地磁极性变化,南太平洋的火山最大值和动物灭绝
1Graduate School of Oceanography, University of Rhode Island, Kingston 02881, USA.
Nature
|August 29, 1970
概括
火山活动峰值与地磁极性转移一致,这表明地球地幔和磁场变化之间存在联系. 这可能解释了火山驱动的气候变化导致的灭绝.
科学领域:
- 地质物理学 地质物理学
- 古气候学 古气候学
- 海洋地质学海洋地质学
背景情况:
- 地磁极性逆转是地球历史的关键标记.
- 深海沉积物保存了过去的地质和环境条件的记录.
- 火山活动可以影响全球气候和生态系统.
研究的目的:
- 研究火山活动与地磁极性变化之间的关系.
- 探索这些现象与动物灭绝之间的潜在联系.
- 了解在极性过渡期间的火山活动对气候的影响.
主要方法:
- 来自南极太平洋水域的深海沉积芯的分析.
- 火山灰层 (火山最大值) 与地磁极性数据的相关性.
- 检查与已识别的地质事件相关的动物灭绝模式.
主要成果:
- 观察到火山活动峰值与地磁极性变化时期之间的巧合.
- 证据表明,上层地幔活动可能会影响地磁极性转移.
- 火山引起的气候变化和极性变化期间的动物灭绝事件之间的潜在相关性.
结论:
- 上层地幔活动和地磁极性变化似乎是相关的.
- 在地磁极性转移期间由火山引起的气候变化可能解释了动物灭绝.
- 深海核心数据为地球动态历史提供了关键的见解.
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