Basic info | Taxonomic history | Classification | Included Taxa |
Morphology | Ecology and taphonomy | External Literature Search | Age range and collections |
Taxonomy
Pseudoceras klausi was named by Frick (1937) [species not even mentioned by Webb 1998a]. Its type specimen is F:AM 31997, a mandible (right ramus), and it is a 3D body fossil. Its type locality is Round Mountain Quarry, which is in a Clarendonian terrestrial horizon in the referred Chamita Formation of New Mexico.
It was recombined as Floridameryx klausi by Webb (2008).
It was recombined as Floridameryx klausi by Webb (2008).
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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.
†Floridameryx klausi Frick 1937
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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, Carroll 1988, Hendy et al. 2009, Lillegraven 1979 |
Age range: Late/Upper Clarendonian or 12.50000 to 9.40000 Ma
Collections: one only
Time interval | Ma | Country or state | Original ID and collection number |
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Late/Upper Clarendonian | USA (New Mexico) | Pseudoceras sp. (type locality: 19528) |