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The Uncalm Development of Proglacial Soils in the European Alps Since 1850

  • Arnaud J. A. M. TemmeEmail author
Chapter
Part of the Geography of the Physical Environment book series (GEOPHY)

Abstract

Glaciers in the Alps and other mountain regions are widely retreating. This contribution focusses on the soils that are forming in the proglacial areas. These soils are important because of the hydrological and ecological effect they will have in future glacierless valleys. A geographical approach is taken that attempts to explain differences in rates of soil formation between proglacial valleys. Through a comparison of published soil chronosequences of European proglacial areas, it is found that age is the most important factor determining rates of soil development—even where morphodynamics are strong. Nonetheless, the effect of geomorphic activity and the effect of vegetation succession have been clearly observed in several studies. The combination of all factors forces us to acknowledge a complex model of soil formation in alpine proglacial valley that among others highlights the heterogenous and dynamic nature of morphodynamics. This model invites us to fill in some blanks in our understanding and suggests that with a larger number of proglacial soil development studies, we may be able to provide pan-alpine information on soils in proglacial areas. This is of importance, for instance, when establishing pan-alpine carbon budgets.

Keywords

Soil development Proglacial area Soil types Chronosequence Morphodynamics 

References

  1. Alexander EB, Ellis CC, Burke R (2007) A chronosequence of soils and vegetation on serpentine terraces in the Klamath Mountains, USA. Soil Sci 172:565–576CrossRefGoogle Scholar
  2. Baewert H, Morche D (2014) Coarse sediment dynamics in a proglacial fluvial system (Fagge River, Tyrol). Geomorphology 218:88–97.  https://doi.org/10.1016/j.geomorph.2013.10.021CrossRefGoogle Scholar
  3. Bardgett RD, Bowman WD, Kaufmann R, Schmidt SK (2005) A temporal approach to linking aboveground and belowground ecology. Trends Ecol Evol 20:634–641CrossRefGoogle Scholar
  4. Beniston M (2003) Climatic change in mountain regions: a review of possible impacts. Clim Change 59:5–31CrossRefGoogle Scholar
  5. Bernasconi SM, Bauder A, Bourdon B et al (2011) Chemical and biological gradients along the Damma Glacier soil chronosequence, Switzerland. Vadose Zone J 10:867.  https://doi.org/10.2136/vzj2010.0129CrossRefGoogle Scholar
  6. Bernasconi SM, BigLink Project Members (2008) Weathering, soil formation and initial ecosystem evolution on a glacier forefield: a case study from the Damma Glacier, Switzerland. Mineral Mag 72:19–22CrossRefGoogle Scholar
  7. Burga CA (1999) Vegetation development on the glacier forefield Morteratsch (Switzerland). Appl Veg Sci 2:17–24CrossRefGoogle Scholar
  8. Burke BC, Heimsath AM, White AF (2007) Coupling chemical weathering with soil production across soil-mantled landscapes. Earth Surf Proc Land 32:853–873CrossRefGoogle Scholar
  9. Carey M (2010) In the shadow of melting glaciers: climate change and Andean society. Oxford University Press, OxfordCrossRefGoogle Scholar
  10. Carnielli T (2005) Snout and area recent variations of Grande di Verra Glacier (Monte Rosa, Alps). Geografia Fisica e Dinamica Quaternaria VII: 79–87Google Scholar
  11. Citterio M, Diolaiuti G, Smiraglia C et al (2007) The fluctuations of Italian glaciers during the last century: a contribution to knowledge about alpine glacier changes. Geogr Ann: Ser A, Phys Geogr 89:167–184CrossRefGoogle Scholar
