530:
320:
312:
2162:
1180:
2148:
1837:
1812:
1515:
1825:
338:
1192:
375:
747:
553:
651:
619:
635:
603:
569:
763:
699:
667:
587:
1527:
731:
683:
715:
537:
119:
2813:
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
2797:
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
2790:
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 . XVIII Congresso Brasileiro de Paleontologia: A Paleontologia e Suas Aplicações, 13–18 July 2003. Sociedade Brasileira de
2786:
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
2423:
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
2782:
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
2341:
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,
2805:
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
2351:
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.
2379:
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,
2801:
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
2572:
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".
2621:
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".
972:. This is the reason, why this biozone recently has been renamed as "Mammaliamorpha Cenozone" to underline the importance of the cynodont fossils. The Caturrita Formation also hosts the stratigraphic marker level "Jachaleria" named after the
2539:
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.
2389:
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.
923:-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.
2249:
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,
2399:
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)
2809:
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
2271:
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".
1615:"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."
2370:
Oliveira É. V. 2006. — Reevaluation of Therioherpeton cargnini Bonaparte & Barberena, 1975 (Probainognathia, Therioherpetidae) from the Upper Triassic of Brazil. Geodiversitas 28 (3) : 447-465.
918:
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, occasionally gravelly deposits of a
464:. 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
2877:
2676:
Sérgio Dias-da-Silva; Eliseu Vieira Dias; Cesar Leandro Schultz (2009). "First record of stereospondyls (Tetrapoda, Temnospondyli) in the Upper Triassic of Southern Brazil".
529:
2794:
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
778:
2657:
2361:
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.
2842:
2180:
2832:
2827:
2764:
Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. 861 pp.
575:
510:
decay) dating found that the Caturrita Formation dated around 225.42 million years ago, putting it less than 10 million years younger than the
2713:"Cranial anatomy of a new genus of hyperodapedontine rhynchosaur (Diapsida, Archosauromorpha) from the Upper Triassic of southern Brazil"
1667:"Three incomplete dinosaur specimens, an isolated sacral vertebra, an articulated left pubis–ischium and an isolated right ischium."
2769:
2545:
753:
2212:
2867:
1014:
625:
2882:
236:
1010:
559:
437:
1676:
of uncertain phylogenetic placement, "probably more primitive than typical 'prosauropods' from the Norian-Early Jurassic".
2857:
2852:
2240:
Bortoluzzi, C.A. 1974. Contribuição à Geologia da Região de Santa Maria, Rio Grande do Sul, Brasil. Pesquisas, 4 (1):7-86
2862:
229:
482:
The Caturrita Formation reaches a maximum thickness of 60 meters, but generally oscillates around values of 30 meters.
2712:
705:
902:
they follow for 250 kilometers a thin band in the central part of the state in an east-westerly fashion right up to
456:
The sediments of the Caturrita Formation belong to the second unit of the Santa Maria Supersequence and overlie the
275:
914:
The sediments of the Caturrita Formation belong to the upper section of the Santa Maria Supersequence. In terms of
2872:
2185:
854:
413:
2837:
2307:
Langer, M.C.; Ramezani, J.; Da Rosa, Á.A.S. (2018). "U-Pb age constraints on dinosaur rise from south Brazil".
2887:
903:
543:
515:
798:
417:
217:
145:
867:
2847:
2651:
2175:
1630:
915:
837:
511:
490:
Until 2018 no absolute ages had been determined, but the formation was most commonly assigned to a late
461:
168:
2727:
2685:
2582:
2487:
2433:
2316:
2281:
824:
783:
393:
135:
2228:
469:
311:
155:
2167:
880:
2743:
2639:
2598:
2449:
997:
811:
476:
769:
1179:
2765:
2541:
2515:
2112:
2067:
2030:
1974:
1935:
1899:
1789:
1699:
1654:
1602:
1558:
1482:
1421:
895:
787:
737:
689:
673:
657:
397:
325:
2787:
Paleontologia de Vertebrados, Boletim de Resumos. Museum Nacional/UFRJ, Rio de Janeiro 55-56
2735:
2693:
2631:
2590:
2505:
2495:
2441:
2324:
2289:
2190:
1949:
1390:
1151:
962:
609:
2216:
1641:
1589:
405:
353:
2731:
2689:
2586:
2491:
2437:
2320:
2285:
2510:
2471:
2209:
2153:
2054:
1958:
1884:
1829:
1714:
1673:
1621:
1580:
1276:
1207:
593:
503:
409:
268:
475:
The Caturrita Formation was once regarded as a member of the stratigraphically higher
2821:
2747:
2453:
2005:
1304:
1170:
920:
445:
70:
31:
27:
2643:
2602:
2147:
2086:
2045:
1915:
1836:
1625:
1543:
1519:
1257:
993:
973:
958:
2445:
1811:
2635:
2594:
2500:
2293:
2711:
Felipe Chinaglia Montefeltro; Max Cardoso Langer; Cesar Leandro Schultz (2010).
