青藏高原湖泊沉积记录与环境变化研究

doi:10.3981/j.issn.1000-7857.2017.06.007

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摘要过去全球变化研究是人类认识气候与环境变化事实与规律，客观评价现代环境在气候与环境发展历史中位置的重要手段，能够为未来气候与环境变化的预测提供科学的检验工具。介绍了湖泊沉积物环境代用指标与气候要素关系定量化的研究，简要回顾利用湖泊沉积物重建高原最近2万年环境变化历史研究成果，阐述高原湖泊沉积对气候变化的敏感响应。

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	朱立平
	郭允

关键词 ：青藏高原, 湖泊沉积, 环境变化, 2万年

Abstract：The study of historical environmental changes is important for understanding the general trends of climatic and environmental changes, objectively evaluating the present environment in the context of the climatic and environmental history. It provides scientific test tools for predicting future climatic and environmental changes. This paper reviews the studies of the relations between the lake sediment proxies and the climatic factors, and the reconstruction of the environmental change history in the last 20 thousand years, based upon the lake sediments, to elucidate the sensitive response of the lake sediments to the climatic changes on the Tibetan Plateau.

Key words： Tibetan Plateau lake sediment environmental changes Last 20 thousand years

收稿日期: 2016-11-24

基金资助:中国科学院战略性科技先导B类专项项目（XDB03030000）

作者简介: 朱立平,研究员,研究方向为湖泊沉积与环境变化,电子信箱:lpzhu@itpcas.ac.cn

引用本文:

朱立平, 郭允. 青藏高原湖泊沉积记录与环境变化研究[J]. 科技导报, 2017, 35(6): 65-70.
ZHU Liping, GUO Yun. Lake sediments and environmental changes on the Tibetan Plateau. Science & Technology Review, 2017, 35(6): 65-70.

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http://www.kjdb.org/CN/10.3981/j.issn.1000-7857.2017.06.007 或 http://www.kjdb.org/CN/Y2017/V35/I6/65

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