Hyolithellus sp.

Kouchinsky, Artem, Bengtson, Stefan, Landing, Ed, Steiner, Michael, Vendrasco, Michael & Ziegler, Karen, 2017, Terreneuvian stratigraphy and faunas from the Anabar Uplift, Siberia, Acta Palaeontologica Polonica 62 (2), pp. 311-440 : 411-412

publication ID

https://doi.org/ 10.4202/app.00289.2016

persistent identifier

https://treatment.plazi.org/id/03AD87A8-FFFF-6D42-FCCF-F89263708210

treatment provided by

Felipe

scientific name

Hyolithellus sp.
status

 

Hyolithellus sp.

Fig. 68B, D–F, H, I View Fig .

Material.—25 fragmentary phosphatic tubes, including SMNH X5970, 5972, 5973, 5975–5977, from samples K2/6 and K2/60 (section 2, Fig. 1), 1/28.5 (section 1, Fig. 4 View Fig ), 5a/6, 5a/34.5, and 5a/34.75 (section 96-5a, Fig. 2 View Fig ), Medvezhya and Emyaksin formations, Anabar Uplift, Siberian Platform, Russia. Correlated with the upper Fortunian and lower part of Cambrian Stage 2.

Description.—Slightly irregularly curved tubes with circular cross-section, 150–200 μm in diameter. External surface smooth, with faint transverse folds perpendicular to the longitudinal axis of the tube.

Remarks.—The form is distinguished from Hyolithellus vladimirovae by the smaller size of its tubes and subdued transverse rugae. Deformation of some tubes ( Fig. 68D View Fig ) indicates that the original material of the tube was relatively flexible and, thus, phosphatization likely was, in part, secondary. See Kouchinsky et al. (2012: online appendix 1) for the first occurrences of hyolithelminths worldwide.

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