Pagrus sp.
publication ID |
https://doi.org/ 10.1515/vzoo-2016-0048 |
DOI |
https://doi.org/10.5281/zenodo.6525587 |
persistent identifier |
https://treatment.plazi.org/id/03AD8798-FFA7-1E53-FF3E-B2B9A2A5FB93 |
treatment provided by |
Felipe |
scientific name |
Pagrus sp. |
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Pagrus sp. (pl. 1, figs 1 View Fig –6)
M a t e r i a l a n d l o c a l i t i e s. Two molariform teeth NMNHU-P 53/5117–5118 (Novopetrovka, lower Pliocene); four molariform teeth (Shirokino 2, upper Pliocene).
D e s c r i p t i o n. The studied material consists of symmetrical and asymmetrical teeth. Symmetrical teeth (pl. 1, figs 1 View Fig –4) are round and slightly elliptically elongated. Teeth are convex and slightly conical in lateral view (pl. 1, fig. 4). The teeth’s apical surface is irregular by the form of holes, which could be attributed to wear and postmortem bioerosion. Basal parts are not preserved. The pulpal cavity is clearly visible in all specimens, and the enamel is brown. Asymmetrical teeth (pl. 1, figs 5–6) are elongated elliptically and are kidney-like in shape. The teeth are convex in lateral section and uniformly curved. Their apical surface is damaged, most likely because of bioerosion (pl. 1, fig. 5). Basal parts are poorly preserved (pl. 1, fig. 6) or absent (pl. 1, fig. 5). The pulpal cavity is filled with sediment. The enamel is dark brown or black.
M e a s u r e m e n t s, i n m m. Length — 10–18 (μ = 15); width — 6–14 (μ = 11).
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Teleostei |
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