摘要
根据气候和海平面变化,讨论了长江三角洲和环太湖地区距今5300～4000年前良渚文化的兴衰。作者认为,良渚文化时期是全新世中期,气候相对比较温凉干燥,海平面相对比较低的时期,为良渚文化的发展提供了良好的环境。全新世中期第四个（最后一个）千年尺度暖湿气候期,造成江河湖泊高水位或海侵,使该地区成为水泽环境,导致良渚文化消失。
According to climate and sea level changes,the prosperity and decline of the Liangzhu Culture are discussed in this paper,which generated in the Yangtze Delta area and the surrounding area of Taihu Lake and dated back to 5300-4000 years ago.The author considers that it was the relative milder climate with lower temperature and less rainfall and lower sea level that provided the favorable environment for Liangzhu Cultures development in the mid-Holocene period.And high sea level and frequent floods during the fourth（last） warm/wet climate period for thousand years scale in the mid-Holocene resulted in disappearance of the Liangzhu Culture.
出处
《干旱气象》
2008年第1期13-16,共4页
Journal of Arid Meteorology
关键词
气候变化
影响
良渚文化
climate change
influence
Liangzhu Culture
