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应用生态学报 ›› 2000, Vol. ›› Issue (3): 465-471.

• 研究论文 • 上一篇    下一篇

BIOME6000计划:重建古生物群区的最新进展

倪健   

  1. 中国科学院植物研究所植被数量生态学开放研究实验室, 北京100093
  • 收稿日期:1999-06-11 修回日期:1999-08-14 出版日期:2000-05-25
  • 基金资助:
    国家自然科学基金青年基金(39700018);瑞典研究院(SI)奖学金资助项目

BIOME 6000 Project:latest advances of reconstructing palaeobiome

NI Jian   

  1. Laboratory of Quantitative Vegetation Ecology, Institute of Botany, Chinese Academy of Sciences, Beijing 100093
  • Received:1999-06-11 Revised:1999-08-14 Online:2000-05-25

摘要: 描述地球系统过去状态的数据,比如特殊时间段(全新世中期6000aBP和末次盛冰期18000aBP)的孢粉和植物大化石记录,一直是全球变化研究所需要的.以往对这些古生态数据的利用大都是零散的、定点的,对古植被的重建往往也是定性的描述,而国际地圈生物圈计划(IGBP)的国际协作项目BIOME 6000(全球古植被制图计划)的创立,为古生态数据的综合与定量研究开辟了新的途径.该项目特别强调利用古生态学记录模拟重建生物群区的方法论,亦即”生物群区化”(Biomization)方法,通过广泛收集全球有质量保证的古生态记录,以及以现代生态学原理为基础的植物功能型,将植物花粉分类群划分为一个或多个植物功能型,利用植物功能型组合成生物群区类型,以此实现利用古生态数据模拟重建陆地生物群区的全球综合,为耦合的大气圈生物圈模型提供检验的标准和依据.这种趋向将促进其它时间段的生物群区制图,并将推动大气圈生物圈模拟和古数据综合与分析的共同发展.

关键词: BIOME 6000计划, 生物群区化, 古植被格局, 植物功能型, 全新世中期, 末次盛冰期, 全球变化

Abstract: Global change research needs the data about the past states of the Earth system,e.g.,the pollen and plant macrofossil records for specified time slices (for example,the mid Holocene interval, ca 6,000 aBP,and the last glacial maximun,LGM, ca 18,000 aBP).In the past,the utilization of these palaeoecological data is mostly scattered and point fixed,and the reconstruction of palaeovegetation is often qualitatively descriptive.The establishment of international collaboration project BIOME 6000 (a global palaeovegetation mapping program)of the International Geosphere Biosphere Project (IGBP) breaks a new approach for the synthesis and quantitative study of palaeoecological data.In the projescts The methodology of biomization for assigning palaeoeclogical records to biomes is emphasized,in which,plant pollen taxa are assigned to one or more plant functional types (PFTs)by collecting widely global palaeoecological records which have quality assurance,and by using PFT definition based on the principles of modern ecology.Through combining PFTs into biome types,the global synthesis of biomes reconstructed by using palaeoecological data can be realized. The biomization method might provide a benchmark for coupled atmosphere-biosphere.This trend will facilitate biome mapping for other time slices,and co-evolution of atmosphere-biosphere modeling and palaeodata synthesis and analysis will continue.

Key words: BIOME 6000 project, Biomization, Palaeovegetation pattern, Plant functional types, Mid-Holocene, Last glacial maximum, Global change