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Different types of Anthropocene signals recorded in Huguangyan Maar Lake over the past 450 years  ( SCI-EXPANDED收录)  

文献类型:期刊文献

英文题名:Different types of Anthropocene signals recorded in Huguangyan Maar Lake over the past 450 years

作者:Jiang, Shiwei[1];Zhou, Xin[1];Ma, Li[1];Cui, Shukun[1];Liu, Xuanqiao[1];Liu, Xiaoyan[1];Chen, Anze[1];Luo, Yong[1];Xu, Liqiang[2];Zeng, Fangming[3];Kong, Deming[4];Huang, Chao[4];Zhang, Guangcheng[1,5]

机构:[1]Univ Sci & Technol China, Sch Earth & Space Sci, Hefei 230026, Peoples R China;[2]Hefei Univ Technol, Sch Resources & Environm Engn, Hefei 230009, Peoples R China;[3]Qinghai Prov Key Lab Geol & Environm Salt Lakes, Xining 810008, Peoples R China;[4]Guangdong Ocean Univ, Coll Ocean & Meteorol, Lab Coastal Ocean Variat & Disaster Predict, Zhanjiang 524088, Peoples R China;[5]Anhui Geol Arch, Hefei 230002, Peoples R China

年份:2024

卷号:247

外文期刊名:CATENA

收录:SCI-EXPANDED(收录号:WOS:001360147100001)、、Scopus(收录号:2-s2.0-85209115880)、WOS

基金:This study was jointly supported by the National Natural Science Foundation of China (42488201, 42301175) and the National Key Research and Development Program of China (2022YFF0801101) .

语种:英文

外文关键词:Anthropocene; Huguangyan Maar Lake; Human activities; Lake sediment; Southern China

外文摘要:Over the past few centuries, human activities have increasingly impacted global climate and ecological environments. The "Anthropocene" has been proposed to highlight the significant influence of human activities on the environment. However, prior research has focused on analyzing a single type of human activity in lake sediments. In this study, we examined the historical changes in water eutrophication, terrestrial vegetation, and heavy metal pollution in the sediments of Huguangyan Maar Lake over the past 450 years. By comparing different human activity records within the same regional and chronological framework, we found that the timing of significant impacts on lake sediments varied by activity type. Eutrophication, induced by population growth and agricultural fertilization, began around 1950 CE. Changes in vegetation owing to agricultural and forestry practices occurred around 1780, 1880, and 1980 CE. Significant enrichment of heavy metals from industrial production began around 1950 CE. We suggest that, in reconstructing the history of human activities or defining the onset of the "Anthropocene," it is crucial to consider both the types of human activities and their spatial extent.

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