Please use this identifier to cite or link to this item: http://dspace.onu.edu.ua:8080/handle/123456789/2356
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dc.contributor.authorDolukhanov, P. M.-
dc.contributor.authorChepalyga, A. L.-
dc.contributor.authorLavrentiev, N. V.-
dc.contributor.authorKadurin, Serhii V.-
dc.contributor.authorLarchenkov, Yevhenii P.-
dc.contributor.authorShkatova, V. K-
dc.date.accessioned2012-04-18T09:37:08Z-
dc.date.available2012-04-18T09:37:08Z-
dc.date.issued2008-
dc.identifier.citationBlack sea-mediterranean corridor during the last 30 ky: sea level change and human adaptation (2005–2009) : IV plenary meeting and field trip IGCP 521 (Bucharest ; Varna, 4–16 Oct. 2008). – Bucharest, 2008uk
dc.identifier.urihttp://dspace.onu.edu.ua:8080/handle/123456789/2356-
dc.descriptionCaspian-Black Sea mediterranean corridor during last 30 ky: sea level change and human adaptive strategies (2008-2010), plenary meeting and fild trip INQUA 0501, (4, 2008);4-16, Oct., 2008uk
dc.description.abstractThe climate of northern Eurasia during the Middle Wiirm/Valdai 'megainterstadial' (OIS 3), which lasted from c. 58 to 23 ka, was cool and unstable, with at least five milder oscillations (including the 'Bryansk interstadial'). The estimated summer and winter temperatures in Eastern Europe were lower than today by 4-6°C and 4-10°C, and the annual precipitation, as low as 150-250 mm (Frenzel et al.,1992).uk
dc.language.isoenuk
dc.publisherS.nuk
dc.relation.ispartofseries;C. 44-47-
dc.subjectBlack Sea,uk
dc.subjectCaspian Seauk
dc.subjectsea-levelsuk
dc.subjectclimateuk
dc.subjectPalaeolithicuk
dc.subjectLate Pleistoceneuk
dc.titleBlack Sea and Caspian Basins in Late Pleistocene: sea-level changes, climate and early human settlementuk
dc.typeArticleuk
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