Climate Control on Erosion: Evolution of Sediment Flux From Mountainous Catchments During a Global Warming Event, PETM, Southern Pyrenees, Spain

Abstract Extreme hydroclimates impact sediment fluxes from mountainous catchments to the oceans. Given modern global warming, a challenge is to assess the sensitivity of erosion in mountainous catchments to extreme climate perturbations. Here, we reconstruct paleo‐sedimentary fluxes across an abrupt global warming, the Paleocene‐Eocene Thermal Maximum (PETM, ∼56 Ma), using sedimentary archives and numerical modeling. In the Tremp Basin (Southern Pyrenees, Spain), our results demonstrate that depositional volumetric rates of siliciclastic sediments increased two‐fold during the PETM. According to the BQART and stream power law models, changes in mean annual temperature and precipitation explain only 9%–27% of the flux increase. This comparison between field data and model predictions suggests that even with high uncertainty on paleoclimate data, extreme rainfall events and landslides may have been crucial sediment generation processes during the PETM. This is consistent with predictions of enhanced climate variability in a warmer world, leading to significant sediment flushing.

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Publication Details

Journal
Geophysical Research Letters
Published
2025-04-05
DOI
https://doi.org/10.1029/2024gl112404
Citations
3
Primary Topic
Soil erosion and sediment transport
Type
article
Field-Weighted Citation Impact
3.56

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article

Climate Control on Erosion: Evolution of Sediment Flux From Mountainous Catchments During a Global Warming Event, PETM, Southern Pyrenees, Spain

Amanda Wild, Fritz Schlunegger, Jean Braun, Charlotte Fillon et al.
3 citations
Geophysical Research Letters
Soil erosion and sediment transport
3.56
article

Climate Control on Erosion: Evolution of Sediment Flux From Mountainous Catchments During a Global Warming Event, PETM, Southern Pyrenees, Spain

Amanda Wild, Fritz Schlunegger, Jean Braun, Charlotte Fillon, Jonah S. McLeod, Alexander C. Whittaker, Romain Vaucher, Sébastien Castelltort A, Tor O. Sømme, Cécile Robin, Luca Claude Malatesta, Rocio Jaimes‐Gutierrez, Marine Prieur
article en
3 citations

Abstract

Abstract Extreme hydroclimates impact sediment fluxes from mountainous catchments to the oceans. Given modern global warming, a challenge is to assess the sensitivity of erosion in mountainous catchments to extreme climate perturbations. Here, we reconstruct paleo‐sedimentary fluxes across an abrupt global warming, the Paleocene‐Eocene Thermal Maximum (PETM, ∼56 Ma), using sedimentary archives and numerical modeling. In the Tremp Basin (Southern Pyrenees, Spain), our results demonstrate that depositional volumetric rates of siliciclastic sediments increased two‐fold during the PETM. According to the BQART and stream power law models, changes in mean annual temperature and precipitation explain only 9%–27% of the flux increase. This comparison between field data and model predictions suggests that even with high uncertainty on paleoclimate data, extreme rainfall events and landslides may have been crucial sediment generation processes during the PETM. This is consistent with predictions of enhanced climate variability in a warmer world, leading to significant sediment flushing.

Geophysical Research LettersVol. 52(7)
Total (France) (FR), University of Geneva (CH), University of Bern (CH), Géosciences Rennes (FR), GFZ Helmholtz Centre for Geosciences (DE), Imperial College London (GB), Equinor (Norway) (NO), Université de Rennes (FR)
European Commission, Horizon 2020 Framework Programme
Openalex Percentile: Top 9%
Soil erosion and sediment transport
3.56
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