Research Article| April 01, 2009 Bioapatite 87Sr/86Sr of the last woolly mammoths—Implications for the isolation of Wrangel Island Laura Arppe; Laura Arppe 11Department of Geology, P.O. Box 64, 00014 University of Helsinki, Finland Search for other works by this author on: GSW Google Scholar Juha A. Karhu; Juha A. Karhu 11Department of Geology, P.O. Box 64, 00014 University of Helsinki, Finland Search for other works by this author on: GSW Google Scholar Sergey L. Vartanyan Sergey L. Vartanyan 22Department of Geography, Herzen Russian State Pedagogical University, 191186, St. Petersburg, Moika 48, Russia Search for other works by this author on: GSW Google Scholar Author and Article Information Laura Arppe 11Department of Geology, P.O. Box 64, 00014 University of Helsinki, Finland Juha A. Karhu 11Department of Geology, P.O. Box 64, 00014 University of Helsinki, Finland Sergey L. Vartanyan 22Department of Geography, Herzen Russian State Pedagogical University, 191186, St. Petersburg, Moika 48, Russia Publisher: Geological Society of America Received: 21 Aug 2008 Revision Received: 24 Nov 2008 Accepted: 26 Nov 2008 First Online: 02 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 © 2009 Geological Society of America Geology (2009) 37 (4): 347–350. https://doi.org/10.1130/G25467A.1 Article history Received: 21 Aug 2008 Revision Received: 24 Nov 2008 Accepted: 26 Nov 2008 First Online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Laura Arppe, Juha A. Karhu, Sergey L. Vartanyan; Bioapatite 87Sr/86Sr of the last woolly mammoths—Implications for the isolation of Wrangel Island. Geology 2009;; 37 (4): 347–350. doi: https://doi.org/10.1130/G25467A.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 movements of terminal Pleistocene and Holocene mammoths on Wrangel Island, off northeastern Siberia, were investigated using the isotopic composition of Sr in skeletal remains. A significant shift toward more radiogenic 87Sr/86Sr ratios, from 0.71218 ± 0.00103 to 0.71491 ± 0.00138 in bioapatite, marks the beginning of the Holocene. The higher Sr isotope values in mid-Holocene mammoth remains are interpreted as an influence of radiogenic Sr derived from the Neoproterozoic rocks in the central part of Wrangel Island. The shift implies a change in the ranging and feeding areas of the animals, ultimately reflecting the inundation of the mainland connection and isolation of the population. The shift indicates also that the late Pleistocene animals were not permanent occupants in the territory that makes up present-day Wrangel Island. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
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