Manzonia crassa ( Kanmacher, 1798 )
publication ID |
https://doi.org/10.5252/geodiversitas2025v47a3 |
publication LSID |
urn:lsid:zoobank.org:pub:BE95BEFE-D4E3-4138-B9BE-5A5656BEA68F |
DOI |
https://doi.org/10.5281/zenodo.14823648 |
persistent identifier |
https://treatment.plazi.org/id/8F310D3D-954B-FFA0-CDD1-FDE5820B68A0 |
treatment provided by |
Plazi |
scientific name |
Manzonia crassa ( Kanmacher, 1798 ) |
status |
|
Manzonia crassa ( Kanmacher, 1798) View in CoL
( Fig. 8D View FIG 1-D View FIG 3 View FIG )
Turbo crassus Kanmacher 1798: 638 View in CoL , fig. 20.
Manzonia (Manzonia) costata View in CoL – Cuerda Barceló 1987: 202, pl. 16, fig. 18.
Manzonia crassa View in CoL – Chirli & Linse 2011: 83, pl. 24, fig. 4. — Van Dingenen et al. 2016: 140, pl. 10, fig. 2. — Landau et al. 2018: 274, pl. 103, fig. 1.
For more, see synonymy list in Van Dingenen et al. (2016) and Landau et al. (2018).
MATERIAL AND DIMENSIONS. — Maximum height 1.7 mm, width 1.0 mm. RGM.1364988 (4), leg. ACJ ; RGM.1365201 (1), leg. ACJ ; RGM.1365093 (16), leg. AWJ .
SPECIES CHARACTERISATION. — Shell small, rissoiform. Protoconch not preserved. Four strongly convex teleoconch whorls separated by deeply impressed suture; sculpture of numerous, regular, flattened spiral cords; about ten high, widely spaced, sinuous, prosocline axial ribs. Ribs stop abruptly at strong, elevated peribasal cord; base narrow, deeply concave forming wide groove between peribasal cord and peristome. Aperture ovate, outer lip strongly thickened by rounded labial varix, peristome complete.
DISTRIBUTION. — Middle Miocene: Atlantic, Loire Basin, France ( de Morgan 1915; Cossmann 1918; Glibert 1949); Paratethys, Austria ( Kowalke & Harzhauser 2004), Hungary ( Strausz 1966), Poland (Friedberg 1923; Bałuk 1975), Romania ( Kowalke & Harzhauser 2004) ; Proto-Mediterranean, Karaman Basin, Turkey ( Landau et al. 2013). — Upper Miocene: Atlantic, NW France ( Calas 1949; Landau et al. 2018); Proto-Mediterranean, Italy ( Sacco 1895; Venzo & Pelosio 1963). — Lower Pliocene: Atlantic of NW France ( Van Dingenen et al. 2016); central Mediterranean, Italy ( Chirli 2006), Tunisia ( Fekih 1975). — Upper Pliocene: Atlantic, Portugal ( Silva 2001); western Mediterranean, Spain ( Landau et al. 2004); central Mediterranean, Italy ( Sacco 1895; Malatesta 1974; Cavallo & Repetto 1992; Sosso & dell’Angelo 2010; Tabanelli et al. 2011). — Lower Pleistocene: NSB, British Isles (Harmer 1918); Atlantic, Selsoif, NW France (this paper); western Mediterranean of France ( Glibert 1962); central Mediterranean, Italy ( Cerulli-Irelli 1914; Buccheri 1970); eastern Mediterranean, Rhodes Island ( Chirli & Linse 2011). — Upper Pleistocene: NSB, the Netherlands (Van Regteren Altena et al. 1954; Raad et al. 2013); western Mediterranean, Balearic Islands ( Cuerda Barceló 1987). Today this species occurs in the northeastern Atlantic from Norway southwards to Morocco, entire Mediterranean, from extreme low tide line to 50 m depth, often on sandy bottoms, but also under stones and in weeds ( Poppe & Goto 1991).
REMARKS
For discussion on fossil populations, see Landau et al. (2013: 74) and Van Dingenen et al. (2016: 140).
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.
Kingdom |
|
Phylum |
|
Class |
|
Order |
|
Family |
|
Genus |
Manzonia crassa ( Kanmacher, 1798 )
Bouchard, Blanche, Wesselingh, Frank P., Pouwer, Ronald & Landau, Bernard 2025 |
Manzonia crassa
LANDAU B. & CEULEMANS L. & VAN DINGENEN F. 2018: 274 |
VAN DINGENEN F. & CEULEMANS L. & LANDAU B. 2016: 140 |
CHIRLI C. & LINSE U. 2011: 83 |
Manzonia (Manzonia) costata
CUERDA BARCELO J. 1987: 202 |
Turbo crassus
KANMACHER F. 1798: 638 |