Paleoceanographic conditions in the western Bering Sea as a response to global sea level changes and remote climatic signals during the last 180 kyr


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We present results from the sediment core SO201-2-85KL retrieved from the western Bering Sea that recovered the past 180 000 years. For the first time, the intense dissolution of calcareous microfossils has been established when the Bering Strait was open during the glacioeustatic sea level rise. Possible mechanisms of climatic teleconnections between remote regions are considered.

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E. Ovsepyan

Shirshov Institute of Oceanology

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Email: eovsepyan@ocean.ru
俄罗斯联邦, Moscow, 117997

E. Ivanova

Shirshov Institute of Oceanology

Email: eovsepyan@ocean.ru
俄罗斯联邦, Moscow, 117997

S. Gulev

Shirshov Institute of Oceanology

Email: eovsepyan@ocean.ru
俄罗斯联邦, Moscow, 117997

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