亚马逊流域的重建 在过去的14,000年里,有效的水分可用性
1Environmental Change Research Centre, Department of Geography, University College London, 26 Bedford Way, London, WC1H 0AP, UK. mmaslin@geog.ucl.ac.uk
概括
亚马逊盆地14000年前经历了严重的干旱,减少了40%的河流排放. 干旱后,有效湿度在整个全新纪期间稳步增加.
科学领域:
- 古气候学 古气候学
- 水文学的水文学
- 海洋学 海洋学 海洋学
背景情况:
- 了解亚马逊盆地湿度历史对于热带雨林的生物多样性和甲循环至关重要.
- 重建过去的水文变化为气候变化影响评估提供了信息.
研究的目的:
- 为了重建过去14000年的亚马逊河流出历史.
- 为亚马逊河排水盆地建立一个水分预算.
主要方法:
- 在浮游生物中氧气同位素组成的分析.
- 检查来自亚马逊河排放区域的海洋沉积物核心.
主要成果:
- 亚马逊盆地在新德里亚斯时期非常干燥.
- 与今天的水平相比,河流排放量减少了至少40%.
- 年轻德里亚斯之后的融水事件随后在全新世纪持续增加了水分.
结论:
- 年轻的干旱对亚马逊盆地的水分水平产生了重大影响.
- 全新世纪的变暖导致了逐渐的恢复和有效湿度的增加.
- 这些发现为长期气候动态和生态系统弹性提供了洞察力.
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