  12. D’Amico ME, Bonifacio E, Zanini E (2014a) Relationships between serpentine soils and vegetation in a xeric inner-alpine environment. Plant Soil 376:111–128CrossRefGoogle Scholar
  13. D’Amico ME, Freppaz M, Filippa G, Zanini E (2014b) Vegetation influence on soil formation rate in a proglacial chronosequence (Lys Glacier, NW Italian Alps). CATENA 113:122–137.  https://doi.org/10.1016/j.catena.2013.10.001CrossRefGoogle Scholar
  14. D’Amico ME, Freppaz M, Leonelli G et al (2015) Early stages of soil development on serpentinite: the proglacial area of the Verra Grande Glacier, Western Italian Alps. J Soils Sediments 15:1292–1310CrossRefGoogle Scholar
  15. D’Amico ME, Catoni M, Terribile F, Zanini E, Bonifacio E (2016) Contrasting environmental memories in relict soils on different parent rocks in the south-western Italian Alps. Quat Int 418:61–74CrossRefGoogle Scholar
  16. Duc L, Noll M, Meier BE et al (2009) High diversity of diazotrophs in the forefield of a receding alpine glacier. Microb Ecol 57:179–190CrossRefGoogle Scholar
  17. Dümig A, Smittenberg R, Kögel-Knabner I (2011) Concurrent evolution of organic and mineral components during initial soil development after retreat of the Damma glacier, Switzerland. Geoderma 163:83–94CrossRefGoogle Scholar
  18. Egli M, Fitze P, Mirabella A (2001) Weathering and evolution of soils formed on granitic, glacial deposits: results from chronosequences of Swiss alpine environments. Catena 45:19–47CrossRefGoogle Scholar
  19. Egli M, Lessovaia SN, Chistyakov K et al (2015) Microclimate affects soil chemical and mineralogical properties of cold alpine soils of the Altai Mountains (Russia). J Soils Sediments 15:1420–1436CrossRefGoogle Scholar
  20. Egli M, Wernli M, Burga C et al (2011) Fast but spatially scattered smectite-formation in the proglacial area Morteratsch: an evaluation using GIS. Geoderma 164:11–21CrossRefGoogle Scholar
  21. Egli M, Wernli M, Kneisel C et al (2006a) Melting glaciers and soil development in the proglacial area Morteratsch (Swiss Alps): II. Modeling the present and future soil state. Arct Antarct, Alp Res 38:510–521CrossRefGoogle Scholar
  22. Egli M, Wernli M, Kneisel C, Haeberli W (2006b) Melting glaciers and soil development in the proglacial area Morteratsch (Swiss Alps): I. Soil Type Chronosequence. Arct Antarct, Alp Res 38:499–509.  https://doi.org/10.1657/1523-0430(2006)38%5b499:MGASDI%5d2.0.CO;2CrossRefGoogle Scholar
  23. Göransson H, Welc M, Bünemann EK et al (2016) Nitrogen and phosphorus availability at early stages of soil development in the Damma glacier forefield, Switzerland; implications for establishment of N2-fixing plants. Plant Soil 404:251–261.  https://doi.org/10.1007/s11104-016-2821-5CrossRefGoogle Scholar
  24. Guelland K, Hagedorn F, Smittenberg RH, Göransson H, Bernasconi SM, Hajdas I, Kretzschmar R (2013) Evolution of carbon fluxes during initial soil formation along the forefield of Damma glacier, Switzerland. Biogeochemistry 113:545–561.  https://doi.org/10.1007/s10533-012-9785-1CrossRefGoogle Scholar
  25. Haas F, Heckmann T, Hilger L, Becht M (2012) Quantification and modelling of debris flows in the proglacial area of the Gepatschferner, Austria, using ground-based LiDAR. IAHS-AISH publication. International Association of Hydrological Sciences, pp 293–302Google Scholar
  26. Haeberli W, Hoelzle M, Paul F, Zemp M (2007) Integrated monitoring of mountain glaciers as key indicators of global climate change: the European Alps. Ann Glaciol 46:150–160CrossRefGoogle Scholar
  27. Hartl L (2010) The Gepatschferner from 1850–2006-changes in length, area and volume in relation to climate. Diploma thesis (unpublished), University of InnsbruckGoogle Scholar
