Zadelsdorfia oblita sp. nov.
urn:lsid:zoobank.org:act: 97D9ABF0-4091-47B6-B631-F2B1DA85452D
Fig. 86; Table 80
Diagnosis
Species of Zadelsdorfia with a conch reaching 50 mm diameter. Conch at 30 mm dm thinly pachyconic, subinvolute (ww/dm ~0.70; uw/dm ~0.30). Whorl profile in the juvenile stage crescent-shaped, at 30 mm dm moderately depressed (ww/wh ~1.75); coiling rate low (WER ~1.60). Venter broadly rounded, umbilical margin narrowly rounded. Growth lines fine, wide-standing, with concavo-convex course. Weak constrictions on the shell surface and prominent internal shell thickenings; sharp, short ribs and coarse spiral lines on the inner flank.
Etymology
From the Latin ‘ oblita ’ = ‘forgotten’; because of the undescribed material in the Vöhringer collection.
Material examined
Holotype
GERMANY • Rhenish Mountains, Oberrödinghausen, railway cutting; Hangenberg Limestone, bed 1; Vöhringer Coll.; illustrated in Fig. 86; MB.C.31174.1.
Paratypes
GERMANY • 2 specimens; Rhenish Mountains, Oberrödinghausen, railway cutting; Hangenberg Limestone, bed 1; Vöhringer Coll.; MB.C.31174.2–3 .
Description
Holotype MB.C.31174.1 is a specimen that was already sectioned by Vöhringer, but no inner whorls are preserved (Fig. 86). The specimen has a diameter of 33 mm and is thinly pachyconic and subinvolute (ww/dm = 0.69; uw/dm = 0.29) with a rounded umbilical margin, a convex umbilical wall and broadly rounded flanks and venter. The specimen shows moderately well preserved shell remains that appear largely smooth. Weak spiral lines are visible on the flank; they cross the fine, wide-standing growth lines. The shell surface shows a concavo-convex constriction forming a shallow lateral sinus, a distinct ventrolateral projection and a moderately deep ventral sinus.
Remarks
Specimens of the new species were placed in Gattendorfia costata by Vöhringer (1960). However, clear differences are present: The holotype of G. costata has a rather wide umbilicus with a uw/dm ratio of 0.44 at 32 mm dm, while in Zadelsdorfia oblita sp. nov. it is only 0.29. Furthermore, G. costata has a pronounced umbilical margin, which is rounded in Z. oblita .
Zadelsdorfia oblita sp. nov. differs from all other species of the genus known from the Hangenberg limestone of Oberrödinghausen by the combination of a pachyconic conch and internal shell thickenings, which show a distinct concavo-convex course. Another characteristic to distinguish Z. oblita from the other species is the presence of spiral lines.