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Quebrada del Barro Formation

Coordinates:31°54′S67°12′W / 31.9°S 67.2°W /-31.9; -67.2
From Wikipedia, the free encyclopedia
Quebrada del Barro Formation
Stratigraphic range:Norian
TypeGeological formation
Unit ofMarayes Group
UnderliesLos Riscos Formation
OverliesCarrizal Formation
Lithology
PrimarySandstone
OtherSiltstone
Location
Coordinates31°54′S67°12′W / 31.9°S 67.2°W /-31.9; -67.2
Approximate paleocoordinates40°48′S30°00′W / 40.8°S 30.0°W /-40.8; -30.0
RegionSan Juan Province
Country Argentina
ExtentMarayes-El Carrizal Basin
Quebrada del Barro Formation is located in Argentina
Quebrada del Barro Formation
Quebrada del Barro Formation (Argentina)

TheQuebrada del Barro Formation is a geologicalformation of theMarayes-El Carrizal Basin inSan Juan Province,Argentina. This formation is the most fossiliferous portion of the TriassicMarayes Group, and is also the youngest unit of the group, overlying theEl Carrizal Formation. Anunconformity at the top of the Quebrada del Barro Formation separates it from theCretaceous-ageLos Riscos Formation of theEl Gigante Group.[1][2][3][4] Part of the formation may be made into a provincial park following the discovery of the fossils ofIngentia, a giant sauropodomorph dinosaur which helped elucidate the early evolution ofsauropods.[5]

Sedimentology

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The Quebrada del Barro Formation formed within arift basin during a period of renewed fracturing. It encompasses 600 to 1,400 metres (2,000 to 4,600 ft) of redsandstones, fineconglomerates, anddiamictites.[3] Early hypotheses on the depositional environment proposed that the sediments formed in analluvial fan orbraided river system, while a newer proposal outlines how four differentfacies within the formation can be used to reconstruct a meanderingsemiarid floodplain deposited bymudflows and discharging inheterolithicterminal splays.[6]

Fossil content

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The fauna of Quebrada del Barro is similar to that of the neighboringLos Colorados Formation which is considered to be from theNorian stage of the Late Triassic.[7] Both formations preserve fossils from groups such assauropodomorphdinosaurs,cynodonts, andtestudinatans. However, Quebrada del Barro is more abundant insphenodontians (Sphenotitan),tritheledontid cynodonts, andcoelophysoid dinosaurs (Lucianovenator), while sauropodomorphs are somewhat less common andaetosaurs are completely absent, in contrast to the Los Colorados Formation.[3] Sphenodontians and cynodonts are also abundant in microfossil assemblages.[6] In addition, the Quebrada del Barro Formation preserves some of the onlypterosaur andDromomeron specimens known from Triassic strata in Argentina. Although the sphenodontian and cynodont-dominated fauna of Quebrada del Barro is akin to that of the Faxinal del Sotorno assemblage of theBrazilianCaturrita Formation, the fauna of the Faxinal del Sotorno assemblage is otherwise indicative of an older part of the Triassic than the Quebrada del Barro Formation.[3]

Dinosaurs

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Theropods of the Quebrada del Barro Formation
GenusSpeciesMaterialNotesImages
Lucianovenator[8]L. bonoiSeveral specimens including vertebrae, hip fragments, and a partial tibiaAcoelophysidtheropod
Sauropodomorphs of the Quebrada del Barro Formation
TaxonSpeciesMaterialNotesImages

Ingentia[9]

I. prima

"cervical and dorsal vertebrae, scapula"

Alessemsauridsauropod

Leyesaurus[2]L. marayensisAmassospondylidsauropodomorph. Known from uppermost layers which may belong to a different unit ofHettangian (Early Jurassic) age.[3]
Sauropodomorphasp.Complete foot and tail vertebraeUndiagnostic sauropodomorph remains originally referred toRiojasaurus[2][10]

Otheravemetatarsalians

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Non-dinosauravemetatarsalias of the Quebrada del Barro Formation
TaxonSpeciesMaterialNotesImages
Dromomeron[11]D. gigasA partial femuralagerpetid
PachagnathusP. benitoiSnout fragmentAraeticodactylidpterosaur[12]
Pterosauriasp.Partial ulnaan indeterminatepterosaur[3]
YelaphomteY. praderioiSnout fragmentAraeticodactylidpterosaur[12]

Pseudosuchians

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Pseudosuchias of the Quebrada del Barro Formation
TaxonSpeciesMaterialNotesImages
"Rauisuchidae"sp.Skull fragments, osteodermsan indeterminate "rauisuchid" smaller thanFasolasuchus[3]
Crocodylomorphasp.A specimen including a partial osteoderm and vertebrae fragmentsIndeterminate, possibly a "sphenosuchid"[3]
Crocodylomorphasp.Two incomplete specimens including osteoderms, vertebrae, and other bonesaprotosuchid, possibly synonymous withHemiprotosuchus[3]

Rhynchocephalians

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Rhynchocephalians of the Quebrada del Barro Formation
GenusSpeciesMaterialNotesImages
Sphenotitan[13]S. leyesinumerous specimens (~50% of all recovered fossils)[3]aneilenodontinesphenodontian

Other reptiles

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Other reptiles of the Quebrada del Barro Formation
TaxonSpeciesMaterialNotesImages
Archosauriformessp.Maxilla, caudal vertebra, metatarsal, indeterminate limb bone (tibia?)Various indeterminate fragments likely belonging topseudosuchians ordinosauromorphs[4]
WaluchelysW. cavitesta2 partial skeletons and carapacesanaustralochelyidstem-turtle[14][3]

