Lignin as an indicator of the sedimentation conditions on the Arctic shelf


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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.

Sobre autores

A. Ulyantsev

Shirshov Institute of Oceanology

Autor responsável pela correspondência
Email: uleg85@gmail.com
Rússia, Nakhimovsky pr. 36, Moscow, 117997

E. Romankevich

Shirshov Institute of Oceanology; Tomsk National Research Polytechnical Institute

Email: uleg85@gmail.com
Rússia, Nakhimovsky pr. 36, Moscow, 117997; Tomsk

V. Peresypkin

Shirshov Institute of Oceanology

Email: uleg85@gmail.com
Rússia, Nakhimovsky pr. 36, Moscow, 117997

N. Belyaev

Shirshov Institute of Oceanology

Email: uleg85@gmail.com
Rússia, Nakhimovsky pr. 36, Moscow, 117997

I. Semiletov

Il’ichev Pacific Oceanological Institute, Far East Branch; Tomsk National Research Polytechnical Institute

Email: uleg85@gmail.com
Rússia, Baltiyskaya ul. 43, Vladivostok, 690041; Tomsk

S. Bratskaya

Institute of Chemistry, Far East Branch

Email: uleg85@gmail.com
Rússia, pr. Stoletiya Vladivostoka 59, Vladivostok, 690022

A. Vetrov

Shirshov Institute of Oceanology

Email: uleg85@gmail.com
Rússia, Nakhimovsky pr. 36, Moscow, 117997

V. Sergienko

Institute of Chemistry, Far East Branch

Email: uleg85@gmail.com
Rússia, pr. Stoletiya Vladivostoka 59, Vladivostok, 690022

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