Composition and genesis of the organic matter in the bottom sediments of the East Siberian Sea

Abstract

The chemical composition of organic matter (C_org, N_org, δ¹³C, δ¹⁵N, and n-alkanes) was studied in the top layer of bottom sediments of the East Siberian Sea. Possible ways were proposed to estimate the amount of the terrigenous component in their organic matter (OM). The fraction of terrigenous OM estimated by the combined use of genetic indicators varied from 15% in the eastern part of the sea, near the Long Strait, to 95% in the estuaries of the Indigirka and Kolyma rivers, averaging 62% over the sea area.

Original language	English
Pages (from-to)	156-167
Number of pages	12
Journal	Geochemistry International
Volume	46
Issue number	2
DOIs	https://doi.org/10.1007/s11476-008-2005-7
Publication status	Published - 1 Feb 2008
Externally published	Yes

ASJC Scopus subject areas

Geophysics
Geochemistry and Petrology

Access to Document

10.1007/s11476-008-2005-7

Fingerprint Dive into the research topics of 'Composition and genesis of the organic matter in the bottom sediments of the East Siberian Sea'. Together they form a unique fingerprint.

Cite this

Vetrov, A. A., Semiletov, I. P., Dudarev, O. V., Peresypkin, V. I., & Charkin, A. N. (2008). Composition and genesis of the organic matter in the bottom sediments of the East Siberian Sea. Geochemistry International, 46(2), 156-167. https://doi.org/10.1007/s11476-008-2005-7

@article{4d4f68c7dd994fd1bd726072f3abd1c4,

title = "Composition and genesis of the organic matter in the bottom sediments of the East Siberian Sea",

abstract = "The chemical composition of organic matter (Corg, Norg, δ13C, δ15N, and n-alkanes) was studied in the top layer of bottom sediments of the East Siberian Sea. Possible ways were proposed to estimate the amount of the terrigenous component in their organic matter (OM). The fraction of terrigenous OM estimated by the combined use of genetic indicators varied from 15% in the eastern part of the sea, near the Long Strait, to 95% in the estuaries of the Indigirka and Kolyma rivers, averaging 62% over the sea area.",

author = "Vetrov, {A. A.} and Semiletov, {Igor Petrovich} and Dudarev, {Oleg Victorovich} and Peresypkin, {V. I.} and Charkin, {A. N.}",

year = "2008",

month = feb,

day = "1",

doi = "10.1007/s11476-008-2005-7",

language = "English",

volume = "46",

pages = "156--167",

journal = "Geochemistry International",

issn = "0016-7029",

publisher = "Maik Nauka-Interperiodica Publishing",

number = "2",

}

TY - JOUR

T1 - Composition and genesis of the organic matter in the bottom sediments of the East Siberian Sea

AU - Vetrov, A. A.

AU - Semiletov, Igor Petrovich

AU - Dudarev, Oleg Victorovich

AU - Peresypkin, V. I.

AU - Charkin, A. N.

PY - 2008/2/1

Y1 - 2008/2/1

N2 - The chemical composition of organic matter (Corg, Norg, δ13C, δ15N, and n-alkanes) was studied in the top layer of bottom sediments of the East Siberian Sea. Possible ways were proposed to estimate the amount of the terrigenous component in their organic matter (OM). The fraction of terrigenous OM estimated by the combined use of genetic indicators varied from 15% in the eastern part of the sea, near the Long Strait, to 95% in the estuaries of the Indigirka and Kolyma rivers, averaging 62% over the sea area.

AB - The chemical composition of organic matter (Corg, Norg, δ13C, δ15N, and n-alkanes) was studied in the top layer of bottom sediments of the East Siberian Sea. Possible ways were proposed to estimate the amount of the terrigenous component in their organic matter (OM). The fraction of terrigenous OM estimated by the combined use of genetic indicators varied from 15% in the eastern part of the sea, near the Long Strait, to 95% in the estuaries of the Indigirka and Kolyma rivers, averaging 62% over the sea area.

UR - http://www.scopus.com/inward/record.url?scp=41849118057&partnerID=8YFLogxK

UR - http://www.scopus.com/inward/citedby.url?scp=41849118057&partnerID=8YFLogxK

U2 - 10.1007/s11476-008-2005-7

DO - 10.1007/s11476-008-2005-7

M3 - Article

AN - SCOPUS:41849118057

VL - 46

SP - 156

EP - 167

JO - Geochemistry International

JF - Geochemistry International

SN - 0016-7029

IS - 2

ER -