Diagnoza

Oval platform of P₁ elements with prominent narrow extension of the posterior lobe.

Porównanie

Elements of the kind attributed to the apparatus of this species by Metzger do not occur in the Holy Cross Mountains (perhaps this is a partial apparatus of a new species of Syncladognathus) and a different composition is suggested here, although the evidence remains very weak. P₁ elements are extremely variable in Wietrznia (Wtr-27), ranging from an outline resembling that of K. triangularis to that of K. circularis

Autekologia

Występowanie geograficzne

Płucki, Wietrznia, Karczówka, and Jabłonna.

Zasięg czasowy

late K. triangularis and the early K. crepida Zones. 

Materiały muzealne

ZPAL: 236 specimens.

Literatura

Dzik, J. 2006. The Famennian "Golden Age" of conodonts and ammonoids in the Polish part of the Variscan sea. Palaeontologia Polonica 63, 1-359.