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《Journal of Earth Environment》 2011-05
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The pollen record from the Hongyuan peatland in the Tibetan Plateau since 13500 year

ZHOU Wei-jian;LIU Zhao;WANG Hao;YU Shi-yong;State Key Laboratory of Loess and Quaternary Geology,Institute of Earth Environment,Chinese Academy of Sciences;Xi'an AMS Center;School of Human Settlements and Civil Engineering,Xi'an Jiaotong University;Graduate University of Chinese Academy of Sciences;  
A pollen record with AMS radiocarbon dates from the Hongyuan peatland reveals the long-term dynamics of an alpine wetland ecosystem on the northeastern margin of the Tibetan Plateau over the last13500 years.Changes in pollen assemblages and influxes suggest that local vegetation has experienced three distinct stages,from alpine coniferous forest- meadow(13500 ~ 11500 cal.a BP),through alpine coniferous forest(11500 ~3000 cal.a BP),back to alpine coniferous forest —meadow(3000 cal.a BP-present).This record reflects this study area is mainly influenced by the South Asian monsoon.The pollen record from the Hongyuan peatland is broadly consistent with oxygen isotope records from Donge and Shanbao caves,and highlights differences between Holocene climate histories at Lake Qinghai.The most obvious cause for such variability is the relative contributions made by the South Asian and East Asian monsoon systems.
【Fund】: 国家自然科学基金项目(41023006);; 国家重点基础研究发展计划项目(2010CB833405);; 黄土与第四纪地质国家重点实验室自主部署项目(LQ0704)
【CateGory Index】: P532;Q914
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