异常长时间的伊欧纪地磁极性逆转
Yuhji Yamamoto1, Slah Boulila2,3, Futoshi Takahashi4
1Marine Core Research Institute, Kochi University, Kochi, Japan.
概括
地球的磁场逆转可能比以前认为的要长得多,一些古老的过渡持续了数万年. 这种延长的持续时间表明,由于辐射增加,地力发电机的变化和对古代生命的潜在影响.
科学领域:
- 地质物理学 地质物理学
- 古磁力学是一种古磁学.
- 地球科学 地球科学 地球科学
背景情况:
- 地球的磁场有着极性逆转的历史.
- 之前的研究表明逆转持续时间为1万年或更短,主要基于最近的地质记录.
研究的目的:
- 为了调查地磁极性过渡在深远过去的持续时间.
- 了解地力学过程的变性.
主要方法:
- 分析了一种异常清晰的深海沉积物古磁记录.
- 约会和分析两个极性过渡可以追溯到大约4000万年前.
主要成果:
- 确定了两个极性过渡,大约在4000万年前发生.
- 这些过渡的持续时间比以前观察到的要长得多,持续时间为18,000年和70,000年.
- 这些发现与预测可变逆转持续时间的数值地力学模型保持一致.
结论:
- 地磁逆转的持续时间不是恒定的,可以远远超过1万年.
- 过渡期间长期存在较弱的地磁场可能会增加地球对太阳辐射的暴露.
- 场强度和持续时间的这种变化可能对古代生命和环境产生影响.
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