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Gojirasaurus

From Wikipedia, the free encyclopedia
Extinct genus of dinosaurs
This article is about the dinosaur. For the giant movie monster also known as "Godzillasaurus", seeGodzilla.

Gojirasaurus
Temporal range:Late Triassic, "Revueltian" (mid-lateNorian),212 Ma
Scale and skeletal diagram
Scientific classificationEdit this classification
Kingdom:Animalia
Phylum:Chordata
Class:Reptilia
Clade:Dinosauria
Clade:Saurischia
Clade:Theropoda
Genus:Gojirasaurus
Carpenter, 1997
Species:
G. quayi
Binomial name
Gojirasaurus quayi
Carpenter, 1997
Synonyms

Gojirasaurus is agenus ofcoelophysoidtheropoddinosaur named after the giant monster movie characterGodzilla. It lived in the Late Triassic Period, containing a single known species,Gojirasaurus quayi.

Discovery

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Gojirasaurus quayi was described and named byKenneth Carpenter in1997 based on a partial skeleton, theholotype specimen UCM 47221, fromQuay County, New Mexico. The holotype is an assortment of various postcranial bones, including a rightscapula, rightpubis, lefttibia, leftmetatarsal V,[1] fourvertebralcentra, aneural arch, and fragments of ribs andgastralia.[2] In addition, a single large serrated tooth is associated with the postcranial material. The holotype is housed in the collections of theUniversity of Colorado Museum of Natural History, in Boulder, Colorado.[2]

The specimen hails from purplish-greymudstones of theBull Canyon Formation (sometimes called theCooper Canyon Formation), a major fossiliferous component of theDockum Group in eastern New Mexico. In particular, it was found at a site in the vicinity of Revuelto Creek, the type locality for theRevueltian "faunachron".[3] The Revueltian is abiostratigraphic unit roughly equivalent to the mid-lateNorian stage of the Triassic Period, approximately 215–207 million years ago.[4] The Revuelto Creek fossils were deposited in the earlier part of the Revueltian, close to around 212 million years ago.[5]

Though it would not be formally named until 1997, the fossils ofGojirasaurus were frequently mentioned through the 1980s and 1990s, as a robustCoelophysis-like theropod from Revuelto Creek.[6][7] Among these preliminary accounts is a short description by Parrish & Carpenter (1986).[8] In 1994, an unpublishedthesis by Adrian Hunt attempted to name the Revuelto Creek theropod as "Revueltoraptor lucasi". Hunt's conception of the species included not just UCM 47221, but also numerous theropod-like fossils stored at the NMMNH (New Mexico Museum of Natural History and Science). As a name, "Revueltoraptor lucasi" was never formally published, and later evaluations recognized that most of Hunt's additional fossils are likely fromShuvosaurus rather than theropods.[2]

Etymology

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Thegeneric nameGojirasaurus is derived from the name of the giant Japanese movie monster "Gojira" (Godzilla) and theGreek word "sauros" (σαυρος) meaning "lizard";[9] thus, "Godzilla lizard". Carpenter (1997) selected "Gojira" in reference to the relatively large size of this theropod, which exceeded that of its Triassic counterparts. Thespecific namequayi is a reference to Quay County.[2]

Description

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Speculative life restoration

Gojirasaurus is one of the largesttheropods known from theTriassic Period, with an estimate total length of 5.5–6 metres (18–20 ft) long and a weight of at least 150 kilograms (330 lb).[2][10] Benson et al. (2018) estimated that it weighed around 190 kilograms (420 lb), only exceeded byHerrerasaurus among Triassiccarnivorousdinosaurs.[11] Carpenter (1997) pointed to features of thepelvis andankle suggesting that this was an immature individual, and could therefore have grown to even a larger size in maturity.[2] Christopher T. Griffin (2019) and Griffin andNesbitt (2020) confirmed thatGojirasaurus possessed features indicative of ontogenetic immaturity.[1][12]

