Teremitra
publication ID |
https://doi.org/ 10.11646/zootaxa.3754.3.2 |
publication LSID |
lsid:zoobank.org:pub:9E645014-5464-4E7C-8D4A-0B3B52A5AA53 |
DOI |
https://doi.org/10.5281/zenodo.5676798 |
persistent identifier |
https://treatment.plazi.org/id/0F4E87BB-7B2C-FFA0-FF22-FC1DA4FCFA23 |
treatment provided by |
Plazi |
scientific name |
Teremitra |
status |
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Teremitra View in CoL ? hortensis (Vinassa de Regny, 1898) comb. nov.
Figures 2 View FIGURE 2 Q, 17A–C
Cerithium hortense Vinassa de Regny, 1898: 191 [149], pl. 20 [7] fig. 33a–b.
Cerithium rectum Vinassa de Regny, 1898: 192 [150], pl. 20 [7] fig. 34a–b, syn. nov. Cerithium (Lovenella?) hortense Vinassa de Regny—Oppenheim 1901: 206, pl. 20 fig. 7–7a Cerithium (Lovenella?) rectum Vinassa de Regny—Oppenheim 1901: 206, pl. 20 fig. 1–1b. Cerithium hortense Vinassa de Regny—Boussac 1911: 49, pl. 11 fig. 13.
Locality/Age. Upper Eocene (Priabonian) of France (Aquitaine Basin) and Italy.
Remarks. We only tentatively classify Cerithium hortense in Teremitra . The species does not fit well in Pyramimitra and Vaughanites , the two fossils genera also having columellar plaits, but strongly differing in sculpture. However, we have only observed young specimens of this species. Full adult specimens (see Boussac 1911, pl. 11 fig. 13) have a slender spire and are in fact quite similar to T. efatensis . The two species have a slender spire, three spiral cords forming nodules on spire whorls, and two pronounced columellar plaits. The siphonal canal of T. hortensis is, however, not as short and broad as in T. efatensis .
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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Teremitra
Kantor, Yuri, Lozouet, Pierre, Puillandre, Nicolas & Bouchet, Philippe 2014 |
Cerithium hortense
Regny 1898: 191 |