西伯利亚陷和Permian-Triassic边界的同步
概括
珀米亚-特里亚斯灭绝事件很可能是由西伯利亚洪水火山活动引起的. 这次大规模的喷发释放了二氧化硫,导致全球变冷和海平面变化,引发了灭绝.
科学领域:
- 地质地质地质地质地质地
- 古生物学的古生物学
- 气候科学 气候科学
背景情况:
- 珀米亚-特里亚斯纪 (P-Tr) 边界标志着一个重要的大规模灭绝事件.
- 西伯利亚陷 (Siberian Traps) 代表了一个与洪水玄武岩火山活动相关的大火性省份.
研究的目的:
- 为了调查诺里尔斯克I入侵的时间,相对于P-Tr边界.
- 测试将西伯利亚洪水火山活动与P-Tr灭绝联系在一起的假设.
主要方法:
- 使用离子探测器测定和的日期.
- 从诺里尔斯克I入侵和P-Tr边界岩中获得的石的地质年代分析.
主要成果:
- 来自诺里尔斯克I入侵的石年龄与P-Tr边界 (在+/- 4百万年内) 的石年龄密切匹配.
- 这些发现支持诺里尔斯克I入侵和西伯利亚陷之间的岩关系.
结论:
- 西伯利亚的洪水火山活动是P-Tr灭绝的可能原因.
- 火山排放 (例如二氧化硫) 可能导致全球变冷,冰盖膨胀,酸雨和海平面波动,导致大规模灭绝.
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