Distinguishing anatomical features

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According to Nesbittet al. (2007),Gojirasaurus can be distinguished based on the fact that itstibia is more robust than that of its relativeCoelophysis. Rauhut (2003) attempted to diagnose this genus based on the fact that the mid/posterior dorsalvertebrae had taller neural spines than those observed in othercoelophysoids.[13]

Griffin (2019) followed Nesbitt (2007)'s diagnosis onGojirasaurus and distinguishes it fromMegapnosaurus andDilophosaurus based on several characteristics of metatarsal V.[1]

Classification

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Parrish and Carpenter (1986) drew similarities between UCM 47221 and "Halticosaurus liliensterni", a largeGermantheropod now known asLiliensternus. Both were assigned to the family "Procompsognathidae", though the authors acknowledged that family names in use at the time were provisional and likely to be obsolete in the future.[8] Conversely, Hunt (1994) and Hunt et al. (1998)[14] argued that the specimen is aherrerasaurid, alongside various other fossils from theLate Triassic ofNorth America.[15][16] The formal naming and description ofGojirasaurus by Carpenter (1997) firmly classified it withinCoelophysoidea. Many traits were comparable toCoelophysis,Dilophosaurus, and particularlyLiliensternus.[2]

Variousphylogenetic analyses in the 2000s supported coelophysoid affinities forGojirasaurus, close to or among the smallerCoelophysidae rather than withDilophosaurus.[13][17][18][19][20] Many studies noted that its remains are too fragmentary for further elaboration. Starting with Yates (2005), themonophyly of Coelophysoidea has been brought into question, withDilophosaurus resolving as more closely related toaverostrans (non-coelophysoid theropods).[18] In some analyses,Gojirasaurus maintains its position among the coelophysids,[18] but other studies instead bring it over to the lineage leading toDilophosaurus and averostrans.[21][22][23]

Validity

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A persistent question regardingGojirasaurus quayi is how much of its fossil material actually belongs to one species.[15]Gojirasaurus coexisted withShuvosaurus, an unusualreptile with a toothless beak and bipedal stance. Though previously regarded as an aberrant dinosaur, by 2007 most specialists agreed thatShuvosaurus was actually more closely related to crocodilians, and that its dinosaur-like traits are merelyconvergent.[24] According to Nesbitt et al. (2007), some components of UCM 47221, such as the tibia and pubis, are clearly coelophysoid in form and distinct fromShuvosaurus.[15] However, other parts of the skeleton, such as the scapula and vertebrae, are not readily distinguishable fromShuvosaurus.[15] The serrated tooth could be from any number of large carnivorousarchosaurs which inhabited the area.[15]

Even the assuredly coelophysoid components of the skeleton have few unambiguous unique features. For example, the robust tibia is similar toCoelophysis-like fossils whichKevin Padian (1986) described fromPetrified Forest National Park in Arizona, only differing in size.[25][15][16] Several studies regardGojirasaurus as a "metataxon": a collection of fossils for which assignment to a single species can neither be proven nor disproven.[13][15] Nevertheless,Gojirasaurus persists in thescientific literature as a useful example of a large Triassic coelophysoid, validity notwithstanding.[11][1][12]

Paleoecology

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Main article:Bull Canyon Formation

Gojirasaurus's assignment to theCoelophysoidea would suggest that it was a bipedal, terrestrial, actively mobilecarnivore.

TheRevuelto Creek area preserves a diverse fauna of both terrestrial and aquatic animals from theBull Canyon Formation.[6][8][7][26] On land,herbivorouspseudosuchians are quite common, including theshuvosauridShuvosaurus inexpectatus,[26] theaetosaursTypothorax coccinarum,[7][26]Paratypothorax,[7] andRioarribasuchus,[27] and the smallaetosauriformRevueltosaurus callenderi.[28] BothShuvosaurus andRevueltosaurus have previously been misidentified asdinosaurs.[7][26]

