Main Regularities of the Late Pleistocene–Holocene Transgression of the Black Sea

Альтернативна назва
Анотація
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.
Опис
Ключові слова
Black Sea, Main Regularities, Late Pleistocene, Holocene Transgression
Бібліографічний опис
Doklady Earth Sciences
DOI
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УДК