2130:
1853:
1341:
1079:
45:
2739:
2720:
Earth and Environmental Science Transactions of the Royal Society of Edinburgh
2143:
2097:
2015:
1874:
1841:
1804:
1684:
1531:
1514:
1502:
1367:
1316:
1307:
1285:
1233:
1196:
1184:
1065:
1002:
986:
977:
965:
815:
802:
90:
55:
2697:
2328:
290:
277:
251:
238:
2476:
and the acquisition of mammaliaform traits among non-mammaliaform cynodonts"
1824:
1774:
1729:
1469:
935:
931:
641:
203:
199:
95:
39:
2519:
1191:
1020:
The following taxa have been discovered so far in the Caturrita Formation:
1984:
1740:
1506:
1435:
1173:
1118:
982:
947:
927:
858:
845:
828:
499:
465:
401:
213:
85:
80:
65:
60:
50:
894:
Outcrops of the Caturrita Formation are found in the Brazilian state of
374:
1924:
1816:
1526:
1072:
899:
884:
871:
721:
507:
491:
379:
100:
75:
118:
2116:
2071:
2034:
1939:
1903:
1793:
1703:
1658:
1606:
1562:
1486:
1425:
969:
495:
433:
343:
1734:
1430:
1113:
1038:
2791:
Paleontologia, Universidade de Brasília. Boletim de Resumos 110-111
1835:
1823:
1810:
1525:
1513:
1190:
1178:
1043:
124:
506:
age of this unit was also advocated in the literature. A U-Pb (
2624:
Historical Biology: An International Journal of Paleobiology
1009:
The fossil finds are concentrated around three major areas:
1575:"Partial postcranial skeleton and a fragmentary hindlimb."
2470:
Guignard, M. L.; Martinelli, A. G.; Soares, M. B. (2019).
1013:
and northern surroundings (Água Negra) Faxinal do Soturno
1624:
of uncertain phylogenetic placement, probably "closer to
2535:
2533:
2531:
2529:
2616:
2614:
2612:
2575:
Alcheringa: An Australasian Journal of Palaeontology
2557:"Table 2.1," in Weishampel, et al. (2004). Page 26.
472:, the third unit of the Santa Maria Supersequence.
364:
359:
349:
331:
306:
267:
228:
223:
209:
195:
190:
182:
174:
161:
151:
141:
131:
21:
2878:Fossiliferous stratigraphic units of South America
2567:
2565:
2563:
2125:"Two nearly complete skulls and a partial skull."
2418:
2416:
2414:
2412:
2410:
2408:
2406:
2465:
2463:
946:The Caturrita Formation contains a biozone for
518:, from where the earliest dinosaurs are known.
479:or was expanded to include the Mata Sandstone.
2266:
2264:
2262:
2260:
2258:
2256:
950:, the so-called "Ictidosauria Assemblage Zone
8:
2656:: CS1 maint: multiple names: authors list (
16:Rock formation in Rio Grande do Sul, Brazil
428:The formation received this name, because
373:
117:
18:
2671:
2669:
2667:
2509:
2499:
926:The sediments are of continental nature (
498:age on paleontological grounds. However,
2274:Journal of South American Earth Sciences
2181:List of dinosaur-bearing rock formations
1737:
1433:
1116:
2202:
2649:
2798:Nacional/UFRJ, Rio de Janeiro 146-147
1420:Unnamed prosauropod genus present in
7:
1634:-like basal–most sauropodomorphs".
1378:Linha São Luiz, Sesmaria do Pinhal
1268:Linha São Luiz, Sesmaria do Pinhal
1244:Linha São Luiz, Sesmaria do Pinhal
1095:Uncertain or tentative taxa are in
746:
552:
1017:and surroundings (Linha São Luis)
650:
618:
14:
1948:The earliest diverging member of
1055:Taxon falsely reported as present
634:
602:
568:
2843:Triassic System of South America
2160:
2146:
1000:that were most likely caused by
762:
761:
745:
729:
713:
698:
697:
681:
666:
665:
649:
633:
617:
601:
586:
585:
567:
551:
535:
528:
368:Caturrita, barrio of Santa Maria
336:
318:
310:
2085:An indeterminate stereospondyl
1060:Dubious taxon or junior synonym
730:
2833:Geography of Rio Grande do Sul
989:have been discovered as well.
