Dapsilodus viruensis (Fåhræus, 1966) from the Mójcza Limestone.

Diagnoza

Elements ornamented with longitudinal striae, usually best developed close to the panderodont furrow, external margins smooth.

Porównanie

The size of the elements increases significantly through the Mójcza section from the appearance of the species up to typical populations and following. The oldest known specimens are more robust than typical ones, with shorter cusps and oval cross-section. In this respect they somewhat resemble Cornuodus elements.

Autekologia

Występowanie geograficzne

Międzygorz and Zalesie in the Holy Cross Mts. Also the Baltic area and South China.

Zasięg czasowy

From 0.8 m below the discontinuity (L. variabilis Zone) up to l,4 m above the
bentonite (A. tvacrensis Zone)

Materiały muzealne

ZPAL

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.