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 |
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| container_end_page | 877 |
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| container_issue | 2 |
| container_start_page | 873 |
| container_title | Doklady earth sciences |
| container_volume | 463 |
| creator | Matul’, A. G. Saidova, Kh. M. Smirnova, M. A. Khusid, T. A. Kazarina, G. Kh Chekhovskaya, M. P. |
| description | 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. |
| doi_str_mv | 10.1134/S1028334X1508022X |
| format | Article |
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| source | SpringerLink Journals - AutoHoldings |
| subjects | 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) |
| title | Rapid diachronous paleoceanographic changes in the Far East marginal areas of the Pacific Ocean at the last glaciation-to-holocene transition |
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