G4, Canada Angelo De Min 3Department of Geosciences, University of Trieste, via E. Weiss 8, 34127 Trieste, Italy Andrea Marzoli 1Department of Geosciences, University of Padua, via Gradenigo 6, 35131 Padua, Italy Kalotina Geraki 4Diamond Light Source, Harwell Science and Innovation Campus, Didcot OX11 0DE, UK Hervé Bertrand 5Laboratoire de Géologie de Lyon, UMR CNRS 5276, Université Lyon 1 et Ecole Normale Supérieure de Lyon, 46 Allée d’Italie, 69364 Lyon Cedex 7, France Cecilia Viti 6Earth Science Section, University of Siena, via Laterina 8, 53100 Siena, Italy Fabrizio Nestola 1Department of Geosciences, University of Padua, via Gradenigo 6, 35131 Padua, Italy Publisher: Geological Society of America Received: 31 Mar 2014 Revision Received: 13 Jun 2014 Accepted: 18 Jul 2014 First Online: 09 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 © 2014 Geological Society of America Geology (2014) 42 (10): 895–898. https://doi.org/10.1130/G35983.1 Article history Received: 31 Mar 2014 Revision Received: 13 Jun 2014 Accepted: 18 Jul 2014 First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Sara Callegaro, Don R. Baker, Angelo De Min, Andrea Marzoli, Kalotina Geraki, Hervé Bertrand, Cecilia Viti, Fabrizio Nestola; Microanalyses link sulfur from large igneous provinces and Mesozoic mass extinctions. Geology 2014;; 42 (10): 895–898. doi: https://doi.org/10.1130/G35983.1 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 Volcanic gases can have devastating impacts on Earth’s environment and life. However, measurement of volatile elements in prehistoric magmas is challenging. We present a new method for determining sulfur contents in magmas using its concentrations in clinopyroxenes and an experimentally determined crystal-melt partition coefficient. Using this method we compared magmatic sulfur contents in the Paraná-Etendeka large igneous province (LIP; South America) and two other similarly sized LIPs, the Central Atlantic magmatic province (CAMP) and the Deccan Traps (India). We found that the CAMP and Deccan Traps, both associated with major extinction events, contained high magmatic sulfur concentrations, up to 1900 ppm. Conversely, the Paraná-Etendeka LIP, lacking significant environmental effects, had substantially lower magmatic sulfur concentrations, less than 800 ppm. 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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• W2322179616 title "Microanalyses link sulfur from large igneous provinces and Mesozoic mass extinctions" @default.
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