682:
1:
2828:Geologic formations of Brazil
2446:10.1080/08912963.2020.1850715
186:30–60 m (98–197 ft)
123:Caturrita Formation. Source:
2636:10.1080/08912963.2012.694881
2595:10.1080/03115518.2012.634111
2501:10.1371/journal.pone.0216672
2472:"The postcranial anatomy of
2294:10.1016/j.jsames.2012.06.017
2080:An incomplete interclavicle
714:
536:
416:in the upper section of the
408:. The formation is from the
269:Approximate paleocoordinates
1809:
1335:A stahleckeriid dicynodont
1022:
2904:
1743:of the Caturrita Formation
1512:
1438:of the Caturrita Formation
1385:A tritheledontid cynodont
1177:
1121:of the Caturrita Formation
2740:10.1017/S1755691010009060
2474:Brasilodon quadrangularis
2186:Laguna Colorada Formation
1360:Brasilodon quadrangularis
1251:A mammaliamorph cynodont
1226:Brasilodon quadrangularis
1029:
1025:
978:Jachaleria candelariensis
855:Sanga do Cabral Formation
414:Santa Maria Supersequence
372:
178:250 km (160 mi)
116:
26:
2698:10.1016/j.gr.2008.07.002
2329:10.1016/j.gr.2018.01.005
1496:Two isolated footprints
1027:
968:, a sister group of the
910:Depositional environment
516:Ischigualasto Formations
2868:Conglomerate formations
1758:Stratigraphic position
1453:Stratigraphic position
1136:Stratigraphic position
522:Geographical occurrence
252:29.695042°S 53.795403°W
2883:Paleontology in Brazil
1845:
1833:
1821:
1535:
1523:
1505:; footprints of large
1200:
1188:
1103:taxa are discredited.
412:and forms part of the
404:were deposited in the
257:-29.695042; -53.795403
2176:Santa Maria Formation
1839:
1827:
1814:
1529:
1517:
1328:Alto Guarda Mor site
1194:
1182:
1003:Unaysaurus tolentinoi
996:have been found near
916:sequence stratigraphy
838:Santa Maria Formation
799:Serra Geral Formation
784:Geological formations
462:Santa Maria Formation
169:Santa Maria Formation
2858:Siltstone formations
2853:Sandstone formations
2210:Formação Santa Maria
1399:Sesmaria do Pinhal,
779:class=notpageimage|
432:is a neighbourhood (
418:Rosário do Sul Group
146:Rosário do Sul Group
136:Geological formation
2863:Mudstone formations
2732:2010EESTR.101...27M
2690:2009GondR..15..131D
2587:2012Alch...36..269B
2492:2019PLoSO..1416672G
2438:2021HBio...33.3101M
2321:2018GondR..57..133L
2286:2012JSAES..39...16D
2168:Paleontology portal
1296:Sesmaria do Pinhal
1162:Sesmaria do Pinhal
930:) and form massive
898:. From the town of
868:Piramboia Formation
842:Caturrita Formation
444:also refers to the
390:Caturrita Formation
287: /
248: /
28:Stratigraphic range
22:Caturrita Formation
2426:Historical Biology
2424:Assemblage Zone".
2215:2008-05-01 at the
1846:
1834:
1822:
1536:
1524:
1201:
1189:
1050:Reclassified taxon
998:Faxinal do Soturno
992:In 1998 tracks of
812:Botucatu Formation
477:Botucatu Formation
2678:Gondwana Research
2432:(11): 3101–3110.
2309:Gondwana Research
2231:, (in Portuguese)
2219:, (in Portuguese)
2137:
2136:
2113:Rio Grande do Sul
2068:Rio Grande do Sul
2031:Rio Grande do Sul
1936:Rio Grande do Sul
1900:Rio Grande do Sul
1790:Rio Grande do Sul
1721:
1720:
1700:Rio Grande do Sul
1672:An indeterminate
1655:Rio Grande do Sul
1620:An indeterminate
1603:Rio Grande do Sul
1559:Rio Grande do Sul
1552:G. candelariensis
1483:Rio Grande do Sul
1422:Rio Grande do Sul
1413:
1412:
1324:J. candelariensis
1292:J. candelariensis
1240:B. quadrangularis
1107:
1106:
1098:
1086:
1085:
1082:
1075:
1068:
1061:
1056:
1051:
1046:
896:Rio Grande do Sul
788:Rio Grande do Sul
468:sediments of the
398:Rio Grande do Sul
386:
385:
326:Rio Grande do Sul
2895:
2873:Fluvial deposits
2752:
2751:
2717:
2708:
2702:
2701:
2673:
2662:
2661:
2655:
2647:
2618:
2607:
2606:
2569:
2558:
2555:
2549:
2537:
2524:
2523:
2513:
2503:
2467:
2458:
2457:
2420:
2401:
2397:
2391:
2387:
2381:
2377:
2371:
2368:
2362:
2359:
2353:
2349:
2343:
2339:
2333:
2332:
2304:
2298:
2297:
2268:
2251:
2247:
2241:
2238:
2232:
2226:
2220:
2207:
2191:Elliot Formation
2170:
2165:
2164:
2163:
2156:
2151:
2150:
1950:Pterosauromorpha
1735:
1431:
1391:Traversodontidae
1214:B. riograndensis
1152:Botucaraitherium
1114:
1096:
1078:
1071:
1064:
1059:
1054:
1049:
1042:
1039:
1023:
942:Vertebrate fauna
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748:
733:
732:
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684:
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440:. In Portuguese
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42:
19:
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2898:
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2892:
2838:Triassic Brazil
2818:
2817:
2779:
2777:Further reading
2761:
2756:
2755:
2715:
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2705:
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2527:
2486:(5): e0216672.
