Cupitheca sp.
publication ID |
https://doi.org/ 10.4202/app.00289.2016 |
persistent identifier |
https://treatment.plazi.org/id/03AD87A8-FFCB-6D77-FF06-FEBC641E8755 |
treatment provided by |
Felipe |
scientific name |
Cupitheca sp. |
status |
|
Fig. 51K.
Material.—Two internal moulds, including figured SMNH X5859,from sample5a/17.5(section96-5a, Fig.2 View Fig ),Emyaksin Formation, eastern Anabar Uplift, Siberian Platform, Russia. Correlated with lower part of Cambrian Stage 2.
Remarks.—The fossils are represented by fragments of internal moulds with longitudinal striation, broadly oval to nearly circular cross-section, and hemispherical narrower end formed by a septum. They are most similar to Actinotheca mira (He in Qian, 1977) from the middle Meishucunian Stage of South China (see discussion of the genera Actinotheca Xiao and Zhou, 1984 and Cupitheca by Bengtson et al. 1990: 203; Gravestock et al. 2001: 97), but have a less prominent blunt termination. Cupitheca mira is also reported from the Tommotian and Atdabanian stages of the Siberian Platform (Parkhaev and Demidenko 2010: 951). Cupitheca sp. is herein interpreted as an orthothecid hyolith with a hemispherical, apically convex septum. A similar fragment of an internal mould, albeit with an oval and less prominent terminal septum, was illustrated by Kouchinsky et al. (2015a: fig. 25D) as Loculitheca ? sp. from the Atdabanian beds of the Emyaksin Formation (section 96-7 therein).
SMNH |
Department of Paleozoology, Swedish Museum of Natural History |
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