Scabbardella altipes (Henningsmoen, 1948)
Sugerowana cytacja: Moczyński 2017. Scabbardella altipes (Henningsmoen, 1948) Ikonoteka (http://ikonoteka.paleo.pan.pl/xwiki/bin/view/Species/Scabbardella+altipes)
 Diagnoza Apparatus composed of flattened, smooth elements with an elongated triangular outline of the basal part and showing an almost continuo us variability in shape within single symmetry transition series; all the elements being asymmetric. The M elements differ from the remaining ones only in their more triangular lateral outline. They bear the panderodont furrow, which occurs also in some other element types. Porównanie Autekologia Występowanie geograficzne Mójcza,Międzygórz and Zalesie. Zasięg czasowy A dominant species of the Late Ordovician Hamarodus fauna. In Mójcza it appears 0.9 m below the bentonite (P. anserinus Zone) and continues to the top of the section in the Zalesie Formation 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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