亚洲尘埃沉积流向亚北极太平洋,估计使用单个石英颗粒
Kana Nagashima1, Hajime Kawakami2, Koji Sugie3
1Research Institute for Global Change, Japan Agency for Marine-Earth Science and Technology, Yokosuka, Japan. nagashimak@jamstec.go.jp.
Scientific reports
|September 29, 2023
概括
亚洲的尘埃对海洋的铁供应产生了重大影响,特别是在西亚北极太平洋. 这项研究量化了尘埃沉积,揭示了其在支持海洋生态系统和碳循环中的关键作用.
科学领域:
- 海洋生物地质化学海洋生物地质化学
- 海洋学 海洋学 海洋学
- 环境科学环境科学
背景情况:
- 铁的可用性是限制海洋生态系统生产力的关键因素,在广的海洋地区.
- 了解铁的来源和季节性供应对于理解表面海洋生物地球化学和碳循环至关重要.
- 西亚北极太平洋是高营养,低叶绿素的地区,夏季植物浮游生物的铁量受到限制.
研究的目的:
- 为了确定亚洲尘埃在西亚北极太平洋的季节性沉积流.
- 用先进的分析技术追踪尘埃颗粒的来源.
- 估计来自尘埃的铁对表面海洋生产力的贡献.
主要方法:
- 扫描电子显微镜-单个石英颗粒的阴极光发光分析.
- 分析2003年至2022年期间从西亚北极太平洋收集的尘埃样本.
- 从尘埃沉积中计算溶解铁流量,并与垂直铁供应进行比较.
主要成果:
- 在五月,六月和七月初观察到亚洲尘埃的高沉积流量 (高达6.9毫克米-2天-1).
- 年平均尘埃沉积流量为1.0 ± 0.2 mg m−2天−1.1.
- 在高生产季节 (四月至七月) 中,来自亚洲尘埃的溶铁流量为0.9 ± 0.3μg m−2 day−1,约占来自深海来源的供应的一半.
结论:
- 亚洲尘埃是西亚北极太平洋表面海洋铁的重要来源.
- 该研究提供了一种可靠的方法来估计来自尘埃的铁供应.
- 这种铁供应对于维持生物生产力至关重要,特别是在未来的海洋分层情景下.
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