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Determination of Paleoenvironmental Changes by Using δ 13 C, 14 C Dating and Rb/Sr Ratio in Critical Karst Area of Yunnan-Guizhou Plateau, Southwestern China

Author

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  • Howard Omar Beckford

    (School of Energy and Environmental Engineering, University of Science and Technology Beijing, Beijing 100083, China)

  • Cheng Chang

    (School of Energy and Environmental Engineering, University of Science and Technology Beijing, Beijing 100083, China)

  • Hongbing Ji

    (School of Energy and Environmental Engineering, University of Science and Technology Beijing, Beijing 100083, China
    State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China)

Abstract

Paleosols preserve archives of vegetation history, environmental changes, and sedimentary systems. The changes in vegetation history and environmental conditions in karst areas of the Yunnan–Guizhou plateau of southwestern China since the late Pleistocene were analyzed using δ 13 C, 14 C and the Rb/Sr ratio. Our δ 13 C results reveal the coexistence of C3 and C4 plants (−10.91 to −30.45‰) in soil organic matter, something that is consistent with the present field vegetation assessment. The large vertical difference in the δ 13 C value (>4‰) is related to the cultivation of agricultural crops and to changes in environmental conditions. Furthermore, the variation in δ 13 C values was influenced by the summer monsoon climate of the Indian Ocean and east Asia. We found that total organic carbon (TOC) concentration decreased exponentially with soil depth, indicating high carbon loss. In addition, 14 C apparent age of the soil profiles ranged from modern times to 20,605 (±63) years before the present (yrs. BP) and is positively correlated with soil depth. The combined results indicate that, since the late Pleistocene era, environmental conditions in the study area have changed intermittently on a scale of millennia from hot-humid to cold-dry conditions. We speculate that there may have been extreme climate events in the study area 14,750 years BP, which are marked by a drastic change in δ 13 C and in the Rb/Sr ratio.

Suggested Citation

  • Howard Omar Beckford & Cheng Chang & Hongbing Ji, 2023. "Determination of Paleoenvironmental Changes by Using δ 13 C, 14 C Dating and Rb/Sr Ratio in Critical Karst Area of Yunnan-Guizhou Plateau, Southwestern China," Sustainability, MDPI, vol. 15(8), pages 1-22, April.
  • Handle: RePEc:gam:jsusta:v:15:y:2023:i:8:p:6480-:d:1120792
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    References listed on IDEAS

    as
    1. Cheng Chang & Howard Omar Beckford & Hongbing Ji, 2022. "Indication of Sr Isotopes on Weathering Process of Carbonate Rocks in Karst Area of Southwest China," Sustainability, MDPI, vol. 14(8), pages 1-16, April.
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