Dr. Nagy I. Zoltán szerk.: Fragmenta Mineralogica Et Palaentologica 2. 1970-71. (Budapest, 1971)

De script ion. Test "big, of three whorls, 3 1/2 chambers each. Trochospire of medium height. Shape of test (hulla left out of consideration) triangular. Chambers rapidly growing, inflated, moderately embracing each other. Sutures on the ventral surface deeply cut; less deeply cut, right and radial on the dorsal one. Umbilicus wide, covered by a bulla. Aperture not visible. Bulla big, cylindrical, elongated perpendicularly to the longitudinal axis of the test. If it is smaller, it is also flatter. No opening is to be seen on it. Test wall of beecell pattern ornamentation, or punctulated. Bulla of thinner wall, more finely perforated and ornamented, than the rest of the test. Occurrence. It is not too common in the Buda Marl; present in the Cylindroclavulina cylindrica Zone and in the Eocene/Oligocene transition. Budapest region, Bükk Mountains foreland. Globigerinita gortanii gortanii (Borsetti) (Plate II. 9/a-c, 10/a-c) Catapsydrax gortanii n. sp. - Borsetti, 1959. Ann. Mus. Geol. Bol., Giorn.Geol. (2a) vol. XXVII. p. 205. tav. I. (XIII.) lad. Description, Test very big, of three whorls, which are tightly coiled. Trochospire very high. Chambers rapidly growing, inflated. Pour chambers in each whorl. Sutures deeply cut, right. Aperture very rarely visible. Bulla big, partly, or completely covering the large umbilicus.More finely perforated, than the rest of the rest. Wall chambered. Tiny knots around the umbilicus. Note. The species is easily identifiable at hand of its considerable size and high trochospire. Occurrence. It is present in the Buda Marl, in the 32