Pleistocene marine microfauna in the Bootlegger Cove Clay, Anchorage, Alaska
Science
By: 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.
Suggested Citation
Schmidt, R., 1963, Pleistocene marine microfauna in the Bootlegger Cove Clay, Anchorage, Alaska: Science, v. 141, no. 3578, p. 350-351, https://doi.org/10.1126/science.141.3578.350.
Study Area
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Pleistocene marine microfauna in the Bootlegger Cove Clay, Anchorage, Alaska |
| Series title | Science |
| DOI | 10.1126/science.141.3578.350 |
| Volume | 141 |
| Issue | 3578 |
| Year Published | 1963 |
| Language | English |
| Publisher | American Association for the Advancement of Science |
| Description | 2 p. |
| First page | 350 |
| Last page | 351 |
| Country | United States |
| State | Alaska |
| City | Anchorage |