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Rahiolisaurus

From Wikipedia, the free encyclopedia
Genus of abelisaurid dinosaur from the Late Cretaceous period

Rahiolisaurus
Temporal range:
Late Cretaceous,70–66 Ma
Life restoration ofRahiolisaurus gujaratensis
Scientific classificationEdit this classification
Kingdom:Animalia
Phylum:Chordata
Class:Reptilia
Clade:Dinosauria
Clade:Saurischia
Clade:Theropoda
Family:Abelisauridae
Subfamily:Carnotaurinae
Genus:Rahiolisaurus
Novaset al.,2010
Species:
R. gujaratensis
Binomial name
Rahiolisaurus gujaratensis

Rahiolisaurus is agenus ofabelisauridtheropoddinosaur which existed inIndia during theLate Cretaceous period. It was described in2010, based on fossils recovered from theLameta Formation in the Indian state ofGujarat. These fossils include elements from at least seven different individuals and are believed to have been from theMaastrichtian stage, sometime between 70 and 66 million years ago, making it one of the last non-avian dinosaurs known in the fossil record. Despite representing a variety of different growth stages, all recovered fossils from the locality indicate a single species, thetype speciesRahiolisaurus gujaratensis.

Discovery and naming

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Rahiolisaurus is located in India
Rahiolisaurus
Rahiolisaurustype locality in Kakda Kho, Rahioli village,Gujarat, India

During two expeditions, one in 1995 and the other in 1997, numerous remains of abelisaurids were recovered from a single quarry 50 square metres in area. The collected remains included cervical, dorsal, sacral, and caudal vertebrae, portions of pectoral and pelvic girdles, and several hind limb bones. Because of the unearthing of seven differently sized right tibiae, it was suggested that the assemblage was formed by at least seven individuals of different ontogenetic stages. Within the collection were several duplicate bones, such as the ilia, pubes, femora and tibiae, that exhibited similar morphological features of typical abelisauroid traits. However, despite these remains being of different size gradation and representing growth series, hardly any taxonomic variation was discovered. It was interpreted by Novas et al. that the entire theropod collection from this quarry may be referred to the single speciesRahiolisaurus.[1]

The landscape of the Indian state ofGujarat, in which the remains ofRahiolisaurus were found

Individual bones of the newly discovered abelisaurid was given separate catalogue numbers. Theholotype ofRahiolisaurus is represented by a partial association of pelvic elements and a femur that were found in the field. It consists of a right ilium (ISIR 550), a right pubis (ISIR 554), and a right femur (ISIR 557). In addition, an axis (ISIR 658) was found in articulation with cervicals 3 (ISIR 659) and 4 (ISIR 660) and are attributed to the species. These bones are currently housed at the collection of the Geology Museum,Indian Statistical Institute, Kolkata.[1]

Rahiolisaurus was named after the village of Rahioli, located near the fossil site where the dinosaurs remains were discovered. The specific name,gujaratensis, means "fromGujarat" in Latin.[1]

Description

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Size ofRahiolisaurus gujaratensis compared to a human

Rahiolisaurus was initially described as a large-sized abelisaurid and around 8 metres (26 ft) long and weighing 2 metric tons (2.2 short tons),[1][2] but the allometry-based estimate for different specimens suggest a shorter body length of 6.22–6.75 metres (20.4–22.1 ft).[3] It shares many similarities with another Indian abelisaurid,Rajasaurus, but includes differences such as an overall more gracile and slender-limbed form.[1] Abelisaurids typically had four fingers, short arms, and, to compensate, a heavily constructed head which was the primary tool for hunting; however, the skull was short, they probably had modest jaw musculature, and the teeth were short.[2] Abelisaurids likely had a bite force similar toAllosaurus at around 3,500 newtons (790 lbf).[4]

Classification

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In 2014, the subfamilyMajungasaurinae was erected by palaeontologist Thierry Tortosa to separate the newly discovered EuropeanArcovenator,Majungasaurus,Indosaurus,Rahiolisaurus, andRajasaurus from South American abelisaurids based on physical characteristics such as elongatedantorbital fenestrae in front of the eye sockets, and a sagittal crest that widens into a triangular surface towards the front of the head. In more recent analyses Rahiolisaurus as appeared as being more closely related to the South American abelisaurids, further strengthening the faunal similarities between India and South America in themesozoic.

The following cladogram was recovered by Tortosa (2014):[5]

Ceratosauria

A phylogeny from 2018 recoveredRahiolisaurus as forming a clade with the Madagascan abelisauridDahalokely within majungasaurinae.[6] Only the phylogenies for Abelisauridae is depicted here.

