Philoxenella spiralis Vostokova, 1962

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 : 351

publication ID

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

persistent identifier

https://treatment.plazi.org/id/03AD87A8-FFB3-6D0F-FCCF-FF62620F8700

treatment provided by

Felipe

scientific name

Philoxenella spiralis Vostokova, 1962
status

 

Philoxenella spiralis Vostokova, 1962 View in CoL

Fig. 24D, E.

Material.—22 internal moulds, including figured SMNH Mo182287 and 182288, from samples 1/29.2 (section 1, Fig. 4 View Fig ) and 3/22.5, K2/52, and K2/60 (section 3, Fig. 3), Medvezhya and basal Kugda-Yuryakh formations, Anabar Uplift, Siberian Platform, Russia. Correlated with Cambrian Stage 2.

Description.—Shell up to 1.3 mm in diameter, dextrally coiled, up to 1.5 moderately expanding whorls with a broadly oval cross-section. The inner shell surface (as replicated by the available internal moulds) is smooth.

Remarks.—Internal moulds of Philoxenella are morphologically identical to those of Barskovia Golubev, 1976 (Fig. 24A–C, F, G), although the latter is sinistral (see below). Parkhaev (2007a, b) tentatively regarded them as dextral and sinistral variants of the same species and assigned them to the family Khairkhaniidae Missarzhevsky, 1989 . This attribution is corroborated by probably similar microstructures of the conch, which is perforated by canals (Parkhaev 2006, 2007b). Philoxenella differs from Aldanella , which lacks canals in its conch walls, in being relatively loosely coiled and with lower rate of shell expansion.

Stratigraphic and geographic range.— Cambrian Stage 2 of the Siberian Platform and probably Avalonia (see Landing 1996: fig. 5b, c).

SMNH

Department of Paleozoology, Swedish Museum of Natural History

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