米兰科维奇假设得到了珊瑚礁和深海沉积物的精确约会的支持
概括
巴巴多斯 巴巴多斯 巴巴多斯
科学领域:
- 海洋地质学 海洋地质学
- 古气候学 古气候学
- 珊瑚礁研究研究珊瑚礁的研究.
背景情况:
- 巴巴多斯的珊瑚礁露台提供了一个独特的地质记录.
- 岛上均的升起率使得研究海平面变化变得更加容易.
研究的目的:
- 利用巴巴多斯的地质特征,重建了普莱斯托时代晚期的海平面高.
- 为了将海平面的波动与地球的气候和轨道周期相关联.
主要方法:
- 高精度的放射测年法使用-230:-234 (Th(230):U(234) 和-231:-235 (Pa(231):U(235)).
- 对珊瑚礁和深海核心进行分析.
主要成果:
- 在大约122,000,103,000和82,000年前确定了三种不同的海平面高位.
- 埃里克森的W-X气候事件约在126,000年前发生.
- 证明了地球气候,海平面变化和预测过去15万年夏季日照周期之间的相关性.
结论:
- 巴巴多斯上升的珊瑚礁为重建过去的海平面提供了可靠的档案.
- 晚期普世时期的海平面波动与地球轨道变化和由此产生的气候变化密切相关.
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