|Mounted skeleton at the Cleveland Museum of Natural History|
Coelophysis (// seh-LOF-ih-sis traditionally; // SEL-o-FY-sis or // SEE-lo-FY-sis, as heard more commonly in recent decades) is an extinct genus of coelophysid theropod dinosaur that lived approximately 216 to 196 million years ago during the latter part of the Triassic Period in what is now the southwestern United States and also in South Africa and Zimbabwe.
Coelophysis was a small, slenderly-built, ground-dwelling, bipedal carnivore, that could grow up to 3 m (9.8 ft) long. It is one of the earliest known dinosaur genera. Scattered material representing similar animals has been found worldwide in some Late Triassic and Early Jurassic formations.
The type species C. bauri, originally given to the genus Coelurus by Edward Drinker Cope in 1887, was described by the latter in 1889. The names Longosaurus and Rioarribasaurus are synonymous with Coelophysis. Another dinosaur genus, Megapnosaurus, has also been considered to be a synonym. This primitive theropod is notable for being one of the most specimen-rich dinosaur genera.
Coelophysis is known from a number of complete fossil skeletons of the species C. bauri, which was a lightly built dinosaur which measured up to 3 metres (9.8 ft) in length and which was more than a meter tall at the hips. Paul (1988) estimated the weight of the gracile form at 15 kg (33 lb), and the weight of the robust form at 20 kg (44 lb). Coelophysis was a bipedal, carnivorous, theropod dinosaur that was a fast and agile runner. Despite being an early dinosaur, the evolution of the theropod body form had already advanced greatly from creatures like Herrerasaurus and Eoraptor. The torso of Coelophysis conforms to the basic theropod body shape, but the pectoral girdle displays some interesting special characteristics: C. bauri had a furcula (wishbone), the earliest known example in a dinosaur. Coelophysis also preserves the ancestral condition of possessing four digits on the hand (manus). It had only three functional digits, the fourth embedded in the flesh of the hand.
Coelophysis had narrow hips, forelimbs adapted for grasping prey, and narrow feet. Its neck and tail were long and slender. The pelvis and hindlimbs of C. bauri are also slight variations on the theropod body plan. It has the open acetabulum and straight ankle hinge that define the Dinosauria. The hindlimb ended in a three-toed foot (pes), with a raised hallux. The tail had an unusual structure within its interlocking prezygapophysis of its vertebrae, which formed a semi-rigid lattice, apparently to stop the tail from moving up and down.
Coelophysis had a long narrow head (approximately 270 mm (0.9 ft)), with large, forward-facing eyes that afforded it stereoscopic vision and as a result excellent depth perception. Rinehart et al. (2004) described the complete sclerotic ring found for a juvenile Coelophysis bauri (specimen NMMNH P-4200), and compared it to data on the sclerotic rings of reptiles and birds and concluded that Coelophysis was a diurnal, visually oriented predator. The study found that the vision of Coelophysis was superior to most lizards' vision, and ranked with that of modern birds of prey. The eyes of Coelophysis appear to be the closest to those of eagles and hawks, with a high power of accommodation. The data also suggested poor night vision, which would mean this dinosaur had a round rather than a split pupil.
Coelophysis had an elongated snout with large fenestrae which helped to reduce skull weight, while narrow struts of bones preserved the structural integrity of the skull. The neck had a pronounced sigmoid curve. The braincase is known in Coelophysis bauri but little data could be derived because the skull was crushed. Unlike some other theropods, the cranial ornamentation of Coelophysis was not located at the top of its skull. Low, laterally raised bony ridges were present on the dorsolateral margin of the nasal and lacrimal bones in the skull, directly above the antorbital fenestra.
Distinguishing anatomical features
A diagnosis is a statement of the anatomical features of an organism (or group) that collectively distinguish it from all other organisms. Some, but not all, of the features in a diagnosis are also autapomorphies. An autapomorphy is a distinctive anatomical feature that is unique to a given organism or group.
According to Ezcurra (2007), and Bristowe and Raath (2004) Coelophysis can be distinguished based on the following features: the absence of an offset rostral process of the maxilla; the quadrate is strongly caudally; a small external mandibular fenestra, which is 9–10% of the mandibular length; and the anteroposterior length of the ventral lacrimal process is greater than 30% of its height.
Several paleontologists consider Coelophysis bauri to be the same dinosaur as Coelophysis rhodesiensis (formerly Syntarsus, alternately Megapnosaurus), however this has been refuted by the following: Downs (2000) concluded that C. bauri differs from C. rhodesiensis in cervical length, proximal and distal hindlimb proportions and proximal caudal vertebral anatomy; Tykoski and Rowe (2004) concluded that C. bauri differs from C. rhodesiensis in that it lacks a pit at the base of the nasal process of the premaxilla; and Bristowe and Raath (2004) concluded that C. bauri differs from C. rhodesiensis in having a longer maxillary tooth row.
