孢粉学定量重建古气候方法探讨  

Numerical Techniques of Spore-pollen Data Analysis on Paleoclimate Reconstruction

作　　者：潘安定[1] 陈碧姗[1] 刘会平[1] 杨木壮[1] 王志英[1] 

机构地区：[1]广州大学地理科学学院,广州510006

出　　处：《热带地理》2008年第6期493-497,共5页Tropical Geography

基　　金：国家自然科学基金资助项目(批准号:40671187);广东省自然科学基金项目(000301)

摘　　要：运用多种数学方法分析孢粉资料定量重建古环境已成为第四纪古环境研究的一个发展趋势。目前被广泛应用的主要有孢粉复合度-气候转换函数、孢粉-气候因子转换函数、孢粉-气候对应分析、孢粉-气候响应面模型、共存因子分析等方法。由于各种分析方法各具特色,并有各自的适用范围和局限性,因此孢粉资料的分析处理,一般都需要使用多种方法互相补充,互相印证,从而使结果更准确、客观。通过对各种方法实际应用的对比分析发现,随着定量重建古气候方法的不断改进,研究结果的准确度和精度在不断提高,推动了孢粉学和古植被定量重建研究手段的引进和应用。With the wide application of computers and the development of quaternary paleoenvironment studies, many numerical techniques are used in the spore-pollen analysis. Pollen compound-climate transfer function, pollen-climate factors transfer function, pollen-climate correspondence analysis, pollen-climate response surface model and the coexistence approach are adopted to explain paleoenviroments. Because different analysis techniques have respective characteristics, the applicable ranges and limits, the numerical analysis methods should supplement and confirm each other, to make the result of quantitative analysis precise and objectivity, and the subjective randomness can be eliminated. By comparison, it is found that the accuracy of researchs is getting improved along with the ameliorating of quantitative methods for paleoclimate reconstruction, which promotes the application of new artifices in Palynology and paleoenviroment reconstruction researchs.

关 键 词：孢粉数据 定量分析 古气候重建 

分 类 号：P532[天文地球—古生物学与地层学]