Steromphala cineraria

Steromphala cineraria (Linnaeus, 1758) (Fig. 4H 1-H 3, I 1-I 3) Trochus cinerarius Linnaeus, 1758: 758. ? non Trochus cinerarius – Wood 1848: 131, pl. 14, fig. 7. Trochus (Gibbula) cinerarius – Harmer 1923: 731 (partim, not pl. 58, figs 25, 26) (Upper Pleistocene records only). Gibbula cineraria – Pouwer & Wesselingh 2012: 151, figs 1-3. — Alf et al. 2020: 70, pl. 50. Steromphala cineraria – Affenzeller et al. 2017: 804, fig. 5. MATERIAL AND DIMENSIONS. — Maximum height 12.7 mm, width 12.4 mm. — RGM.1364902 (64), leg. WG; RGM.1364968 (125), leg. ACJ; RGM.1365177 (1), leg. ACJ; RGM.1310831 (1), leg. ACJ; RGM.1365066 (146), leg. AWJ. SPECIES CHARACTERISATION. — Shell low trochiform; five weakly shouldered teleoconch whorls separated by narrowly impressed suture; sculpture of numerous, fine, irregular spiral cords; axial sculpture reduced to prosocline growth-lines; base depressed bearing numerous concentric cords; umbilicus well developed, moderately narrow and deep; columella short, straight, oblique; colour pattern of red-orange zigzag flammules preserved in all specimens. DISTRIBUTION. — (Late Pliocene-Early Pleistocene: NSB and Irish Sea [Wood 1848; Harmer 1923] likely based on misidentifications [Pouwer & Wesselingh 2012]). Lower Pleistocene: Atlantic, Selsoif, France (this paper). Upper Pleistocene: British Isles (Harmer 1923). — Holocene: NSB (Strand Petersen 2004).Today this species is predominantly found in cooler waters in the NSB and along the European Atlantic coasts North Norway, Iceland to Gibraltar (Fretter & Graham 1977) and adjacent western Mediterranean (Giannuzzi-Savelli et al. 1994). Records south of Gibraltar in the Atlantic and into the Mediterranean, such as southManousis (2021), need to be confirmed. REMARKS Based on molecular data, this species is now placed in the genus Steromphala Gray, 1847 (Affenzeller et al. 2017). Most specimens from Selsoif are small and depressed (Fig. 4I 1-I 3). One large, gerontic specimen (Fig. 4H 1-H 3) is taller spired, with more strongly shouldered whorls, the shoulder marked by two slightly strengthened cords. In general, the Selsoif specimens have slightly more shouldered whorls than extant specimens, but we consider them conspecific.

Institutions

Publication Details

Journal
Zenodo (CERN European Organization for Nuclear Research)
Published
2025-02-06
DOI
https://doi.org/10.5281/zenodo.14850553
Primary Topic
Geology and Paleoclimatology Research
Type
article
Field-Weighted Citation Impact
0.00
Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
article

Steromphala cineraria

Zenodo (CERN European Organization for Nuclear Research)
Geology and Paleoclimatology Research
article

Steromphala cineraria

article en

Abstract

Steromphala cineraria (Linnaeus, 1758) (Fig. 4H 1-H 3, I 1-I 3) Trochus cinerarius Linnaeus, 1758: 758. ? non Trochus cinerarius – Wood 1848: 131, pl. 14, fig. 7. Trochus (Gibbula) cinerarius – Harmer 1923: 731 (partim, not pl. 58, figs 25, 26) (Upper Pleistocene records only). Gibbula cineraria – Pouwer & Wesselingh 2012: 151, figs 1-3. — Alf et al. 2020: 70, pl. 50. Steromphala cineraria – Affenzeller et al. 2017: 804, fig. 5. MATERIAL AND DIMENSIONS. — Maximum height 12.7 mm, width 12.4 mm. — RGM.1364902 (64), leg. WG; RGM.1364968 (125), leg. ACJ; RGM.1365177 (1), leg. ACJ; RGM.1310831 (1), leg. ACJ; RGM.1365066 (146), leg. AWJ. SPECIES CHARACTERISATION. — Shell low trochiform; five weakly shouldered teleoconch whorls separated by narrowly impressed suture; sculpture of numerous, fine, irregular spiral cords; axial sculpture reduced to prosocline growth-lines; base depressed bearing numerous concentric cords; umbilicus well developed, moderately narrow and deep; columella short, straight, oblique; colour pattern of red-orange zigzag flammules preserved in all specimens. DISTRIBUTION. — (Late Pliocene-Early Pleistocene: NSB and Irish Sea [Wood 1848; Harmer 1923] likely based on misidentifications [Pouwer & Wesselingh 2012]). Lower Pleistocene: Atlantic, Selsoif, France (this paper). Upper Pleistocene: British Isles (Harmer 1923). — Holocene: NSB (Strand Petersen 2004).Today this species is predominantly found in cooler waters in the NSB and along the European Atlantic coasts North Norway, Iceland to Gibraltar (Fretter & Graham 1977) and adjacent western Mediterranean (Giannuzzi-Savelli et al. 1994). Records south of Gibraltar in the Atlantic and into the Mediterranean, such as southManousis (2021), need to be confirmed. REMARKS Based on molecular data, this species is now placed in the genus Steromphala Gray, 1847 (Affenzeller et al. 2017). Most specimens from Selsoif are small and depressed (Fig. 4I 1-I 3). One large, gerontic specimen (Fig. 4H 1-H 3) is taller spired, with more strongly shouldered whorls, the shoulder marked by two slightly strengthened cords. In general, the Selsoif specimens have slightly more shouldered whorls than extant specimens, but we consider them conspecific.

Zenodo (CERN European Organization for Nuclear Research)
Naturalis Biodiversity Center (NL), Utrecht University (NL), Université de Rennes (FR)
Life below water
Openalex Percentile: Top 53%
Geology and Paleoclimatology Research
AI Navigator

Ask Laika to Summarize, Analyze, and Connect papers live on the map.

Summarize Papers & Methodologies

Extract key findings, datasets, and comparative methods across publications.

Benchmark Rankings & Visual Analytics

Rank top research institutions, authors, funders, topics, and journals by Field-Weighted Citation Impact (FWCI) and paper volume with instant charts.

Connect Distant Disciplines

Bridge topological clusters on the map to find hidden collaborative intersections.