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Formación Sarmiento

La Formación Sarmiento ( en español : Formación Sarmiento ), en la literatura más antigua descrita como Formación Casamayor , es una formación geológica en la provincia de Chubut , Argentina , en la Patagonia central , que abarca alrededor de 30 millones de años desde mediados del Eoceno hasta principios del Mioceno . Se compone predominantemente de depósitos piroclásticos , [1] que se depositaron en un ambiente semiárido . [2] Se divide en varios miembros. [1] La diversa fauna de la Formación Sarmiento, que incluye una variedad de aves, cocodrilos, tortugas y serpientes, también incluye muchos mamíferos como ungulados nativos sudamericanos ( notoungulados , litopternos , astrapotheres ), así como armadillos y roedores caviomorfos . [3]

Paleofauna

Anfibios

Pájaros

Reptiles

Crocodilomorfos

Lepidosaurios

Testudinas

Mamíferos

Meridiolestidanos

Meridiungulados

Xenartros

Metaterianos

Roedores

Primates

Murciélagos

Referencias

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