在最后一个冰川时期,大气14C度的极大变化
J W Beck1, D A Richards, R L Edwards
1NSF-Arizona Accelerator Mass Spectrometry Facility, Department of Physics, University of Arizona, Tucson, AZ 85721, USA. wbeck@physics.arizona.edu
概括
大气中的碳-14 (14C) 水平在45,000年前至11,000年前大幅波动,这表明碳循环的主要转移超出了太阳或磁力影响.
科学领域:
- 古气候学 古气候学
- 地质化学 地质化学
- 放射性约会方法 放射性约会方法
背景情况:
- 大气中的放射性碳 (14C) 变化为地球过去的气候和碳循环动态提供了洞察力.
- 斯塔拉格米特是重建过去环境条件的宝贵档案.
研究的目的:
- 为了生成大气14C度的高分辨率记录,覆盖了45,000至11,000年前的时间.
- 在此期间调查14C主要波动的驱动因素.
主要方法:
- 高精度热电离质谱230Th测定石石的年代.
- 加速器质谱测量14C测量石.
- 与来自冰核的宇宙同位素记录 (36Cl,10Be) 的比较.
主要成果:
- 长期观察到大气中的Delta14C从45到33ka增加,并出现快速偏离,特别是在44.3到43.3ka之间.
- 德尔塔14C的显著下降发生在26至11ka之间,从每毫升约700至100,略有波动.
- 观察到的14C模式表明与宇宙同位素峰值的相关性.
结论:
- 仅仅太阳和地磁场的变化无法解释观察到的14C记录.
- 地球碳循环中的大量波动是必要的,以解释14C记录的主要特征.
- 这些发现强调了外部强迫和内部碳循环动态在塑造大气14C水平方面的复杂相互作用.
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