Septopora flabellata Nikiforova, 1933
publication ID |
https://doi.org/ 10.5281/zenodo.4665450 |
persistent identifier |
https://treatment.plazi.org/id/F157A84D-1A34-FFEA-FF61-D4EDF5A8FA5A |
treatment provided by |
Felipe |
scientific name |
Septopora flabellata Nikiforova, 1933 |
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Septopora flabellata Nikiforova, 1933 View in CoL ( Figs 7 View FIG I-M; 8A-C; Table 18)
Septopora flabellata Nikiforova, 1933: 27 View in CoL , text-fig. 8. — Morozova 1970a: 197, 198, pl. 43, figs 3, 4, text-figs 10, 11. — Gorjunova 1975: 90, 91, pl. 22, fig. 2.
LECTOTYPE (designated by Morozova 1970a). — Central Museum of Geological Prospecting , Saint Petersburg, Russia. Thin section No. 62. Transcaucasia (Nakhichevan); Gnishik Horizon , Middle Permian, Murgabian (= Wordian).
MATERIAL EXAMINED. — 1-1-(1-3), 1-3-(1-3), 1-7-(1- 4), 2-(1-3), 3-1, 4-5-4, 4-5-7, 4-6-2, 4-6-4, 4-12-4, 4-15-(6-7), 5-3-1, 5-8-3, 7-1-2, 7-3-(3-4), 7-5-(5-6), 8-1-(1-3), 9-4-2, 9-4-3, 9-4-7, 9-5-2, 9-6-2, 9-6-4, 9-7-1, 10-2-8, 11-2-2, 12-1-(7-8), 13-4-4, 19-4-4, 19-4-7, 20-1-4, 20-2-(1-6), 22-1-1, 23-6-2, 23-6-3, 23-6-9, 24-5-8, 25-1-1, 25-4-2, 25-9-2, 25-9-3, 25- 13, 26-1-2.
OCCURRENCE. — Transcaucasia (Nakhichevan), Gnishik Horizon, Middle Permian, Murgabian (= Wordian) ( Morozova 1970a). Lakaftari: central Iran, Jamal Formation, Middle Permian.
DESCRIPTION
Micrometric formula: 11-16/11-14//16-20. Slender funnel-shaped, reticulated colonies with straight branches, joined by dissepiments; up to 30 cm high. New branches appearing by development of dissepiments to new branches or by bifurcation of branches. Autozooecia arranged in two alternating rows on branches and dissepiments, open on inside of the colony. Apertures circular to slightly oval, with low and thin peristomes bearing few small nodes, usually spaced 2 per length of a fenestrule. Shape of fenestrules varying from oval, narrow oval to rectangular and V-shaped. Obverse keel high with irregularly shaped elongated and prominent nodes. Nodes long, irregularly shaped, often having stellate shape, widening in the upper part. Smaller nodes of similar shape distributed on the reverse side, often arranged in 2-3 rows. Abundant microacanthostyles on the reverse surface of the colony arranged in regular rows. Internal granular skeleton thick, well developed, continuous with obverse keel, nodes, microacanthostyles, rods, peristome and across dissepiments. Outer lamellar skeleton sometimes extremely thick, containing small hyaline rods. Cyclozooecia abundant, spaced throughout the colony, often embedded by the outer lamellar skeleton.
INTERIOR DESCRIPTION
Autozooecia rectangular in the middle tangential section, relatively high and short in longitudinal section, with well developed vestibule; elongate to branch length; aperture positioned at distal to distalabaxial end of chamber. Hemisepta absent.
COMPARISON
Septopora flabellata is similar to S. flabellatiformis Romantchuk in Morozova, 1970 ( Morozova 1970a) from the Upper Permian (Osachtin Series) of the Khabarovsk region (Russian Far East). The latter species has considerably thicker branches (0.54-0.65 vs. 0.30-0.45 mm in S. flabellata ).
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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Septopora flabellata Nikiforova, 1933
Ernst, Andrej, Senowbari-Daryan, Baba & Hamedani, Ali 2006 |
Septopora flabellata
GORJUNOVA R. V. 1975: 90 |
MOROZOVA I. P. 1970: 197 |
NIKIFOROVA A. I. 1933: 27 |