Basic info | Taxonomic history | Classification | Included Taxa |
Morphology | Ecology and taphonomy | External Literature Search | Age range and collections |
Adunator meizon
Taxonomy
Diacocherus meizon was named by Gingerich (1983) [NOT the genotype]. Its type locality is Cedar Point Quarry, which is in a Tiffanian fluvial-lacustrine siliciclastic in the Fort Union Formation of Wyoming.
It was recombined as Adunator meizon by Secord (2008).
It was recombined as Adunator meizon by Secord (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.
†Adunator meizon Gingerich 1983
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
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Source: o = order, subc = subclass, subp = subphylum, p = phylum | |||||
References: Carroll 1988, Nowak 1999, Kiessling 2004, Lillegraven 1979, Ji et al. 2002 |
Age range: Tiffanian or 60.90000 to 56.20000 Ma
Collections (5 total)
Time interval | Ma | Country or state | Original ID and collection number |
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Ti4 | Canada (Saskatchewan) | Diacocherus meizon (14978) | |
Tiffanian | Canada (Alberta) | Diacocherus meizon (14934) Diacocherus minutus (14995) | |
Tiffanian | USA (Wyoming) | Diacocherus meizon (14936) Mckennatherium ladae (type locality: 15017) |