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Koreanaornis dodsoni
Taxonomy
Koreanaornis dodsoni was named by Xing et al. (2011). It is considered to be a form taxon. Its type specimen is MGCM.H14, a footprint, and it is a trace fossil. Its type locality is Huangyangquan tracksite, Site B, which is in a Hauterivian/Barremian lacustrine deltaic sandstone/mudstone in the Hutubihe Formation of China.
It was recombined as Koreanornis dodsoni by Xing et al. (2011) and Lockley et al. (2013).
It was recombined as Koreanornis dodsoni by Xing et al. (2011) and Lockley et al. (2013).
Synonymy list
Year | Name and author |
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2011 | Koreanaornis dodsoni Xing et al. p. 310 fig. 3 |
2011 | Koreanornis dodsoni Xing et al. p. 310 fig. 3 |
2013 | Koreanornis dodsoni Lockley et al. p. 14 |
2013 | Koreanaornis dodsoni Xing et al. p. 42 |
2016 | Koreanaornis dodsoni Buckley et al. p. 261 |
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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.
†Koreanaornis dodsoni Xing et al. 2011
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Diagnosis
Reference | Diagnosis | |
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L.-D. Xing et al. 2011 | Different from K. hamanensis tracks in having smaller divarication angles between digits II and IV, greater overall track length and width, persistent absence of digit I, and absence of digital pad impressions. |
Measurements
No measurements are available
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Source: subo = suborder, o = order | |||||
References: Marsh 1875, Benton 1983 |
Age range: base of the Hauterivian to the top of the Barremian or 132.90000 to 125.00000 Ma
Collections: one only
Time interval | Ma | Country or state | Original ID and collection number |
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Hauterivian - Barremian | China (Xinjiang) | Koreanaornis dodsoni (type locality: 156126) |