Basic info | Taxonomic history | Classification | Included Taxa |
Morphology | Ecology and taphonomy | External Literature Search | Age range and collections |
Anchitheriomys stouti
Taxonomy
Anchitheriomys stouti was named by Korth (2001). It is not a trace fossil. Its type locality is Dunlap Camel Quarry, which is in a Hemingfordian terrestrial horizon in the Runningwater Formation of Nebraska.
Synonymy list
Year | Name and author |
---|---|
2001 | Anchitheriomys stouti Korth |
Is something missing? Join the Paleobiology Database and enter the data
|
|
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.
†Anchitheriomys stouti Korth 2001
show all | hide all
Diagnosis
No diagnoses are available
Measurements
No measurements are available
|
|
||||
|
|
||||
|
|
||||
|
|
||||
Source: f = family, subc = subclass, c = class, subp = subphylum | |||||
References: Carroll 1988, Nowak 1991, Ji et al. 2002, Lillegraven 1979, Hendy et al. 2009 |
Age range: Early/Lower Hemingfordian or 20.43000 to 15.97000 Ma
Collections: one only
Time interval | Ma | Country or state | Original ID and collection number |
---|---|---|---|
Early/Lower Hemingfordian | USA (Nebraska) | Anchitheriomys stouti (type locality: 17898) |