加利福尼亚州圣莫尼卡架的Holocene海平面曲线,加利福尼亚大陆边境
概括
圣莫尼卡货架上的海平面在18000年内大幅波动,在弗兰德人的过渡期间出现了显著的上升. 这项研究使用多种约会和分析方法重建了过去的海平面变化.
科学领域:
- * 四季地质地质学
- * 古海洋学 古代海洋学
- * 海平面研究.
背景情况:
- *了解过去的海平面波动对于预测未来的沿海变化至关重要.
- * 圣塔莫尼卡货架提供了关于四季纪晚期海平面历史的宝贵记录.
研究的目的:
- *为了重建圣莫尼卡货架过去18,000年的海平面曲线.
- * 分析在弗兰德斯跨越期间海平面变化的动态.
主要方法:
- * 沉积物的放射性碳测年.
- * 沉积物学数据分析.
- * 晚四年纪梯田沉积物的高分辨率地震分层分析.
主要成果:
- *大约18000年前,海平面比现在低117米.
- * 在弗兰德斯的过渡期间,海平面上升,下降,然后再次上升,保持在现在的水平以下.
- * 跨越后的海平面上升速度较慢,并没有中断到目前的位置.
结论:
- *海平面曲线显示了四年纪末期复杂的波动.
- * 佛兰德斯的过渡涉及到海平面的显著,非线性移动.
- * 该研究提供了千年来区域海平面变化的详细记录.
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