由罗纪沙丘记录的年度季风雨
D B Loope1, C M Rowe, R M Joeckel
1Department of Geosciences, University of Nebraska, Lincoln, Nebraska 68588-0340, USA. dloope1@unl.edu
Nature
|July 14, 2001
概括
在罗纪沙丘沉积物中发现了潘盖亚古代季风的证据. 沉降质量揭示了年度降雨模式,这表明这个时期的极端季节性.
科学领域:
- 古气候学 古气候学
- 沉积物学的沉积物学
- 在平流体学上,平流体学是平流体学.
背景情况:
- 潘盖亚在古老时代晚期和中新时代早期的赤道位置.
- 之前的建模和平流图研究表明季风循环和极端季节性.
- 缺乏关于年度降雨周期性的直接证据.
研究的目的:
- 提供潘盖亚每年降雨周期的直接证据.
- 为了重建史前季节性降雨模式.
主要方法:
- 在年度沉积周期内分析低谷质量.
- 在美国西南部考察纳瓦霍沙岩突出.
- 解读下滑位置以确定降雨季节性.
主要成果:
- 在沙丘迁移的36年间隔内确定了24个沉降质量.
- 解读了20个条是由于夏季季风雨造成的.
- 解释4个低迷是由于冬季风暴造成的.
结论:
- 罗纪沙丘的低沉的面提供了每年降雨事件的史前记录.
- 支持了由潘盖亚上空季风循环驱动的极端季节性假设.
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