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- Souvrství Santa Maria je geologická formace na území brazilského státu Rio Grande do Sul. (cs)
- Die Santa-Maria-Formation ist eine lithostratigraphische Formation sedimentären Ursprungs aus der Mittleren Trias des südlichen Brasiliens. Sie gehört zur aus der und damit zur im Paraná-Becken abgelagerten . Die Formation besitzt eine überaus reichhaltige Wirbeltierfauna. (de)
- La Formación Santa María es una formación geológica. El suelo es Lutolita de color rojo. Recibió este nombre de la ciudad de Santa Maria (Rio Grande do Sul), Brasil. Esta formación geológica se encuentra en geoparque de paleorrota. El distinguido Inglés paleontólogo Arthur Smith Woodward determinó la edad de la Formación Santa María de la Era Mesozoica, período Triásico Superior (alrededor de doscientos veinte millones de años). (es)
- La formation de Santa Maria est une formation géologique du Trias située dans l'état de Rio Grande do Sul au Brésil. Son âge géologique est à cheval sur une partie du Trias moyen et du Trias supérieur, soit environ entre −245 et −225 Ma (millions d'années). Cette formation a livré une abondante faune fossile de vertébrés, dont les dinosaures Staurikosaurus, Saturnalia, Pampadromaeus, Gnathovorax et Buriolestes, ce dernier ayant été découvert aux côtés du dinosauromorphe Ixalerpeton. (fr)
- The Santa Maria Formation is a sedimentary rock formation found in Rio Grande do Sul, Brazil. It is primarily Carnian in age (Late Triassic), and is notable for its fossils of cynodonts, "rauisuchian" pseudosuchians, and early dinosaurs and other dinosauromorphs, including the herrerasaurid Staurikosaurus, the basal sauropodomorphs Buriolestes and Saturnalia, and the lagerpetid Ixalerpeton. The formation is named after the city of Santa Maria in the central region of Rio Grande do Sul, where outcrops were first studied. The Santa Maria Formation makes up the majority of the Santa Maria Supersequence, which extends through the entire Late Triassic. The Santa Maria Supersequence is divided into four geological sequences, separated from each other by short unconformities. The first two of these sequences (Pinheiros-Chiniquá and Santa Cruz sequences) lie entirely within the Santa Maria Formation, while the third (the Candelária sequence) is shared with the overlying Norian-age Caturrita Formation. The fourth and youngest sequence (the Mata sequence) is equivalent to the Rhaetian-age . The oldest sequence in the formation is the Pinheiros-Chiniquá Sequence (latest Ladinian-earliest Carnian, ~237 Ma), which is biostratigraphically equivalent to the Dinodontosaurus Assemblage Zone. It is followed by the shorter Santa Cruz Sequence (early Carnian-middle Carnian, ~236 Ma), biostratigraphically equivalent to the Santacruzodon Assemblage Zone. The final sequence, which is only partially present within the formation, is the Candelária Sequence (middle Carnian-latest Carnian, ~233-228 Ma). The lower portion of this sequence, coinciding with the upper part of the Santa Maria Formation, is equivalent to the Hyperodapedon Assemblage Zone.The Hyperodapedon Assemblage Zone is itself subdivided into Hyperodapedon Acme Zone (most of the zone, where the rhynchosaur Hyperodapedon is widely reported) and Exaeretodon Zone (restricted to about three known and sampled localities, where rhynchsaurs are almost completely absent, but the traversodontid cynodont Exaeretodon is widely reported). These subdivisions are also known as Lower and Upper Hyperodapedon Assemblage Zone, respectively. U-Pb radiometric dating of a locality in the Upper portion of the Santa Maria Formation found an estimated age of 233.23±0.73 million years ago, putting that locality 1.5 million years older than the Ischigualasto Formation and younger than Los Chañares Formation. The Santa Maria and Ischigualasto formations are approximately equal as having the earliest dinosaur localities. (en)
