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岩溶洞穴次生碳酸盐沉积铀及其同位素组成古气候环境研究进展

陈 琼 陈 琳 黄嘉仪 刘淑华 杨 亮 米小建 周厚云

陈 琼, 陈 琳, 黄嘉仪, 刘淑华, 杨 亮, 米小建, 周厚云. 岩溶洞穴次生碳酸盐沉积铀及其同位素组成古气候环境研究进展[J]. 中国岩溶, 2015, 34(5): 479-485. doi: 10.11932/karst20150508
引用本文: 陈 琼, 陈 琳, 黄嘉仪, 刘淑华, 杨 亮, 米小建, 周厚云. 岩溶洞穴次生碳酸盐沉积铀及其同位素组成古气候环境研究进展[J]. 中国岩溶, 2015, 34(5): 479-485. doi: 10.11932/karst20150508
CHEN Qiong, CHEN Lin, HUANG Jia-yi, LIU Shu-hua, YANG Liang, MI Xiao-jian, ZHOU Hou-yun. Progress in the study of paleoclimate reconstruction from speleothem uranium and its isotope[J]. CARSOLOGICA SINICA, 2015, 34(5): 479-485. doi: 10.11932/karst20150508
Citation: CHEN Qiong, CHEN Lin, HUANG Jia-yi, LIU Shu-hua, YANG Liang, MI Xiao-jian, ZHOU Hou-yun. Progress in the study of paleoclimate reconstruction from speleothem uranium and its isotope[J]. CARSOLOGICA SINICA, 2015, 34(5): 479-485. doi: 10.11932/karst20150508

岩溶洞穴次生碳酸盐沉积铀及其同位素组成古气候环境研究进展

doi: 10.11932/karst20150508
基金项目: 国家自然科学基金项目(41473093,41271212,40973009)、教育部博士点基金项目(20124407110012)和中国科学院黄土与第四纪地质国家重点实验室开放基金项目(SKLLQG1431)

Progress in the study of paleoclimate reconstruction from speleothem uranium and its isotope

  • 摘要: 洞穴沉积铀含量及其同位素初始234U/238U[(234U/238U)0]变化均与过去气候环境变化关系密切。文章分别对石笋中U含量和(234U/238U)0的气候意义进行统计分析发现,多数研究认为洞穴沉积U含量和(234U/238U)0可能指示土壤湿度和有效降水变化。然而,不管是对洞穴沉积的U含量还是(234U/238U)0,其气候环境意义解读还存在两种观点。但无论如何,这些研究成果都显示了洞穴沉积的U含量和(234U/238U)0是研究过去气候环境变化的重要替代指标。在未来的研究中,除了土壤环境和过程,还应关注U来源的相对贡献变化和其他微量元素与U元素的关系。这一指标可能在对东亚地区的大气粉尘活动和冬季风演化、地表生物量的变化研究等方面发挥重要作用。

     

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  • 刊出日期:  2015-10-25

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