Sources of karst cave deposits in Xiaodong Cave in Cangyuan, Southwest Yunnan

SHI Lin; YANG Qing; LIU Lianwen; ZHANG Jin; ZHENG Yan; ZHANG Yu; YANG Wanshu; ZOU Zining; ZHENG Hongbo

doi:10.16562/j.cnki.0256-1492.2024011701

Marine Geology & Quaternary Geology > 2024 > 44(2): 81-96. > DOI: 10.16562/j.cnki.0256-1492.2024011701

SHI Lin，YANG Qing，LIU Lianwen，et al. Sources of karst cave deposits in Xiaodong Cave in Cangyuan, Southwest Yunnan[J]. Marine Geology & Quaternary Geology，2024，44(2)：81-96. DOI: 10.16562/j.cnki.0256-1492.2024011701

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Sources of karst cave deposits in Xiaodong Cave in Cangyuan, Southwest Yunnan

1.
Yunnan Key Laboratory of Earth System Science, Yunnan University, Kunming 650500, China
2.
Yunnan Provincial Key Laboratory of Digital Humanities Technology Research and Development and Application, School of History and Archives, Yunnan University, Kunming 650032, China
3.
School of Earth Sciences and Engineering. Nanjing University, Nanjing 210023, China
4.
Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China
5.
Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing 100044, China

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Received Date: January 16, 2024
Revised Date: March 09, 2024
Accepted Date: March 09, 2024
Available Online: April 24, 2024

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Abstract

Abstract

Karst caves are valuable locations for studying prehistoric human activities during the Quaternary Period. Analyzing the depositional characteristics and provenance of clastic deposits in karst caves is crucial for understanding the evolutionary history of the depositional environment and shedding light on past human behaviors. Xiaodong Cave in Cangyuan, Southwest Yunnan was studied to unveil the source of clastic sediments. The grain size and mineralogical features of various clay minerals within and around the cave were analyzed. Results show that the cave sediments came mainly from the sediments in higher places outside the cave through sheet flow as shown in grain size characteristics. In addition, a small amount of insoluble material from limestone and materials formed after further weathering and pedogenesis were also accumulated. Overall, there might be four periods of further weathering and pedogenesis. Moreover, there were limestone breccias and rock debris fallen off from cave walls, from which four events of accumulation of limestone breccia or debris were recognized. The latest accumulation was obviously affected by human activities, to which sufficient attention should be paid in research works.
- karst cave deposits,
- source tracking,
- grain size,
- clay minerals

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References (78)

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