Diagnoza

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

Porównanie

Maturee lements 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

In the Mojcza Limestone

Zasięg czasowy

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

Materiały muzealne

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.