由于海洋和库存的变化,冰川海洋中的固定减少
Raja S Ganeshram1, Thomas F Pedersen, Stephen Calvert
1Department of Geology and Geophysics, University of Edinburgh, West Mains Road, Edinburgh EH9 3JW, UK. Raja.Ganeshram@glg.ed.ac.uk
Nature
|January 24, 2002
概括
在冰川时期,海洋和的含量增加,但较高的N/P比率可能抑制了固定,从而质疑铁化肥假说的增加海洋生产力和二氧化碳吸收.
科学领域:
- 古海洋学是古海洋学.
- 海洋生物地质化学海洋生物地质化学
- 气候科学 气候科学
背景情况:
- 冰川时期大气中二氧化碳的降低通常是由海洋浮游生物的生产力增加所解释的.
- 铁受精假说表明,增加的铁粉刺激了固,促进了植物浮游生物的生长和二氧化碳的吸收.
研究的目的:
- 研究营养物质的可用性和固定在冰川时期调节海洋生产力的作用.
- 通过检查营养动力学来挑战当前的铁化肥假设.
主要方法:
- 来自墨西哥西北部大陆边缘的沉积物核心的分析.
- 在冰川时期的脱和酸盐形成速度的重建.
主要成果:
- 冰川时期的脱和化形成减少,增加了海洋的和库存.
- 的增加速度不如的增加速度快,导致N/P比率升高.
- 增加的N/P比率可能会抑制固,这与铁受精假说相反.
结论:
- 在冰川时期增加的营养物质库存或铁供应可能不会提高海洋生产力.
- 建议的铁刺激固化的机制可能无法解释较低的冰川二氧化碳水平.
- 海洋营养循环和N/P比率在调节海洋生产力和碳捕获方面发挥着至关重要的作用.
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