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2378:
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2369:
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2356:
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2340:
2336:
2315:(18): 133–140.
2306:
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2239:
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2227:
2223:
2217:Wayback Machine
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2145:
2142:
2106:T. sulcognathus
1975:Proterochampsid
1862:C. brasiliensis
1726:
1724:Other tetrapods
1642:Sauropodomorpha
1590:Sauropodomorpha
1570:Linha São Luiz
1418:
1112:
1094:
1037:
944:
912:
892:
891:
890:
889:
874:
861:
848:
831:
825:Guará Formation
818:
805:
781:
775:
774:
773:
772:
766:
758:
757:
756:
750:
742:
741:
740:
734:
726:
725:
724:
718:
710:
709:
708:
702:
694:
693:
692:
686:
678:
677:
676:
670:
662:
661:
660:
654:
646:
645:
644:
638:
630:
629:
628:
622:
614:
613:
612:
606:
598:
597:
596:
590:
582:
581:
580:
577:
572:
564:
563:
562:
556:
548:
547:
546:
540:
524:
488:
454:
426:
378:
337:
335:
319:
317:
316:
295:
293:
289:
286:
281:
278:
276:
274:
273:
256:
254:
250:
247:
242:
239:
237:
235:
234:
166:
127:
111:
110:
109:
108:
103:
98:
93:
88:
83:
78:
73:
68:
63:
58:
53:
48:
37:
36:
34:
17:
12:
11:
5:
2901:
2899:
2891:
2890:
2885:
2880:
2875:
2870:
2865:
2860:
2855:
2850:
2845:
2840:
2835:
2830:
2820:
2819:
2816:
2815:
2811:
2807:
2803:
2799:
2795:
2792:
2788:
2784:
2778:
2775:
2774:
2773:
2760:
2757:
2754:
2753:
2703:
2684:(1): 131–136.
2663:
2608:
2581:(2): 269–278.
2559:
2550:
2525:
2459:
2402:
2392:
2382:
2372:
2363:
2354:
2344:
2334:
2299:
2252:
2242:
2233:
2229:Paleoformações
2221:
2201:
2200:
2198:
2195:
2194:
2193:
2188:
2183:
2178:
2172:
2171:
2157:
2154:Geology portal
2141:
2138:
2135:
2134:
2127:
2122:
2120:
2109:
2102:
2092:
2091:
2082:
2077:
2075:
2064:
2062:Indeterminate
2059:
2055:Stereospondyli
2050:
2049:
2042:
2040:
2038:
2027:
2020:
2010:
2009:
2006:Procolophonian
2002:
2000:
1998:
1996:
1989:
1979:
1978:
1971:
1969:
1967:
1965:
1963:
1959:Proterochampsa
1953:
1952:
1946:
1944:
1942:
1933:
1928:
1920:
1919:
1911:
1909:
1907:
1896:
1889:
1885:Faxinalipterus
1879:
1878:
1871:
1869:
1867:
1865:
1858:
1848:
1847:
1830:Proterochampsa
1820:skull material
1808:
1801:
1799:
1797:
1786:
1779:
1769:
1768:
1765:
1762:
1759:
1756:
1753:
1750:
1746:
1745:
1725:
1722:
1719:
1718:
1715:Sauropodomorph
1711:
1709:
1707:
1696:
1689:
1679:
1678:
1674:sauropodomorph
1669:
1664:
1662:
1651:
1649:Indeterminate
1646:
1637:
1636:
1628:(...) than to
1622:sauropodomorph
1617:
1612:
1610:
1599:
1597:Indeterminate
1594:
1585:
1584:
1581:Sauropodomorph
1577:
1572:
1567:
1555:
1548:
1538:
1537:
1511:
1498:
1493:
1491:
1479:
1477:Indeterminate
1474:
1464:
1463:
1460:
1457:
1454:
1451:
1448:
1445:
1441:
1440:
1417:
1414:
1411:
1410:
1408:
1406:
1404:
1397:
1396:Indeterminate
1394:
1387:
1386:
1383:
1381:
1379:
1376:
1371:
1363:
1362:
1356:
1354:
1352:
1350:
1345:
1337:
1336:
1333:
1331:
1329:
1326:
1320:
1311:
1310:
1301:
1299:
1297:
1294:
1289:
1281:
1280:
1277:tritheledontid
1273:
1271:
1269:
1266:
1261:
1253:
