Caturrita Formation
The Caturrita Formation is a rock formation found in Rio Grande do Sul, Brazil. Its sediments were deposited in the Paraná Basin. The formation is from the Upper Triassic and forms part of the Santa Maria Supersequence in the upper section of the Rosário do Sul Group.
| Caturrita Formation | |
|---|---|
| Stratigraphic range: Late Triassic ~ | |
Caturrita Formation. Source: UFSM | |
| Type | Geological formation |
| Unit of | Rosário do Sul Group |
| Underlies | Mata Sandstone |
| Overlies | Alemoa Member Santa Maria Formation |
| Area | 250 km (160 mi) |
| Thickness | 30–60 m (98–197 ft) |
| Lithology | |
| Primary | Sandstone, siltstone |
| Other | Mudstone, conglomerate |
| Location | |
| Coordinates | 29°41′42″S 53°47′43″W / 29.695042°S 53.795403°WCoordinates: 29°41′42″S 53°47′43″W / 29.695042°S 53.795403°W |
| Approximate paleocoordinates | 37°18′S 16°00′W / 37.3°S 16.0°W |
| Region | Paleorrota Rio Grande do Sul |
| Country | Brazil |
| Extent | Paraná Basin |
| Type section | |
| Named for | Caturrita, barrio of Santa Maria |
Geopark of Paleorrota | |
Etymology
The formation received this name, because Caturrita is a neighbourhood (barrio) of Santa Maria. [1][2] In Portuguese caturrita also refers to the monk parakeet.
Stratigraphy
The sediments of the Caturrita Formation belong to the second unit of the Santa Maria Supersequence and overlie the Alemoa Member of the Santa Maria Formation. The clayey sediments of the Alemoa Member gradually give way to the more sandy, rarely conglomeratic, Caturrita Formation, which finishes with an unconformity. After this erosional event follow the Rhaetian sediments of the Mata Sandstone, the third unit of the Santa Maria Supersequence.
The Caturrita Formation was once regarded as a member of the stratigraphically higher Botucatu Formation[3] or was expanded to include the Mata Sandstone.[4]
The Caturrita Formation reaches a maximum thickness of 60 meters, but generally oscillates around values of 30 meters.
Age
Until 2018 no absolute ages had been determined, but the formation was most commonly assigned to a late Carnian to early Norian age on paleontological grounds. However, Rhaetian or even Early Jurassic age of this unit was also advocated in the literature.[5] A U-Pb (Uranium decay) dating found that the Caturrita Formation dated around 225.42 million years ago, putting it less than 10 million years younger than the Santa Maria and Ischigualasto Formations, from where the earliest dinosaurs are known.[6]
Geographical occurrence
- 1) Serra Geral Formation, Cretaceous
- 2) Botucatu Formation, Cretaceous
- 3) Guará Formation, Jurassic
- 4) Santa Maria Formation & Caturrita Formation, Triassic
- 5) Sanga do Cabral Formation, Triassic
- 6) Piramboia Formation, Permian
- 7) Itararé Group, Permian
Outcrops of the Caturrita Formation are found in the Brazilian state of Rio Grande do Sul. From the town of Taquari they follow for 250 kilometers a thin band in the central part of the state in an east-westerly fashion right up to Mata.
Depositional environment
The sediments of the Caturrita Formation belong to the upper section of the Santa Maria Supersequence. In terms of sequence stratigraphy they are equivalent to a highstand systems tract. The scarlet, ephemeral, mainly clayey fluvio-lacustrine deposits of the Alemoa Member gradually cede to more sandy,[7] occasionally gravelly deposits of a braided river-system that was operational all-year-round. These deposits of the Caturrita Formation settled out in an alluvial flood-plain. The changeover in sedimentary facies was accompanied by a climatic change to more humid conditions.[8]
The sediments are of continental nature (red beds) and form massive sandstone and siltstone bodies.[9]
Vertebrate fauna
The Caturrita Formation contains a biozone for tetrapods, the so-called “Ictidosauria Assemblage Zone″ Ca-1.[10]Ictidosaurs are tritheledontid cynodonts, a sister group of the mammals. This is the reason, why this biozone recently has been renamed as “Mammaliamorpha Cenozone” to underline the importance of the cynodont fossils.[11] The Caturrita Formation also hosts the stratigraphic marker level “Jachaleria”[12] named after the dicynodont Jachaleria candelariensis. Dinosaurs and other vertebrates have been discovered as well.
