The responses of benthic foraminifera to paleoceanographic changes during the last glacial maximum, deglaciation, and the Holocene in the northwestern Pacific

Author:

Psheneva O. Yu.,Gorbarenko S. A.

Publisher

Pleiades Publishing Ltd

Subject

Aquatic Science,Oceanography

Reference29 articles.

1. Gorbarenko, S.A. and Gol’dberg, E.L., Assessment of variations of primary production in the Sea of Okhotsk, Bering Sea, and Northwestern Pacific over the Last Glaciation Maximum and Holocene, Dokl. Earth Sci., 2005, vol. 405, no. 9, pp. 1380–1383.

2. Ovsepyan, E.A., Ivanova, E.V., Murdmaa, L.O., and Alekhina, G.N., Sea-surface bioproductivity changes in the Northwest Pacific over the last 25 kyr, Oceanology (Engl. Transl.), 2014, vol. 54, no. 4, pp. 505–518.

3. Psheneva, O.Yu. and Gorbarenko, S.A., Response of bottom environments in the central Sea of Okhotsk to orbital- and millennial-scale climate changes during the last 130 000 years according to benthic foraminifera, Dokl. Earth Sci., 2013, vol. 452, no. 2, pp. 1030–1033.

4. Saidova, Kh.M., Ekologiya foraminifer i paleogeografiya dal’nevostochnykh morei SSSR i severo-zapadnoi chasti Tikhogo okeana (Ecology of Foraminifera and Paleogeography of the Far Eastern Seas of the USSR and the Northwestern Pacific Ocean), Moscow: Akad. Nauk SSSR, 1961.

5. Shuntov, V.P., Biologiya dal’nevostochnykh morei Rossii (Biology of the Far Eastern Seas of Russia), Vladivostok: Tikhookean. Nauchno–Issled. Rybokhoz. Tsentr, 2001, vol. 1, pp. 8–16.

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