A rapid late Holocene lake ecosystem shift driven by climate change:evidence from the first cladoceran record from an alpine lake in northern China
气候驱动下的晚全新世高山湖泊生态系统快速转变:来自中国北方高山湖泊沉积的首个枝角类记录证据作者机构:Key Laboratory of Western China’s Environmental Systems(Ministry of Education)College of Earth and Environmental SciencesLanzhou UniversityLanzhou 730000China Key Laboratory of Alpine EcologyCenter for Excellence in Tibetan Plateau Earth SciencesInstitute of Tibetan Plateau ResearchChinese Academy of SciencesBeijing 100101China Yunnan Key Laboratory of Plateau Geographical Processes and Environmental ChangeSchool of Tourism and GeographyYunnan Normal UniversityKunming 650000China Institute of Loess PlateauShanxi UniversityTaiyuan 030006China
出 版 物:《Science Bulletin》 (科学通报(英文版))
年 卷 期:2020年第65卷第4期
页 面:253-256页
核心收录:
学科分类:070905[理学-第四纪地质学] 0709[理学-地质学] 07[理学] 08[工学] 081501[工学-水文学及水资源] 0815[工学-水利工程]
基 金:supported by the National Natural Science Foundation of China (41790421 41722105)
摘 要:An increasing number of studies have shown that many alpine lakes have experienced rapid ecosystem transformations over the past^200 years[1–3].However,the mechanisms responsible for triggering these changes are often ambiguous in paleolimnological records and hence they are often debated.A major reason for this is that lake ecosystems are under increasing pressure from both anthropogenic activities and climate *** means of distinguishing the effects of different regional drivers of lake ecosystem changes include the study of paleolimnological contexts which predate human activity,or the study of alpine lakes which are still largely unaffected by local human activity.