Abstract of ref. 1803:
The 1st paleontologically confirmed occurrence of Upper Cretaceous sediments in the Little Carpathians was described. A series of strata of carbonate-sandstones through fine grained conglomerates of the Campanian with large Foraminifera of the genera Orbitoides, Pseudosidlerites and Lepidorbitoides was exposed on the southern slope of Vapenkova skala near Rozbehy. Bodies of biohermal reef limestone with corals and Dasycladaceae, probably of the Maastrichtian, were found on the walls of the Campanian strata. The find represents an important connecting link between the Brezova development of the Upper Cretaceous and Senonian sediments found to exist on the floor of the Vienna basin in drillings in the area of Zavod and Studienka. O. tissoti, O. media, P. vidali and L. minima are discussed in detail.