IMIS

Publications | Institutes | Persons | Datasets | Projects | Maps
[ report an error in this record ]basket (1): add | show Print this page

one publication added to basket [228339]
Cenozoic migrations of marine invertebrates through the Bering Strait region
Durham, J.W.; MacNeil, F.S. (1967). Cenozoic migrations of marine invertebrates through the Bering Strait region, in: Hopkins, D.M. (Ed.) The Bering Land Bridge. pp. 326-349
In: Hopkins, D.M. (Ed.) (1967). The Bering Land Bridge. Stanford University Press: Stanford. ISBN 0-8047-0272-1. ix, 495 pp., more

Available in  Authors 

Keywords
    Aquatic organisms > Marine organisms > Aquatic animals > Marine invertebrates
    Behaviour > Migrations
    Distribution
    Environments > Aquatic environment > Marine environment
    Geography > Biogeography
    Geological time > Phanerozoic > Geological time > Cenozoic
    Brachiopoda [WoRMS]; Echinoidea [WoRMS]; Pelecypoda [WoRMS]
    INE, Bering Strait [Marine Regions]
    Marine/Coastal

Authors  Top 
  • Durham, J.W.
  • MacNeil, F.S.

Abstract
    Marine molluscan genera that have simple biogeographic histories and that originated and developed in the middle and higher latitudes of the North Pacific and North Atlantic Oceans are most significant in evaluating marine migrations through Bering Strait and the Arctic Ocean. The available evidence suggests that no transarctic Cenozoic marine migrations occurred earlier than about late Miocene (Pontian) time; during late Pliocene and Pleistocene time, migrations are well documented. These data do not require the connecting seaways to have remained open continuously after their first establishment. It seems more probable that the seaways were intermittently open and closed, but the molluscan paleontologic data on hand do not permit accurate dating of these fluctuations.

All data in the Integrated Marine Information System (IMIS) is subject to the VLIZ privacy policy Top | Authors