History of discovery
Named in 1887, the type species of Coelophysis was originally named as a species of Coelurus. Edward Drinker Cope first named Coelophysis in 1889 to name a new genus, outside of Coelurus and Tanystrophaeus to which C. bauri was previously classified in for C. bauri, C. willistoni and C. longicollis. An amateur fossil collector working for Cope, David Baldwin, had found the first remains of the dinosaur in 1881 in the Chinle Formation in northwestern New Mexico. Early in 1887, Cope referred the specimens collected to two new species, C. bauri and C. longicollis of the genus Coelurus. Later in 1887 Cope reassigned the material to a yet another genus, Tanystrophaeus. Two years later, Cope corrected his classification after realizing differences in the vertebrae, and named Coelophysis, with C. bauri as the type species, which was named for Georg Baur, a comparative anatomist whose ideas were similar to Cope's. The name Coelophysis comes from the Greek words κοῖλος/koilos (meaning 'hollow') and φύσις/physis (meaning 'form'), thus "hollow form" which is a reference to its hollow vertebrae. However, these first finds were too poorly preserved to give a complete picture of this new dinosaur. In 1947, a substantial 'graveyard' of Coelophysis fossils was found by George Whitaker, the assistant of Edwin H. Colbert, in New Mexico, at the Ghost Ranch, close to the original find. American Museum of Natural History paleontologist Edwin H. Colbert conducted a comprehensive study of all the fossils found up to that date and assigned them to Coelophysis. The Ghost Ranch specimens were so numerous, including many well-preserved and fully articulated specimens, that one of them has since become the diagnostic, or type specimen, for the entire genus, replacing the original, poorly preserved specimen.
"Syntarsus" rhodesiensis was first described by Raath (1969) and assigned to Podokesauridae. The taxon "Podokesauridae", was abandoned since its type specimen was destroyed in a fire and can no longer be compared to new finds. Over the years paleontologists assigned this genus to Ceratosauridae (Welles, 1984), Procompsognathidae (Parrish and Carpenter, 1986) and Ceratosauria (Gauthier, 1986). In 2004 "Syntarsus" was found synonymous with Coelophysis by Tykoski and Rowe (2004). Ezcurra and Novas (2007) and Ezcurra (2007) also concluded that "Syntarsus" was synonymous with Coelophysis, which is the current scientific consensus.
Coelophysis is a distinct taxonomic unit (genus), composed of two species; C. bauri and C. rhodesiensis (the latter formerly classified as the genus Megapnosaurus). Two additional originally described species, C. longicollis and C. willistoni, are now considered synonymous with C. bauri. C. rhodesiensis is probably part of this generic complex, and is known from the Jurassic of southern Africa. A third possible species is Coelophysis kayentakatae, previously referred to the genus Megapnosaurus. There is not a clear consensus at this point.
In the early 1990s, there was debate over the diagnostic characteristics of the first specimens collected, compared to the material excavated at the Ghost Ranch Coelophysis quarry. Some paleontologists were of the opinion that the original specimens were not diagnostic beyond themselves and, therefore, that the name C. bauri could not be applied to any additional specimens. They therefore applied a different name, Rioarribasaurus, to the Ghost Ranch quarry specimens.
Since the numerous well-preserved Ghost Ranch specimens were used as Coelophysis in most of the scientific literature, the use of Rioarribasaurus would have been very inconvenient for researchers, so a petition was given to have the type specimen of Coelophysis transferred from the poorly preserved original specimen to one of the well-preserved Ghost Ranch specimens. This would make Rioarribasaurus a definite synonym of Coelophysis, specifically a junior objective synonym. In the end, the International Commission on Zoological Nomenclature (ICZN) voted to make one of the Ghost Ranch samples the actual type specimen for Coelophysis and dispose of the name Rioarribasaurus altogether (declaring it a nomen rejectum, or "rejected name"), thus resolving the confusion. The name Coelophysis therefore became a nomen conservandum ("conserved name").
In a situation affecting many dinosaur taxa, some more recently discovered fossils were originally classified as new genera but may be species of Coelophysis. For example, Prof. Mignon Talbot's 1911 discovery which she named Podokesaurus holyokensis, has long been considered to be related to Coelophysis, and some modern scientists consider Podokesaurus a synonym of Coelophysis. Another specimen from the Portland Formation of the Hartford Basin, now at the Boston Museum of Science, has also been referred to Coelophysis. This specimen consists of sandstone casts of a pubis, tibia, three ribs, and a possible vertebra, and probably originated in a quarry in Middletown, Connecticut. However, both the type specimen of Podokesaurus and the Middletown specimen are typically considered indeterminate theropods today.
Sullivan & Lucas (1999) referred one specimen from Cope's original material of Coelophysis (AMNH 2706) to what they thought was a newly discovered theropod, Eucoelophysis. However, subsequent studies have shown that Eucoelophysis was misidentified, and is actually a primitive, non-dinosaurian ornithodiran closely related to Silesaurus.
