早期全新纪大气中二氧化碳度的百年级变化
1Laboratory of Palaeobotany and Palynology, Utrecht University, Budapestlaan 4, 3584 CD Utrecht, Netherlands. Netherlands Centre for Geo-ecological Research, Faculty of Earth Sciences, Free University, De Boelelaan 1085, 1081 HV Amsterdam, Netherla.
概括
化石树叶揭示了过去大气中的二氧化碳水平. 早期的Holocene二氧化碳度比以前估计的要高,超过300 ppmv.
科学领域:
- 古气候学 古气候学
- 古植物学是古植物学.
- 地质化学 地质化学
背景情况:
- 大气中的二氧化碳 (CO2) 波动影响气候.
- 树叶中的口腔频率与大气中的CO2相反相关.
- 化石叶子为重建过去的二氧化碳水平提供了一个代理.
研究的目的:
- 利用化石树叶中的口腔频率来重建早期的全新纪大气中的二氧化碳度.
- 为了将这些重建与现有的冰芯数据进行比较.
主要方法:
- 在早期全新纪的化石树叶中分析口腔频率.
- 基于口腔-CO2关系的世纪级二氧化碳波动的量化.
主要成果:
- 胃腔频率信号表明,在全新纪开始时,二氧化碳急剧增加.
- 随后的二氧化碳下降与预boreal振荡冷却事件相对应.
- 早期的全新世二氧化碳水平被重建为300 ppmv以上,与冰芯估计相反.
结论:
- 胃口频率分析提供了一种可靠的方法来评估过去大气中的CO2.
- 早期的全新纪大气中的二氧化碳度明显高于从冰核中先前估计的.
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