Coastal sand dunes at 100m under sea level as proof of a post Younger-Dryas Black Sea lowstand

A 3D geometric interpretation of very high-resolution seismic Chirp profiles acquired on the Romanian shelf demonstrates that the last climate change known during Holocene times was well recorded in the Black Sea basin and particularly provides a good record of its water level fluctuations.

Keyword(s)

pseudo 3D, seismic sequences, rapid transgression, forced regression

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Lericolais Gilles, Bulois C, Gillet H (2006). Coastal sand dunes at 100m under sea level as proof of a post Younger-Dryas Black Sea lowstand. IGCP 521 2nd plenary meeting and field trip , 20-28 August 2006, Odessa, Ukraine. https://archimer.ifremer.fr/doc/00000/4936/

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