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Evolução dos Toxodontia da América do Sul durante o Cenozoico: aspectos dentários, paleoclimáticos e paleoambientais
Reconstrução de uma manada de Aelosaurus maximus com indivíduos de idades variadas (Pintura de Ariel Milani Martine).
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Palavras-chave

Cenozoico. Mudanças paleoambientais. Mudanças paleoclimáticas. Notoungulata. Paleohistologia dentária.

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BRAUNN, Patrícia Rodrigues; RIBEIRO, Ana Maria. Evolução dos Toxodontia da América do Sul durante o Cenozoico: aspectos dentários, paleoclimáticos e paleoambientais. Terrae Didatica, Campinas, SP, v. 13, n. 2, p. 127–145, 2017. DOI: 10.20396/td.v13i2.8650100. Disponível em: https://periodicos.sbu.unicamp.br/ojs/index.php/td/article/view/8650100. Acesso em: 25 abr. 2024.

Resumo

Os notoungulados são ungulados nativos sul-americanos registrados do Paleoceno ao Pleistoceno, e cuja diversidade declinou drasticamente durante o Plioceno, alcançando a América Central e América do Norte durante o Pleistoceno. Notoungulados evoluíram sob influência climática e ambiental, de linhagens arcaicas, com sistema mastigatório generalizado, com dentição completa, sem diastema, com molares e pré-molares braquiodontes, a formas especializadas com incisivos hipertrofiados, padrões oclusais da coroa simplificados e formas proto-hipsodontes e eu-hipsodontes. Estas comunidades viveram primeiramente em hábitats florestais quentes e úmidos, e posteriormente, em pastagens relativamente temperadas de hábitats abertos, com forte tendência à aridização e ao resfriamento ao longo do Cenozoico. Além da evolução da morfologia macroscópica dentária observada em Notoungulata, também é possível evidenciar a evolução dos tipos de microestrutura do esmalte, através da presença de características mais derivadas em formas eu-hipsodontes, indicando adaptação funcional e conferindo maior resistência ao consumo de vegetação mais abrasiva.
https://doi.org/10.20396/td.v13i2.8650100
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