Diagnoza
P1 elements relatively elongated and M elements usually with relatively wide angle between processes. Porównanie
A variable species, both in respect to the outline of platform in P1 elements, which ranges from that typical to K. ultima to that of early species of Palmatolepis, but also in the prominence of the cusp and curvature of P2 elements. The mean value of elongation index of the P1 elements is, however, distinctly higher than in K. ultima (Dzik 2002, 2004), remaining elements of the apparatus being hardly distinguishable. In fact, to distinguish these chronospecies a large sample is needed and singler elements are of little taxonomic value. Some late populations (e.g., Pł-1; Fig. 80H-R) show robust denticulation of ramiform elements and widely angular processes of the M element Autekologia
Poorly recognised; apparently an open-sea species. Występowanie geograficzne
Płucki, Karczówka, Kowala, and Wietrznia. Zasięg czasowy
Zone of its own. Materiały muzealne
ZPAL: 422 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. |