中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Pollen-based biome reconstruction on the Qinghai-Tibetan Plateau during the past 15,000 years

文献类型:期刊论文

作者Li, Zhen4; Wang, Yongbo4; Herzschuh, Ulrike2,3,5; Cao, Xianyong6; Ni, Jian7; Zhao, Yan1
刊名PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
出版日期2022-10-15
卷号604页码:12
ISSN号0031-0182
关键词Biomization Pollen Vegetation migration Qinghai-Tibetan Plateau Holocene
DOI10.1016/j.palaeo.2022.111190
通讯作者Wang, Yongbo(yongbowang@cnu.edu.cn)
英文摘要Reconstruction of past vegetation change is critical for better understanding the potential impact of future global change on the fragile alpine ecosystems of the Qinghai-Tibetan Plateau (QTP). In this paper, pollen assemblages comprising 58 records from the QTP, spanning the past 15 kyrs, were collected to reconstruct biome compositions using a standard approach. Six forest biomes were identified mainly on the southeastern plateau, exhibiting a pattern of gradual expansion along the eastern margin during early to mid-Holocene times. The alpine meadow biome was separately identified based on an updated scheme, and showed notable westward expansions towards lower latitudes and higher altitudes during early Holocene times. Consistent patterns of migration could also be identified for the alpine steppe biome, which moved eastward during the late Holocene after 4 ka. As the dominant biome type, temperate steppe was distributed widely over the QTP with minor migration patterns, except for a progressive expansion to lower altitudes in the late Holocene times. The desert biome was inferred mainly as covering the northwestern plateau and the Qaidam Basin, in relatively restricted areas. The spatial distribution of the reconstructed biomes represent the large-scale vegetation gradient on the QTP. Monsoonal precipitation expressed predominant controls on the development of alpine ecosystems, while the variations in desert vegetation responded to regional moisture brought by the mid-latitude Westerlies. Temperature changes played relatively minor roles in the variations of alpine vegetation, but exerted more significant impacts on the forest biomes.
WOS关键词HOLOCENE MONSOON CLIMATE ; BASIN WESTERN TIBET ; MID-LATE HOLOCENE ; ASIAN MONSOON ; VEGETATION CHANGES ; PALEOENVIRONMENTAL CHANGES ; ALPINE ECOSYSTEM ; HIGH-RESOLUTION ; WATER RELATIONS ; HURLEG LAKE
资助项目National Natural Science Foundation of China[41877282] ; National Natural Science Foundation of China[41861134030]
WOS研究方向Physical Geography ; Geology ; Paleontology
语种英语
出版者ELSEVIER
WOS记录号WOS:000861228300001
资助机构National Natural Science Foundation of China
源URL[http://ir.igsnrr.ac.cn/handle/311030/185377]  
专题中国科学院地理科学与资源研究所
通讯作者Wang, Yongbo
作者单位1.Inst Geog Sci & Nat Resources Res, Beijing 100101, Peoples R China
2.Univ Potsdam, Inst Environm Sci & Geog, D-14476 Potsdam, Germany
3.Helmholtz Ctr Polar & Marine Res, Res Unit Potsdam, Alfred Wegener Inst, D-14473 Potsdam, Germany
4.Capital Normal Univ, Coll Resource Environm & Tourism, Beijing 100048, Peoples R China
5.Univ Potsdam, Inst Biochem & Biol, D-14476 Potsdam, Germany
6.Chinese Acad Sci, Inst Tibetan Plateau Res, State Key Lab Tibetan Plateau Earth Syst Resources, Grp Alpine Paleoecol & Human Adaptat ALPHA, Beijing 100101, Peoples R China
7.Zhejiang Normal Univ, Coll Chem & Life Sci, Jinhua 321004, Peoples R China
推荐引用方式
GB/T 7714
Li, Zhen,Wang, Yongbo,Herzschuh, Ulrike,et al. Pollen-based biome reconstruction on the Qinghai-Tibetan Plateau during the past 15,000 years[J]. PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,2022,604:12.
APA Li, Zhen,Wang, Yongbo,Herzschuh, Ulrike,Cao, Xianyong,Ni, Jian,&Zhao, Yan.(2022).Pollen-based biome reconstruction on the Qinghai-Tibetan Plateau during the past 15,000 years.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,604,12.
MLA Li, Zhen,et al."Pollen-based biome reconstruction on the Qinghai-Tibetan Plateau during the past 15,000 years".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 604(2022):12.

入库方式: OAI收割

来源:地理科学与资源研究所

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