Branmehla bohlenana Helms, 1959
Sugerowana cytacja: Dzik 2014. Branmehla bohlenana Helms 1959. Ikonoteka (http://ikonoteka.paleo.pan.pl/xwiki/bin/view/Species/Branmehla+bohlenana+)
Diagnoza Elongated and rather robust P1 element with relatively low cusp. Porównanie The geologically oldest populations of Branmehla from Łagów closely resemble the earliest Famennian Pluckidina lipperti and that species is likely to be its ancestor. The main difference is in the morphology of the M element, which is higly arched in B. bohlenana. The transition from B. bohlenana to B. inornata is gradual and it is virtually impossible to delimit these species even if for most of their range they occur allopatrically. The species is rather variable, especially in respect to the denticulation of P1 elements. Denticles are wide and short, densely distributed in some specimens , or elongate and sparsely distributed in others. Autekologia Występowanie geograficzne Wietrznia, Łagów, Miedzianka, Kowala, Ostrówka, and Dzikowiec. Zasięg czasowy Possibly ancestral population in the K. crepida Zone , the typical form from the C. quadrantinodosa Zone to the end of the Famennian Materiały muzealne ZPAL: 1,664 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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