Published October 27, 2021 | Version v1
Taxonomic treatment Open

Pseudogastrioceras relicuum Korn & Ghaderi 2016

  • 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

Pseudogastrioceras relicuum Korn & Ghaderi in Korn et al., 2016

Fig. 16; Table 1

Pseudogastrioceras relicuum Korn & Ghaderi in Korn et al., 2016: 852, text-fig. 12.

Diagnosis

Pseudogastrioceras with moderately large conch; diameter attaining 70 mm. Conch shape thinly discoidal (ww/dm=0.40–0.45), involute (uw/dm = 0.05–0.10) with converging flanks and broadly rounded venter. Ornament with about 15 faint spiral lines on the venter.

Material examined

Holotype IRAN • East Azerbaijan, Ali Bashi N section; Paratirolites Limestone; illustrated by Korn & Ghaderi in Korn et al. (2016: text-fig. 12); MB.C.25173.

Additional material

IRAN • 2 specimens; Esfahan Province, Baghuk Mountain 1 section; Hambast Formation; MB.C.29659 to MB.C.29660 • 1 specimen; Esfahan Province, Baghuk Mountain G section; Hambast Formation; MB.C.29661 • 2 specimens; Esfahan Province, Baghuk Mountain H section; Hambast Formation; MB.C.29662 to MB.C.29663.

Description

All specimens are rather poorly preserved, but MB.C.29661 is the best of them, though somewhat deformed (Fig. 16). It is a corroded specimen with a 56 mm conch diameter, which does not allow accurate measurements of the conch.

Stratigraphic range

Paratirolites Limestone; 6.80 to 3.30 m below the extinction horizon (Dzhulfites nodosus Zone to Paratirolites lanceolobatus Zone).

Notes

Published as part of Korn, Dieter, Hairapetian, Vachik, Ghaderi, Abbas, Leda, Lucyna, Schobben, Martin & Akbari, Amir, 2021, The Changhsingian (Late Permian) ammonoids from Baghuk Mountain (Central Iran), pp. 1-106 in European Journal of Taxonomy 776 on pages 16-17, DOI: 10.5852/ejt.2021.776.1559, http://zenodo.org/record/5604715

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Linked records

Additional details

References

  • 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