Palaeozygopleura prantli Horný, 1955
publication ID |
https://doi.org/ 10.11646/zootaxa.3669.4.3 |
publication LSID |
lsid:zoobank.org:pub:CD30BE63-C779-45CD-A25E-D633BBC0B9FF |
DOI |
https://doi.org/10.5281/zenodo.6165364 |
persistent identifier |
https://treatment.plazi.org/id/03F687FA-C540-C25D-FF3E-FB8900C8FE2F |
treatment provided by |
Plazi |
scientific name |
Palaeozygopleura prantli Horný, 1955 |
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Palaeozygopleura prantli Horný, 1955
Holotype. NMP 34882 (Horný 1955: pl. VI, fig. 5).
Paratype. NMP 34883 (Horný 1955: pl. VI, fig. 6), 80 unnumbered specimens, NMP. Type locality. Section in small quarry NE of the village of Holynĕ and W of the Prastav quarry (50°1'57.627"N, 14°21'5.471"E).
Type horizon. Uppermost part of the Třebotov Limestone (Daleje-Třebotov Formation); the latest Emsian to early Eifelian, Middle Devonian.
Remarks. Horný (1955: 128) considered P. prantli to be closely related and a younger form of P. bohemica . However, P. prantli comes from the same stratigraphic level as P. bohemica . In addition, both species have hitherto only been known from their type locality from where the fossil material collected by Mr. V. Plas and Mr. F. Hanuš was later used by Horný (1955). Detailed morphometric analysis of the both taxa is a subject of on-going study. Stratigraphic and geographic distributions. This species is only known from its type horizon and locality.
No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.
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