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 |
DOI | 10.1016/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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