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作 者:牛东风[1] 李保生[1,2] 魏建国[3] 温小浩[1] 舒培仙 司月君[1]
机构地区:[1]华南师范大学地理科学学院,广东广州510631 [2]中国科学院地球环境研究所黄土与第四纪地质国家重点实验室,陕西西安710061 [3]山东省菏泽市国土资源局土地监管中心,山东菏泽274000
出 处:《地球化学》2016年第2期155-163,共9页Geochimica
基 金:国家重点基础研究发展计划(2013CB955903);国家自然科学基金(41471159)
摘 要:萨拉乌苏河流域米浪沟湾剖面全新世地层MGS1层段记录了11个由风成砂与河流相或湖沼相构成的沉积旋回。对该层段63个样品的Rb、Sr数据进行了分析,结果显示由沙丘砂至上覆河湖相Rb和Sr含量由低增高,而Rb/Sr比值的分布则显示出与Rb和Sr含量变化相反的趋势,三者与平均粒径Mz(?)的相关系数都在0.43以上。研究表明MGS1至少经历了11次冷干和11次暖湿的气候波动。米浪沟湾剖面MGS1记录的千年尺度气候波动既是对东亚季风环流演变历史的体现,同时也是对全球气候与环境变化的响应。The MGS 1 stratigraphical segment of Milanggouwan section is located in the Salawusu River Valley of southeast Mu Us Desert. The segment documents 11 sedimentary cycles consisting of aeolian facies and fluvial facies or lacustrine-swamp facies. Totally 63 samples were analyzed for rubidium (Rb) and strontium (Sr) concentrations. The results show that Rb and Sr concentrations increase as the sediments vary from aeolian facies to lacustrine-swamp facies, however, variation of the Rb/Sr ratios shows reversed trends in contrast to that of Rb and Sr concentrations. The line correlation coefficients of Rb and Sr concentrations and Rb/Sr ratios with mean grain size are all above 0.43. All these indicate that the MGS 1 stratigraphic segment at least records 11 cold-dry and 11 warm-humid millennium-scale climatic oscillations, which represent the evolution history of East Asian monsoon circulation and show good correspondence to global climatic and environment variations.
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