| Abstract: | Previous work on surface (modern) sediments has defined diatom species which appear to be good indicators of various oceanographic/ecologic conditions in the North Pacific Ocean and marginal seas. Three long cores from the eastern and northern sides of the Aleutian Basin show changes in species assemblage which can be interpreted in terms of changes in the ocean environment during the last glaciation (Wisconsin) and the Holocene. The early and late Wisconsin maxima were times of prolonged annual sea-ice cover and a short cool period of phytoplankton productivity during the ice-free season. The middle Wisconsin interstade, at least in the southern Bering Sea, had greater seasonal contrast than today, with some winter sea-ice cover, an intensified temperature minimum, and high spring productivity. Variations in clastic and reworked fossil material imply varying degrees of transport to the basin by Alaskan rivers. The results of Jouse?? from the central Bering Sea generally correspond with those presented here, although there are problems with direct comparison. ?? 1983. |
| Genre: | Article |
| ProdID: | 70011179 |
| Citation Author: | Sancetta, C.; Robinson, S. W. |
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| Citation End Page: | 245 |
| Citation Issue: | 2 |
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| Citation Language: | English |
| Citation Larger Work Title: | Quaternary Research |
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| Citation Number Of Pages: | 14 |
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| Citation Publisher: | Elsevier |
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| Citation Search Results Text: | Diatom evidence on Wisconsin and Holocene events in the Bering Sea; 1983; Article; Journal; Quaternary Research; Sancetta, C.; Robinson, S. W. |
| Citation Start Page: | 232 |
| Citation Volume: | 20 |
| Citation Year: | 1983 |
| Type: | citation/reference |
| Text: | Diatom evidence on Wisconsin and Holocene events in the Bering Sea; 1983; Article; Journal; Quaternary Research; Sancetta, C.; Robinson, S. W. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| URL (DIGITAL OBJECT IDENTIFIER): | http://dx.doi.org/10.1016/0033-5894(83)90079-0 |
| Date Other: | Sat, 1 Jan 1983 00:00 -0600 |
| Publisher: | Elsevier |