Among terrestrial carnivores,Gojirasaurus was joined by at least a few other true dinosaurs. Bull Canyon dinosaur fragments are sometimes identified ascoelophysids,herrerasaurids,[26] and/orChindesaurus,[7] but most are too fragmentary to assess in great detail.[15][1][5]Lepidosauromorphs,crocodylomorphs, and large carnivorousrauisuchians are also represented by rare fragments.[26] Particularly robustarchosauromorph limb fragments, previously thought to be from a late-survivingrhynchosaur ("Otischalkia"),[7][26] are probably frommalerisaurineazendohsaurids instead.[29] The earlyturtleChinlechelys tenertesta is a notable component of the terrestrial fauna.[30][31]

Phytosaurfossils are common at Revuelto Creek. One particularly impressive phytosaurskull was initially referred toSmilosuchus gregorii,[6][8] and later toArribasuchus buceros.[7] It and other Bull Canyon phytosaur remains most likely belong to a species ofMachaeroprosopus (Pseudopalatus).[26][32] Smallmetoposauridamphibians, sometimes identified as "Apachesaurus gregorii",[7][26] frequent the area alongside larger metoposaurids.[6][26] Variousfish inhabited the waterways:arganodontidlungfish,coelacanths (Quayia zideki), andactinopterygians.[6][26]

