氧化和性驱动了过去32亿年来湖的同位素记录
Diana Velazquez1, Nathan D Sheldon1, Michael T Hren2
1Department of Earth and Environmental Sciences, University of Michigan, Ann Arbor, Michigan, USA.
Geobiology
|September 18, 2025
概括
这项研究揭示了氧气水平和pH值如何影响湖泊沉积物中的和碳同位素. 淡水同位素记录追踪了微生物进化,而不是直接追踪大气氧化事件.
科学领域:
- 地质化学 地质化学
- 古气候学 古气候学
- 微生物生态学 微生物生态学
背景情况:
- 前坎布里亚时代的氧化极大地改变了地球的碳和循环.
- 与海洋环境相比,湖 (湖泊) 环境对营养循环演变的研究不足.
研究的目的:
- 为了研究水柱氧对现代湖中的沉积碳 (δ13Corg) 和 (δ15N) 同位素的影响.
- 用现代数据解释过去的湖 δ15N记录在大气氧化的背景下.
主要方法:
- 现代湖泊沉积物数据集的编制和分析.
- 在不同氧气和pH条件下检查沉积 δ13Corg和 δ15N值.
- 现代同位素图案与古代湖 δ15N 记录的比较.
主要成果:
- 已建立的值为d13Corg用于氧化/无毒条件和d15N用于环中性/性pH.
- 拉库斯特林 δ15N 显示了与有氧代谢途径相关的逐渐增加,而不是直接的氧化事件.
- 在性湖泊 (古老和现代) 中,富含的 δ15N 值 (>+10‰) 作为基本性代理值.
结论:
- 湖 δ15N 记录反映了微生物代谢和沉积环境条件的演变.
- 湖泊中循环的反应不同于直接的大气氧化信号.
- 沉积态同位素提供了关于前剑桥纪和罗纪环境变化的见解.
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