Prestonella nuptialis ( Melvill & Ponsonby, 1894 )
publication ID |
https://doi.org/ 10.5281/zenodo.7910199 |
persistent identifier |
https://treatment.plazi.org/id/03ED8781-6A66-FD67-FE8F-FF0070A2FC7E |
treatment provided by |
Felipe |
scientific name |
Prestonella nuptialis ( Melvill & Ponsonby, 1894 ) |
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Prestonella nuptialis ( Melvill & Ponsonby, 1894) View in CoL View at ENA
Figs 8 View Figs 7, 8 , 12, 13 View Figs 12–15 , 16–18 View Fig View Figs 17, 18 , 20–24 View Figs 19, 20 View Figs 21–25 , 26–28 View Fig View Figs 27, 28
Buliminus nuptialis: Melvill & Ponsonby 1894: 92 , pl. 1, fig. 5. Type loc.: ‘ Craigie Burn, Somerset East’ ,
South Africa, leg. Mrs Mary Layard Barber [née Bowker].
Buliminus nuptialis: Sturany 1898: 602 .
Buliminus (Pachnodes) nuptialis: Kobelt 1902: 762 , pl. 111, fig. 22.
Ena nuptialis: Connolly 1912: 172 .
Prestonella nuptialis: Connolly 1939: 293 View in CoL .
Etymology: The origin of this somewhat unusual species name is explained by a note with the paratype at the RMCA, which states ‘found by goddaughter and sent to me on the eve of her wedding day’; the initials are unclear, but could well be E.L.L. of Edgar L. Layard, who was indeed Mary Bowker’s godfather.
Description ( Figs 8 View Figs 7, 8 , 12, 13 View Figs 12–15 ): Shell succineiform to bulimiform, thin; suture weakly to moderately indented. Aperture ovate to roundly D-shaped; upper part of columella lip reflected over umbilical region, but umbilicus remaining relatively widely patent; apertural rim obliquely tangential, and peristome thus in one plane; aperture without teeth, denticles or varices. Sculpture almost devoid of spiral elements (except on protoconch, see below), comprising only relatively strong, somewhat irregular rounded growth-ridges, strongest below suture and somewhat sinuous in this region.
Colour: Shell translucent when fresh, overlain by yellow-ochre to ochre-brown periostracum with irregular darker and lighter bands corresponding with growth-ridges; apex usually only slightly darker; periostracum and underlying shell often heavily eroded, particularly near apex; frequently with adherent particles of debris. Head-foot dark brown.
Dimensions: Length up to 15.5 mm, width up to 10.0 mm; adult L/W 1.37–1.69; body whorl length = 81.4–90.4% of shell length; aperture length = 48.2–62.9% of shell length (N=17).
Protoconch ( Fig. 8 View Figs 7, 8 ): Diameter 1.5–1.75 mm, comprising 1.75–2.0 whorls; basic shape similar to that of P. bowkeri , but lacking axial riblets; fine surface detail eroded in most specimens, but traces of microscopic spiral striae present in some; junction between protoconch and teleoconch usually not well defined.
Holotype: SOUTH AFRICA: Eastern Cape: BMNH 1905.1 .26.29, ‘ Craigie Burn’, Somerset East, J.H. Ponsonby Esq. [originally collected by Mrs Mary Layard Barber (née Bowker), and sent by E. L. Layard]; length 11.5 mm ( Fig. 12 View Figs 12–15 ).
Paratype: ‘ Craigie Burn’, Somerset East ( RMCA 26584 View Materials ) .
Type locality: The locality cited in the original description, ‘Craigie Burn’, is a farm on the eastern slopes of the Bosberg, south-east of the hill ‘Graskop’ and immediately north of ‘Avon Heights’ farm, co-ordinates 32°41.1'S: 25°40.7'E, altitude approx. 1000 m a.s.l.
