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Updated: Jul 11, 2026

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Isolation of Quartz Grains for Optically Stimulated Luminescence (OSL) Dating of Quaternary Sediments for Paleoenvironmental Research
Published on: August 2, 2021
Cuarzo sacudido en el límite triásico-jurásico en Italia
Resumen
Se produjeron múltiples impactos al final del período Triásico, evidenciado por granos de cuarzo chocado encontrados en lechos de esquisto italiano. Estos impactos coinciden con la extinción de la fauna de los Rhaetavicula.
Área de la Ciencia:
- Geología Geología Geología.
- Paleontología Paleontología.
- Ciencias planetarias Ciencias planetarias.
Sus antecedentes:
- El evento de extinción de finales del Triásico es una gran extinción masiva.
- Comprender los desencadenantes de esta extinción es crucial para las reconstrucciones paleoclimáticas y paleoambientales.
Objetivo del estudio:
- Para investigar posibles eventos de impacto en el límite Triásico-Jurásico.
- Para analizar el cuarzo de choque en formaciones geológicas italianas.
Principales métodos:
- Examen microscópico de granos de cuarzo para las características de deformación plana.
- Análisis estratigráfico de los lechos de esquisto en los Apeninos del Norte.
- Análisis petrográfico de cuarzo sacudido.
Principales resultados:
- Grano de cuarzo metamorfoseado por choque identificado en tres capas de esquisto distintas.
- Características de deformación plana observadas en el 5-10% de los granos de cuarzo.
- La posición estratigráfica de las capas de cuarzo sacudido se correlaciona con la terminación de la fauna de Rhaetavicula.
Conclusiones:
- La evidencia sugiere al menos tres eventos de impacto muy espaciados al final del Triásico.
- Estos impactos pueden haber contribuido a los cambios ambientales en el límite Triásico-Jurásico.
- Se necesitaban más investigaciones para confirmar el origen extraterrestre y el momento preciso de los impactos.
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