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Significant increase in relief of the European Alps during mid-Pleistocene glaciations

Nature Geoscience volume 4, pages 688–692 (2011)Cite this article

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Abstract

Some of Earth’s greatest relief occurs where glacial processes act on mountain topography1,2. This dramatic landscape is thought to be an imprint of Pleistocene glaciations3,4. However, whether the net effect of glacial erosion on mountains is to increase5,6,7 or decrease8,9,10 relief remains disputed. It has been suggested that in the European Alps, the onset of widespread glaciation since the mid-Pleistocene climate transition11 led to the growth of large, long-lived and strongly erosive alpine glaciers12,13 that profoundly influenced topography14. Here we use 4He/3He thermochronometry15 and thermal-kinematic models to show that the Rhône Valley in Switzerland deepened by about 1–1.5 km over the past one million years. Our results indicate that while the valley was incised and back-cut, high-altitude areas were preserved from erosion. We find an approximately two-fold increase in both local topographic relief and valley concavity, which occurred around the time of the mid-Pleistocene transition. Our results support the proposed link12,13,14 between the onset of efficient glacial erosion in the European Alps and the transition to longer, colder glacial periods at the middle of the Pleistocene epoch.

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Figure 1: Topography, sample locations and AHe age–elevation relationships.
Figure 2: 4He/3He thermochronometry of SIO samples.
Figure 3: Modelled cooling paths for VIS samples.
Figure 4: Predicted cooling paths for different exhumation/relief scenarios and inferred Rhône valley evolution.

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References

  1. Brocklehurst, S. H. & Whipple, K. X. Response of glacial landscapes to spatial variations in rock uplift rate. J. Geophys. Res. 112, F02035 (2007).

    Article  Google Scholar 

  2. Meigs, A. & Sauber, J. Southern Alaska as an example of the long-term consequences of mountain building under the influence of glaciers. Quat. Sci. Rev. 19, 1543–1562 (2000).

    Article  Google Scholar 

  3. Penck, A. Glacial features in the surface of the Alps. J. Geol. 13, 1–19 (1905).

    Article  Google Scholar 

  4. Molnar, P. & England, P. Late Cenozoic uplift of mountain ranges and global climate change: Chicken or egg? Nature 346, 29–34 (1990).

    Article  Google Scholar 

  5. Montgomery, D. R. Valley formation by fluvial and glacial erosion. Geology 30, 1047–1050 (2002).

    Article  Google Scholar 

  6. Small, E. E. & Anderson, R. S. Geomorphically driven late Cenozoic rock uplift in the Sierra Nevada, California. Science 270, 277–280 (1995).

    Article  Google Scholar 

  7. Shuster, D. L., Cuffey, K. M., Sanders, J. W. & Balco, G. Thermochronometry reveals headward propagation of erosion in an alpine landscape. Science 332, 84–88 (2011).

    Article  Google Scholar 

  8. Brozovic, N., Burbank, D. & Meigs, A. Climatic limits on landscape development in the northwestern Himalaya. Science 276, 571–574 (1997).

    Article  Google Scholar 

  9. Egholm, D. L., Nielsen, S. B., Pedersen, V. K. & Lesemann, J-E. Glacial effects limiting mountain height. Nature 460, 884–887 (2009).

    Article  Google Scholar 

  10. Whipple, K. X., Kirby, E. & Brocklehurst, S. H. Geomorphic limits to climate induced increases in topographic relief. Nature 401, 39–43 (1999).

    Article  Google Scholar 

  11. Lisiecki, L. E. Links between eccentricity forcing and the 100,000-year glacial cycle. Nature Geosci. 3, 349–352 (2010).

    Article  Google Scholar 

  12. Muttoni, G. et al. Onset of major Pleistocene glaciations in the Alps. Geology 31, 989–992 (2003).

    Article  Google Scholar 

  13. Garzanti, E., Vezzoli, G. & Andò, S. Paleogeographic and paleodrainage changes during Pleistocene glaciations (Po Plain, Northern Italy). Earth Sci. Rev. 105, 25–48 (2011).

    Article  Google Scholar 

  14. Haeuselmann, P., Granger, D. E., Jeannin, P-Y. & Lauritzen, S-E. Abrupt glacial valley incision at 0.8 Ma dated from cave deposits in Switzerland. Geology 35, 143–146 (2007).

    Article  Google Scholar 

  15. Shuster, D. L. & Farley, K. A. 4He/3He thermochronometry. Earth Planet. Sci. Lett. 217, 1–17 (2004).

    Article  Google Scholar 

  16. Farley, K. A. (U–Th)/He dating: techniques, calibrations, and applications. in Noble Gases in Geochemistry and Cosmochemistry (eds Porcelli, D.,Ballentine, C. J. & Wieler, R.) 819–844 (Reviews in Mineralogy and Geochemistry, Vol. 47, 2002).

    Chapter  Google Scholar 

  17. Shuster, D. L., Ehlers, T. A., Rusmore, M. E. & Farley, K. A. Rapid glacial erosion at 1.8 Ma revealed by 4He/3He thermochronometry. Science 310, 1668–1670 (2005).

