植物生态学报 ›› 2010, Vol. 34 ›› Issue (8): 1000-1005.DOI: 10.3773/j.issn.1005-264x.2010.08.013

所属专题: 青藏高原植物生态学:植被生态学

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中国第四纪晚期孢粉记录整理

倪健1,2,*(), 陈瑜1,3, Ulrike HERZSCHUH2, 董丹1,3   

  1. 1中国科学院植物研究所植被与环境变化国家重点实验室, 北京 100093
    2阿尔弗瑞德-魏格纳极地与海洋研究所, 波茨坦 14473
    3中国科学院研究生院, 北京 100049
  • 收稿日期:2009-07-24 接受日期:2009-11-09 出版日期:2010-08-01 发布日期:2010-09-28
  • 通讯作者: 倪健
  • 作者简介:* E-mail: jni@ibcas.ac.cn

Late Quaternary pollen records in China

NI Jian1,2,*(), CHEN Yu1,3, Ulrike HERZSCHUH2, DONG Dan1,3   

  1. 1State Key Laboratory of Vegetation and Environmental Change, Institute of Botany, Chinese Academy of Sciences, Beijing 100093, China
    2Alfred-Wegener-Institute for Polar and Marine Research, Potsdam 14473, Germany
    3Graduate University of Chinese Academy of Sciences, Beijing 100049, China
  • Received:2009-07-24 Accepted:2009-11-09 Online:2010-08-01 Published:2010-09-28
  • Contact: NI Jian

摘要:

孢粉数据库是重建过去植被格局以及研究古气候变化和大气圈-生物圈-人类活动相互关系的基础, 而孢粉取样信息的记录和整理是建立孢粉数据库的重要前提。该文在收集我国1960-2008年发表的孢粉研究文献的基础上, 整理分析了第四纪晚期, 尤其是2万年以来(全新世为主)全国孢粉采样点的信息, 包括采样地点名称、详细采样位置、省份、采样点经纬度和海拔高度、样品类型、取样深度、孢粉样品数量、14C测年数量及年代记录、覆盖的时间段和参考文献。总结发现, 我国目前共有2 324个表土/湖泊表层花粉采样点和987个第四纪晚期的地层沉积剖面和钻孔, 其中高质量的地层孢粉采样点714个。虽然我国以及部分国际上从事第四纪研究的科学家尽了最大努力开展中国疆域的孢粉学研究, 但由于人力、物力以及地形条件的限制, 在我国仍然存在部分孢粉采样的“地理空隙”, 比如北方和西北荒漠地区、青藏高原无人区、中南部山区和东部人类活动频繁区域。然而, 该数据信息库的不断完善, 将为中国第四纪孢粉数据库的建立奠定良好基础。

关键词: 中国孢粉数据库, 地层孢粉, 全新世, 第四纪晚期, 现代花粉

Abstract:

Pollen data are the foundation of reconstructing past vegetation patterns and of studying past climate changes and interactions among atmosphere, biosphere and human activities. We searched for pollen-related literature published and reported from the 1960s to 2008 and collected late Quaternary pollen sampling information for China. We focused on the past 20 000 years before present (aBP), especially the Holocene. Information includes site name, detailed location in text and in latitude, longitude and elevation, sample type, sediment depth, number of pollen samples, radiocarbon dating, time period, and reference. There are 2 324 surface pollen samples from soils and lakes and 987 cores/profiles of sediment fossil records. Among them there are 714 fossil pollen sampling sites with high quality data of pollen and radiocarbon dating. Despite research has been performed by domestic and international paleo-scientists in collecting pollen samples and in Quaternary studies in China, geographical gaps exist due to the limitation of financial support and poor topographical conditions. These include the northern and northwestern desert areas, non-settlement area of the Tibetan Plateau, mountainous areas of middle-southern China and highly disturbed areas of eastern China. More pollen sampling records are needed to update and complete the information database. Such information will greatly benefit the Quaternary Chinese Pollen Database. Furthermore, scientific questions can be addressed based on the databases, such as what the geographical patterns of paleovegetation in China were during the late Quaternary, what were the key times of vegetation shifts (abrupt changes), what were the driving factors of vegetation changes, climate change or human disturbances, and how have vegetation changes influenced local and regional climates?

Key words: Chinese Pollen Database, fossil pollen, Holocene, late Quaternary, modern pollen