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| Morphology | Ecology and taphonomy | External Literature Search | Age range and collections |
Doublatia pyriforme
Taxonomy
Doublatia pyriforme was named by Wass and Banks (1971). It is a 3D body fossil. Its type locality is Ray's Hill, St Marys, which is in an Artinskian carbonate limestone in the Enstone Park Formation of Australia.
Synonymy list
| Year | Name and author |
|---|---|
| 1971 | Doublatia pyriforme Wass and Banks p. 229 figs. Pl 37, figs 1-12,14,15; text-fig 2 |
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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.
†Doublatia pyriforme Wass and Banks 1971
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
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| Source: f = family, o = order, c = class | |||||
| References: Aberhan et al. 2004, Whittington et al. 1997, Fortey and Owens 1999 | |||||
Age range: Artinskian or 290.10000 to 279.30000 Ma
Collections (2 total)
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Artinskian | Australia (Tasmania) | Doublatia pyriforme (120242 type locality: 120244) |