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Paracimexomys magnus
Taxonomy
Cimexomys magnus was named by Sahni (1972). Its type locality is Clambank Hollow Quarry, which is in a Campanian/Campanian fine channel fill claystone in the Judith River Formation of Montana.
It was recombined as Paracimexomys magnus by Archibald (1982).
It was recombined as Paracimexomys magnus by Archibald (1982).
Sister species lacking formal opinion data
Synonymy list
Year | Name and author |
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1972 | Cimexomys magnus Sahni |
1979 | Cimexomys magnus Clemens and Kielan-Jaworowska p. 101 |
1982 | Paracimexomys magnus Archibald |
2004 | Cimexomys magnus Kielan-Jaworowska et al. pp. 254, 320-321 |
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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.
†Paracimexomys magnus Sahni 1972
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
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Source: o = order, c = class, subp = subphylum | |||||
References: Hopson 1973, Carroll 1988, Hendy et al. 2009, Jenkins and Krause 1983 |
Age range: base of the Middle Campanian to the top of the Late/Upper Campanian or 83.50000 to 70.60000 Ma
Collections (2 total)
Time interval | Ma | Country or state | Original ID and collection number |
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Judithian | USA (Utah) | Paracimexomys magnus (14467) | |
Middle Campanian - Late/Upper Campanian | USA (Montana) | Cimexomys magnus (type locality: 14446) |