title: The surozhian epoch in the late pleistocene history of the Black Sea
abstract: The paper presents the results of a palaeogeographic study based on facies-lithological, malacofaunal, and radiocarbon analyses of cores from three boreholes from the Black Sea shelf, 12 km southeast of the Zhelezny Rog Cape. The findings confirm the existence of the Surozh transgressive basin in the Late Pleistocene history of the Black Sea. Coarse-grained sand and shell deposits associated with the Surozh coastal facies were identified at varying depths, ranging from 9,0-6,0 to 5,2-4,2 m, at t
journal: Lomonosov Geography Journal