By Vasicek Z., Michalic J.
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Extra resources for Early Cretaceous stratigraphy, palaeogeography and life in Western Carpathians
S. , filicoslatus STEFANOV belemnites Duvalia dilatata dilatata (BIANVILLE) (R. fractocostatus TRAI~~H, L. didayi (COQUAND) and the belemnites Pseudohelus brevis PAQUER(PI. 29, Figs. 29, Figs. 1, 2), D. dilatata hinervioides STOYANOVAVERGILOV~ D. d. -VERGILOVA (PI. 28, 5 , 6 ) and Duvalia sp. 3, 4), and Pseudoduvalia hahiformis (DIJVALFigs. The redeposited Early Hauterivian cephalopal association from the Strsovce Turbidite (StAZovcc JOUVE)(PI. 29, Figs. 7-9). The Late Hauterivian association in the central part section, Text-fig.
1991), and VAS~CEKet al. (1992) camcd out a detailed lithostratigraphic study of the formation in the Brodno section (Text-fig. 11) situated in the Kysuca Gate near 2ilina. The lower member of this formation consists of thick-bedded creamy-grey biomicrites. They contain only aptychi and belernnite guard fragments and fairly well preserved Beniasian calpionellid associations (PI. 2, Fig. 7). The clasts in several microclastic pelbiomicrosparite to pelbiosparite intercalations are formed by Tithonian and earlicst Berriasian biomicrites indicating erosion of adjacent synsedimentary faulted block segments (the bottom rclief must have been greater than ten meters).
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