Orania cf. bellardiana ( Foresti, 1884 )
publication ID |
https://doi.org/ 10.11646/zootaxa.5295.1.1 |
publication LSID |
lsid:zoobank.org:pub:F3A52660-70B8-439F-A7A0-F45ADC975EA5 |
DOI |
https://doi.org/10.5281/zenodo.7975970 |
persistent identifier |
https://treatment.plazi.org/id/03CF879C-2C58-090F-FF1D-FBFAFBF6721B |
treatment provided by |
Plazi |
scientific name |
Orania cf. bellardiana ( Foresti, 1884 ) |
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Orania cf. bellardiana ( Foresti, 1884)
Plate 5 F View PLATE 5 1 -F View PLATE 1 2 View PLATE 2
cf. * Pollia bellardiana Foresti, 1884: 304 , pl. 1, fig. 2.
cf. Pollia bellardiana Foresti, 1884 — Ceregato et al. 2010: 56, pl. 1, figs. 10-12.
cf. Orania bellardiana ( Foresti, 1884) — Brunetti & Cresti 2018: 74, fig. 267.
Santa Maria material examined. Maximum height 17.0 mm, width 12.0 mm. DBUA-F 828-2 (1), Ponta dos Frades, Santa Maria Island, Azores, Touril Complex, Lower Pliocene.
Discussion. The single specimen from Santa Maria is too poorly preserved to offer a description. Orania fusulus ( Brocchi, 1814) , from the Upper Miocene to present-day Mediterranean and eastern Atlantic from Portugal to Angola, including the oceanic islands of Azores, Madeira, and Canary Islands, is slenderer, with a longer siphonal canal. Orania turrita ( Borson, 1821) has a similarly short siphonal canal, but is squatter, broader with a more scalate spire. In profile, the Azorean specimen is most like O. bellardiana ( Foresti, 1884) from the Lower Pliocene of Italy. That species had not been refigured since its original description until recently ( Ceregato et al. 2010: pl. 1, figs. 10- 12; Brunetti & Cresti 2018: fig. 267). Better preserved material would be needed to confirm this identification.
Distribution. Lower Pliocene: Atlantic, Santa Maria Island, Azores (this paper).
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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SuperFamily |
Muricoidea |
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SubFamily |
Ergalataxinae |
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