- Formacja Santa Maria (port. Formação Santa Maria) – formacja geologiczna składająca się ze skał osadowych, występująca w Rio Grande do Sul (Brazylia), w . Jej wiek oceniany jest na późny ladyn – wczesny karnik (trias środkowy – trias górny). (pl)
- A Formação Santa Maria é uma formação geológica com extensão de 250Km que vai do município de Venâncio Aires até o município de Mata, no estado brasileiro do Rio Grande do Sul. Possui datação dos período Triássico (médio e superior), mais especificamente do Ladiniano e Carniano. Recebeu este nome devido a cidade de Santa Maria. Está subdividida em dois membros: Alemoa no topo e Passo das Tropas na base. É composta por lamitos vermelhos. O paleontólogo inglês Arthur Smith Woodward determinou a idade da formação Santa Maria datada da era Mesozóica, período Triássico Superior (aproximadamente duzentos e vinte milhões de anos). A formação Santa Maria está no livros dos recordes, Guinness World Records, como o local mais antigo ao qual dinossauros foram encontrados. A solicitação partiu de um grupo de especialistas e paleontólogos denominado DinOrigin que escava na região desde 1998. (pt)
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- Souvrství Santa Maria je geologická formace na území brazilského státu Rio Grande do Sul. (cs)
- Die Santa-Maria-Formation ist eine lithostratigraphische Formation sedimentären Ursprungs aus der Mittleren Trias des südlichen Brasiliens. Sie gehört zur aus der und damit zur im Paraná-Becken abgelagerten . Die Formation besitzt eine überaus reichhaltige Wirbeltierfauna. (de)
- La Formación Santa María es una formación geológica. El suelo es Lutolita de color rojo. Recibió este nombre de la ciudad de Santa Maria (Rio Grande do Sul), Brasil. Esta formación geológica se encuentra en geoparque de paleorrota. El distinguido Inglés paleontólogo Arthur Smith Woodward determinó la edad de la Formación Santa María de la Era Mesozoica, período Triásico Superior (alrededor de doscientos veinte millones de años). (es)
- La formation de Santa Maria est une formation géologique du Trias située dans l'état de Rio Grande do Sul au Brésil. Son âge géologique est à cheval sur une partie du Trias moyen et du Trias supérieur, soit environ entre −245 et −225 Ma (millions d'années). Cette formation a livré une abondante faune fossile de vertébrés, dont les dinosaures Staurikosaurus, Saturnalia, Pampadromaeus, Gnathovorax et Buriolestes, ce dernier ayant été découvert aux côtés du dinosauromorphe Ixalerpeton. (fr)
- Formacja Santa Maria (port. Formação Santa Maria) – formacja geologiczna składająca się ze skał osadowych, występująca w Rio Grande do Sul (Brazylia), w . Jej wiek oceniany jest na późny ladyn – wczesny karnik (trias środkowy – trias górny). (pl)
- The Santa Maria Formation is a sedimentary rock formation found in Rio Grande do Sul, Brazil. It is primarily Carnian in age (Late Triassic), and is notable for its fossils of cynodonts, "rauisuchian" pseudosuchians, and early dinosaurs and other dinosauromorphs, including the herrerasaurid Staurikosaurus, the basal sauropodomorphs Buriolestes and Saturnalia, and the lagerpetid Ixalerpeton. The formation is named after the city of Santa Maria in the central region of Rio Grande do Sul, where outcrops were first studied. (en)
- A Formação Santa Maria é uma formação geológica com extensão de 250Km que vai do município de Venâncio Aires até o município de Mata, no estado brasileiro do Rio Grande do Sul. Possui datação dos período Triássico (médio e superior), mais especificamente do Ladiniano e Carniano. Recebeu este nome devido a cidade de Santa Maria. Está subdividida em dois membros: Alemoa no topo e Passo das Tropas na base. É composta por lamitos vermelhos. (pt)
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