Fomitchella acinaciformis Missarzhevsky, 1977

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 : 408

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

 

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).

Darwin Core Archive (for parent article) View in SIBiLS Plain XML RDF