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Dynamic model of integrated processes in the ecosystem of the northwest shelf of the Black Sea

โœ Scribed by I. E. Timchenko; V. A. Zhorov; E. M. Igumnova; I. P. Lazarchuk


Publisher
Springer
Year
2007
Tongue
English
Weight
193 KB
Volume
17
Category
Article
ISSN
0928-5105

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During latest Quaternary glaciation, the Black Sea became a giant freshwater lake. The surface of this lake drew down to levels more than 100 m below its outlet. When the Mediterranean rose to the Bosporus sill at 7,150 yr BP', saltwater poured through this spillway to refill the lake and submerge,