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Arrudatitan maximus
Taxonomy
Aeolosaurus maximus was named by Santucci and Arruda-Campos (2011). Its type specimen is MPMA 12-0001-97, a partial skeleton, and it is a 3D body fossil. Its type locality is Santa Irene farm, which is in a Campanian/Maastrichtian terrestrial sandstone in the Adamantina Formation of Brazil.
It was recombined as Arrudatitan maximus by Silva Junior et al. (2022) and Navarro et al. (2022).
It was recombined as Arrudatitan maximus by Silva Junior et al. (2022) and Navarro et al. (2022).
Synonymy list
Year | Name and author |
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2011 | Aeolosaurus maximus Santucci and Arruda-Campos p. 6 |
2014 | Aeolosaurus maximus González Riga and Ortiz David p. 10 |
2015 | Aeolosaurus maximus Filippi p. 25 |
2015 | Aeolosaurus maximus de Jesus Faria et al. p. 155 |
2017 | Aeolosaurus maximus Gorscak et al. p. 13 |
2022 | Arrudatitan maximus Navarro et al. p. 346 |
2022 | Arrudatitan maximus Silva Junior et al. |
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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.
†Arrudatitan maximus Santucci and Arruda-Campos 2011
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Diagnosis
Reference | Diagnosis | |
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R. M. Santucci and A. C. d. Arruda-Campos 2011 | Titanosaur characterized by the following unique association of characteristics: well-developed posterior protuberance below the articular area on the anterior and middle haemal arches and lateral bulge on the distal portion of the articular process of the mid-posterior haemal arches. An additional set of ambiguous synapomorphies includes: presence of posterior centrodiapophyseal lamina (pcdl) at least 50% thicker than the postzygodiapophyseal lamina (podl) in posterior cervical vertebrae; posterior dorsal vertebrae with intrapostzygapophyseal lamina and an oblique anterior centropostzygapophyseal lamina (acpol) which bifurcates from the proximal portion of the centropostzygapophyseal lamina (acpol); mid-thoracic ribs bearing well-developed anterior and posterior crests with a D-shaped cross section. These features are considered ambiguous because they cannot be assessed in other Aeolosaurus species so far, and may correspond to a set of synapomorphies of Aeolosaurus or even Aeolosaurini. |