Colpantyx Pojeta and Gilbert-Tomlinson, 1977

Jakobsen, Kristian G., Brock, Glenn A., Nielsen, Arne T. & Harper, David A. T., 2016, A Darriwilian (Middle Ordovician) bivalve-dominated molluscan fauna from the Stairway Sandstone, Amadeus Basin, central Australia, Acta Palaeontologica Polonica 61 (4), pp. 897-924 : 916-917

publication ID

https://doi.org/ 10.4202/app.00215.2015

persistent identifier

https://treatment.plazi.org/id/03A787E2-FFEC-FFE7-FCF4-FCF7959CFF53

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scientific name

Colpantyx Pojeta and Gilbert-Tomlinson, 1977
status

 

Genus Colpantyx Pojeta and Gilbert-Tomlinson, 1977

Type species: Colpantyx woolleyi Pojeta and Gilbert-Tomlinson, 1977 from the late Cambrian to Early Ordovician Pacoota Sandstone, Amadeus Basin, Australia; original designation .

Colpantyx ? sp. A

Fig. 12C, D View Fig .

Material.—10 fragmentary internal and external moulds found in beds A +1 to A + 3 in the Areyonga Gorge section only ( Fig. 4 View Fig ), Middle Ordovician of Australia. The two figured specimens ( CPC 41483 and CPC 41484) are latex casts made from external moulds.

Description.—Small slightly rounded triangular colpomyid with well-defined umbonal radial ribs, of which two are present anteriorly and one posteriorly ( Fig. 12D View Fig ). Except for radial ribs the surface appears smooth. Anterior ribs short and almost straight, radiating until they reach anterior-most part of ventral margin. Posterior rib long and curving towards posterior margin. Anterior and ventral margins straight to broadly rounded; posterior margin straight, oblique towards dorsum. Umbo subdued ( Fig. 12C View Fig ) and shell profile low.

Remarks.— Colpantyx is endemic to Australia. The only other species assigned is Colpantyx woolleyi Pojeta and Gilbert-Tomlinson, 1977 from the upper Tremadocian part of the Pacoota Sandstone of the Amadeus Basin (e.g., Shergold 1991; Cope 2004).

The slightly rounded triangular overall shape, the radial well-defined umbonal ribs and the delineation of the margins are quite similar among the two Colpantyx species. However, C. woolleyi has pronounced commarginal ornament and only one or two posterior umbonal radial ribs. Furthermore the posteroventral margin is sinuous between the ribs. In comparison Colpantyx ? sp. A possesses a smooth surface completely lacking commarginal ornament. It is unknown whether these differences are due to preservational artefacts, as the material from the Stairway Sandstone is dolomitized. The posteroventral margin is somewhat sinuous between the ribs but not nearly as pronounced as observed on C. woolleyi . The three umbonal ribs present on Colpantyx ? sp. A are very consistent and differ from the condition in C. woolleyi where only one or two ribs are developed (compare Fig. 12D View Fig vs. Pojeta and Gilbert-Tomlinson 1977: pl. 24).

The related species Colpantyx woolleyi occurs in the Pacoota Sandstone at 11 different localities in the Amadeus Basin (Pojeta and Gilbert-Tomlinson 1977: 28). When more material from the Stairway Sandstone becomes available the generic assignment should be investigated, and if identified with confidence as Colpantyx , the range of this genus should be extended from the Tremadocian into the Darriwilian.

CPC

Culture collection of Pedro Crous

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