Chindesaurus
Chindesaurus | |
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Skeletal reconstruction of Chindesaurus bryansmalli. Known elements in white and light grey, and unknown in dark gray. Missing elements based on Tawa hallae. | |
Scientific classification | |
Domain: | Eukaryota |
Kingdom: | Animalia |
Phylum: | Chordata |
Clade: | Dinosauria |
Clade: | Saurischia |
Genus: | †Chindesaurus Long & Murray, 1995 |
Species: | †C. bryansmalli
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Binomial name | |
†Chindesaurus bryansmalli Long & Murry, 1995
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Synonyms | |
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Chindesaurus (
Chindesaurus's classification is debated, and various papers have had different conclusions on its affinities. Its fossils were originally believed to belong to "
Discovery
Holotype
Although many specimens have been referred to Chindesaurus, only one specimen has enough material to remain within the genus with certainty.[1] This specimen, holotype PEFO 10395, is a partial skeleton, found within Petrified Forest National Park in Apache County, Arizona. PEFO 10395 was discovered in 1984 by Bryan Small, who recovered the skeleton from a blue mudstone layer in the Chinle Formation's Upper Petrified Forest Member.[3][7][1] Based on U-Pb dating of overlying and underlying units, the mudstone layer was deposited about 213 to 210 million years ago, during the Norian stage of the Triassic.[1]
PEFO 10395 mainly consists of vertebrae, limb bones, and hip fragments. Vertebrae include several partial cervical (neck) dorsal (back), and caudal (tail) vertebrae, along with two sacral (hip) vertebrae, a chevron, and rib fragments. Each of the three bones making up the hip (the ilium, pubis, and ischium) are represented by isolated fragments. Leg bones include a complete right femur, the upper part of the left femur, an incomplete right tibia, and a right astragalus bone of the ankle.[1][3] A single serrated tooth has also been considered as part of the specimen,[8] but this may be in error.[9]
When the holotype specimen was discovered, it was nicknamed "Gertie" (after Gertie the Dinosaur) and received much publicity. "Gertie" was subsequently airlifted by helicopter on June 6, 1985, and brought to the University of California Museum of Paleontology (UCMP) in Berkeley, CA, where it was prepared over the next several years.[1] The anniversary of the airlift and the media interest it generated for Petrified Forest National Park is celebrated at the park every year. "Gertie" was described and given a proper binomial name by R.A. Long and P.A. Murry in 1995. It was also initially known as the "Chinde Point dinosaur", in reference to a geological landmark close to the site which it was recovered from. This reference was carried over to its generic name, derived from the Navajo word chindi (meaning "ghost" or "evil spirit") and the Greek word "sauros" (σαυρος) (meaning "lizard"). Its name could therefore be translated as "ghost lizard" or "Lizard from Chinde Point". The specific name, bryansmalli, honors the discoverer, Bryan Small.[3]
Referred specimens
Several more incomplete specimens have been referred to the genus. These specimens consist of various vertebrae and femur fragments found throughout the American southwest. Eight referred specimens are stored at PEFO (Petrified Forest National Park, AZ), where the holotype was discovered. Two are stored at the UCMP (University of California Museum of Paleontology), where the holotype was prepared. Up to six more are stored at the
Though most specimens referred to Chindesaurus hail from
Though specimens referred to Chindesaurus are widely distributed and sometimes well-preserved, none of them exhibit features unique to the genus. The referral of two specimens (NMMNH P16656 and NMMNH P17325) to Chindesaurus came under question as soon as 2007.[9] Marsh et al. (2019) argued that only the holotype specimen of Chindesaurus should be considered as belonging to the genus. They removed all specimens except for the holotype from the genus, placing the rest as indeterminate material from the Chindesaurus + Tawa clade of their analysis.[1]