Abelisauridae

In 2021,Rahiolisaurus andDahalokely were again recovered as sister taxa, however they were placed outside of majungasaurinae as basalbrachyrostrans.[7]

Abelisauridae

Palaeoecology

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India was an island in theLate Cretaceous

Rahiolisaurus has been found in theLameta Formation, a rock unitradiometrically dated to theMaastrichtianage of the latest Cretaceous representing anarid orsemi-arid landscape with a river flowing through it–probably providing shrub cover near the water–which formed between episodes of volcanism in theDeccan Traps.[8][9]Rahiolisaurus likely inhabited what is now the Narmada River Valley. The formation is known for being a sauropod nesting site, yielding several dinosaur eggs, and sauropod herds likely chose sandy soil for nesting;[10] though eggs belonging to large theropods have been found, it is unknown if they belong toRahiolisaurus.[11] Sauropodcoprolite remains indicate they lived in a forested landscape, consuming plants such asPodocarpus,Araucaria, andCheirolepidiaceaeconifers;cycads;palm trees; earlygrass; andCaryophyllaceae,Sapindaceae, andAcanthaceae flowering plants.[12]

Several dinosaurs have been described from theLameta Formation, such as thenoasauridLaevisuchus; abelisauridsIndosaurus,Indosuchus,Lametasaurus, andRajasaurus; and thetitanosaurian sauropodsJainosaurus,Titanosaurus, andIsisaurus. The diversity of abelisauroid and titanosaurian dinosaurs in Cretaceous India indicates they shared close affinities to the dinosaur life of the otherGondwanan continents, which had similar inhabitants.[13] Dinosaurs in India probably went extinct due to volcanic activity around 350,000 years before theCretaceous–Paleogene boundary. They likely avoided areas with volcanicfissure vents andlava flows.[14]

