Guizhoudella triangularis Wang et Wang, 1978 from the P. jugosus Zone at Ostrówka (sample Ost-185 and Ost-265), the K crepida Zone at Jablonna (sample J-46, bed 27, sample J-66), the late K. triangularis Zone at Wietrznia (sample Wtr-27) in the Holy Cross Mountains, and the P. jugosus Zone at Dzikowiec (sample Dz-8) in the Sudetes; specimens ZPAL cXVI/1806, 1808, 1775, 1807, 1809-1811, 1862, 1909, 1901, 1861and 1892.

Diagnoza

Elements with thin walls of the very deep basal cone, strongly curved cusps; sharp, numerous denticles.

Porównanie

The holotype of the type species represents an S₁ element. S_3-4 elements from the same sample were named Belodella bilinearis. This is so bizarre a conodont that identification of its elements does not cause any difficulties, even if they are very rare in samples. Some specimens resemble P elements of typical prioniodinids but variability is so wide that recognition of discrete element types may not be possible.

Autekologia

Występowanie geograficzne

The L. styriacus to D. trigonica Zones at Jabłonna, Kowala, Ostrówka, and Dzikowiec.

Zasięg czasowy

Materiały muzealne

ZPAL: 28 specimens.

Literatura

Dzik, J. 2006. The Famennian "Golden Age" of conodonts and ammonoids in the Polish part of the Variscan sea. Palaeontologia Polonica 63, 1-359.