The genus Syntarsus was named by Raath in 1969 for the type species Syntarsus rhodesiensis from Africa, and later applied to the North American Syntarsus kayentakatae. It was renamed by American entomologist Dr. Michael Ivie (Montana State University of Bozeman), Polish Australian Dr. Adam Ślipiński, and Polish Dr. Piotr Węgrzynowicz (Muzeum Ewolucji Instytutu Zoologii PAN of Warsaw), the three scientists who discovered that the genus name Syntarsus was already taken by a colydiine beetle described in 1869. Many paleontologists did not like the naming of Megapnosaurus, partially because taxonomists are generally expected to allow original authors of a name to correct any mistakes in their work. Raath was aware of the homonymy between the dinosaur Syntarsus and beetle Syntarsus, but the group who published Megapnosaurus were led to believe Raath was deceased and therefore unable to correct his mistake, and proceeded accordingly. Mortimer (2012) pointed out that "Paleontologists might have reacted more positively if the replacement name (Megapnosaurus) hadn't been facetious, translating to "big dead lizard". Yates (2005) analyzed Coelophysis and Megapnosaurus and concluded that the two genera are almost identical, and suggested that Megapnosaurus was possibly synonymous with Coelophysis. In 2004, Raath co-authored two papers in which he argued that Megapnosaurus (formerly Syntarsus) was a junior synonym of Coelophysis. Megapnosaurus was regarded by Paul (1988) and Downs (2000) as being congeneric with Coelophysis. Then in 1993, Paul suggested that Coelophysis should be placed in Megapnosaurus (then known as Syntarsus) to get around the above-mentioned taxonomic confusion. Downs (2000) examined Camposaurus and concluded that it was a junior synonym of Coelophysis, because of its similarity to some of the Coelophysis Ghost Ranch specimens. However, a reassessment of the Camposaurus holotype by Martin Ezcurra and Stephen Brusatte published in 2011 revealed a pair of autapomorphies in the holotype, indicating that C. arizonensis was not a synonym of C. bauri, although it was a close relative of C. rhodesensis.
The teeth of Coelophysis were typical of predatory dinosaurs, blade-like, recurved, sharp and jagged with fine serrations on both the anterior and posterior edges. Its dentition shows that it was carnivorous, probably preying on the small, lizard-like animals that were discovered with it. It may also have hunted in packs to tackle larger prey.Coelophysis bauri has approximately 26 teeth on the maxillary bone of the upper jaw and 27 teeth on the dentary bone of the lower jaw. Carpenter (2002) examined the bio-mechanics of theropods forelimbs and attempted to evaluate their usefulness in predation. He concluded that the forelimb of Coelophysis was flexible and had a good range of motion, but its bone structure suggested that it was comparatively weak. The "weak" forelimbs and small teeth in this genus, suggested that Coelophysis preyed upon animals that were substantially smaller than itself. Rinehart et al. agreed that Coelophysis was a "hunter of small, fast-moving prey". Carpenter also identified three distinct models of theropod forelimb use and noted that Coelophysis was a "combination grasper-clutcher" as compared to other dinosaurs that were "clutchers" or "long armed graspers".
It has been suggested that C. bauri was a cannibal, based on supposed juvenile specimens found "within" the abdominal cavities of some Ghost Ranch specimens. However, Robert J. Gay showed in 2002 that these specimens were misinterpreted. Several specimens of "juvenile coelophysids" were actually small crurotarsan reptiles such as Hesperosuchus. Gay's position was lent support in a 2006 study by Nesbitt et al. In 2009, new evidence of cannibalism came to light when additional preparation of previously excavated matrix revealed regurgitate material in and around the mouth of Coelophysis specimen NMMNH P-44551. This material included tooth and jaw bone fragments that Rinehart et al. considered "morphologically identical" to a juvenile Coelophysis.
In 2010, Gay examined the bones of juveniles found within the thoracic cavity of AMNH 7224, and calculated that the total volume of these bones was 17 times greater than the maximum estimated stomach volume of the Coelophysis specimen. Gay observed that the total volume would be even greater when considering that there would have been flesh on these bones. This analysis also noted the absence of tooth marks on the bones as would be expected in defleshing, and the absence of expected pitting by stomach acids. Finally, Gay demonstrated that the alleged cannibalized juvenile bones were deposited stratigraphically below the larger animal that had supposedly cannibalized them. Taken together these data suggested that the Coelophysis specimen AMNH 7224 was not a cannibal and that the bones of the juvenile and adult specimens were found in their final position as a result of "coincidental superposition of different sized individuals.
The discovery of over 1000 specimens of Coelophysis at the Whitaker quarry at Ghost Ranch, has suggested gregarious behavior to researchers like Schwartz and Gillette. There is a tendency to see this massive congregation of animals as evidence for huge packs of Coelophysis roaming the land. No direct evidence for flocking exists; the deposits only indicate that large numbers of Coelophysis, along with other Triassic animals, were buried together. Some of the evidence from the taphonomy of the site indicates that these animals may have been gathered together to feed or drink from a depleted water hole or to feed on a spawning run of fish, and then became buried in a catastrophic flash flood or a drought.
With 30 specimens of C. rhodesiensis found together in Zimbabwe some palaeontologists have suggested that Coelophysis was indeed gregarious. Again there is no direct evidence of flocking in this case and it has also been suggested that these individuals were also victims of flash flooding as it appears to have been commonplace during this period.
Growth and sexual dimorphism
Rinehart (2009) assessed the ontogenic growth of this genus using data gathered from the length of its upper leg bone (femur) and concluded that Coelophysis juveniles grew rapidly, especially during the first year of life. Coelophysis likely reached sexual maturity between the second and third year of life and reached its full size, just above 10 feet in length, by its eighth year. This study identified four distinct growth stages: 1-year, 2-year, 4-year, and 7+ year. It was also thought, that as soon as they were hatched, they would have to fend for themselves.
