Mehlina lunaria Dzik, 2006
Sugerowana cytacja: Dzik 2015. Mehlina lunaria Dzik 2006. Ikonoteka (http://ikonoteka.paleo.pan.pl/xwiki/bin/view/Species/Mehlina+lunaria+)
Diagnoza Whole P1 element transformed into elaborate peniculus built of bifurcating lateral processes radiating from the center of element. Porównanie This is a commonly occurring species with bizarre elements. This species was reported from the K. crepida Zone of the Frankenwald, from coeval strata at Jabłonna in the Holy Cross Mountains. At first glance it does not resemble a conodont at all. When seen from the base it shows bifurcation of lateral processes that resulted in developing so unusual pattern of the peniculus. Also the basally pointed outline in lateral view is consistent with the characterictic appearance of P1 elements of Mehlina. A peniculus developed widely in other members of the Mehlina-Polynodosus branch, as well as in the possibly related Frasnian Ancyrodella and the difference between them and M. lunaria is actually not great. An almost complete gradation can be assembled. The relatively stable morphology of P1 elements of M. lunaria sp. n. (shown by both mine and earlier published specimens) and the morphologic gap between its morphology and variability expressed by other known peniculi indicates that this is a separate species. Autekologia Występowanie geograficzne Kadzielnia. Zasięg czasowy The K. crepida Zone. Materiały muzealne ZPAL: 2 specimens. Literatura Dzik, J. 2006. The Famennian "Golden Age" of conodonts and ammonoids in the Polish part of the Variscan sea. Palaeontologia Polonica 63, 1-359. |
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