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  1. Home
  2. El Tallo Cecílico Triásico Apoya El Origen Disorófobo De Los Anfibios Vivos.
  1. Home
  2. El Tallo Cecílico Triásico Apoya El Origen Disorófobo De Los Anfibios Vivos.

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El tallo cecílico triásico apoya el origen disorófobo de los anfibios vivos.

Ben T Kligman1,2, Bryan M Gee3, Adam D Marsh4

  • 1Department of Resource Management and Science, Petrified Forest National Park, Petrified Forest, AZ, USA. bkligman@vt.edu.

Nature
|January 25, 2023

Ver abstracta en PubMed

Resumen
Este resumen es generado por máquina.

Los caecilianos fósiles del Triásico tardío extienden el registro fósil en 35 millones de años. Estos descubrimientos revelan la evolución temprana de los anfibios y apoyan un solo origen para los anfibios vivos dentro de los temnospondilos disorófobos.

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Área de la Ciencia:

  • Paleontología
  • Biología evolutiva
  • Zoología de los vertebrados

Sus antecedentes:

  • Las relaciones evolutivas y el registro fósil de Lissamphibia (ranas, salamandras y caecilianos) se entienden incompletamente, particularmente para los caecilianos (Gymnophiona).
  • La evidencia fósil anterior para los lisanfibios de la corona se remonta principalmente al período Triásico, con una notable falta de fósiles caecilianos tempranos que dificultan las interpretaciones filogenéticas.

Objetivo del estudio:

  • Para describir el ceciliano de tallo geológicamente más antiguo conocido, un lisanfibio de corona del Triásico tardío de Arizona.
  • Para aclarar la evolución morfológica y funcional temprana de los caecilianos y sus afinidades filogenéticas.

Principales métodos:

  • Excavación paleontológica y análisis de restos fósiles.
  • Análisis morfológico comparativo con anfibios y tetrápodos existentes y fósiles.
  • Inferencia filogenética basada en datos morfológicos.
  • Principales resultados:

    • Descubrimiento del tallo ceciliano más antiguo, extendiendo el registro fósil ceciliano en aproximadamente 35 millones de años.
    • Los fósiles exhiben un mosaico de características y rasgos cecilianos únicos compartidos con los batraquios y los temnospondilos disorófobos.
    • La evidencia sugiere una adquisición tardía de adaptaciones fósiles especializadas en los primeros caecilianos.

    Conclusiones:

    • Los hallazgos proporcionan evidencia convincente de un único origen de los anfibios vivos dentro de los temnospondilos disorófobos.
    • La distribución biogeográfica de los caecilianos modernos puede reflejar tanto los rasgos funcionales / fisiológicos conservados como la vicarianza tectónica de placas.
    • Este descubrimiento mejora significativamente nuestra comprensión de los orígenes de los lisanfibios y la evolución temprana de los tetrápodos.