Polynodosus triphyllatus


Sugerowana cytacja: Dzik 2015. Polynodosus triphyllatus Ziegler 1962. Ikonoteka (http://ikonoteka.paleo.pan.pl/xwiki/bin/viewrev/Species/Polynodosus+triphyllatus+)

Diagnoza

Platform of Pelement strongly constricted in the midlength.

Porównanie

According to Helms (1961) and Vorontzova (1993) a few chronospecies of polygnathids with ornate platform preceded this species in its lineage. In my material there seems to be a continuity between P. confluens and P. triphyllatus and gradual increase in depth of platform constriction, the character highly variable within each sample.

Juvenile elements described as Polygnathus cf. P. diversus by Metzger (1994), who identified Pelements and illustrated their ontogeny, probably belong to a population transitional between P. confluens and P. triphyllatus, as suggested by co-occurrence with mature Pelements.

Nomenclatorial problems connected with this species have been discussed by Glenister and Klapper (1966, p. 834).

Autekologia

Występowanie geograficzne

Kowala, Łagów and Miedzianka.

Zasięg czasowy

C. quadrantinodosa to C. marginifera Zones. 

Materiały muzealne

ZPAL: 1,106 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.

Specyfikacja

Królestwo
ANIMALIA 

Typ
CHORDATA 

Podtyp
CONODONTA

Gromada
CONODONTOPHORIDA

Podgromada
EUCONODONTA

Rząd
Ozarkodinida

Podrząd
Ozarkodinina

Rodzina
Polygnathidae

Rodzaj
Polynodosus

Gatunek
Polynodosus triphyllatus

Synonimy

Populacja typowa gatunku

Holotyp

Locus typicus

Rhenish Slate Mountains.

Stratum typicum

Pebble in the late Permian conglomerate of Rossenray.


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Created by Administrator on 2015/05/13 15:19

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