Epitainoceras lutense Korn & Hairapetian, 2025, gen. et sp. nov.

Epitainoceras lutense gen. et sp. nov. urn:lsid:zoobank.org:act: 5A1405B2-C14D-4533-8089-A1C3435EBC18 Fig. 24; Table 18 Diagnosis Species of Epitainoceras gen. nov. with thickly discoidal, subinvolute conch (ww/dm ~ 0.55; uw/dm ~0.25) and weakly depressed whorl profile (ww/wh ~ 1.35) and very high coiling rate (WER ~ 2.35) at a conch diameter of 70 mm. Whorl profile polygonal with convergent flanks; venter tectiform with broad longitudinal midventral groove, flanks flattened, umbilical margin narrowly rounded. Sculpture with about 15 coarse ventrolateral, transversely elongated nodes per volution. Suture line with a small, rounded V-shaped external lobe, a broadly rounded, very shallow lateral lobe and a very shallow umbilical lobe. Etymology Named after the Lut desert (Central Iran), at which margin Baghuk Mountain is located. Type material Holotype IRAN – Esfahan Province • Baghuk Mountain; Hambast Formation, Araxoceras beds (early Wuchiapingian); 2011; Korn et al. leg.; illustrated in Fig. 24; MB.C.32136. Paratype IRAN – Esfahan Province • 1 specimen; same data as for holotype; MB.C.32137. Description Holotype MB.C.32136 is a corroded phragmocone specimen with a diameter of 75 mm (Fig. 24B). It allows the conch form, sculpture and suture line to be studied, but some conch dimensions can only be estimated. The conch is thickly discoidal and subinvolute (ww/dm ~0.55; uw/dm ~0.25) with a very high coiling rate (WER ~2.35). The whorl profile is slightly depressed (ww/wh ~ 1.35) and widest at the narrowly rounded umbilical margin. The venter possesses a moderately wide median groove; the ventrolateral shoulder is flattened and oblique, the flanks are weakly flattened and convergent and the umbilical margin is narrowly rounded (Fig. 24A). Because of partial corrosion of the specimen, the sculpture cannot be examined in detail. It consists of two rows of nodes arranged on each side of the ventrolateral shoulder. The ventral row has nodes that are elongated in a lateral direction to form short ribs; the dorsal row consists of much weaker, circular nodes. The suture line of the holotype has a shallow, broadly V-shaped external lobe, a low and broadly rounded, slightly asymmetric ventrolateral saddle, a shallow and very wide lateral lobe and a very shallow and small lobe on the umbilical wall (Fig. 24C). The last half volution has 15 phragmocone chambers (CLI =12). Remarks Epitainoceras lutense gen. et sp. nov. is similar to the Transcaucasian species E. dorsoplicatum comb. nov., but differs in having a much wider midventral groove and significantly larger ventral nodes. These nodes are laterally elongated in E. lutense, whereas they are simply conical in E. dorsoplicatum.

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Publication Details

Journal
Zenodo (CERN European Organization for Nuclear Research)
Published
2025-09-24
DOI
https://doi.org/10.5281/zenodo.17227779
Primary Topic
Geochemistry and Geologic Mapping
Type
article
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article

Epitainoceras lutense Korn & Hairapetian, 2025, gen. et sp. nov.

Zenodo (CERN European Organization for Nuclear Research)
Geochemistry and Geologic Mapping
article

Epitainoceras lutense Korn & Hairapetian, 2025, gen. et sp. nov.

article en

Abstract

Epitainoceras lutense gen. et sp. nov. urn:lsid:zoobank.org:act: 5A1405B2-C14D-4533-8089-A1C3435EBC18 Fig. 24; Table 18 Diagnosis Species of Epitainoceras gen. nov. with thickly discoidal, subinvolute conch (ww/dm ~ 0.55; uw/dm ~0.25) and weakly depressed whorl profile (ww/wh ~ 1.35) and very high coiling rate (WER ~ 2.35) at a conch diameter of 70 mm. Whorl profile polygonal with convergent flanks; venter tectiform with broad longitudinal midventral groove, flanks flattened, umbilical margin narrowly rounded. Sculpture with about 15 coarse ventrolateral, transversely elongated nodes per volution. Suture line with a small, rounded V-shaped external lobe, a broadly rounded, very shallow lateral lobe and a very shallow umbilical lobe. Etymology Named after the Lut desert (Central Iran), at which margin Baghuk Mountain is located. Type material Holotype IRAN – Esfahan Province • Baghuk Mountain; Hambast Formation, Araxoceras beds (early Wuchiapingian); 2011; Korn et al. leg.; illustrated in Fig. 24; MB.C.32136. Paratype IRAN – Esfahan Province • 1 specimen; same data as for holotype; MB.C.32137. Description Holotype MB.C.32136 is a corroded phragmocone specimen with a diameter of 75 mm (Fig. 24B). It allows the conch form, sculpture and suture line to be studied, but some conch dimensions can only be estimated. The conch is thickly discoidal and subinvolute (ww/dm ~0.55; uw/dm ~0.25) with a very high coiling rate (WER ~2.35). The whorl profile is slightly depressed (ww/wh ~ 1.35) and widest at the narrowly rounded umbilical margin. The venter possesses a moderately wide median groove; the ventrolateral shoulder is flattened and oblique, the flanks are weakly flattened and convergent and the umbilical margin is narrowly rounded (Fig. 24A). Because of partial corrosion of the specimen, the sculpture cannot be examined in detail. It consists of two rows of nodes arranged on each side of the ventrolateral shoulder. The ventral row has nodes that are elongated in a lateral direction to form short ribs; the dorsal row consists of much weaker, circular nodes. The suture line of the holotype has a shallow, broadly V-shaped external lobe, a low and broadly rounded, slightly asymmetric ventrolateral saddle, a shallow and very wide lateral lobe and a very shallow and small lobe on the umbilical wall (Fig. 24C). The last half volution has 15 phragmocone chambers (CLI =12). Remarks Epitainoceras lutense gen. et sp. nov. is similar to the Transcaucasian species E. dorsoplicatum comb. nov., but differs in having a much wider midventral groove and significantly larger ventral nodes. These nodes are laterally elongated in E. lutense, whereas they are simply conical in E. dorsoplicatum.

Zenodo (CERN European Organization for Nuclear Research)
Museum für Naturkunde (DE), Islamic Azad University, Isfahan (IR)
Life in Land
Openalex Percentile: Top 26%
Geochemistry and Geologic Mapping
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