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Rapida formación de la meseta de Java de Ontong por el manto Aptiano pluma de volcanismo
Resumen
La meseta de Ontong Java (OJP) se formó rápidamente durante el Aptiano temprano, probablemente debido a una pluma del manto. Su formación puede haber causado el aumento del nivel del mar y la anoxia oceánica, contribuyendo al clima de invernadero del Cretácico sin grandes extinciones.
Área de la Ciencia:
- Geofísica y paleoclimatología.
- Tectónica de placas y volcanismo.
Sus antecedentes:
- La meseta de Ontong Java (OJP) es una de las mayores grandes provincias ígneas de la Tierra.
- Comprender el momento y los mecanismos de su formación es crucial para comprender el clima y los eventos oceanográficos del Cretácico.
Objetivo del estudio:
- Para determinar con precisión el momento en que OJP inundó el basalto volcánico.
- Investigar las tasas de emplazamiento y el posible origen del penacho del manto de la OJP.
- Evaluar las consecuencias ambientales de la formación de OJP, incluidos los cambios en el nivel del mar, la anoxia oceánica y los impactos climáticos.
Principales métodos:
- Análisis de datos paleomagnéticos para establecer un marco de edad preciso.
- Interpretación de datos paleontológicos para la correlación estratigráfica y la datación.
- Modelado geofísico para inferir las tasas de emplazamiento de la corteza terrestre y la dinámica del penacho.
Principales resultados:
- La mayoría de la formación de OJP ocurrió rápidamente, en un lapso de 3 millones de años, durante el Aptiano temprano.
- Las tasas de emplazamiento de la corteza eran significativamente más altas que las de las trampas del Decán.
- La rápida formación es consistente con el impacto de una gran cabeza de penacho del manto en la base de la litosfera oceánica.
Conclusiones:
- La formación de OJP fue un evento rápido impulsado por la actividad de la pluma del manto.
- El volcanismo de OJP probablemente desencadenó un aumento global del nivel del mar e indujo una anoxia oceánica generalizada.
- Si bien contribuyó al clima de efecto invernadero del Cretácico medio, la formación de OJP no causó grandes extinciones biológicas.
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