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• W2110991103 abstract "Research Article| July 01, 2007 Synchronous millennial-scale climatic changes in the Great Basin and the North Atlantic during the last interglacial Rhawn F. Denniston; Rhawn F. Denniston 1Department of Geology, Cornell College, 600 1st Street West, Mount Vernon, Iowa 52314, USA Search for other works by this author on: GSW Google Scholar Yemane Asmerom; Yemane Asmerom 2Department of Earth and Planetary Science, Northrop Hall, University of New Mexico, Albuquerque, New Mexico 87131, USA Search for other works by this author on: GSW Google Scholar Victor Polyak; Victor Polyak 2Department of Earth and Planetary Science, Northrop Hall, University of New Mexico, Albuquerque, New Mexico 87131, USA Search for other works by this author on: GSW Google Scholar Jeffrey A. Dorale; Jeffrey A. Dorale 3Department of Geoscience, Trowbridge Hall, University of Iowa, Iowa City, Iowa 52242, USA Search for other works by this author on: GSW Google Scholar Scott J. Carpenter; Scott J. Carpenter 3Department of Geoscience, Trowbridge Hall, University of Iowa, Iowa City, Iowa 52242, USA Search for other works by this author on: GSW Google Scholar Charles Trodick; Charles Trodick 4Department of Geology, Cornell College, 600 1st Street West, Mount Vernon, Iowa 52314, USA Search for other works by this author on: GSW Google Scholar Brian Hoye; Brian Hoye 4Department of Geology, Cornell College, 600 1st Street West, Mount Vernon, Iowa 52314, USA Search for other works by this author on: GSW Google Scholar Luis A. González Luis A. González 5Department of Geology, 1475 Jayhawk Boulevard, University of Kansas, Lawrence, Kansas 66045-7613, USA Search for other works by this author on: GSW Google Scholar Author and Article Information Rhawn F. Denniston 1Department of Geology, Cornell College, 600 1st Street West, Mount Vernon, Iowa 52314, USA Yemane Asmerom 2Department of Earth and Planetary Science, Northrop Hall, University of New Mexico, Albuquerque, New Mexico 87131, USA Victor Polyak 2Department of Earth and Planetary Science, Northrop Hall, University of New Mexico, Albuquerque, New Mexico 87131, USA Jeffrey A. Dorale 3Department of Geoscience, Trowbridge Hall, University of Iowa, Iowa City, Iowa 52242, USA Scott J. Carpenter 3Department of Geoscience, Trowbridge Hall, University of Iowa, Iowa City, Iowa 52242, USA Charles Trodick 4Department of Geology, Cornell College, 600 1st Street West, Mount Vernon, Iowa 52314, USA Brian Hoye 4Department of Geology, Cornell College, 600 1st Street West, Mount Vernon, Iowa 52314, USA Luis A. González 5Department of Geology, 1475 Jayhawk Boulevard, University of Kansas, Lawrence, Kansas 66045-7613, USA Publisher: Geological Society of America Received: 12 Oct 2006 Revision Received: 22 Feb 2007 Accepted: 03 Mar 2007 First Online: 09 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (2007) 35 (7): 619–622. https://doi.org/10.1130/G23445A.1 Article history Received: 12 Oct 2006 Revision Received: 22 Feb 2007 Accepted: 03 Mar 2007 First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Rhawn F. Denniston, Yemane Asmerom, Victor Polyak, Jeffrey A. Dorale, Scott J. Carpenter, Charles Trodick, Brian Hoye, Luis A. González; Synchronous millennial-scale climatic changes in the Great Basin and the North Atlantic during the last interglacial. Geology 2007;; 35 (7): 619–622. doi: https://doi.org/10.1130/G23445A.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 Stalagmites from Goshute Cave, located in the Great Basin of the western United States, preserve ∼20,000 yr of millennial-scale oxygen isotopic variability during marine isotope stages 5c and 5b, similar in timing and structure to Dansgaard-Oeschger (D-O) events 23–21 from the Greenland Ice Sheet Project 2 record. That D-O interstades 23–21 were of longer duration than many of the later D-O events, coupled with the asymmetric shape of the D-O oxygen isotope curve, and the direct U-Th dating of the Goshute Cave stalagmites, allows for an improved understanding of the synchroneity of climatic changes between the western continental United States and the North Atlantic. Eastern Pacific–atmosphere interactions are a likely mechanism for transmission of millennial-scale climate variability into the Great Basin. 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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