Pseudooneotodus sp. from Mójcza limestone

Diagnoza

Porównanie

Elements of Pseudooneotodus of oval shape from the latest Ordovician are traditionally referred to as P. beckmanni. The material at hand is too small to make any taxonomic
decision.

Autekologia

Występowanie geograficzne

Mójcza, Holy Cross Mts.

Zasięg czasowy

In Mójcza the species occurs in the topmost layers of the outcrop (A. ordovicicus Zone, Ashgill), elsewhere known from strata of the same age.

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.