Articles | Volume 6, issue 1
https://doi.org/10.5194/esurf-6-121-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/esurf-6-121-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| Highlight paper
| 
05 Mar 2018
Research article | Highlight paper |
| 05 Mar 2018
| 05 Mar 2018
U–Th and 10Be constraints on sediment recycling in proglacial settings, Lago Buenos Aires, Patagonia
Antoine Cogez
CORRESPONDING AUTHOR
University of Lausanne, Institut des Dynamiques de la Surface Terrestre, Quartier Unil-Mouline, Bâtiment Geopolis, 1015 Lausanne, Switzerland
Frédéric Herman
University of Lausanne, Institut des Dynamiques de la Surface Terrestre, Quartier Unil-Mouline, Bâtiment Geopolis, 1015 Lausanne, Switzerland
Éric Pelt
University of Strabourg, Laboratoire d'Hydrologie et de Géochimie de Strasbourg, Strasbourg, France
Thierry Reuschlé
University of Strabourg, Institut de Physique du Globe de Strasbourg, Strasbourg, France
Gilles Morvan
University of Strabourg, Laboratoire d'Hydrologie et de Géochimie de Strasbourg, Strasbourg, France
Christopher M. Darvill
Geography Program and Natural Resources and Environmental Studies Institute, University of Northern British Columbia, 3333 University Way,
Prince George, BC, V2N 4Z9, Canada
Kevin P. Norton
Victoria Univeristy of Wellington, School of Geography, Environment, and Earth Sciences, Wellington, New Zealand
Marcus Christl
Swiss Federal Institute of Zürich, Ion Beam Physics Laboratory, Zürich, Switzerland
Lena Märki
University of Lausanne, Institut des Dynamiques de la Surface Terrestre, Quartier Unil-Mouline, Bâtiment Geopolis, 1015 Lausanne, Switzerland
François Chabaux
University of Strabourg, Laboratoire d'Hydrologie et de Géochimie de Strasbourg, Strasbourg, France
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Cited
18 citations as recorded by crossref.
- The evolution of the Patagonian Ice Sheet from 35 ka to the present day (PATICE) B. Davies et al. 10.1016/j.earscirev.2020.103152
- Cosmogenic (un-)steadiness revealed by paired-nuclide catchment-wide denudation rates in the formerly half-glaciated Vosges Mountains (NE France) T. Jautzy et al. 10.1016/j.epsl.2023.118490
- The last two glacial cycles in central Patagonia: A precise record from the Ñirehuao glacier lobe C. Peltier et al. 10.1016/j.quascirev.2022.107873
- A marine record of Patagonian ice sheet changes over the past 140,000 years J. Hagemann et al. 10.1073/pnas.2302983121
- Pleistocene glacial geomorphology and chronology of the Nahuel Huapi-Limay and Traful catchments, northern Patagonia I. Mizerit et al. 10.1016/j.geomorph.2025.109836
- Field biotite weathering rate determination using U-series disequilibria S. Rihs et al. 10.1016/j.gca.2020.01.023
- Quaternary landscape evolution of patagonia at the Chilean Triple Junction: Climate and tectonic forcings J. Tobal et al. 10.1016/j.quascirev.2021.106960
- Quantifying production rates of tropical granitic regolith in Hainan Island, south China: A multi-stage U-series disequilibrium study G. Jia et al. 10.1016/j.gsf.2025.102002
- The Influence of Climate on the Dynamics of Mountain Building Within the Northern Patagonian Andes E. García Morabito et al. 10.1029/2020TC006374
- Controls on sediment residence times in an Alpine river catchment inferred from uranium isotopes M. Thollon et al. 10.1016/j.epsl.2023.118130
- Extensive mountain glaciation in central Patagonia during Marine Isotope Stage 5 M. Mendelová et al. 10.1016/j.quascirev.2019.105996
- Palaeolake Jeinimeni and ice-marginal geomorphology of the central Patagonian Lago General Carrera/Buenos Aires ice-lobe (46.5°S) J. Pike et al. 10.1016/j.jsames.2024.104985
- A cosmogenic nuclide-derived chronology of pre-Last Glacial Cycle glaciations during MIS 8 and MIS 6 in northern Patagonia T. Leger et al. 10.5194/cp-19-35-2023
- New constraints on the late Quaternary landscape evolution of the eastern Tibetan Plateau from 10Be and 26Al in-situ cosmogenic nuclides Y. Yang et al. 10.1016/j.quascirev.2019.07.020
- Determination of regolith production rates from 238U-234U-230Th disequilibrium in deep weathering profiles (Longnan, SE China) G. Jia et al. 10.1016/j.chemgeo.2021.120241
- The Last Glacial Maximum and Deglacial History of the Seno Skyring Ice Lobe (52°S), Southern Patagonia M. Lira et al. 10.3389/feart.2022.892316
- Uranium-series isotopes as tracers of physical and chemical weathering in glacial sediments from Taylor Valley, Antarctica G. Edwards et al. 10.1016/j.chemgeo.2024.122463
- Modelling the effects of ice transport and sediment sources on the form of detrital thermochronological age probability distributions from glacial settings M. Bernard et al. 10.5194/esurf-8-931-2020
18 citations as recorded by crossref.
