Dr. Nagy I. Zoltán szerk.: Fragmenta Mineralogica Et Palaentologica 3. 1972. (Budapest, 1972)

Chambers subglobular and inflated, arranged in 2 ^whorls, increasing rapidly in size. The final whorl composed of 4 inflated semi-spherical chambers, the final chamber is large, almost spherical. Wall calcareous perforate, surface spinose. Sutures depressed, slightly curved on the spiral side, straight radial on the umbilical side. Umbilicus small, open. Aperture a low arch, interiomarginal

, extraumbilical- umbilical, bordered by a distinct lip. Diameter: 0,32 mm Occurrence : This species occurs in small number in sample no. 8 (

G. uncinata zone) Taramsa section. Stratigraphie range: This species was first described by SUBBOTINA (1953) from the Danian, Paleocene and lower Eocene of the Kuba and Kheu River northern Caucasus, U.S.S.R. LOEBLICH & TAPPAN (1957) removed this species to genus Globoro talia and recorded it from the Paleocene of the Gulf and Atlantic Coastal Plain. HILLEBRANDT (1962) found this species in the Danian - Landenian of the basin of Reichenhall and Salzburg, Austria. In Egypt , this species was figured and described by SAID & KERDANY (196I) from the lower part of the Esna Shale of Parafra Oasis, Western Desert. SAID & SABRY (1964) recorded this species in the G. pseudome nardii zone of Gebel Aweina section, Nile Valley. Globorotalia velascoensis (CUSHMAN) (pl. VII. fig. 1.) 1925 Pulvinulina velascoensis CUSHMAN. - CUSHMAN, p. 19, pi.

3, figs. 5a, c.