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.
| Original language | English |
|---|---|
| Pages (from-to) | 156-167 |
| Number of pages | 12 |
| Journal | Geochemistry International |
| Volume | 46 |
| Issue number | 2 |
| DOIs | |
| Publication status | Published - 1 Feb 2008 |
| Externally published | Yes |
Fingerprint
ASJC Scopus subject areas
- Geophysics
- Geochemistry and Petrology
Cite this
Composition and genesis of the organic matter in the bottom sediments of the East Siberian Sea. / Vetrov, A. A.; Semiletov, Igor Petrovich; Dudarev, Oleg Victorovich; Peresypkin, V. I.; Charkin, A. N.
In: Geochemistry International, Vol. 46, No. 2, 01.02.2008, p. 156-167.Research output: Contribution to journal › Article
}
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 -