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| Morphology | Ecology and taphonomy | External Literature Search | Age range and collections |
Pseudofaunus bravoensis
Taxonomy
Pseudofaunus bravoensis was named by Olsson (1931). Its type locality is Punta Bravo Grits at Caleto Sal, which is in an Oligocene marine sandstone/conglomerate in the Mancora Formation of Peru.
Synonymy list
| Year | Name and author |
|---|---|
| 1931 | Pseudofaunus bravoensis Olsson p. 86 figs. Plate 15, Figs. 9, 11 |
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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.
†Pseudofaunus bravoensis Olsson 1931
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
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| Source: f = family, superf = superfamily, c = class | |||||
| References: Kiessling 2004, Bush and Bambach 2015, Hendy et al. 2009 | |||||
Age range: base of the Priabonian to the top of the Early/Lower Oligocene or 38.00000 to 28.40000 Ma
Collections (2 total)
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Priabonian | Peru (Piura) | Pseudofaunus bravoensis (64544) | |
| Early/Lower Oligocene | Peru (Piura) | Pseudofaunus bravoensis (type locality: 55433) |