Permodomatoceras hamdii, Korn & Ghaderi, 2025

Korn, Dieter & Ghaderi, Abbas, 2025, Late Permian nautiloids from Julfa (NW Iran), European Journal of Taxonomy 1018, pp. 1-113 : 19-21

publication ID

https://doi.org/10.5852/ejt.2025.1018.3069

publication LSID

lsid:zoobank.org:pub:74A6C5AD-7328-444C-9478-36F290657B6E

DOI

https://doi.org/10.5281/zenodo.17234891

persistent identifier

https://treatment.plazi.org/id/03D4F01A-FFC8-9E08-3C71-F8E5FB6AE7D4

treatment provided by

Plazi

scientific name

Permodomatoceras hamdii
status

sp. nov.

Permodomatoceras hamdii sp. nov.

urn:lsid:zoobank.org:act:

Fig. 11 View Fig ; Table 3 View Table 3

Domatoceras hunicum – Shimansky 1965b: 161, pl. 15 fig. 12. — Teichert & Kummel 1973: 421, pl. 1 figs 7–8, pl. 2 figs 3–4.

Diagnosis

Species of Permodomatoceras with extremely discoidal, subevolute conch (ww/dm ~ 0.30; uw/dm ~ 0.40), weakly compressed whorl profile (ww/wh ~ 0.80) and very high coiling rate (WER ~ 2.45) at a conch diameter of 80 mm. Whorl profile with weakly concave venter, subangular ventrolateral shoulder, gently convergent, flattened flanks and narrowly rounded umbilical margin. Ornament with fine growth lines, without ribs or nodes. Suture line with a narrow and very shallow external lobe and a much larger and deeper, broadly rounded lateral lobe.

Etymology

Named after the late Bahaeddin Hamdi (1935–2019), the promoter of palaeontology in Iran.

Type material

Holotype

IRAN – East Azerbaijan • Ali Bashi 4; Araxoceras Beds of the Julfa Formation ( early Wuchiapingian); 2018; Ghaderi leg.; illustrated in Fig. 11 View Fig ; MB.C.32006 .

Paratypes

IRAN – West Azerbaijan • 1 specimen; Aras Valley ; Araxoceras Beds of the Julfa Formation ( early Wuchiapingian); 2018; Ghaderi leg.; MB.C.32007 1 specimen; same data as for preceding; 2011; Korn et al. leg.; MB.C.32008 1 specimen; same data as for preceding; 2013; Korn et al. leg.; MB.C.32009 2 specimens; same data as for preceding; 2018; Korn et al. leg.; MB.C.32010 to MB.C.32011 . – East Azerbaijan • 1 specimen; Ali Bashi 4; Araxoceras Beds of the Julfa Formation ( early Wuchiapingian); 2018; Ghaderi leg.; MB.C.32012 1 specimen; same data as for preceding; 2010; Korn et al. leg.; MB.C.32013 1 specimen; same data as for preceding; 2011; Korn et al. leg.; MB.C.32014 1 specimen; Zal; Araxoceras Beds of the Julfa Formation ( early Wuchiapingian); 2018; Ghaderi leg.; MB.C.32015 .

Description

Holotype MB.C.32006 is a phragmocone fragment with a whorl height of 30 mm ( Fig. 11A View Fig ) and allows for examination of the dorsal whorl area. The shape of the conch was reconstructed using this fragment; this results in a diameter of 80 mm. The whorl profile of the specimen is compressed (ww/wh=0.80) and trapezoidal with a very weakly concave venter, subangular ventrolateral shoulders, flattened and convergent flanks, a rounded umbilical margin and a very shallow dorsal zone ( Fig. 11B View Fig ). The dorsal zone shows that the penultimate whorl also had a weakly concave venter. The complete suture line is exposed. It shows that the external lobe is very shallow and that the ventrolateral saddle is subangular. The lateral lobe is broadly rounded and continues, at the umbilical seam, into a very shallow internal lobe, in which a very low and rounded saddle is raised ( Fig. 11C View Fig ). The septa are closely spaced; there are about ten chambers on a quarter of a volution ( SD ~9 degrees).

Some of the other specimens, such as paratype MB.C.32015, which is not illustrated, show a transformation of the ventrolateral shoulder from a subangular to a tightly rounded shape in the adult stage. In this specimen the shape change takes place at about 28 mm whorl height.

Remarks

It is most likely that the specimens illustrated by Shimansky (1965b) and Teichert & Kummel (1973) under the name “ Domatoceras hunicum ” belong to this species. However, P. hunicum differs from the new species in having septa in much larger distances (about five septa per quarter volution) than P. hamdii sp. nov. (10 septa per quarter volution). Another difference is the rate on whorl overlap, which is rather great in P. hunicum ( IZR ~ 0.15), while it is very low in P. hamdii ( IZR ~ 0.05).

The new species has a narrower whorl profile (ww/wh = 0.80) than the type species of the genus. However, as its conch shape with the almost rectangular, rather wide whorl profile clearly distinguishes it from the species of the genus Domatoceras , it is classified here as Permodomatoceras .

Table 3. Conch dimensions (in mm) and ratios of Permodomatoceras hamdii sp. nov.; reconstructed dimensions and ratios in italics.

Nr. dm ww wh uw ah ww/dm ww/wh uw/dm WER IZR
MB.C.32006 80.0 24.4 30.5 31.0 29.0 0.31 0.80 0.39 2.46 0.05
MB.C.32009 30.6 35.3 0.87
MB.C.32010 28.0 35.0 0.80
MB.C.32015 29.5 33.3 0.89
MB.C.32007 25.5 28.6 0.89
MB.C.32013 21.8 25.4 0.86

Kingdom

Animalia

Phylum

Mollusca

Class

Cephalopoda

SubClass

Nautiloidea

Order

Nautilida

SubOrder

Domatoceratina

SuperFamily

Grypoceratoidea

Family

Domatoceratidae

Genus

Permodomatoceras

Loc

Permodomatoceras hamdii

Korn, Dieter & Ghaderi, Abbas 2025
2025
Loc

Domatoceras hunicum

Teichert C. & Kummel B. & Sweet W. C. 1973: 421
Shimansky V. N. 1965: 161
1965
GBIF Dataset (for parent article) Darwin Core Archive (for parent article) View in SIBiLS Plain XML RDF