概括
底流侵蚀了塔斯曼盆地的深海沉积物,揭示了主要的不一致性. 这种侵蚀很可能是由于与气候冷却和南极冰川化相关的南极地底水速度增加造成的.
科学领域:
- 海洋地质 海洋地质学
- 古海洋学是古海洋学.
- 沉积地质学的地质学
背景情况:
- 深海沉积物记录了地球的历史.
- 海流在沉积物运输和沉积中起着至关重要的作用.
- 塔斯曼盆地是了解南大洋动态的一个关键区域.
研究的目的:
- 调查塔斯曼盆地南部的沉积物侵蚀和沉积模式.
- 为了确定一个重要的沉积物不一致的年龄和程度.
- 了解底部增强电流活动的古海洋学驱动因素.
主要方法:
- 沉积核心的古磁分析.
- 在沉积物中微化石的微古生物学约会.
- 海底的地质绘制,以确定侵蚀特征.
主要成果:
- 在塔斯曼盆地南部确定了一个广泛的沉积物侵蚀区域.
- 像早期普略纪一样古老的沉积物已经被侵蚀.
- 侵蚀表面代表了一个主要的沉积物不一致性.
结论:
- 南极地底水速度的增加是观察到的侵蚀的主要原因.
- 这种速度的增加很可能与晚代代代时期的气候降温有关.
- 增强的南极冰川可能有助于加剧的底流.
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