Pleistocene Marine Microfauna in the Bootlegger Cove Clay, Anchorage, Alaska
- 26 July 1963
- journal article
- research article
- Published by American Association for the Advancement of Science (AAAS) in Science
- Vol. 141 (3578) , 350-351
- https://doi.org/10.1126/science.141.3578.350
Abstract
Ostracods and Foraminifera, associated with molluscs, indicate a marine depositional environment for part of the Bootlegger Cove Clay. The definite Arctic and North Atlantic affinities of the microfauna suggest a possible migration through the Bering-Chukchi seaway during the late Pleistocene.This publication has 2 references indexed in Scilit:
- Cenozoic History of the Bering Land BridgeScience, 1959
- IX International Congress of PaediatricsPediatrics International, 1959