Monsoonal imprint on late Quaternary landscapes of the Rub’ al Khali Desert

Abundant geomorphological, biological, and isotopic records show that Arabia repeatedly underwent significant climate-driven environmental changes during late Quaternary humid periods. Precisely mapping how the enhancement and expansion of the African Monsoon during these humid periods have affected landscape evolution and human occupation dynamics in Arabia remains a scientific challenge. Here we reconstruct an ancient water-sculpted landscape consisting of lake and river deposits, coupled with a large outlet valley in the Rub' al Khali Desert of Saudi Arabia. During the peak of the Holocene Humid Period or before, intense rainfall reactivated alluvial floodplains and filled a ~1100 km² topographic depression, which eventually breached, carving a deep ~150 km-long valley. Coupling geologic reconstructions with transient Earth system model simulations shows that this hydrological activity was linked to higher seasonal precipitation punctuated by repeated heavy events. Analysis of lacustrine and fluvial sedimentary deposits implies sediment routing across distances of up to 1000 km from the Asir Mountains. Our results indicate that such intense flooding challenges the conventional view of simple, weak, and linear landscape stabilization following increased rainfall in Arabia. Our findings highlight the crucial role of an enhanced African Monsoon in driving rapid landscape transformations in the Arabian Desert.

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Publication Details

Journal
Communications Earth & Environment
Published
2025-04-03
DOI
https://doi.org/10.1038/s43247-025-02224-1
Citations
2
Primary Topic
Geology and Paleoclimatology Research
Type
article
Field-Weighted Citation Impact
2.60

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article

Monsoonal imprint on late Quaternary landscapes of the Rub’ al Khali Desert

Hany Khalil, Negar Haghipour, Omar Wani, Michael D. Petraglia et al.
2 citations
Communications Earth & Environment
Geology and Paleoclimatology Research
2.60
article

Monsoonal imprint on late Quaternary landscapes of the Rub’ al Khali Desert

Hany Khalil, Negar Haghipour, Omar Wani, Michael D. Petraglia, Sébastien Castelltort A, Abdallah S. Zaki, Guillaume Baby, Anne Dallmeyer, Antoine Delaunay, Pietro Sternai, Cécile Blanchet, Giovan Peyrotty, Mathieu Schuster, Abdulkader M. Afifi, Frans van Buchem, Sam Woor, Mohamed R. Ali, Florence Sylvestre
article en
2 citations

Abstract

Abundant geomorphological, biological, and isotopic records show that Arabia repeatedly underwent significant climate-driven environmental changes during late Quaternary humid periods. Precisely mapping how the enhancement and expansion of the African Monsoon during these humid periods have affected landscape evolution and human occupation dynamics in Arabia remains a scientific challenge. Here we reconstruct an ancient water-sculpted landscape consisting of lake and river deposits, coupled with a large outlet valley in the Rub' al Khali Desert of Saudi Arabia. During the peak of the Holocene Humid Period or before, intense rainfall reactivated alluvial floodplains and filled a ~1100 km² topographic depression, which eventually breached, carving a deep ~150 km-long valley. Coupling geologic reconstructions with transient Earth system model simulations shows that this hydrological activity was linked to higher seasonal precipitation punctuated by repeated heavy events. Analysis of lacustrine and fluvial sedimentary deposits implies sediment routing across distances of up to 1000 km from the Asir Mountains. Our results indicate that such intense flooding challenges the conventional view of simple, weak, and linear landscape stabilization following increased rainfall in Arabia. Our findings highlight the crucial role of an enhanced African Monsoon in driving rapid landscape transformations in the Arabian Desert.

Communications Earth & EnvironmentVol. 6(1)
Ain Shams University (EG), University of Geneva (CH), Griffith University (AU), California Institute of Technology (US), Centre National de la Recherche Scientifique (FR), Planetary Science Institute (US), National Museum of Natural History (US), University of British Columbia (CA), The University of Queensland (AU), University of the Fraser Valley (CA), ETH Zurich (CH), Institut National de Recherche pour l'Agriculture, l'Alimentation et l'Environnement (FR), Centre de Recherche et d’Enseignement de Géosciences de l’Environnement (FR), GFZ Helmholtz Centre for Geosciences (DE), Max Planck Institute for Meteorology (DE), Institut de Recherche pour le Développement (FR), New York University (US), University of Milano-Bicocca (IT), Université de Strasbourg (FR), King Abdullah University of Science and Technology (SA), Alexandria University (EG), The University of Texas at Austin (US)
Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung
Openalex Percentile: Top 13%
Geology and Paleoclimatology Research
2.60
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