Microalgae and the Climate of the North Atlantic

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Resumo

The results of a micropaleontological study of the sediment core obtained in the northeastern part of the Norwegian–Greenland basin from a sea depth of 3013 m are presented. The microalgae species composition indicates repeated changes in marine environments during the sedimentation.

Sobre autores

T. Klyuvitkina

Lomonosov Moscow State University

Email: t.klyuvitkina@mail.ru
Moscow, Russia

E. Novichkova

Shirshov Institute of Oceanology, Russian Academy of Sciences

Moscow, Russia

L. Kireenko

Shirshov Institute of Oceanology, Russian Academy of Sciences

Moscow, Russia

M. Chekhovskaya

Shirshov Institute of Oceanology, Russian Academy of Sciences

Moscow, Russia

A. Matul

Shirshov Institute of Oceanology, Russian Academy of Sciences

Moscow, Russia

Bibliografia

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