Buccinum undatum Linnaeus 1758

Buccinum undatum Linnaeus, 1758 (Fig. 11D 1-D 3) Buccinum undatum Linnaeus, 1758: 740. — Wood 1848: 35, pl. 3, fig. 12a-b. — Harmer 1914: 90, pl. 6, figs 1-10, pl. 7, figs 1-6, pl. 8, figs 1-2, pl. 10, fig. 13. — Domènech & Martinell 1982: 52, fig. 16. — Marquet 1997: 91, pl. 7, fig. 6. — Wesselingh et al. 2014: 194, fig. 1. — Símonarson & Eiríksson in Eiríksson & Símonarson 2021: 277, pl. 7.5, fig. 2. For more, see synonymy list in Marquet (1997) and Símonarson et al. (2021). MATERIAL AND DIMENSIONS. — Maximum height 32.1 mm, width 18.7 mm. — RGM.1364922 (2), leg. WG; RGM.1365005 (3), leg. ACJ; RGM.1365109 (11), leg. AWJ; RGM.1365187 (1), leg. AWJ. SPECIES CHARACTERISATION. — Shell large, relatively fragile, broadly fusiform; protoconch not preserved; teleoconch of four strongly convex whorls separated by impressed linear suture; sculpture of weak spirals cords with secondaries variably developed; sinuous axial ribs variably developed on early whorls weakening abapically, obsolete on last 1-2 whorls; aperture large, ovate; outer lip weakly thickened by varix, sinuous in profile; columella twisted at fasciole, columella and parietal callus moderately expanded over base, variably thickened. DISTRIBUTION. — Lower Pliocene: NSB, Coralline Crag, England (Wood 1848; Harmer 1914). — Upper Pliocene: NSB, Belgium (Marquet 1997), Red Crag, England (Wood 1848; Harmer 1914). — Lower Pleistocene: Atlantic, Iceland (Eiriksson & Símonarson 2021), Atlantic, West Greenland (Símonarson 1981), Selsoif, NW France (this paper). — Upper Pleistocene: western Mediterranean, Spain (Domènech & Martinell 1982); central Mediterranean, Italy (Malatesta & Zarlenga 1986), Baltic (Funder et al. 2002). — Holocene: NSB (Strand Petersen 2004). Today, this species is present in the North Atlantic, from Greenland and New Jersey on the western side and Iceland to the Bay of Biscay (Fretter & Graham 1984). Occurs in every kind of habitat, but prefers soft bottoms, lowest tide line to 1200 m depth. REMARKS Although highly variable, it cannot be confused with any other species.The Selsoif specimens are mostly incomplete but ascribed to the species without doubt. This is a boreal species.

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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.14823663
Primary Topic
Climate Change Policy and Economics
Type
article
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article

Buccinum undatum Linnaeus 1758

Zenodo (CERN European Organization for Nuclear Research)
Climate Change Policy and Economics
article

Buccinum undatum Linnaeus 1758

article en

Abstract

Buccinum undatum Linnaeus, 1758 (Fig. 11D 1-D 3) Buccinum undatum Linnaeus, 1758: 740. — Wood 1848: 35, pl. 3, fig. 12a-b. — Harmer 1914: 90, pl. 6, figs 1-10, pl. 7, figs 1-6, pl. 8, figs 1-2, pl. 10, fig. 13. — Domènech & Martinell 1982: 52, fig. 16. — Marquet 1997: 91, pl. 7, fig. 6. — Wesselingh et al. 2014: 194, fig. 1. — Símonarson & Eiríksson in Eiríksson & Símonarson 2021: 277, pl. 7.5, fig. 2. For more, see synonymy list in Marquet (1997) and Símonarson et al. (2021). MATERIAL AND DIMENSIONS. — Maximum height 32.1 mm, width 18.7 mm. — RGM.1364922 (2), leg. WG; RGM.1365005 (3), leg. ACJ; RGM.1365109 (11), leg. AWJ; RGM.1365187 (1), leg. AWJ. SPECIES CHARACTERISATION. — Shell large, relatively fragile, broadly fusiform; protoconch not preserved; teleoconch of four strongly convex whorls separated by impressed linear suture; sculpture of weak spirals cords with secondaries variably developed; sinuous axial ribs variably developed on early whorls weakening abapically, obsolete on last 1-2 whorls; aperture large, ovate; outer lip weakly thickened by varix, sinuous in profile; columella twisted at fasciole, columella and parietal callus moderately expanded over base, variably thickened. DISTRIBUTION. — Lower Pliocene: NSB, Coralline Crag, England (Wood 1848; Harmer 1914). — Upper Pliocene: NSB, Belgium (Marquet 1997), Red Crag, England (Wood 1848; Harmer 1914). — Lower Pleistocene: Atlantic, Iceland (Eiriksson & Símonarson 2021), Atlantic, West Greenland (Símonarson 1981), Selsoif, NW France (this paper). — Upper Pleistocene: western Mediterranean, Spain (Domènech & Martinell 1982); central Mediterranean, Italy (Malatesta & Zarlenga 1986), Baltic (Funder et al. 2002). — Holocene: NSB (Strand Petersen 2004). Today, this species is present in the North Atlantic, from Greenland and New Jersey on the western side and Iceland to the Bay of Biscay (Fretter & Graham 1984). Occurs in every kind of habitat, but prefers soft bottoms, lowest tide line to 1200 m depth. REMARKS Although highly variable, it cannot be confused with any other species.The Selsoif specimens are mostly incomplete but ascribed to the species without doubt. This is a boreal species.

Zenodo (CERN European Organization for Nuclear Research)
Naturalis Biodiversity Center (NL), Utrecht University (NL), Université de Rennes (FR)
Life below water
Openalex Percentile: Top 41%
Climate Change Policy and Economics
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