Eoneoprioniodus alatus (Dzik, 1976) from the Mójcza Limestone.

Diagnoza

Porównanie

Only a single specimen, probably representing an oz element has been found in the sample MA-42. It closely resembles E. alatus occurring widely in coeval and younger strata of the Baltic region and North American Midcontinent . With no other element found any interpretation must remaintentative, however.

Autekologia

Występowanie geograficzne

Zasięg czasowy

Only in the bed immediately above the discontinuity. The specimen may be
reworked from slightly older strata.

Materiały muzealne

Literatura

Dzik, J. 1994a Conodonts of the Mójcza Limestone. In: J. Dzik, E. Olempska, & A. Pisera. Ordovician carbonate platform of the Holy Cross Mountains. Palaeontologia Polonica 53, 43-128.