Bojozyga parallela (Horný, 1955), Horny, 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.6165336 |
persistent identifier |
https://treatment.plazi.org/id/03F687FA-C549-C255-FF3E-FF5005B8FC71 |
treatment provided by |
Plazi |
scientific name |
Bojozyga parallela (Horný, 1955) |
status |
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Bojozyga parallela (Horný, 1955)
Holotype. NMP 34877 (Horný 1955: pl. III, fig. 6).
Type locality. Hlubočepy, Prague 5 (50°2'24.549"N, 14°24'0.039"E).
Type horizon. Třebotov Limestone (Daleje-Třebotov Formation); upper Emsian-early Eifelian, Devonian.
Remarks. This species is based on fossil material collected by Mr. J. Bouška and its exact age is unknown. Only two shell fragments were gathered; a fragment having four whorls was selected as holotype. Horný (1955) noted the Choteč Limestone (Eifelian) as the type horizon for the species. However, Chlupáč (1959) later reevaluated its stratigraphic position and noted that this species came from the Třebotov Limestone of the Daleje- Třebotov Formation (upper Emsian-early Eifelian).
Stratigraphic and geographic distributions. Bojozyga parallela is only known from its type locality and horizon.
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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