Two "morphs" of Coelophysis have been identified: a more gracile form, as in specimen AMNH 7223, and a slightly more robust form, as in specimens AMNH 7224 and NMMNH P-42200. Skeletal proportions were different between these two forms; the gracile form has a longer skull, a longer neck, shorter forelimbs, and has sacral neural spines that are fused; and the robust form has a shorter skull, a shorter neck, longer forelimbs, and unfused sacral neural spines. Historically, many arguments have been made that this represents some sort of dimorphism in the population of Coelophysis, probably sexual dimorphism. Raath agreed that dimorphism in Coelophysis is evidenced by the size and structure of the forelimb. Rinehart et al. studied 15 individuals, and agreed that two morphs were present, even in juvenile specimens, and suggested that sexual dimorphism was present early in life, prior to sexual maturity. Rinehart concluded that the gracile form was female and the robust form was male based on differences in the sacral vertebrae of the gracile form, which allowed for greater flexibility for egg laying. Further support for this position was provided by an analysis showing that each morph comprised 50% of the population, as would be expected in a 50/50 sex ratio.
However, more recent research has found that C. bauri and C. rhodesiensis had highly variable growth between individuals, with some specimens being larger in their immature phase than smaller adults were when completely mature; this indicates that the supposed presence of distinct morphs is simply the result of individual variation. This highly variable growth was likely ancestral to dinosaurs but later lost, and may have given such early dinosaurs an evolutionary advantage in surviving harsh environmental challenges.
Through the compilation and analysis of a database of nearly three dozen birds and reptiles, and comparison with existing data about the anatomy of Coelophysis Rinehart et al. (2009) drew the following conclusions. It was estimated that average egg of Coelophysis was 31–33.5 millimeters across its minor diameter, and that each female would lay between 24 and 26 eggs in each clutch. The evidence suggested that some parental care was necessary to nurture the relatively small hatchlings during the first year of life, where they would reach 1.5 meters in length by the end of their first growth stage. Coelophysis bauri invested as much energy in reproduction as other extinct reptiles of its approximate size.
In C. rhodesiensis, healed fractures of the tibia and metatarsus have been observed, but are very rare. "[T]he supporting butresses of the second sacral rib" in one specimen of Syntarsus rhodesiensis showed signs of fluctuating asymmetry. Fluctuating asymmetry results from developmental disturbances and is more common in populations under stress and can therefore be informative about the quality of conditions a dinosaur lived under.
Specimens of Coelophysis have been recovered from the Chinle Formation of New Mexico and Arizona, more famously at the Ghost Ranch (Whitaker) quarry in the Rock Point member among other quarries in the underlying Petrified Forest member, the sediments of which have been dated to approximately 212 million years ago, making them part of the middle Norian stage of the Late Triassic.
C. rhodesiensis has been recovered in the Upper Elliott Formation in the Cape and Free State provinces of South Africa as well as the Chitake River bonebed quarry at the Forest Sandstone Formation in Zimbabwe.
Fauna and habitat
Ghost Ranch was located close to the equator over 200 million years ago, and had a warm, monsoon-like climate with heavy seasonal precipitation. Hayden Quarry, a new excavation site at Ghost Ranch, New Mexico, has yielded a diverse collection of fossil material that included the first evidence of dinosaurs and less-advanced dinosauromorphs from the same time period. The discovery indicates that the two groups lived together during the early Triassic period 235 million years ago.
Therrien and Fastovsky (2001) examined the paleoenvironment of Coelophysis and other early theropods from Petrified Forest National Park in Arizona, and determined that this genus lived in an environment that consisted of floodplains marked by distinct dry and wet seasons. There was a great deal of competition during drier times when animals struggled for water in riverbeds that were drying up.
In the upper sections of the Chinle Formation where Coelophysis is found, dinosaurs were rare, so far only Chindesaurus and Daemonosaurus are known, the terrestrial fauna being dominated instead by other reptiles like the rhynchocephalian Whitakersaurus; the pseudosuchian Revueltosaurus; the aetosaurs Desmatosuchus, Typothorax and Heliocanthus; the crocodilomorph Hesperosuchus; the "rauisuchians" Shuvosaurus, Effigia and Vivaron; along other rare components like the dinosauriform Eucoelophysis, and the amniote Kraterokheirodon. In the waterways we find the phytosaur Machaeroprosopus; the archosauromorph Vancleavea; the amphibians Apachesaurus and Koskinonodon; and the fishes Reticulodus, Arganodus and Lasalichthyes.
The Upper Elliot Formation is thought to have been an ancient floodplain. Fossils of the prosauropod dinosaur Massospondylus and Ignavusaurus have been recovered from the Upper Elliot Formation, which boasts the world's most diverse fauna of early Jurassic ornithischian dinosaurs, including Abrictosaurus, Fabrosaurus, Heterodontosaurus, and Lesothosaurus, among others. The Forest Sandstone Formation was the paleoenvironment of protosuchid crocodiles, sphenodonts, the dinosaur Massospondylus and indeterminate remains of a prosauropod. Paul (1988) noted that Megapnosaurus rhodesiensis lived among desert dunes and oases and hunted juvenile and adult prosauropods.
