Hemilistrona pulchra


Sugerowana cytacja: Dzik 2015. Hemilistrona pulchra Chauff & Dombrowski 1977. Ikonoteka (http://ikonoteka.paleo.pan.pl/xwiki/bin/viewrev/Species/Hemilistrona+pulchra+)

Diagnoza

Porównanie

Longitudinal ribs on the platform of Pelements characterize this species. Outside Missouri, it has been known from Thuringia. In the Holy Cross Mountains only a few elements have been found and they hardly offer anything new regarding the apparatus composition. In sample Ko-6 two Pelements of different ontogenetic age are associated. Both show an unusually low and sinusoidal blade and are lacking a free carina (blade), suggesting that this is the end-member of the lineage, well represented in the material of Chauff and Dombrowski (1977).

Autekologia

Występowanie geograficzne

Kowala.

Zasięg czasowy

L. styriacus and P. jugosus Zones. 

Materiały muzealne

ZPAL: 14 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
Hemilistrona

Gatunek
Hemilistrona pulchra

Synonimy

Populacja typowa gatunku

Holotyp

Locus typicus

Sulphur Springs Formation near Pevely, Missouri.

Stratum typicum

Basal shale member, lower costatus Zone 


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Created by Administrator on 2015/05/18 14:45

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