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Overoraptor

From Wikipedia, the free encyclopedia
Extinct genus of theropod dinosaurs
Not to be confused withOviraptor orOverosaurus.

Overoraptor
Life restoration
Scientific classificationEdit this classification
Kingdom:Animalia
Phylum:Chordata
Class:Reptilia
Clade:Dinosauria
Clade:Saurischia
Clade:Theropoda
Clade:Maniraptora
Clade:Pennaraptora
Clade:Paraves
Genus:Overoraptor
Type species
Overoraptor chimentoi

Overoraptor (/ˌʊuvərʊuˈræptər/, meaning "piebald thief") is anextinct genus ofparaviantheropod ofuncertain affinities from theLate CretaceousHuincul Formation of ArgentinianPatagonia. The genus contains asingle species,O. chimentoi, known from several bones of thehands,feet, andhips alongside somevertebrae.

Discovery and naming

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Overoraptor is located in Argentina
Overoraptor

The fossil specimens ofOveroraptor were unearthed by Dr. Roberto Nicolás Chimento in the Violante Farm locality, which is southeast of the Ezequiel Ramos-Mexía lake, in the northwestern portion ofRio Negro Province, Argentina. This outcrop is part of theHuincul Formation, which is dated to theCenomanian-Turonian boundary in theCretaceous period. Thisformation has yielded some of the largestSouth American dinosaurs including the massivesauropodArgentinosaurus and thetheropodMapusaurus.[1]

The precise date of the discovery of the type series ofOveroraptor is not publicly known, but the specimens were reposited in the collections of theCarlos Ameghino Provincial Museum inCipolletti, which is near the outcrop of the Huincul Formation where the specimens were discovered. The fossils weredescribed as a new genus and species of paravian theropod in May 2020 by Matías Motta, Federico Agnolín, Federico Brissón Egli, andFernando Novas in the journalThe Science of Nature (orNaturwissenschaften).[1]

Theholotype specimen, MACN-Pv 805, was disarticulated when it was found and it is relatively fragmentary. It consists of twophalanges and ametacarpal of the right hand, twohemal arches, the rightscapula, the rightulna, a partialilium, a partialpubis, twometatarsals from each foot, and several phalanges andunguals from the left foot.[1]

Theparatype specimen, MPCA-Pv 818, was discovered at the same locality in association with the holotype. It is about 20% smaller than the holotype, which led the researchers describing it to conclude that they were likely not from a fully-grown animal. The paratype consists of two phalanges from the right hand, a fragment of the ilium, the right pubis, one of the right metatarsals, and one pedal phalanx from each foot.[1]

The generic name,Overoraptor, comes from theSpanish word "overo", meaning "piebald"—referencing the coloration of the fossils—and theLatin word "raptor", meaning "thief". Thespecific epithet, "chimentoi", was given in honor of Roberto Nicolás Chimento, who initially discovered its remains.[1]

Description

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In their 2020 description of the genus, Motta and colleagues estimated thatOveroraptor would have been about 1.3 metres (4.3 ft) in length, although they do not provide an estimate of the animal's mass.[1]Gregory S. Paul estimated the size ofOveroraptor to be about 3 metres (9.8 ft) long and weighing about 30 kilograms (66 lb).[2]

Motta and colleagues diagnosedOveroraptor as being distinct from all otherparavians from the following unique autapomorphies: a medial deflection at the distal end of thescapula, a reduced and ridge-likeacromial process, an extensive crest onmetacarpal I, a crest ending in a distal posterior tubicle onmetatarsal II, and ametatarsal III that is taller than it is wide at the midpoint along its length. Motta and colleagues further diagnosed the genus by the co-occurrence of the following autapomorphies: lateral ridges on thecaudalcentra, a robustulna, a saddle-shapedradial cotyle on the ulna, a non-hinged joint at the distal end of metatarsal III, and dorsally displaced pits on thesecond toe. In the description of itsosteology, Motta and colleagues considered both the holotype and paratype together, rather than describing each specimen individually.[1]

Thescapular anatomy ofOveroraptor resembles that of stem-avialans in the presence of a cup-shapedglenoidfossa, but it differs from most otherparavians in that the acromial process projects dorsally rather than medially. The overall morphology of the scapula resembles the enigmatic paravian taxonRahonavis because the scapular blade projects medially outward at its distal-most end. The ratio of the lengths of theulna to themetacarpals is similar to the ratio found indromaeosaurs and less than that of more derived avialans. The ulna itself is also curved, which is theplesiomorphic condition in paravians, unlike the straight ulnae ofAnchiornis and related taxa. However, the ulna ofOveroraptor resembles the derived avialan condition in the presence of a saddle-shaped cotyle on the ulnar-radial articular surface.[1]

