Diagnoza

The external crista of the ne elements strongly inclined posteriorly above the base, forms a wide furrow. Elements of the main symmetry transition series smooth, their cusps rich in white matter.

Porównanie

Mature elements of D. kielcensis are much smaller than those in associated species of the genus . They differ also in a whitish coloration and thicker cusps of the ne elements .

Autekologia

Występowanie geograficzne

Mójcza Limeston

Zasięg czasowy

The species occurs below the discontinuity surface, that is in the Early Kundan L. variabilis Zone.

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.