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Volume 33 Issue 1
Mar.  2014
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Article Contents
LIU Zi-qi, XIONG Kang-ning, LI Gao-cong, XIAO Shi-zhen, WANG Ling-yu, WANG Heng-song, LUO Ding. Geomorphologic value and contributions of the Huanjiang Karst Extension to South China Karst World Heritage[J]. CARSOLOGICA SINICA, 2014, 33(1): 64-76. doi: 10.3969/j.issn.1001-4810.2014.01.011
Citation: LIU Zi-qi, XIONG Kang-ning, LI Gao-cong, XIAO Shi-zhen, WANG Ling-yu, WANG Heng-song, LUO Ding. Geomorphologic value and contributions of the Huanjiang Karst Extension to South China Karst World Heritage[J]. CARSOLOGICA SINICA, 2014, 33(1): 64-76. doi: 10.3969/j.issn.1001-4810.2014.01.011

Geomorphologic value and contributions of the Huanjiang Karst Extension to South China Karst World Heritage

doi: 10.3969/j.issn.1001-4810.2014.01.011
  • Received Date: 2014-01-23
  • Publish Date: 2014-03-25
  • “South China Karst” is a serial World Natural Heritage site, nominated in phases by the government of China to the UNESCO World Heritage Committee. In this paper, based on the geomorphologic characteristic research of Huanjiang Karst, is compared with Libo Karst and other sites of “South China Karst”. It is concluded that: (1) Huanjiang Karst and Libo Karst have the same geomorphic landscape type-cone karst. (2) The extension adds the geomorphologic rejuvenation value to Libo Karst. (3) Huanjiang Karst in the nomination will make an important addition to the integrity problem about the boundary of the southern buffer zone of Libo Karst World Heritage Site, resulting from the administrative boundary between Guizhou and Guangxi Provinces, including geology and geomorphology, biology and ecology, natural landscape, etc., further more meeting the integrity requirements of world heritage; (4) In the history of South China karst, Libo-Huanjiang Karst recorded the sedimentary history of the second cycle of carbonate rocks. After experiencing the transformation processes of karst landforms from Dongwu, Indosinian and Neotectonic movements, they represent the cone karst landform in the transition zone from the Yunnan-Guizhou Plateau to the Guilin Basin in southern China and the ongoing evolution process of cone karst geomorphology. It is the model site for tropical-subtropical cone karst in the world.

     

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