化石丰富的Lana'i沉积物是由多个事件形成的,而不是一个单一的巨大海
K H Rubin1, C H Fletcher, C Sherman
1Department of Geology and Geophysics, SOEST, University of Hawaii, Honolulu 96822, USA. krubin@soest.hawaii.edu
Nature
|December 29, 2000
概括
巨大的海并不是夏威夷岛屿石沉积的原因. 相反,由正常的波浪和风暴活动驱动的长期多次沉积事件形成了这些特征.
科学领域:
- 地质地质地质地质地质地
- 古气候学 古气候学
- 海洋科学 海洋科学
背景情况:
- 以前,人们认为夏威夷群岛的海底滑坡会导致巨大的海.
- 假设这些海在Lana'i和Moloka'i的高处沉积了混乱的石.
- 在Lana'i的Hulopoe石沉积物一直是这个假设的关键焦点.
研究的目的:
- 为了调查巨大的海导致夏威夷岛屿石沉积的假设.
- 确定Lanai上的Hulopoe砂沉积物的形成过程和时间.
- 重新评估沿海砂沉积的"巨浪"假设.
主要方法:
- - (U-Th) 在Hulopoe石内珊瑚的约会.
- 对地平面关系的分析,包括面变化和间隙.
- 在沉积物中对珊瑚年龄组的地理和层级学评估.
主要成果:
- 胡洛波石含有来自两个不同的年龄组的珊瑚:海洋同位素阶段5e (约135,000年前) 和7 (约240,000年前).
- 石沉积物显示出显著的地理和地层学排序,表明多个沉积事件.
- 这些事件相隔相当长的时间,这与单一的巨大海事件相矛盾.
结论:
- "巨浪"假说被多个时间相隔的沉积事件的证据无效.
- 在冰河间时期,石很可能是由夏威夷海岸线的常规过程 (季节性波浪,风暴,正常的海) 沉积的.
- 目前的Hulopoe石的高度归因于Lana'i在地质时间上的升起.
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