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Evidências da origem e ascensão dos dinossauros sauropodomorfos preservadas em leitos fossilíferos do Triássico do Sul do Brasil
Entrada monumental da Gruta do Lago Azul, ricamente ornamentada por estalactites e estalagmites, situada no município de Bonito, a E da Serra da Bodoquena e a sudoeste do município de Miranda. A região serrana foi edificada em unidades carbonáticas dos grupos Cuiabá e Corumbá, de idade Neoproterozoica. Fotografia: Adriano Gambarini.
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Palavras-chave

Sauropodomorpha
Dinosauria
Evolução
Era Mesozoica
Saurischia

Como Citar

MÜLLER, Rodrigo Temp; GARCIA, Maurício Silva; SILVA, Sérgio Dias da. Evidências da origem e ascensão dos dinossauros sauropodomorfos preservadas em leitos fossilíferos do Triássico do Sul do Brasil. Terrae Didatica, Campinas, SP, v. 16, p. e020013, 2020. DOI: 10.20396/td.v16i0.8657367. Disponível em: https://periodicos.sbu.unicamp.br/ojs/index.php/td/article/view/8657367. Acesso em: 20 abr. 2024.

Resumo

Embora o grupo dos dinossauros sauropodomorfos seja amplamente conhecido em virtude dos gigantescos saurópodes, sua origem ainda é pouco compreendida em virtude da escassez de esqueletos completos ou datações precisas. Entretanto, novos achados e datações realizadas em rochas Triássicas do Brasil têm trazido à tona informações valiosas no que tange essa questão. A combinação desses novos dados com técnicas mais avançadas de investigação (e.g. tomografias computadorizadas) vem possibilitando o estabelecimento dos padrões macroevolutivos que direcionaram a evolução inicial do grupo. Por meio das descobertas realizadas nos leitos Triássicos do Rio Grande do Sul, podemos entender de forma mais refinada de que forma os sauropodomorfos passaram de animais pequenos e pouco abundantes aos maiores animais que já andaram sobre a Terra.

https://doi.org/10.20396/td.v16i0.8657367
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