Klapperilepis triangularis
Sugerowana cytacja: Dzik, J 2013. Klapperilepis triangularis (Sannemann, 1955) . Ikonoteka (http://ikonoteka.paleo.pan.pl/xwiki/bin/viewrev/Species/Klapperilepis+triangularis+)
Diagnoza From its abcestor, K. ultima, differs in more elongated P1 elements and M elements usually with relatively wide angle between processes, from successors of various lineages in underived, lambda-shaped M elements. 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 distinctly higher than in K. ultima, remaining elements of the apparatus being hardly distinguishable. In fact, to distinguish these chronospecies a large sample is needed and single elements are of little taxonomic value. Some late populations 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, Kadzielnia, Kostomłoty, Śluchowice, Psie Górki, Dalnia, Górno, Karczówka, Kowala, and Wietrznia in the Holy Cross Mts.; borehole near Siewierz in Upper Silesia 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. Nehring, M. 1967. Konodonty dolnego famenu z profilu Winowno w okolicach Siewierza (Wyżyna Śląsko−Krakowska). Biuletyn Instytutu Geologicznego 209, 113–169. Szulczewski, M. 1971. Upper Devonian conodonts, stratigraphy and facies development in the Holy Cross Mts. Acta Geologica Polonica 21, 1-129. Wolska, Z. 1967. Górno-dewońskie konodonty z południowo-zachodniego regionu Gór Świętokrzyskich. Acta Palaeontologica Polonica 12, 363-435. Sannemann, D. 1955. Beitrag zur Untergliederung des Oberdevons nach Conodonten. Neues Jahrbuch für Geologie und Paläontologie, Abhandlungen 100, 324-331. |
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