See also

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References

[edit]
  1. ^abcdeGriffin, Christopher T. (September 2019)."Large neotheropods from the Upper Triassic of North America and the early evolution of large theropod body sizes".Journal of Paleontology.93 (5):1010–1030.Bibcode:2019JPal...93.1010G.doi:10.1017/jpa.2019.13.ISSN 0022-3360.
  2. ^abcdefgCarpenter, Kenneth (13 August 1997)."A Giant Coelophysoid (Ceratosauria) Theropod from the Upper Triassic of New Mexico, USA".Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen.205 (2):189–208.Bibcode:1997NJGPA.205..189C.doi:10.1127/njgpa/205/1997/189.ISSN 0077-7749.
  3. ^Lucas, Spencer G (1 November 1998)."Global Triassic tetrapod biostratigraphy and biochronology".Palaeogeography, Palaeoclimatology, Palaeoecology.143 (4):347–384.Bibcode:1998PPP...143..347L.doi:10.1016/S0031-0182(98)00117-5.ISSN 0031-0182.
  4. ^Martz, J. W.; Parker, W. G. (1 January 2017), Zeigler, Kate E.; Parker, William G. (eds.),"Revised Formulation of the Late Triassic Land Vertebrate "Faunachrons" of Western North America: Recommendations for Codifying Nascent Systems of Vertebrate Biochronology",Terrestrial Depositional Systems, Elsevier, pp. 39–125,ISBN 978-0-12-803243-5, retrieved28 August 2022{{citation}}: CS1 maint: work parameter with ISBN (link)
  5. ^abMarsh, Adam D.; Parker, William G. (12 November 2020)."New dinosauromorph specimens from Petrified Forest National Park and a global biostratigraphic review of Triassic dinosauromorph body fossils"(PDF).PaleoBios.37:1–56.doi:10.5070/p9371050859.ISSN 2373-8189.
  6. ^abcdeCarpenter, Kenneth; Parrish, Michael (1985)."Late Triassic Vertebrates from Revuelto Creek, Quay County, New Mexico"(PDF).New Mexico Geological Society Guidebook, 36th Field Conference, Santa Rosa:197–198.
  7. ^abcdefghiLong, 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.
  8. ^abcdParrish, Michael; Carpenter, Kenneth (1986)."A new vertebrate fauna from the Dockum Formation (Late Triassic) of eastern New Mexico". In Padian, Kevin (ed.).The Beginning of the Age of Dinosaurs. New York: Cambridge University Press. pp. 151–160.ISBN 0521303281.
  9. ^Liddell, Henry George andRobert Scott (1980).A Greek-English Lexicon (Abridged ed.). United Kingdom: Oxford University Press.ISBN 978-0-19-910207-5.
  10. ^Paul, Gregory S. (2010).The Princeton Field Guide to Dinosaurs. Princeton, NJ: Princeton University Press. p. 74.ISBN 978-0-691-13720-9.
  11. ^abBenson, Roger B. J.; Hunt, Gene; Carrano, Matthew T.; Campione, Nicolás (2018). Mannion, Philip (ed.)."Cope's rule and the adaptive landscape of dinosaur body size evolution".Palaeontology.61 (1):13–48.Bibcode:2018Palgy..61...13B.doi:10.1111/pala.12329.ISSN 0031-0239.
  12. ^abGriffin, Christopher T.; Nesbitt, Sterling J. (2020)."Does the Maximum Body Size of Theropods Increase across the Triassic–Jurassic Boundary? Integrating Ontogeny, Phylogeny, and Body Size".The Anatomical Record.303 (4):1158–1169.doi:10.1002/ar.24130.ISSN 1932-8486.PMID 30968581.
  13. ^abcRauhut, Oliver W.M. (2003)."The interrelationships and evolution of basal theropod dinosaurs"(PDF).Special Papers in Palaeontology.69:1–213.
  14. ^Hunt, Adrian P.; Lucas, Spencer G.; Heckert, Andrew B.; Sullivan, Robert M.; Lockley, Martin G. (1998)."Late Triassic dinosaurs from the western United States"(PDF).Geobios.31 (4):511–531.Bibcode:1998Geobi..31..511H.doi:10.1016/S0016-6995(98)80123-X.
  15. ^abcdefghNesbitt, Sterling J.; Irmis, Randall B.; Parker, William G. (June 2007)."A critical re-evaluation of the Late Triassic dinosaur taxa of North America"(PDF).Journal of Systematic Palaeontology.5 (2):209–243.Bibcode:2007JSPal...5..209N.doi:10.1017/S1477201907002040.S2CID 28782207.
  16. ^abMortimer, Mickey (2012)."Coelophysoidea".The Theropod Database.
  17. ^Tykoski, R.S. & Rowe, T. (2004). "Ceratosauria". In: Weishampel, D.B., Dodson, P., & Osmolska, H. (Eds.) The Dinosauria (2nd edition). Berkeley: University of California Press. pp. 47–70ISBN 0-520-24209-2
  18. ^abcYates, Adam M. (2005)."A new theropod dinosaur from the Early Jurassic of South Africa and its implications for the early evolution of theropods"(PDF).Palaeontologia Africana.41:105–122.
  19. ^Carrano, Matthew T.; Hutchinson, John R.; Sampson, Scott D. (30 December 2005)."New information onSegisaurus halli, a small theropod dinosaur from the Early Jurassic of Arizona".Journal of Vertebrate Paleontology.25 (4):835–849.doi:10.1671/0272-4634(2005)025[0835:niosha]2.0.co;2.ISSN 0272-4634.
