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River terraces along the Liujiang River in Southwest China and their implications for understanding fluvial processes on the Guizhou Plateau since the Late Pleistocene

Published online by Cambridge University Press:  13 March 2025

Huan Qian Open the ORCID record for Huan Qian [Opens in a new window] ,
Xi Jiang ,
Hua Chen ,
Renchang Mi ,
Gary G. Lash  and
Huan Li Open the ORCID record for Huan Li [Opens in a new window]
Huan Qian
Affiliation:
College of Resources and Environmental Engineering, Key Laboratory of Karst Georesources and Environment, Ministry of Education, Guizhou University, Guiyang, Guizhou 550025, China
Xi Jiang*
Affiliation:
College of Resources and Environmental Engineering, Key Laboratory of Karst Georesources and Environment, Ministry of Education, Guizhou University, Guiyang, Guizhou 550025, China Guizhou Karst Environmental Ecosystems Observation and Research Station, Guizhou University, Guiyang, Guizhou 550025, China
Hua Chen
Affiliation:
College of Resources and Environmental Engineering, Key Laboratory of Karst Georesources and Environment, Ministry of Education, Guizhou University, Guiyang, Guizhou 550025, China
Renchang Mi
Affiliation:
College of Resources and Environmental Engineering, Key Laboratory of Karst Georesources and Environment, Ministry of Education, Guizhou University, Guiyang, Guizhou 550025, China
Gary G. Lash
Affiliation:
Department of Geosciences, State University of New York, Fredonia, New York 14063, USA
Huan Li
Affiliation:
Key Laboratory of Metallogenic Prediction of Nonferrous Metals and Geological Environment Monitoring, Ministry of Education, School of Geosciences and Info-Physics, Central South University, Changsha, Hunan 410083, China
*
Corresponding author: X. Jiang; Email: xjiang@gzu.edu.cn
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Abstract

River terraces serve as excellent indicators of the landform evolution of the Guizhou Plateau. This paper presents the results of terrace investigation and optically stimulated luminescence (OSL) dating focused on five sections along the Liujiang River of the southeastern Guizhou Plateau. The OSL ages of the terraces range from 0.21 ± 0.02 to 16.0 ± 1.4 ka for the first terraces (T1) and from 3.5 ± 0.3 to 26.5 ± 3.3 ka for the second terraces (T2), which are much younger than those of other basins on the Guizhou Plateau. These ages, considered in tandem with the results of previous investigations, enhance our understanding of the fluvial landform evolution of the Guizhou Plateau since the Late Pleistocene. On the Guizhou Plateau platform, terraces are considered to be the response of river evolution to tectonic uplift, indicating a relatively slow geomorphic process. In the slope zone, climate change has had a significant impact on the fluvial landform processes, driving the formation of the younger terraces along the Liujiang River. In the platform–slope transition zone, the evolution of terraces was driven by both tectonic uplift and climate change, where the landform processes were dominated by strong headward erosion.

Keywords

River terraceOSL datinggeomorphic evolutiontectonic upliftGuizhou Plateau

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Type
Research Article
Information
Quaternary Research , Volume 125 , May 2025 , pp. 118 - 133
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© The Author(s), 2025. Published by Cambridge University Press on behalf of Quaternary Research Center

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