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Towards quantificat...
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Li, FurongLinnéuniversitetet,Institutionen för biologi och miljö (BOM)
(author)
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
- Article/chapterEnglish2020
Publisher, publication year, extent ...
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Elsevier,2020
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printrdacarrier
Numbers
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LIBRIS-ID:oai:DiVA.org:lnu-95381
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https://urn.kb.se/resolve?urn=urn:nbn:se:lnu:diva-95381URI
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https://doi.org/10.1016/j.earscirev.2020.103119DOI
Supplementary language notes
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Language:English
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Summary in:English
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Subject category:ref swepub-contenttype
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Subject category:for swepub-publicationtype
Notes
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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.
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Gaillard, Marie-José,1953-Linnéuniversitetet,Institutionen för biologi och miljö (BOM)(Swepub:lnu)egama
(author)
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Cao, XianyongHelmholtss Ctr Polar & Marine Res, Germany;Chinese Acad Sci, China
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Herzschuh, UlrikeHelmholtss Ctr Polar & Marine Res, Germany
(author)
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Sugita, ShinyaTallinn Univ, Estonia
(author)
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Tarasov, Pavel E.Free Univ Berlin, Germany
(author)
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Wagner, MaykeGerman Archaeol Inst, Germany
(author)
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Xu, QinghaiHebei Normal Univ, China
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Ni, JianZhejiang Normal Univ, China
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Wang, WeimingChinese Acad Sci, China
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Zhao, YanChines E Acad Sci, China;Univ Chinese Acad Sci, China
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An, ChengbangLanzhou Univ, China
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Beusen, A. H. W.Univ Utrecht, Netherlands;PBL Netherlands Environm Assessment Agcy, Netherlands
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Chen, FahuChinese Acad Sci, China
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Feng, ZhaodongHenan Univ, China
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Goldewijk, C. G. M. KleinPBL Netherlands Environm Assessment Agcy, Netherlands;Univ Utrecht, Netherlands
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Huang, XiaozhongLanzhou Univ, China
(author)
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Li, YuecongHebei Normal Univ, China
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Li, YuLanzhou Univ, China
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Liu, HongyanPeking Univ, China
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Sun, AizhiUniv Chinese Acad Sci, China
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Yao, YifengChinese Acad Sci, China
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Zheng, ZhuoSun Yat Sen Univ, China
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Jia, XinNanjing Normal Univ, China
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LinnéuniversitetetInstitutionen för biologi och miljö (BOM)
(creator_code:org_t)
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In:Earth-Science Reviews: Elsevier203, s. 1-250012-82521872-6828
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Li, Furong
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Gaillard, Marie- ...
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Cao, Xianyong
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Herzschuh, Ulrik ...
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Sugita, Shinya
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Tarasov, Pavel E ...
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Wagner, Mayke
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Xu, Qinghai
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Ni, Jian
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Wang, Weiming
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Zhao, Yan
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An, Chengbang
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Beusen, A. H. W.
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Chen, Fahu
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Feng, Zhaodong
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Goldewijk, C. G. ...
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Huang, Xiaozhong
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Li, Yuecong
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Li, Yu
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Liu, Hongyan
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Sun, Aizhi
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Yao, Yifeng
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Zheng, Zhuo
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Jia, Xin
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Linnaeus University