Zospeum njunjicae Jochum, Schilthuizen & Ruthensteiner, 2024
publication ID |
https://doi.org/ 10.5852/ejt.2024.926.2469 |
publication LSID |
lsid:zoobank.org:pub:A00D7669-2151-46AE-A066-9AF4D0F2BEEE |
DOI |
https://doi.org/10.5281/zenodo.10854259 |
persistent identifier |
https://treatment.plazi.org/id/F762D981-D8FB-4EE7-BB0F-489E3D596A04 |
taxon LSID |
lsid:zoobank.org:act:F762D981-D8FB-4EE7-BB0F-489E3D596A04 |
treatment provided by |
Plazi |
scientific name |
Zospeum njunjicae Jochum, Schilthuizen & Ruthensteiner |
status |
sp. nov. |
Zospeum njunjicae Jochum, Schilthuizen & Ruthensteiner View in CoL sp. nov.
urn:lsid:zoobank.org:act:F762D981-D8FB-4EE7-BB0F-489E3D596A04
Fig. 11 View Fig , 22A–B View Fig
Diagnosis
The smallest species of southern Balkan Zospeum , ca 1.2 mm, conical with 5 regularly coiled irregularly formed whorls; protoconch askew; peristome heavily callused on basal columellar side with a low, blunt, more or less conspicuous denticle some distance inside; columella centrally aligned, moderately thick, swollen at base; low lamella; well-defined umbilical depression.
Etymology
This species is dedicated to the biospeleologist and collector, Iva Njunjić.
Type material
Holotype
MONTENEGRO • ( Fig. 11C–I View Fig ); Virpazar, Gornja Seoca , Golubova pećina ; 42.2093° N, 19.1306° E; 26 Jun. 2018; M. Schilthuizen and I. Njunjić leg.; in cave entrance; NMBE 572617 View Materials . GoogleMaps
Paratypes
MONTENEGRO • 2 specs; same collection data as for holotype; NMBE 572616 View Materials GoogleMaps • 2 specs; same collection data as for holotype; SMF 349426 About SMF GoogleMaps • 2 specs; same collection data as for holotype; NHMWMO-113651 GoogleMaps • 3 specs; same collection data as for holotype; TxEx-DU0018 GoogleMaps .
Description
MEASUREMENTS. Holotype: sh: 1.271 mm; sw: 0.914 mm; ah: 0.560 mm; aw: 0.578 mm; hlw: 0.811 mm; SA: 69.69 deg. Paratypes (N = 2): sh: 1.214 –1.248 mm; sw: 0.944 –0.947 mm; ah: 0.578 –0.588 mm; aw: 0.507 –0.524 mm; hlw: 0.764 –0.790 mm; SA: 71.38–71.83 deg.; NMBE 572616.
Shell minute, ca 1.2 mm, conical, with 5 regularly coiled convex whorls; transparent when fresh, opaque when older; protoconch leans slightly left (frontal view); aperture reniform; teleoconch sculpture with few irregular and occasional course growth lines, last whorl weakly crossed by radial banding; some weak axial ribbing present immediately behind palatal lip; palatal rim narrowly reflected; peristome thickly callused, notch indentation at upper parietal and palatal junction pronounced, upper palatal side thin and expanded, columellar side oblique and angular with a low, blunt, more or less conspicuous denticle inside; parietal shield thickly callused, long and straight, extending beyond half of height of last whorl; last whorl height about half of shell height ( Fig. 11E View Fig ), last whorl tightly coiled and almost disappearing under spire at last ⅓ of coiling (apical view); upper rim of peristome recedes ca 1/6 the width of the penultimate whorl (aperture facing left); columella centrally aligned, moderately thick ( Fig. 11E View Fig ), lamella loosely coiled on columella under penultimate whorl; umbilical depression callused, puckered; columellar side of peristome arches high over with curvature of whorl on top of umbilical depression, alignment of last 1/4 whorl is not compact.
Distribution
This species is only known from its type locality cave, Golubova pećina in southwestern Montenegro.
Remarks
This species differs from all others in that it demonstrates the smallest shells of the Southern Balkan region so far. The columella is more robust than that of Z. troglobalcanicum and the lamella comprises a low bulge rather than an incomplete thread atop of the columella directly under the penultimate whorl as in Z. troglobalcanicum . The columella of this species is also unevenly contoured with a few low humps due to the tight twisting of the inner coiling.
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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