2018
DOI: 10.1016/j.quaint.2016.06.019
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Evolutionary mechanisms of the Paratethys Sea and its separation into the Black Sea and Caspian Sea

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Cited by 21 publications
(8 citation statements)
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“…The Kuban barbel B. kubanicus Berg, 1912 inhabits the Kuban drainage, which is the extended riverine system of West Ciscaucasia. This species was also detected in the Manych system due to recent water diversion from the Kuban tributaries via canals (Poznyak, 1987); the Manych valley served in the past as a connecting passage between the Caspian and Black Sea basins (Esin et al, 2016). The Rioni barbel B. rionicus Kamensky, 1899, was described as originating from the Rioni basin, West Transcaucasia, but was later found to be synonymous with B. escherichii Steindachner, 1897 by Berg (1914).…”
Section: Introductionmentioning
confidence: 99%
“…The Kuban barbel B. kubanicus Berg, 1912 inhabits the Kuban drainage, which is the extended riverine system of West Ciscaucasia. This species was also detected in the Manych system due to recent water diversion from the Kuban tributaries via canals (Poznyak, 1987); the Manych valley served in the past as a connecting passage between the Caspian and Black Sea basins (Esin et al, 2016). The Rioni barbel B. rionicus Kamensky, 1899, was described as originating from the Rioni basin, West Transcaucasia, but was later found to be synonymous with B. escherichii Steindachner, 1897 by Berg (1914).…”
Section: Introductionmentioning
confidence: 99%
“…At its greatest extent, Lake Urmia was the largest lake in the Middle East and the sixth-largest hypersaline lake on Earth 10 . Despite its distance from the sea, based on palaeogeographic studies, the lake has marine origin as a remnant of the Paratethys sea, which started to dry from the Pleistocene epoch, leaving Lake Urmia, Aral and the Caspian Sea 11 . In terms of salinity, Lake Urmia is characterized by an extreme salinity, about 27% (w/v), with a high level of Cl − , Na + , SO 4 2− , Mg 2+ , K + , and Ca 2+ ions.…”
Section: Introductionmentioning
confidence: 99%
“…It is known that the Caspian Sea is a relict basin from the ancient oceans Tethys and Paratethys that existed in the Mesozoic and early Cenozoic eras. Thus, the Caspian Sea was part of the World Ocean and finally separated from it about 14-10 million years ago as part of the Sarmatian Sea [110]. Therefore, probably, the general profile of the Caspian Sea virome retained some features of and similarity to the viromes of the open seas.…”
Section: Discussionmentioning
confidence: 98%