三百五十万年来,西藏高原的植被动态对气候变化的反应
Yan Zhao1,2, Feng Qin3, Qiaoyu Cui3
1Key Laboratory of Land Surface Pattern and Simulation, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing, China. zhaoyan@igsnrr.ac.cn.
Nature ecology & evolution
|June 13, 2025
概括
在西藏高原的西藏高原.
科学领域:
- 古气候学和古生态学.
- 西藏高原生态系统动力学 西藏高原生态系统动力学
- 四季度植被历史 四季度植被历史
背景情况:
- 西藏高原拥有世界上最大的高山草原,易受全球变暖的影响.
- 了解温暖气候下的过去植被变化对于预测生态系统临界点至关重要.
研究的目的:
- 在过去的350万年里,重建西藏高原过去的植被动态.
- 确定生态系统制度转移的关键温度值.
主要方法:
- 来自湖泊沉积物核心的连续,多个百年解决的花粉记录的分析.
- 生物化,数值分析,统计建模和植被模拟的应用.
主要成果:
- 植被从纪森林转变为四季纪森林-草原,后来在1.540万年前后转变为草原主导地位.
- 植被变化与冰川 - 冰川间周期和千年级变化相关.
- 2-3°C的升温代表了森林扩张和草原丧失的关键值.
结论:
- 西藏高原过去的植被变化主要是由温度波动驱动的.
- 目前的高山草地面临着由于持续的全球变暖和不足的排放减少而面临的转型风险.
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