Sixty dinoflagellate cyst taxa have been found in Middle to Late Eocene marl clasts that occur in an exotic-bearing submarine slump within the Lower Oligocene Szaflary beds (Podhale Flysch, Inner Carpathians, Poland). Eocene dinoflagellate cyst assemblages are evidenced for the first time from these deposits. Their taxonomic composition is compared with previously described Oligocene dinocyst assemblages from the Podhale Flysch. On this basis, different palaeoenviron- mental conditions during Middle-Late Eocene and Oligocene in Central Carpathian basin are suggested.
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