Inadunata Wachsmuth and Springer, 1885

Głuchowski, Edward, Casier, Jean-Georges & Olempska, Ewa, 2006, Crinoid and ostracod succession within the Early-Middle Frasnian interval in the Wietrznia quarry, Holy Cross Mountains, Poland, Acta Palaeontologica Polonica 51 (4), pp. 695-706 : 697

publication ID

https://doi.org/ 10.5281/zenodo.13748684

persistent identifier

https://treatment.plazi.org/id/B318330E-9C4F-FFC0-067F-EC54634DFD2F

treatment provided by

Felipe

scientific name

Inadunata Wachsmuth and Springer, 1885
status

 

Subclass Inadunata Wachsmuth and Springer, 1885 Order Disparida Moore and Laudon, 1943 Family Haplocrinitidae Bassler, 1938

Haplocrinites sp. ( Fig. 3C, D View Fig ).—The aboral cup is wide and cupuliform with pentagonal outline in oral view. Radial facets are narrow, trapezoidal. Oral pyramid is as high as the calyx. The external surface of the oral plates is flat. The thecae are most similar to Haplocrinites stellaris ( Roemer, 1844) reported from Givetian–Frasnian Red Iron Horizon of the East Sauerland, Germany ( Roemer 1844; Sandberger and Sandberger 1850 –1856), but differ in having a relatively less elevated oral part. They differ from Haplocrinites gluchowskii Hauser, 2002 reported from Late Frasnian Detrital Beds of the Holy Cross Mountains ( Głuchowski 1993), Upper Wallersheim Dolomite of the Eifel Mountains, Germany ( Hauser 2002) and the Neuville Formation of the Dinant Basin, Belgium ( Hauser 2003) in having distinctly less prominent radial facets.

Loc

Inadunata Wachsmuth and Springer, 1885

Głuchowski, Edward, Casier, Jean-Georges & Olempska, Ewa 2006
2006
Loc

Haplocrinites gluchowskii

Hauser 2002
2002
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