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Erosion rates on subalpine paleosurfaces in the western Mediterranean by in-situ 10Be concentrations in granites: implications for surface processes and long-term landscape evolution in Corsica (France)

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Abstract

A study of erosion rates by in-situ 10Be concentrations in granites of Miocene high-elevation paleosurfaces in Corsica indicates maximum erosion rates between 8 and 24 mm/kyear. The regional distribution of measured erosion rates indicates that the local climatic conditions, namely precipitation, the petrographic composition of granites, and the degree of brittle deformation govern erosion rates. Chemical erosion dominates even at elevations around 2,000 m in presently subalpine climate conditions. Field evidence indicates that erosion operates by continuous dissolution and/or disintegration to grains (grusification). The erosion rates are relatively high with respect to the preservation of inferred Early Miocene landscapes. We infer temporal burial in the Middle Miocene and significantly lower erosion rates in the Neogene until ∼3 Ma to explain the preservation of paleosurfaces, in line with fission track data. Valley incision rates that are a magnitude higher than erosion rates on summit surfaces result in relief enhancement and long-term isostatic surface uplift. On the other hand, widening and deepening of valleys by cyclic glaciation progressively destroys the summit surface relics.

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Notes

  1. http://www.meteofrance.com/FR/montagne/obs.jsp?LIEUID = MONT_MANIC

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Acknowledgments

This study has been funded by the German Science Foundation (DFG Project Ku 1298/2). We are obliged to Martin Staiger for technical support in core drilling on top of tors and Gerlinde Kost, Dagmar Höckh and Dorothea Mühlbayer-Renner for purification of quartz samples. We thank Greg Balco (Seattle) for technical advice for quartz purification, and Peter Kubik (Zürich) for measuring the exposure age of a Holocene roche moutonnée. The samples were processed by Ingrid Krumrei in the frame of DFG Project Ku 1298/7. Constructive reviews by Peter Molnar, Robert Anderson, and anonymous reviewers helped to improve an earlier version of this paper. The present manuscript benefitted from reviews of Derek Fabel, Kevin Norton and Friedhelm v. Blanckenburg.

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  1. University of Tübingen, Institute of Geosciences, Sigwartstrasse 10, 72076 , Tübingen, Germany

    Joachim Kuhlemann, Paul D. Bons, Martin Danišík & Wolfgang Frisch

  2. Subatomic Physics Department, Van de Graaff Laboratory, Utrecht University, P.O. Box 80.000, 3508 TA, Utrecht, The Netherlands

    Klaas van der Borg

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  1. Joachim Kuhlemann
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Correspondence to Joachim Kuhlemann.

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Kuhlemann, J., van der Borg, K., Bons, P.D. et al. Erosion rates on subalpine paleosurfaces in the western Mediterranean by in-situ 10Be concentrations in granites: implications for surface processes and long-term landscape evolution in Corsica (France). Int J Earth Sci (Geol Rundsch) 97, 549–564 (2008). https://doi.org/10.1007/s00531-007-0169-z

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