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dc.contributor.author Pavlidis, Yury A
dc.contributor.author Shcherbakov, Fyodor A
dc.coverage.spatial MEDIAN LATITUDE: 72.350000 * MEDIAN LONGITUDE: 59.125000 * SOUTH-BOUND LATITUDE: 72.190000 * WEST-BOUND LONGITUDE: 57.850000 * NORTH-BOUND LATITUDE: 72.510000 * EAST-BOUND LONGITUDE: 60.400000 * MINIMUM DEPTH, sediment/rock: 1.0 m * MAXIMUM DEPTH, sediment/rock: 202.5 m
dc.date.accessioned 2019-11-23T10:15:31Z
dc.date.available 2019-11-23T10:15:31Z
dc.date.issued 2000-06-15
dc.identifier https://doi.pangaea.de/10.1594/PANGAEA.761701
dc.identifier https://doi.org/10.1594/PANGAEA.761701
dc.identifier.citation Pavlidis, Yury A; Shcherbakov, Fyodor A (2000): Recent bottom sediments of the Eurasian Arctic Seas. Translated from Okeanologiya, 2000, 40(1), 137-147, Oceanology, 40(1), 129-138
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/7274
dc.description.abstract A new generalized schematic map of distribution of recent sediments within Eurasian Arctic shelves is considered. The sediments have accumulated as a result of interaction of various factors and processes specific to high latitudes. They include input of terrigenous material by modern glaciers, ice transport, thermal abrasion, sedimentation controlled by many years of ice cover, and others. Characteristic regularity is marked over Arctic shelves: in seas with heavier ice cover, the most fine-grained deposits are distributed, they contain minimum amount of coarse-grained ice rafted debris; in seas with lighter ice cover mosaic distribution of various types of sediments is observed. Composition of surface sediments from the Arctic shelves corresponds to a relatively cool stage of the modern interglacial period. In the 21-st century a new warming is expected.
dc.format text/tab-separated-values, 64 data points
dc.language.iso en
dc.publisher PANGAEA
dc.rights CC-BY-3.0: Creative Commons Attribution 3.0 Unported
dc.rights Access constraints: unrestricted
dc.source Supplement to: Pavlidis, Yury A; Shcherbakov, Fyodor A (2000): Recent bottom sediments of the Eurasian Arctic Seas. Translated from Okeanologiya, 2000, 40(1), 137-147, Oceanology, 40(1), 129-138
dc.subject Archive of Ocean Data
dc.subject ARCOD
dc.subject DEPTH, sediment/rock
dc.subject Epoch
dc.subject GC
dc.subject Grain size analysis after Petelin (1967, Nauka, Moscow)
dc.subject Gravity corer
dc.subject Kara Sea
dc.subject Professor Shtokman
dc.subject PSh12
dc.subject PSh12-1405
dc.subject PSh12-1407
dc.subject Size fraction < 0.001 mm, clay
dc.subject Size fraction < 0.010 mm
dc.subject Size fraction > 1 mm, gravel
dc.subject Size fraction 0.100-0.010 mm
dc.subject Size fraction 1-0.1 mm
dc.title Recent bottom sediments of the Eurasian Arctic Seas.
dc.title.alternative (Table 3) Grain size composition of Holocene deposits from the Kara Sea
dc.type Dataset


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