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An extraterrestrial trigger for the Early Cretaceous massive volcanism? Evidence from the paleo-Tethys Ocean

机译:是白垩纪早期大规模火山爆发的外星触发因素?来自古特提斯海洋的证据

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摘要

The Early Cretaceous Greater Ontong Java Event in the Pacific Ocean may have covered ca. 1% of the Earth's surface with volcanism. It has puzzled scientists trying to explain its origin by several mechanisms possible on Earth, leading others to propose an extraterrestrial trigger to explain this event. A large oceanic extraterrestrial impact causing such voluminous volcanism may have traces of its distal ejecta in sedimentary rocks around the basin, including the paleo-Tethys Ocean which was then contiguous with the Pacific Ocean. The contemporaneous marine sequence at central Italy, containing the sedimentary expression of a global oceanic anoxic event (OAE1a), may have recorded such ocurrence as indicated by two stratigraphic intervals with 187Os/188Os indicative of meteoritic influence. Here we show, for the first time, that platinum group element abundances and inter-element ratios in this paleo-Tethyan marine sequence provide no evidence for an extraterrestrial trigger for the Early Cretaceous massive volcanism.
机译:太平洋上的白垩纪早期的大昂通爪哇事件可能已经覆盖了大约2009年。 1%的地球表面带有火山作用。它使试图通过地球上几种可能的机制来解释其起源的科学家感到困惑,导致其他人提出了一个外星触发来解释这一事件。造成这种巨大火山作用的巨大海洋外星撞击可能在盆地周围的沉积岩石中包括其远侧顶出的痕迹,包括古特提斯海洋,然后与太平洋毗连。意大利中部的同期海相序列可能包含全球性海洋缺氧事件(OAE1a)的沉积物表达,可能已记录到这种发生,如两个地层间隔所指示的187Os / 188Os代表了气象学影响。在这里,我们首次显示,在这个古特提斯海洋序列中,铂族元素的丰度和元素间比率没有提供任何证据表明白垩纪早期大规模火山活动是由外星触发的。

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