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Paraconularia derwentensis
Taxonomy
Conularia derwentensis was named by Johnston (1887). It is a 3D body fossil. Its type locality is Bridgewater limestone (Tasmanian museum), which is in a Kungurian carbonate wackestone in the Berriedale Formation of Australia.
It was recombined as Paraconularia derwentensis by Waterhouse (1979), Waterhouse (1986) and Parfrey (1988).
It was recombined as Paraconularia derwentensis by Waterhouse (1979), Waterhouse (1986) and Parfrey (1988).
Sister species lacking formal opinion data
Synonymy list
| Year | Name and author |
|---|---|
| 1887 | Conularia derwentensis Johnston p. 17 |
| 1938 | Conularia derwentensis Fletcher p. 253 figs. Pl 26, fig 9 |
| 1979 | Paraconularia derwentensis Waterhouse p. 480 figs. 1.1-1.6 |
| 1986 | Paraconularia derwentensis Waterhouse p. 15 figs. Pl 1, figs 7,9,12; pl 15, fig 1 |
| 1988 | Paraconularia derwentensis Parfrey p. 9 figs. Pl 2, fig 6 |
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If no rank is listed, the taxon is considered an unranked clade in modern classifications. Ranks may be repeated or presented in the wrong order because authors working on different parts of the classification may disagree about how to rank taxa.
†Paraconularia derwentensis Johnston 1887
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Diagnosis
No diagnoses are available