2017 Vol. 44, No. 5
Article Contents

CAO Jianhua, JIANG Zhongcheng, YUAN Daoxian, XIA Riyuan, ZHANG Cheng. 2017. The progress in the study of the karst dynamic system and global changes in the past 30 years[J]. Geology in China, 44(5): 874-900. doi: 10.12029/gc20170504
Citation: CAO Jianhua, JIANG Zhongcheng, YUAN Daoxian, XIA Riyuan, ZHANG Cheng. 2017. The progress in the study of the karst dynamic system and global changes in the past 30 years[J]. Geology in China, 44(5): 874-900. doi: 10.12029/gc20170504

The progress in the study of the karst dynamic system and global changes in the past 30 years

    Fund Project: Supported by National Key Research and Development Plan of China (No. 2016YFC0502500), Key Project of National Natural Scientific Foundation of China (No. 41530316), Innovational Program on Geological Environment of China Geological Survey, and IGCP project 661 entitled"Processes, Cycle, and Sustainability of the Critical Zone in Karst Systems"
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  • Author Bio: CAO Jianhua, male, born in 1963, doctor, majors in the basic and applied fundamental research on karst ecosystem, karst carbon cycle and rocky desertification integrated treatment; E-mail: jhcaogl@karst.ac.cn
  • Carbonate rock is the material basis of karst development. It recorded some environmental changes, stored most carbon and played an important role in the primitive atmosphere and life evolution during the earth evolution. Karst covers 22×106 km2 of the whole world, possessing~15% of the continent surface. The effects of the karst process on climate and environmental changes are considerable, and hence the karst dynamic system (KDS) is an important component of the Earth's Surface System. In this paper, the authors made a review on the progress of the karst science in the past 30 years, which includes the conception, intention and development of the karst dynamics, geological and ecological mechanisms of driving the KDS, and some new results and findings in the fields of KDS and carbon cycle, water cycle and calcium cycle. Finally, the karst critical zone and global karst was introduced.

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