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| Morphology | Ecology and taphonomy | External Literature Search | Age range and collections |
Talahphiomys lavocati
Taxonomy
Phiomys lavocati was named by Wood (1968). It is a 3D body fossil. Its type locality is Quarry E (Jebel Qatrani Formation), which is in a Rupelian fluvial sandstone/mudstone in the Jebel Qatrani Formation of Egypt.
It was recombined as Talahphiomys lavocati by Jaeger et al. (2010), Marivaux et al. (2017).
It was recombined as Talahphiomys lavocati by Jaeger et al. (2010), Marivaux et al. (2017).
Synonymy list
| Year | Name and author |
|---|---|
| 1968 | Phiomys lavocati Wood |
| 2010 | Talahphiomys lavocati Jaeger et al. |
| 2017 | Talahphiomys lavocati Marivaux et al. |
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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.
†Talahphiomys lavocati Wood 1968
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
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| Source: o = order, subc = subclass, c = class, subp = subphylum | |||||
| References: Nowak 1999, Ji et al. 2002, Lillegraven 1979, Carroll 1988, Hendy et al. 2009 | |||||
Age range: base of the Bartonian to the top of the Early/Lower Oligocene or 41.03000 to 27.30000 Ma
Collections (7 total)
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Middle Eocene - Late/Upper Eocene | Libya (Sirt) | Talahphiomys lavocati (175362) | |
| Bartonian | Namibia (Sperrgebiet) | Phiomys lavocati (165176) | |
| Early/Lower Oligocene | Libya | Talahphiomys lavocati (105925) | |
| Early/Lower Oligocene | Oman (Dhofar) | Phiomys lavocati (162464 175334) | |
| Rupelian | Egypt (Fayum) | Phiomys lavocati (12968 60127) |