概括
随着大气中的二氧化碳 (CO2) 增加,叶子胃细胞减少. 化石叶子分析揭示了这种关系,作为过去1000万年CO2水平的生物指标.
科学领域:
- 古植物学是古植物学.
- 气候科学 气候科学
- 环境科学 环境科学
背景情况:
- 大气中二氧化碳 (CO2) 度的上升与叶子口腔密度的下降有关.
- 这种现象在最近的植被和受控实验中被观察到.
- 化石植物证据为这种关系提供了长期的视角.
研究的目的:
- 调查使用化石叶子口腔频率作为古大气CO2水平的生物指标.
- 为了重建晚期新生代大气中的CO2波动.
主要方法:
- 在化石Quercus petraea叶子中分析口腔频率.
- 应用已知的口腔密度与CO2度之间的关系.
主要成果:
- 化石叶子中的口腔频率提供了过去CO2水平的可靠指标.
- 晚期新生代大气中的CO2度估计在大约280和370 ppm之间变化.
结论:
- 化石叶的口腔频率作为重建历史大气CO2水平的有价值的生物指标.
- 古大气中的CO2在新一代晚期经历了显著的波动.
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