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• W2071465187 abstract "Research Article| June 01, 2000 Central American paleogeography controlled Pliocene Arctic Ocean molluscan migrations Louie Marincovich, Jr Louie Marincovich, Jr 1Department of Invertebrate Zoology and Geology, California Academy of Sciences, Golden Gate Park, San Francisco, California 94118-4599, USA Search for other works by this author on: GSW Google Scholar Author and Article Information Louie Marincovich, Jr 1Department of Invertebrate Zoology and Geology, California Academy of Sciences, Golden Gate Park, San Francisco, California 94118-4599, USA Publisher: Geological Society of America Received: 24 Nov 1999 Revision Received: 14 Mar 2000 Accepted: 28 Mar 2000 First Online: 02 Jun 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (2000) 28 (6): 551–554. https://doi.org/10.1130/0091-7613(2000)28<551:CAPCPA>2.0.CO;2 Article history Received: 24 Nov 1999 Revision Received: 14 Mar 2000 Accepted: 28 Mar 2000 First Online: 02 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Louie Marincovich; Central American paleogeography controlled Pliocene Arctic Ocean molluscan migrations. Geology 2000;; 28 (6): 551–554. doi: https://doi.org/10.1130/0091-7613(2000)28<551:CAPCPA>2.0.CO;2 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 Pliocene interchange of North Pacific and North Atlantic marine faunas via the Arctic Ocean was long thought to have been a single episode of faunal exchange between the northern oceans that took place as soon as the Bering Strait first opened. New evidence implies that there were two northern migration events instead of one, and that the second phase of migration was much later than the first. The migration of Atlantic-Arctic mollusks into the Bering Sea and North Pacific when the Bering Strait first opened at 4.8–5.5 Ma constituted the initial phase of this interchange, but the abrupt appearance of North Pacific mollusks in the North Atlantic at 3.6 Ma postdated the first opening of the Bering Strait by 1.2–1.9 m.y. This second phase of trans-Arctic migration was also coeval with shoaling of the Central American seaway between North and South America. This late Pliocene trans-Arctic migration of North Pacific mollusks is evidence for the reversal of marine flow to northward through the Bering Strait, which was one consequence of the reorganization of Northern Hemisphere ocean circulation caused by substantial closure of the Central American seaway. This inferred causal link between the histories of the Beringian and Panamanian ocean gateways is in agreement with ocean circulation models. 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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• W2071465187 title "Central American paleogeography controlled Pliocene Arctic Ocean molluscan migrations" @default.
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