全新世大暖期时中国夏季风向西北大幅度漂移的一个古生物地层学证据  

A bio-stratigraphy evidence of summer monsoon drift on a large scale toward NW China during the Holocene Megathermal

作　　者：李保生[1,2] HOFMANN Jürgen 陈德牛[4] 温小浩[1] 闫满存[5] ZHANG David Dian 牛东风[1] 李志文[7] 邱世藩[8] 王丰年[1] 杜恕环[1] 

机构地区：[1]华南师范大学地理科学学院,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,西安710075 [3]Leibniz Institute of Freshwater Ecology and Inland Fisheries [4]中国科学院动物研究所,北京100080 [5]中国人民解放军第二炮兵部队第三研究所,北京100085 [6]香港大学地理系 [7]中山大学地理科学与规划学院,广州510275 [8]中国科学院广州地球化学研究所,广州510640

出　　处：《地球环境学报》2010年第2期133-138,共6页Journal of Earth Environment

基　　金：国家重点基础研究发展计划(973计划)(2010CB833405)

摘　　要：巴丹吉林沙漠东南部边缘巴丹海子全新世大暖期6-9kaBP的湖相沉积中含有大量腹足类化石——Radix cucunorica （Moellendorff）, Succinea erythrophana Ancey, Gyraulus sibricus （Dunker）, Radix lagotis （Schranck）, Gyraulus albus（Miiller）, Lymnaea stagnalis（Linnaeus）,Gyraulus convexiusculus （HuRon）,除Succinea erythrophana Ancey属陆生蜗牛外，余皆为淡水腹足类。这些化石代表了当时温暖湿润的气候环境。其中，现生的Gyraulus convexiusculus （Hutton）生活的最NW位置为地处暖温带的南泥湾，据此推知，6-9kaBP时的巴丹海子的气温和降水至少较今分别高出1．1℃和440mnl；从南泥湾至巴丹海子，气候带向NW移动了差不多700km；那时夏季风暖锋位置可向NW移动到从玉门其以NE走向至额济纳旗及其以北的中蒙国界一线，夏季风的波及范围可以漂越甘新交界的深居内陆的星星峡。The lacustrine sediment contains a great amount of gasteropod fossils of the Holocene Megathermal （6-9 ka BP） of the Badanhaizi Lower Land located at southeastern margin of Badainjaran Desert, China. These are Radix cucunorica （Moellendorff）, Succinea erythrophana Ancey, Gyraulus sibricus （Dunker）, Radix lagotis （Schranck）, Gyraulus albus（Muller）, Lymnaea stagnalis（Linnaeus）,Gyraulus convexiusculus （Hutton）, in which, except terraneous Succinea erythrophana Ancey, the rest belongs to freshwater gasteropods. They indicate then warm-humid climate, among which the existent northwesternmost of the extant Gyraulus convexiusculus （Hutton） is of Nanniwan of Shanxi Province of Chinese warm temperate belt. Hence, it is assumed that during 6-9 ka B. P. the annual average temperature and precipitation of Badanhaizi probably were respectively 1.1 ℃ and 440 mm higher than those of the present-day; from Nanniwan to Badanhaizi, the climate belt almost migrated northwestward 700 kin; the warm front of summer monsoon may moved to northwestward the range from Yumen to Ejin Qi in NE strike and further to the Sino-Mongolia boundary at that time, and its influencing extension probably attained to Xingxingxia, the inner continent, of the boundary between Gansu and Xinjiang, China.

关 键 词：全新世大暖期 巴丹吉林沙漠东南缘 巴丹海子剖面 6~9 ka BP 腹足类化石 夏季风暖锋位置 

分 类 号：P534.632[天文地球—第四纪地质学] P532[天文地球—古生物学与地层学]