Synapsids

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Synapsids of the Quebrada del Barro Formation
TaxonSpeciesMaterialNotesImages
Tritheledontidaesp.36 specimens, including a partial skeletonan undescribedtritheledontidcynodont. May be two taxa based on two morphotypes: "long-snout" and "short-snout".[3]

References

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  1. ^Gardini et al., 2009, p.554
  2. ^abcCecilia Apaldetti; Ricardo N. Martinez; Oscar A. Alcober; Diego Pol (2011). Claessens, Leon (ed.)."A New Basal Sauropodomorph (Dinosauria: Saurischia) from Quebrada del Barro Formation (Marayes-El Carrizal Basin), Northwestern Argentina".PLOS ONE.6 (11): e26964.Bibcode:2011PLoSO...626964A.doi:10.1371/journal.pone.0026964.PMC 3212523.PMID 22096511.
  3. ^abcdefghijklMartínez, Ricardo N.; Apaldetti, Cecilia; Correa, Gustavo; Colombi, Carina E.; Fernández, Eliana; Malnis, Paula Santi; Praderio, Angel; Abelín, Diego; Benegas, Laura G.; Aguilar-Cameo, Andrea; Alcober, Oscar A. (August 2015)."A New Late Triassic Vertebrate Assemblage from Northwestern Argentina".Ameghiniana.52 (4):379–390.doi:10.5710/AMGH.27.04.2015.2889.hdl:11336/111650.ISSN 0002-7014.S2CID 131662341.
  4. ^abGianechini, Federico A.; Codorniú, Laura; Arcucci, Andrea B.; Castillo Elías, Gabriela; Rivarola, David (March 2016)."Archosauriform remains from the Late Triassic of San Luis province, Argentina, Quebrada del Barro Formation, Marayes–El Carrizal Basin".Journal of South American Earth Sciences.66:110–124.Bibcode:2016JSAES..66..110G.doi:10.1016/j.jsames.2015.12.012.hdl:11336/60591.ISSN 0895-9811.
  5. ^"Uac wants a provincial park in the cradle of Ingenia Prima".Naaju. Retrieved2018-07-15.
  6. ^abColombi, Carina E.; Martínez, Ricardo N.; Correa, Gustavo; Fernández, Eliana; Malnis, Paula Santi; Praderio, Angel; Apaldetti, Cecilia; Abelín, Diego; Alcober, Oscar; Aguilar-Cameo, Andrea (October 2015)."First Argentine Microfossil Bonebed from the Upper Triassic Marayes—El Carrizal Basin, San Juan Province".PALAIOS.30 (10):743–757.Bibcode:2015Palai..30..743C.doi:10.2110/palo.2014.055.hdl:11336/4899.ISSN 0883-1351.S2CID 131239254.
  7. ^Weishampel, David B; et al. (2004). "Dinosaur distribution (Late Triassic, South America)." In: Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. Pp. 527–528.ISBN 0-520-24209-2.
  8. ^Ricardo N. Martínez; Cecilia Apaldetti (2017). "A late Norian-Rhaetian coelophysid neotheropod (Dinosauria, Saurischia) from the Quebrada del Barro Formation, northwestern Argentina". Ameghiniana. in press.doi:10.5710/AMGH.09.04.2017.3065.
  9. ^Apaldetti; Martínez, Ricardo N.; Cerda, Ignatio A.; Pol, Diego; Alcober, Oscar (2018). "An early trend towards gigantism in Triassic sauropodomorph dinosaurs".Nature Ecology & Evolution.2 (8):1227–1232.Bibcode:2018NatEE...2.1227A.doi:10.1038/s41559-018-0599-y.hdl:11336/89332.PMID 29988169.S2CID 49669597.
  10. ^"Riojasaurus." In: Dodson, Peter & Britt, Brooks & Carpenter, Kenneth & Forster, Catherine A. & Gillette, David D. & Norell, Mark A. & Olshevsky, George & Parrish, J. Michael & Weishampel, David B.The Age of Dinosaurs. Publications International, LTD. p. 41.ISBN 0-7853-0443-6.
  11. ^Ricardo N. Martínez; Cecilia Apaldetti; Gustavo A. Correa; Diego Abelín (2016). "A Norian lagerpetid dinosauromorph from the Quebrada del Barro Formation, northwestern Argentina".Ameghiniana.53 (1):1–13.doi:10.5710/AMGH.21.06.2015.2894.S2CID 131613066.
  12. ^abMartínez, Ricardo N.; Andres, Brian; Apaldetti, Cecilia; Cerda, Ignacio A. (March 2022)."The dawn of the flying reptiles: first Triassic record in the southern hemisphere".Papers in Palaeontology.8 (2).Bibcode:2022PPal....8E1424M.doi:10.1002/spp2.1424.ISSN 2056-2799.S2CID 247494547.
  13. ^Martinez, R. N.; Apaldetti, C.; Colombi, C. E.; Praderio, A.; Fernandez, E.; Malnis, P. S.; Correa, G. A.; Abelin, D.; Alcober, O. (2013)."A new sphenodontian (Lepidosauria: Rhynchocephalia) from the Late Triassic of Argentina and the early origin of the herbivore opisthodontians".Proceedings of the Royal Society B: Biological Sciences.280 (1772): 20132057.doi:10.1098/rspb.2013.2057.PMC 3813332.PMID 24132307.
  14. ^Sterli, Juliana; Martínez, Ricardo N.; Cerda, Ignacio A.; Apaldetti, Cecilia (2021)."Appearances can be deceptive: bizarre shell microanatomy and histology in a new Triassic turtle (Testudinata) from Argentina at the dawn of turtles".Papers in Palaeontology.7 (2):1097–1132.Bibcode:2021PPal....7.1097S.doi:10.1002/spp2.1334.ISSN 2056-2802.S2CID 225515560.

Bibliography

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