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conodont faunas, with particular emphasis on the Polygnathus pseudofoliatus Group. The material comes from the Jirásek quarry at Koněprusy (Fig. 1), which represents a unique section in the Barrandian area where the kockelianus–ensensis boundary interval corresponding to the Kačák Episode, is developed in a carbonate suc­ cession. (Note: In this paper we use the designation Kačák Episode sensu Walliser & Bultynck 2011, which better reflects its polyphase nature). Conodonts from the Jirásek quarry were previously studied by Kalvoda & Zikmundová in Galle & Hladil (1991), Kalvoda (1992) and Kalvoda in Hladil & Kalvoda (1993a, b). The following conodonts were reported by the above mentioned authors from the

bulletin of geosciences

Middle Devonian (Eifelian, australis-ensensis zones) conodonts from the Jirásek quarry near Koněprusy (Barrandian area, Czech Republic) with special emphasis on the Polygnathus pseudofoliatus Group and notes on environmental changes related to the Kačák Episode