Eoplacognathus lindstroemi (Hamar, 1964) from the Mójcza Limestone.

Diagnoza

In both elements of the P₂ pair the inner and anterior processes meet approximately at a right angle. In the P₁ elements the inner and outer processes are arranged almost linearly.

Porównanie

In Mójcza only a few elements have been found, so it is impossible to establish if there is a continuum with the preceding species of the lineage. A short barren interval separates it from E. reclinatus, each represented by rather few specimens.

Autekologia

Występowanie geograficzne

Mójcza; Baltic area and south China, also other temperate zone regions,

Zasięg czasowy

Specimens definitely belonging to the species occur from 1.5 m to 1.2 m below
the bentonite.

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.