一个同位素的观点,关于碳和循环的演变
Boriana Kalderon-Asael1, Joachim A R Katchinoff2, Noah J Planavsky3
1Earth and Planetary Sciences, Yale University, New Haven, CT, USA. boriana.kalderon-asael@yale.edu.
Nature
|July 15, 2021
概括
同位素记录揭示了地球碳和循环的长期变化,表明从前坎布里亚到现代过程的转变. 这种进化与对的生物控制和陆地植物的兴起有关.
科学领域:
- 地质化学 地质化学
- 古气候学 古气候学
- 地球科学 地球科学 地球科学
背景情况:
- 全球碳和循环影响地球的长期气候稳定.
- 对这些循环的反机制和定量约束仍然不太了解.
- 同位素记录为跟踪这些元素循环提供了一个新的代理.
研究的目的:
- 利用同位素记录来研究长期的碳和循环演变.
- 建立一个全面的碳酸盐基同位素记录,跨越过去的30亿年.
- 了解同位素值观测趋势背后的驱动因素.
主要方法:
- 分析来自不同层级统计单位的600多个浅水海洋碳酸盐样本.
- 建立一个30亿年碳酸基同位素记录.
- 质量平衡建模用于解释同位素趋势.
主要成果:
- 鉴定出碳酸盐同位素价值在地质时间上的显著增加.
- 这一趋势归因于海水中同位素条件的演变.
- 数据表明,从前坎布里亚到现代碳和循环的过渡.
结论:
- 同位素记录为地球不断发展的碳和循环提供了关键的见解.
- 观察到的趋势反映了这些生物地球化学循环的根本转变.
- 这种转变可能与生物介导的循环和陆地植物生命的出现有关.
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