Morpho-sedimentary characteristics of Holocene paleochannels in the Upper Rhine alluvial plain, France
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2022
- handle: 10670/1.2r5gjk
- hal: hal-03779738
- doi: 10.5194/egqsj-71-191-2022
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info:eu-repo/semantics/altIdentifier/doi/10.5194/egqsj-71-191-2022
info:eu-repo/semantics/OpenAccess
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Mubarak Abdulkarim et al., « Morpho-sedimentary characteristics of Holocene paleochannels in the Upper Rhine alluvial plain, France », HAL-SHS : géographie, ID : 10.5194/egqsj-71-191-2022
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Résumé
The French Upper Rhine alluvial plain is characterized by a complex system of paleochannels inherited from Late Glacial to Holocene fluvial dynamics of the Rhine and Ill river systems, among other smaller rivers. These paleochannels represent valuable archives for understanding and reconstructing the fluvial and landscape evolution of the area. However, the Holocene temporal trajectories of the paleochannels, in response to a range of environmental changes, remain poorly understood. This study presents a detailed and systematic mapping and characterization of an extensive network of paleochannels spanning the entire width (19 km) of a reach of the central French Rhine plain. Based on qualitative and quantitative lidar analysis, field investigations, and provenance investigations of paleochannel infill sequences, five distinct paleochannel groups (PG 1 to PG 5) were identified in the study area. These paleochannel groups differ considerably regarding their channel patterns, morphological characteristics, and sedimentary sources of the infilling sediments. The interpretation of the different datasets indicates that the development of these different paleomorphologies is attributed to significant changes in hydro-geomorphodynamic processes in the area during the Holocene, especially lateral migrations of the Rhine and Ill rivers. The findings reported here are promising and will have significant implications for reconstructing the long-term (Late Glacial to Holocene) evolution of the Upper Rhine fluvial hydrosystem in response to various controlling factors.