Fomitchella acinaciformis Missarzhevsky, 1977
publication ID |
https://doi.org/ 10.4202/app.00289.2016 |
persistent identifier |
https://treatment.plazi.org/id/03AD87A8-FFFA-6D46-FFF3-FD49640D8479 |
treatment provided by |
Felipe |
scientific name |
Fomitchella acinaciformis Missarzhevsky, 1977 |
status |
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Fomitchella acinaciformis Missarzhevsky, 1977
Figs. 66F, G View Fig , 67 View Fig .
Material.—About 50 phosphatic sclerites, including figured SMNH X5959, 5960, 5962–5968, from samples 5a /17.5 and 5a/18.5 (section 96-5a, Fig. 2 View Fig ), Emyaksin Formation, eastern Anabar Uplift, Siberian Platform, Russia. Correlated with the lower part of Cambrian Stage 2.
Description.—Phosphatic, elongated, conical, hollow sclerites, gently curved and slightly compressed in a single plane. Apex somewhat more elongate, almost straight. Basal margin ovoid, lateral sides may have gentle longitudinal depression. Outer surface with radial striation or smooth. Inner surface smooth.
Remarks.—See Fomitchella infundibuliformis for comparison. The holotype of F. acinaciformis came from sample M314/5-10, a mixed sample collected by Vladimir V. Missarzhevsky from the lower Medvezhya Formation at a horizon located 5‒10 m above the base of section M314 Rozanov et al. 1969: 44, fig. 9). The type material of F. infundibuliformis (see above) was collected ca. 4 m above the base of section M314.
Two sclerites illustrated as Maldeotaia bandalica Singh and Shukla, 1981 , from the Watsonella crosbyi Zone of Avalonian southeast Newfoundland (Landing et al. 1989: fig. 7.5, 7.6) are morphologically comparable to Fomitchella acinaciformis and are brought to the latter species. This lowest occurrence in the Fortunian‒Cambrian Stage 2 transition interval is comparable to the species’ lowest known appearance in Siberia.
Stratigraphic and geographic range.—Terminal Fortunian‒ Cambrian Stage 2 of the Siberian Platform and, probably, western Mongolia (see Missarzhevsky 1977) and Avalonia Landing et al. 1989, discussed above).
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