The metacarpal bones ofOveroraptor were noted by Motta and colleagues to be unusual in shape, namely that it is proportionally much wider and shorter than those known from other non-avialan paravians and there is a distinctly asymmetrical ginglymoidal surface which articulates with the lateralcondyle. The manualphalanges are slender and elongate, which is common in the paravian taxa that retain their fingers. Similarly, the manualunguals are mediolaterally compressed, sharp, and curved, similar to the condition seen in dromaeosaurs.[1]

The foot bones ofOveroraptor are sub-arctometatarsalian, meaning the middle metatarsal narrows at the medial end but it is not completely pinched together by the other two bones of the ankle. The foot also bears the archetypal raptorial second digit (the characteristic toe claw of dromaeosaurs), which is short in length and proportionally robust relative to other taxa with this claw.[1]

Classification

[edit]

In order to evaluate thephylogenetic position ofOveroraptor withinparaves, Motta and colleagues employed the data sets used by Agnolin and Novas (2013), Brusatte and colleagues (2014), Gianechini and colleagues (2017), and Hu and colleagues (2018) and added the scored characters of the new taxon. They also modified these data sets to include data found in more recently published research for some taxa.[1]

Their analyses recoveredOveroraptor in a variety of positions including as a basalmaniraptoran, a basalpennaraptoran, and a basal paravian, but they found the tree with the highest support values in their analysis recoveredOveroraptor as the sister taxon ofRahonavis in a clade that is the sister-taxon ofavialae and to whichunenlagiidae is basal. TheOveroraptor-Rahonavis clade was recovered with the followingsynapomorphies: a complex set of ridges on the lateral surfaces of the caudalcentra and a medial deflection of the distal end of thescapular blade. Even considering the similarities between the two taxa, Motta and colleagues also remark that the recovery of this clade may be the result of the unique mix of plesiomorphic and derived characters present inOveroraptor. The recovery of this clade is also suggested to be an early indicator of a much more diverse community of paravians acrossGondwana that have yet to be fully uncovered.[1]

A number of unorthodox results were obtained from the analysis of Motta and colleagues. They recoveredmicroraptorians andunenlagiines as being outside ofdromaeosauridae as successive stem clades to avialae. They similarly foundtroodontids as being the sister group of all other paravians rather than being either the sister group of dromaeosaurs or avialans,[1] which have been the results obtained by other recent analyses.[3][4][5][6][7] An abbreviated version of the strict consensus tree from their analysis using the data set from Agnolin and Novas (2013) is shown below.[1]

Paraves

In 2021, Andrea Cau and Daniel Madzia published their redescription of thetroodontidBorogovia, which contained a phylogenetic analysis using a wide variety ofcoelurosaur taxa. They used several different interpretive frameworks including the coding ofRahonavis as anunenlagiine,Balaur as avelociraptorine, andhalszkaraptorines as being basal to thetroodontid-dromaeosaurid split as well as an unweighted analysis without these constraints. The poorly-understood taxonFukuivenator was also coded as a paravian,[8] although recent studies have resolved that it is probably a basaltherizinosaur[9] or some other non-paravianmaniraptoran.[4] The most strongly-supported result of their analysis was one in which troodontidae was the sister taxon of avialae, which includesOveroraptor,Rahonavis,Balaur, and several other taxa. An abbreviated version of the tree recovered by their parsimony analysis can be seen below.[8]

Paraves

Paleoecology

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Paleoenvironment

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Huinculsaurus was discovered in the Argentine Province ofNeuquén. It was originally reported from the Huincul Group of the Río Limay Formation,[10] which have since become known as theHuincul Formation and theRío Limay Subgroup, the latter of which is a subdivision of theNeuquén Group. Thisunit is located in theNeuquén Basin inPatagonia. The Huincul Formation is composed of yellowish and greenishsandstones of fine-to-medium grain, some of which aretuffaceous.[11] These deposits were laid down during the Upper Cretaceous, either in the middleCenomanian to earlyTuronian stages[12] or the early Turonian to lateSantonian.[13] The deposits represent thedrainage system of abraided river.[14]

