揭示埃迪亚卡兰循环
Matthew S Dodd1,2,3,4,5, Wei Shi1,3, Chao Li6,7,8
1State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu, China.
Nature
|May 31, 2023
概括
海洋水平在埃迪亚卡兰舒拉姆游览期间激增,导致氧气增加. 这表明外部因素如硫酸盐气候变化, 不仅仅是内部循环,
科学领域:
- 地质化学
- 古代海洋学
- 生物地质化学
背景情况:
- 是控制海洋氧气水平的关键营养物质.
- 在埃迪亚卡拉时期,海洋的增加与氧气的增加有关.
- 在这个关键时期的循环仍然不太清楚.
研究的目的:
- 在Ediacaran Shuram旅行 (SE) 期间重建海洋度.
- 在此期间调查海洋氧化的驱动因素.
- 了解,碳同位素和氧气水平之间的关系.
主要方法:
- 来自六个全球部分的碳酸盐相关酸盐 (CAP) 的分析.
- 海洋度的重建.
- 应用一个定量生物地化学模型.
主要成果:
- 在SE期间观察到海洋度的脉冲增加.
- 模型表明有机物氧化和土地气候变化的释.
- 在不同无氧水平下发现了相当的度.
结论:
- 外部刺激,如硫酸盐气候,可能控制了埃迪卡拉海洋的氧化.
- 和氧气循环可能已经脱, 与现代海洋不同.
- 这提供了对大气氧气水平持续上升的洞察力.
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