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Deltapodus curriei
Taxonomy
Deltapodus curriei was named by Xing et al. (2013). It is considered to be a form taxon. Its type specimen is MGCM.SA2m, SA2p, a footprint, and it is a trace fossil. Its type locality is Huangyangquan tracksite, Site B, which is in a Berriasian/Valanginian lacustrine deltaic sandstone/mudstone in the Hutubihe Formation of China.
Synonymy list
Year | Name and author |
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2013 | Deltapodus curriei Xing et al. p. 56–57 fig. 3–6 |
2015 | Deltapodus curriei Pascual-Arribas and Hernández-Medrano p. 23 |
2016 | Deltapodus curriei Borinder et al. p. 67 |
2016 | Deltapodus curriei Salisbury et al. p. 97 |
2020 | Deltapodus curriei Xing et al. p. 81 |
2021 | Deltapodus curriei Xing et al. p. 68 |
2025 | Deltapodus curriei Foster et al. p. 318 |
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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.
†Deltapodus curriei Xing et al. 2013
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Diagnosis
Reference | Diagnosis | |
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L. Xing et al. 2013 | The manus track is entaxonic and oval-shaped, although somewhat irregular. The manus is approximately twice as wide as long. The impression of manual digit I is distinct and robust. The medial metacarpophalangeal pad region is slightly concave, while the lateral region is slightly convex. The length of the pes track slightly exceeds its width by 35%. The pes tracks have three func- tional digits (IIeIV) that are distinct but short, bluntly rounded impressions. These digit impressions are subequal in length and display a higher degree of entaxony than other species of Deltapodus. The heel region is elongate and has smoothly curved margins; the divarication between digits II and III appears slightly greater than that between digits III and IV, but this is difficult to measure accurately in tracks with such short, blunt toe traces. The trackway (both manus and pes) exhibits slight outward rotation. |
Measurements
No measurements are available
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Source: o = order | |||||
Reference: Marsh 1875 |
Age range: base of the Berriasian to the top of the Valanginian or 145.00000 to 132.90000 Ma
Collections (2 total)
Time interval | Ma | Country or state | Original ID and collection number |
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Berriasian - Valanginian | China (Xinjiang) | Deltapodus curriei (type locality: 156126 220466) |