Alibashites mojsisovicsi ( Stoyanow, 1910 )
publication ID |
https://doi.org/ 10.5852/ejt.2021.776.1559 |
publication LSID |
lsid:zoobank.org:pub:226B6C59-8620-4A29-9BEF-359BE67A1A2C |
DOI |
https://doi.org/10.5281/zenodo.5711332 |
persistent identifier |
https://treatment.plazi.org/id/03CC87BF-FF8B-FF90-FD96-F9D4FC82FAD0 |
treatment provided by |
Felipe |
scientific name |
Alibashites mojsisovicsi ( Stoyanow, 1910 ) |
status |
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Alibashites mojsisovicsi ( Stoyanow, 1910) View in CoL
Fig. 47 View Fig ; Table 23
Xenodiscus (Paratirolites View in CoL ?) Mojsisovicsi Stoyanow, 1910: 79, pl. 8 fig. 1.
Abichites mojsisovicsi – Shevyrev 1965: 180, pl. 23 fig. 4; 1968: 95, pl. 4 fig. 3. — Stepanov et al. 1969: pl. 13 fig. 4.
Alibashites mojsisovicsi View in CoL – Korn & Ghaderi in Korn et al. 2016: 870, text-fig. 29.
Diagnosis
Alibashites with conch reaching 90 mm dm. Subadult stage with circular, weakly depressed whorl profile (ww/wh =1.00–1.20) and rounded venter; 13 coarse ventrolateral nodes per volution. Adult stage with quadrate and weakly compressed whorl profile (ww/wh=0.95–1.00), almost flat venter and subangular
ventrolateral shoulder; low ribs on flanks, forming very weak dorsolateral and ventrolateral nodes. Prongs of external lobe variable, simple to trifid; 8–13 notches of E, A and L lobes.
Material examined
IRAN • 1 specimen; Esfahan Province, Baghuk Mountain C section ; Hambast Formation; MB.C.29969 • 1 specimen; Esfahan Province, Baghuk Mountain H section ; Hambast Formation; MB.C.299670 • 2 specimens; Esfahan Province, Baghuk Mountain ; Hambast Formation; MB.C.299671 to MB.C.29972 .
Description
Specimen MB.C.29969 has 55 mm conch diameter with a moderately well-preserved last volution of the phragmocone but a weathered body chamber ( Fig. 47A View Fig ). It possesses a nearly quadrate whorl profile with angular ventrolateral shoulder and weakly concave venter at its largest diameter. Half of a whorl earlier, the venter is nearly flat and another half of a whorl earlier, it is broadly convex. At this stage, the whorl profile is trapezoidal with strongly diverging flanks. The sculpture of the phragmocone shows about 20 ventrolateral nodes with a tendency to become weaker during growth of the conch.
The suture line of specimen MB.C.29969 shows a V-shaped external lobe with diverging flanks, a parallel-sided ventrolateral saddle with weak dorsal inclination and adventive and lateral lobes with moderate serration ( Fig. 47B View Fig ). They are separated by a rather low, symmetric lateral saddle.
Remarks
Alibashites ferdowsii also has coarse nodes in the subadult stage like A. mojsisovicsi , but this species shows a much wider whorl profile (ww/wh=1.25–1.50) than A. mojsisovicsi (ww/wh = 0.95–1.00) in the adult stage. A. mojsisovicsi differs from the species of Abichites , which may develop a similar adult stage, in the coarse subadult ventrolateral nodes.
Stratigraphic range
Upper part of the Hambast Formation; 1.35 to 0.75 m below the extinction horizon (upper part of the Lutites profundus Zone to Abichites stoyanowi Zone ).
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 |
Paraceltitina |
SuperFamily |
Xenodiscoidea |
Family |
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Genus |
Alibashites mojsisovicsi ( Stoyanow, 1910 )
Korn, Dieter, Hairapetian, Vachik, Ghaderi, Abbas, Leda, Lucyna, Schobben, Martin & Akbari, Amir 2021 |
Alibashites mojsisovicsi
Korn D. & Ghaderi A. & Leda L. & Schobben M. & Ashouri A. R. 2016: 870 |
Abichites mojsisovicsi
Shevyrev A. A. 1965: 180 |
Xenodiscus (Paratirolites
Stoyanow A. A. 1910: 79 |