我国上更新统至全新统千年尺度气候地层划分研究进展  

Research of Millennial-scale' Climatic Stratigraphic Division on Upper Pleistocene-Holocene Series in China and Research Progress

作　　者：李保生[1] 温小浩[1] 王丰年[2] 郭元军[1] 李忠云[1] 郭亿华[3] 司月君[4] 牛东风[1] 胡观冠[1] 郑春红[1] 

机构地区：[1]华南师范大学地理科学学院,广东广州510631 [2]惠州学院旅游学院,广东惠州516007 [3]广州地理研究所,广东广州510070 [4]河南师范大学旅游学院,河南新乡453007

出　　处：《华南师范大学学报（自然科学版）》2013年第6期171-181,共11页Journal of South China Normal University(Natural Science Edition)

基　　金：国家重大科学研究计划项目(2013CB955903);国家自然科学基金重大项目(41290250)

摘　　要：基于对最近20年来国际上更新统至全新统千年尺度气候地层划分认识的基础,粗略解析了2012年编制的过去270 ka以来区域年代地层对比表,并评述了我国上更新统至全新统千年尺度气候地层划分与研究进展.对于气候变化不稳定性的原因,列举了一些学者对其驱动机制的看法,并倾向地认为千年尺度变化是在地球外部太阳活动强迫因子影响下与地球气候系统内部耦合发生的气候的震荡.Based on the international research on division of Upper Pleistocene-Holocene millennial-scale climate strata in the latest 20 years, the regional chronostratigraphy comparison table for the past 270 ka compiled in 2012 is analyzed, and division of Upper Pleistocene-Holocene millennial-scale climate strata and research progress in China are reviewed. To the reasons of climate instability, a number of scholars view that accounted for the driving mechanism are cited, and the conclusion that millennial-scale climate changes were climate oscillations caused by the forcing factors of solar activity outside the Earth coupling with the Earth inner climate system is drawn.

关 键 词：中国 上更新统至全新统 千年尺度气候地层 划分 

分 类 号：P532[天文地球—古生物学与地层学]