Palaeozygopleura chlupaci Frýda, 1993
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.6165356 |
persistent identifier |
https://treatment.plazi.org/id/03F687FA-C545-C259-FF3E-F8BA0785F849 |
treatment provided by |
Plazi |
scientific name |
Palaeozygopleura chlupaci Frýda, 1993 |
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Palaeozygopleura chlupaci Frýda, 1993
Holotype. UUG JF 50 (Frýda 1993: figs 2.1–2.3, 2.6, 2.7).
Paratypes. UUG JF 51–54 (Frýda 1993: figs 2.5, 2.6).
Type locality. Koukolová Hora hill near Beroun, Barrandian area, central Bohemia (49°55'18.346"N, 14°1'13.357"E).
Type horizon. Monograptus uniformis graptolite Biozone, Early Lochkovian, Early Devonian.
Remarks. Palaeozygopleura chlupaci is hitherto the oldest species of the genus. The first occurrence of Palaeozygopleura is connected with a period of global increase of δ13C in the marine ecosystem, known as the Klonk Event (Manda & Frýda 2010), which was followed by a rapid occupation of the free water column by different animal groups, an increase of free-swimming predators as well as distinct changes in the plankton composition (Nützel & Frýda 2003; Berkyová et al. 2007; Klug et al. 2010).
Stratigraphic and geographic distributions. Besides from its type locality and the "Nad roklí" section near Černá rokle Gorge (SW Prague; Frýda & Manda 1997), this species has been newly recorded from the Pod Kotýsem section (W of the village of Konĕprusy).
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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