Articles | Volume 4, issue 2
https://doi.org/10.5194/gchron-4-455-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/gchron-4-455-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Cosmogenic nuclide weathering biases: corrections and potential for denudation and weathering rate measurements
Richard F. Ott
CORRESPONDING AUTHOR
Earth Surface Geochemistry, GFZ German Centre for Geoscience Research, Potsdam, Germany
Sean F. Gallen
Department of Geosciences, Colorado State University, Fort Collins,
CO, USA
Darryl E. Granger
Department of Earth, Atmospheric, and Planetary Sciences, Purdue
University, Purdue, IN, USA
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We compile data on carbonate denudation, the sum of mechanical erosion and chemical weathering, from cosmogenic nuclides and use them in conjunction with weathering data to constrain the partitioning of denudation into erosion and weathering. We show how carbonate erosion and weathering respond to different climatic and tectonic conditions and find that variations in denudation partitioning can be used to explain the vastly different morphology of carbonate landscapes on Earth.
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The Klados River catchment contains seemingly overlarge, well-preserved alluvial terraces and fans. Unlike previous studies, we argue that the deposits formed in the Holocene based on their position relative to a paleoshoreline uplifted in 365 CE and seven radiocarbon dates. We also find that constant sediment supply from high-lying landslide deposits disconnected the valley from regional tectonics and climate controls, which resulted in fan and terrace formation guided by stochastic events.
William Kearney, Gina Arnau, Theophil Bringezu, Michael Dietze, Boris Gailleton, Anna-Lena Lamprecht, Kilian Lenz, Richard Ott, Dirk Scherler, Philippe Steer, and Wolfgang Schwanghart
EGUsphere, https://doi.org/10.5194/egusphere-2026-2478, https://doi.org/10.5194/egusphere-2026-2478, 2026
This preprint is open for discussion and under review for Earth Surface Dynamics (ESurf).
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TopoToolbox is a software package that enables users to analyze maps of the Earth's surface. The newest version of TopoToolbox makes it accessible to more users, makes it easier to integrate TopoToolbox with other software used to study the Earth's surface and establishes a new development process to ensure that TopoToolbox continues to meet the needs of its community of users. We present a series of examples to demonstrate how users can incorporate the new TopoToolbox version into their work.
Angus K. Moore and Darryl E. Granger
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Cosmogenic nuclide geochronology requires accurately scaling production rates with altitude. The energy spectrum of cosmic radiation changes with altitude, and reactions that are sensitive to different energies may have different scaling behavior. Here, we model the altitude scaling of 36Cl production from Fe and evaluate this model against calibration data. The data are broadly consistent with the prediction of larger-altitude scaling factors for 36Cl from Fe than for other reactions.
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We compile data on carbonate denudation, the sum of mechanical erosion and chemical weathering, from cosmogenic nuclides and use them in conjunction with weathering data to constrain the partitioning of denudation into erosion and weathering. We show how carbonate erosion and weathering respond to different climatic and tectonic conditions and find that variations in denudation partitioning can be used to explain the vastly different morphology of carbonate landscapes on Earth.
Elena T. Bruni, Richard F. Ott, Vincenzo Picotti, Negar Haghipour, Karl W. Wegmann, and Sean F. Gallen
Earth Surf. Dynam., 9, 771–793, https://doi.org/10.5194/esurf-9-771-2021, https://doi.org/10.5194/esurf-9-771-2021, 2021
Short summary
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The Klados River catchment contains seemingly overlarge, well-preserved alluvial terraces and fans. Unlike previous studies, we argue that the deposits formed in the Holocene based on their position relative to a paleoshoreline uplifted in 365 CE and seven radiocarbon dates. We also find that constant sediment supply from high-lying landslide deposits disconnected the valley from regional tectonics and climate controls, which resulted in fan and terrace formation guided by stochastic events.
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Short summary
Cosmogenic nuclides are a tool to quantify denudation – the total removal of mass from near the Earth's surface. Chemical weathering can introduce biases to cosmogenic-nuclide-based denudation rates measurements. Here, we investigate the effects of weathering on cosmogenic nuclides and develop tools to correct for this influence. Our results highlight which additional measurements are required to determine accurate denudation rates in regions where weathering is not negligible.
Cosmogenic nuclides are a tool to quantify denudation – the total removal of mass from near the...