1252:
1249:
1247:
1245:
1242:
1237:
1229:
1228:
1222:
1220:
1218:
1216:
1211:
1208:Brasilitherium
1203:
1202:
1176:
1167:
1165:
1163:
1160:
1155:
1147:
1146:
1143:
1140:
1137:
1134:
1131:
1128:
1124:
1123:
1111:
1108:
1105:
1104:
1089:
1087:
1084:
1083:
1076:
1069:
1062:
1057:
1052:
1047:
1031:
1030:
1028:
1026:
963:tritheledontid
943:
940:
911:
908:
888:
887:
875:
862:
849:
832:
819:
806:
792:
777:
776:
768:
767:
760:
759:
752:
751:
744:
743:
736:
735:
728:
727:
720:
719:
712:
711:
704:
703:
696:
695:
688:
687:
680:
679:
672:
671:
664:
663:
656:
655:
648:
647:
640:
639:
632:
631:
624:
623:
616:
615:
608:
607:
600:
599:
592:
591:
584:
583:
574:
573:
566:
565:
558:
557:
550:
549:
542:
541:
534:
533:
527:
526:
525:
523:
520:
504:Early Jurassic
487:
484:
470:Mata Sandstone
453:
450:
425:
422:
410:Upper Triassic
400:, Brazil. Its
394:rock formation
384:
383:
370:
369:
366:
362:
361:
357:
356:
351:
347:
346:
333:
329:
328:
308:
304:
303:
271:
265:
264:
232:
226:
225:
221:
220:
211:
207:
206:
197:
193:
192:
188:
187:
184:
180:
179:
176:
172:
171:
163:
159:
158:
156:Mata Sandstone
153:
149:
148:
143:
139:
138:
133:
129:
128:
122:
114:
113:
106:
105:
104:
99:
94:
89:
84:
79:
74:
69:
64:
59:
54:
49:
44:
43:
24:
23:
15:
13:
10:
9:
6:
4:
3:
2:
2900:
2889:
2886:
2884:
2881:
2879:
2876:
2874:
2871:
2869:
2866:
2864:
2861:
2859:
2856:
2854:
2851:
2849:
2846:
2844:
2841:
2839:
2836:
2834:
2831:
2829:
2826:
2825:
2823:
2814:83(1):329-354
2812:
2808:
2804:
2802:42(1):191-208
2800:
2796:
2793:
2789:
2785:
2781:
2780:
2776:
2771:
2770:0-520-24209-2
2767:
2763:
2762:
2758:
2749:
2745:
2741:
2737:
2733:
2729:
2725:
2721:
2714:
2707:
2704:
2699:
2695:
2691:
2687:
2683:
2679:
2672:
2670:
2668:
2664:
2659:
2653:
2645:
2641:
2637:
2633:
2629:
2625:
2617:
2615:
2613:
2609:
2604:
2600:
2596:
2592:
2588:
2584:
2580:
2576:
2568:
2566:
2564:
2560:
2554:
2551:
2547:
2546:0-520-24209-2
2543:
2536:
2534:
2532:
2530:
2526:
2521:
2517:
2512:
2507:
2502:
2497:
2493:
2489:
2485:
2481:
2477:
2475:
2466:
2464:
2460:
2455:
2451:
2447:
2443:
2439:
2435:
2431:
2427:
2419:
2417:
2415:
2413:
2411:
2409:
2407:
2403:
2396:
2393:
2386:
2383:
2376:
2373:
2367:
2364:
2358:
2355:
2348:
2345:
2338:
2335:
2330:
2326:
2322:
2318:
2314:
2310:
2303:
2300:
2295:
2291:
2287:
2283:
2279:
2275:
2267:
2265:
2263:
2261:
2259:
2257:
2253:
2246:
2243:
2237:
2234:
2230:
2225:
2222:
2218:
2214:
2211:
2206:
2203:
2196:
2192:
2189:
2187:
2184:
2182:
2179:
2177:
2174:
2173:
2169:
2158:
2155:
2149:
2144:
2139:
2133:
2132:
2128:
2126:
2123:
2121:
2119:
2118:
2114:
2110:
2108:
2107:
2103:
2101:
2100:
2099:
2094:
2093:
2090:
2088:
2083:
2081:
2078:
2076:
2074:
2073:
2069:
2065:
2063:
2060:
2058:
2056:
2052:
2051:
2048:
2047:
2043:
2041:
2039:
2037:
2036:
2032:
2028:
2026:
2025:
2024:S. agudoensis
2021:
2019:
2018:
2017:
2012:
2011:
2008:
2007:
2003:
2001:
1999:
1997:
1995:
1994:
1990:
1988:
1987:
1986:
1981:
1980:
1977:
1976:
1972:
1970:
1968:
1966:
1964:
1962:
1961:
1960:
1955:
1954:
1951:
1947:
1945:
1943:
1941:
1937:
1934:
1932:
1931:M. bonapartei
1929:
1927:
1926:
1922:
1921:
1918:
1917:
1912:
1910:
1908:
1906:
1905:
1901:
1897:
1895:
1894:
1890:
1888:
1887:
1886:
1881:
1880:
1877:
1876:
1872:
1870:
1868:
1866:
1864:
1863:
1859:
1857:
1856:
1855:
1850:
1849:
1844:
1843:
1838:
1832:
1831:
1826:
1819:
1818:
1813:
1807:
1806:
1802:
1800:
1798:
1796:
1795:
1791:
1787:
1785:
1784:
1783:C. enigmatica
1780:
1778:
1777:
1776:
1771:
1770:
1766:
1763:
1760:
1757:
1754:
1751:
1748:
1747:
1744:
1742:
1736:
1733:
1731:
1728:Undetermined
1723:
1717:
1716:
1712:
1710:
1708:
1706:
1705:
1701:
1697:
1695:
1694:
1693:U. tolentinoi
1690:
1688:
1687:
1686:
1681:
1680:
1677:
1675:
1670:
1668:
1665:
1663:
1661:
1660:
1656:
1652:
1650:
1647:
1645:
1643:
1639:
1638:
1635:
1633:
1632:
1627:
1623:
1618:
1616:
1613:
1611:
1609:
1608:
1604:
1600:
1598:
1595:
1593:
1591:
1587:
1586:
1583:
1582:
1578:
1576:
1573:
1571:
1568:
1566:
1564:
1560:
1556:
1554:
1553:
1549:
1547:
1546:
1545:
1540:
1539:
1534:
1533:
1528:
1522:
1521:
1516:
1510:
1508:
1504:
1499:
1497:
1494:
1492:
1490:
1488:
1484:
1480:
1478:
1475:
1473:
1472:
1471:
1466:
1465:
1461:
1458:
1455:
1452:
1449:
1446:
1443:
1442:
1439:
1437:
1432:
1429:
1427:
1423:
1415:
1409:
1407:
1405:
1402:
1398:
1395:
1392:
1389:
1388:
1384:
1382:
1380:
1377:
1375:
1374:R. guaibensis
1372:
1370:
1369:
1365:
1364:
1361:
1357:
1355:
1353:
1351:
1349:
1346:
1344:
1343:
1339:
1338:
1334:
1332:
1330:
1327:
1325:
1321:
1319:
1318:
1313:
1312:
1309:
1306:
1305:stahleckeriid
1302:
1300:
1298:
1295:
1293:
1290:
1288:
1287:
1283:
1282:
1278:
1274:
1272:
1270:
1267:
1265:
1264:I. hernandezi
1262:
1260:
1259:
1255:
1254:
1250:
1248:
1246:
1243:
1241:
1238:
1236:
1235:
1231:
1230:
1227:
1223:
1221:
1219:
1217:
1215:
1212:
1210:
1209:
1205:
1204:
1199:
1198:
1193:
1187:
1186:
1181:
1175:
1172:
1171:mammaliamorph
1168:
1166:
1164:
1161:
1159:
1158:B. belarminoi
1156:
1154:
1153:
1149:
1148:
1144:
1141:
1138:
1135:
1132:
1129:
1126:
1125:
1122:
1120:
1115:
1109:
1102:
1093:
1090:
1088:
1081:
1077:
1074:
1070:
1067:
1063:
1058:
1053:
1048:
1045:
1041:
1040:
1036:
1033:
1032:
1024:
1021:
1018:
1016:
1012:
1007:
1005:
1004:
999:
995:
990:
988:
984:
980:
979:
975:
971:
967:
964:
960:
956:
953:
949:
941:
939:
937:
933:
929:
924:
922:
921:braided river
917:
909:
907:
905:
901:
897:
886:
882:
881:Itararé Group
879:
876:
873:
869:
866:
863:
860:
856:
853:
850:
847:
843:
839:
836:
833:
830:
826:
823:
820:
817:
813:
810:
807:
804:
800:
797:
794:
793:
791:
789:
785:
780:
771:
755:
739:
723:
707:
691:
675:
659:
643:
627:
611:
595:
579:
561:
545:
531:
521:
519:
517:
513:
509:
505:
501:
497:
493:
485:
483:
480:
478:
473:
471:
467:
463:
459:
458:Alemoa Member
451:
449:
447:
446:monk parakeet
443:
439:
435:
431:
423:
421:
419:
415:
411:
407:
403:
399:
395:
391:
382:of Paleorrota
381:
376:
371:
367:
363:
358:
355:
352:
348:
345:
334:
330:
327:
313:
309:
305:
300:
291:37.3°S 16.0°W
272:
270:
266:
261:
233:
231:
227:
222:
219:
215:
212:
208:
205:
201:
198:
194:
189:
185:
181:
177:
173:
170:
165:Alemoa Member
164:
160:
157:
154:
150:
147:
144:
140:
137:
134:
130:
126:
120:
115:
102:
97:
92:
87:
82:
77:
72:
67:
62:
57:
52:
47:
41:
33:
32:Late Triassic
29:
25:
20:
2888:Paraná Basin
2848:Norian Stage
2759:Bibliography
2726:(1): 27–52.
