Tuoraconus sp.
publication ID |
https://doi.org/ 10.4202/app.00289.2016 |
persistent identifier |
https://treatment.plazi.org/id/03AD87A8-FF80-6D3C-FFF3-F9F3625487D3 |
treatment provided by |
Felipe |
scientific name |
Tuoraconus sp. |
status |
|
Fig. 12 View Fig .
Material.—Three phosphatic internal moulds, SMNH Mo181968–181970, from samples 5a/34.5 (section 96-5a, Fig. 2 View Fig ) and 7/31.5 (section 96-7, Kouchinsky et al. 2015a); Emyaksin Formation, eastern Anabar Uplift.Correlated with lower part of Cambrian Stage 2 (5a/34.5) and Delgadella anabara Zone, Atdabanian Stage (Cambrian Stage 3; sample 7/31.5; see Kouchinsky et al. 2015a: fig. 2).
Remarks.—Internal moulds triangular in transverse view ( Fig. 12A View Fig 2 View Fig ), narrow dorsum, laterally compressed apex projects beyond apertural margin. Imbricated micro-ornament on lateral parts of the mould near the aperture ( Fig. 12A View Fig 4 View Fig ) is similar to that in T. acutatus (Ushatinskaya and Parkhaev 2005: fig. 1) and reminiscent of foliated aragonite fabric (Vendrasco et al. 2011a, b). Specimens from samples 7/31.5 are represented by narrower internal moulds ( Fig. 12B, C View Fig ) than the specimen from sample 5a/34.5 and the material may therefore belong to two different species. Clear distinction is however hampered by preservation.
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