Fauna z łupków graptolitowych syluru niecki bardziańskiej Gór•Świętokrzyskich

Abstract

FAUNA FROM SILURIAN GRAPTOLITIC SHALES OF THE BARDO BASIN IN THE ŚWIĘTY KRZYŻ MOUNTAINS

The Bardo syncline is situated in the central part of the Święty Krzyż Mountains. south of the Kielce-Łagów (central) synclinorium from the latter, the Bardo syncline is separated by Cambrian sediments.

In the central part of this syncline, especially in the region of Bardo, there appear Devonian sediments; from underneath them, in the flanks of the syncline. Silurian deposits are exposed (Fig. 1). This Silurian has here been developed in the shape form of two fundamental facies of graptolitic shales and of greywacke rocks.