海洋生物学在冰川-冰川间二氧化碳循环中的作用
Karen E Kohfeld1, Corinne Le Quéré, Sandy P Harrison
1Max Planck Institute for Biogeochemistry, Jena, Germany. office@kohfeld.com
概括
海洋生物的变化并不能完全解释冰川二氧化碳 (CO2) 的吸收. 铁化肥可能只占冰河时代观察到的二氧化碳减少的一半以下.
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:
- 大气中的二氧化碳 (CO2) 含量在冰川时期显著降低.
- 海洋生物是大气二氧化碳的关键调节器.
- 假设表明,海洋生产力的变化导致了冰川二氧化碳的减少.
研究的目的:
- 研究海洋生物在冰川二氧化碳减排中的作用.
- 测试涉及铁受精,营养利用和浮游生物转移的假设.
- 量化这些机制对过去二氧化碳变化的贡献.
主要方法:
- 对海洋生产力的沉积物记录的分析.
- 检查了最后一个冰川周期的高峰和中期的数据.
主要成果:
- 南洋营养利用的变化并不能解释二氧化碳的减少.
- 主导浮游生物类型的变化不足以解释二氧化碳的减少.
- 铁肥和相关过程最多可以解释50%的冰川二氧化碳减少.
结论:
- 海洋生物在冰川二氧化碳吸收中的作用不如以前假设的那么重要.
- 仅靠铁化肥无法完全解释冰河时代大气二氧化碳的减少.
- 其他机制可能有助于显著的冰川二氧化碳减少.
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