整个河流-河口-海连续的矿化/固定化动态:有机物和微生物的影响
Hengchen Wei1, Peiyi Wang1, Jing Li2
1School of Environmental Science and Technology, Nanjing Tech University, Nanjing 210008, China.
Marine pollution bulletin
|November 14, 2024
概括
通过对长江-河口-东中国海的矿化和固定化等气循环路径进行了比较. 从河到海观察到的限制,受温度和铁的影响.
科学领域:
- 环境科学 环境科学
- 生物地质化学生物地质化学
- 海洋生态海洋生态学
背景情况:
- (N) 矿化和固定是关键的N循环过程.
- 研究往往侧重于单个息地,忽视了河流-河口-海洋连续.
- 了解跨越多样化的沿海系统的N循环对于生态系统健康至关重要.
研究的目的:
- 为了研究和比较总矿化 (GNM) 和总固定化 (GAI) 率.
- 为了分析长江-河口-东中国海系统的河流,河口和海洋息地的这些速率.
- 为了确定影响N循环沿着这个梯度的环境因素.
主要方法:
- 在河流-河口-海域连续的30个站点进行现场采样.
- 使用丰富15N稳定同位素技术量化GNM和GAI率.
- 分析环境变量,包括有机碳,真菌/细菌比率,温度和铁.
主要成果:
- 从河到海观察到总有机碳的减少和真菌/细菌比率的增加.
- 在梯度上,GNM从5.41降至2.41μgNg-1d-1而GAI则从6.08降至3.27.
- 限制 (GNM/GAI比率>1) 是普遍存在的,温度和Fe被确定为重要的驱动因素.
结论:
- 交叉息地比较对于理解复杂沿海系统中的N循环至关重要.
- 河流-河口-海洋连续体表现出明显的N循环动态和营养限制.
- 温度和铁等环境因素显著调节了这些连接的息地之间的N循环.
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