中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Plant Diversity Changes During the Middle Miocene in the Lunpola Basin, Tibetan Plateau

文献类型:期刊论文

作者Wu, Bingyue2,3; Li, Quan2,3; Sun, Jimin1,2
刊名DIVERSITY-BASEL
出版日期2026-03-19
卷号18期号:3页码:187
关键词Tibetan Plateau Lunpola Basin Middle Miocene pollen and spores Hill numbers plant diversity
DOI10.3390/d18030187
产权排序1
文献子类Article
英文摘要The Tibetan Plateau (TP) experienced significant climatic transitions and tectonic uplift during the Middle Miocene. Little is known about plant diversity changes and their relationship with climatic and tectonic processes in spite of extensive reconstructions of vegetation change over this period. Based on palynological assemblages spanning similar to 15-12 Ma from the Lunpola Basin, we quantitatively reconstruct the evolution of plant diversity around the Middle Miocene Climatic Transition (MMCT) in the central TP. Plant taxa richness and evenness of three groups of tree, shrub and herb, and pteridophyte are estimated using Hill numbers methods. Three distinct diversity phases are identified. From similar to 15 to 14.2 Ma, plant richness gradually increased while evenness decreased, possibly due to the development of vertical vegetation zones driven by the uplift of the central TP. From similar to 14.2 to 13.8 Ma, richness dropped sharply in response to rapid climatic deterioration in the MMCT. From similar to 13.8 to 12 Ma, both richness and evenness increased under fluctuations, associated with paleo-lake shrinkage and expansion of lakeside wetlands caused by persistent plateau uplift and climatic aridification. Long-term changes in plant diversity within the Lunpola Basin were influenced by global climate changes, the uplift of central TP, and regional hydrological dynamics during the Middle Miocene. Our findings provide paleoecological insights into the coevolution of TP growth, climate change, hydrological process, and biodiversity of alpine ecosystem.
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WOS关键词PALYNOLOGICAL EVIDENCE ; SPECIES-DIVERSITY ; BIODIVERSITY ; TEMPERATE ; EVENNESS ; RECORD ; EXTRAPOLATION ; RAREFACTION ; OLIGOCENE ; RICHNESS
WOS研究方向Biodiversity & Conservation ; Environmental Sciences & Ecology
语种英语
WOS记录号WOS:001727308600001
出版者MDPI
源URL[http://ir.igsnrr.ac.cn/handle/311030/221576]  
专题陆地表层格局与模拟院重点实验室_外文论文
通讯作者Li, Quan
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher & Environm Coevolut, Beijing 100029, Peoples R China
2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China;
3.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Land Surface Pattern & Simulat, Beijing 100101, Peoples R China;
推荐引用方式
GB/T 7714
Wu, Bingyue,Li, Quan,Sun, Jimin. Plant Diversity Changes During the Middle Miocene in the Lunpola Basin, Tibetan Plateau[J]. DIVERSITY-BASEL,2026,18(3):187.
APA Wu, Bingyue,Li, Quan,&Sun, Jimin.(2026).Plant Diversity Changes During the Middle Miocene in the Lunpola Basin, Tibetan Plateau.DIVERSITY-BASEL,18(3),187.
MLA Wu, Bingyue,et al."Plant Diversity Changes During the Middle Miocene in the Lunpola Basin, Tibetan Plateau".DIVERSITY-BASEL 18.3(2026):187.

入库方式: OAI收割

来源:地理科学与资源研究所

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