2723:
2719:
2706:
2681:
2677:
2652:cite journal
2627:
2623:
2578:
2574:
2553:
2483:
2479:
2473:
2429:
2425:
2395:
2385:
2375:
2366:
2357:
2347:
2337:
2312:
2308:
2302:
2277:
2273:
2245:
2236:
2224:
2205:
2129:
2124:
2111:
2105:
2104:
2096:
2095:
2087:temnospondyl
2084:
2079:
2066:
2061:
2053:
2044:
2029:
2023:
2022:
2014:
2013:
2004:
1992:
1991:
1983:
1982:
1973:
1957:
1956:
1930:
1923:
1913:
1898:
1892:
1891:
1883:
1882:
1873:
1861:
1860:
1852:
1851:
1840:
1828:
1815:
1803:
1788:
1782:
1781:
1773:
1772:
1738:
1727:
1713:
1698:
1692:
1691:
1683:
1682:
1671:
1666:
1653:
1648:
1640:
1629:
1626:Plateosauria
1619:
1614:
1601:
1596:
1588:
1579:
1574:
1569:
1557:
1551:
1550:
1544:Guaibasaurus
1542:
1541:
1530:
1520:Guaibasaurus
1518:
1500:
1495:
1481:
1476:
1468:
1467:
1434:
1419:
1400:
1373:
1366:
1359:
1347:
1340:
1323:
1315:
1291:
1284:
1263:
1258:Irajatherium
1256:
1239:
1232:
1225:
1213:
1206:
1195:
1183:
1157:
1150:
1117:
1100:
1091:
1034:
1019:
1008:
1001:
994:prosauropods
991:
976:
954:
951:
945:
925:
913:
893:
877:
864:
851:
841:
834:
821:
808:
795:
782:
489:
481:
474:
457:
455:
452:Stratigraphy
441:
429:
427:
406:Paraná Basin
389:
387:
360:Type section
354:Paraná Basin
296:-37.3; -16.0
218:conglomerate
38:225.42
2342:161:85-105.
2131:Rhynchosaur
1993:S. caliodon
1854:Clevosaurus
1509:dinosaurs.
1358:Synonym of
1342:Minicynodon
1224:Synonym of
1101:crossed out
1080:Morphotaxon
1011:Santa Maria
987:vertebrates
959:Ictidosaurs
754:São Gabriel
560:Santa Maria
512:Santa Maria
438:Santa Maria
294: /
255: /
230:Coordinates
2822:Categories
2806:61:120-128
2352:1589-1609.
2250:p.659-673.
2197:References
2098:Teyumbaita
2046:Silesaurid
2016:Sacisaurus
1916:lagerpetid
1893:F. minimus
1875:Sphenodont
1842:Sacisaurus
1805:Lepidosaur
1685:Unaysaurus
1631:Saturnalia
1532:Unaysaurus
1503:ichnotaxon
1401:Sacisaurus
1368:Riograndia
1317:Jachaleria
1308:dicynodont
1286:Jachaleria
1234:Brasilodon
1197:Riograndia
1185:Brasilodon
1097:small text
1066:Ichnotaxon
1015:Candelária
985:and other
974:dicynodont
816:Cretaceous
803:Cretaceous
658:Santa Cruz
626:Candelária
315:Paleorrota
243:53°47′43″W
240:29°41′42″S
2783:15:89-109
2748:129472459
2630:: 81–93.