  20. ^Ezcurra, Martin D.; Novas, Fernando E. (2007)."Phylogenetic relationships of the Triassic theropod Zupaysaurus rougieri from NW Argentina".Historical Biology.19 (1):35–72.Bibcode:2007HBio...19...35E.doi:10.1080/08912960600845791.ISSN 0891-2963.
  21. ^Ezcurra, Martín D; Butler, Richard J; Maidment, Susannah C R; Sansom, Ivan J; Meade, Luke E; Radley, Jonathan D (1 January 2021)."A revision of the early neotheropod genus Sarcosaurus from the Early Jurassic (Hettangian–Sinemurian) of central England".Zoological Journal of the Linnean Society.191 (1):113–149.doi:10.1093/zoolinnean/zlaa054.hdl:11336/160038.ISSN 0024-4082.
  22. ^Spiekman, Stephan N. F.; Ezcurra, Martín D.; Butler, Richard J.; Fraser, Nicholas C.; Maidment, Susannah C. R. (2021)."Pendraig milnerae, a new small-sized coelophysoid theropod from the Late Triassic of Wales".Royal Society Open Science.8 (10) 210915.Bibcode:2021RSOS....810915S.doi:10.1098/rsos.210915.ISSN 2054-5703.PMC 8493203.PMID 34754500.
  23. ^Ezcurra, Martín D.; Marke, Daniel; Walsh, Stig A.; Brusatte, Stephen L. (20 November 2023)."A revision of the 'coelophysoid-grade' theropod specimen from the Lower Jurassic of the Isle of Skye (Scotland )".Scottish Journal of Geology.59 (1–2): 012.Bibcode:2023ScJG...59...12E.doi:10.1144/sjg2023-012.ISSN 0036-9276.
  24. ^Lucas, Spencer G.; Spielmann, Justin A.; Hunt, Adrian P. (2007)."Taxonomy ofShuvosaurus, a Late Triassic archosaur from the Chinle Group, American Southwest".New Mexico Museum of Natural History and Science Bulletin.41:259–261.
  25. ^Padian, Kevin (1986)."On the type material of Coelophysis Cope (Saurischia: Theropoda) and a new specimen from the Petrified Forest of Arizona (Late Triassic: Chinle Formation)". In Padian, Kevin (ed.).The Beginning of the Age of Dinosaurs. New York: Cambridge University Press. pp. 45–60.ISBN 0521303281.
  26. ^abcdefghijkHunt, Adrian P. (2001)."The vertebrate fauna, biostratigraphy and biochronology of the type Revultian land vertebrate faunachron, Bull Canyon Formation (Upper Triassic), east-central New Mexico"(PDF).New Mexico Geological Society Guidebook, 52nd Field Conference, Geology of the Llano Estacado. New Mexico Geological Society:123–151.doi:10.56577/FFC-52.123 (inactive 23 September 2025).ISBN 978-1-58546-087-8.{{cite journal}}: CS1 maint: DOI inactive as of September 2025 (link)
  27. '^Parker, W. G. (2007)."Reassessment of the aetosaurDesmatosuchus' chamaensis with a reanalysis of the phylogeny of the Aetosauria (Archosauria:Pseudosuchia)"(PDF).Journal of Systematic Palaeontology.5 (1):41–68.Bibcode:2007JSPal...5...41P.doi:10.1017/S1477201906001994.S2CID 85826683.
  28. ^Parker, William G.; Nesbitt, Sterling J.; Irmis, Randall B.; Martz, Jeffrey W.; Marsh, Adam D.; Brown, Matthew A.; Stocker, Michelle R.; Werning, Sarah (2022)."Osteology and relationships ofRevueltosaurus callenderi (Archosauria: Suchia) from the Upper Triassic (Norian) Chinle Formation of Petrified Forest National Park, Arizona, United States".The Anatomical Record.305 (10):2353–2414.doi:10.1002/ar.24757.ISSN 1932-8486.PMC 9544919.PMID 34585850.
  29. ^Christian A. Sidor; Marsh, Adam D.; Smith, Elliot Armour (30 May 2024)."The Allokotosaur (Reptilia: Archosauromorpha) Assemblage from a Multitaxic Bonebed in the Sonsela Member (Jim Camp Wash Beds, Chinle Formation) at Petrified Forest National Park, U.s.a.".Lithodendron: The Science and History Journal of Petrified Forest National Park.1 (Spring 2024):95–118.doi:10.69575/FAIY7658.
  30. ^Joyce, W.G.; Lucas, S.G.; Scheyer, T.M.; Heckert, A.B.; Hunt, A.P. (2009)."A thin-shelled reptile from the Late Triassic of North America and the origin of the turtle shell".Proceedings of the Royal Society B.276 (1656):507–513.doi:10.1098/rspb.2008.1196.ISSN 1471-2954.JSTOR 30244885.PMC 2664348.PMID 18842543.
  31. ^Lichtig, A. J.; Lucas, S. G. (2021)."Chinlechelys from the Upper Triassic of New Mexico, USA, and the origin of turtles".Palaeontologia Electronica.24 (1): Article number 24.1.a13.doi:10.26879/886.
  32. ^Hunt, Adrian P.; Lucas, Spencer G.; Spielmann, Justin A. (2006)."Sexual dimorphism in a large brachyrostral phytosaur (Archosauria: Crurotarsi) from the Late Triassic of western North America".New Mexico Museum of Natural History and Science Bulletin.37:563–567.

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