Conotheca cf. longiconica ( Qian, 1978 )
publication ID |
https://doi.org/ 10.4202/app.00930.2021 |
persistent identifier |
https://treatment.plazi.org/id/03B4442D-F84F-FFD4-7AB5-143FFDAEF842 |
treatment provided by |
Felipe |
scientific name |
Conotheca cf. longiconica ( Qian, 1978 ) |
status |
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Conotheca cf. longiconica ( Qian, 1978)
Fig. 40E, F View Fig .
Material.—Over 20 phosphatised conchs, including figured SMNH X11142 and 11143, from sample 19/25.5, Erkeket Formation, Khorbusuonka River, Toyonian stage (correlated with the Cambrian Stage 4) and samples 21/46.1, 21/51, 21/52, 21/54, Tyuser Formation, Lena River, Delgadella anabara – Nevadella Zone, Atdabanian stage (correlated with the Cambrian Stage 3). Siberia, Russia.
Description.—Conch gently curved in sagittal plane, with circular cross-section and straight aperture. Apical angle ca. 10°. Juvenile conch rounded blunt, not clearly separated. Wall porous consisting of a network of fibers, similarly to other hyoliths.
Remarks.—This form is more curved and slimmer than the holotype of C. mammilata . It occurs in the Cambrian Stages 2 and 3 of the Siberian Platform. Similar conchs are illustrated by Kouchinsky et al. (2015a: figs. 25E–G, 27E; 2017: fig. 52). Qian and Bengtson (1989) synonymised Circotheca longiconica Qian, 1978 , with Conotheca subcurvata ( Yu, 1974) . We support herein placement within Conotheca , but find difference between these two species. Conotheca longiconica ( Qian, 1978) has a conch regularly curved in a single plane, whereas Conotheca subcurvata shows irregular curvature (see Luo et al. 1984: pl. 7: 8).
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