The multitude of specimens deposited so closely together at Ghost Ranch was probably the result of a flash flood, which swept away a large number of Coelophysis and buried them quickly and simultaneously. In fact, it seems that such flooding was commonplace during this period of the Earth's history and, indeed, the Petrified Forest of nearby Arizona is the result of a preserved log jam of tree trunks that were caught in one such flood. Whitaker quarry at Ghost Ranch is considered a monotaxic site because it features multiple individuals of a single taxon. The quality of preservation and the ontogenic (age) range of the specimens helped make Coelophysis one of the best known of all genera. In 2009, Rinehart et al. noted that in one case the Coelophysis specimens were "washed into a topographic low containing a small pond, where they probably drowned and were buried by a sheet flood event from a nearby river."
The 30 specimens of C. rhodesiensis found together in Zimbabwe was also probably the result of a flash flood, which swept away a large number of Coelophysis and buried them quickly and simultaneously as well.
Edwin H. Colbert has suggested that the theropod footprints referred to the ichnogenus Grallator, located in the Connecticut River Valley across Connecticut and Massachusetts, may have been made by Coelophysis. The footprints are from the Late Triassic to Early Jurassic aged Newark Supergroup. They clearly show digits II III and IV but not I or V. That condition is strange for footprints of their age. The digits were presumed to be stubby and ineffective, not touching the ground when the dinosaur was walking or running. They have been thought to be from an unidentified, primitive saurischian similar to Coelophysis by David B. Weishampel and L. Young more recently. Skeletal remains resembling Coelophysis have also been found in the valley, supporting the idea that a species similar to Coelophysis is responsible for the footprints.
Dinosaur footprints that were later attributed to C. rhodesiensis were discovered in Rhodesia in 1915. These tracks were discovered at the Nyamandhlovu Sandstones Formation, in eolian red sandstone that was deposited in the Late Triassic, approximately 235 to 201 million years ago.
In popular culture
Coelophysis was the second dinosaur in space, following Maiasaura (STS-51-F). A Coelophysis skull from the Carnegie Museum of Natural History was aboard the Space Shuttle Endeavour mission STS-89 when it left the atmosphere on 22 January 1998. It was also taken onto the space station Mir before being returned to Earth.
As being over 100 years old, Coelophysis is one of the best-known dinosaurs in literature. It was designated as the official state fossil of New Mexico in 1981, and is now the logo of the New Mexico Museum of Natural History.
- Bristowe, A. & M.A. Raath (2004). "A juvenile coelophysoid skull from the Early Jurassic of Zimbabwe, and the synonymy of Coelophysis and Syntarsus.(USA)". Palaeontologica Africana. 40 (40): 31–41.CS1 maint: uses authors parameter (link)
- Carrano, Matthew T.; Benson, Roger B. J.; Sampson, Scott D. (2012). "The phylogeny of Tetanurae (Dinosauria: Theropoda)". Journal of Systematic Palaeontology. 10 (2): 211–300. doi:10.1080/14772019.2011.630927. S2CID 85354215.
- Nesbitt, Sterling J.; Irmis, Randall B.; Parker, William G. (2007). "A critical re-evaluation of the Late Triassic dinosaur taxa of North America" (PDF). Journal of Paleontology. 5 (2): 209–243. doi:10.1017/s1477201907002040. S2CID 28782207.
- Nesbitt, Irmis and Parker, 2007. A critical re-evaluation of the Late Triassic dinosaur taxa of North America. Journal of Systematic Palaeontology. 5(2), 209–243.
- "RE: Afrovenator pronunciation". dml.cmnh.org. Retrieved 26 May 2019.
- Gaines, Richard M. (2001). Coelophysis. ABDO Publishing Company. p. 4. ISBN 978-1-57765-488-9.
- Weishampel, David B; et al. (2004). "Dinosaur distribution (Early Jurassic, Africa)." In: Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. Pp. 535–536. ISBN 0-520-24209-2.
- Schwartz, Hilde L.; Gillette, David D. (1994). "Geology and taphonomy of the Coelophysis quarry, Upper Triassic Chinle Formation, Ghost Ranch, New Mexico". Journal of Paleontology. 68 (5): 1118–1130. doi:10.1017/S0022336000026718. JSTOR 1306181.
- Paul, Gregory S. (1988). Predatory Dinosaurs of the World. Simon & Schuster. p. 260. ISBN 978-0-671-61946-6.
- Rinehart, L.F.; Lucas, S.G.; Heckert, A.B.; Spielmann, J.A. & Celesky, M.D. (2009). "The paleobiology of Coelophysis bauri (Cope) from the Upper Triassic (Apachean) Whitaker quarry, New Mexico, with detailed analysis of a single quarry block". New Mexico Museum of Natural History & Science, A Division of the Department of Cultural Affairs Bulletin. 45: 260.CS1 maint: uses authors parameter (link)
- Rinehart, Larry F.; Lucas, Spencer G.; Hunt, Adrian P. (2007). "Furculae in the Late Triassic theropod dinosaur Coelophysis bauri". Paläontologische Zeitschrift. 81 (2): 174–180. doi:10.1007/bf02988391. S2CID 129076419.
- Tykoski, R.S. & Rowe, T. (2004). "Ceratosauria": In: Weishampel, D.B.; Dodson, P.; Osmolska, H., eds. (6 November 2004). The Dinosauria (Second ed.). Berkeley: University of California Press. pp. 47–70. ISBN 978-0-520-24209-8.
- Gay, R.J. (2001). "An unusual adaptation in the caudal vertebrae of Coelophysis bauri (Dinosauria: Theropoda)". PaleoBios. 21: 55.
