Scolopodus quadratus Pander, 1856

Zhen, Yong Yi, Percival, Ian G. & Webby, Barry D., 2003, Early Ordovician Conodonts from Far Western New South Wales, Australia, Records of the Australian Museum 55 (2), pp. 169-220 : 212

publication ID

https://doi.org/ 10.3853/j.0067-1975.55.2003.1383

persistent identifier

https://treatment.plazi.org/id/37439A20-CB00-FF16-FC47-FE35FAE3F9AC

treatment provided by

Felipe

scientific name

Scolopodus quadratus Pander, 1856
status

 

Scolopodus quadratus Pander, 1856

Fig. 27A–O View Fig

Scolopodus quadratus Pander, 1856: 26 , pl. 2, fig. 6a–d, pl.A, fig. 5d.

Scolopodus costatus Pander, 1856: 26 , pl. 2, fig. 7a–d, pl.A, fig. 5e.

Scolopodus striatus Pander, 1856: 26 , pl. 2, fig. 8a–d, pl. A, fig. 5f.

Scolopodus rex Lindström, 1955: 595 , 596, pl. 3, fig. 32.

Scolopodus rex var. paltodiformis Lindström, 1955: 596 , pl. 3, figs. 33, 34.

Scolopodus quadratus .– Fåhraeus, 1982: 21, pl. 2, figs. 1–14, pl. 3, figs. 1–8, 15.

Scolopodus rex .– Seo et al., 1994, fig. 10.10–10.12.

Scolopodus rex .–Albanesi, in Albanesi et al., 1998: 133, pl. 12, figs. 14–17 (cum syn.).

Scolopodus quadratus .–Zhen et al., in press: pl. 5, figs. 15–21 (cum syn.).

Material. One specimen (Sd) from limestone nodules within shales of the upper Yandaminta Quartzite and 37 specimens (4 Pb, 12 Sa, 12 Sb, 1 Sc, 8 Sd) from the overlying Tabita Formation at Mount Arrowsmith ; two specimens (1 Sa, 1 Sd) from the unnamed dolomitic limestone unit at Koonenberry Gap .

Remarks. Five element types have been recovered from the Tabita Formation, including a scandodiform Pb element with a proclined cusp, four costae on the inner lateral face and a smooth outer lateral face ( Fig. 27A–C View Fig ), and four scolopodiform elements: the symmetrical Sa ( Fig. 27D–F View Fig ), nearly symmetrical Sb ( Fig. 27G–I View Fig ), laterally compressed nearly symmetrical Sc element ( Fig. 27M–O View Fig ), and asymmetrical Sd element with slightly twisted cusp ( Fig. 27J–L View Fig ). However, the species is highly variable, and there are intermediate morphotypes varying in the number of costae, symmetry, curvature of the cusp, and degree of lateral compression. Scolopodus quadratus also occurs in the slightly older Hensleigh Siltstone of the Lachlan Fold Belt (Zhen et al., in press).

Triangulodus van Wamel, 1974

Type species. Paltodus volchovensis Sergeeva, 1963 .

Kingdom

Animalia

Phylum

Chordata

Class

Conodonta

Order

Protopanderodontida

Family

Strachanognathidae

Genus

Scolopodus

Loc

Scolopodus quadratus Pander, 1856

Zhen, Yong Yi, Percival, Ian G. & Webby, Barry D. 2003
2003
Loc

Scolopodus rex

Albanesi, G 1998: 133
1998
Loc

Scolopodus quadratus

Fahraeus, L 1982: 21
1982
Loc

Scolopodus rex Lindström, 1955: 595

Lindstrom, M 1955: 595
1955
Loc

Scolopodus rex var. paltodiformis Lindström, 1955: 596

Lindstrom, M 1955: 596
1955
Loc

Scolopodus quadratus

Pander, C 1856: 26
1856
Loc

Scolopodus costatus

Pander, C 1856: 26
1856
Loc

Scolopodus striatus

Pander, C 1856: 26
1856
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