在北冰洋西部的楚克奇海架上对氨积累的生物地质化学和物理控制
Yanpei Zhuang1, Yangjie Li2, Ling Chen2
1Polar and Marine Research Institute, Jimei University, Xiamen, China; Key Laboratory of Marine Ecosystem Dynamics, Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou, China; Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai, China.
Marine environmental research
|July 10, 2023
概括
在2012年至2018年期间,在楚克奇货架的两个不同区域发现了高度的氨. 这些池是生物地球化学和物理过程的结果,可能会影响北极生态系统.
科学领域:
- 海洋化学 海洋化学
- 生物地质化学生物地质化学
- 北极海洋学 北极海洋学
背景情况:
- 氨是海洋生态系统的关键营养素,影响了初级生产力和热量动态.
- 了解氨循环对于评估北极海洋环境的健康和功能至关重要.
研究的目的:
- 调查楚克奇货架上氨度的空间变化和驱动因素.
- 确定持久高含量区域及其潜在的生态影响.
主要方法:
- 对沿着重复横断线收集的空间和时间氨度数据的分析.
- 检查影响氨积累的生物地球化学和物理因素.
主要成果:
- 在楚克奇架上,在约67.5°N和72.5°N处发现了两个接近底部的高氨池 (>1μmol/kg).
- 氨的积累归因于有机物质的细菌再矿化和由于密度分层而导致的有限的向上混合.
结论:
- 楚克奇岩架展示了独特的富含氨的区域,由结合的生物地球化学和物理过程驱动.
- 增加的初级生产可能会导致更大的氨池,可能会改变楚克奇海架生态系统结构和生产力.
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