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Geochemistry of organic matter of bottom sediments in the rises of the central Arctic Ocean. / Petrova, V. I.; Batova, G. I.; Kursheva, A. V.; Litvinenko, I. V.

In: Russian Geology and Geophysics, Vol. 51, No. 1, 01.01.2010, p. 88-97.

Research output: Contribution to journal › Article › peer-review

Harvard

Petrova, VI, Batova, GI, Kursheva, AV & Litvinenko, IV 2010, 'Geochemistry of organic matter of bottom sediments in the rises of the central Arctic Ocean', Russian Geology and Geophysics, vol. 51, no. 1, pp. 88-97. https://doi.org/10.1016/j.rgg.2009.12.008

APA

Petrova, V. I., Batova, G. I., Kursheva, A. V., & Litvinenko, I. V. (2010). Geochemistry of organic matter of bottom sediments in the rises of the central Arctic Ocean. Russian Geology and Geophysics, 51(1), 88-97. https://doi.org/10.1016/j.rgg.2009.12.008

Vancouver

Petrova VI, Batova GI, Kursheva AV, Litvinenko IV. Geochemistry of organic matter of bottom sediments in the rises of the central Arctic Ocean. Russian Geology and Geophysics. 2010 Jan 1;51(1):88-97. https://doi.org/10.1016/j.rgg.2009.12.008

Author

Petrova, V. I. ; Batova, G. I. ; Kursheva, A. V. ; Litvinenko, I. V. / Geochemistry of organic matter of bottom sediments in the rises of the central Arctic Ocean. In: Russian Geology and Geophysics. 2010 ; Vol. 51, No. 1. pp. 88-97.

BibTeX

@article{ce6e8e0c80bc4e7db0e2366d4e7ae69d,
title = "Geochemistry of organic matter of bottom sediments in the rises of the central Arctic Ocean",
abstract = "Based on geomorphological, lithological, and facial characteristics of the East Arctic continental margin, we studied the main factors controlling the Late Cenozoic supply of organic matter (OM) to the bottom sediments of the Central Arctic rises of the Arctic Ocean. Complex analysis of dispersed OM in the samples taken during the expeditions of the R/V {"}Akademik Fedorov{"} in 2000 and 2005 showed a significant difference between the sediments of the Lomonosov Ridge and Mendeleev Rise. The bottom sediments of the latter are strongly transformed and lack terrigenous components, as evidenced results from the main geochemical characteristics (contents of Corg, Ccarb, Norg, bitumens, and humic acids) and the composition and distribution of hydrocarbon molecular markers (alkanes, saturated and aromatic cyclanes). The obtained data evidence that ancient sedimentary rocks containing genetically uniform deeply transformed (up to mesocatagenesis) OM played a significant role in the formation of the Pleistocene-Holocene sediments of the axial part of the Mendeleev Rise.",
keywords = "Arctic, Arctic Ocean, bottom sediments, dispersed organic matter, geochemistry, hydrocarbon molecular markers",
author = "Petrova, {V. I.} and Batova, {G. I.} and Kursheva, {A. V.} and Litvinenko, {I. V.}",
year = "2010",
month = jan,
day = "1",
doi = "10.1016/j.rgg.2009.12.008",
language = "English",
volume = "51",
pages = "88--97",
journal = "Russian Geology and Geophysics",
issn = "1068-7971",
publisher = "Elsevier",
number = "1",

}

RIS

TY - JOUR

T1 - Geochemistry of organic matter of bottom sediments in the rises of the central Arctic Ocean

AU - Petrova, V. I.

AU - Batova, G. I.

AU - Kursheva, A. V.

AU - Litvinenko, I. V.

PY - 2010/1/1

Y1 - 2010/1/1

N2 - Based on geomorphological, lithological, and facial characteristics of the East Arctic continental margin, we studied the main factors controlling the Late Cenozoic supply of organic matter (OM) to the bottom sediments of the Central Arctic rises of the Arctic Ocean. Complex analysis of dispersed OM in the samples taken during the expeditions of the R/V "Akademik Fedorov" in 2000 and 2005 showed a significant difference between the sediments of the Lomonosov Ridge and Mendeleev Rise. The bottom sediments of the latter are strongly transformed and lack terrigenous components, as evidenced results from the main geochemical characteristics (contents of Corg, Ccarb, Norg, bitumens, and humic acids) and the composition and distribution of hydrocarbon molecular markers (alkanes, saturated and aromatic cyclanes). The obtained data evidence that ancient sedimentary rocks containing genetically uniform deeply transformed (up to mesocatagenesis) OM played a significant role in the formation of the Pleistocene-Holocene sediments of the axial part of the Mendeleev Rise.

AB - Based on geomorphological, lithological, and facial characteristics of the East Arctic continental margin, we studied the main factors controlling the Late Cenozoic supply of organic matter (OM) to the bottom sediments of the Central Arctic rises of the Arctic Ocean. Complex analysis of dispersed OM in the samples taken during the expeditions of the R/V "Akademik Fedorov" in 2000 and 2005 showed a significant difference between the sediments of the Lomonosov Ridge and Mendeleev Rise. The bottom sediments of the latter are strongly transformed and lack terrigenous components, as evidenced results from the main geochemical characteristics (contents of Corg, Ccarb, Norg, bitumens, and humic acids) and the composition and distribution of hydrocarbon molecular markers (alkanes, saturated and aromatic cyclanes). The obtained data evidence that ancient sedimentary rocks containing genetically uniform deeply transformed (up to mesocatagenesis) OM played a significant role in the formation of the Pleistocene-Holocene sediments of the axial part of the Mendeleev Rise.

KW - Arctic

KW - Arctic Ocean

KW - bottom sediments

KW - dispersed organic matter

KW - geochemistry

KW - hydrocarbon molecular markers

UR - http://www.scopus.com/inward/record.url?scp=72549083394&partnerID=8YFLogxK

U2 - 10.1016/j.rgg.2009.12.008

DO - 10.1016/j.rgg.2009.12.008

M3 - Article

AN - SCOPUS:72549083394

VL - 51

SP - 88

EP - 97

JO - Russian Geology and Geophysics

JF - Russian Geology and Geophysics

SN - 1068-7971

IS - 1

ER -

ID: 47855643