- Rinehart, L.F.; Heckert, A.B.; Lucas, S.G. & Hunt, A.P. (2004). "The sclerotic ring of the Late Triassic theropod dinosaur Coelophysis". New Mexico Geological Society Spring Meeting. 26: 64.CS1 maint: uses authors parameter (link)
- Colbert, E. (1989). "The Triassic Dinosaur Coelophysis". Museum of Northern Arizona Bulletin. 57: 160.
- Ezcurra, M.D. (2007). "The cranial anatomy of the coelophysoid theropod Zupaysaurus rougieri from the Upper Triassic of Argentina". Historical Biology. 19 (2): 185–202. doi:10.1080/08912960600861467. S2CID 129449572.
- Bristowe, A. & Raath, M.A. (2004). "A juvenile coelophysoid skull from the Early Jurassic of Zimbabwe, and the synonymy of Coelophysis and Syntarsus" (PDF). Palaeontologia Africana. 40: 31–41. ISSN 0078-8554.CS1 maint: uses authors parameter (link)
- Downs, A. (2000). "Coelophysis bauri and Syntarsus rhodesiensis compared, with comments on the preparation and preservation of fossils from the Ghost Ranch Coelophysis quarry": In: Lucas, S.G.; Heckert, A.B. (eds.). "Dinosaurs of New Mexico". New Mexico Museum of Natural History Bulletin. 17: 33–37.
- Colbert, E.H.; Charig, A.J.; Dodson, P.; Gillette, D.D.; Ostrom, J.H. & Weishampel, D.B. (1992). "Coelurus bauri Cope, 1887 (currently Coelophysis bauri; Reptilia, Saurischia): Proposed replacement of the lectotype by a neotype" (PDF). Bulletin of Zoological Nomenclature. 49 (4): 276–279.CS1 maint: uses authors parameter (link)
- Cope, E.D. (1889). "On a new genus of Triassic Dinosauria". The American Naturalist. 23 (271): 621–633. doi:10.1086/274979.
- Glut, D.F. (1999). Dinosaurs, the Encyclopedia, Supplement 1. McFarland & Company, Inc. p. 442. ISBN 978-0-7864-0591-6.
- Cope, E.D. (1887). "The Dinosaurian Genus Coelurus". The American Naturalist. xxi 5: 367-369.
- Haines, T. & Chambers, P. (2007). The Complete Guide to Prehistoric Life. Firefly Books. pp. 70–71. ISBN 978-1-55407-181-4.CS1 maint: uses authors parameter (link)
- International Commission on Zoological Nomenclature (1996). "Opinion 1842: Coelurus bauri Cope, 1887 (currently Coelophysis bauri; Reptilia, Saurischia): lectotype replaced by a neotype" (PDF). Bulletin of Zoological Nomenclature. 53 (2): 142–144.
- Raath (1969). "A new Coelurosaurian dinosaur from the Forest Sandstone of Rhodesia." Arnoldia Rhodesia. 4 (28): 1–25.
- Tykoski, R. S., and Rowe, T., 2004, Ceratosauria, Chapter Three: In: The Dinosauria, Second Edition, edited by Weishampel, D.B., Dodson, P., and Osmolska, H., California University Press, p. 47-70.
- Sues, H.D.; Nesbitt, S.J.; Berman, D.S.; Henrici, A.C. (2011). "A late-surviving basal theropod dinosaur from the latest Triassic of North America". Proceedings of the Royal Society B. 278 (1723): 3459–3464. doi:10.1098/rspb.2011.0410. PMC 3177637. PMID 21490016.
- "Coelophysoidea". theropoddatabase.com. Retrieved 5 February 2016.
- "Facial variation in Coelophysis bauri and the status of Megapnosaurus (Syntarsus)". nmstatefossil.org. Retrieved 5 February 2016.
- Hunt, Adrian P.; Lucas, Spencer G. (1991). "Rioarribasaurus, a new name for a Late Triassic dinosaur from New Mexico (USA)". Paläontologische Zeitschrift. 65 (1/2): 191–198. doi:10.1007/bf02985783. S2CID 129577216.
- Talbot, M. (1911). "Podokesaurus holyokensis, a new dinosaur from the Triassic of the Connecticut Valley". American Journal of Science. 4. 31 (186): 469–479. Bibcode:1911AmJS...31..469T. doi:10.2475/ajs.s4-31.186.469.
- Colbert, E. (1964). "The Triassic dinosaur genera Podokesaurus and Coelophysis". American Museum Novitates. 2168: 1–12.
- Colbert, E.; Baird, D. (1958). "Coelurosaur bone casts from the Connecticut Valley Triassic". American Museum Novitates. 1901: 1–11.
- Getty, P. R.; Bush, A. M. (2011). "Sand pseudomorphs of dinosaur bones: Implications for (non-) preservation of tetrapod skeletal material in the Hartford Basin, USA". Palaeogeography, Palaeoclimatology, Palaeoecology. 302 (3–4): 407–414. Bibcode:2011PPP...302..407G. doi:10.1016/j.palaeo.2011.01.029.
- Olshevsky, G. (1991). "A revision of the parainfraclass Archosauria Cope, 1869, excluding the advanced Crocodylia" (PDF). Mesozoic Meanderings 2: 196.
