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在白纪/三级纪边界点燃全球野火
H J Melosh1, N M Schneider, K J Zahnle
1Lunar and Planetary Laboratory, University of Arizona, Tucson 85721, USA.
Nature
|January 18, 1990
概括
纪古时期的灭绝事件可能是由小行星撞击引发全球野火的事件引发的. 从撞击中重新进入的喷射物激烈地加热了地球,可能导致广泛的火灾和伤害动物.
科学领域:
- 地质科学 地质科学
- 行星科学 行星科学
- 古生物学的古生物学
背景情况:
- 有证据表明,小行星或彗星撞击结束了白纪.
- 在白纪和三级纪的边界处,全球一层烟尘层表明森林大火蔓延.
研究的目的:
- 调查冲击事件可能引发全球野火的机制.
- 为了量化由撞击喷射物重新进入产生的热辐射.
主要方法:
- 从重新进入撞击喷射物中建模热辐射流.
- 与太阳能输入相比,估计全球辐射的增加.
主要成果:
- 重新进入的喷射物可以增加全球热辐射50-150倍的太阳输入.
- 这种强烈的辐射持续了一到几个小时.
结论:
- 撞击喷射的热辐射提供了一个引发全球野火的可信机制.
- 这种现象可能导致了白纪古时期的灭绝事件,并损害了不受保护的生命.
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