C14 dating and facies control of paleo-shorelines location on NW Black Sea shelf in Holocene
Kadurin, Serhii V.
Larchenkov, Yevhenii P.
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The northwestern Black Sea shelf was an alluvial plain that was flooded in the course of the Late Neoeuxinian and Chernomorian transgression (Larchenov and Kadurin, 2011). The latter started ca. 9.4 ka BP (all radiocarbon dates in this paper are in non-calibrated years BP), and occurred in an oscillatory or transgressive-regressive manner. Each transgressive-regressive stage formed its own paleocoastline, which is well expressed in the shelf relief (Larchenkov and Kadurin, 2011). Because the number of samples dated by l4C from paleocoastlines is relatively small, interpolation and extrapolation methods along with facies analysis of bottom sediments are required.
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