代海水硫酸盐的硫同位素组成
1A. Paytan, M. Kastner, and D. Campbell are in the Geosciences Research Division, Scripps Institution of Oceanography, 9500 Gilman Drive, La Jolla, CA 92093, USA. M. H. Thiemens is in the Chemistry Department, University of California, San Dieg.
概括
这项研究呈现了纪海水硫酸硫同位素曲线,揭示了数百万年来的显著变化. 研究结果表明,硫和碳循环不仅仅控制了大气中的氧气在Cenozoic.
科学领域:
- 地质化学 地质化学
- 古海洋学是古海洋学.
- 同位素地球化学 同位素地球化学
背景情况:
- 了解代硫循环对于重建过去的海洋条件和大气组成至关重要.
- 海洋巴里特作为海水硫酸盐同位素组成的宝贵档案.
研究的目的:
- 为了生成一个高分辨率的硫同位素曲线为Cenozoic海水硫酸盐.
- 研究硫和碳循环之间的关系及其对大气氧气水平的影响.
主要方法:
- 分析海洋巴里特样本以确定硫同位素组成.
- 产生的硫同位素曲线与现有的海洋碳酸盐碳同位素记录的比较.
主要成果:
- 一个详细的Cenozoic海水硫酸硫同位素曲线 (大约. 一百万年决议) 成立.
- 曲线显示了从65-55万年前的下降,从55-45万年前的急剧增长,从35-2万年前的稳定,以及最近的下降.
- 在数百万年的硫和碳循环之间没有发现明确的系统合.
结论:
- 化硫和有机碳埋葬率的变化不仅仅是在简短的代时间尺度上决定大气中的氧气.
- 这些发现影响了大气氧气调节模型和纪气候动态.
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