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Tataromys plicidens
Taxonomy
Tataromys plicidens was named by Matthew and Granger (1923). Its type specimen is AMNH 19082, a maxilla, and it is a 3D body fossil. Its type locality is Loh, which is in an Oligocene terrestrial horizon in the Hsanda Gol Formation of Mongolia. It is the type species of Tataromys.
Synonymy list
Year | Name and author |
---|---|
1923 | Tataromys plicidens Matthew and Granger |
2006 | Tataromys plicidens Vianey-Liaud 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.
†Tataromys plicidens Matthew and Granger 1923
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
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Source: f = family, subc = subclass, c = class, subp = subphylum | |||||
References: Lillegraven 1979, Ji et al. 2002, Nowak 1999, Hendy et al. 2009, Carroll 1988 |
Age range: base of the Early/Lower Oligocene to the top of the Late/Upper Oligocene or 33.90000 to 23.03000 Ma
Collections (15 total)
Time interval | Ma | Country or state | Original ID and collection number |
---|---|---|---|
Early/Lower Oligocene | Mongolia | Tataromys plicidens (type locality: 53979) | |
Early/Lower Oligocene | China (Gansu) | Tataromys plicidens (182899) | |
Early/Lower Oligocene | China (Nei Mongol) | Tataromys plicidens (174759 175386 175387 175406) | |
Early/Lower Oligocene | China (Ningxia) | Tataromys plicidens (182895) | |
Late/Upper Oligocene | Mongolia | Tataromys plicidens (75599) | |
Late/Upper Oligocene | China (Nei Mongol) | Tataromys plicidens (175408 175409 175411) | |
Late/Upper Oligocene | China (Gansu) | Tataromys plicidens (176451 176453) | |
Late/Upper Oligocene | Mongolia (Övörkhangai) | Tataromys plicidens (182075 182077) |