Paleoceanographic conditions in the western Bering Sea as a response to global sea level changes and remote climatic signals during the last 180 kyr
- Авторлар: Ovsepyan E.A.1, Ivanova E.V.1, Gulev S.K.1
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Мекемелер:
- Shirshov Institute of Oceanology
- Шығарылым: Том 468, № 2 (2016)
- Беттер: 557-560
- Бөлім: Geology
- URL: https://ogarev-online.ru/1028-334X/article/view/188460
- DOI: https://doi.org/10.1134/S1028334X16060052
- ID: 188460
Дәйексөз келтіру
Аннотация
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.
Авторлар туралы
E. Ovsepyan
Shirshov Institute of Oceanology
Хат алмасуға жауапты Автор.
Email: eovsepyan@ocean.ru
Ресей, Moscow, 117997
E. Ivanova
Shirshov Institute of Oceanology
Email: eovsepyan@ocean.ru
Ресей, Moscow, 117997
S. Gulev
Shirshov Institute of Oceanology
Email: eovsepyan@ocean.ru
Ресей, Moscow, 117997
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