Protoconus cf. crestatus Yu, 1979

Kouchinsky, Artem, Bengtson, Stefan, Landing, Ed, Steiner, Michael, Vendrasco, Michael & Ziegler, Karen, 2017, Terreneuvian stratigraphy and faunas from the Anabar Uplift, Siberia, Acta Palaeontologica Polonica 62 (2), pp. 311-440 : 371

publication ID

https://doi.org/ 10.4202/app.00289.2016

persistent identifier

https://treatment.plazi.org/id/03AD87A8-FFA7-6D1B-FCCF-FCDF644884CD

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Felipe

scientific name

Protoconus cf. crestatus Yu, 1979
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Protoconus cf. crestatus Yu, 1979 View in CoL

Fig. 41 View Fig .

Material.—Three internal moulds, SMNH Mo182379– 182381, from samples 1/50 and 1/6 (section 1, Fig. 4 View Fig ), Medvezhya and Kugda-Yuryakh formations, western Anabar Uplift, Siberian Platform, Russia. Correlated with upper Fortunian and lower part of Cambrian Stage 2.

Description.—Bilaterally symmetrical, cap-shaped shell with broad oval aperture. Apex rounded, not clearly separated from the rest of the shell. Inner surface of the shell (replicated by the internal mould) with two parallel longitudinal thickenings that flank a wide median buttress that defines the entire dorsal side of the internal mould ( Fig. 41A View Fig 1, B 3, C 1).

Remarks.—Subapical side short with the subapical shelf that is diagnostic for the genus Protoconus ( Devaere et al. 2013; Fig. 41A View Fig 3). The furrows and median buttress are covered with a low nodular texture with positive relief on the mould ( Fig. 41C View Fig 1, C 4). The nodules are ca. 5 μm in diameter. Yang et al. (2014) reported moulds and partial conchs of P. crestatus from the late Fortunian (Assemblage Zone 2) of South China. The latter species is similar and probably synonymous with Purella tianzhushanensis Yu, 1979 . The latter was also described by Hamdi (1995: pl. 12: 1, 2) from the Latouchella Obtusoconus Assemblage Zone (Upper Shale Member, Soltanieh Formation, Albortz Mountains, Iran).

→ Fig. 36. Molluscs Yunnanopleura accurata ( Bokova, 1985) , internal moulds with partly phosphatized shells (B, H), from early Cambrian Nemakit-Daldyn (A, E, H) and Emyaksin (B–D, F, G) formations, Anabar Uplift, Siberia, Russia; samples K1a/47 (A) and 2/A (E), section 2; 3/0 (H), section 3; 4/27.5 (C, G), section 96-4, and 5/0 (B, D, F), section 96-5. A–H. SMNH Mo182349 (A), SMNH Mo160405 (B; see also Kouchinsky 2000a: fig. 4I), SMNH Mo182350–182355 (C–H, respectively). A 1, B 1, C 2, D, E 1, F 1, G 2, H 1, upper; A 2, B 3, E 2, F 3, H 3, subapical; A 3, B 2, C 1, F 2, G 1, H 2, lateral views. Scale bar 500 μm (A, B, C 2, D–G, H 3), 1 mm (C 1, H 1, H 2).

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