摘要
对岷江上游地区叠溪古堰塞湖底部沉积物进行AMS14C定年,得到其沉积时间起始时间约为40.5kaBP。通过沉积物粒度特征的研究得知,粒度指标可以反映降水量变化进而反映气候干湿变化,此外,粒度均值曲线与格陵兰冰心(GISP2)及南京葫芦洞石笋氧同位素曲线的显著相似性说明,粒度特征对全球性气候变化有响应,可以反映气候的冷暖变化。由此,研究区古气候演变可以划分为3个阶段:阶段Ⅰ(40.5~33.4kaBP)气候冷干,阶段Ⅱ(33.4~31.7kaBP)气候暖湿,阶段Ⅲ(31.7~31.1kaBP)气候较暖湿。而粒度均值曲线与冰心及石笋氧同位素曲线的差异,一方面可能是由于地理位置的差异,另一方面可能与当时太阳辐射变化情况以及季风作用有关。
The deposition of Diexi ancient barrier lake in the upper reaches of Minjiang River was re-dated by AMS14C dating,and the result shows it started at 40.5 ka BP.The grain-size proxy index can reflect the precipitation and thus the climate dry-wet change.In addition,the obvious comparability between the mean grain-size curve of Diexi Section lacustrine deposits and the δ18O of Greenland ice core and Nanjing Hulu Cave stalagmites shows that the grain-size proxy index could respond to the global climate change,and reflect the chilling and warming.Thus the paleoclimate evolution in the studied area could be divided into three stages:40.5-33.4 ka BP,cold and dry;33.4-31.7 ka BP,warm and humid;31.7-31.1 ka BP,warm and humid,but not as much as the previous stage.The differences between these curves could be interpreted by the variation in location,insolation and monsoon.
出处
《地学前缘》
EI
CAS
CSCD
北大核心
2009年第5期91-98,共8页
Earth Science Frontiers
基金
国家重点基础研究发展计划"973"项目(2006CB701406)
同济大学海洋地质国家重点实验室基金项目
关键词
岷江
叠溪海盆地
堰塞湖
粒度
快速气候变化
Minjiang River
Diexihai Basin
barrier lake
grain-size
rapid climate change