The Lower Cretaceous sediments of the Ceahlǎu Nappe(from the bend region of the Romanian Carpathians)were investigated from lithological and micropaleontological(calcareous nannoplankton)points of view.Our investigations revealed that the studied deposits were sedimented within the latest Tithonian-Albian interval.The calcareous nannofossil assemblages of the turbidite calcareous successions(the Sinaia Formation)were assigned to the NJK-?NC5 calcareous nannofossil zones,which cover the Late Tithonian-Eariy Barremian interval.The sandy-shaly turbidites,which followed the calcareous turbidites of the Sinaia Formation,are Early Barremian-Early Albian in age (interval covered by the ?NCS-NC8 calcareous nannofossil zones).Because the studied deposited are mainly turbidites,many reworked nannofossils from older deposits are present in the calcareous nannofloras.Thus,some biozones(i.e.,NC5),defined based on the last occurrences of nannofossils, could not be identified.The calcareous nannofossil assemblages are composed of Tethyan taxa(which dominate the nannofloras)and cosmopolitan taxa.During two intervals(the Late Valanginian and across the Barremian/Aptian boundary),Tethyan and cosmopolitan nannofossils,together with Boreal ones,were observed.This type of mixed calcareous nannoplankton assemblage is indicative for sea-level high-stand,which allows the nannofloral exchange between the Tethyan and Boreal realms, within the two-above mentioned intervals. The Lower Cretaceous sediments of the Ceahlǎu Nappe (from the bend region of the Romanian Carpathians) were investigated from lithological and micropaleontological (calcareous nannoplankton) points of view. Our investigations revealed that the held deposits were sedimented within the latest Tithonian-Albian interval. calcareous nannofossil assemblages of the turbidite calcareous successions (the Sinaia Formation) were assigned to the NJK-? NC5 calcareous nannofossil zones, which cover the Late Tithonian-Eariy Barremian interval.The sandy-shaly turbidites, which followed the calcareous turbidites of the Sinaia Formation are early Barremian-Early Albian in age (interval covered by the NCS-NC8 calcareous nanofossil zones) .Because the studied deposited are mainly turbidites, many reworked nannofossils from older deposits are present in the calcareous nannofloras.Thus, some biozones (ie , NC5), defined based on the last occurrences of nannofossils, could not be identified. The calcareous nannofos sil assemblages are composed of Tethyan taxa (which dominate the nannofloras) and cosmopolitan taxa. Two of the intervals (the Late Valanginian and across the Barremian / Aptian boundary), Tethyan and cosmopolitan nannofossils, together with Boreal ones, were observed. This type of mixed calcareous nannoplankton assemblage is indicative for sea-level high-stand, which allows the nannofloral exchange between the Tethyan and Boreal realms, within the two-above mentioned intervals.