  28. Heckmann T, Haas F, Morche D, Schmidt K-H, Rohn J, Moser M, Leopold M, Kuhn M, Briese C, Pfeifer N, Becht M (2012) Investigating an alpine proglacial sediment budget using field measurements, airborne and terrestrial LiDAR data, vol 356. IAHS-AISH publication, pp 438–447Google Scholar
  29. Huggel C, Kääb A, Haeberli W et al (2002) Remote sensing based assessment of hazards from glacier lake outbursts: a case study in the Swiss Alps. Can Geotech J 39:316–330CrossRefGoogle Scholar
  30. Jacobsen D, Milner AM, Brown LE, Dangles O (2012) Biodiversity under threat in glacier-fed river systems. Nat Clim Change 2:361–364CrossRefGoogle Scholar
  31. Jürgens C (2006) A visual system for the interactive study and experimental simulation of climate-induced 3D Mountain Glacier Fluctuations. JSTORGoogle Scholar
  32. Kabala C, Zapart J et al (2009) Recent, relic and buried soils in the forefield of Werenskiold Glacier, SW Spitsbergen. Pol Polar Res 30:161–178Google Scholar
  33. Karlstrom ET, Osborn G (1992) Genesis of buried paleosols and soils in Holocene and late Pleistocene tills, Bugaboo Glacier area, British Columbia, Canada. Arct Alp Res 108–123CrossRefGoogle Scholar
  34. Khaziev FK (2011) Soil and biodiversity. Russ J Ecol 42:199–204CrossRefGoogle Scholar
  35. Knight J, Harrison S (2014) Mountain Glacial and paraglacial environments under global climate change: lessons from the past, future directions and policy implications. Geogr Ann: Ser A, Phys Geogr 96:245–264.  https://doi.org/10.1111/geoa.12051CrossRefGoogle Scholar
  36. Langston AL, Tucker GE, Anderson RS, Anderson SP (2015) Evidence for climatic and hillslope-aspect controls on vadose zone hydrology and implications for saprolite weathering. Earth Surf Process Land 40:1254–1269CrossRefGoogle Scholar
  37. Mahaney WC, Hancock RG, Melville H (2011) Late glacial retreat and Neoglacial advance sequences in the Zillertal Alps, Austria. Geomorphology 130:312–326CrossRefGoogle Scholar
  38. Mavris C, Egli M, Plötze M, Blum JD, Mirabella A, Giaccai D, Haeberli W (2010) Initial stages of weathering and soil formation in the Morteratsch proglacial area (Upper Engadine, Switzerland). Geoderma 155:359–371CrossRefGoogle Scholar
  39. Morche D, Haas F, Baewert H, Heckmann T, Schmidt K-H, Becht M (2012) Sediment transport in the proglacial Fagge River (Kaunertal/Austria), vol 356. IAHS-AISH Publication, pp 72–80Google Scholar
  40. Morche D, Schuchardt A, Dubberke K, Baewert H (2014) Channel morphodynamics on a small proglacial braid plain (Fagge River, Gepatschferner, Austria), vol 367. IAHS-AISH Publication, pp 109–116.  https://doi.org/10.5194/piahs-367-109-2015CrossRefGoogle Scholar
  41. Nicol GW, Tscherko D, Embley TM, Prosser JI (2005) Primary succession of soil Crenarchaeota across a receding glacier foreland. Environ Microbiol 7:337–347CrossRefGoogle Scholar
  42. Philippot L, Tscherko D, Bru D, Kandeler E (2011) Distribution of high bacterial taxa across the chronosequence of two alpine glacier forelands. Microbial Ecol 61:303–312CrossRefGoogle Scholar
  43. Prietzel J, Wu Y, Dümig A, Zhou J, Klysubun W (2013) Soil sulphur speciation in two glacier forefield soil chronosequences assessed by S K-edge XANES spectroscopy: S speciation in glacier forefield soils by XANES. Eur J Soil Sci 64:260–272.  https://doi.org/10.1111/ejss.12032CrossRefGoogle Scholar
  44. Richardson SD, Reynolds JM (2000) An overview of glacial hazards in the Himalayas. Quat Int 65:31–47CrossRefGoogle Scholar
  45. Schmalenberger A, Noll M (2009) Shifts in desulfating bacterial communities along a soil chronosequence in the forefield of a receding glacier. FEMS Microbiol Ecol 71:208–217CrossRefGoogle Scholar
