The first ikaite find in bottom sediments of the East Siberian Sea

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Resumo

The first ikaite find in bottom sediments of the East Siberian Sea is described. The ikaite was crystallized under low temperatures (probably around 7°C) with the participation of carbon from oxidized organic matter (diagenesis).

Sobre autores

O. Kolesnik

V.I. Il’ichev Pacific Oceanological Institute, Far Eastern Branch of the Russian Academy of Sciences

Email: kolesnik_o@poi.dvo.ru
Vladivostok, Russia

A. Kolesnik

V.I. Il’ichev Pacific Oceanological Institute, Far Eastern Branch of the Russian Academy of Sciences

Vladivostok, Russia

A. Gorbarev

V.I. Il’ichev Pacific Oceanological Institute, Far Eastern Branch of the Russian Academy of Sciences; Far Eastern Federal University

Vladivostok, Russia; Vladivostok, Russia

A. Karabtsov

Far East Geological Institute, Far Eastern Branch of the Russian Academy of Sciences

Vladivostok, Russia

E. Vologina

Institute of the Earth’s Crust, Siberian Branch of the Russian Academy of Sciences

Irkutsk, Russia

N. Zarubina

Far East Geological Institute, Far Eastern Branch of the Russian Academy of Sciences

Vladivostok, Russia

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