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Volume 41 Issue 4
Aug.  2022
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Article Navigation >  CARSOLOGICA SINICA  > 2022  >  41(4): 660-674
XU Yuzhen, LI Tingyong, LI Junyun, YANG Yan. Progress in reconstruction of karst rocky desertification by stalagmite δ13C[J]. CARSOLOGICA SINICA, 2022, 41(4): 660-674. doi: 10.11932/karst2022y11
Citation: XU Yuzhen, LI Tingyong, LI Junyun, YANG Yan. Progress in reconstruction of karst rocky desertification by stalagmite δ13C[J]. CARSOLOGICA SINICA, 2022, 41(4): 660-674. doi: 10.11932/karst2022y11
shu

Progress in reconstruction of karst rocky desertification by stalagmite δ13C

doi: 10.11932/karst2022y11
  • 1.

    Chongqing Key Laboratory of Karst Environment/School of Geographical Sciences, Southwest University, Chongqing 400715, China

  • 2.

    Yunnan Key Laboratory of Plateau Geographical Processes & Environmental Changes/Faculty of Geography, Yunnan Normal University, Kunming, Yunnan 650500, China

  • Received Date: 2022-01-20
    Abstract
  • The formation and evolution mechanism of karst rocky desertification is a scientific problem that has been paid increasing attention, and the ecological environment in karst areas is not only fragile, but also unstable. Therefore, the study of karst rocky desertification is of practical significance for the restoration of ecological environment in karst areas. Cave stalagmite δ13C is affected by many factors and can respond sensitively to the changes of surface ecological environment and karst hydrological conditions. Hence, the use of stalagmites δ13C on the study of evolution history of ecological environment in karst areas has become an important direction. In this paper, we discuss the main factors affecting stalagmite δ13C from two aspects, i.e., the overlying surface environment and cave deposition. Combining the results of modern cave monitoring with model simulation, we analyze the main factors and mechanisms affecting δ13C in cave drop water and sediment. Under the influence of multiple factors, the environmental significance of stalagmites δ13C has multiple implications. According to the published research results, in this paper, we summarize the indicative significance of stalagmite δ13C from three aspects, different time scales, different regional distribution, and different cave sedimentary environments. In order to accurately interpret the environmental significance of stalagmite δ13C, we put forward the solutions-comprehensive analysis, modern monitoring and model simulation. In this paper, we discuss the concept, genesis, development process and environmental effects of karst rocky desertification, and analyze the close relationship between surface rocky desertification and stalagmite δ13C records in caves. We also summarize published research results about the application of stalagmites δ13C to the reconstruction of regional rocky desertification. Meanwhile, we discuss main problems faced in the current research, (1) How to interpret the indicative meaning of stalagmite δ13C correctly? This problem is the premise that stalagmite δ13C can be used to reconstruct the history of regional rocky desertification. (2) Spatially, the area of the overlying surface reflected by stalagmites δ13C records is limited, so it is necessary for us to carefully consider whether the selected stalagmite region reflects the same spatial distribution as that of the study area, and whether it represents the environmental changes of the target study area, when using stalagmite δ13C to reconstruct the evolution history of rocky desertification in a certain region. (3) Karst rocky desertification can develop rapidly on the decadal time scale, while a certain age error may occur in stalagmite dating. Can stalagmite δ13C record sensitively record the changes of surface environment in such a short period and reconstruct the process of regional rocky desertification? In order to accurately reconstruct the regional karst environment and the evolution history of rocky desertification, we put forward the following suggestions, (1) In order to avoid the uncertainty of stalagmite δ13C in paleo-environment reconstruction, the comparative analysis of stalagmite δ13C and δ18O, trace elements and mineral structure can be integrated with modern monitoring and model simulation to correctly interpret the indicative significance of stalagmite δ13C. On this basis, the karst hydrological process can be reconstructed more accurately and the evolution history of rocky desertification can be determined. (2) By comparing the evolution process of rocky desertification recorded by stalagmites from multiple caves in the study area and multiple stalagmites from the same cave, the regional representativeness of single stalagmite record can be reduced. (3) Multi-index stalagmite records with high resolution and high precision chronological control can accurately record the changes of the land surface environment during the rapid occurrence and development of the rocky desertification process.

     

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