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• W1994585387 abstract "Research Article| December 01, 2006 The enigma of early Miocene biserial planktic foraminifera Christopher W. Smart; Christopher W. Smart 1School of Earth, Ocean and Environmental Sciences, University of Plymouth, Drake Circus, Plymouth, Devon PL4 8AA, UK Search for other works by this author on: GSW Google Scholar Ellen Thomas Ellen Thomas 2Department of Geology and Geophysics, Yale University, P.O. Box 208109, New Haven, Connecticut 06520-8109, USA, and Department of Earth and Environmental Sciences, Wesleyan University, Middletown, Connecticut 06459, USA Search for other works by this author on: GSW Google Scholar Author and Article Information Christopher W. Smart 1School of Earth, Ocean and Environmental Sciences, University of Plymouth, Drake Circus, Plymouth, Devon PL4 8AA, UK Ellen Thomas 2Department of Geology and Geophysics, Yale University, P.O. Box 208109, New Haven, Connecticut 06520-8109, USA, and Department of Earth and Environmental Sciences, Wesleyan University, Middletown, Connecticut 06459, USA Publisher: Geological Society of America Received: 25 May 2006 Revision Received: 10 Jul 2006 Accepted: 14 Jul 2006 First Online: 09 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 The Geological Society of America, Inc. Geology (2006) 34 (12): 1041–1044. https://doi.org/10.1130/G23038A.1 Article history Received: 25 May 2006 Revision Received: 10 Jul 2006 Accepted: 14 Jul 2006 First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Christopher W. Smart, Ellen Thomas; The enigma of early Miocene biserial planktic foraminifera. Geology 2006;; 34 (12): 1041–1044. doi: https://doi.org/10.1130/G23038A.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 Small biserial foraminifera were abundant in the early Miocene (ca. 18.9–17.2 Ma) in the eastern Atlantic and western Indian Oceans, but absent in the western equatorial Atlantic Ocean, Weddell Sea, eastern Indian Ocean, and equatorial Pacific Ocean. They have been assigned to the benthic genus Bolivina, but their high abundances in sediments without evidence for dysoxia could not be explained. Apertural morphology, accumulation rates, and isotopic composition show that they were planktic (genus Streptochilus). Living Streptochilus are common in productive waters with intermittent upwelling. The widespread early Miocene high Streptochilus abundances may reflect vigorous but intermittent upwelling, inducing high phytoplankton growth rates. However, export production (estimated from benthic foraminiferal accumulation rates) was low, possibly due to high regeneration rates in a deep thermocline. The upwelled waters may have been an analog to Subantarctic Mode Waters, carrying nutrients into the eastern Atlantic and western Indian Oceans as the result of the initiation of a deep-reaching Antarctic Circumpolar Current, active Agulhas Leakage, and vigorous vertical mixing in the Southern Oceans. 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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• W1994585387 title "The enigma of early Miocene biserial planktic foraminifera" @default.
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