- Sullivan, Robert M.; Lucas, Spencer G. (1999). "Eucoelophysis baldwini, a new theropod dinosaur from the Upper Triassic of New Mexico, and the status of the original types of Coelophysis". Journal of Vertebrate Paleontology. 19 (1): 81–90. doi:10.1080/02724634.1999.10011124.
- Nesbitt, Sterling J.; Irmis, Randall B.; Parker, William G. (2007). "A critical re-evaluation of the Late Triassic dinosaur taxa of North America". Journal of Systematic Palaeontology. 5 (2): 209–243. doi:10.1017/S1477201907002040. S2CID 28782207.
- Ivie, M. A.; Ślipiński, S. A.; Węgrzynowicz, P. (2001). "Generic homonyms in the Colydiinae (Coleoptera: Zopheridae)". Insecta Mundi. 15: 63–64.
- Mortimer, Mickey (2012). "Coelophysoidea". Archived from the original on 4 May 2013.
- Yates, A.M. (2005). "A new theropod dinosaur from the Early Jurassic of South Africa and its implications for the early evolution of theropods". Palaeontologia Africana. 41: 105–122.
- Paul G.S. (1993). "Are Syntarsus and the Whitetaker theropod the same genus?": In: Lucas, S.G.; Morales, M. (eds.). "The Nonmarine Triassic". New Mexico Museum of Natural History Bulletin. 3: 397–402.
- Ezcurra, M.D.; Brusatte, S.L. (2011). "Taxonomic and phylogenetic reassessment of the early neotheropod dinosaur Camposaurus arizonensis from the Late Triassic of North America". Palaeontology. 54 (4): 763–772. doi:10.1111/j.1475-4983.2011.01069.x.
- Benton, M. (1993). Dinosaur and other prehistoric animal Fact Finder. Kingfisher Books Ldt. p. 256. ISBN 978-0-86272-949-3.
- Carpenter, K. (2002). "Forelimb bio-mechanics of non-avian theropod dinosaurs in predation". Senckenbergiana Lethaea. 82: 59–76. doi:10.1007/bf03043773. S2CID 84702973.
- Gay, R.J. (2002). "The myth of cannibalism in Coelophysis bauri". Journal of Vertebrate Paleontology. 22 (3): 57A.
- Nesbitt, S. J.; Turner, A. H; Erickson, G. M; Norell, M. A (2006). "Prey choice and cannibalistic behaviour in the theropod Coelophysis". Biology Letters. 22. 2 (4): 611–614. doi:10.1098/rsbl.2006.0524. PMC 1834007. PMID 17148302.
- Gay, R.J. (2010a). Notes on Early Mesozoic Theropods (First ed.). Lulu press. pp. 9–24. ISBN 978-0-557-46616-0.
- Schwartz, H.L. & Gillette, D.D. (1994). "Geology and taphonomy of the Coelophysis quarry, Upper Triassic Chinle Formation, Ghost Ranch, New Mexico". Journal of Paleontology. 68 (5): 1118–1130. doi:10.1017/S0022336000026718. JSTOR 1306181.CS1 maint: uses authors parameter (link)
- G. Bond, 1965. Some new fossil localities in the Karroo System of Rhodesia. Arnoldia, Series of Miscellaneous Publications, National Museum of Southern Rhodesia 2(11):1–4
- M. A. Raath, 1977. The Anatomy of the Triassic Theropod Syntarsus rhodesiensis (Saurischia: Podokesauridae) and a Consideration of Its Biology. Department of Zoology and Entomology, Rhodes University, Salisbury, Rhodesia 1–233
- Paul, Gregory S. (2010). The Princeton Field Guide to Dinosaurs. Princeton University Press. p. 74. ISBN 978-0-691-13720-9.
- Carpenter, K.; Currie, P.J. (1990). Dinosaur Systematics: Approaches and Perspectives. Cambridge: Cambridge University Press. pp. 91–105. ISBN 978-0-521-43810-0.
- Gay, R. (2005). "Sexual Dimorphism in the Early Jurassic Theropod Dinosaur Dilophosaurus and a Comparison with Other Related Forms": In: Carpenter, K., ed. (2005). The Carnivorous Dinosaurs. Bloomington: Indiana University Press. pp. 277–283. ISBN 978-0-253-34539-4.
- Rinehart, L.F.; Lucas, S.G.; Heckert, A.B. (2001). "Preliminary statistical analysis defining the juvenile, robust and gracile forms of the Triassic dinosaur Coelophysis". Journal of Vertebrate Paleontology. 21: 93A. doi:10.1080/02724634.2001.10010852. S2CID 220414868.
- Griffin, C.T.; Nesbitt, S.J. (2016). "Anomalously high variation in postnatal development is ancestral for dinosaurs but lost in birds". Proceedings of the National Academy of Sciences of the United States of America. 113 (51): 14757–14762. Bibcode:2016PNAS..11314757G. doi:10.1073/pnas.1613813113. PMC 5187714. PMID 27930315.
- Glut, D.F. (2012). Dinosaurs, the Encyclopedia, Supplement 7. McFarland & Company, Inc. p. 866. ISBN 978-0-7864-4859-3.
- Rothschild, B.; Tanke, D.H. & Ford, T.L. (2001). "Theropod stress fractures and tendon avulsions as a clue to activity": In: Tanke, D. H.; Carpenter, K., eds. (2001). Mesozoic Vertebrate Life. Indiana University Press. pp. 331–336. ISBN 978-0-253-33907-2.
