Clay-mineral distribution in surface sediments of the Eurasian Arctic Ocean and continental margin as indicator for source areas and transport pathways - a synthesis.

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dc.contributor.author Wahsner, Monika
dc.contributor.author Müller, Claudia
dc.contributor.author Stein, Ruediger
dc.contributor.author Ivanov, Gennadiy I
dc.contributor.author Levitan, Mikhail A
dc.contributor.author Shelekhova, E S
dc.contributor.author Tarasov, Gennadiy A
dc.coverage.spatial MEDIAN LATITUDE: 79.023264 * MEDIAN LONGITUDE: 92.931037 * SOUTH-BOUND LATITUDE: 63.367000 * WEST-BOUND LONGITUDE: 0.165000 * NORTH-BOUND LATITUDE: 90.000000 * EAST-BOUND LONGITUDE: -6.766800 * DATE/TIME START: 1987-03-08T00:00:00 * DATE/TIME END: 1996-09-18T13:00:00 * MINIMUM DEPTH, sediment/rock: 0 m * MAXIMUM DEPTH, sediment/rock: 0 m
dc.date.accessioned 2019-11-26T04:00:23Z
dc.date.available 2019-11-26T04:00:23Z
dc.date.issued 1999-09-18
dc.identifier https://doi.pangaea.de/10.1594/PANGAEA.57249
dc.identifier https://doi.org/10.1594/PANGAEA.57249
dc.identifier.citation Wahsner, Monika; Müller, Claudia; Stein, Ruediger; Ivanov, Gennadiy I; Levitan, Mikhail A; Shelekhova, E S; Tarasov, Gennadiy A (1999): Clay-mineral distribution in surface sediments of the Eurasian Arctic Ocean and continental margin as indicator for source areas and transport pathways - a synthesis. Boreas, 28(1), 215-233, https://doi.org/10.1111/j.1502-3885.1999.tb00216.x
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/8050
dc.description.abstract Clay-mineral distributions in the Arctic Ocean and the adjacent Eurasian shelf areas are discussed to identify source areas and transport pathways of terrigenous material in the Arctic Ocean. The main clay minerals in Eurasian Arctic Ocean sediments are illite and chlorite. Smectite and kaolinite occur in minor amounts in these sediments, but show strong variations in the shelf areas. These two minerals are therefore reliable in reconstructions of source areas of sediments from the Eurasian Arctic. The Kara Sea and the western part of the Laptev Sea are enriched in smectite, with highest values of up to 70% in the deltas of the Ob and Yenisey rivers. Illite is the dominant clay mineral in all the investigated sediments except for parts of the Kara Sea. The highest concentrations with more than 70% illite occur in the East Siberian Sea and around Svalbard. Chlorite represents the clay mineral with lowest concentration changes in the Eastern Arctic, ranging between 10 and 25%. The main source areas for kaolinite in the Eurasian Arctic are Mesozoic sedimentary rocks on Franz-Josef Land islands. Based on clay-mineral data, transport of the clay fraction via sea ice is of minor importance for the modern sedimentary budget in the Arctic basins.
dc.format text/tab-separated-values, 2010 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: Wahsner, Monika; Müller, Claudia; Stein, Ruediger; Ivanov, Gennadiy I; Levitan, Mikhail A; Shelekhova, E S; Tarasov, Gennadiy A (1999): Clay-mineral distribution in surface sediments of the Eurasian Arctic Ocean and continental margin as indicator for source areas and transport pathways - a synthesis. Boreas, 28(1), 215-233, https://doi.org/10.1111/j.1502-3885.1999.tb00216.x
dc.subject 41
dc.subject 42
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dc.subject AG80/2-1
dc.subject AG80/3-1
dc.subject AG80/4-1
dc.subject AG80/5-1
dc.subject AG80/6-1
dc.subject AG80/7-1
dc.subject AG80/8-1
dc.subject AG80/9-1
dc.subject Akademik Golitsyn
dc.subject Amundsen Basin
dc.subject Arctic Ocean
dc.subject ARK-IV/3
dc.subject ARK-IX/4
dc.subject ARK-VIII/2
dc.subject ARK-VIII/3
dc.subject ARK-XI/1
dc.subject AWI_Paleo
dc.subject Barents Sea
dc.subject BC
dc.subject BCR
dc.subject Bear Island Trough
dc.subject Box corer
dc.subject Box corer (Reineck)
dc.subject Chlorite
dc.subject Chuk17
dc.subject Chuk181
dc.subject Chuk183
dc.subject Chuk184
dc.subject Chuk186
dc.subject Chuk189
dc.subject Chuk201
dc.subject Chuk21
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dc.subject Chuk9
dc.subject CTD/Rosette
dc.subject CTD-RO
dc.subject DEPTH, sediment/rock
dc.subject DM49
dc.subject Dmitry Mendeleev
dc.subject East Siberian Sea
dc.subject ES281
dc.subject ES282
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dc.subject ES290
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dc.subject ES315
dc.subject ES316
dc.subject ES317
dc.subject ES318
dc.subject ES320
dc.subject ES323
dc.subject ES326
dc.subject Fram Strait
dc.subject Franz Joseph Land/St. Anna Trough
dc.subject Gakkel Ridge, Arctic Ocean
dc.subject Giant box corer
dc.subject Giant piston corer
dc.subject GIK21520-10 PS11/310-10
dc.subject GIK21521-13 PS11/340-13
dc.subject GIK21522-19 PS11/358-19
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dc.subject GPC
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dc.subject Gravity corer (Russian type)
dc.subject Illite
dc.subject Jenissei
dc.subject KAL
dc.subject KAL_R
dc.subject Kaolinite
dc.subject Kaolinite/Chlorite ratio
dc.subject Kara Sea
dc.subject Kara Sea/St. Anna Trough
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dc.subject Kasten corer RUS
dc.subject Laptev Sea
dc.subject Laptev Sea, Taymyr Island
dc.subject Lomonosov Ridge, Arctic Ocean
dc.subject Makarov Basin
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dc.subject Mooring (long time)
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dc.subject Morris Jesup Rise
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dc.subject Ob
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dc.subject Paleoenvironmental Reconstructions from Marine Sediments @ AWI
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dc.subject Quaternary Environment of the Eurasian North
dc.subject QUEEN
dc.subject RGC
dc.subject RUS_unspec
dc.subject SL
dc.subject Smectite
dc.subject Smectite/Illite ratio
dc.subject SPASIBAIII
dc.subject Svalbard
dc.subject van Veen Grab
dc.subject VGRAB
dc.subject Vilkitsky Strait
dc.subject Water sample
dc.subject WS
dc.subject X-ray diffraction TEXTUR, clay fraction
dc.subject Yermak Plateau
dc.title Clay-mineral distribution in surface sediments of the Eurasian Arctic Ocean and continental margin as indicator for source areas and transport pathways - a synthesis.
dc.title.alternative Distribution of clay minerals in surface sediments of the Eurasian Arctic Ocean
dc.type Dataset


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