微量金属的可用性对可可利托化化的作用
K G Schulz1, I Zondervan, L J A Gerringa
1Alfred Wegener Institute for Polar and Marine Research, PO Box 120161, 27515 Bremerhaven, Germany. kschulz@ifm-geomar.de
Nature
|August 6, 2004
概括
大气中的尘埃大气中的尘埃.
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
- 古气候学 古气候学
背景情况:
- 海洋尘埃沉积量随着地质时间的推移而变化.
- 尘埃中的微量金属,如铁和,是植物浮游生物的重要营养素.
- 尘埃供应的变化可能会影响海洋初级生产和碳循环.
研究的目的:
- 调查铁和对Emiliania huxleyi的影响.
- 确定微量金属限制如何影响生物生成化.
- 了解尘埃沉积对海洋生物碳的影响.
主要方法:
- 在不同度的铁和下培养了海洋微藻Emiliania huxleyi.
- 测量的增长率和碳酸 (CaCO3) 产量.
- 分析了有机颗粒碳与CaCO3出口的比率 (雨量比率).
主要成果:
- 低铁减少了Emiliania huxleyi的生长和化.
- 低脱增长从化,导致更多的化细胞.
- 限制的细胞表现出不受影响的每细胞CaCO3生产率,尽管增长速度较慢.
结论:
- 微金属的可用性,特别是,显著影响生物生成化.
- 尘埃沉积的变化可以改变微量金属有限的海洋地区的化.
- 化的变化可能会影响海洋的二氧化碳捕获和大气分区.
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