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Glasbius intricatus
Taxonomy
Glasbius intricatus was named by Clemens (1966). Its type specimen is UCMP 48047 and is not a trace fossil. Its type locality is Bushy Tailed Blowout, which is in a Lancian terrestrial shale in the Lance Formation of Wyoming. It is the type species of Glasbius.
Synonymy list
| Year | Name and author |
|---|---|
| 1966 | Glasbius intricatus Clemens |
| 1979 | Glasbius intricatus Clemens p. 193 |
| 2004 | Glasbius intricatus Kielan-Jaworowska et al. pp. 443, 462 |
| 2007 | Glasbius intricatus Davis p. 247 |
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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.
†Glasbius intricatus Clemens 1966
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
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| Source: g = genus, subc = subclass, c = class, subp = subphylum | |||||
| References: Hopson 1973, Clemens 1979, Lillegraven 1979, Hendy et al. 2009, Carroll 1988 | |||||
Age range: Late/Upper Maastrichtian or 70.60000 to 66.00000 Ma
Collections (4 total)
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Lancian | USA (Wyoming) | Glasbius intricatus (type locality: 14519 14522) | |
| Late/Upper Maastrichtian | USA (Wyoming) | Glasbius intricatus (14585) | |
| Late/Upper Maastrichtian | USA (New Mexico) | Glasbius intricatus (59068) |