Triplicatella, Conway Morris, 1990

Kouchinsky, Artem, Bengtson, Stefan, Clausen, Sébastien & Vendrasco, Michael J., 2015, An early Cambrian fauna of skeletal fossils from the Emyaksin Formation, northern Siberia, Acta Palaeontologica Polonica 60 (2), pp. 421-512 : 453

publication ID

https://doi.org/ 10.4202/app.2012.0004

persistent identifier

https://treatment.plazi.org/id/03C3891D-150C-C252-FF00-FBB1CD2FF970

treatment provided by

Felipe

scientific name

Triplicatella
status

 

Triplicatella cf. T. peltata Skovsted, Peel, and Atkins, 2004

Fig. 29D View Fig .

Material.—Single phosphatised operculum, SMNH X 4649, from sample 7/70; uppermost Emyaksin Formation, Bol’shaya Kuonamka River; Calodiscus -Erbiella Zone, lower Botoman Stage.

Description.—The operculum has a rounded trapezoidal shape in plan view, ca. 1 mm wide, convex, with a single and prominent fold on the dorsal margin. In lateral view, the crest of the fold reaches the apex ( Fig. 29D View Fig 4 View Fig ). The internal surface is smooth, with a deep median depression in the sub-central part. Two short and rounded converging lateral ridges are situated near the dorsal margin.

Remarks.—Specimens of Triplicatella peltata Skovsted, Peel, and Atkins, 2004 from the Cambrian Stage 4 of Laurentia are similar in outline, number of folds and structure of the inner surface, although the dorsal fold is broader and more prominent than in the fossil herein.

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