Travunijana tribunicae ( Schütt, 1963 ) Grego, 2020
publication ID |
https://doi.org/ 10.5852/ejt.2020.691 |
publication LSID |
lsid:zoobank.org:pub:CC8487E0-169D-4B32-A2AB-F9B34DFB3F3B |
DOI |
https://doi.org/10.5281/zenodo.4336036 |
persistent identifier |
https://treatment.plazi.org/id/039F7945-8409-FFDC-BFD7-FBE764B82127 |
treatment provided by |
Valdenar |
scientific name |
Travunijana tribunicae ( Schütt, 1963 ) |
status |
comb. nov. |
Travunijana tribunicae ( Schütt, 1963) View in CoL comb. nov.
Figs 13C View Fig , 14 View Fig C–D
Plagigeyeria tribunicae Schütt, 1963: 208–209 View in CoL , figs 4–7.
Plagigeyeria tribunicae View in CoL – Schütt 1972: 116, 123, pl. 8. figs 21–22. — Willmann & Pieper 1978: 126 — Bole & Velkovrh 1986: 202 — Bodon, Manganelli & Giusti 1996: 33, fig. 13. — Bank 2013. Fauna Europaea v. 2.6 — Bank & Neubert 2017: 25
Diagnosis
Flat discoid shell 1.9–2.5 mm high with prominent body whorl having angled basal keel at its lower part and an ear-shaped aperture. Spire height variable, from entirely flat to elevated broad conical shape. Shell shape unique within the genera Travunijana and Plagigeyeria . Lateral labral profile straight and columellar labrum possesses a weak sinuation. Protoconch surface regularly and deeply pitted.
Distribution
Only known from the springs of Trebišnjica River (342 m a.s.l.) in Bileća (Schütt 1972), currently flooded under the lake behind the Grančarevo Dam (Bilećko Jezero). The Trebišnjica River springs represent a rather complicated hydrological drainage pattern. Most of the springs receive their water supplies from Gatačko Polje (936 m a.s.l.), Cerničko Polje (816 m a.s.l.) and partly through Fatničko Polje (452 m a.s.l.), but at least two of the springs, Vrelo “Oko” and Nikšićko Vrelo, collecting also the interim divergent groundwaters from Northern Nikšićko Polje (643 m a.s.l.).
Remarks
The distinct shells of T. tribunicae ( Schütt, 1963) detected in the subsidiary spring of the Trebišnjica (Nikšićko Vrelo, 342 m a.s.l.), show a remarkable variability in spire height from flat to pyramidal form (Schütt 1972). Unfortunately the type locality is currently flooded by the Grančarevo Dam, and it is questionable whether the lake had altered the subterranean aquifer water streams in a negative way leading to the species’ extinction, or if the species might still have survived in some other part of the aquifer. The shell morphology with dominant body whorl and keeled umbilicus significantly resembles the Plagigeyeria sp. morphotypes found at the north-western edge of Nikšićko Polje ( Montenegro, 643 m a.s.l.), confirming the transboundary communication of aquifers at least during high groundwater periods. However, the pitted protoconch structure is more similar to that of the genus Travunijana . The slightly reflexed margin is unique in the genus Travunijana and its position within this genus is only provisional. Based on the conditions of empty shells, the habitat is most likely upstream inside the undiscovered cave system, far from the actual spring water outlet (recently under the Bilećko Jezero) where the empty shells were collected.
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Genus |
Travunijana tribunicae ( Schütt, 1963 )
Grego, Jozef 2020 |
Plagigeyeria tribunicae
Bank R. A. & Neubert E. 2017: 25 |
Bodon M. & Manganelli G. & Giusti F. 1996: 33 |
Bole J. & Velkovrh F. 1986: 202 |
Willmann R. & Pieper H. 1978: 126 |
Plagigeyeria tribunicae Schütt, 1963: 208–209
Schutt H. 1963: 209 |