Description
Long & Murry reconstructed Chindesaurus with a stout body, long legs, a fairly long neck, and a total estimated length of 3 to 4 meters (9.9 to 13.1 feet).[3] Benson & Brusatte (2012) suggested that Chindesaurus was smaller, up to 2 to 2.3 metres (6.6 to 7.5 ft) in length.[11] Holtz (2012) estimated that Chindesaurus had a length of about 2 meters (6.6) feet and a weight equivalent to that of a wolf (23–45 kg, or about 50-100 pounds).[2] The skeletal anatomy of Chindesaurus is incompletely known, so these full body estimates are very rough approximations. The holotype specimen may not be fully grown due to its unfused ankle and dorsal neurocentral sutures. However, these features may not be fully correlated with development in early dinosaurs, and the specimen has other traits indicating a post-juvenile stage, such as a trochanteric shelf and fused caudal neurocentral sutures.[1]
Vertebrae
The cervical (neck) vertebrae, at least near the head, had a low keel along the front half of their lower edge. They also had a pair of shallow oval-shaped depressions on their sides, similar to those found in Tawa, Liliensternus, and Cryolophosaurus. The dorsal (trunk) vertebrae are deep, wide, and fairly short (from front-to-back), closer to the condition in herrerasaurids rather than Tawa and coelophysoids. Both the sides and the lower edge of each dorsal are constricted, and small pockets lie below the sutures with the neural arch. These pockets, known as centrodiapophyseal fossae, are ancestral to dinosaurs but lost by most theropods. Neural spines expand outwards and backwards, forming "spine-tables", structures which are otherwise only observed in Herrerasaurus and Dilophosaurus among potential theropods.[3][9][1]
The two preserved
Hip and hindlimb
The postacetabular process (rear blade) of the ilium is low, with a horizontal ridge on its inner edge and a large roughly-textured tubercle on its outer surface. These characteristics are also known in Caseosaurus. There is no distinct brevis fossa, also like Caseosaurus and herrerasaurids. Both the pubic and ischiadic peduncles of the ilium expand lengthwise towards their lower edges. Unlike herrerasaurids, the supraacetabular crest of the ilium does not extend as far forwards as its contact with the pubis. The pubis is thin, straight, and slightly curved back, widening slightly towards the ilium. On the other hand, the ischium seems to widen slightly away from the ilium.[9][1]
The femur is large and sigmoid, with a smooth, rectangular femoral head. Like Tawa (but unlike coelophysoids), the anterior trochanter has the appearance of a bulbous ridge, not separated from the shaft by a cleft. However, Chindesaurus lacks a groove at the top of its femoral head, possesses a trochanteric shelf, and has a dorsolateral trochanter which is low and rounded, traits which contrast with Tawa. The fourth trochanter is low and located further distally than that of Herrerasaurus. The lower end of the femur has two distinct condyles which are triangular in cross-section. The tibia is very similar to that of Tawa in several respects. For example, the rear face of the upper end of the tibia is nearly straight, with the exception of a large notch on its medial half and a smaller notch slightly lateral to it. Moreover, the cnemial crest running down the front of the tibia is quite low, <35% the total anteroposterior thickness of the bone. Finally, the lower end of the tibia has a large and triangular posterolateral process which extends downwards and outwards from the rest of the bone, a trait also shared by Lesothosaurus and Guaibasaurus. The front edge of the astragalus has a deep and broad cleft which subdivides the bone vertically. This cleft actually extends onto the lower surface of the bone, giving it a characteristic "glutealiform" shape shared with Tawa. There is a distinct ascending process on the upper and outer part of the astragalus, surrounded by a system of pits, ridges, and depressions which connect to the tibia.[9][1]
Classification
As a herrerasaurid
Chindesaurus has been difficult to classify, and has been recovered in several different positions at the base of the
