一个碳同位素记录二氧化碳水平在四年纪晚期
1Department of Geological Sciences, Indiana University, Bloomington 47405-5101, USA.
Nature
|October 4, 1990
概括
大气中的二氧化碳 (CO2) 水平在地球上最后一个冰川 - 间冰川过渡期间大幅上升. 这项研究揭示了一种使用沉积物核心同位素追踪过去二氧化碳变化的方法,将我们的气候记录进一步延伸到过去.
科学领域:
- 古气候学 古气候学
- 地质化学 地质化学
- 海洋学 海洋学 海洋学
背景情况:
- 大气中的二氧化碳在最后一个冰川期和冰川间时期从180 ppm增加到280 ppm.
- 这种大气变化是由海洋混合层中溶解的二氧化碳增加所驱动的.
- 光合作用将溶解的二氧化碳与有机物质的碳同位素组成联系起来.
研究的目的:
- 研究大气中的二氧化碳和海洋有机物中的碳同位素之间的关系.
- 从沉积物核中建立一个用于重建过去大气二氧化碳水平的代理.
- 为了将沉积物同位素记录与现有的冰芯CO2数据相关联.
主要方法:
- 分析被冰盖所困的气体,以确定过去大气中的二氧化碳度.
- 在半沉积物核心中检查碳同位素组成 (13C).
- 沉积物核的同位素记录与沃斯托克冰核的二氧化碳记录的相关性.
主要成果:
- 在沉积物核心的同位素记录中发现了一种反映大气二氧化碳水平的信号.
- 这一信号成功地与沃斯托克冰核的二氧化碳记录相关联.
- 该研究表明,碳同位素分离与大气中的二氧化碳度之间存在联系.
结论:
- 海洋沉积物中的碳同位素记录可以作为大气CO2的代理.
- 这种方法允许重建超出冰芯记录时间框架的二氧化碳水平.
- 进一步校准可以将古气候CO2重建延伸到更早的地质时期.
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