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The sedimentary record of the Tarcău and Vrancea Nappes, belonging to the flysch accretionary zone of theEastern Carpathians (Eastern Carpathian Outer Flysch), registered Cretaceous-Miocene events during the evolution ofthe Moldavidian Basin. Our biostratigraphic data indicate that the deposits studied are younger than previously reported.The comparison of sedimentary record studied with the Late Cretaceous—Early Miocene global eustatic curveindicates that eustatic factor played a secondary role, after the tectonic one. Four main stages of different processes influencedby tectonics are recognized in the sedimentary record: (1) Campanian—Maastrichtian—earliest Paleocene; (2) latestYpresian—Lutetian; (3) late Chattian—earliest Aquitanian, and (4) late Aquitanian-early Burdigalian. The late Chattian—earliest Aquitanian and late Aquitanian-early Burdigalian records indicate a high tectonic influence. The first event wasrelated to the foredeep stage of the sedimentary domain studied, and the second one to the deformation stage of the samedomain. The sedimentary records of tectonic influence recognized during these stages are useful tools for geodynamicreconstructions. The stratigraphic correlation of Tarcău and Vrancea sedimentary records are used to propose someconstraints in the timing of the deformation for the central Moldavidian Basin and close domains

Tectonic control on the sedimentary record of the central Moldavidian Basin (Eastern Carpathians, Romania)