中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Early human impacts on vegetation on the northeastern Qinghai-Tibetan Plateau during the middle to late Holocene

文献类型:期刊论文

作者Huang, Xiao-zhong1; Liu, Si-si1; Dong, Guang-hui1; Qiang, Ming-rui1; Bai, Zhi-juan1; Zhao, Yan2; Chen, Fa-hu1
刊名PROGRESS IN PHYSICAL GEOGRAPHY
出版日期2017-06-01
卷号41期号:3页码:286-301
关键词Qinghai-Tibetan Plateau Stellera pollen human impact on vegetation Neolithic grazing activity Anthropocene
ISSN号0309-1333
DOI10.1177/0309133317703035
通讯作者Huang, Xiao-zhong(xzhuang@lzu.edu.cn)
英文摘要The ecosystems of the Qinghai-Tibetan Plateau are regarded as being primarily regulated by climate because of the harsh environment of the region and the resulting sparse human population. Recent studies have revealed that Neolithic farmers and nomads extensively settled in the northeastern Qinghai-Tibetan Plateau from 5.2 ka (ka = cal ka BP); however, it is unclear how and to what extent human activity has affected its vegetation. Here we combine the results of the pollen analysis of a sediment core from Genggahai Lake, a shallow lake in Gonghe Basin on the northeastern Qinghai-Tibetan Plateau, with archaeological evidence and use them to assess the extent and nature of human impacts on the regional vegetation during the middle and late Holocene. The pollen record indicates that Stellera, an indicator of the extent of grazing-induced grassland degradation, first appeared at 4.7 ka, expanded during 3.6-3.0 ka, and finally increased significantly after 1.6 ka. In support of this finding, archaeological data indicate that the agro-pastoral Majiayao people arrived at approximate to 5 ka and groups of Kayue people, who practiced pastoralism, intensively colonized the Gonghe Basin and nearby Qinghai Lake basin during 3.6-3.0 ka. After approximate to 1.6 ka, from the Tang Dynasty onwards, human settlement and grazing activity intensified on the northeastern Qinghai-Tibetan Plateau, and this is in accord with the observed high percentages of Stellera in the pollen record. Based on comparison with other records, we conclude that the sediments of Genggahai Lake provide a record of anthropogenic impacts on vegetation, and that human activity may have contributed to regional forest decline during the middle Holocene, and to grassland degradation in the late Holocene. Grassland degradation caused by human activity may be an indicator of the start of the Anthropocene and potentially may have contributed to global climate change via increased dust emission to the atmosphere.
WOS关键词BASIN WESTERN TIBET ; CLIMATE-CHANGE ; SOUTHERN TIBET ; ENVIRONMENTAL-CHANGES ; POLLEN RECORD ; SICHUAN PROVINCE ; CENTRAL CHINA ; LAKE ; MOUNTAINS ; HISTORY
资助项目National Natural Science Foundation of China[41171168] ; National Natural Science Foundation of China[41271219] ; National Natural Science Foundation of China[41620104007]
WOS研究方向Physical Geography ; Geology
语种英语
WOS记录号WOS:000403608600003
出版者SAGE PUBLICATIONS LTD
资助机构National Natural Science Foundation of China
源URL[http://ir.igsnrr.ac.cn/handle/311030/63157]  
专题中国科学院地理科学与资源研究所
通讯作者Huang, Xiao-zhong
作者单位1.Lanzhou Univ, Coll Earth & Environm Sci, Key Lab Western Chinas Environm Syst, Minist Educ, Lanzhou, Gansu, Peoples R China
2.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Beijing, Peoples R China
推荐引用方式
GB/T 7714
Huang, Xiao-zhong,Liu, Si-si,Dong, Guang-hui,et al. Early human impacts on vegetation on the northeastern Qinghai-Tibetan Plateau during the middle to late Holocene[J]. PROGRESS IN PHYSICAL GEOGRAPHY,2017,41(3):286-301.
APA Huang, Xiao-zhong.,Liu, Si-si.,Dong, Guang-hui.,Qiang, Ming-rui.,Bai, Zhi-juan.,...&Chen, Fa-hu.(2017).Early human impacts on vegetation on the northeastern Qinghai-Tibetan Plateau during the middle to late Holocene.PROGRESS IN PHYSICAL GEOGRAPHY,41(3),286-301.
MLA Huang, Xiao-zhong,et al."Early human impacts on vegetation on the northeastern Qinghai-Tibetan Plateau during the middle to late Holocene".PROGRESS IN PHYSICAL GEOGRAPHY 41.3(2017):286-301.

入库方式: OAI收割

来源:地理科学与资源研究所

浏览0
下载0
收藏0
其他版本

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。