Cornuodus bergstroemi
Sugerowana cytacja: Moczyński 2017. Cornuodus bergstroemi Serpagli 1967. Ikonoteka (http://ikonoteka.paleo.pan.pl/xwiki/bin/viewrev/Species/Cornuodus+bergstroemi)
Diagnoza The P2 elements with a strongly convex profile of the base, gracile elements with obliquely cut bases and angularly bent cusps. Porównanie Elements of the species are generally more gracile than those of C. longibasis, their most characteristic feature is the shape of their bases. Autekologia Występowanie geograficzne Baltic area and the Carnic Alps. Zasięg czasowy Llanvirn (Baltic area), Ashgill (Carnic Alps), from 0.5 m above the discontinuity (E.robustus Subzone) to 1.2 m above the bentonite (A. tvaerensis Zone)(Mójcza). 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. |
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