Chlupacina sp.

Baliński, Andrzej, 2012, The brachiopod succession through the Silurian-Devonian boundary beds at Dnistrove, Podolia, Ukraine, Acta Palaeontologica Polonica 57 (4), pp. 897-924 : 906

publication ID

https://doi.org/ 10.4202/app.2011.0138

persistent identifier

https://treatment.plazi.org/id/03E20437-BD52-FFEB-FCA8-FC42908DF8BA

treatment provided by

Felipe

scientific name

Chlupacina sp.
status

 

Chlupacina sp.

Fig. 5K, L View Fig .

Material.—11 mostly incomplete specimens embedded in rock was found at 5.5 m above the S–D boundary (beds 47–48).

Remarks.—The collection is small and poorly preserved. The specimens show radial ornament which is weak to absent posteriorly and better developed peripherally. The characteristic stronger median costa is usually well developed and reaches the anterior margin. On one specimen a 2.8 mm long (117% of the valve length), proximally cyrtomorph intraverse and distally gently arched spine is well preserved ( Fig. 5L View Fig ). Although preservation of spines on the studied specimens is rare, it seems that they are developed on the right side of the ventral valve only.

The present specimens differ from all chonetoid species known from the Siluro–Devonian of Podolia. The former resembles externally Pseudostrophochonetes mediocostalis ( Kozłowski, 1929) from the lower Chortkiv Horizon (former Bogdanovka Beds) in having distinct median costa, but differs mainly in thicker shell ribbing and a much older stratigraphic range. Small shell dimensions, presence of distinct median costa, and long spine developed on one side of the hinge line only suggest that the specimens from the studied section may be Chlupacina . Unfortunately, the paucity of the material and unknown internal shell structure does not allow for a more detailed determination.

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