Diagnoza

Porównanie

Late Ordovician population s of Panderodus in the Mójcza section differ from the preceding ones in having more gently curved, slender ne elements , more gracile appearance and
distinct striation of all elements, as well as in the lack of symmetrica l elements in the apparatus.

Autekologia

Występowanie geograficzne

The lower boundary of the occurrence is difficult to trace because of the rarity
and poor pre servation of the elements;bprobably appears 1.2 m above the bentonite (A. tvaerensis Zone) but typical forms occur much higher in the marly lime stones of the Zalesie Formation (A. ordovicicus Zone) in Mójcza, Miedzygórz, and Zalesie .

Zasięg czasowy

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.