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Cratonemopteryx audax
Taxonomy
Megalopteryx audax was named by Martins-Neto and Vulcano (1989). Its type specimen is CV-1187, an exoskeleton, and it is a compression fossil. Its type locality is Crato (Vulcano collection), which is in an Aptian lacustrine - large carbonate in the Crato Formation of Brazil.
It was recombined as Cratonemopteryx audax by Martins-Neto (1997), Martins-Neto and Vulcano (1997), Martins-Neto (2000), Martins-Neto (2002), Martins-Neto et al. (2007), Lu et al. (2019).
It was recombined as Cratonemopteryx audax by Martins-Neto (1997), Martins-Neto and Vulcano (1997), Martins-Neto (2000), Martins-Neto (2002), Martins-Neto et al. (2007), Lu et al. (2019).
Synonymy list
| Year | Name and author |
|---|---|
| 1989 | Megalopteryx audax Martins-Neto and Vulcano p. 389 figs. 11C, 12A, 26 |
| 1997 | Cratonemopteryx audax Martins-Neto p. 75 |
| 1997 | Cratonemopteryx audax Martins-Neto and Vulcano p. 68 fig. 8B |
| 2000 | Cratonemopteryx audax Martins-Neto p. 116 figs. 16E-G |
| 2002 | Cratonemopteryx audax Martins-Neto p. 38 |
| 2007 | Cratonemopteryx audax Martins-Neto et al. fig. 11.64c,d |
| 2019 | Cratonemopteryx audax Lu et al. p. 263 |
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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.
†Cratonemopteryx audax Martins-Neto and Vulcano 1989
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
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| Source: c = class, p = phylum | |||||
| References: Kiessling 2004, Bush and Bambach 2015 | |||||
Age range: Late/Upper Aptian or 119.57000 to 113.20000 Ma
Collections: one only
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Late/Upper Aptian | Brazil (Ceará) | Megalopteryx audax (type locality: 125511) |