Alkanes in Quaternary deposits of the Laptev Sea


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Resumo

The distribution and genesis of n-alkanes in sediments from the 38-m sequence obtained during core boring in the Ivashkina lagoon were studied. Sediments were formed in the Holocene as a result of thermokarst and penetration of seawater. The sequence mostly includes permafrost rocks partially molten in the upper horizons and covered by Quaternary deposits, which are mostly the products of thermoabrasion.

Sobre autores

E. Romankevich

Shirshov Institute of Oceanology; Tomsk National Research Polytechnic University

Email: ratnick@mail.ru
Rússia, Moscow, 119991; Tomsk

A. Vetrov

Shirshov Institute of Oceanology

Email: ratnick@mail.ru
Rússia, Moscow, 119991

N. Belyaev

Shirshov Institute of Oceanology; Tomsk National Research Polytechnic University

Autor responsável pela correspondência
Email: ratnick@mail.ru
Rússia, Moscow, 119991; Tomsk

V. Sergienko

Institute of Chemistry, Far East Branch

Email: ratnick@mail.ru
Rússia, Vladivostok, 690022

I. Semiletov

Il’ichev Pacific Institute of Oceanology, Far East Branch; Tomsk National Research Polytechnic University

Email: ratnick@mail.ru
Rússia, Vladivostok, 690041; Tomsk

S. Sukhoverkhov

Institute of Chemistry, Far East Branch

Email: ratnick@mail.ru
Rússia, Vladivostok, 690022

S. Bratskaya

Institute of Chemistry, Far East Branch

Email: ratnick@mail.ru
Rússia, Vladivostok, 690022

N. Prokuda

Institute of Chemistry, Far East Branch

Email: ratnick@mail.ru
Rússia, Vladivostok, 690022

A. Ulyantsev

Shirshov Institute of Oceanology

Email: ratnick@mail.ru
Rússia, Moscow, 119991

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