Distribution of Trace and Rare-Earth Elements, and Nd, Pb, and Sr Isotopes in the Surface Sediments of the Barents Sea. / Maslov, A. V.; Kuznetsov, A. B.; Politova, N. V.; Shevchenko, V. P.; Kozina, N. V.; Novigatsky, A. N.; Kravchishina, M. D.; Alexeeva, T. N.
In: Geochemistry International, Vol. 58, No. 6, 01.06.2020, p. 687-703.Research output: Contribution to journal › Article › peer-review
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TY - JOUR
T1 - Distribution of Trace and Rare-Earth Elements, and Nd, Pb, and Sr Isotopes in the Surface Sediments of the Barents Sea
AU - Maslov, A. V.
AU - Kuznetsov, A. B.
AU - Politova, N. V.
AU - Shevchenko, V. P.
AU - Kozina, N. V.
AU - Novigatsky, A. N.
AU - Kravchishina, M. D.
AU - Alexeeva, T. N.
N1 - Publisher Copyright: © 2020, Pleiades Publishing, Ltd. Copyright: Copyright 2020 Elsevier B.V., All rights reserved.
PY - 2020/6/1
Y1 - 2020/6/1
N2 - Abstract—The distribution of Sc, Co, Hf, Cr, Th, and rare-earth elements in samples of surface sediments collected during cruises 67th and 68th of the R/V Akademik Mstislav Keldysh in the Barents Sea and in its bays is analyzed. The results obtained suggest that the predominant part of the bottom sediments of the Barents Sea is composed of thin-grained siliciclastics that was supplied with suspended particulate matter of the North Cape (Atlantic) Current through the erosion of the northwestern Scandinavian coasts and some seafloor areas. Some sediments in the northern part of the sea were formed through the erosion of rocks of the Novaya Zemlya and Franz Josef Land. A certain role in their formation was probably played by material from Svalbard as well as by the Pechora River suspended particulate matter. The established isotopic characteristics (εNd, 207Pb/206Pb and 87Sr/86Sr) of surface sediments suggest that the main contribution to the formation of bottom sediments of the central Barents Sea was made by rocks of the mainland part affected by the North Cape Current. The comparison of the 87Sr/86Sr values in the surface sediments of the central part of the Barents Sea and in the ice-rafted sediments carried by the Transpolar Drift showed their significant difference. This suggests a reatively small contribution of ice-rafted material to the formation of surface sediments of the Barents Sea.
AB - Abstract—The distribution of Sc, Co, Hf, Cr, Th, and rare-earth elements in samples of surface sediments collected during cruises 67th and 68th of the R/V Akademik Mstislav Keldysh in the Barents Sea and in its bays is analyzed. The results obtained suggest that the predominant part of the bottom sediments of the Barents Sea is composed of thin-grained siliciclastics that was supplied with suspended particulate matter of the North Cape (Atlantic) Current through the erosion of the northwestern Scandinavian coasts and some seafloor areas. Some sediments in the northern part of the sea were formed through the erosion of rocks of the Novaya Zemlya and Franz Josef Land. A certain role in their formation was probably played by material from Svalbard as well as by the Pechora River suspended particulate matter. The established isotopic characteristics (εNd, 207Pb/206Pb and 87Sr/86Sr) of surface sediments suggest that the main contribution to the formation of bottom sediments of the central Barents Sea was made by rocks of the mainland part affected by the North Cape Current. The comparison of the 87Sr/86Sr values in the surface sediments of the central part of the Barents Sea and in the ice-rafted sediments carried by the Transpolar Drift showed their significant difference. This suggests a reatively small contribution of ice-rafted material to the formation of surface sediments of the Barents Sea.
KW - Barents Sea
KW - geochemistry
KW - Nd
KW - Pb and Sr isotopic composition
KW - surface sediments
UR - http://www.scopus.com/inward/record.url?scp=85086525398&partnerID=8YFLogxK
U2 - 10.1134/S0016702920060075
DO - 10.1134/S0016702920060075
M3 - Article
AN - SCOPUS:85086525398
VL - 58
SP - 687
EP - 703
JO - Geochemistry International
JF - Geochemistry International
SN - 0016-7029
IS - 6
ER -
ID: 75949557