Diagnoza

Elements subtriangular in occlusal view with the inner lobe delimited by shallow sinuses . Single cusp.

Porównanie

Autekologia

Występowanie geograficzne

In Mójcza the species occurs sporadically beginning from the level 0.4 m above the discontinuity surface (E. robustus Subzone; Late L1anvirn ) up to the top of the section. Known
also from other outcrops of the Mójcza Limestone and Zalesie Formation in Miedzygorz and Zalesie.
The species is reported to occurin England and other areas also in the Late Caradoc and Ashgill up to the base of the Himantian.

Zasięg czasowy

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.