Excess Freshwater Outflow from the Black Sea-Lake during Glacial and Deglacial Periods and Delayed Entry of Marine Water in the Early Holocene Require Evolving Sills
The Black Sea becomes periodically isolated from the global ocean during each glacial period. This occurs when the elevation of the global ocean is lower than the Bosporus sill, putting a stop to inflow of salt water to the Black Sea. This phenomenon allows the Black Sea to evolve from a marine envi...
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| Language: | English |
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2016
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| Online Access: | https://doi.org/10.7916/D8QJ7H72 |