Abstract
It is shown for the first time that the proportion of lignin in shelf deposits may range from 1/3 to the total concentration of organic carbon. The distribution of wood residues and lignin in the studied sedimentary formation is very uneven, which reflects the dynamic flux environment of sedimentation and OM supply. The calculated molecular indexes showed that most of the OM in deposits underwent insignificant diagenetic alterations.
| Original language | English |
|---|---|
| Pages (from-to) | 264-269 |
| Number of pages | 6 |
| Journal | Doklady Earth Sciences |
| Volume | 467 |
| Issue number | 1 |
| DOIs | |
| Publication status | Published - 1 Mar 2016 |
Fingerprint
ASJC Scopus subject areas
- Earth and Planetary Sciences (miscellaneous)
- Earth and Planetary Sciences(all)
Cite this
Lignin as an indicator of the sedimentation conditions on the Arctic shelf. / Ulyantsev, A. S.; Romankevich, E. A.; Peresypkin, V. I.; Belyaev, N. A.; Semiletov, I. P.; Bratskaya, S. Yu; Vetrov, A. A.; Sergienko, V. I.
In: Doklady Earth Sciences, Vol. 467, No. 1, 01.03.2016, p. 264-269.Research output: Contribution to journal › Article
}
TY - JOUR
T1 - Lignin as an indicator of the sedimentation conditions on the Arctic shelf
AU - Ulyantsev, A. S.
AU - Romankevich, E. A.
AU - Peresypkin, V. I.
AU - Belyaev, N. A.
AU - Semiletov, I. P.
AU - Bratskaya, S. Yu
AU - Vetrov, A. A.
AU - Sergienko, V. I.
PY - 2016/3/1
Y1 - 2016/3/1
N2 - It is shown for the first time that the proportion of lignin in shelf deposits may range from 1/3 to the total concentration of organic carbon. The distribution of wood residues and lignin in the studied sedimentary formation is very uneven, which reflects the dynamic flux environment of sedimentation and OM supply. The calculated molecular indexes showed that most of the OM in deposits underwent insignificant diagenetic alterations.
AB - It is shown for the first time that the proportion of lignin in shelf deposits may range from 1/3 to the total concentration of organic carbon. The distribution of wood residues and lignin in the studied sedimentary formation is very uneven, which reflects the dynamic flux environment of sedimentation and OM supply. The calculated molecular indexes showed that most of the OM in deposits underwent insignificant diagenetic alterations.
UR - http://www.scopus.com/inward/record.url?scp=84969919775&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=84969919775&partnerID=8YFLogxK
U2 - 10.1134/S1028334X16030089
DO - 10.1134/S1028334X16030089
M3 - Article
AN - SCOPUS:84969919775
VL - 467
SP - 264
EP - 269
JO - Doklady Earth Sciences
JF - Doklady Earth Sciences
SN - 1028-334X
IS - 1
ER -