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Dinoflagellate cysts are reported from 20 Upper Cretaceous claystone samples from the Godula and Istebna formationsof the Silesian unit. Age-assessment of the sediments based on 150 species suggests a Late Campanian to probably earliestMaastrichtian age for the middle and upper part of the Godula Formation and a Early Maastrichtian age for the basalpart of the Istebna Formation. Key biotic events are especially the first occurrence datums of Areoligera senonensis,Cerodinium diebelii, Palaeocystodinium golzowense and Trithyrodinium evittii, and the last occurrence datums ofOdontochitina, Palaeohystrichophora infusorioides, Raeteiaedinium truncigerum, Trihyrodinium suspectum andXenascus ceratioides. Palynofacies analysis shows deposition in an offshore marine environment subjected to influxesof terrestrial material. Organic matter is dominated by phytoclasts and contains very little amorphous organic material.The succession is also characterized by a low percentage of dinoflagellate cysts and a very low percentage of spores andpollen grains. The presence of thermophilitic dinoflagellate cysts points to a warm-temperate to subtropical climate duringLate Campanian to Early Maastrichtia

Campanian to Maastrichtian palynofacies and dinoflagellate cysts of the Silesian Unit, Outer Western Carpathians, Czech Republic