概括
研究人员在比利时Frasnian-Famennian边界附近发现了类似于microtektites的玻璃球体. 它们的特征表明它们的撞击起源,可能将这一事件与上代沃龙纪大规模灭绝联系起来.
科学领域:
- 地质地质地质地质地质地
- 古生物学的古生物学
- 行星科学 行星科学
背景情况:
- 弗拉斯尼亚-法门尼亚 (F/F) 边界标志着在上德沃尼亚时期发生的一次重大海洋大规模灭绝事件.
- 微型石通常与大型撞击事件有关.
研究的目的:
- 调查在比利时Senzeilles的F/F边界附近发现的玻璃球体的起源和意义.
- 评估外星撞击与F/F大灭绝之间的潜在联系.
主要方法:
- 玻璃球体的形态分析.
- 球体组成的地质化学分析.
- 与已知的微铁克石和冲击结构进行比较.
主要成果:
- 在Senzeilles发现的玻璃球体表现出类似微铁的形态 (滴,子,复合物).
- 这些球体缺乏结晶体,只有很少的囊泡,并且具有较低的挥发性物质含量,与撞击喷射相一致.
- 有类似年龄的候选撞击坑存在 (Siljan Ring,Charlevoix).
结论:
- 森赛尔球体的特点强烈支持撞击起源.
- 在F/F边界附近存在这些类似微铁石的球体,为撞击事件提供了证据.
- 这次撞击事件是上代沃纪大规模灭绝的潜在原因.
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