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Hulsanpes perlei
Taxonomy
Hulsanpes perlei was named by Osmolska (1982). Its type specimen is ZPAL MgD-I/173, a set of limb elements, and it is a 3D body fossil. Its type locality is Khulsan, site 2 [PMPE], which is in a Campanian/Campanian terrestrial sandstone in the Baruungoyot Formation of Mongolia. It was considered monophyletic by Currie (2000).
Synonymy list
| Year | Name and author |
|---|---|
| 1982 | Hulsanpes perlei Osmolska |
| 1992 | Hulsanpes perlei Currie p. 246 |
| 1997 | Hulsanpes perlei Barsbold p. 447 |
| 1997 | Hulsanpes perlei Osmólska p. 41 |
| 1998 | Hulsanpes perlei Le Loeuff and Buffetaut p. 110 |
| 2000 | Hulsanpes perlei Burnham et al. p. 7 |
| 2000 | Hulsanpes perlei Currie p. 436 |
| 2003 | Hulsanpes perlei Rauhut p. 37 |
| 2004 | Hulsanpes perlei Senter et al. p. 3 |
| 2017 | Hulsanpes perlei Cau et al. |
| 2018 | Hulsanpes perlei Cau and Madzia p. 5–6 |
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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.
†Hulsanpes perlei Osmolska 1982
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Diagnosis
| Reference | Diagnosis | |
|---|---|---|
| A. Cau et al. 2017 | Halszkaraptorine dromaeosaurid with unique combination of: dorsal overlap of metatarsal III on distal third of metatarsal II more extensive than in M. omnogovae; in extensor view, medial margin of metatarsal III with constriction between distal shaft and trochlea; distal end of shaft of metatarsal IV diverges from metatarsal III proximal to metatarsal III distal constriction (divergence absent in Ha. escuilliei; in M. omnogovae, the divergence starts at level of the distal constriction of metatarsal III shaft). | |
| A. Cau and D. Madzia 2018 | A paravian theropod with the following unique combination of features (autapomorphies among Dromaeosauridae and Halszkaraptorinae marked with *): distal third of metatarsal II shaft extensively overlapped by metatarsal III in extensor view*; proximal shaft of metatarsal III unconstricted and wider than adjacent metatarsals*; metatarsal III–IV contact straight in extensor view; distal end of metatarsal IV diverges laterodistally. |
Measurements
No measurements are available
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| Source: f = family, o = order | |||||
| References: Holtz et al. 2000, Kiessling 2004, Marsh 1875 | |||||
Age range: base of the Middle Campanian to the top of the Late/Upper Campanian or 83.60000 to 72.20000 Ma
Collections: one only
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Middle Campanian - Late/Upper Campanian | Mongolia (Omnogov) | Theropoda indet. (type locality: 181415) |