Protowenella flemingi Runnegar and Jell, 1976
publication ID |
https://doi.org/ 10.4202/app.00930.2021 |
persistent identifier |
https://treatment.plazi.org/id/03B4442D-F84D-FFD6-7AB5-16A4FC20FCC7 |
treatment provided by |
Felipe |
scientific name |
Protowenella flemingi Runnegar and Jell, 1976 |
status |
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Protowenella flemingi Runnegar and Jell, 1976 View in CoL
Fig. 24I View Fig .
Material.—Several calcium phosphatic and glauconised internal moulds, including figured SMNH Mo194712, from sample 22/50, Sekten Formation, Lena River, Siberia, Russia. Upper Toyonian stage (correlated with the Cambrian Stage 4).
Description.—Planispiral calcium phosphatic internal mould, ca. 0.5 mm in size, coiled through half of a whorl, with rounded cross-section and globose initial part. Subapical side of the mould is delimited by a symmetrically located pair of shallow diverging grooves, termed circumbilical channels.
Remarks.— Peel (2021b) described Protowenella flemingi from the Wuliuan Stage of Greenland with an in-place operculum of a hyolith-type and suggested affinity with orthothecid hyoliths. This is corroborated by presence of planispirally coiled forms among early–middle Cambrian hyoliths (Feng et al. 2001; Kouchinsky et al. 2011; and herein).
Stratigraphic and geographic range.— Cambrian Stage 4– Drumian Stage, Siberian Platform ( Russia), Cambrian
Series 2 of North China and Miaolingian Series of Australia, Laurentia and Bornholm (Baltica) (see Li et al. 2019 for discussion).
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