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Procidaris edwardsii
Taxonomy
Cidaris edwardsii was named by Wright (1854). Its type specimen is NHM 75689, a test, and it is a 3D body fossil. Its type locality is Mickleton Tunnel, near Chipping Campden, which is in a Davoei transition zone/lower shoreface shale in the Charmouth Mudstone Formation of the United Kingdom. It is the type species of Procidaris.
It was recombined as Procidaris edwardsii by Smith (2015).
It was recombined as Procidaris edwardsii by Smith (2015).
Synonymy list
| Year | Name and author |
|---|---|
| 1854 | Cidaris edwardsii Wright |
| 2015 | Procidaris edwardsii Smith p. 9 figs. Pl 3, figs 2,3; text-fig 2B |
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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.
†Procidaris edwardsii Wright 1854
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
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| Source: o = order, c = class, p = phylum | |||||
| References: Aberhan 1992, Kiessling 2004 | |||||
Age range: base of the Hettangian to the top of the Davoei or 201.30000 to 183.00000 Ma
Collections (4 total)
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Hettangian | United Kingdom (England) | Cidaris edwardsii (149321) | |
| Davoei | United Kingdom (England) | Cidaris edwardsii (33336) | |
| Early/Lower Pliensbachian | United Kingdom | Procidaris edwardsii (195950) | |
| Margaritatus | United Kingdom (England) | Procidaris edwardsii (59033) |