Minilya perelegans ( Waagen & Pichl, 1885 )
publication ID |
https://doi.org/ 10.5281/zenodo.4665450 |
DOI |
https://doi.org/10.5281/zenodo.4664979 |
persistent identifier |
https://treatment.plazi.org/id/F157A84D-1A30-FFEF-FD13-D3D4F2D6FD52 |
treatment provided by |
Felipe |
scientific name |
Minilya perelegans ( Waagen & Pichl, 1885 ) |
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Minilya perelegans ( Waagen & Pichl, 1885) View in CoL ( Fig. 6M, N View FIG ; Table 15)
Fenestella perelegans Waagen & Pichl, 1885: 777 View in CoL , 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 View in CoL – 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 View in CoL 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 View in CoL 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.
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.
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Minilya perelegans ( Waagen & Pichl, 1885 )
Ernst, Andrej, Senowbari-Daryan, Baba & Hamedani, Ali 2006 |
Minilya perelegans
CROCKFORD J. 1944: 173 |
Fenestella perelegans
YANG J. & LU L. & XIA F. 1981: 89 |
FANTININ SESTINI F. N. 1965: 28 |
WAAGEN W. & PICHL I. 1885: 777 |