Crepidula gibbosa Defrance 1818

Crepidula gibbosa Defrance, 1818 (Fig. 10B 1, B 2) Crepidula gibbosa Defrance, 1818: 397. — Chirli & Forli 2017: 53, fig. 15c. — Landau et al. 2018: 317, pl. 148, fig. 1. MATERIAL AND DIMENSIONS. — Maximum height 3.5 mm, diameter 12.3 mm. — RGM.1364917 (1), leg. WG; RGM.1364996 (2), leg. ACJ; RGM.1365101 (62), leg. AWJ; RGM.1365185 (1), leg. AWJ. SPECIES CHARACTERISATION. — Thick, low, smooth, convex shell. Aperture ovate. Concave, shallow septum covering almost 2/3 of the aperture. DISTRIBUTION. — Middle Miocene: Atlantic, Aquitaine Basin, France (Cossmann & Peyrot 1919), Loire Basin, France (Glibert 1949); Paratethys, Austria (Hörnes 1856), Poland (Bałuk 1975), Hungary (Strausz 1966); Proto-Mediterranean, Karaman Basin, Turkey (Landau et al. 2013). — Upper Miocene: Atlantic, NW France (Landau et al. 2018); Proto-Mediterranean, Italy (Sacco 1896b). — Lower Pliocene: Atlantic, NW France (Van Dingenen et al. 2016); SW Spain (González-Delgado 1988; Landau et al. 2011). — Upper Pliocene: Atlantic, Morocco (Lecointre 1952); western Mediterranean, S Spain (Landau et al. 2004); central Mediterranean, Italy (Chirli 1988; Cavallo & Repetto 1992). — Upper Pliocene-Pleistocene: NW France (Glibert 1963). — Lower Pleistocene, Atlantic, Selsoif, NW France (this paper); central Mediterranean (Chirli & Forli 2017). Today, this species occurs in the Mediterranean Sea, below low tide line, often attached to other molluscs (Poppe & Goto 1991). REMARKS Our assignment of Crepidula to C. gibbosa does not conform to its treatment in WoRMS and follows arguments provided in Landau et al. (2004: 74). In our opinion the taxonomy of European Crepidula is not resolved and requires in-depth studies that are beyond the scope of this paper.

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Publication Details

Journal
Zenodo (CERN European Organization for Nuclear Research)
Published
2025-02-06
DOI
https://doi.org/10.5281/zenodo.14850611
Primary Topic
Geological Formations and Processes Exploration
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article
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article

Crepidula gibbosa Defrance 1818

Zenodo (CERN European Organization for Nuclear Research)
Geological Formations and Processes Exploration
article

Crepidula gibbosa Defrance 1818

article en

Abstract

Crepidula gibbosa Defrance, 1818 (Fig. 10B 1, B 2) Crepidula gibbosa Defrance, 1818: 397. — Chirli & Forli 2017: 53, fig. 15c. — Landau et al. 2018: 317, pl. 148, fig. 1. MATERIAL AND DIMENSIONS. — Maximum height 3.5 mm, diameter 12.3 mm. — RGM.1364917 (1), leg. WG; RGM.1364996 (2), leg. ACJ; RGM.1365101 (62), leg. AWJ; RGM.1365185 (1), leg. AWJ. SPECIES CHARACTERISATION. — Thick, low, smooth, convex shell. Aperture ovate. Concave, shallow septum covering almost 2/3 of the aperture. DISTRIBUTION. — Middle Miocene: Atlantic, Aquitaine Basin, France (Cossmann & Peyrot 1919), Loire Basin, France (Glibert 1949); Paratethys, Austria (Hörnes 1856), Poland (Bałuk 1975), Hungary (Strausz 1966); Proto-Mediterranean, Karaman Basin, Turkey (Landau et al. 2013). — Upper Miocene: Atlantic, NW France (Landau et al. 2018); Proto-Mediterranean, Italy (Sacco 1896b). — Lower Pliocene: Atlantic, NW France (Van Dingenen et al. 2016); SW Spain (González-Delgado 1988; Landau et al. 2011). — Upper Pliocene: Atlantic, Morocco (Lecointre 1952); western Mediterranean, S Spain (Landau et al. 2004); central Mediterranean, Italy (Chirli 1988; Cavallo & Repetto 1992). — Upper Pliocene-Pleistocene: NW France (Glibert 1963). — Lower Pleistocene, Atlantic, Selsoif, NW France (this paper); central Mediterranean (Chirli & Forli 2017). Today, this species occurs in the Mediterranean Sea, below low tide line, often attached to other molluscs (Poppe & Goto 1991). REMARKS Our assignment of Crepidula to C. gibbosa does not conform to its treatment in WoRMS and follows arguments provided in Landau et al. (2004: 74). In our opinion the taxonomy of European Crepidula is not resolved and requires in-depth studies that are beyond the scope of this paper.

Zenodo (CERN European Organization for Nuclear Research)
Naturalis Biodiversity Center (NL), Utrecht University (NL), Université de Rennes (FR)
Openalex Percentile: Top 56%
Geological Formations and Processes Exploration
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