Anabarites kelleri Missarzhevsky, 1989
publication ID |
https://doi.org/ 10.4202/app.00289.2016 |
persistent identifier |
https://treatment.plazi.org/id/03AD87A8-FFF7-6D4B-FF06-F8B263ED84C1 |
treatment provided by |
Felipe |
scientific name |
Anabarites kelleri Missarzhevsky, 1989 |
status |
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Anabarites kelleri Missarzhevsky, 1989
Fig. 75H–J View Fig .
Material.—Several thousand internal moulds, including figured SMNH X6024–6026, from samples 1/50, 1/46, 1/45, 1/39.3, 1/29.5 (section 1, Fig. 4 View Fig ), 3/0.1, 3/6.5, 3/12, 3/12.2, K2/12, K2/13, K2/20, K2/21, K2/22, K2/23, K2/24, K2/25, K2/26 (section 3, Fig. 3), 5/10, 5/10B, 5a/1, 5a/1.2, 5a/5, 5a/6, 5a/10.5, 5a/17.5 (section 96-5a, Fig. 2 View Fig ), Medvezhya Formation, western Anabar Uplift, Siberian Platform, Russia (SOM 1). Correlated with the uppermost Fortunian Stage.
Description.—Small, almost straight conchs with rounded triangular or tri-lobate cross-section; weakly developed longitudinal grooves; thin, straight growth lines present (see also Kouchinsky et al. 2009).
Remarks.—See Kouchinsky et al. (2009) for discussion of the validity of the species and Kouchinsky et al. (2015a) for probable lower part of Cambrian Stage 3 occurrence in the Emyaksin Formation.
Stratigraphic and geographic range.— Upper Fortunian Stage–Cambrian Stage 2 and probably lower part of Cambrian Stage 3, Siberian Platform (Kouchinsky et al. 2015a).
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