Eoplacognathus elongatus (Bergstrom, 1962)
Sugerowana cytacja: Moczyński 2018. Eoplacognathus elongatus (Bergstrom, 1962) Ikonoteka (http://ikonoteka.paleo.pan.pl/xwiki/bin/view/Species/Eoplacognathus+elongatus)
Diagnoza The sp elements with the outer and inner processes meeting at an angle in the center of the elements, which results in a star-s haped appearance. The oz elements Y-shaped , with a wide platform. Synonims: Amorphognathus elongata n. sp.: BERGSTROM, 1962; Eoplacognathus elongatus (BERGSTROM); BERGSTROM, 1971; Eoplacognathus elongatus (BERGSTROM); DZIK, 1976; Eoplacognathus elongatus (BERGSTROM); BARRETTet al ., 1983; Eoplacognathus elongatus (BERGSTROM); BERGSTROM and ORCHARD, 1985. Porównanie Autekologia the Tvaren area, Sweden. Występowanie geograficzne Zasięg czasowy The presumably oldest specimen from Mójcza has been found in sample MA-74,n 0.7 m above the bentonite, but undisputable occurrences are from 1.0 to 1.5 m above the bentonite. 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. |
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