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Graciliceratops mongoliensis
Taxonomy
Graciliceratops mongoliensis was named by Sereno (2000). It is a 3D body fossil. Its type locality is Shiregin Gashun (PMPE), which is in a Cenomanian/Santonian terrestrial horizon in the Baynshire Formation of Mongolia. It is the type species of Graciliceratops.
Synonymy list
Year | Name and author |
---|---|
2000 | Graciliceratops mongoliensis Sereno |
2001 | Graciliceratops mongoliensis Lambert et al. p. 6 |
2003 | Graciliceratops mongoliensis Tereshchenko and Alifanov p. 301 |
2004 | Graciliceratops mongoliensis You and Dodson p. 480 |
2008 | Graciliceratops mongoliensis Alifanov p. 622 |
2009 | Graciliceratops mongoliensis Butler and Sullivan p. 30 |
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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.
†Graciliceratops mongoliensis Sereno 2000
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
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Source: subo = suborder, o = order | |||||
References: Marsh 1875, Norman and Weishampel 1991 |
Age range: base of the Cenomanian to the top of the Santonian or 100.50000 to 83.60000 Ma
Collections: one only
Time interval | Ma | Country or state | Original ID and collection number |
---|---|---|---|
Cenomanian - Santonian | Mongolia (Omnogov) | Microceratops gobiensis (type locality: 13411) |