Morpho-sedimentary characteristics of Holocene paleochannels in the Upper Rhine alluvial plain, France

<p>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 reconstr...

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Main Authors: M. Abdulkarim, S. Chapkanski, D. Ertlen, H. Mahmood, E. Obioha, F. Preusser, C. Rambeau, F. Salomon, M. Schiemann, L. Schmitt
Format: Article
Language:deu
Published: Copernicus Publications 2022-09-01
Series:Eiszeitalter und Gegenwart
Online Access:https://egqsj.copernicus.org/articles/71/191/2022/egqsj-71-191-2022.pdf
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author M. Abdulkarim
M. Abdulkarim
S. Chapkanski
D. Ertlen
H. Mahmood
E. Obioha
F. Preusser
C. Rambeau
F. Salomon
M. Schiemann
L. Schmitt
author_facet M. Abdulkarim
M. Abdulkarim
S. Chapkanski
D. Ertlen
H. Mahmood
E. Obioha
F. Preusser
C. Rambeau
F. Salomon
M. Schiemann
L. Schmitt
author_sort M. Abdulkarim
collection DOAJ
description <p>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.</p>
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spelling doaj.art-37fcee29a4e84d9fa87f7a2697049f9a2022-12-22T03:12:12ZdeuCopernicus PublicationsEiszeitalter und Gegenwart0424-71162199-90902022-09-017119121210.5194/egqsj-71-191-2022Morpho-sedimentary characteristics of Holocene paleochannels in the Upper Rhine alluvial plain, FranceM. Abdulkarim0M. Abdulkarim1S. Chapkanski2D. Ertlen3H. Mahmood4E. Obioha5F. Preusser6C. Rambeau7F. Salomon8M. Schiemann9L. Schmitt10Institute of Earth and Environmental Science, University of Freiburg, Freiburg, GermanyDepartment of Geology, Federal University Birnin Kebbi, Kebbi, Nigeria​​​​​​​Laboratoire de Géographie Physique (UMR-8591), CNRS/Université Paris 1, Meudon, FranceLaboratoire Image, Ville, Environnement (LIVE UMR 7362), CNRS/Université de Strasbourg/ENGEES, Strasbourg, FranceInstitute of Earth and Environmental Science, University of Freiburg, Freiburg, GermanyInstitute of Earth and Environmental Science, University of Freiburg, Freiburg, GermanyInstitute of Earth and Environmental Science, University of Freiburg, Freiburg, GermanyLaboratoire Image, Ville, Environnement (LIVE UMR 7362), CNRS/Université de Strasbourg/ENGEES, Strasbourg, FranceLaboratoire Image, Ville, Environnement (LIVE UMR 7362), CNRS/Université de Strasbourg/ENGEES, Strasbourg, FranceInstitute of Earth and Environmental Science, University of Freiburg, Freiburg, GermanyLaboratoire Image, Ville, Environnement (LIVE UMR 7362), CNRS/Université de Strasbourg/ENGEES, Strasbourg, France<p>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.</p>https://egqsj.copernicus.org/articles/71/191/2022/egqsj-71-191-2022.pdf
spellingShingle M. Abdulkarim
M. Abdulkarim
S. Chapkanski
D. Ertlen
H. Mahmood
E. Obioha
F. Preusser
C. Rambeau
F. Salomon
M. Schiemann
L. Schmitt
Morpho-sedimentary characteristics of Holocene paleochannels in the Upper Rhine alluvial plain, France
Eiszeitalter und Gegenwart
title Morpho-sedimentary characteristics of Holocene paleochannels in the Upper Rhine alluvial plain, France
title_full Morpho-sedimentary characteristics of Holocene paleochannels in the Upper Rhine alluvial plain, France
title_fullStr Morpho-sedimentary characteristics of Holocene paleochannels in the Upper Rhine alluvial plain, France
title_full_unstemmed Morpho-sedimentary characteristics of Holocene paleochannels in the Upper Rhine alluvial plain, France
title_short Morpho-sedimentary characteristics of Holocene paleochannels in the Upper Rhine alluvial plain, France
title_sort morpho sedimentary characteristics of holocene paleochannels in the upper rhine alluvial plain france
url https://egqsj.copernicus.org/articles/71/191/2022/egqsj-71-191-2022.pdf
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