Minilya perelegans ( Waagen & Pichl, 1885 )

Ernst, Andrej, Senowbari-Daryan, Baba & Hamedani, Ali, 2006, Middle Permian Bryozoa from the Lakaftari area, northeast of Esfahan (central Iran), Geodiversitas 28 (4), pp. 543-590 : 559-560

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 )
status

 

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.

Kingdom

Animalia

Phylum

Bryozoa

Class

Stenolaemata

Order

Fenestrida

Family

Fenestellidae

Genus

Minilya

Loc

Minilya perelegans ( Waagen & Pichl, 1885 )

Ernst, Andrej, Senowbari-Daryan, Baba & Hamedani, Ali 2006
2006
Loc

Minilya perelegans

CROCKFORD J. 1944: 173
1944
Loc

Fenestella perelegans

YANG J. & LU L. & XIA F. 1981: 89
FANTININ SESTINI F. N. 1965: 28
WAAGEN W. & PICHL I. 1885: 777
1885
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