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Article
Lithology and Stratigraphy of the Quaternary Sediments from the Ameghino Segment of the Atlantic Patagonian Margin
The paper provides the first lithological and age data from the Ameghino segment of the Atlantic Patagonian Margin. The multiproxy study, which involves lithology, microfossils, magnetic susceptibility, color ...
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Article
Environments in the Central Norwegian–Greenland Basin during Neoglaciation in the Last 5000 Years
A comparison of new results on diatom micropaleontology with the available paleoclimatic data on the sediment core PS1243-2 and global/regional paleoclimate archives allowed assuming that Neoglaciation in the ...
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Article
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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Article
Diatom evidence for paleoclimate changes in the northwestern Pacific during the last 20000 years
The micropaleontological study of two sediment cores taken from the continental slope of the Eastern Kamchatka Peninsula and from the northern Shirshov Ridge in the Bering Sea in the scope of the international...
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Article
Sedimentation in the Angola and Cape basins during the quaternary
Reference cores of sediments from the Angola and Cape basins were subjected to lithological, geochemical, and micropaleontological investigations. Based on nannofossil and diatom assemblages, the examined sedi...
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Article
Diatomaceous oozes of the Middle Caspian Sea
Ten cores taken by a gravity corer from an area 5 × 5 km in size at the foot of the western slope of the Derbent Basin recovered uniform sections composed of variegated clotted diatomaceous oozes and soft gray...
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Article
Quaternary sediments in the axial zone of the Brazil Basin
Lithological and micropaleontological studies of sediments were carried out along the meridional profile across the Brazil Basin. Based on nannoplankton and diatom assemblages, the sediments represented by oxi...
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Article
Paleoceanography of the central sea of Okhotsk during the middle Pleistocene (350–190 ka) as inferred from micropaleontological data
The distribution of diatoms, radiolarians, planktonic and benthic foraminifers, and sediment components in the fraction >0.125 mm was analyzed in the core obtained from the central Sea of Okhotsk within the fr...