Pleistocene marine microfauna in the Bootlegger Cove Clay, Anchorage, Alaska

R.A.M. Schmidt

doi:10.1126/science.141.3578.350

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Pleistocene marine microfauna in the Bootlegger Cove Clay, Anchorage, Alaska

R.A.M. Schmidt

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Abstract

Ostracods and Foraminifera, associated with mollusks, 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.

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Source-reported bounding extent: 61.1046048078652° to 61.27817705429962° latitude; -150.0872180734081° to -149.62700471668575° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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R.A.M. Schmidt. 1963. Pleistocene marine microfauna in the Bootlegger Cove Clay, Anchorage, Alaska. https://doi.org/10.1126/science.141.3578.350

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