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. |