Linevitus? minutus Missarzhevsky

Kouchinsky, Artem, Bengtson, Stefan, Clausen, Sébastien & Vendrasco, Michael J., 2015, An early Cambrian fauna of skeletal fossils from the Emyaksin Formation, northern Siberia, Acta Palaeontologica Polonica 60 (2), pp. 421-512 : 454-455

publication ID

https://doi.org/ 10.4202/app.2012.0004

persistent identifier

https://treatment.plazi.org/id/03C3891D-150D-C250-FCBF-F9D6CC77F99E

treatment provided by

Felipe

scientific name

Linevitus? minutus Missarzhevsky
status

 

Linevitus? minutus Missarzhevsky in Rozanov and Missarzhevsky, 1966

Fig. 27G, J View Fig .

Material.— Single specimen from sample 7/30, three specimens, including SMNH X 4657 View Materials , from sample 7/31.5 and four specimens from sample 7/31.9; correlated with the Delgadella anabara Zone, Atdabanian Stage. One specimen, SMNH X 4658 View Materials , from sample 7/70; Calodiscus - Erbiella Zone, lower Botoman Stage. Emyaksin Formation, Bol’shaya Kuonamka River .

Description.—Conch straight sided, with a sub-triangular cross-section. Dorsal surface rounded in the middle, with flanks dipping towards rounded lateral longitudinal ridges, grading into a slightly convex ventral surface. In dorsal view, the apical angle is ca. 30°. The conch is covered with transverse growth lines slightly curved towards the apex on dorsum. On venter, the growth lines are strongly curved towards the aperture and parallel with the edge of a long semi-circular ligula. Growth lines produce small lateral sinuses.Apical end not preserved.

Remarks.—This is very similar to the holotype of Linevitus minutus Missarzhevsky illustrated by Rozanov and Missarzhevsky (1966: 108, pl. 11: 7, 8; John Malinky, personnal communication in 2008), from the Tommotian Stage of Siberia. The curvature towards dorsum seen in the species is not apparent in the fragments available. The fossils are also similar to Hyolithida indet. 3 ( Kouchinsky et al. 2011: fig. 11G–I).

SMNH

Department of Paleozoology, Swedish Museum of Natural History

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