- Molnar, R. E., 2001, Theropod paleopathology: a literature survey: In: Mesozoic Vertebrate Life, edited by Tanke, D. H., and Carpenter, K., Indiana University Press, p. 337-363.
- Irmis, Randall B.; Mundil, Roland; Martz, Jeffrey W.; Parker, William G. (15 September 2011). "High-resolution U–Pb ages from the Upper Triassic Chinle Formation (New Mexico, USA) support a diachronous rise of dinosaurs". Earth and Planetary Science Letters. 309 (3–4): 258–267. Bibcode:2011E&PSL.309..258I. doi:10.1016/j.epsl.2011.07.015.
- Braginetz, Donna (2007). "A new species of dinosauromorph (lower left) was among the mixed assemblage of dinosaurs and dinosauromorphs found at Hayden Quarry in Ghost Ranch, N.M." American Museum of Natural History. Retrieved 31 March 2013.
- Therrien, F.; Fastovsky, D. E. (2000). "Paleoenvironments of early theropods, Chinle Formation (Late Triassic), Petrified Forest National Park, Arizona". PALAIOS. 3. 15 (3): 194–211. Bibcode:2000Palai..15..194T. doi:10.1669/0883-1351(2000)015<0194:POETCF>2.0.CO;2.
- Sues, H. -D.; Nesbitt, S. J.; Berman, D. S.; Henrici, A. C. (2011). "A late-surviving basal theropod dinosaur from the latest Triassic of North America". Proceedings of the Royal Society B: Biological Sciences. 278 (1723): 3459–64. doi:10.1098/rspb.2011.0410. PMC 3177637. PMID 21490016.
- Heckert, A.B.; Lucas, S.G.; Rinehart, L.F.; Hunt, A.P. (2008). "A new genus and species of sphenodontian from the Ghost Ranch Coelophysis Quarry (Upper Triassic: Apachean), Rock Point Formation, New Mexico, USA". Palaeontology. 51 (4): 827–845. doi:10.1111/j.1475-4983.2008.00786.x.
- Irmis, R.B. (2005). "The vertebrate fauna of the Upper Triassic Chinle Formation in northern Arizona": In: Nesbitt, S.J.; Parker, W.G.; Irmis, R.B. (eds.). "Guidebook to the Triassic formations of the Colorado Plateau in northern Arizona: Geology, Paleontology, and History" (PDF). Mesa Southwest Museum Bulletin. 9: 63–88. Archived from the original (PDF) on 4 October 2012. Retrieved 2 January 2014.
- Benson, R.J.; Brusatte, S.; Clack, J.; Anderson, J.; Dennis-Bryan, K.; Hone, D.; Duffin, C.; Johanson, Z.; Milner, A.; Naish, D.; Parsons, K.; Prothero, D.; Xu, X. (2012). Prehistoric Life. London: Dorling Kindersley. pp. 214–215. ISBN 978-0-7566-9910-9.CS1 maint: uses authors parameter (link)
- Emily J. Lessner; Michelle R. Stocker; Nathan D. Smith; Alan H. Turner; Randall B. Irmis; Sterling J. Nesbitt (2016). "A new rauisuchid (Archosauria, Pseudosuchia) from the Upper Triassic (Norian) of New Mexico increases the diversity and temporal range of the clade". PeerJ. 4: e2336. doi:10.7717/peerj.2336. PMC 5018681. PMID 27651983.
- Weishampel, D.B.; Dodson, P.; & Osmólska, H. (2004). The Dinosauria (Second ed.). Berkeley: University of California Press. pp. 518–521. ISBN 978-0-520-24209-8.CS1 maint: uses authors parameter (link)
- Mueller, B.D. (2007). "Koskinonodon Branson and Mehl, 1929, a replacement name for the preoccupied temnospondyl Buettneria Case, 1922". Journal of Vertebrate Paleontology. 27 (1): 225. doi:10.1671/0272-4634(2007)27[225:KBAMAR]2.0.CO;2.
- Paul, G. S., 1988, Predatory Dinosaurs of the World, a complete Illustrated guide: New York Academy of sciences book, 464pp.
- Glut, D.F. (2006). Dinosaurs, the Encyclopedia, Supplement 4. McFarland & Company, Inc. p. 749. ISBN 978-0-7864-2295-1.
- Colbert, Edwin H. (1965). The Age of Reptiles. W. W. Norton & Company. p. 97. ISBN 978-0-486-29377-6.
- Weishampel, D.B; Young, L. (1998). Dinosaurs of the East Coast. Johns Hopkins University Press. ISBN 978-0-8018-5217-6.
- "Dinosaur footprints of the Connecticut River Valley". Nash Dinosaur Track Site and Rock Shop.
- M. A. Raath. 1972. First record of dinosaur footprints from Rhodesia. Arnoldia 5(37):1–5
- Chure, D. (2009). "dino bones in space – was it a PR thing". Cleveland Museum of Natural History. Retrieved 12 November 2011.
- Parker, Steve (2003). Dinosaurs: the complete guide to dinosaurs. Firefly Books. ISBN 978-1-55297-772-9.
|Wikimedia Commons has media related to Coelophysis.|
|Wikispecies has information related to Coelophysis|
- Coelophysis in the Dino Directory