现代海洋沉积物中同位素信号的全球模式和驱动因素
Xueshi Sun1, Dejiang Fan2,3, Limin Hu2,3
1College of Marine Geosciences, Key Laboratory of Submarine Geosciences and Prospecting Techniques, Ocean University of China, Qingdao, China. sunxueshi@ouc.edu.cn.
Nature communications
|November 25, 2025
概括
全球海洋沉积物显示同位素 (δ15N) 的百年增长,表明输入增加和加速脱. 然而,河流输入可以改变沿海地区的信号.
科学领域:
- 海洋地质化学海洋地质化学
- 海洋学 海洋学 海洋学
- 生物地质化学循环是什么
背景情况:
- 海洋循环对于海洋生产力至关重要,并通过同位素比 (δ15N) 记录.
- 使用 δ15N 量化海洋循环的空间和时间变化是具有挑战性的.
- 需要一个全球沉积物 δ15N 数据库来了解过去的变化.
研究的目的:
- 创建一个全面的海洋沉积物的全球数据库 δ15N.
- 分析海洋气循环的百年级变化.
- 为了研究沉积 δ15N 和输入/损失过程之间的关系.
主要方法:
- 汇编了超过8400个海底沉积物样本,用于全球数据库.
- 从沉积物核心开发148个时间序列,涵盖了上个世纪.
- 对散装沉积物 δ15N 的分析,以推断气循环的动态.
主要成果:
- 沉积物 δ15N 主要反映有机物质,无机有着显著的作用.
- 观察到沉积物 δ15N 的全球增加 (平均每世纪1.3 ‰).
- 这种增加与丰富相关,表明外部投入,生产率和脱率增加.
结论:
- 沉积 δ15N 为重建过去的海洋循环提供了有价值的代理.
- 百年规模的缩和加速的脱是沿海海洋中普遍存在的.
- 陆地输入,特别是来自河流的输入,可以修改沉积物记录中的δ15N信号.
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