与南极洲的珀米亚-三叠纪边界相关的体石碎片
Asish R Basu1, Michail I Petaev, Robert J Poreda
1Department of Earth and Environmental Sciences, University of Rochester, Rochester, NY 14627, USA. abasu@earth.rochester.edu
概括
在南极的波斯末期岩石中发现了地质石碎片,与在中国发现的岩石相匹配. 这支持了在珀米亚-特里亚斯纪边界发生全球冲击事件的理论.
科学领域:
- 地质地质地质地质地质地
- 宇宙化学 宇宙化学
- 古生物学的古生物学
背景情况:
- 珀米亚-特里亚斯纪的边界标志着一个重要的大规模灭绝事件.
- 石撞击是大规模环境变化的潜在触发因素.
- 以前的发现表明,在这个边界处可能发生撞击事件.
研究的目的:
- 为了分析在南极沉积岩中发现的石碎片.
- 将南极发现与全球类似的地质记录进行比较.
- 为了评估证据,在米-三叠纪边界的全球冲击事件.
主要方法:
- 对石碎片进行地质化学分析.
- 对金属颗粒,橄,氧化物,氧化物和氧化物的矿物学检查.
- 化学和同位素比率与已知的石类型 (CM型石) 的比较.
主要成果:
- 在南极洲石墨峰 (Graphite Peak) 的波斯纪末期沉积岩中发现了多个CM型的体石碎片.
- 碎片中的金属颗粒和酸盐矿物质的化学组成与CM型地质相一致.
- 离散的金属颗粒,类似于在中国的Meishan发现的,也存在于一个南极样本.
结论:
- 在南极洲发现CM型的体石,为在波斯纪末期外星物质沉积提供了进一步的证据.
- 这些发现支持了围绕波斯-三叠纪边界发生的全球冲击事件的假设.
- 这一事件可能导致了环境变化,导致了波斯纪末期的大规模灭绝.
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