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

1957 Globorotalia elongata GLAESSNER. - BOLLI, p. 77, pl. 20, figs. 11-13. 1957a Globorotalia elongata GLAESSNER. - LOEBLICH & TAPPAN, p. 189, pl. 45, fig. 5; nl. 46, fig. 5.; pi. 48, fig. 5; pi. 49, fig. 7; pi. 54, fig. 1-5. pi. 59, fig. 9; pi. 63, fig. 2. I960 Globorotalia elongata GLAESSNER. - OLSSON, p. 45, pi. 9, figs. 4-6. 1962 Globorotalia (Globorotalia) elongata GLAESSNER. - HILLEBRANDT, p. 127. 1966 Globorotalia emilei sp. nov. - EL NAGGAR, p. 208, pi. 17, figs. 9a-c. Description : Test medium, low trochospiral, compressed, dorsal side almost flat, umbilical side moderately convex; composed of 2 -s- whorls. Equatorial periphery elongate, slightly lobate; axial periphery acute. Chambers compressed, about 12 on the dorsal side arranged in 2 i whorls. The last whorl is composed 1 of 4 2 chambers increasing rapidly in size, the last chamberconstitutes about 1/3 of the test. Wall calcareous, perforate, surface smooth. Sutures on the dorsal side curved, strongly depressed, on the ventral side radial. Umbilicus wide open. Aperture a low arch, irteriomarginal

, extraumbilical - umbilical. Diameter: 0,38 mm Occurrence : Some specimens of this species occur in the G.pseu domenardii zone of the Taramsa section. Stratigraphie range: BOLLI (1957) recorded this species from the Paleocene of the lower Lizard Springs formation in Trinidad, where he considered it to range through the G. pseudome nardii - G. velascoensis zones. This species was also recorded from the Paleocene of the Gulf and Atlantic Coastal Plain and in New Jersey Coastal Plain (LOEBLICH & TAPPAN, 1957; OLSSON, I960). HILLEBRANDT (1962) found this species in zone "P" in the basin of Reichenhall and Salzburg, which he considered to be a Landenian age.