Alibashites mojsisovicsi A. Lateral
Creators
- 1. Museum für Naturkunde, Leibniz Institut for Research on Evolution and Biodiversity, Invalidenstrasse 43, 10115 Berlin, Germany.
- 2. Department of Geology, Esfahan (Khorasgan) Branch, Islamic Azad University, Esfahan, Iran.
- 3. Department of Geology, Faculty of Science, Ferdowsi University of Mashhad, Azadi Square, 9177948974, Mashhad, Iran.
- 4. Utrecht University, Department of Earth Sciences, Princetonlaan 8 A, 3584 CB Utrecht, The Netherlands. & Department of Geology, Esfahan (Khorasgan) Branch, Islamic Azad University, Esfahan, Iran.
- 5. Department of Geology, Esfahan (Khorasgan) Branch, Islamic Azad University, Esfahan, Iran
Description
Alibashites mojsisovicsi (Stoyanow, 1910)
Fig. 47; Table 23
Xenodiscus (Paratirolites ?) 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 – Korn & Ghaderi in Korn et al. 2016: 870, text-fig. 29.
DiagnosisAlibashites 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 examinedIRAN • 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.
DescriptionSpecimen 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). 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). They are separated by a rather low, symmetric lateral saddle.
RemarksAlibashites 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 rangeUpper 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).
Notes
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Linked records
Additional details
Identifiers
Biodiversity
- Collection code
- MB
- Family
- Dzhulfitidae
- Genus
- Alibashites
- Kingdom
- Animalia
- Material sample ID
- MB.C.299670 , MB.C.299671, MB.C.29972 , MB.C.29969
- Order
- Ammonoidea
- Phylum
- Mollusca
- Scientific name authorship
- A. Lateral
- Species
- mojsisovicsi
- Taxon rank
- species
- Taxonomic concept label
- Alibashites mojsisovicsi (Stoyanow, 1910) sec. Korn, Hairapetian, Ghaderi, Leda, Schobben & Akbari, 2021
References
- Stoyanow A. A. 1910. On the character of the boundary of Palaeozoic and Mesozoic near Djulfa. Zapiski Imperatorskago St. - Peterburgskago Mineralogiceskago Obscestva [= Verhandlungen der Russisch- Kaiserlichen Mineralogischen Gesellschaft zu St. Petersburg], 2 nd Series 47: 61 - 135.
- Shevyrev A. A. 1965. Nadortyad Ammonoidea. In: Ruzhencev V. E. & Sarytcheva T. G. (eds) Rasvitie i smena morskikh organizmov na rubezhe Paleozoya i Mezozoya. Trudy Paleontologicheskogo Instituta Akademiya Nauk SSSR 108: 166 - 182.
- Stepanov D. L., Golshani F. & Stocklin J. 1969. Upper Permian and Permian - Triassic Boundary in North Iran. Geolological Survey of Iran, Report 12: 1 - 72.
- Korn D., Ghaderi A., Leda L., Schobben M. & Ashouri A. R. 2016. The ammonoids from the Late Permian Paratirolites Limestone of Julfa (East Azerbaijan, Iran). Journal of Systematic Palaeontology 14: 841 - 890. https: // doi. org / 10.1080 / 14772019.2015.1119211