2454:229399221
2280:: 16–23.
1775:Cargninia
1761:Material
1755:Location
1741:tetrapods
1730:phytosaur
1470:Eubrontes
1456:Material
1450:Location
1436:Dinosaurs
1416:Dinosaurs
1348:M. maieri
1279:cynodont
1139:Material
1133:Location
1119:Synapsids
1110:Synapsids
1035:Color key
983:Dinosaurs
966:cynodonts
948:tetrapods
936:siltstone
932:sandstone
642:Rio Pardo
610:Cachoeira
494:to early
442:caturrita
430:Caturrita
424:Etymology
402:sediments
396:found in
365:Named for
204:siltstone
200:Sandstone
191:Lithology
183:Thickness
152:Underlies
2810:Sciences
2644:55260304
2603:55842625
2520:31075140
2480:PLOS ONE
2400:303–310.
2390:107-108.
2213:Archived
2140:See also
1985:Soturnia
1752:Species
1507:theropod
1447:Species
1174:cynodont
1130:Species
938:bodies.
928:red beds
859:Triassic
846:Triassic
829:Jurassic
770:Caçapava
706:Alegrete
674:Venâncio
594:São Sepé
502:or even
500:Rhaetian
466:Rhaetian
224:Location
214:Mudstone
162:Overlies
2728:Bibcode
2686:Bibcode
2583:Bibcode
2511:6510408
2488:Bibcode
2434:Bibcode
2317:Bibcode
2282:Bibcode
2057:indet.
1925:Maehary
1817:Maehary
1767:Images
1732:genus.
1644:indet.
1592:indet.
1462:Images
1393:indet.
1145:Images
1073:Ootaxon
970:mammals
900:Taquari
885:Permian
872:Permian
738:Rosário
508:Uranium
492:Carnian
460:of the
380:Geopark
332:Country
282:16°00′W
279:37°18′S
196:Primary
142:Unit of
107:↓
2768:
2746:
2642:
2601:
2544:
2518:
2508:
2452:
2117:Brazil
2072:Brazil
2035:Brazil
1940:Brazil
1904:Brazil
1794:Brazil
1764:Notes
1749:Genus
1704:Brazil
1659:Brazil
1607:Brazil
1563:Brazil
1487:Brazil
1459:Notes
1444:Genus
1426:Brazil
1142:Notes
1127:Genus
840:&
690:Aceguá
496:Norian
434:barrio
350:Extent
344:Brazil
341:
323:
307:Region
167:
2744:S2CID
2716:(PDF)
2640:S2CID
2599:S2CID
2450:S2CID
2380:2006.
1739:Misc
1403:site
1092:Notes
1044:Taxon
578:Pedro
436:) of
392:is a
210:Other
2766:ISBN
2658:link
2542:ISBN
2516:PMID
1322:cf.
1314:cf.
961:are
955:Ca-1
934:and
904:Mata
722:Bagé
544:Mata
514:and
388:The
175:Area
132:Type
125:UFSM
46:PreꞒ
2736:doi
2724:101
2694:doi
2632:doi
2591:doi
2506:PMC
2496:doi
2442:doi
2325:doi
2290:doi
1501:An
786:in
576:São
486:Age
2824::
2742:.
2734:.
2722:.
2718:.
2692:.
2682:15
2680:.
2666:^
2654:}}
2650:{{
2638:.
2628:25
2626:.
2611:^
2597:.
2589:.
2579:36
2577:.
2562:^
2528:^
2514:.
2504:.
2494:.
2484:14
2482:.
2478:.
2462:^
2448:.
2440:.
2430:33
2428:.
2405:^
2323:.
2311:.
2288:.
2278:39
2276:.
2255:^
2115:,
2089:.
2070:,
2033:,
1938:,
1914:A
1902:,
1792:,
1702:,
1657:,
1605:,
1565:.
1561:,
1489:.
1485:,
1428:.
1424:,
1303:A
1275:A
1169:A
1099:;
1006:.
981:.
906:.
883:,
878:7)
870:,
865:6)
857:,
852:5)
844:,
835:4)
827:,
822:3)
814:,
809:2)
801:,
796:1)
448:.
420:.
216:,
202:,
96:Pg
40:Ma
30::
2772:.
2750:.
2738::
2730::
2700:.
2696::
2688::
2660:)
2646:.
2634::
2605:.
2593::
2585::
2548:.
2522:.
2498::
2490::
2456:.
2444::
2436::
2331:.
2327::
2319::
2313:X
2296:.
2292::
2284::
957:.
952:″
790::
101:N
91:K
86:J
81:T
76:P
71:C
66:D
61:S
56:O
51:Ꞓ
35:~
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