海洋循环的矿物学控制
Lena Chen1, Autum R Downey2, Corey Archer3
1School of Earth and Environment, University of Leeds, Leeds, LS2 9JT, UK. lena.chen@bristol.ac.uk.
Nature communications
|August 15, 2025
概括
矿物质通过吸附和结合过程影响海洋沉积物中的 (Ni) 同位素组成. 矿物质老化和转化释放更重的Ni同位素,影响海水档案和金属同位素代理.
科学领域:
- 地质化学 地质化学
- 海洋科学 海洋科学
- 古代海洋学 古代海洋学 古代海洋学
背景情况:
- 过渡金属同位素是宝贵的古生产力代理物.
- 了解沉积物和海水之间的金属循环对于代理实用性至关重要.
- 在海洋沉积物中 (Ni) 同位素的行为需要进一步调查.
研究的目的:
- 阐明 (Mn) 矿物质在控制氧化海洋沉积物中Ni同位素组成中的作用.
- 研究在Mn矿物质老化和转化过程中Ni同位素分离的机制.
- 评估矿工艺对海水的影响 同位素记录.
主要方法:
- 合成和天然海洋沉积物样本的分析.
- 模拟沉积物生成过程的模拟.
- 同位素质量平衡计算以建模海水的Ni同位素灵敏度.
主要成果:
- 富含Mn沉积物的Ni同位素变异性主要通过对Mn氧化物的吸附和结构性纳入来控制.
- 这些结合机制在Mn矿物质的老化和转化过程中演变.
- 同位素重的Ni在Mn矿物转化过程中优先释放.
结论:
- Mn矿物质的衰老和转化过程共同修改了沉积物和海水的Ni同位素组成.
- Mn矿物过程对于解释Ni同位素数据作为古生产力代理来说至关重要.
- 这些发现对理解与Mn矿物形成相结合的其他金属同位素代理物有影响.
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