Pedan, Halyna S.Konikov, Yevhenii G.Педан, Галина Сергіївна2012-04-182012-04-182010Black sea-mediterranean corridor during the last 30 ky: sea level change and human adaptation (2005–2010) : VI plenarry meeting and field trip IGCP-521 (Rhodes, 27 Sept. – 5 Oct., 2010). – Rhodes, 2010.https://dspace.onu.edu.ua/handle/123456789/2370Caspian-Black Sea-mediterranean corridor during last 30 ky: sea level change and human adaptiv strategies (2005-2011), plenary meeting and field trip INQUA 501 (6,2010),27 Sept.-5 Oct., 2010The Northern Black Sea shelf is a subaerial plain and regional zone of the continental platform. It is a classic example of a transgression-regression shelf. During the Late Pleistocene and Holocene, the shelf was flooded and drained repeatedly as the coastline migrated across its surface (Shcherbakov et al., 1976; Ivanov et al., 1982). According to Morgunov et al. (1981), the modern relief of the coastal part of the shelf is a zone of flooded valleys of late generationenshelfLute PleistoceneHolocenetransgressiongeomorphology structureArticle