Coloradisaurus brevis was originally named Coloradia brevis by José Bonaparte in 1978,[4] but that genus name was preoccupied by the pine moth Coloradia,[5] so it needed a replacement name. In 1983, David Lambert used the name Coloradisaurus for the genus, but did not indicate it was a replacement or diagnose it.[6] Lambert had gotten the name from Bonaparte in a personal communication and mistakenly thought that Bonaparte had already published it.[3]Peter Galton was the next to use the name Coloradisaurus in 1990, which he credited to Lambert, when he gave the taxon a diagnosis in his review of prosauropods in The Dinosauria.[2][3]Authorship of Coloradisaurus has traditionally been attributed to Lambert, but in 2020, Greenfield et al. judged Lambert's use of the name to be a nomen nudum. They concluded that authorship should be attributed to Galton, who was the first to use the name Coloradisaurus in a way that met the requirements of the ICZN.[3]
Description
The holotype of Coloradisaurus (PVL 3967) is a mostly complete skull found associated with an undescribed partial skeleton.[4] While the right side of the skull is well-preserved with almost all bones intact, the left side is distorted and missing more bones.[7] The holotype individual has been estimated to have been 3 m (10 ft) long with a mass of 70 kg (150 lb).[8] A referred specimen (PVL 5904) is a partial skeleton including most of the dorsal vertebrae and parts of the pectoral and pelvic girdles and limbs.[9] Like Lufengosaurus, it have the angle between the pterygoid and quadratojugal rami nearly 90°. There is also a possibility that the postorbital bones of Coloradisaurus and Sarahsaurus are similar, but due to the deformation of the skull this is difficult to say.[10]
Coloradisaurus was classified as a plateosaurid in the original description by Bonaparte,[4] but this pre-dated the use of phylogenetic analyses in paleontology. He later became opposed to cladistics[11] and continued to consider Coloradisaurus a plateosaurid without testing its phylogenetic position.[12] The analyses of Galton (1990), Galton & Upchurch (2004), and Upchurch et al. (2007) found it to be a plateosaurid, supporting Bonaparte's placement.[2][13][14] However, the analyses of Benton et al. (2000) and Yates (2003) recovered it in a polytomy with other basal sauropodomorphs or as a massospondylid, respectively.[15][16] Subsequent analyses such as Yates et al. (2010), Apaldetti et al. (2013; 2014), Wang et al. (2017), and Müller (2020) have reached the consensus that Coloradisaurus is a massospondylid most closely related to Lufengosaurus and Glacialisaurus.[7][9][17][18][10][19] These three taxa share four synapomorphies found in the metatarsals and femur.[9]
Below is a simplified cladogram after Galton & Upchurch (2004), reflecting its early placement as a plateosaurid.[13]
^ abcGalton, P.M. (1990). "Basal Sauropodomorpha - Prosauropoda". In Weishampel, D.B.; Dodson, P.; Osmólska, H. (eds.). The Dinosauria. Berkeley, CA: University of California Press. pp. 320–344. ISBN0-520-06726-6.
^ abcdeGreenfield, T.; Bivens, G.; Fonseca, A. (2020). "The correct authorship of Coloradisaurus (Dinosauria, Sauropodomorpha): Galton, 1990, not Lambert, 1983". Bulletin of Zoological Nomenclature. 77 (1): 153–155. doi:10.21805/bzn.v77.a050. S2CID229723564.
^ abcApaldetti, C.; Martinez, R.N.; Pol, D.; Souter, T. (2014). "Redescription of the Skull of Coloradisaurus brevis (Dinosauria, Sauropodomorpha) from the Late Triassic Los Colorados Formation of the Ischigualasto-Villa Union Basin, northwestern Argentina". Journal of Vertebrate Paleontology. 34 (5): 1113–1132. Bibcode:2014JVPal..34.1113A. doi:10.1080/02724634.2014.859147. hdl:11336/36518. S2CID86158311.
^ abGalton, P.M.; Upchurch, P. (2004). "Prosauropoda". In Weishampel, D.B.; Dodson, P.; Osmólska, H. (eds.). The Dinosauria (2nd ed.). Berkeley, CA: University of California Press. pp. 232–258. ISBN0-520-24209-2.
^Benton, M.J.; Juul, L.; Storrs, G.W.; Galton, P.M. (2000). "Anatomy and systematics of the prosauropod dinosaur Thecodontosaurus antiquus from the upper Triassic of southwest England". Journal of Vertebrate Paleontology. 20 (1): 77–108. doi:10.1671/0272-4634(2000)020[0077:AASOTP]2.0.CO;2.