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《科学通报(英文版)》 2003-03
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Surface pollen and vegetation reconstruction from central and northern mountains of Taiwan

YU Ge1, LIEW Pingmei2, XUE Bin1 & LI Zhengyi2 1. Nanjing Institute of Geography & Limnolog of the Chinese Academof Sciences, Nanjing 210008, China; 2. Department of Geology, Taiwan University, Taibei 106-17, Taiwan, China  
Surface pollen from various montane vegeta-tions in Shalixian Mt. and Lepei Mt. of central and northern Taiwan have been explored and analyzed. The pollen datawere used to simulate vegetation types by using the biomisa-tion technique. Computing three matrixes of pollen taxa,plant functional types and combined biomes, vegetation types at each site have been finally defined through the fuzselections of a tie-breaking rule. The results show that sur-face pollen data can simulate the subtropical Castanopsis andCyclobalanopsis forests, alpine warm-temperate Quercus and Quercus-Pinus forests, and alpine temperate/cool-temperate conifers of Tsuga-Picea and Picea-Abies forests. Simulatedelevations of the forests are similar to actual locations of the forests. This study can add vertical surface pollen data forextending investigation of various vegetation types in China, provide PFT schemes and vegetation types in low-latitude and montane areas, and be applied as modern analogues for fossil pollen in order to reconstruct Quaternary vegetations
【CateGory Index】: Q948.1
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1 CHEN Yu1, 2 and NI Jian1 1State Key Laboratory of Vegetation and Environmental Change, Institute of Botany, Chinese Academy of Sciences, Beijing 100093, China, and 2Graduate University of Chinese Academy of Sciences, Beijing 100049, China;QUANTITATIVE PALAEOVEGETATION RECONSTRUCTION AT LARGE SCALE BASED ON POLLEN RECORDS[J];Journal of Plant Ecology;2008-05
Chinese Journal Full-text Database 1 Hits
1 Yu Ge and Wang Su min (Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008);STUDIES OF THE CLIMATIC DYNAMICS FOR THE MID- HOLOCENE VEGETATIONAL CHANGES IN CHINA[J];ACTA MICROPALAEONTOLOGICA SINICA;2000-02
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