Dolukhanov, P. M.Chepalyga, A. L.Lavrentiev, N. V.Kadurin, Serhii V.Larchenkov, Yevhenii P.Shkatova, V. K2012-04-182012-04-182008Black 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, 2008https://dspace.onu.edu.ua/handle/123456789/2356Caspian-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., 2008The 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).enBlack Sea,Caspian Seasea-levelsclimatePalaeolithicLate PleistoceneArticle