Opis

Apparatus composed of simple coniform elements of approximately uniform size with smooth gradation of shapes and flattened cusps, forming a single symmetry transition series.
The family differs from the Belodellidae and Panderodontidae in the lack of any prominent size gradient in the apparatus, from the Scolopodontidae in less robust appearance of elements and from the Protopanderodontidae in having only a single symmetry transition series in the apparatus. 

Synonimy
Cornuodontidae Stouge, 1984

Zasięg czasowy

Literatura

Stouge S, Bagnoli G. 1990. Lower Ordovician (Volkhovian–Kundan) conodonts from Hagudden, northern Öland, Sweden. Palaeontographica Italica 77, 1–54.

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.