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

被引：3
|
作者：
Esin, N. V. [1 ]
Yanko-Hombach, V. [2 ]
Kukleva, O. N. [1 ]
Esin, N. I. [3 ]
机构：
[1] Russian Acad Sci, PP Shirshov Oceanol Inst, Southern Branch, Gelendzhik, Krasnodar Krai, Russia
[2] Avalon Inst Appl Sci, Winnipeg, MB, Canada
[3] So Fed Univ, Rostov Na Donu, Russia
来源：
DOKLADY EARTH SCIENCES | 2010年 / 430卷 / 02期
关键词：
DOKLADY Earth Science; Late Pleistocene; Main Regularity; Holocene Transgression; Freshwater Balance;
D O I：
10.1134/S1028334X10020108
中图分类号：
P [天文学、地球科学];
学科分类号：
07 ;
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 similar 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.
引用
收藏
页码：194 / 197
页数：4
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