Published December 31, 2006 | Version v1
Taxonomic treatment Open

Minilya perelegans

  • 1. Institut für Geowissenschaften der Christian-Albrechts-Universität zu Kiel, Ludewig-Meyn-Str. 10, D- 24118 Kiel (Germany) ae @ gpi. uni-kiel. de
  • 2. Institute of Paleontology, University of Erlangen-Nürnberg, Loewenichstr. 28, D- 91054 Erlangen (Germany) basendar @ pal. uni-erlangen. de
  • 3. University of Esfahan, Faculty of Earth Sciences, Esfahan (Iran) hamedani _ ali @ hotmail. com

Description

Minilya perelegans (Waagen & Pichl, 1885) (Fig. 6M, N; Table 15)

Fenestella perelegans Waagen & Pichl, 1885: 777, 778, pl. 87, figs 1-3. — Fantini Sestini 1965: 28, 29, pl. 2, fig. 1. — Yang et al. 1981: 89, pl. 2, fig. 7.

Non Meek, 1872: 153, pl. 7, fig. 3-3d.

Minilya perelegans – Crockford 1944a: 173.

MATERIAL EXAMINED. — 4-1, 4-5-2, 4-6-3, 4-8, 5-1-1, 5-6-3, 5-8-5, 12-1, 16-1, 19-4, 24-1-2, 25-3-5, 25-7.

OCCURRENCE. — Salt Range: Pakistan, Middle Permian (Guadalupian) (Waagen & Pichl 1885). Xizang: Tibet, China, Lower Permian. Lakaftari: central Iran, Jamal Formation, Middle Permian.

DESCRIPTION

Micrometric formula: 21-26/17-21//17-21. Reticulated colonies with straight branches, joined by thin dissepiments. Bifurcation common. Autozooecia arranged in 2 alternating rows on branches. Apertures circular having high peristomes with small nodes, spaced 1-2 per length of a fenestrule. Shape of fenestrules varying from oval to rectangular with rounded corners. Keel low, carrying two alternating rows of small closely spaced nodes. Internal granular skeleton thin, continuous with obverse keel, nodes, peristome and across dissepiments. Outer lamellar skeleton thin. Abundant microacanthostyles on the reverse surface, having distinct hyaline cores and dark laminated sheaths, 10-25 µm in diameter.

INTERIOR DESCRIPTION

Autozooecia triangular in the middle tangential section, low and elongated, with well developed vestibule; aperture positioned at distal to distalabaxial end of chamber. Superior hemisepta short; inferior hemisepta absent.

COMPARISON

Minilya perelegans is similar to M. paratuberculifera (Yang & Lu, 1962) from the Upper Permian of China and Khabarovsk region (Russia) (Morozova 1970a), differing from it in having thicker branches (0.24-0.35 vs. 0.22-0.24 mm in M. paratuberculifera). Another similar species is M. shurae (Morozova, 1970) from the Middle Permian (Kazanian) of the Russian Platform, which differs from M. perelegans in having smaller fenestrules.

REMARK

Waagen & Pichl (1885) referred this bryozoan to the species Fenestella perelegans Meek, 1872 (Meek 1872: 153, pl. 7, fig. 3-3d) from the Upper Carboniferous of Nebraska (see also Fantini Sestini 1965: 28, 29, who placed it into Fenestrellina). Crockford (1944a: 173) included the species Fenestella perelegans Waagen & Pichl, 1885 (not Meek, 1872) in her new genus Minilya. She recognized that these are different species (and genera), with the occurrence in the Upper Carboniferous of Nebraska (Meek 1872) and in the Middle Permian of Salt Range (Waagen & Pichl 1885). We support this conclusion and use the name “ Minilya perelegans ” for the species established by Waagen & Pichl (1885). The species of Meek (1872) should keep its specific name but change the generic assignment.

Notes

Published as part of Ernst, Andrej, Senowbari-Daryan, Baba & Hamedani, Ali, 2006, Middle Permian Bryozoa from the Lakaftari area, northeast of Esfahan (central Iran), pp. 543-590 in Geodiversitas 28 (4) on pages 559-560, DOI: 10.5281/zenodo.4665450

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Linked records

Additional details

Biodiversity

References

  • WAAGEN W. & PICHL I. 1885. - Salt Range fossils. Productus - limestone fossils. Memoirs of the Geological Survey of India, Paleontologica Indica Series 13, 1 (5): 771 - 966.
  • FANTININ SESTINI F. N. 1965. - The geology of the upper Djadjerud and Lar valleys (north-Iran). II, Palaeontology. Bryozoans, brachiopods and molluscs from Ruteh limestone (Permian). Revista Italiana di Paleontologia 71 (1): 13 - 108.
  • YANG J., LU L. & XIA F. 1981. - [Upper Paleozoic bryozoans from Xizang], in [Palaeontology of Xizang]. Science Press, Beijing: 81 - 100 (in Chinese).
  • MEEK F. B. 1872. - Report on the paleontology of Eastern Nebraska, with some remarks on the Carboniferous rocks of that district. Hayden's Final Report of the U. S. Geological Survey of Nebraska and Portions of Adjacent Territories. Government Printing Office, Washington D. C .. Part II. Paleontology: 81 - 264; Bryozoa: 141 - 158.
  • CROCKFORD J. 1944 a. - Bryozoa from Wandagee and Nooncanbah Series of Western Australia. Journal of the Royal Society of Western Australia 28: 165 - 185.
  • YANG J. & LU L. 1962. - [Paleozoic bryozoans of Gilianshan], in [Geology of Gilianshan]. Science Press, Beijing 4: 1 - 114 (in Chinese).
  • MOROZOVA I. P. 1970 a. - [Late Permian Bryozoa]. Trudy Paleontologicheskogo Instituta 122: 1 - 347 (in Russian).