Selindeochrea tricarinata
publication ID |
https://doi.org/ 10.4202/app.00289.2016 |
persistent identifier |
https://treatment.plazi.org/id/03AD87A8-FFFD-6D41-FF06-FAC263C5860B |
treatment provided by |
Felipe |
scientific name |
Selindeochrea tricarinata |
status |
|
Selindeochrea tricarinata (Missarzhevsky in Rozanov et al., 1969)
Fig. 69 View Fig .
Material.— Over 50 specimens, including figured SMNH X3412 View Materials , 5978 View Materials , 5980–5982 View Materials , from samples K2/21, K2/25, K2/50, 3/12, and 3/12.2 (section 3, Fig. 3), Medvezhya Formation , western Anabar Uplift , Siberian Platform , Russia. Correlated with the upper Fortunian and lowermost Cambrian Stage 2 .
Description.—Slowly expanding slightly curved tubes with tri-lobate cross-sections, slightly twisted clockwise (from apex to the aperture, in the direction of growth). Grooves (depressions) between extended lobes are wide and shallow with flattened middle part. There is a narrow median ridge on the flattened depressions between the lobes (as replicated by internal moulds). In the flattened depressions, the growth lines are arched and point at an acute angle towards the aperture. In preserved thecae, the lobes are extended distally by prominent keels. The keels undulate, with folds running towards the aperture at ca. 45°. The lobes of the internal moulds are rounded or somewhat swollen and almost straight.
Stratigraphic and geographic range.— Upper Fortunian– lower part of Cambrian Stage 2 of the Siberian Platform.
SMNH |
Department of Paleozoology, Swedish Museum of Natural History |
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