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

Cylindroclavulina cylindrica Zone and in the Eocene/Oligocene transition. Budapest region, Bükk Mountains foreland. Rare. * Globigerinita martini scandretti Blow et Banner (Plate V. 27/a-d) Globigerinita martini scandretti Blow et Banner subsp. nov.

, 1962, in Eames et al,

: Fundamentals of Mid-Tertiary etc. pp. 111-112» pl. XIY. figs. V-X. Description. Test small, of three whorls. Chambers tightly disposed in the low trochospire. Dorsal surface flat. Chambers inflated, rapidly growing. The last chamber is the biggest. There are four chambers in it. Sutures deep, right, obliquely disposed. Umbilicus small, deep. Aperture is a high arch at the base of the last chamber, with a thin, rim-like lip. Bulla small, inflated, situated at the equatorial margin, on the suture between the first and last chamber of the last whorl. It covers the major part of the umbilicus and the aperture as well. The supplementary aperture visible on the bulla is a low, long arch, with a well developed, rim-like lip. Test wall smooth, finely perforated^ Note. Well discernible from the other species by the features of the bulla. Occurrence. Rare in the Buda Marl, but present in all of its horizons, and in the Kiscell Clay, too. Budapest region, Bükk Mountains foreland. Globigerinita cf. unicava primitiva Blow et Banner (Plate V. 28/a-c) cf

, Globigerinita unicava primitiva Blow et Banner subsp. nov,