Gattenpleura concava ( Vöhringer, 1960 ) Korn & Weyer, 2023
publication ID |
https://doi.org/ 10.5852/ejt.2023.882.2177 |
publication LSID |
lsid:zoobank.org:pub:67C909E4-C700-4F8D-B8CE-5FD9B2C5D549 |
DOI |
https://doi.org/10.5281/zenodo.8184497 |
persistent identifier |
https://treatment.plazi.org/id/03EA5C14-CA9C-85D8-FE2C-FBFAFB4180B3 |
treatment provided by |
Felipe |
scientific name |
Gattenpleura concava ( Vöhringer, 1960 ) |
status |
comb. nov. |
Gattenpleura concava ( Vöhringer, 1960) comb. nov.
Figs 10C View Fig , 89–90 View Fig View Fig ; Tables 87–88 View Table 87 View Table 88
Gattendorfia concava Vöhringer, 1960: 157 View in CoL , pl. 5 fig. 2, text-fig. 32.
Gattendorfia concava View in CoL – Korn 1994: 74, text-figs 65d, 66k, 67f. — Kullmann 2000: text-fig. 4l; 2009: text-fig. 3.6c. — Korn & Weyer 2003: 100, pl. 2 figs 16–17.
Diagnosis
Species of Gattenpleura with a conch reaching 30 mm diameter. Conch at 15 mm dm thickly discoidal, subinvolute (ww/dm ~0.48; uw/dm ~0.22). Whorl profile at 15 mm dm weakly compressed (ww/wh ~0.95); coiling rate low (WER ~1.70). Venter rounded, umbilical margin raised and narrowly rounded, accompanied by a dorsolateral spiral groove. Growth lines very fine, narrow-standing, with convex course. With shallow constrictions on the shell surface; with weak internal shell thickenings. Suture line with narrowly lanceolate external lobe and V-shaped adventive lobe.
Material examined
Holotype
GERMANY • Rhenish Mountains, Oberrödinghausen , railway cutting; Hangenberg Limestone , bed 4; Vöhringer Coll.; illustrated by Vöhringer (1960: pl. 5 fig. 2) and Korn (1994: text-fig. 65d); re-illustrated here in Fig. 89 View Fig ; GPIT-PV-63926.
Paratype
GERMANY • Rhenish Mountains , Oberrödinghausen, railway cutting; Hangenberg Limestone, bed 4; Vöhringer Coll.; GPIT-PV-63920 .
Additional material
GERMANY • 1 specimen; Rhenish Mountains, Oberrödinghausen , railway cutting ; Hangenberg Limestone , bed 3c ; Vöhringer Coll.; MB.C.31175 • 1 specimen; Rhenish Mountains, Oberrödinghausen , railway cutting ; Hangenberg Limestone , bed 3e ; Vöhringer Coll.; MB.C.31176 • 1 specimen; Rhenish Mountains, Oberrödinghausen , railway cutting ; Hangenberg Limestone , bed 3a; Weyer 1993–1994 Coll.; MB.C.31177 • 1 specimen; Rhenish Mountains, Oese , old quarry ; Hangenberg Limestone , bed 28; Weyer & Korn 2000 Coll.; MB.C.5260.1.
Description
Holotype GPIT-PV-63926 is a moderately well-preserved specimen with 19 mm conch diameter ( Fig. 89 View Fig ). The conch is thinly discoidal and involute (ww/dm ~0.42; uw/dm ~0.10) with a moderate coiling rate (WER = 1.75). The whorl profile is characteristic with a slightly raised umbilical margin, which is accompanied on the flank by a shallow spiral groove; the venter is broadly rounded. The shell ornament consists of delicate growth lines with convex course.
The sectioned paratype GPIT-PV-63920 provides a view into the conch ontogeny between 2.5 and 18 mm diameter ( Fig. 90A View Fig ). In this interval, the whorl profile changes from originally crescent-shaped to circular to slightly compressed. The dorsolateral groove is formed at about 12 mm conch diameter. The suture line of the paratype has a lanceolate external lobe, inverted U-shaped ventrolateral saddle and a V-shaped adventive lobe with slightly convex flanks ( Fig. 90B View Fig ).
Remarks
Gattenpleura concava differs from the other species of the genus by the lack of radial folds.
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 |
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Phylum |
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Class |
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Order |
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SubOrder |
Tornoceratina |
SuperFamily |
Prionoceratoidea |
Family |
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SubFamily |
Gattendorfiinae |
Genus |
Gattenpleura concava ( Vöhringer, 1960 )
Korn, Dieter & Weyer, Dieter 2023 |
Gattendorfia concava
Korn D. & Weyer D. 2003: 100 |
Kullmann J. 2000: 150 |
Korn D. 1994: 74 |
Gattendorfia concava Vöhringer, 1960: 157
Vohringer E. 1960: 157 |