The Huincul Formation is thought to represent an arid environment with ephemeral or seasonalstreams.[15] In some areas, it is up to 250 metres (820 ft) thick. It is mainly composed of green and yellowsandstones and can easily be differentiated from the overlying Lisandro Formation, which is red in color. TheCandeleros Formation, underlying the Huincul, is composed of darker sediments, making all three formations easily distinguishable.[16][17]

Fossilised pollen indicates a wide variety of plants were present in the Huincul Formation. A study of the El Zampal section of the formation foundhornworts,liverworts,ferns,conifers, and someangiosperms (flowering plants).[18]

Contemporary fauna

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Size comparison of some of the fauna of the Huincul Formation, withOveroraptor shown in red

TheHuincul Formation is among the richest Patagonian vertebrate associations, preserving fish includinglungfish andgar,chelid turtles,squamates,sphenodonts,neosuchiancrocodilians, and a wide variety of dinosaurs.[12][19] Vertebrates are most commonly found in the lower, and therefore older, part of the formation.[20]

The Violante Farm locality is one of the most productive in the Huincul Formation, having yielded specimens of a wide variety of non-aviandinosaur species. Among these were theabelisaurTralkasaurus, themegaraptoranAoniraptor, thecarcharodontosaurTaurovenator, and the enigmatic taxonGualicho in addition to a variety of remains from indeterminate abelisaurs andcoelurosaurs. Specimens of thetitanosaurChoconsaurus were also discovered at this locality and represent the largest animal confidently known to have coexisted at this locality.[21]

Many other non-avian dinosaurs are known from the Huincul Formation, although it is not known with confidence if all of them coexisted withOveroraptor.[22]Sauropods are represented by the giant titanosaursBustingorrytitan,Chucarosaurus, andArgentinosaurus as well as therebbachisauridsCathartesaura,Limaysaurus, andSidersaura.[23][24] Theropods are also diverse and include the abelisaursIlokelesia andSkorpiovenator, thenoasauridHuinculsaurus, the carcharodontosauridsMapusaurus andMeraxes.[25]

