Scabbardella altipes (Henningsmoen, 1948) from the Mójcza Limestone.

Diagnoza

Apparatus composed of flattened, smooth elements with an elongated triangular
outline of the basal part and showing an almost continuo us variability in shape within single symmetry transition series; all the elements being asymmetric. The ne elements differ from the remaining ones only in their more triangular lateral outline . They bear the panderodont furrow, which occurs also in some other element types.

Porównanie

Autekologia

Występowanie geograficzne

Mójcza,similarly in Międzygórz and Zalesie.

Zasięg czasowy

A dominant species of the Late Ordovician Hamarodus fauna. In Mójcza it appears 0.9 m below the bentonite (P. anserinus Zone) and continues to the top of the section in the Zalesie Formation

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.