  46. Schurig C, Smittenberg RH, Berger J, Kraft F, Woche SK, Goebel MO, Heipieper HJ, Miltner A, Kaestner M (2013) Microbial cell-envelope fragments and the formation of soil organic matter: a case study from a glacier forefield. Biogeochemistry 113:595–612CrossRefGoogle Scholar
  47. Sigler W, Zeyer J (2002) Microbial diversity and activity along the forefields of two receding glaciers. Microb Ecol 43:397–407CrossRefGoogle Scholar
  48. Singh P, Bengtsson L (2005) Impact of warmer climate on melt and evaporation for the rainfed, snowfed and glacierfed basins in the Himalayan region. J Hydrol 300:140–154CrossRefGoogle Scholar
  49. Smittenberg RH, Gierga M, Göransson H, Christl I, Farinotti D, Bernasconi SM (2012) Climate-sensitive ecosystem carbon dynamics along the soil chronosequence of the Damma glacier forefield, Switzerland. Global Change Biol 18:1941–1955.  https://doi.org/10.1111/j.1365-2486.2012.02654.xCrossRefGoogle Scholar
  50. Sommer M, Gerke H, Deumlich D (2008) Modelling soil landscape genesis—a “time split” approach for hummocky agricultural landscapes. Geoderma 145:480–493CrossRefGoogle Scholar
  51. Stöcklin J, Bäumler E (1996) Seed rain, seedling establishment and clonal growth strategies on a glacier foreland. J Veg Sci 7:45–56CrossRefGoogle Scholar
  52. Temme AJAM, Heckmann T, Harlaar P (2016) Silent play in a loud theatre—dominantly time-dependent soil development in the geomorphically active proglacial area of the Gepatsch glacier, Austria. Catena 147:40–50CrossRefGoogle Scholar
  53. Temme AJAM, Lange K, Schwering MF (2015) Time development of soils in mountain landscapes—divergence and convergence of properties with age. J Soils Sed 15:1373–1382CrossRefGoogle Scholar
  54. Temme AJAM, Lange K (2014) Pro-glacial soil variability and geomorphic activity—the case of three Swiss valleys. Earth Surf Process Land 39:1492–1499.  https://doi.org/10.1002/esp.3553CrossRefGoogle Scholar
  55. Tscherko D, Rustemeier J, Richter A, Wanek W, Kandeler E (2003) Functional diversity of the soil microflora in primary succession across two glacier forelands in the Central Alps. Eur J Soil Sci 54:685–696CrossRefGoogle Scholar
  56. Vavtar F (1981) Syngenetische metamorphe Kiesanreicherungen in Paragneisen des Ötztal-Kristallins (Kaunertal, Tirol). Veröff Museum Ferdinandeum Innsbruck, S 151–169Google Scholar
  57. Welc M, Bünemann EK, Fließbach A, Frossard E, Jansa J (2012) Soil bacterial and fungal communities along a soil chronosequence assessed by fatty acid profiling. Soil Biol Biochem 49:184–192.  https://doi.org/10.1016/j.soilbio.2012.01.032CrossRefGoogle Scholar
  58. Wösten J, Lilly A, Nemes A, Le Bas C (1999) Development and use of a database of hydraulic properties of European soils. Geoderma 90:169–185CrossRefGoogle Scholar
  59. WRB (2015) World reference base for soil resources 2014, update 2015 International soil classification system for naming soils and creating legends for soil maps. FAO, RomeGoogle Scholar
  60. Xu J, Grumbine RE, Shrestha A, Eriksson M, Yang X, Wang Y, Wilkes A (2009) The melting Himalayas: cascading effects of climate change on water, biodiversity, and livelihoods. Conserv Biol 23:520–530CrossRefGoogle Scholar
  61. Zech W, Wilke B (1977) Vorläufige Ergebnisse einer Bodenchronosequenzstudie im Zillertal. Mitteilungen der Deutschen Bodenkundlichen Gesellschaft 25:571–586Google Scholar

Copyright information

© Springer Nature Switzerland AG 2019

Authors and Affiliations

  1. 1.Department of GeographyKansas State UniversityManhattanUSA
  2. 2.Soil Geography and Landscape, Wageningen UniversityWageningenThe Netherlands
  3. 3.Institute for Arctic and Alpine Research, University of ColoradoBoulderUSA

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