概括
地质记录显示,被沉积了数千年,而不是瞬间沉积. 证据表明火山活动,而不是小行星撞击,导致了这些末纪环境事件.
科学领域:
- 地质化学 地质化学
- 古生物学的古生物学
- 火山学 火山学是一门学科.
背景情况:
- 末纪时期的环境发生了重大变化.
- 在地质记录中发现的和相关元素的起源一直在争论中.
- 区分撞击事件和火山活动对于理解过去的灭绝至关重要.
研究的目的:
- 分析和相关元素的沉积时间框架.
- 为了确定这些元素的起源 (地幔与石).
- 评估小行星撞击与火山事件的可能性,以此作为终极白时期环境变化的原因.
主要方法:
- 地质记录分析地质记录分析
- 基本沉积分析的基本沉积分析
- 地质层的时间表约会.
主要成果:
- 和相关元素在一万到十万年的时间里沉积起来.
- 地质证据支持这些元素的地幔起源.
- 这些发现与剧烈火山活动的场景一致,而不是单一的小行星撞击.
结论:
- 和相关元素的沉积并不是瞬间发生的.
- 火山活动被认为是这些元素的来源.
- 一系列的火山事件,而不是小行星撞击,可能导致了末端白时期的环境变化.
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