海洋环境的晚期古老生态氧化得到了多洛米特U-Pb的支持
Michal Ben-Israel1,2, Robert M Holder3, Lyle L Nelson4,5
1The The Fredy & Nadine Herrmann Institute of Earth Sciences, The Hebrew University of Jerusalem, Jerusalem, Israel.
Nature communications
|April 3, 2024
概括
一种新的多洛米特U-Pb地球时间学方法重建了过去的海洋U/Pb比率. 这揭示了古老时代晚期海洋氧化增加,支持进化驱动的海洋变化.
科学领域:
- 地质化学 地质化学
- 古海洋学是古海洋学.
- 地质时间学 (Geochronology)
背景情况:
- 重建海洋氧气水平对于理解进化和海洋学至关重要.
- 通常使用的是对氧化回收敏感的地化学代理,但需要可靠的校准.
研究的目的:
- 开发一种使用多洛米特U-Pb地质年代学来重建海水U/Pb比率的新型代理.
- 建立一种用于评估过去海洋氧化水平的新方法.
主要方法:
- 利用多洛米特U-Pb地质年代学分析U-Pb日期和初始的207Pb/206Pb比率.
- 解释了U-Pb系统中的偏差,作为沉积过程中对氧化还原敏感的U/Pb比率的函数.
- 重建的海水U/Pb比率基于多洛米特地质年代学数据.
主要成果:
- 多洛米特样本给出了U-Pb日期和初始的207Pb/206Pb比率,这些比率与预期的地层学年龄有所不同.
- 这些偏差归因于U-Pb系统的存款后重置.
- 重建的初始U/Pb比率显示,在古老时代晚期出现了显著的增加.
结论:
- /Pb比率的增加表明,在古老时代晚期,海洋环境的氧化增强.
- 这些发现与其他氧化还原代理数据一致,并支持进化驱动的海洋氧化.
- 这表明,与今天相比,早期的动物生活存在于历史上氧气有限的海洋中.
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