Euthria walaszczyki, Harzhauser & Landau, 2024
publication ID |
https://doi.org/ 10.11646/zootaxa.5427.1.1 |
publication LSID |
lsid:zoobank.org:pub:923206B0-E8C5-4FD5-B882-55009ABB0282 |
persistent identifier |
https://treatment.plazi.org/id/03CE9F1C-FFD8-0C03-FF65-F99AEE4DFE72 |
treatment provided by |
Plazi |
scientific name |
Euthria walaszczyki |
status |
sp. nov. |
Euthria walaszczyki nov. sp.
Figs 34B View FIGURE 34 , 35A–C View FIGURE 35
[ Fusus ] corneus — Naumann 1852: plate captions, pl. 70, fig. 8 [non Euthria cornea ( Linnaeus, 1758) View in CoL ].
Fusus corneus Linn. —Hoernes 1853: 280, pl. 31, figs 3a–b [non Euthria cornea ( Linnaeus, 1758) View in CoL ].
Fusus corneus Linné — Neugeboren 1854: 184 [non Euthria cornea ( Linnaeus, 1758) View in CoL ].
[ Fusus ] corneus Brocc. — Naumann 1854: 1066 [non Euthria cornea ( Linnaeus, 1758) View in CoL ].
Fusus (Euthria) corneus Linn. —Hoernes & Auinger 1890: 257 [non Euthria cornea ( Linnaeus, 1758) View in CoL ].
E [uthria]. (E [uthria].) cornea View in CoL (L.)— Sieber 1958: 150 [non Euthria cornea ( Linnaeus, 1758) View in CoL ].
Type material. Holotype: NHMW 1851 View Materials /0002/0044, SL: 43.1 mm, MD: 19.8 mm, Grund ( Austria), illustrated in Hoernes (1853: pl. 31, fig. 3); Figs 35A View FIGURE 35 1 –A View FIGURE 1 2 View FIGURE 2 . Paratypes: NHMW 1863 View Materials /0015/1270, SL: 39.6 mm , MD: 17.8 mm, Grund ( Austria), Figs 35B View FIGURE 35 1 –B View FIGURE 1 2 View FIGURE 2 . NHMW 1869 View Materials /0001/0281, SL: 33.3 mm , MD: 14.5 mm, Grund ( Austria), Figs 35C View FIGURE 35 1 –C View FIGURE 1 2 View FIGURE 2 . NHMW 1868 View Materials /0001/0223, SL: 16.7 mm , MD: 7.7 mm, Grund ( Austria), Figs 34B View FIGURE 34 .
Additional material. 5 spec., NHMW 1868 View Materials /0001/0223, Grund ( Austria) .
Type locality. Grund ( Austria) .
Type stratum. Silt and clay of the Grund Formation.
Age. Middle Miocene, early Badenian (Langhian).
Etymology. In honor of Ireneusz Piotr Walaszczyk (Faculty of Geology, University of Warsaw, Poland) for his help searching for type material.
Diagnosis. Medium-sized, moderately slender fusiform shell with moderately high spire of convex whorls, early teleoconch whorls weakly shouldered just above suture, sculpture changing early in ontogeny from prominent axial and spiral sculpture to relatively smooth on third teleoconch whorl, last whorl evenly rounded, lacking subsutural ramp, base strongly constricted with moderately long, narrow siphonal canal.
Description. Medium-sized, moderately slender fusiform shell of up to seven teleoconch whorls; apical angle ~45°. Protoconch damaged in all available specimens; last protoconch whorl high, convex. Early teleoconch whorls slightly shouldered; periphery just above abapical suture. Relatively narrow axial ribs, separated by broad interspaces, weakening adapically, overrun by four primary spiral cords and delicate secondaries intercalated; ribs fading on third teleoconch whorl. Later teleoconch whorls convex, separated by moderately incised suture, bearing faint spiral threads, periphery below mid-whorl. Last whorl attaining ~65% of total height, with regularly convex periphery, base strongly constricted, fasciole indistinct; surface smooth except for weak spirals over fasciole.Aperture moderately wide, pyriform. Columella broadly excavated, angled at transition to siphonal canal often accentuated by small denticle. Columellar callus indistinct, weakly delimited from base, smooth; Anal canal moderately incised, accentuated by weak parietal swelling or denticle; no anal denticle. Outer lip thin at peristome, bearing 12–14 elongated denticles a short distance behind peristome that extend as fine lirae deep within aperture. Siphonal canal moderately long, narrow, deflected to the left, shallowly notched.
Discussion. This species was confused by Naumann (1852), Hoernes (1853) and Hoernes & Auinger (1890) with the Pleistocene and Recent Mediterranean Euthria cornea ( Linnaeus, 1758) . The extant species differs in its shorter spire and shouldered whorls with markedly concave subsutural ramp (see Brunetti & Della Bella 2016: figs 4A–D; Fraussen & Stahlschmidt 2017: pl. 4, figs 67–84). The Middle Miocene Paratethyan Euthria brunettii nov. sp. differs in its prominent axial ribs on the spire whorls that persist at least onto the penultimate whorl. Euthria perpiniana ( Fontannes, 1879) , from the Pliocene of the Mediterranean Sea, is very similar in general appearance and in the early disappearance of its axial sculpture but is larger (SL up to 55 mm), has less convex whorls with a distinct subsutural concavity, although weaker than in E. cornea , and more prominent spiral cords on early teleoconch whorls ( Fraussen & Stahlschmidt 2017: pl. 2, figs 40–48). The Pliocene Mediterranean Euthria plioelongata ( Sacco, 1904) is distinguished by its comparatively flat-sided spire whorls and axials that persist slightly longer, fading on the fourth teleoconch whorl (see Brunetti & Della Bella 2016: figs 2A–E; Fraussen & Stahlschmidt 2017: pl. 1, figs 26–33).
Paleoenvironment. At the locality Grund fossiliferous channel fills, which formed in middle to outer neritic environments bear allochthonous assemblages uniting coastal-mudflat faunas with inner neritic ones ( Zuschin et al. 2005; Roetzel 2009).
Distribution in Central Paratethys. Badenian (Middle Miocene): North Alpine Foreland Basin: Grund ( Austria) (Hoernes & Auinger 1890).
MD |
Museum Donaueschingen |
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 |
Euthria walaszczyki
Harzhauser, Mathias & Landau, Bernard M. 2024 |
Fusus corneus Linné
Neugeboren, J. L. 1854: 184 |
Fusus
Naumann, C. F. 1854: 1066 |