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Morfología del más antiguo tetrápodo reconstruible Parmastega aelidae
Pavel A Beznosov1, Jennifer A Clack2, Ervīns Lukševičs3
1Institute of Geology, Komi Science Centre, Ural Branch of the Russian Academy of Sciences, Syktyvkar, Russia.
Nature
|October 25, 2019
Resumen
Parmastega aelidae, un tetrápodo devónico temprano de Rusia, ofrece nuevas ideas sobre la evolución de los vertebrados. Este fósil proporciona datos cruciales sobre la anatomía temprana de los tetrápodos y las relaciones evolutivas.
Área de la Ciencia:
- Paleontología
- Biología evolutiva
- Paleontología de los vertebrados
Sus antecedentes:
- La diversidad de tetrápodos del Devónico ha crecido, pero los fósiles son a menudo fragmentarios.
- Los fósiles clave como Ichthyostega y Acanthostega dominan nuestra comprensión de los primeros tetrápodos.
- Los fósiles existentes son más jóvenes que las primeras huellas y fragmentos de tetrápodos.
Objetivo del estudio:
- Para describir un nuevo tetrápodo Famenniano temprano, Parmastega aelidae.
- Para reconstruir el cráneo y el cinturón del hombro de P. aelidae utilizando material 3D.
- Para inferir la posición paleobiológica y filogenética de P. aelidae.
Principales métodos:
- Descripción del material fósil de Rusia.
- Reconstrucción del cráneo y el cinturón del hombro.
- Análisis filogenéticos basados en Bayes y parsimonia.
Principales resultados:
- Parmastega aelidae gen. y sp. Nov. se describe desde el Famenniano más antiguo (aprox. Hace 372 millones de años).
- El material 3D permitió la reconstrucción del cráneo y el cinturón del hombro.
- P. aelidae exhibe características que sugieren un estilo de vida acuático y de crucero por la superficie.
- Los análisis filogenéticos colocan a Parmastega como hermana de todos los demás tetrápodos en la mayoría de los árboles.
Conclusiones:
- Parmastega aelidae representa uno de los tetrápodos más antiguos y basales conocidos.
- Este descubrimiento mejora nuestra comprensión de la evolución y diversificación de los primeros tetrápodos.
- Los hallazgos proporcionan un punto de datos crucial para la transición de la vida acuática a la terrestre.
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