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Palaeoloxodon lomolinoi
Taxonomy
Palaeoloxodon lomolinoi was named by van der Geer et al. (2014). Its type specimen is AMPG 999, a maxilla (isolated maxilla preserving both third molars ), and it is a 3D body fossil. Its type locality is near Trypiti River, which is in a Pleistocene terrestrial sandstone in Greece.
Sister species lacking formal opinion data
Synonymy list
| Year | Name and author |
|---|---|
| 2014 | Palaeoloxodon lomolinoi van der Geer et al. |
| 2018 | Palaeoloxodon lomolinoi Athanassiou et al. |
| 2019 | Palaeoloxodon lomolinoi Athanassiou 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.
†Palaeoloxodon lomolinoi van der Geer et al. 2014
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Diagnosis
| Reference | Diagnosis | |
|---|---|---|
| A. van der Geer et al. 2014 | Palaeoloxodon lomolinoi is about ten percent the body mass of Palaeoloxodon antiquus, has a higher lamellar frequency and thicker enamel. It differs from Palaeoloxodon creutzburgi, Palaeoloxodon ‘mnaidriensis’ and P. sp. from Delos in its greater size reduction. It differs from Palaeoloxodon cypriotes and Palaeoloxodon falconeri (Spinagallo, Sicily) in its lesser size reduction. Palaeoloxodon lomolinoi has thicker enamel (ranging between 2 and 3 mm) than all other Mediterranean dwarf Palaeoloxodon, except for Palaeoloxodon tiliensis. |
Measurements
No measurements are available
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| Source: f = family, subc = subclass, c = class, subp = subphylum | |||||
| References: Ji et al. 2002, Carroll 1988, Lillegraven 1979, Hendy et al. 2009, Nowak 1991 | |||||
Age range: Late/Upper Pleistocene or 0.12900 to 0.01170 Ma
Collections: one only
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Late/Upper Pleistocene | Greece (Naxos) | Palaeoloxodon lomolinoi (type locality: 203848) |