安徽蓬莱仙洞不同滴水点差异PCP作用及其古气候记录研究意义
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  • 英文篇名:Prior Calcite Precipitation at Different Drip-water Sites in Penglaixian Cave,Anhui Province and the Paleoclimatic Implications
  • 作者:李吉龙 ; 段武辉 ; 吴江滢
  • 刊名:第四纪研究
  • 英文刊名:Quaternary Sciences
  • 出版日期:2014-07-31
  • 出版单位:第四纪研究
  • 机构:南京师范大学地理科学学院;中国科学院地质与地球物理研究所新生代地质与环境重点实验室;
  • 年:2014
  • 期:04
  • 基金:国家自然科学基金项目(批准号 ; 41030103)资助
  • CN:11-2708/P
  • ISSN:1001-7410
  • 页:225-226
  • 页数:2
  • 分类号:P532;P641.134
  • 语种:中文;
  • 文件大小:507K
摘要
<正>石笋由于分布广泛、定年准确,并且具有丰富的气候和环境代用指标(如氧碳稳定同位素~([1,2])、微层厚度~([3])、微量元素~([4~6])等),因而受到古气候学家广泛关注。其中,微量元素和稳定碳同位素常被用来间接地反映局地干湿变化。当降水减少时,洞穴滴水在洞顶储存时间较长,使岩溶水在补给石笋之前已经发生了方解石沉积作用。由于Mg,Sr和Ba在方解石和溶液中的分配系数远小于1~([7,8]),从而使Ca优先于Mg,Sr和Ba沉积出来,使得溶液(渗流水及其所形成的滴水)和现代次生碳酸盐沉积物中的Mg,Sr和Ba富集,进而导致Mg/Ca,Sr/Ca和Ba/Ca比值增大~([4,5,9]),这种现象被称为方解石前期沉积作用(Prior Calcite Precipitation,简称PCP)。此外,当降水减少,洞穴滴水滴率变慢(即PCP作用增强)时,CO_2脱气时间增长也会导致石笋碳同位素偏
        
引文
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