| Basic info | Taxonomic history | Classification | Included Taxa |
| Morphology | Ecology and taphonomy | External Literature Search | Age range and collections |
Fanimus ultimus
Taxonomy
Fanimus ultimus was named by Korth et al. (1990). Its type locality is Hemingford Quarry 7B, which is in a Hemingfordian terrestrial horizon in the Runningwater Formation of Nebraska.
Synonymy list
| Year | Name and author |
|---|---|
| 1990 | Fanimus ultimus Korth 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.
†Fanimus ultimus Korth et al. 1990
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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: Lillegraven 1979, Nowak 1999, Carroll 1988, Ji et al. 2002, Hendy et al. 2009 | |||||
Age range: Early/Lower Hemingfordian or 20.43000 to 15.97000 Ma
Collections (2 total)
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Early/Lower Hemingfordian | USA (Nebraska) | Fanimus ultimus (type locality: 17934 69808) |