作为海洋档案的独立时间标记,在米奥森末期出现了一种宇宙10Be异常
Dominik Koll1,2,3, Johannes Lachner4, Sabrina Beutner5
1Accelerator Mass Spectrometry and Isotope Research, Helmholtz-Zentrum Dresden-Rossendorf, Dresden, Germany. d.koll@hzdr.de.
Nature communications
|February 10, 2025
概括
研究人员在深海铁甲地中发现了一种显著的,长期存在的宇宙性36Cl异常,该异常来自中新世纪晚期. 这一发现为海洋地质档案在百万年时间尺度上提供了潜在的新时间标记.
科学领域:
- 地质化学 地质化学
- 古海洋学是古海洋学.
- 地质时间学 (Geochronology)
背景情况:
- 宇宙核年代测定依赖于一致的放射性核产量和在地质记录中的纳入.
- 全新世和新世的异常作为统一数据的全球基准.
- 一个百万年时间尺度的约会之前是不可用的.
研究的目的:
- 在百万年时间尺度上识别和描述潜在的约会.
- 为了调查海洋档案中的宇宙核化物度异常.
主要方法:
- 对宇宙源10 (10Be) 度的分析.
- 来自太平洋中部和北部的深海铁甲皮的约会.
- 对地质,气候,太阳和天体物理事件的检查.
主要成果:
- 长期存在的宇宙10Be异常被确定在米奥森晚期的铁甲皮.
- 异常发生在9至1150万年前,达到1010万年前的峰值.
- 该异常被记录在多个太平洋深海样本中.
结论:
- 发现的10Be异常代表了百万年时间尺度上与常数的显著偏差.
- 这种异常有可能成为海洋档案的独立时间标记.
- 需要进一步的研究才能充分了解这种异常的起源和影响.
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