Nesbitt et al. (2007) and Irmis et al. (2007) argued that Chindesaurus was a probable basal saurischian dinosaur, and noted that it shares a wide range of characteristics with several lineages of basal saurischians, making any classification problematic.[9][10] Rauhut (2003) noted that the medially expanded brevis shelf of Chindesaurus resembles that of "crurotarsans" (pseudosuchians), unlike that of most dinosaurs, which is usually laterally expanded.[16]
A partial ilium originally assigned to Chindesaurus, from the Tecovas Formation of Texas, was later placed in its own genus and species, Caseosaurus crosbyensis, by Hunt et al. (1998).[8] Langer (2004) argued that this separation was probably in error, and that the two forms represent the same species.[17] Nesbitt et al. (2007) corroborated this, stating that the differences between Caseosaurus and Chindesaurus cited by Hunt et al. (1998) were probably a result of size-related variation. However, Nesbitt et al. refrained from formally synonymizing the two taxa due to the fragmentary nature of Chindesaurus's ilium.[9] Baron & Williams redescribed Caseosaurus in 2018, and considered it to be a valid herrerasaurian taxon closely related to, but not within, the family Herrerasauridae, in the larger clade Herrerasauria.[5] An analysis by Novas et al. (in 2021) also placed Chindesaurus as a non-herrerasaurid herrerasaurian, forming a clade with Daemonosaurus and Tawa (also see below)[6]
The following is a
Dinosauria
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As a relative of Tawa
A phylogenetic analysis by Cabreira et al. (2016) found an unusual result, where Chindesaurus was placed as the sister taxon of Tawa hallae, a carnivorous dinosaur from the Hayden Quarry of Ghost Ranch in New Mexico.[18] Tawa lived at roughly the same time as the holotype specimen of Chindesaurus, and material referred to Chindesaurus has also been found at the Hayden Quarry.[10][1] Though Chindesaurus was often considered a herrerasaurid and Tawa was often considered a theropod, this study suggested that neither position was correct. Instead, it placed the Chindesaurus + Tawa clade within basal Saurischia, prior to the split between sauropodomorphs and theropods.[18] A Chindesaurus + Tawa clade was also found in a revision to Baron et al. (2017)'s controversial Ornithoscelida hypothesis.[19]
The hypothesis of close relations to Tawa was elaborated upon in 2019, when the holotype specimen of Chindesaurus was redescribed by Adam D. Marsh, William G. Parker, Max C. Langer, and Sterling J. Nesbitt. They included a phylogenetic analysis which placed the Chindesaurus + Tawa clade in the base of Theropoda, a similar position to that first described for Tawa.Their sister-taxon relationship was supported by one
The following cladogram represents the phylogenetic analysis of Marsh et al. (2019), recovering a Chindesaurus + Tawa clade in basal Theropoda:[1]
Dinosauria
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Paleoecology
The Upper
References
- ^ S2CID 202865005.
- ^ a b Holtz, Thomas R. Jr. (2012) Dinosaurs: The Most Complete, Up-to-Date Encyclopedia for Dinosaur Lovers of All Ages, Winter 2011 Appendix.
- ^ a b c d e f g h i j k l Long, Robert A.; Murry, Phillip A. (1995). "Late Triassic (Carnian and Norian) tetrapods from the Southwestern United States". New Mexico Museum of Natural History and Science Bulletin. 4: 1–254.
- ^ S2CID 220415208.
- ^ .
- ^ .
- ^ Parker, William G.; Irmis, Randall B.; Nesbitt, Sterling J. (2006). Parker, W. G.; Ash, S. R.; Irmis, R. B. (eds.). "Review of the Late Triassic dinosaur record from Petrified Forest National Park". Museum of Northern Arizona Bulletin. 62: 160–161.
- ^ .
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- ^ Meyer, (1986). "D-Day on the Painted Desert." Arizona Highways, 62(7): 3–13.
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- ^ PMID 21490016.
- S2CID 205254710.
- ^ Rauhut, Oliver W.M. (2003). "The Interrelationships and Evolution of Basal Theropod Dinosaur" (PDF). Special Papers in Palaeontology. 69: 1–213.
- OL 3305845M.
- ^ PMID 27839975.
- S2CID 205260360.