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

HILLEBRANDT, p. SAID & SABRY, p. Description ; Test small, almost lenticular in form, biconvex. Equatorial periphery circular, slightly lobate, axial periphery acute. Chambers crescentic, about 13 arranged in 3 whorls, increasing slowly in size. .The last whorl composed of 6 large roughly triangular chambers, almost equal in size. Wall calcareous perforate, surface smooth to lightly spinose. Aperture an elongate arch,covered by a delicate lip, interiomarginal extraumbilical - umbilical. Diameter: 0,7 mm Occurrence :

. Some specimens of this species are found in G. ve- lascoensi

s zone (Sample No. 4) of the Taramsa section. Stratigraphie range: GLAESSNER (1937) described this species from the lower Eocene of nordwest Caucasus. LOEBLICH & TAPPAN (1957) recorded this species from the middle Paleocene (velascoensis -acuta- spiralis subzone) of the Gulf & Atlantic Coastal Plain. SAID & KERDANY (1961) found G. pseudoscitula in the Esna Shale formation of Oasis Parafra, Western Desert, Egypt. This species was recorded by HILLEBRANDT (1962) from zone "P" of Landenian age in the Basin of Reichenhall and Salzburg, Austria

. SAID & SABRY (1964) recorded this species from the G. pseudome nardii zone of the Gebel Aweina section, Nile Valley, Egypt. 1962 Globorotalia pseudoscitula GLAESSNER. 129, pi. 12, figs. 12a-c. 1964 Globorotalia pseudoscitula GLAESSNER. 3OA, pi. 2, fig. 1.