自小冰河时代以来,西藏高原南部的人类活动与环境变化之间的关系
Cunlin Li1, Liping Zhu1, Qingfeng Ma2
1State Key Laboratory of Tibetan Plateau Earth System, Environment and Resources (TPESER), Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China; University of Chinese Academy of Sciences, Beijing 100049, China.
The Science of the total environment
|June 10, 2024
概括
自小冰河时代以来,西藏高原的人类活动对环境产生了重大影响. 随着时间的推移,受气候影响的人口增长和农业发展导致了土壤侵蚀的变化.
科学领域:
- 古气候学 古气候学
- 环境科学 环境科学
- 考古学的考古学
背景情况:
- 西藏高原 (TP) 为人类定居带来了极端的环境挑战.
- 了解人与环境的相互作用对于适应气候变化至关重要.
研究的目的:
- 阐明自小冰河时代 (LIA) 以来在南方TP上人类活动和环境变化之间的关系.
- 通过便斯坦重建过去的人类人口和草食动物的动态.
主要方法:
- 对便中醇 (coprostanol,epicoprostanol等) 的分析 在各种环境样本 (便,沉积物,土壤) 中.
- 使用粒度大小,元素分析和沉积率重建环境变化.
- 整合气候记录以解释人类与环境的动态.
主要成果:
- 从公元1820年到2021年,人类人口显著增加,这可以通过便中醇指数S1.1的上升来表明.
- 在LIA期间的气候变化影响了农业发展,人口和牲畜数量.
- 自1951年以来,土地复苏和养殖的增加导致了土壤侵蚀,近几十年来由于保护工作的努力,土壤侵蚀已经下降.
结论:
- 人类活动,特别是人口增长和土地利用,已经明显改变了西藏高原的环境.
- 气候变化和政策在塑造TP上人类与环境的互动方面发挥了重要作用.
- 这项研究为未来极端环境中的气候变化适应战略提供了宝贵的见解.
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