Opis

The P1 elements are morphologically clearly distinct from the P2 elements (P3 may have developed), with at least a tendency to develop platform and a ramified anterior process.

Synonimy

Zasięg czasowy

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.