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古生物学时期海平面变化的时间表
Bilal U Haq1, Stephen R Schutter
1National Science Foundation, Arlington, VA 22230, USA. bhaq@nsf.gov
概括
这项研究重建了古生物学时代的海平面,揭示了长期趋势和172个静态事件. 海平面的波动很大,幅度高达125米,受赫尔南特冰川等事件的影响.
科学领域:
- 古生物学的古生物学
- 在平流体学上,平流体学是平流体学.
- 古海洋学是古海洋学.
背景情况:
- 古生物学时代的海平面历史仍然不完全整合.
- 之前的研究集中在特定时期,缺乏全面的概述.
- 了解过去的海平面变化对于古气候和构造学重建至关重要.
研究的目的:
- 为了重建整个古生物学时代的海平面波动的全面历史.
- 为了识别和记录个别的静电事件及其大小.
- 分析海平面的长期趋势及其驱动因素.
主要方法:
- 利用了来自周边地和地盆地的地层划分.
- 评估了个别海平面事件的时间和幅度.
- 综合数据,建立一个统一的海平面曲线的古世.
主要成果:
- 记录了172个Eustatic事件在整个古生物学.
- 确定了长期的海平面上升,从坎布里亚到奥尔多维纪晚期的顶峰.
- 观测到海平面的显著波动,包括在Hirnantian冰川时期的退出以及随后的高低.
- 海平面变化的幅度从几十米到大约125米不等.
结论:
- 已经建立了一个详细的海平面历史的古生物学时代.
- 海平面的波动是动态的,受冰川和构造活动的影响.
- 准确估计海平面变化大小仍然是一个挑战.
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