Complexodus originalis Chen &Zhang, 1984 from the Mójcza Limestone.

Diagnoza

An almost straight external branch of the posterior process of the sp elements, which have denticles with sharp tips.

Porównanie

Autekologia

Występowanie geograficzne

Zasięg czasowy

In China the species occurs from the E. reclinatus Subzone to the P. anserinus
Zone (CHEN and ZHANG 1984); according to AN (1987 ) its ancestor is Amorphognathus complexoides AN. In Mójcza it appear s 1.1 m below the bentonite (E. lindstroemi Subzone), 0.2 m below the bentonite it is replaced by C. pugionifer but seems to reappear 1.0 m above and continue up to 1.7 m
above the bentonite (A . tvaerensis 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