Main regularities of the Late Pleistocene-Holocene transgression of the Black Sea

被引：0
|
作者：
N. V. Esin
V. Yanko-Hombach
O. N. Kukleva
N. I. Esin
机构：
[1] Russian Academy of Sciences,Southern Branch, Shirshov Institute of Oceanology
[2] Avalon Institute of Applied Science,undefined
[3] Southern Federal University,undefined
来源：
Doklady Earth Sciences | 2010年 / 430卷
关键词：
DOKLADY Earth Science; Late Pleistocene; Main Regularity; Holocene Transgression; Freshwater Balance;
D O I：
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摘要：
A mathematical model describing the Black Sea level change in the Late Pleistocene-Holocene is offered. A theoretical curve for temporal change in the sea level is obtained. It is established that, in the range from 20 to 12 ky BP, the sea level rose to ∼20 m and fluctuated with various amplitudes and periods. In the range from 12 to 11 ky BP during the Bosphorus Strait formation, there was a sea regression by 30–50 meters, and level of the Black Sea dropped to the World Ocean level. Further, it mirrored variation of the ocean level.
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页码：194 / 197
页数：3
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