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Erlikosaurus andrewsi
Taxonomy
Erlikosaurus andrewsi was named by Barsbold and Perle (1980). Its type specimen is GIN 100/111, a partial skeleton, and it is a 3D body fossil. Its type locality is Bayshin-Tsav [SMPE] (PIN coll. 100), which is in a Cenomanian/Santonian terrestrial horizon in the Baynshire Formation of Mongolia. It is the type species of Erlicosaurus. It was considered monophyletic by Currie (2000).
Synonymy list
Year | Name and author |
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1980 | Erlikosaurus andrewsi Barsbold and Perle |
1981 | Erlicosaurus andrewsi Perle |
1983 | Erlikosaurus andrewsi Barsbold p. 106 |
1992 | Erlicosaurus andrewsi Currie p. 247 |
1993 | Erlikosaurus andrewsi Clark et al. pp. 30A-31A |
1993 | Erlicosaurus andrewsi Currie and Eberth p. 138 |
1994 | Erlicosaurus andrewsi Clark et al. |
1994 | Erlikosaurus andrewsi Russell and Dong p. 2108 |
1995 | Erlikosaurus andrewsi Nessov p. 37 |
1997 | Erlikosaurus andrewsi Barsbold p. 448 |
1997 | Erlikosaurus andrewsi Varricchio p. 752 |
1998 | Erlicosaurus andrewsi Makovicky and Norell p. 12 |
2000 | Erlikosaurus andrewsi Currie p. 440 |
2002 | Erlicosaurus andrewsi Xu et al. p. 236 |
2003 | Erlikosaurus andrewsi Rauhut p. 41 |
2004 | Erlikosaurus andrewsi Clark et al. p. 152 |
2005 | Erlicosaurus andrewsi Kirkland et al. p. 90 |
2007 | Erlikosaurus andrewsi Averianov p. 540 |
2007 | Erlikosaurus andrewsi Turner et al. p. 5 |
2010 | Erlikosaurus andrewsi Zanno p. 521–522 |
2011 | Erlikosaurus andrewsi Turner et al. p. 59 |
2012 | Erlikosaurus andrewsi Bell et al. p. 188 |
2012 | Erlikosaurus andrewsi Qian et al. p. 339 |
2013 | Erlikosaurus andrewsi Pu et al. |
2014 | Erlikosaurus andrewsi Evans et al. p. 733 |
2015 | Erlicosaurus andrewsi Tsuihiji et al. p. 64 |
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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.
†Erlikosaurus andrewsi Barsbold and Perle 1980
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Diagnosis
Reference | Diagnosis | |
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L. E. Zanno 2010 | The original diagnosis for Erlikosaurus by Barsbold & Perle (1980, p. 190): “medium-sized [therizinosaurian] with laterally compressed pedal unguals” does not adequately diagnose this taxon. Barsbold (1983, p. 105) added two characters to the diagnosis: “mandibular teeth small and closely positioned; and rostral portion of lower jaw edentulous”. However, these characters are more widespread within the clade. Clark et al. (1994) redescribed the skull of Erlikosaurus and provided a comprehensive diagnosis on the basis of this study. However, as noted by Clark et al. (1994), the near complete absence of comparative cranial materials prevented assessment of these features as autapomorphic, synapomorphic or plesiomorphic. The recent discovery of therizinosaurian cranial materials pertaining to Falcarius (Zanno 2010) and No. mckinleyi (Kirkland & Wolfe 2001) is shedding light on the utility of these features in differentiating Erlikosaurus. The following features noted as possible autapomorphies by Clark et al. (1994, pp. 36–37) are now known to have a broader distribution among therizinosaurians: edentulous premaxilla with sharp, vertical ventrolateral edge; vomer extremely elongate and extending caudally to meet cultriform process; parabasisphenoid with extremely large pneumatic spaces; external auditory meatus restricted ventrally by lateral expansion of braincase; medial wall of antorbital fossa extensive; and maxilla with medially inset dentition and few nutrient foramina on caudal part of facial process. The taxonomic distribution of the following features (Clark et al. 1994, pp. 36–37) remains unknown: extremely elongate nares due to regression of the maxilla; antorbital fossa with well-developed over-hanging lip; medial wall of antorbital fossa imperforate; caudal process of jugal covering cranial surface of quadratojugal; and a homodont maxillary dentition of numerous (23) small, lanceolate, coarsely serrated, unrecurved, transversely flattened teeth constricted at the base. Unfortunately, the skull of Erlikosaurus could not be accessed during this study and the holotype postcranial materials cannot be located (see Specimen Availability), preventing a re-evaluation of Erlikosaurus. |
Measurements
No measurements are available
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Source: subo = suborder, o = order | |||||
References: Benton 1983, Marsh 1875 |
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 |
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Cenomanian - Santonian | Mongolia (Omnogov) | Erlikosaurus andrewsi (type locality: 67974) |