Szabó János szerk.: Fragmenta Mineralogica Et Palaentologica 21. 2003. (Budapest, 2003)
Nodosaria. setosa (HANTKEN, 1875) (Plate I: 11, Plate II: 11) 1875a Dentalina setosa n. sp. — HANTKEN, S. 39, Taf. XIII, Fig 9. 1875b Dentalina setosa — HANTKEN, p. 33, pl. XIII, fig. 9. 1962 Dentalina setosa HANTKEN — MAJZON, pl. XLI(XIII), fig. 9. 1979 Dentalina setosa HANTKEN — SZTRÁKOS, pl. 11, fig. 10. Neotype — M.Ol.17. Type locality — Budapest, Újlak. Type level — Kiscell Clay Formation, Upper Kiscellian. Material — One specimen. Dimension — Length 0.6 mm, width 0.1 mm. Diagnosis — The elongate, uniserial test consists of only a few chambers. Proloculus is small and spherical, gradually increasing four or five chambers follow it. Short and wide neck connects the neighbouring chambers. The calcareous wall is ornamented by fine granulae. Aperture is terminal, rounded and developed on a neck. Remarks — HANTKEN described this species on the basis of a single specimen from the upper part of the Clavulina Szabói layers in the Kiscell Clay, Upper Kiscellian, Óbuda-Újlak (HANTKEN 1875 a-b). No specimen is preserved in the Hantken collections in Hungary. Stratigraphical range — In Hungary, this species occurs in the Kiscell Clay, Upper Kiscellian SZTRÁKOS (1979). SZTRÁKOS (2000) found a questionable form in the Upper Eocene in Aquitaine (France). Ecology — Nodosaria setosa may range from neritic to bathyal zone. Genus Pyramidulina FORNASINI, 1894 Pyramidulina minor (HANTKEN, 1875) (Plate V: 6) 1866b Nodosaria badllum — HANTKEN, p. 235 (in list) 1875a Nodosaria badllum DEFR. var. minor — HANTKEN, S. 26. 1875a Nodosaria latejugata DEFR. var. minor — HANTKEN, S. .21.Taf. II, Fig. 7. 1875b Nodosaria badllum DEFR. var. minor — HANTKEN, p. 21, pl. II, fig. 7. 1961 Nodosaria minor HANTKEN — KAASSCHIETER, p. 177, pl. VII, fig. 21. 1962 Nodosaria badllum HANTKEN — MAJZON, pi. XXX(II), fig. 7. 1970 Nodosaria barilla minor HANTKEN — KIESEL, S. 219, Taf. VII, Fig. 15. 1978 Nodosaria minor HANTKEN — SZTRÁKOS, pl. 9, fig. 5. 1979 Nodosaria minor HANTKEN — SZTRÁKOS, pi. 9, fig. 3. 1982 Nodosaria minor HANTKEN — SZTRÁKOS, pl. 5, fig. 13. Dimension — Length 4-6 mm (HANTKEN 1875a-b). Diagnosis — Test is elongate, uniserial. Chambers are globular and regularly increasing; orizontal sutures separate them. Wall is calcareous and perforate, 7—9 distinct, longitudinal ribs ornament it. Aperture is terminal and rounded. Remarks — P. minor differs from P. latejugata (GlJMBEL, 1868; S.619, Taf. I, Fig. 32.) in inflation of the chambers. No specimen remained in the Hantken collections. Stratigraphical range — In Hungary this species is rare, it has been found in the Oligoccene HANTKEN (1875 a-b), SZTRÁKOS (1979, 1982). In other parts of Europe, KAASSCHIETER (1961) and KIESEL (1970) recognised it in the Eocene. Subfamily Lingulininae LOEBLICH & TAPPAN, 1961 Genus IJngulina D'ORBIGNY, 1826. Lingulina glabra HANTKEN, 1875 (Plate I: 12, Plate II: 12) 1875b Lingulina glabra n. sp. — HANTKEN, S. 42. Taf. XIII, Fig. 14. 1875a Lingulina glabra — HANTKEN, p. 35, pl. XIII, fig. 14. 1956 Lingulina glabra HANTKEN — HAGN, S. 139, Taf. 13, Fig. 2. 1962 Lingulina glabra HANTKEN — MAJZON, pi. XLI(XII), fig. 14. 1971 Lingulina aff. glabra HANTKEN — POPESCU & IVA, pl. V, fig. 3 Lectotype — M.99.59. Type locality — Budapest, Vár-hegy. Type level — Buda Marl Formation, Upper Eocene. Material — One specimen (broken). Dimensions — Length 1.2 mm, width 0.8 mm. Diagnosis — Test is elongate, compressed and lenticular. The uniserially arrenged, overlapping chambers are rectilinear, their numbers are 5 to 7. Sutures are horizontal and slighdy depressed. Wall is calcareous, perforate, its surface is smooth. Aperture is a terminal slit in the plane of compression. Remarks — A single specimen has been preserved in the Hantken Collections in Hungary. Stratigraphical range — This species is known from the Eocene and Oligocène (HANTKEN 1875a-b HAGN 1956; POPESCU & IVA 1971). Ecology — There are no data on the distribution of IJngulina species.