Additional material examined: SOUTH AFRICA: Eastern Cape: Cradock area, Elandsberg Mountain (32°07.488'S: 25°42.348'E), approx. 1450 m a.s.l., just below summit, on southern slope, D. Herbert, M. Bursey & G. Redman, 23.i.2002 ( NMSA V9781 About NMSA ) GoogleMaps ; Cradock area, inselberg south of Tarkastad road, near ‘ Plankfontein’ farm (32°07.822'S: 25°47.795'E), 1530 m a.s.l., just below summit on south-facing slope, D. Herbert, M. Bursey & G. Redman, 24.i.2002 ( NMSA V9778 About NMSA ) GoogleMaps ; Cradock area, ‘found in narrow fissures in the rocks on the mountain tops’ (NMSA 1592); Cradock area, Elandsberg Mountain (W901and NMW) ; Cradock ( NMSA B117 About NMSA , V5275 About NMSA ) ; Cradock, J. Farquhar ( NMSA W437 About NMSA ) ; Cradock , ( RMCA 26585 View Materials and RBINS) ; Adelaide area, Fenella Falls (32.367°S: 26.367°E), in crevices in rocks behind high waterfall, M. Bursey, v.2007 ( NMSA W5507 About NMSA ) GoogleMaps .
Distribution ( Fig. 16 View Fig ): Endemic to South Africa, and recorded only from Eastern Cape province, in the environs of Somerset East and Cradock, and the Winterberge mountain range, at altitudes of 1000–1600 m a.s.l. In the Somerset East area it is only known from the type locality and has not been collected in this area since its description.
Habitat ( Figs 17, 18 View Figs 17, 18 ): Living specimens have recently been collected at two localities. Firstly near the summit of two ‘inselbergs’ in the Cradock area, and secondly at the Fenella Falls in the Winterberge.At the Cradock site, the specimens were found wedged in crevices and under overhangs in the near vertical face of a narrow band of reddish mudstone just below the summit of the mountains. The aspect was largely south-facing and thus for the most part shaded. The rock was mostly bare of superficial encrustations. A note stating ‘found in narrow fissures in the rocks on the mountain tops around Cradock’ associated with specimen lot NMSA 1592 indicates that W. Farquhar’s material cited by Connolly (1939) was collected in a similar habitat. In contrast, the Fenella Falls site closely resembled sites at which P. bowkeri has been found—a shaded, gorgelike habitat with a high waterfall, the snails being found in crevices in bare rock walls in the immediate environs of the waterfall. Nothing is known of the precise habitat in which the type specimens were collected at ‘Craigie Burn’.
As with the habitat of P. bowkeri , orographic phenomena associated with these sites will mean that they provide moister habitats than those of the surrounding landscape matrix. In overcast weather, the tops of Karoo inselberg mountains frequently project into the cloud layer (as they did when the Cradock material was collected, Fig. 17 View Figs 17, 18 ) and thus will be subject to moist conditions, while the intervening, lower-lying land remains dry and typical of the Nama Karoo biome ( Low & Rebelo 1996).Although not measured, the temperature near the Elandsberg summit was significantly cooler, and made more so by wind.At Fenella Falls, mist associated with the Winterberge mountains combined with wind-blown spray from the waterfall and the shaded aspect of the habitat are likely result in relatively mesic conditions.
Notes: Differs from P. bowkeri in being smaller and generally broader with more convex whorls (but adult L/W ratios overlap, Table 2), and in lacking both fine granular sculpture on the adapical surface of the spire whorls and axial riblets on the protoconch. The living animal is of a much darker colour than that of P. bowkeri . P. quadingensis (below) is identical, except that it possesses fine spiral sculpture on later whorls, has axial riblets on the protoconch and is perhaps slightly more obese.
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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Prestonella nuptialis ( Melvill & Ponsonby, 1894 )
Herbert, D. G. 2007 |
Ena nuptialis:
CONNOLLY, M. 1912: 172 |
Buliminus nuptialis:
STURANY, R. 1898: 602 |
Buliminus nuptialis:
MELVILL, J. C. & PONSONBY, J. H. 1894: 92 |