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Almost black shale filling fissures in the Štramberk Limestone belonging to the Silesian Unit, Outer WesternCarpathians contain prolific and poorly to moderately well preserved spores, pollen, organic-walled dinoflagellate cysts,foraminifers, and calcareous nannofossils. A detailed micropaleontological analysis of the proved stratigraphical intervalfrom the Valanginian to the Albian indicated sedimentary conditions of brackish, restricted marine, shallow-marine andneritic sedimentation. Moreover, it drew attention to occasional influence from the Boreal province in the depositional areaof the NW part of Tethys, especially during the Early Valanginian and Hauterivian, as supported by the presence of highlatitudenannofossils and organic-walled dinoflagellate cysts. Terrestrial miospores form a significant component ofpalynoassemblages and give evidence of continent proximity in the Valanginian-Barremian interval. Samples were acquiredfrom isolated fissure fills in the Štramberk Limestone and, therefore, they do not represent a continuous section.Web of Science62433230

Biostratigraphy and paleoecology of the Lower Cretaceous sediments in the Outer Western Carpathians (Silesian Unit, Czech Republic)