See also

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References

[edit]
  1. ^abcdefghijklmnMatías J. Motta; Federico L. Agnolín; Federico Brissón Egli; Fernando E. Novas (2020). "New theropod dinosaur from the Upper Cretaceous of Patagonia sheds light on the paravian radiation in Gondwana".The Science of Nature.107 (3) 24.Bibcode:2020SciNa.107...24M.doi:10.1007/s00114-020-01682-1.hdl:11336/135530.PMID 32468191.S2CID 218913199.
  2. ^Paul, Gregory S. (2024).The Princeton Field Guide to Dinosaurs (Third ed.). Princeton, New Jersey: Princeton University Press.ISBN 978-0691231570.
  3. ^Napoli, J. G.; Ruebenstahl, A. A.; Bhullar, B.-A. S.; Turner, A. H.; Norell, M. A. (2021)."A New Dromaeosaurid (Dinosauria: Coelurosauria) from Khulsan, Central Mongolia"(PDF).American Museum Novitates (3982):1–47.doi:10.1206/3982.1.hdl:2246/7286.ISSN 0003-0082.S2CID 243849373.
  4. ^abWang, Xuri; Cau, Andrea; Wang, Zhengdong; Yu, Kaifeng; Wu, Wenhao; Wang, Yang; Liu, Yichuan (2023-06-05)."A new theropod dinosaur from the Lower Cretaceous Longjiang Formation of Inner Mongolia (China)".Cretaceous Research.151 105605.Bibcode:2023CrRes.15105605W.doi:10.1016/j.cretres.2023.105605.ISSN 0195-6671.
  5. ^Wang, Xuri; Cau, Andrea; Guo, Bin; Ma, Feimin; Qing, Gele; Liu, Yichuan (2022-11-19)."Intestinal preservation in a birdlike dinosaur supports conservatism in digestive canal evolution among theropods".Scientific Reports.12 (1): 19965.Bibcode:2022NatSR..1219965W.doi:10.1038/s41598-022-24602-x.ISSN 2045-2322.PMC 9675785.PMID 36402874.
  6. ^Pei, R.; Qin, Yuying; Wen, Aishu; Zhao, Q.; Wang, Z.; Liu, Z.; Guo, W.; Liu, P.; Ye, W.; Wang, L.; Yin, Z.; Dai, R.; Xu, X. (2022). "A New Troodontid from the Upper Cretaceous Gobi Basin of Inner Mongolia, China".Cretaceous Research.130 105052.Bibcode:2022CrRes.13005052P.doi:10.1016/j.cretres.2021.105052.
  7. ^Turner, Alan H.; Montanari, Shaena; Norell, Mark A. (2021)."A New Dromaeosaurid from the Late Cretaceous Khulsan Locality of Mongolia"(PDF).American Museum Novitates (3965):1–48.doi:10.1206/3965.1.ISSN 0003-0082.S2CID 231597229.
  8. ^abCau A, Madzia D (2021)."The phylogenetic affinities and morphological peculiarities of the bird-like dinosaurBorogovia gracilicrus from the Upper Cretaceous of Mongolia".PeerJ.9 e12640.doi:10.7717/peerj.12640.PMC 8656384.PMID 34963824.
  9. ^Hattori, S.; Kawabe, S.; Imai, T.; Shibata, M.; Miyata, K.; Xu, X.; Azuma, Y. (2021)."Osteology ofFukuiraptor paradoxus: A bizarre maniraptoran theropod from the Early Cretaceous of Fukui, Japan"(PDF).Memoir of the Fukui Prefectural Dinosaur Museum.20:1–82.
  10. ^Bonaparte, J.; Coria, R. (1993). "Un nuevo y gigantesco sauropodo titanosaurio de la Formacion Rio Limay (Albiano-Cenomaniano) de la Provincia del Neuquen, Argentina".Ameghiniana (in Spanish).30 (3):271–282.
  11. ^Leanza, H.A; Apesteguı́a, S.; Novas, F.E; de la Fuente, M.S. (February 1, 2004). "Cretaceous terrestrial beds from the Neuquén Basin (Argentina) and their tetrapod assemblages".Cretaceous Research.25 (1):61–87.Bibcode:2004CrRes..25...61L.doi:10.1016/j.cretres.2003.10.005.ISSN 0195-6671.
  12. ^abMotta, M.J.; Aranciaga Rolando, A.M.; Rozadilla, S.; Agnolín, F.E.; Chimento, N.R.; Egli, F.B.; Novas, F.E. (2016)."New theropod fauna from the upper cretaceous (Huincul Formation) of Northwestern Patagonia, Argentina".New Mexico Museum of Natural History and Science Bulletin.71:231–253.
  13. ^Corbella, H.; Novas, F.E.; Apesteguía, S.; Leanza, H. (2004)."First fission-track age for the dinosaur-bearing Neuquén Group (Upper Cretaceous), Neuquén Basin, Argentina".Revista del Museo Argentino de Ciencias Naturales. Nueva Serie.6 (21): 227=232.doi:10.22179/REVMACN.6.84.
  14. ^Rainoldi, A.L.; Franchini, Marta; Beaufort, D.; Mozley, P.; Giusiano, A.; Nora, C.; Patrier, P.; Impiccini, A.; Pons, J. (2015)."Mineral reactions associated with hydrocarbon paleomigration in the Huincul High, Neuquén Basin, Argentina".GSA Bulletin.127 (11–12):1711–1729.Bibcode:2015GSAB..127.1711R.doi:10.1130/B31201.1.hdl:11336/36686.
  15. ^Coria, R.A.; Currie, P.J. (2006)."A new carcharodontosaurid (Dinosauria, Theropoda) from the Upper Cretaceous of Argentina".Geodiversitas.28:71–118. Retrieved2019-02-16.