- The evolution of the Patagonian Ice Sheet from 35 ka to the present day (PATICE) B. Davies et al. 10.1016/j.earscirev.2020.103152
- Cosmogenic (un-)steadiness revealed by paired-nuclide catchment-wide denudation rates in the formerly half-glaciated Vosges Mountains (NE France) T. Jautzy et al. 10.1016/j.epsl.2023.118490
- The last two glacial cycles in central Patagonia: A precise record from the Ñirehuao glacier lobe C. Peltier et al. 10.1016/j.quascirev.2022.107873
- A marine record of Patagonian ice sheet changes over the past 140,000 years J. Hagemann et al. 10.1073/pnas.2302983121
- Pleistocene glacial geomorphology and chronology of the Nahuel Huapi-Limay and Traful catchments, northern Patagonia I. Mizerit et al. 10.1016/j.geomorph.2025.109836
- Field biotite weathering rate determination using U-series disequilibria S. Rihs et al. 10.1016/j.gca.2020.01.023
- Quaternary landscape evolution of patagonia at the Chilean Triple Junction: Climate and tectonic forcings J. Tobal et al. 10.1016/j.quascirev.2021.106960
- Quantifying production rates of tropical granitic regolith in Hainan Island, south China: A multi-stage U-series disequilibrium study G. Jia et al. 10.1016/j.gsf.2025.102002
- The Influence of Climate on the Dynamics of Mountain Building Within the Northern Patagonian Andes E. García Morabito et al. 10.1029/2020TC006374
- Controls on sediment residence times in an Alpine river catchment inferred from uranium isotopes M. Thollon et al. 10.1016/j.epsl.2023.118130
- Extensive mountain glaciation in central Patagonia during Marine Isotope Stage 5 M. Mendelová et al. 10.1016/j.quascirev.2019.105996
- Palaeolake Jeinimeni and ice-marginal geomorphology of the central Patagonian Lago General Carrera/Buenos Aires ice-lobe (46.5°S) J. Pike et al. 10.1016/j.jsames.2024.104985
- A cosmogenic nuclide-derived chronology of pre-Last Glacial Cycle glaciations during MIS 8 and MIS 6 in northern Patagonia T. Leger et al. 10.5194/cp-19-35-2023
- New constraints on the late Quaternary landscape evolution of the eastern Tibetan Plateau from 10Be and 26Al in-situ cosmogenic nuclides Y. Yang et al. 10.1016/j.quascirev.2019.07.020
- Determination of regolith production rates from 238U-234U-230Th disequilibrium in deep weathering profiles (Longnan, SE China) G. Jia et al. 10.1016/j.chemgeo.2021.120241
- The Last Glacial Maximum and Deglacial History of the Seno Skyring Ice Lobe (52°S), Southern Patagonia M. Lira et al. 10.3389/feart.2022.892316
- Uranium-series isotopes as tracers of physical and chemical weathering in glacial sediments from Taylor Valley, Antarctica G. Edwards et al. 10.1016/j.chemgeo.2024.122463
- Modelling the effects of ice transport and sediment sources on the form of detrital thermochronological age probability distributions from glacial settings M. Bernard et al. 10.5194/esurf-8-931-2020
Latest update: 31 Jul 2025
Short summary
Sediments produced by glaciers are transported by rivers and wind toward the ocean. During their journey, these sediments are weathered, and we know that this has an impact on climate. One key factor is time, but the duration of this journey is largely unknown. We were able to measure the average time that sediment spends only in the glacial area. This time is 100–200 kyr, which is long and allows a lot of processes to act on sediments during their journey.
Sediments produced by glaciers are transported by rivers and wind toward the ocean. During their...
