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Biostratigraphy of Upper Quaternary sediments in the southern part of the Oceanology Institute Rise,Sea of Okhotsk
Authors:S P Pletnev  M V Cherepanova  E D Ivanova  I V Utkin  Ya V Kuz’min  G S Burr
Institution:1.Pacific Oceanological Institute, Far-Eastern Branch,Russian Academy of Sciences,Vladivostok,Russia;2.Institute of Biology and Soil Sciences, Far-Eastern Branch,Russian Academy of Sciences,Vladivostok,Russia;3.Pacific Institute of Geography, Far-Eastern Branch,Russian Academy of Sciences,Vladivostok,Russia;4.Institute of Geology and Mineralogy, Siberian Branch,Russian Academy of Sciences,Novosibirsk,Russia;5.University of Arizona,Tucson,USA
Abstract:The diversified analysis (data on radiocarbon ages, diatoms, planktonic and benthic foraminifers) of sediments from the central part of the Sea of Okhotsk (core from a depth of 1186 m) made it possible to define five sedimentary units corresponding to five marine oxygen-isotope stages MIS 5-MIS 1 (the last 120 ka) and provide their thorough paleontological characteristic, using different microfossil groups. Microfossil assemblages demonstrate variations in their abundance, distribution of individual species, and representatives of different ecological groups through the section.
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