The Sanga do Cabral Formation is an Early Triassic sedimentary rock formation found in Rio Grande do Sul, Brazil.[1]
Sanga do Cabral Formation | |
---|---|
Stratigraphic range: Early Triassic | |
Type | Geological formation |
Unit of | Rosário do Sul Group |
Underlies | Santa Maria Formation |
Overlies | Pirambóia Formation |
Lithology | |
Primary | Sandstone, conglomerate |
Location | |
Coordinates | 29°36′S 55°06′W / 29.6°S 55.1°W |
Approximate paleocoordinates | 49°00′S 24°36′W / 49.0°S 24.6°W |
Region | Paleorrota Rio Grande do Sul |
Country | Brazil |
Extent | Paraná Basin |
Geopark of Paleorrota |
Description
editThis rock formation is located in the geopark of Paleorrota, and is located to the south of another geopark. The formation dates to 249 million years ago and belongs to the Lower Triassic.[2]
The Sanga do Cabral Formation is correlated with the "impoverished zone" (Procolophon subzone) of the Lystrosaurus Assemblage Zone of the Karoo Basin of South Africa by some authors on the basis of the abundant records of Procolophon.
Fossil content
editAmong others, the following fossils have been reported from the formation:[3]
Formations
editSee also
editReferences
edit- ^ Sanga do Cabral Formation at Fossilworks.org
- ^ (in Portuguese) Es Sincro Archived May 1, 2008, at the Wayback Machine
- ^ Cachoeira do Sul at Fossilworks.org
- ^ Pinheiro, Felipe L.; Eltink, Estevan; Paes-Neto, Voltaire D.; Machado, Arielli F.; Simões, Tiago R.; Pierce, Stephanie E. (2024-01-19). "Interrelationships among Early Triassic faunas of Western Gondwana and Laurasia as illuminated by a new South American benthosuchid temnospondyl". The Anatomical Record. 307 (4): 726–743. doi:10.1002/ar.25384. ISSN 1932-8486. PMID 38240478.
- ^ Cisneros & Schultz, 2002
- ^ Dias da Silva et al., 2006
- ^ Eltink et al., 2017
- ^ Dias da Silva & Ramos Ilha, 2009
Bibliography
edit- De Oliveira, T. M.; Pinheiro, F. L.; Stock Da Rosa, A. A.; Dias Da Silva, S.; Kerber, L. (2020), "A new archosauromorph from South America provides insights on the early diversification of tanystropheids", PLoS ONE, 15 (4): e0230890, Bibcode:2020PLoSO..1530890D, doi:10.1371/journal.pone.0230890, PMC 7141609, PMID 32267850
- Eltink, E.; Da Rosa, A. A. S.; Dias Da Silva, S. (2017), "A capitosauroid from the Lower Triassic of South America (Sanga do Cabral Supersequence: Paraná Basin), its phylogenetic relationships and biostratigraphic implications", Historical Biology, 29 (7): 863–874, Bibcode:2017HBio...29..863E, doi:10.1080/08912963.2016.1255736
- Da Rosa, A. A. S.; Pineiro, G.; Dias Da Silva, S.; Cisneros, J. C.; Feltrin, F. F.; Neto, L. W. (2009), "Bica São Tomé, um novo sítio fossilífero para o Triássico inferior do sul do Brasil", Revista Brasileira de Paleontologia, 12: 67–76
- Dias Da Silva, Sérgio; Ramos Ilha, Ana Luiza (2009), "On the presence of a pustulated temnospondyl in the Lower Triassic of southern Brazil", Acta Palaeontologica Polonica, 54 (4): 609–614, doi:10.4202/app.2008.0073
- Dias Da Silva, S.; Marsicano, C.; Schultz, C. L. (2006), "Rhytidosteid temnospondyls in Gondwana: a new taxon from the Lower Triassic of Brazil", Palaeontology, 49 (2): 381–390, Bibcode:2006Palgy..49..381D, doi:10.1111/j.1475-4983.2006.00545.x, hdl:11336/93652
- Cisneros, J. C.; Schultz, C. L. (2002), "Procolophon brasiliensis n. sp., a new procolophonid reptile from the Lower Triassic of southern Brazil", Neues Jahrbuch für Geologie und Paläontologie - Monatshefte, 2002 (11): 641–648, doi:10.1127/njgpm/2002/2002/641
- Lavina, E. L (1983), "Procolophon pricei sp. n., um novo réptil procolofonídeo do Triássico do Rio Grande do Sul", Iheringia, Série Geologia, 9: 51–78
Further reading
edit- "First record of non-mammalian cynodonts (Therapsida) in the Sanga do Cabral Formation (Early Triassic) of southern Brazil". Wiredspace.wits.ac.za. Retrieved 2015-09-08.