湖泊N:P的静态度和营养限制的变化是由大气中沉积驱动的
James J Elser1, Tom Andersen, Jill S Baron
1School of Life Sciences, Arizona State University, Tempe, AZ 85287, USA. j.elser@asu.edu
概括
大气中的沉积改变了湖泊的营养比率,将植物浮游生物的生长从限制转移到限制. 这凸显了人类活动对水生生态系统的广泛影响.
科学领域:
- 环境科学 环境科学
- 生态生态学 生态生态学
- 临界技术 临界技术
背景情况:
- 人类活动显著增加了全球 (N) 循环.
- 大气中 (N) 沉积是人为N进入生态系统的主要途径.
研究的目的:
- 研究大气 (N) 沉积对湖泊营养限制的影响.
- 为了确定改变的 (N) 和 (P) 比率如何影响浮游生物的生长.
主要方法:
- 在挪威,瑞典和科罗拉多州的湖泊中分析 (N) 和 (P) 的石化比率.
- 观察生态营养限制模式的变化.
主要成果:
- 大气中的N沉积增加了研究湖泊中的N:P比率.
- 植物浮游生物的生长从高沉积湖中的 (N) 有限转变为 (P) 有限.
结论:
- 人为 (N) 丰富改变了湖泊中的基本生态过程.
- 这些变化影响生物地球化学循环,热量动力学和生物多样性,即使在偏远的湖泊.
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