The Lena River Discharge and the Climate of the Laptev Sea in the Holocene: New Reconstructions Based on Micropaleontological Data

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Resumo

Micropaleontological study of the core PS51/080-13, obtained in the shallow southeastern part of the Laptev Sea, in the area adjacent to the Lena Delta, reveals the intervals of runoff redistribution along the branches of the delta and episodes of possible cold periods in the Middle and Late Holocene.

Sobre autores

T. Klyuvitkina

Lomonosov Moscow State University

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

E. Polyakova

Lomonosov Moscow State University

Moscow, Russia

E. Novichkova

Shirshov Institute of Oceanology, Russian Academy of Sciences

Moscow, Russia

Bibliografia

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