Jumudontus gananda Cooper, 1981
publication ID |
https://doi.org/ 10.3853/j.0067-1975.55.2003.1383 |
persistent identifier |
https://treatment.plazi.org/id/37439A20-CB36-FF20-FC46-FBF1FB0EF813 |
treatment provided by |
Felipe |
scientific name |
Jumudontus gananda Cooper, 1981 |
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Jumudontus gananda Cooper, 1981
Fig. 18H–J View Fig
Jumudontus gananda Cooper, 1981: 170 , pl. 31, fig. 13.
Jumudontus gananda .– Nicoll, 1992: 216–223, figs. 4–8 (cum syn.).
Jumudontus gananda .– Pohler, 1994, pl. 3, figs. 15, 16.
New genus A n. sp. 1 s.f. Pohler, 1994: 42, pl. 7, fig. 29, text-fig. 15T,U (= S elements ).
New genus A n. sp. 2 s.f. Pohler, 1994: 42, pl. 7, figs. 27, 28, textfig. 15R,S (= Pb element).
New genus C n. sp. 1 s.f. Pohler, 1994: 43, pl. 7, fig. 26, text-fig. 15X (= Pb element).
Jumudontus gananda .–Johnston & Barnes, 2000, pl. 4, fig. 22.
Jumudontus gananda ?.–Zhen et al., in press: pl. 3, fig. 19 (cum syn.).
Material. Six specimens (all Pa) from the Tabita Formation at Mount Arrowsmith, and eleven specimens (10 Pa, 1 Pb) from unnamed dolomitic limestone unit at Koonenberry Gap .
Remarks. Jumudontus gananda was originally described ( Cooper, 1981) as a form species with only the Pa element recognized from the Horn Valley Siltstone of the Amadeus Basin. Nicoll (1992) revised the species as consisting of a septimembrate coniform-pectiniform apparatus, also based on a collection from the Horn Valley Siltstone, with a recovered element ratio of 60(Pa):21(Pb):2(M):1(Sa): 5(Sb): 3(Sc):8(Sd). In samples from western New South Wales, the species is comparatively rare, and only the more common Pa and Pb elements were recovered. Pohler (1994) briefly documented some Pb and S elements of this species, assigning them to three informal form species without knowledge of Nicoll’s (1992) revision.
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Jumudontus gananda Cooper, 1981
Zhen, Yong Yi, Percival, Ian G. & Webby, Barry D. 2003 |
Jumudontus gananda
Nicoll, R 1992: 216 |
Jumudontus gananda
Cooper, B 1981: 170 |