    Article  Google Scholar 

  18. Valla, P. G., Herman, F., van der Beek, P. A. & Braun, J. Inversion of thermochronological age–elevation profiles to extract independent estimates of denudation and relief history—I: Theory and conceptual model. Earth Planet. Sci. Lett. 295, 511–522 (2010).

    Article  Google Scholar 

  19. Schlüchter, C. The Quaternary glaciations of Switzerland, with special reference to the Northern alpine foreland. Quat. Sci. Rev. 5, 413–419 (1986).

    Article  Google Scholar 

  20. Norton, K. P., Abbühl, L. M. & Schlunegger, F. Glacial conditioning as an erosional driving force in the Central Alps. Geology 38, 655–658 (2010).

    Article  Google Scholar 

  21. Schmid, S. M., Fügenschuh, B., Kissling, E. & Schuster, R. Tectonic map and overall architecture of the Alpine orogen. Ecl. Geol. Helv. 97, 93–117 (2004).

    Article  Google Scholar 

  22. Glotzbach, C., van der Beek, P. A. & Spiegel, C. Episodic exhumation and relief growth in the Mont Blanc massif, Western Alps from numerical modelling of thermochronology data. Earth Planet. Sci. Lett. 304, 417–430 (2011).

    Article  Google Scholar 

  23. van der Beek, P. A. et al. Inversion of thermochronological age–elevation profiles to extract independent estimates of denudation and relief history—II: Application to the French Western Alps. Earth Planet. Sci. Lett. 296, 9–22 (2010).

    Article  Google Scholar 

  24. Schildgen, T. F., Balco, G. & Shuster, D. L. Canyon incision and knickpoint propagation recorded by apatite 4He/3He thermochronometry. Earth Planet. Sci. Lett. 293, 377–387 (2010).

    Article  Google Scholar 

  25. Flowers, R. M., Ketcham, R. A., Shuster, D. L. & Farley, K. A. Apatite (U–Th)/He thermochronometry using a radiation damage accumulation and annealing model. Geochim. Cosmochim. Acta 73, 2347–2365 (2009).

    Article  Google Scholar 

  26. Braun, J. Pecube: A new finite-element code to solve the 3D heat transport equation including the effects of a time-varying, finite amplitude surface topography. Comp. Geosci. 29, 787–794 (2003).

    Article  Google Scholar 

  27. Mudelsee, M. & Raymo, M. E. Slow dynamics of the Northern Hemisphere glaciation. Paleoceanography 20, PA4022 (2005).

    Article  Google Scholar 

  28. Berger, A. L. et al. Quaternary tectonic response to intensified glacial erosion in an orogenic wedge. Nature Geosci. 1, 793–799 (2008).

    Article  Google Scholar 

  29. Champagnac, J-D., Molnar, P., Anderson, R. S., Sue, S. & Delacou, B. Quaternary erosion-induced isostatic rebound in the western Alps. Geology 35, 195–197 (2007).

    Article  Google Scholar 

  30. Hinderer, M. Late Quaternary denudation of the Alps; valley and lake fillings and modern river loads. Geodin. Acta 14, 231–263 (2001).

    Google Scholar 

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Acknowledgements

We thank J-D. Champagnac for field assistance, F. Cœur, B. Lum and F. Senebier for help during sample preparation. The staff of the Caltech Noble Gas Laboratory is acknowledged for conducting (U–Th–Sm)/He analyses. We thank G. Balco for development of the 4He/3He thermochronometry search algorithm, F. Chirouze and R. Delunel for fruitful discussions. M. Brandon and S. Brocklehurst provided constructive reviews. Financial support for this work was provided by the French Agence Nationale de la Recherche (ANR-08-BLAN-0303-01 grant to P.A.vd.B.), European Science Foundation Topo-Europe Eurocores programme, France-Berkeley Fund, US National Science Foundation (EAR-0720225 grant to D.L.S.) and the Ann and Gordon Getty Foundation.

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Authors and Affiliations

  1. Institut des Sciences de la Terre, Université Joseph Fourier, CNRS, BP 53, F-38041 Grenoble, France

    Pierre G. Valla & Peter A. van der Beek

  2. Berkeley Geochronology Center, 2455 Ridge Road, Berkeley, California 94709, USA

    David L. Shuster

  3. Department of Earth and Planetary Science, University of California, Berkeley, California 94720, USA

    David L. Shuster

Authors
  1. Pierre G. Valla
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Contributions

P.G.V. conducted fieldwork, processed samples and performed numerical modelling; P.G.V. and D.L.S. conducted 4He/3He analyses; all authors contributed equally to the design of the study and writing of the paper.

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Correspondence to Pierre G. Valla.

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The authors declare no competing financial interests.

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Valla, P., Shuster, D. & van der Beek, P. Significant increase in relief of the European Alps during mid-Pleistocene glaciations. Nature Geosci 4, 688–692 (2011). https://doi.org/10.1038/ngeo1242

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