热层中的区域14CO2抵消:规模,机制和后果
B Kromer1, S W Manning, P I Kuniholm
1Heidelberger Akademie der Wissenschaften, Institut für Umweltphysik der Universität Heidelberg, Im Neuenheimer Feld 229, D-69120 Heidelberg, Germany. bernd.kromer@iup.uni-heidelberg.de
概括
放射性碳测年依赖于恒定的大气二氧化碳 (CO2). 这项研究发现了区域二氧化碳的变化,影响了日期准确性和古气候研究.
科学领域:
- 古气候学 古气候学
- 通过放射性碳测年法进行测年.
- 大气科学 大气科学
背景情况:
- 放射性碳测年法假定北半球的热层二氧化碳 (CO2) 水平均.
- 之前的研究通常支持低至中度地区的这一假设.
研究的目的:
- 调查热层 (14) 碳化合物 (2) 水平的潜在区域变化.
- 评估这些变异对放射性碳年代和古气候重建的影响.
主要方法:
- 来自德国南部和安纳托利亚的树环 (14) C 数据的比较.
- 分析短期区域 (14) CO ((2) 的抵消.
主要成果:
- 树环数据通常支持统一的热层 (14) CO(2) 假设,但揭示了显著的短期区域抵消.
- 这些偏移与一个强化的季节性 (14) CO(2) 周期有关,在太阳磁活性较低和大气冷却期间受到平流层 (14) C 流量的影响.
结论:
- 短期的区域 (14) CO(2) 变化可能会发生,挑战同质性的假设.
- 了解这些偏移对于准确的古气候研究和高分辨率的考古约会至关重要.
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