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

Diagnoza

Porównanie

Only a single specimen, probably representing a P₂ element has been found. 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 remain tentative, 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

ZPAL

Literatura

Dzik, J. 1994. 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.