Carinacyathus sp.

Kouchinsky, Artem, Alexander, Ruaridh, Bengtson, Stefan, Bowyer, Fred, Clausen, Sébastien, Holmer, Lars E., Kolesnikov, Kirill A., Korovnikov, Igor V., Pavlov, Vladimir, Skovsted, Christian B., Ushatinskaya, Galina, Wood, Rachel & Zhuravlev, Andrey Y., 2022, Early-middle Cambrian stratigraphy and faunas from northern Siberia, Acta Palaeontologica Polonica 67 (2), pp. 341-464 : 450

publication ID

https://doi.org/ 10.4202/app.00930.2021

persistent identifier

https://treatment.plazi.org/id/03B4442D-F81E-FF85-7A40-11FDFDA6FB50

treatment provided by

Felipe

scientific name

Carinacyathus sp.
status

 

Carinacyathus sp.

Fig. 79D View Fig .

Material. —A single phosphatised fragment, SMNH Sp11542, from sample 20/1B, Erkeket Formation, Khorbusuonka River, Siberia, Russia. Lower Botoman stage (correlated with the lower part of Cambrian Stage 4).

Remarks.—Phosphatic crust replicating a fragment of a thick cup wall with geniculate tubular canals, elliptical in cross-section and 30–50 µm across. Among forms of archaeocyaths described from the lower Botoman part of the Erkeket Formation, tubular noncommunicating (lacking lateral pores) canals from the inner wall are known only from Carinacyathus , while other genera are characterised either by simple inner walls or flattened and S-shaped in vertical section scales. From investigation of Carinacyathus cups in thin sections, it was suggested that all of the species have the inner wall with downwardly projecting, straight canals, connected to the central cavity by supplementary structures, bracts (Debrenne et al. 2015). The new material indicates that the inner wall is pierced by geniculate (V-shaped in longitudinal section) canals without bracts.

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