In 1998 tracks of prosauropods have been found near Faxinal do Soturno that were most likely caused by Unaysaurus tolentinoi.[13]
The fossil finds are concentrated around three major areas: Santa Maria and northern surroundings (Água Negra) Faxinal do Soturno Candelária and surroundings (Linha São Luis)
The following taxa have been discovered so far in the Caturrita Formation:
Color key
| Notes Uncertain or tentative taxa are in small text; |
Synapsids
| Synapsids of the Caturrita Formation | ||||||
|---|---|---|---|---|---|---|
| Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
| Botucaraitherium[14] | B. belarminoi | Sesmaria do Pinhal | A mammaliamorph cynodont | |||
| Brasilitherium | B. riograndensis | Synonym of Brasilodon quadrangularis[15] | ||||
| Brasilodon[14] | B. quadrangularis | Linha São Luiz, Sesmaria do Pinhal | A mammaliamorph cynodont | |||
| Irajatherium[14] | I. hernandezi | Linha São Luiz, Sesmaria do Pinhal | A tritheledontid cynodont | |||
| Jachaleria[14] | J. candelariensis | Sesmaria do Pinhal | A stahleckeriid dicynodont | |||
| cf. Jachaleria[14] | cf. J. candelariensis | Alto Guarda Mor site | A stahleckeriid dicynodont | |||
| Minicynodon | M. maieri | Synonym of Brasilodon quadrangularis[15] | ||||
| Riograndia[14] | R. guaibensis | Linha São Luiz, Sesmaria do Pinhal | A tritheledontid cynodont | |||
| Traversodontidae indet.[14] | Indeterminate | Sesmaria do Pinhal, Sacisaurus site | ||||
Dinosaurs
Unnamed prosauropod genus present in Rio Grande do Sul, Brazil.[16]
| Dinosaurs of the Caturrita Formation | ||||||
|---|---|---|---|---|---|---|
| Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
| Indeterminate[5] | Two isolated footprints[5] | An ichnotaxon; footprints of large theropod dinosaurs.[5] | ||||
| G. candelariensis[16] | Linha São Luiz | "Partial postcranial skeleton and a fragmentary hindlimb."[17] | ||||
| Sauropodomorpha indet.[18] | Indeterminate | "An incomplete right ilium, uninformative vertebral remains and other indeterminate fragments, plus four isolated and incomplete bones including a possible pubis, an ischium, a possible tibia and a metatarsal IV."[18] | An indeterminate sauropodomorph of uncertain phylogenetic placement, probably "closer to Plateosauria (...) than to Saturnalia–like basal–most sauropodomorphs".[18] | |||
| Sauropodomorpha indet.[19] | Indeterminate | "Three incomplete dinosaur specimens, an isolated sacral vertebra, an articulated left pubis–ischium and an isolated right ischium."[19] | An indeterminate sauropodomorph of uncertain phylogenetic placement, "probably more primitive than typical ‘prosauropods’ from the Norian-Early Jurassic".[19] | |||
| U. tolentinoi | ||||||
Other tetrapods
Undetermined phytosaur genus.
| Misc tetrapods of the Caturrita Formation | ||||||
|---|---|---|---|---|---|---|
| Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
| C. enigmatica | Maehary skull material | |||||
| C. brasiliensis | ||||||
| F. minimus | ||||||
| Maehary | M. bonapartei | Rio Grande do Sul, Brazil | The earliest diverging member of Pterosauromorpha | |||
| S. caliodon | ||||||
| S. agudoensis | ||||||
| Stereospondyli indet.[20] | Indeterminate | An incomplete interclavicle[20] | An indeterminate stereospondyl temnospondyl.[20] | |||
| T. sulcognathus | "Two nearly complete skulls and a partial skull." | |||||
See also
References
- ^ Formação Santa Maria 2008-05-01 at the Wayback Machine, (in Portuguese)
- ^ Paleoformações[permanent dead link], (in Portuguese)
- ^ Bortoluzzi, C.A. 1974. Contribuição à Geologia da Região de Santa Maria, Rio Grande do Sul, Brasil. Pesquisas, 4 (1):7-86
- ^ Andreis, R.R.; Bossi, G.E. & Montardo, D.K. 1980. O Grupo Rosário do Sul (Triássico) no Rio grande do Sul. In: CONGRESSO BRASILEIRO DE GEOLOGIA,31, Balneário 16 Camboriú, 1980. Anais... Balneário de Camboriú, SBG, v. 2, p.659-673.
