证据反对以尘埃为媒介控制大气二氧化碳的冰川间冰川变化
1Centre for Environmental Magnetism and Palaeomagnetism (CEMP) and Stable Isotope Laboratory, School of Environmental Sciences, University of East Anglia, Norwich NR4 7TJ, UK. b.maher@lancaster.ac.uk
Nature
|May 11, 2001
概括
大气尘埃对南大洋的铁化肥在最后一次脱冰过程中并没有显著影响大气中的二氧化碳水平. 北大西洋的尘埃峰与二氧化碳变化没有相关性,挑战了这种气候调节理论.
科学领域:
- 古气候学 古气候学
- 海洋学 海洋学 海洋学
- 地质化学 地质化学
背景情况:
- 大气中的二氧化碳度在冰川时期较低,可能是由于海洋铁肥增加.
- 南大洋中的浮游生物可能因铁沉积而增加了二氧化碳的吸收.
- 南大洋的尘埃流量较低,导致偏远铁源影响生产力的假设.
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