The Karangatian epoch in the Neopleistocene history of the Black Sea

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dc.contributor.authorYanko-Hombach, Valentyna V.
dc.contributor.authorMotnenko, Irena
dc.contributor.authorЯнко-Хомбах, Валентина Венедиктовна
dc.contributor.authorЯнко-Хомбах, Валентина Венедиктівна
dc.contributor.authorМотненко, Ірена
dc.contributor.authorМотненко, Ирэна
dc.date.accessioned2017-12-01T13:15:50Z
dc.date.available2017-12-01T13:15:50Z
dc.date.issued2016
dc.description.abstractBlack Sea Quaternary history shows an alternation of transgressive and regressive stages that are related to global climate change and pronounced due to semi-isolation from the World Ocean. In warm epochs, the Black Sea is connected to the Mediterranean Sea (i.e. World Ocean) via connecting seas and straits. In cold epochs, it becomes isolated or connects to the Caspian Sea via the Manych outlet. During transgressions, sea level rises as does salinity. During regressions, when it drops below the Bosphorus sill, the basin transforms into an isolated lake. During transgressions, organisms migrate into the Black Sea from either the Mediterranean or Caspian. Such migrations affect assemblage structure and increase the number of species, especially in case of Mediterranean transgressions. During regressive stages, the number of species drops, and only holeuryhaline Mediterranean species can survive the lowering of salinity (Yanko-Hombach, 2007).uk
dc.identifier.citationGeophysical Research Abstractsuk
dc.identifier.urihttps://dspace.onu.edu.ua/handle/123456789/11659
dc.language.isoenuk
dc.relation.ispartofseries;Vol. 18
dc.subjectKarangatian epochuk
dc.subjectNeopleistocene historyuk
dc.subjectBlack Seauk
dc.titleThe Karangatian epoch in the Neopleistocene history of the Black Seauk
dc.typeArticleuk
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