云南全新世气候变化研究综述  

SUMMARY OF CLIMATE CHANGES RESEARCH DURING HOLOCENE EPOCH IN YUNNAN PROVINCE

作　　者：杨冬琴[1] 刘波[1] 

机构地区：[1]昭通师范高等专科学校政史系,云南昭通657000

出　　处：《云南地理环境研究》2011年第4期106-111,共6页Yunnan Geographic Environment Research

摘　　要：大尺度时间段气候的研究成果,特别是最年轻的地质时期全新世(11 500年前至今)的气候特点是研究现在气候变化的重要依据。通过对比云南不同地点的湖泊沉积、岩溶化学沉积物、洞穴沉积物等例证研究,总的来说,云南全新世气候整体演化与全球气候变化具有一致性,在地理位置、季风等因素的影响下又具有独特的气候特征。It＇ the vital evidence to research on climate changes through the large-scale time of climate research, especially research on the Holocene （ 11, 500 years ago to the present） during the youngest geological period. By comparing the lake sediments, karst chemical sediments, cave deposits and other examples of research at different locations in Yunnan, In general, the overall evolution of Holocene climate in Yunnan is the consistency of global climate changes. It had the unique climate characteristics under the location, monsoon and other factors influence.

关 键 词：云南 全新世 气候变化 钙化 孢粉 

分 类 号：P532[天文地球—古生物学与地层学]