. Bulletin of the British Museum (Natural History), Geology. 248 CLEEVELY & MORRIS. Fig. 6 Austrian cassiopids. 1, Cassiope kefersteinii (Muenster in Goldfuss, 1844). Gosauschichten, Upper Coniacian; Drei- stetten no. 5; Fiirst colln (19F), Naturhistorisches Museum, Vienna; x 0-9. 2, 3, specimens from Bed f, Zottbach, Brandenberg, Austria; colld N. J. Morris, June 1985. 2, Cassiope ? kefersteinii var.; BMNH , x 11. 3, Cassiope bicostata (Mennessier); BMNH , x 10. 4, 5, Cassiope suffarcinata (Muenster in Goldfuss, 1844). 4, ? cf. coquandiana (Zekeli); BMNH , xO-95; G
. Bulletin of the British Museum (Natural History), Geology. 248 CLEEVELY & MORRIS. Fig. 6 Austrian cassiopids. 1, Cassiope kefersteinii (Muenster in Goldfuss, 1844). Gosauschichten, Upper Coniacian; Drei- stetten no. 5; Fiirst colln (19F), Naturhistorisches Museum, Vienna; x 0-9. 2, 3, specimens from Bed f, Zottbach, Brandenberg, Austria; colld N. J. Morris, June 1985. 2, Cassiope ? kefersteinii var.; BMNH , x 11. 3, Cassiope bicostata (Mennessier); BMNH , x 10. 4, 5, Cassiope suffarcinata (Muenster in Goldfuss, 1844). 4, ? cf. coquandiana (Zekeli); BMNH , xO-95; Gams, Steiermark; purchd from Dr A. Krantz. 5, EM 30423, xO-5; 'Gosau'; formerly in Ecole des Mines, Paris and now in Dept des Sciences de la Terre, Lyon; De Verneuil colln. 6, Cassiope lanzingensis (Mennessier, 1984). BMNH , xO-7; Lanzing, Miesenbach; colld N. J. Morris, June 1985. 7, Cassiope suffarcinata (Muenster in Goldfuss, 1844). BMNH (ex ), xO-9; lectotype of Araratella (Quadriglauconia) conoidea (J. de C. Sowerby, 1832, non Lamarck 1824) Mennessier, 1984; 'Gosau'; Murchison colln. See also Fig. , 3. invalid conoideum J. de C. Sowerby] as species of Cassiope, and believe that several other described species are merely synonyms of these. (A Neotype of C. suffarcinata was selected by Mennessier (1984: 42, 141; pi. 9, figs 9a-c) from the material in the collections of the Geological Survey of Austria, Vienna.) We are uncertain whether the form shown here (Figs and ), obtained from underneath the coral-rudist bed at Lanzing and described as Hexaglauconia (//.) lanzingensis Mennessier, is distinct from C. suffarcinata. It is ornamented by evenly-distributed noded spiral cords, in contrast to the more closely-packed cords present on the type of suffar- cinata 1 = conoideum], but is very similar to the forms of the latter shown in Fig. 3. Lack of sufficient material prevents us from considering the species giebeli and gamsensis (which Mennessie
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