See also

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References

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  1. ^abcdeNovas, Fernando E., Chatterjee, Sankar, Rudra, Dhiraj K., Datta, P.M. (2010). "Rahiolisaurus gujaratensis, n. gen. n. sp., A New Abelisaurid Theropod from the Late Cretaceous of India" in: Saswati Bandyopadhyay (ed.):New Aspects of Mesozoic Biodiversity. Springer Berlin / Heidelberg. pp. 45–62.doi:10.1007/978-3-642-10311-7.ISBN 978-3-642-10310-0.
  2. ^abPaul, G. S. (2010).The Princeton Field Guide to Dinosaurs. Princeton University Press. pp. 84–86.ISBN 978-0-691-13720-9.
  3. ^Grillo, O. N.; Delcourt, R. (2016). "Allometry and body length of abelisauroid theropods:Pycnonemosaurus nevesi is the new king".Cretaceous Research.69:71–89.Bibcode:2017CrRes..69...71G.doi:10.1016/j.cretres.2016.09.001.
  4. ^Delcourt, R. (2018)."Ceratosaur Palaeobiology: New Insights on Evolution and Ecology of the Southern Rulers".Scientific Reports.8 (9730) 9730.Bibcode:2018NatSR...8.9730D.doi:10.1038/s41598-018-28154-x.PMC 6021374.PMID 29950661.
  5. ^Tortosa, T.; Buffetaut, E.; Vialle, N.; Dutour, Y.; Turini, E.; Cheylan, G. (2014). "A new abelisaurid dinosaur from the Late Cretaceous of southern France: Palaeobiogeographical implications".Annales de Paléontologie.100 (1):63–86.Bibcode:2014AnPal.100...63T.doi:10.1016/j.annpal.2013.10.003.
  6. ^Delcourt, Rafael (June 2018)."Ceratosaur palaeobiology: New insights on evolution and ecology of the southern rulers".Scientific Reports.8 (1) 9730.Bibcode:2018NatSR...8.9730D.doi:10.1038/s41598-018-28154-x.PMC 6021374.PMID 29950661.Archived from the original on 9 November 2022 – via ResearchGate.
  7. ^Gianechini, Federico A.; Méndez, Ariel H.; Filippi, Leonardo S.; Paulina-Carabajal, Ariana; Juárez-Valieri, Rubén D.; Garrido, Alberto C. (10 December 2020)."A new furileusaurian abelisaurid from La Invernada (Upper Cretaceous, Santonian, Bajo de la Carpa Formation), northern Patagonia, Argentina".Journal of Vertebrate Paleontology.40 (6) e1877151.Bibcode:2020JVPal..40E7151G.doi:10.1080/02724634.2020.1877151.ISSN 0272-4634.Archived from the original on 13 June 2024. Retrieved13 June 2024.
  8. ^Brookfield, M. E.; Sanhi, A. (1987). "Palaeoenvironments of the Lameta beds (late Cretaceous) at Jabalpur, Madhya Pradesh, India: Soils and biotas of a semi-arid alluvial plain".Cretaceous Research.8 (1):1–14.Bibcode:1987CrRes...8....1B.doi:10.1016/0195-6671(87)90008-5.
  9. ^Mohabey, D. M. (1996). "Depositional environment of Lameta Formation (late Cretaceous) of Nand-Dongargaon inland basin, Maharashtra: the fossil and lithological evidences".Memoirs of the Geological Survey of India.37:1–36.
  10. ^Tandon, S. K.; Sood, A.; Andrews, J. E.; Dennis, P. F. (1995)."Palaeoenvironments of the dinosaur-bearing Lameta Beds (Maastrichtian), Narmada Valley, Central India"(PDF).Palaeogeography, Palaeoclimatology, Palaeoecology.117 (3–4):153–184.Bibcode:1995PPP...117..153T.doi:10.1016/0031-0182(94)00128-U.
  11. ^Lovgren, S. (13 August 2003)."New Dinosaur Species Found in India".National Geographic News. Archived fromthe original on 11 December 2003. Retrieved8 April 2009.
  12. ^Sonkusare, H.; Samant, B.; Mohabey, D. M. (2017)."Microflora from Sauropod Coprolites and Associated Sedimentsof Late Cretaceous (Maastrichtian) Lameta Formation of Nand-Dongargaon Basin, Maharashtra".Geological Society of India.89 (4):391–397.Bibcode:2017JGSI...89..391S.doi:10.1007/s12594-017-0620-0.S2CID 135418472.
  13. ^Weishampel, D. B.; Barrett, P. M.; Coria, R.; Le Loeuff, J.; Xijin, Z.; Xing, X.; Sahni, A.; Gomani, E. M. P.; Noto, C. R. (2004). "Dinosaur Distribution". In Weishampel, D. B.; Dodson, P.; Osmólska, H. (eds.).The Dinosauria (2nd ed.). Berkeley: University of California Press. p. 595.ISBN 978-0-520-24209-8.
  14. ^Mohabey, D. M.; Samant, B. (2013)."Deccan continental flood basalt eruption terminated Indian dinosaurs before the Cretaceous–Paleogene boundary".Geological Society of India Special Publication (1):260–267.
Avemetatarsalia
Theropoda
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Coelophysoidea
Coelophysidae
Averostra
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Dubious neotheropods
Coelophysis bauri
Dilophosaurus wetherilli
Ceratosauridae
Abelisauroidea
Noasauridae
Elaphrosaurinae
Noasaurinae
Abelisauridae
Majungasaurinae
Carnotaurinae
Brachyrostra
Furileusauria
Tetanurae
    • see below↓
Ceratosaurus nasicornis
Limusaurus inextricabilis
Rajasaurus narmadensis
Aucasaurus garridoi
Piatnitzkysauridae
Megalosauridae
Megalosaurinae
Afrovenatorinae
Baryonychinae
Ceratosuchopsini
Spinosaurinae
Spinosaurini
Avetheropoda
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Piatnitzkysaurus floresi

Torvosaurus tanneri

Spinosaurus aegyptiacus
Metriacanthosauridae
Metriacanthosaurinae
Allosauridae
Carcharodontosauria
Neovenatoridae
Carcharodontosauridae
Carcharodontosaurinae
Giganotosaurini
Megaraptora?
Megaraptoridae
Coelurosauria
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Xuanhanosaurus qilixiaensis
Allosaurus fragilis

Neovenator saleriiCarcharodontosaurus saharicus

Australovenator wintonensis
Coeluridae?
Proceratosauridae
Albertosaurinae
Tyrannosaurinae
Alioramini
Daspletosaurini
Teratophoneini
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Maniraptoromorpha
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Dubious coelurosaurs
Zuolong salleei
Stokesosaurus clevelandi

Alioramus remotus

Tarbosaurus bataar
Compsognathidae
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Ornithomimosauria
Macrocheiriformes
Deinocheiridae
Ornithomimidae
Maniraptora
Sinosauropteryx prima

Deinocheirus mirificus

Qiupalong henanensis
Rahiolisaurus
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