盆地规模重建欧基尼亚和晚代纪大规模灭绝
Swapan K Sahoo1, Geoffrey J Gilleaudeau2, Kathleen Wilson3
1Equinor US, Houston, TX, USA. swas@equinor.com.
Nature
|March 8, 2023
概括
由于植物进化和海洋变化,纪-碳纪过渡期发生了环境变化. 有毒的硫化水扩散到浅海导致了纪晚期的灭绝,
科学领域:
- 古代海洋学
- 地质化学
- 古生物学
背景情况:
- 代 - 碳期过渡是一个显著的环境变化时期,以海洋 - 大气氧化状态的转变为标志.
- 影响这些变化的因素包括血管陆地植物的繁殖,冰川衰退,缩和大规模灭绝事件.
研究的目的:
- 编制和分析来自巴肯页岩的综合地化学数据,以了解纪-碳期过渡时期的环境动态.
- 记录eocinic水域的过渡及其对德纪晚期灭绝事件的影响.
主要方法:
- 从90个沉积物中收集的地化学数据的空间和时间编制.
- 对海洋学条件重建的地化学代理物进行分析,特别是 euxinia (硫化的存在).
主要成果:
- 详细记录有毒海水逐步进入浅海环境的情况.
- 这些违规事件与多次德纪晚期灭绝事件的相关性.
结论:
- 由于硫化的毒性,浅水eocinia的扩张是纪晚期大规模灭绝的主要因素.
- 这一发现表明硫化的毒性是整个世生物多样性丧失的关键驱动因素.
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