Cambrocyathellus sp.
publication ID |
https://doi.org/ 10.4202/app.00930.2021 |
persistent identifier |
https://treatment.plazi.org/id/03B4442D-F81C-FF87-7A40-116CFD3BFC28 |
treatment provided by |
Felipe |
scientific name |
Cambrocyathellus sp. |
status |
|
Fig. 79F View Fig .
Material. —A single phosphatised fragment SMNH Sp11543 from sample 21/21, Tyuser Formation, Lena River, Siberia, Russia. Dokodocyathus regularis Zone, Tommotian stage correlated with the upper part of Cambrian Stage 2).
Remarks. —Fragment of the outer wall pierced by relatively large pores of rounded shapes and uneven sizes, 80–140 µm in dimeter. Ridges representing remains of vertical plate-like elements are observed on the inner surface of the wall. Outer walls with irregularly situated pores of variable sizes are more characteristic of archaeocyathids than ajacicyathids, while the presence of septum-like elements infers the affinity to the Loculicyathina (Debrenne et al. 2015). Two vertical rows of pores per each interseptal space is typical of Cambrocyathellus Zhuravleva, 1960 , which is known on the Siberian Platform from the Tommotian and lowermost Atdabanian (correlated with the lower part of the Cambrian Stage 3) strata ( Zhuravleva 1960; Zhuravlev et al. 1983).
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