LATE PLEISTOCENE-HOLOCENE BENTHIC FORAMINIFERS AND EVOLUTION OF NEAR-BOTTOM ENVIRONMENTS IN THE CENTRAL SEA OF OKHOTSK
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dc.contributor.author | Khusid T.A. | |
dc.contributor.author | Basov I.A. | |
dc.date.accessioned | 2021-02-18T10:36:41Z | |
dc.date.available | 2021-02-18T10:36:41Z | |
dc.date.issued | 2001 | |
dc.identifier | https://elibrary.ru/item.asp?id=13370353 | |
dc.identifier.citation | Stratigraphy and Geological Correlation, 2001, 9, 1, 93-103 | |
dc.identifier.issn | 0869-5938 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/25137 | |
dc.description.abstract | Taxonomic composition and distribution of benthic foraminifers in the upper Pleistocene-Holocene sediments that are penetrated by the gravity core in the southern slope of the Akademii Nauk Rise in the central part of the Sea of Okhotsk (Station V34-90) are discussed. Four established assemblages of benthic foraminifers successively replacing each other upward in the section reflect relevant stages of hydrological evolution of the basin: the terminal stage of the last glacial (2000-12500 years ago), deglaciation stage (12500-8500 years ago), and the early (8500-4000 years ago) and late (the last 4000 years) phases of the current interglacial. A comparison between foraminiferal assemblages from the Akademii Nauk Rise and from coeval sediments studied before in the southeastern part of the Sea of Okhotsk revealed that the near-bottom environments during both the deglaciation and current interglacial periods differed in these areas. It is assumed that these regional differences point to the time-variable influence of the Pacific warm water. | |
dc.subject | Foraminifers | |
dc.subject | Pleistocene | |
dc.subject | Holocene | |
dc.subject | Sea of Okhotsk | |
dc.title | LATE PLEISTOCENE-HOLOCENE BENTHIC FORAMINIFERS AND EVOLUTION OF NEAR-BOTTOM ENVIRONMENTS IN THE CENTRAL SEA OF OKHOTSK | |
dc.type | Статья | |
dc.subject.age | Cenozoic::Quaternary::Holocene | en |
dc.subject.age | Cenozoic::Quaternary::Pleistocene | en |
dc.subject.age | Кайнозой::Четвертичная::Голоцен | ru |
dc.subject.age | Кайнозой::Четвертичная::Плейстоцен | ru |
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