- ^ a b c d e f Rafael Costa da Silva; Ronaldo Barboni; Tânia Dutra; Michel Marques Godoy; Raquel Barros Binotto (2012). "Footprints of large theropod dinosaurs and implications on the age of Triassic biotas from Southern Brazil". Journal of South American Earth Sciences. 39: 16–23. Bibcode:2012JSAES..39...16D. doi:10.1016/j.jsames.2012.06.017.
- ^ Langer, M.C.; Ramezani, J.; Da Rosa, Á.A.S. (2018). "U-Pb age constraints on dinosaur rise from south Brazil". Gondwana Research. X (18): 133–140. Bibcode:2018GondR..57..133L. doi:10.1016/j.gr.2018.01.005.
- ^ Zerfass, H.; Lavina, E.L.; Schultz, C.L.; Garcia, A.J.V.; Faccini, U.F. & Chemale Jr., F. 2003. Sequence stratigraphy of continental Triassic strata of Southernmost Brazil: a contribution to Southwestern Gondwana palaeogeography and palaeoclimate. Sedimentary Geology, 161:85-105.
- ^ Holz, M. und Scherer, C.M.S., 2000, Sedimentological and paleontological evidence of paleoclimatic change during the Southbrazilian Triassic: the register of a global trend towards a humid paleoclimate: Zentralblatt für Geologie und Paläontologie, Teil I, v. 11-12, p. 1589-1609.
- ^ Rubert, R. R. & Schultz, C. L. 2004. — Um novo horizonte de correlação para o Triássico Superior do Rio Grande do Sul. Pesquisas em Geociências 31: 71-88.
- ^ Oliveira É. V. 2006. — Reevaluation of Therioherpeton cargnini Bonaparte & Barberena, 1975 (Probainognathia, Therioherpetidae) from the Upper Triassic of Brazil. Geodiversitas 28 (3) : 447-465.
- ^ Soares, M.B. & Schultz, C.L., 2006. Proposta de nova denominação para a Cenozona de Ictidosauria, do Triássico Superior (Formação Caturrita) do Rio Grande do Sul. V Simpósio Brasileiro de Paleontologia de Vertebrados, Boletim de Resumos, p. 41, Santa Maria, RS, 2006.
- ^ Schultz. C.L.; Scherer, C.M.S. & Barberena, M.C. 1994. Uma nova proposta de zoneamento estratigráfi co para o Triássico Superior Sul-Rio-Grandense. In: Congresso Brasileiro de Geologia, 38, Camboriú - SC, 1994. Boletim de Resumos, p. 107-108.
- ^ Rafael Costa Da Silva, Ismar De Souza Carvalho, Cibele Schwanke, 2006. Vertebrate dinoturbation from the Caturrita Formation (Late Triassic, Paraná Basin), Rio Grande do Sul State, Brazil. Gondwana Research 11 (2007) 303–310.
- ^ a b c d e f g Martinelli, A. G.; Escobar, J. A.; Francischini, H.; Kerber, L.; Müller, R. T.; Rubert, R.; Schultz, C. L.; Da-Rosa, Á. A. S. (2021). "New record of a stahleckeriid dicynodont (Therapsida, Dicynodontia) from the Late Triassic of southern Brazil and biostratigraphic remarks on the Riograndia Assemblage Zone". Historical Biology. 33 (11): 3101–3110. doi:10.1080/08912963.2020.1850715.
- ^ a b Guignard, M. L.; Martinelli, A. G.; Soares, M. B. (2019). "The postcranial anatomy of Brasilodon quadrangularis and the acquisition of mammaliaform traits among non-mammaliaform cynodonts". PLOS ONE. 14 (5): e0216672. doi:10.1371/journal.pone.0216672.
- ^ a b c d 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.
- ^ "Table 2.1," in Weishampel, et al. (2004). Page 26.
- ^ a b c Jonathas S. Bittencourt; Luciano A. Leal; Max C. Langer; Sérgio A. K. Azevedo (2012). "An additional basal sauropodomorph specimen from the Upper Triassic Caturrita Formation, southern Brazil, with comments on the biogeography of plateosaurids". Alcheringa: An Australasian Journal of Palaeontology. 36 (2): 269–278. doi:10.1080/03115518.2012.634111. S2CID 55842625.
- ^ a b c Jonathas Souza Bittencourt, Átila Augusto Stock da Rosa, Cesar Leandro Schultz and Max Cardoso Langer (2012). "Dinosaur remains from the 'Botucaraí Hill' (Caturrita Formation), Late Triassic of south Brazil, and their stratigraphic context". Historical Biology: An International Journal of Paleobiology. 25: 81–93. doi:10.1080/08912963.2012.694881. S2CID 55260304.
