Kaiho Kunio, Oshima Naga
Department of Earth Science, Graduate School of Science, Tohoku University, Sendai, 980-8578, Japan.
Meteorological Research Institute, Tsukuba, 305-0052, Japan.
Sci Rep. 2017 Nov 9;7(1):14855. doi: 10.1038/s41598-017-14199-x.
Sixty-six million years ago, an asteroid approximately 9 km in diameter hit the hydrocarbon- and sulfur-rich sedimentary rocks in what is now Mexico. Recent studies have shown that this impact at the Yucatan Peninsula heated the hydrocarbon and sulfur in these rocks, forming stratospheric soot and sulfate aerosols and causing extreme global cooling and drought. These events triggered a mass extinction, including dinosaurs, and led to the subsequent macroevolution of mammals. The amount of hydrocarbon and sulfur in rocks varies widely, depending on location, which suggests that cooling and extinction levels were dependent on impact site. Here we show that the probability of significant global cooling, mass extinction, and the subsequent appearance of mammals was quite low after an asteroid impact on the Earth's surface. This significant event could have occurred if the asteroid hit the hydrocarbon-rich areas occupying approximately 13% of the Earth's surface. The site of asteroid impact, therefore, changed the history of life on Earth.
六千六百万年前,一颗直径约9公里的小行星撞击了如今墨西哥境内富含碳氢化合物和硫的沉积岩。最近的研究表明,这次在尤卡坦半岛的撞击使这些岩石中的碳氢化合物和硫升温,形成了平流层烟尘和硫酸盐气溶胶,并导致了全球极端降温与干旱。这些事件引发了包括恐龙在内的大规模物种灭绝,并导致了随后哺乳动物的宏观进化。岩石中碳氢化合物和硫的含量因地点而异,差异很大,这表明降温程度和灭绝程度取决于撞击地点。我们在此表明,小行星撞击地球表面后,导致全球显著降温、大规模物种灭绝以及随后哺乳动物出现的可能性相当低。如果小行星撞击了占地球表面约13%的富含碳氢化合物的区域,那么这一重大事件就有可能发生。因此,小行星撞击的地点改变了地球的生命史。