globalchange  > 气候变化与战略
DOI: 10.1016/j.earscirev.2020.103119
论文题名:
Towards quantification of Holocene anthropogenic land-cover change in temperate China: A review in the light of pollen-based REVEALS reconstructions of regional plant cover
作者: Li F.; Gaillard M.-J.; Cao X.; Herzschuh U.; Sugita S.; Tarasov P.E.; Wagner M.; Xu Q.; Ni J.; Wang W.; Zhao Y.; An C.; Beusen A.H.W.; Chen F.; Feng Z.; Goldewijk C.G.M.K.; Huang X.; Li Y.; Li Y.; Liu H.; Sun A.; Yao Y.; Zheng Z.; Jia X.
刊名: Earth Science Reviews
ISSN: 00128252
出版年: 2020
卷: 203
语种: 英语
中文关键词: Climate change ; HYDE ; Land-use history ; Pollen-vegetation modelling ; Relative pollen productivities
英文关键词: anthropogenic effect ; climate change ; Holocene ; land cover ; land use ; pollen ; quantitative analysis ; temperate environment ; vegetation cover ; China
英文摘要: In an attempt to quantify Holocene anthropogenic land-cover change in temperate China, we 1) applied the REVEALS model to estimate plant-cover change using 94 pollen records and relative pollen productivity for 27 plant taxa, 2) reviewed earlier interpretation of pollen studies in terms of climate- and human-induced vegetation change, and 3) reviewed information on past land use from archaeological studies. REVEALS achieved a more realistic reconstruction of plant-cover change than pollen percentages in terms of openland versus woodland. The study suggests successive human-induced changes in vegetation cover. The first signs of human- induced land-cover change (crop cultivation, otherwise specified) are found c. 7 ka BP in the temperate deciduous forest, and S and NE Tibetan Plateau (mainly grazing, possibly crop cultivation), 6.5–6 ka BP in the temperate steppe and temperate desert (grazing, uncertain), and 5.5–5 ka BP in the coniferous-deciduous mixed forest, NE subtropical region, and NW Tibetan Plateau (grazing). Further intensification of anthropogenic land-cover change is indicated 5–4.5 ka BP in the E temperate steppe, and S and NE Tibetan Plateau (grazing, cultivation uncertain), 3.5–3 ka BP in S and NE Tibetan Plateau, W temperate steppe, temperate desert (grazing), and NW Tibetan Plateau (probably grazing), and 2.5–2 ka BP in the temperate deciduous forest, N subtropical region, and temperate desert (grazing). These changes generally agree with increased human activity as documented by archaeological studies. REVEALS reconstructions have a stronger potential than biomization to evaluate scenarios of anthropogenic land-cover change such as HYDE, given they are combined with information from archaeological studies. © 2020 LINNAEUS UNIVERSITY
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/166143
Appears in Collections:气候变化与战略

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作者单位: Department of Biology and Environmental Science, Linnaeus University, Kalmar, 39182, Sweden; Alfred Wegener Institute Helmholtz Center for Polar and Marine Research, Research Unit Potsdam, Potsdam, 14473, Germany; Institute of Ecology, University of Tallinn, Tallinn, 10120, Estonia; Section Paleontology, Institute of Geological Sciences, Free University of Berlin, Berlin, 12249, Germany; Eurasia Department, German Archaeological Institute, Berlin, 14195, Germany; College of Resources and Environment Science, Hebei Normal University, Shijiazhuang, 050024, China; College of Chemistry and Life Sciences, Zhejiang Normal University, Jinhua, 321004, China; Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing, 210008, China; Institute of Geographic Sciences and Natural Resources Research, Chines e Academy of Sciences, Beijing, 100101, China; University of Chinese Academy of Sciences, Beijing, 100101, China; College of Earth and Environmental Sciences, Lanzhou University, Lanzhou, 730000, China; Faculty of Geosciences, Department of Earth Sciences - Geochemistry, Utrecht University, Utrecht, TA 3508, Netherlands; PBL Netherlands Environmental Assessment Agency, The Hague, 2500 GH, Netherlands; Key Laboratory of Alpine Ecology (LAE), CAS Center for Excellence in Tibetan Plateau Earth Sciences, Institute of Tibetan Plateau Research, Chinese Academy of Sciences(CAS), Beijing, 100101, China; College of Environment and Planning, Henan University, Zhengzhou, 475001, China; Faculty of Geosciences, Copernicus Institute of Sustainable Development, Environmental Sciences Group, Utrecht University, Utrecht, 3508 TA, Netherlands; College of Urban and Environmental Sciences and MOE Laboratory for Earth Surface Processes, Peking University, Beijing, 100871, China; Institute of Botany, Chinese Academy of Sciences, Beijing, 100093, China; School of Earth Sciences and Engineering, Sun Yat-sen University, Guangzhou, Guangdong 510275, China; School of Geography, Nanjing Normal University, Nanjing, 210023, China

Recommended Citation:
Li F.,Gaillard M.-J.,Cao X.,et al. Towards quantification of Holocene anthropogenic land-cover change in temperate China: A review in the light of pollen-based REVEALS reconstructions of regional plant cover[J]. Earth Science Reviews,2020-01-01,203
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