Esin, Nikolay V.Yanko-Hombach, Valentyna V.Kuklevaa, O. N.Esin, Nikolay I.Янко-Хомбах, Валентина ВенедиктовнаЯнко-Хомбах, Валентина ВенедиктівнаЕсин, Николай В.Есин, Николай ИгоревичЄсін, Микола ІгоровичЄсін, Микола В.Куклева, О. Н.2018-11-082018-11-082010Doklady Earth Scienceshttps://dspace.onu.edu.ua/handle/123456789/19428A 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.enBlack SeaMain RegularitiesLate PleistoceneHolocene TransgressionArticle