Rapid diachronous paleoceanographic changes in the Far East marginal areas of the Pacific Ocean at the last glaciation-to-holocene transition

The analysis of the distribution of diatoms and benthic foraminifers in two sediment cores taken from the continental slope of eastern Kamchatka and Shir shov Ridge revealed rapidia diachronous regional paleoceanographic changes during the global warming epoch at the transition from the last glaciat...

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Veröffentlicht in:	Doklady earth sciences 2015-08, Vol.463 (2), p.873-877
Hauptverfasser:	Matul’, A. G., Saidova, Kh. M., Smirnova, M. A., Khusid, T. A., Kazarina, G. Kh, Chekhovskaya, M. P.
Format:	Artikel
Sprache:	eng
Schlagworte:	Climate change Continental slope Earth and Environmental Science Earth Sciences Geological time Geology Glaciation Global warming Holocene Interglacial periods Ocean Oceanology Paleogeography Paleontology Relative dating (Chronology) Sediments Sediments (Geology)
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Zusammenfassung:	The analysis of the distribution of diatoms and benthic foraminifers in two sediment cores taken from the continental slope of eastern Kamchatka and Shir shov Ridge revealed rapidia diachronous regional paleoceanographic changes during the global warming epoch at the transition from the last glaciation to the Holocene.
ISSN:	1028-334X 1531-8354
DOI:	10.1134/S1028334X1508022X