By Vasicek Z., Michalic J.
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Additional info for Early Cretaceous stratigraphy, palaeogeography and life in Western Carpathians
3, Fig. 6), sponge spicules, and nannoconids. The upper part of this member is dated by an ammonite association as Late Valanginian. - - 31 The third member consists of bedded spotted limestones with grey cherts. They contain obliquipitbonelloids, orthopithonelloids, pithonelloids, colomiellids, foraminifers, ostracods, radiolarians, nannoplankton, and calpionellids. Macrofauna is represented by rare aptychi, ammonites, belemnites, echinoids and scattered skeletal fragments of neritic benthic organisms.
8), Bochianites oosteri SARASIN & SCH~NDELMAYER, Lytoceras ex gr. 2 Hauterivian associations IMMEL (PI. 18, Fig. l), E. cf spiniger SOENEN), and Ptychophylloceras sp. Very poorly prcsewed Berriasian f a d remains Boreal elements [Endemoceras amblygonium come from peripheral sequences of the Fatric which (NEUMI\YR & UHLIG), Aegocrioceras atf. ] were reported have been deposited on the southern slope of the Tatric (NEUMAYR a common Mediterranean Hauterivian ammonite from Ridge. Punctaptychus sp. and Lamellaptychus sp.
3 m m k . BIRKENMAJER (1977) defined the Pieniny Limestone Formation as well bedded pale and pale grccn subpclitic limestones of the "rnaiolica" facies with green chert nodules. This formation represents a substantial part of the Lowcr Cretaceous sequence (BcrriasianBarremian) in several Picniny Klippen Belt units (predominantly in the Pieniny and Kysuca successions). BORZA(1969), ANDRUSOV& SAMUEL(1983), SAMUEL Ct al. (1988), MICHAL~K et al. (1990), HALASOVAet al. (1991), and VAS~CEKet al. (1992) camcd out a detailed lithostratigraphic study of the formation in the Brodno section (Text-fig.