甘肃省临夏盆地更新世早期湖泊沉积孢粉记录的古气候演化  

EARLY PLEISTOCENE LACUSTRINE SPORE-POLLEN RECORDS AND EVOLUTION OF PALEOCLIMATE IN LINXIA BASIN, GANSU PROVINCE, CHINA

作　　者：董铭[1,2] 方小敏[3] 史正涛[1,2] 明庆忠[1,2] 苏怀[1,2] 

机构地区：[1]云南师范大学旅游与地理科学学院,昆明650092 [2]云南省高原地理过程与环境变化重点实验室,昆明650092 [3]中国科学院青藏高原研究所,北京100085

出　　处：《第四纪研究》2011年第1期104-111,共8页Quaternary Sciences

基　　金：国家自然科学委-云南省人民政府联合资助基金项目(批准号:U0933604);云南省科技计划项目(批准号:2007D199M);国家自然科学基金项目(批准号:40872118和40871018)联合资助

摘　　要：根据孢粉组合特征,将临夏盆地早更新统东山组(2.50～1.76Ma)的孢粉划分为3个孢粉带(含6个亚带),即3个植被、气候阶段:第一阶段(2.50～1.91Ma,带Ⅰ),植被类型是以柏科、榆属和禾本科为优势种的温带森林,气候表现为温凉稍干,并有逐渐干旱化的趋势。第二阶段(1.91～1.80Ma,带Ⅱ)是以云杉属、榆属和禾本科为主的温带森林,气候冷湿;尤其在1.89～1.87Ma期间,云杉林面积最大,气候最为湿润;第三阶段(1.80～1.76Ma,带Ⅲ),植被类型为以云杉属、梣属和禾本科为主的温带森林,云杉林面积逐渐减小,禾本科逐渐增加,气候逐渐干旱。In most of Chinese Northern areas, the Early Pleistocene is one of the important transition period, before which the climate was relative warm and humid in the Tertiary and after which the extremely arid environment in the Later Quaternary developed. It is of great significant theoretical basis and scientific foundation to establish the ecological and climatic change sequence in this period, which can improve our understanding of the arid evolution trend in the northwest of China and predict its future climatic change and the rule of development. Linxia Basin, which located at the northeast rim of the Tibet Plateau, is the intersection zone of eastern monsoon area, northwest arid area and Tibet Plateau alpine-cold area. Continuous and complete Upper Cenozoic strata are well developed in this basin. So it was one of the ideal areas for extracting information of the ecological evolution and climatic change in the North West China since the Late Cenozoic Era. We present a continuous 78m thick Dongshanding Paleo-lake sediment section based mainly on clayey siltstone and siltstone, which is situated at Jinggou township Dongshanding village （35 °35＇N, 103 °04＇E, an elevation of 2429.5m）. According to previous research results, the formation age of the section is 2. 50 - 1. 76Ma. 88 spore-pollen samples were collected systematically with the sampling interval of 1.0m besides 0.5m individually. The result of the identification showed that 91% samples pollen amount attained statistical standard among them. Pollen types belong to 44 families and 57 genera, which includes Arbor trees pollen, such as Pinus, Picea, Cupressceae, Juniperus, Quercus, Betula, Fraxinus, and Shrub and Herb pollen, such as Poaceae,Amnthemis type,Aster type,Artemisia, Chenopodiaceae. In the whole section, Arbor trees pollen（ 37.0% -98.5%, average of 66.9% ）absolute dominated, suggesting forest landscape in Linxia Basin during 2.50 - 1.76Ma. According to variation characteristics of spore-pollen assemblage,Dongshanding Formation （Don

关 键 词：孢粉组合 临夏盆地 早更新世 古气候 

分 类 号：P534.631[天文地球—第四纪地质学] Q944.571[天文地球—古生物学与地层学]