概括
3400万年前的一次巨大的石撞击可能导致了灭绝,在加勒比海深海核心中发现的富含的沉积物和微矿石证明了这一点.
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:
- 深海沉积物核心提供了地球历史的宝贵档案.
- 古世纪时期经历了重要的地质和生物事件.
- 流星碎片可以用来测定地质事件的日期,并识别撞击坑.
研究的目的:
- 调查大约3400万年前大规模灭绝事件的原因.
- 为了分析加勒比海深海核心中独特的沉积层的组成.
- 为了将地质发现与生物灭绝相关联.
主要方法:
- 沉积物核心分析 沉积物核心分析
- 对丰富的地质化学分析.
- 微铁石的鉴定和年代鉴定
- 对灭绝模式的放射性化石分析.
主要成果:
- 鉴定出一种独特的沉积层,高度丰富于石的化.
- 这层被发现在北美微岩下面,可追溯到3440万年前.
- 层与五种主要的放射性菌物种的灭绝相吻合.
结论:
- 这些发现表明,大约3400万年前发生了巨大的石撞击.
- 撞击事件可能产生了观察到的微构和异常.
- 这一撞击被认为是观察到的Radiolaria大灭绝的原因.
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