碳酸盐沉积,气候稳定性和新新生代的冰河时代
Andy J Ridgwell1, Martin J Kennedy, Ken Caldeira
1Department of Earth Sciences, University of California-Riverside, Riverside, CA 92521, USA. andyr@citrus.ucr.edu
概括
浮游生物化物在法内罗纪期间进化,通过缓冲海洋碳酸盐来稳定气候. 这保留了海洋的化学成分,与前剑桥时期的碳循环不同.
科学领域:
- 地质化学 地质化学
- 古气候学 古气候学
- 海洋学 海洋学 海洋学
背景情况:
- 前坎布里亚碳循环对浅水环境和二氧化碳气候反很敏感,导致新新生代的冰河时代.
- 前坎布里亚气候缓冲依赖浅水碳酸盐沉积,平衡大陆气候输入.
- 浮游生物化的进化标志着地球气候调节的重大转变.
研究的目的:
- 为了解释Phanerozoic气候系统的稳定.
- 阐明浮游体化剂在缓冲海洋碳酸离子度中的作用.
- 了解新新生代冰河时代和碳酸盐形成的原因.
主要方法:
- 在海底沉积物中碳酸盐保存的分析.
- 海洋碳酸离子度动态的建模.
- 预坎布里亚和法内罗纪碳循环过程的重建.
主要成果:
- 浮游生物化剂引入了碳酸盐的和依赖性保存,缓冲了海洋化学.
- 这种新机制稳定了法内罗纪时期的气候系统.
- 前坎布里亚时期的气候不稳定与这种缓冲机制的缺失有关.
结论:
- 浮游生物化的进化是气候稳定的一个关键事件.
- 碳酸盐的和依赖性保护是长期气候调节的一个关键因素.
- 了解过去的碳循环动态,有助于我们了解地球系统的灵敏度.
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