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在五次大规模灭绝期间全球气候变化的机制
1Department of Earth Science, Graduate School of Science, Tohoku University, Sendai, 980- 8578, Japan. kunio.kaiho.a6@tohoku.ac.jp.
Scientific reports
|May 12, 2025
概括
大规模灭绝与气候变化有关. 火山活动和石撞击导致了最初的冷却,随后是变暖,推动了灭绝事件.
科学领域:
- 古气候学 古气候学
- 地质化学 地质化学
- 古生物学的古生物学
背景情况:
- 自坎布里亚时代爆发以来,发生了五次大规模灭绝,每一次都与显著的气候变化有关.
- 奥尔多维纪灭绝,第一个和最不了解的灭绝,是这项研究的重点.
- 了解灭绝触发因素对于预测未来的生物多样性危机至关重要.
研究的目的:
- 为了研究气候异常和奥尔多维纪灭绝事件之间的关系.
- 分析主要灭绝事件的两个阶段性质.
- 确定火山活动和石撞击在引发大规模灭绝中的作用.
主要方法:
- 对奥尔多维纪时期的沉积物有机分子的分析.
- 应用冠指数来评估沉积岩中的热异常.
- 将五个主要的灭绝事件分类为十个不同的阶段 (每个事件两个).
主要成果:
- 五分之四的大型灭绝始于全球变冷,并以全球变暖结束.
- 灭绝的初始阶段涉及不同温度的热异常 (低,中等,高).
- 随后的变暖阶段始终表现出中等温度加热.
结论:
- 火山喷发和石撞击可能释放了平流层的SO2或烟尘,导致全球初始冷却和灭绝.
- 随后碳化合物和碳酸盐的温和加热释放了二氧化碳,导致了长期的全球变暖和二次灭绝.
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