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• W2053383349 abstract "Research Article| April 01, 2009 Circum-Pacific arc flare-ups and global cooling near the Eocene-Oligocene boundary Brian R. Jicha; Brian R. Jicha * 1Department of Geology and Geophysics, University of Wisconsin, Madison, Wisconsin 53706, USA *E-mail: bjicha@geology.wisc.edu. Search for other works by this author on: GSW Google Scholar David W. Scholl; David W. Scholl 2Department of Geology and Geophysics, University of Alaska Fairbanks, Fairbanks, Alaska 99775, USA Search for other works by this author on: GSW Google Scholar David K. Rea David K. Rea 3Department of Geological Sciences, University of Michigan, Ann Arbor, Michigan 48109, USA Search for other works by this author on: GSW Google Scholar Geology (2009) 37 (4): 303–306. https://doi.org/10.1130/G25392A.1 Article history received: 06 Aug 2008 rev-recd: 06 Nov 2008 accepted: 11 Nov 2008 first online: 02 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 Brian R. Jicha, David W. Scholl, David K. Rea; Circum-Pacific arc flare-ups and global cooling near the Eocene-Oligocene boundary. Geology 2009;; 37 (4): 303–306. doi: https://doi.org/10.1130/G25392A.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 Explosive eruptions from subaerial arc volcanoes can have significant environmental impact because of the discharge of ash and volatiles directly into the atmosphere and oceans. The link between climate cooling and voluminous volcanic eruptions has remained speculative due to a lack of supporting evidence. A compilation of 2814 K-Ar and 40Ar/39Ar age determinations from four circum-Pacific arcs indicates that periods of high volcanic output (i.e., flare-ups) have been episodic and, in some cases, synchronous. Peak periods and subsequent lulls in arc magmatism over the past 50 m.y. have occurred coeval with major fluctuations in global climate, including the Eocene-Oligocene transition, one of the most prominent global climate reorganizations in the Cenozoic. Hundreds of intermediate to silicic eruptions occurred during an extremely vigorous period of circum-Pacific volcanism beginning in the late Eocene, which likely led to the production of sulfur aerosols in the stratosphere and fertilization of surface waters of the Pacific Ocean. We provide a mechanism that may have been partly responsible for the climatic preconditioning that must have preceded and ultimately promoted Antarctic ice sheet growth ~34 m.y. ago. 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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• W2053383349 date "2009-04-01" @default.
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• W2053383349 title "Circum-Pacific arc flare-ups and global cooling near the Eocene-Oligocene boundary" @default.
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• W2053383349 doi "https://doi.org/10.1130/g25392a.1" @default.
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