关于在白纪 - 古纪边界的冲击和火山活动
Pincelli M Hull1, André Bornemann2, Donald E Penman3
1Department of Geology and Geophysics, Yale University, New Haven, CT 06511, USA. pincelli.hull@yale.edu.
概括
纪末期的大规模灭绝主要是由石撞击造成的,而不是火山活动. 撞击引发了碳循环的变化,缓解了随后的火山活动造成的极端全球变暖.
科学领域:
- 古生物学
- 气候科学
- 地质学
背景情况:
- 纪末期的大规模灭绝的原因仍在争论中,石撞击和洪岩火山活动都是潜在的驱动因素.
- 关于这些事件的时间及其特定灭绝机制存在不确定性.
研究的目的:
- 确定石撞击与火山活动在白纪末大规模灭绝中的相对重要性.
- 限制火山产生的排气时间及其与撞击和灭绝事件的关系.
主要方法:
- 使用碳循环模型分析潜在的气候场景.
- 综合古气温记录以确定地质事件的时间表.
主要成果:
- 证据表明大火山产生的排气发生在波利德撞击之前.
- 这次撞击与大规模灭绝和碳循环的重大扰动相吻合.
- 由灭绝相关的碳循环变化驱动的海洋二氧化碳吸收限制了灭绝后火山活动的全球变暖.
结论:
- 石撞击,而不是火山活动,是白纪末期大规模灭绝的主要驱动因素.
- 对碳循环的影响对缓解气候变化起到了至关重要的作用.
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