大气中二氧化碳水平的下限是在32亿年前
Angela M Hessler1, Donald R Lowe, Robert L Jones
1Department of Geological and Environmental Sciences, Stanford University, Stanford, California 94305-2115, USA. hesslera@gvsu.edu
Nature
|April 16, 2004
概括
古代气候模型可能需要除了二氧化碳之外的温室气体. 关于古代土壤的新研究表明,二氧化碳水平比以前认为的要高,但仍然可能不足以解释地球早期的温暖.
科学领域:
- * 早期的地球研究.
- * 地质化学 * 地质化学
- * 古气候学 * 古气候学
背景情况:
- * 了解古代大气组成是早期地球演变的关键.
- *二氧化碳和甲是影响气候的潜在温室气体.
- * 之前的研究限制了二氧化碳水平低于热量的模型要求.
研究的目的:
- * 为了研究阿基亚时代大气组成.
- *确定二氧化碳和其他温室气体在维持地球早期温度方面的作用.
主要方法:
- *分析了32亿年前河流石上的风化皮肤.
- * 模型平衡反应的应用.
- * 富含铁的碳酸盐和粘土矿物的地化学分析.
主要成果:
- *富含铁的碳酸盐表明二氧化碳的最小部分压力是当今水平的几倍.
- * 这些所需的二氧化碳水平仍然低于一些气候模型所需的水平.
- *这些发现挑战了对二氧化碳的单一依赖,以获得阿热量.
结论:
- * 古代大气中的二氧化碳含量可能高于一些估计.
- *甲或其他温室气体可能在维持早期地球温度方面发挥了重要作用.
- * 需要进一步的研究才能充分理解古老气候调节.
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