从2022年Hunga Tonga-Hunga Ha'apai喷发到南太平洋的大量微量金属输入
Zhouling Zhang1, Antao Xu2,3, Ed Hathorne2
1GEOMAR Helmholtz Centre for Ocean Research Kiel, Kiel, Germany. zzhang@geomar.de.
Nature communications
|October 17, 2024
概括
2022年洪加通加-洪加哈帕伊火山爆发对南太平洋生物地质化学产生了重大影响. 火山喷射物提供了必需的营养,可能刺激海洋生物和改变海洋化学.
科学领域:
- 海洋学 海洋学 海洋学
- 海洋生物地质化学海洋生物地质化学
- 火山学 火山学是一门学科.
背景情况:
- 2022年1月的洪加通加 - 洪加哈帕伊 (HTHH) 喷发将大量的喷射物释放到南太平洋.
- 了解这种大规模火山事件的生物地质化学后果对于海洋生态系统健康至关重要.
研究的目的:
- 调查HTHH火山爆发对南太平洋旋流 (SPG) 生物地质化学的影响.
- 量化从喷发中释放到海洋环境中的和铁等关键元素的数量.
主要方法:
- 在GEOTRACES GP21巡航 (2022年2月至4月) 期间采集的地表水样本的分析.
- 测量新同位素和稀土元素组合物.
- 评估微量金属度和叶绿素-a库存.
主要成果:
- 在西的SPG中观察到对新同位素和稀土元素的重大火山影响,可能会到达东部地区.
- 检测到增加的微量金属度和叶绿素-a水平,表明营养供应和生物反应.
- 据估计,新 (0.16 kt) 和铁 (32 kt) 从喷发中大量释放到SPG中.
结论:
- HTHH火山爆发大大改变了南太平洋旋转的生物地化学条件.
- 火山的营养投入相当于全球的尘埃流量,这凸显了它对海洋生态系统的重要性.
- 由于营养丰富,喷发可能刺激了SPG中的生物反应.
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