{{cite journal}}: CS1 maint: multiple names: authors list (link) - ^ a b c Sérgio Dias-da-Silva; Eliseu Vieira Dias; Cesar Leandro Schultz (2009). "First record of stereospondyls (Tetrapoda, Temnospondyli) in the Upper Triassic of Southern Brazil". Gondwana Research. 15 (1): 131–136. Bibcode:2009GondR..15..131D. doi:10.1016/j.gr.2008.07.002.
- ^ Felipe Chinaglia Montefeltro; Max Cardoso Langer; Cesar Leandro Schultz (2010). "Cranial anatomy of a new genus of hyperodapedontine rhynchosaur (Diapsida, Archosauromorpha) from the Upper Triassic of southern Brazil" (PDF). Earth and Environmental Science Transactions of the Royal Society of Edinburgh. 101: 27–52. doi:10.1017/S1755691010009060. S2CID 129472459.[permanent dead link]
Bibliography
- Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. 861 pp. ISBN 0-520-24209-2.
Further reading
- J. F. Bonaparte, J. Ferigolo, and A. M. Ribeiro. 1999. A new early Late Triassic saurischian dinosaur from Rio Grande do Sol state, Brazil. In Y. Tomida, T. H. Rich, and P. Vickers-Rich (eds.), Proceedings of the Second Gondwanan Dinosaur Symposium, National Science Museum Monographs 15:89-109
- G. Brea, J. F. Bonaparte, C. L. Schultz and A. G. Martinelli. 2005. A new specimen of Guaibasaurus candelariensis (basal Saurischia) from the Late Triassic Caturrita Formation of southern Brazil. In A. W. A. Kellner, D. D. R. Henriques, and T. Rodrigues (eds.), II Congresso Latino-Americano de Paleontologia de Vertebrados, Boletim de Resumos. Museum Nacional/UFRJ, Rio de Janeiro 55-56
- R. Costa, I. d. S. Carvalho, and C. Schwanke. 2003. Icnofósseis de vertebrados na Formação Caturrita (Neotriássico da Bacia do Paraná) no Estado do Rio Grande do Sul, Brasil [Vertebrate ichnofossils from the Caturrita Formation (Late Triassic of the Paraná Basin) in Rio Grande do Sul State, Brazil]. XVIII Congresso Brasileiro de Paleontologia: A Paleontologia e Suas Aplicações, 13–18 July 2003. Sociedade Brasileira de Paleontologia, Universidade de Brasília. Boletim de Resumos 110-111
- E.-E. Kischlat and M. C. Barbarena. 1999. Triassic Brazilian dinosaurs: new data. I Simpósio Brasileiro de Paleontologia de Vertebrados. Paleontologia em Destaque 26:56
- M. C. Langer and J. Ferigolo. 2005. The first ornithischian body-fossils in Brazil: Late Triassic (Caturrita Formation) of Rio Grande do Sul. In A. W. A. Kellner, D. D. R. Henriques, and T. Rodrigues (eds.), II Congresso Latino-Americano de Paleontologia de Vertebrados, Boletim de Resumos. Museum Nacional/UFRJ, Rio de Janeiro 146-147
- A. G. Martinelli, J. F. Bonaparte, C. L. Schultz and R. Rubert. 2005. A new tritheledontid (Therapsida, Eucynodontia) from the Late Triassic of Rio Grande do Sul (Brazil) and its phylogenetic relationships among carnivorous non-mammalian eucynodonts. Ameghiniana 42(1):191-208
- R. T. Müller, A. A. S. da Rosa, L. R. Silva, A. S. S. Aires, C. P. Pacheco, A. E. B. Pavanatto, and S. Dias-da-Silva. 2015. Wachholz, a new exquisite dinosaur-bearing fossiliferous site from the Upper Triassic of southern Brazil. Journal of South American Earth Sciences 61:120-128
- R. C. da Silva, R. Barboni, T. Dutra, M. M. Godoy, and R. B. Binotto. 2012. Footprints of large theropod dinosaurs and implications on the age of Triassic biotas from Southern Brazil. Journal of South American Earth Sciences
- M. B. Soares, C. L. Schultz, and B. I. D. Horn. 2011. New information on Riograndia guaibensis Bonaparte, Ferigolo & Ribeiro, 2001 (Eucynodontia, Tritheledontidae) from the Late Triassic of southern Brazil: anatomical and biostratigraphic implications. Anais da Academia Brasileira de Ciências 83(1):329-354