Journal of Natural Resources, Volume. 35, Issue 12, 3064(2020)

The response of stalagmite gray-level and isotopes to the climatic events during the last glacial period

Meng WANG1,2,3, Shi-tao CHEN1,2,3、*, Wan-chun HUANG1,2,3, Wen-qin CAI4, Qing-lin GONG1,2,3, Yi-jia LIANG1,2,3, Xian-feng WANG5, and Yong-jin WANG1,2,3
Author Affiliations
  • 1Key Laboratory of Virtual Geographic Environment, Ministry of Education, School of Geography Science, Nanjing Normal University, Nanjing 210023, China
  • 2State Key Laboratory of Cultivation Base of Geographical Environment Evolution (Jiangsu Province), Nanjing 210023, China
  • 3Jiangsu Center for Collaborative Innovation in Geographical Environment Resource Development and Application, Nanjing 210023, China
  • 4Department of Marine Science and Engineering, Nanjing Normal University, Nanjing 210023, China
  • 5Nanyang Technological University, Earth Observatory of Singapore, Singapore 639798, Singapore
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    Figures & Tables(4)
    The monthly precipitation for the four meteorological stations from 1951-2010
    The plain view of Yongxing Cave and the sampling location of YX55
    The δ13C, δ18O and gray-level records and the polished section of YX55 stalagmite
    Comparison of gray-level, δ13C and δ18O records of YX55 with other paleoclimatic records
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    Meng WANG, Shi-tao CHEN, Wan-chun HUANG, Wen-qin CAI, Qing-lin GONG, Yi-jia LIANG, Xian-feng WANG, Yong-jin WANG. The response of stalagmite gray-level and isotopes to the climatic events during the last glacial period[J]. Journal of Natural Resources, 2020, 35(12): 3064

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    Paper Information

    Received: May. 24, 2019

    Accepted: --

    Published Online: May. 8, 2021

    The Author Email: CHEN Shi-tao (chenshitao@njnu.edu.cn)

    DOI:10.31497/zrzyxb.20201220

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