  16. ^Sánchez, María Lidia; Heredia, Susana; Calvo, Jorge O. (2006)."Paleoambientes sedimentarios del Cretácico Superior de la Formación Plottier (Grupo Neuquén), Departamento Confluencia, Neuquén" [Sedimentary paleoenvironments in the Upper Cretaceous Plottier Formation (Neuquen Group), Confluencia, Neuquén)].Revista de la Asociación Geológica Argentina.61:3–18. Retrieved2019-02-16.
  17. ^Leanza, H.A.; Apesteguia, S.;Novas, F.E.; De la Fuente, M.S. (2004)."Cretaceous terrestrial beds from the Neuquén Basin (Argentina) and their tetrapod assemblages".Cretaceous Research.25 (1):61–87.Bibcode:2004CrRes..25...61L.doi:10.1016/j.cretres.2003.10.005. Retrieved2019-02-16.
  18. ^Vallati, P. (2001)."Middle cretaceous microflora from the Huincul Formation ("Dinosaurian Beds") in the Neuquén Basin, Patagonia, Argentina".Palynology.25 (1):179–197.Bibcode:2001Paly...25..179V.doi:10.2113/0250179.
  19. ^Motta, M.J.; Brissón Egli, F.; Aranciaga Rolando, A.M.; Rozadilla, S.; Gentil, A. R.; Lio, G.; Cerroni, M.; Garcia Marsà, J.; Agnolín, F. L.; D'Angelo, J. S.; Álvarez-Herrera, G. P.; Alsina, C.H.; Novas, F.E. (2019)."New vertebrate remains from the Huincul Formation (Cenomanian–Turonian;Upper Cretaceous) in Río Negro, Argentina".Publicación Electrónica de la Asociación Paleontológica Argentina.19 (1): R26.doi:10.5710/PEAPA.15.04.2019.295.hdl:11336/161858.S2CID 127726069.Archived from the original on December 14, 2019. RetrievedDecember 14, 2019.
  20. ^Bellardini, F.; Filippi, L.S. (2018). "New evidence of saurischian dinosaurs from the upper member of the Huincul Formation (Cenomanian) of Neuquén Province, Patagonia, Argentina".Reunión de Comunicaciones de la Asociación Paleontológica Argentina: 10.
  21. ^Carrano, Matthew (2016)."Violante farm (Cretaceous of Argentina) Also known as Violante's farm, Pueblo Blanco Natural Reserve".The Paleobiology Database.
  22. ^Calvo, Jorge Orlando; Valieri, Ruben D. Juarez; Ríos, Sergio D. (2011). "Sauropods crossing formations: Biostratigraphical implications for Patagonian Faunal Assemblages". In Calvo, Jorge O.; Riga, Bernardo Gonzalez; Porfiri, Juan; Dos Santos, Domenica (eds.).Paleontología y Dinosaurios desde América Latina [Paleontology and Dinosaurs from Latin America]. EDIUNC, Universidad Nacional de Cuyo. p. 153-160.
  23. ^Salgado, Leonardo (2023)."A new gigantic titanosaur (Dinosauria, Sauropoda) from the early Late Cretaceous of Patagonia (Neuquén Province, Argentina)".Acta Palaeontologica Polonica.68.doi:10.4202/app.01086.2023.
  24. ^Lerzo, Lucas Nicolás; Gallina, Pablo Ariel; Canale, Juan Ignacio; Otero, Alejandro; Carballido, José Luis; Apesteguía, Sebastián; Makovicky, Peter Juraj (2024-01-03). "The last of the oldies: a basal rebbachisaurid (Sauropoda, Diplodocoidea) from the early Late Cretaceous (Cenomanian–Turonian) of Patagonia, Argentina".Historical Biology.37 (2):208–233.doi:10.1080/08912963.2023.2297914.ISSN 0891-2963.
  25. ^Canale, Juan I.; Apesteguía, Sebastián; Gallina, Pablo A.; Mitchell, Jonathan; Smith, Nathan D.; Cullen, Thomas M.; Shinya, Akiko; Haluza, Alejandro; Gianechini, Federico A.; Makovicky, Peter J. (July 2022)."New giant carnivorous dinosaur reveals convergent evolutionary trends in theropod arm reduction".Current Biology.32 (14): 3195–3202.e5.doi:10.1016/j.cub.2022.05.057.PMID 35803271.S2CID 250343124.
Avemetatarsalia
Theropoda
Maniraptora
    • see below↓
Alvarezsauridae
Parvicursorinae
Ceratonykini
Mononykini
Therizinosauria
Therizinosauroidea
Therizinosauridae
Pennaraptora
Oviraptorosauria
Paraves
    • see below↓
Patagonykus puertai

Mononykus olecranus

Therizinosaurus cheloniformis
Scansoriopterygidae?
Anchiornithidae
Archaeopterygidae
Dromaeosauridae
Troodontidae
Jeholornithiformes
Omnivoropterygidae?
Confuciusornithidae
Jinguofortisidae
Ornithothoraces
Enantiornithes
Euornithes
    • see below↓
Ambopteryx longibrachium

Archaeopteryx lithographica

Confuciusornis sp.
Schizoouridae
Patagopterygiformes
Ambiortiformes
Hongshanornithidae
Songlingornithidae
Yanornithidae
Gansuidae?
Ichthyornithes
Hesperornithes
Hesperornithidae
Cimolopterygidae
Aves / Neornithes
    • see below↓
Patagopteryx deferrariisiIchthyornis dispar
Palaeognathae
Neognathae
Galloanserae
Anserimorphae
Pangalliformes
Incertae sedis
Dromornithidae
Gastornithiformes
Pelagornithidae
Asteriornis maastrichtensisDromornis stirtoni
Overoraptor chimentoi
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