Denudation variability of the Sila Massif upland (Italy) from decades to millennia using 10Be and 239+240Pu

Gerald Raab, Fabio Scarciglia, Kevin Norton, Dennis Dahms, Dagmar Brandová, Raquel de Castro Portes, Marcus Christl, Michael E Ketterer, Annina Ruppli, Markus Egli

Research output: Contribution to journalArticle

2 Citations (Scopus)

Abstract

Landscapes and soils evolve in non-linear ways over millennia. Current knowledge is incomplete as only average denudation (or erosion) rates are normally estimated, neglecting the temporal discontinuities of these processes. The determination of regressive and progressive phases of soil evolution is important to our understanding of how soils and landscapes respond to environmental changes. The Sila Massif (Italy) provides a well-defined geomorphological and geological setting to unravel temporal variations in soil redistribution rates. We used a combination of in situ cosmogenic radionuclide measurements (10Be) along tor (residual rock) height profiles, coupled with fallout radionuclides (239+240Pu) in soils, to model soil denudation rates over the last 100 ka. We measured rates prior to the Last Glacial Maximum (LGM) of ≤30 t km−2 yr−1 (~0.036 mm yr−1). Following the LGM, during the transition from the Pleistocene to the Holocene, these rates increased to ~150–200 t km−2 yr−1 and appeared to be above soil production rates, causing regressive soil evolution. For the last ~50 years, we even describe erosion rates of ≥1,000 t km−2 yr−1 (~1.23 mm yr−1) and consider human impact as the decisive factor for this development. Consequently, the natural soil production rates cannot cope with the current erosion rates. Thus, a distinct regressive phase of soil formation exists, which will give rise to shallowing of soils over time. Overall, our multimethod approach traced denudation and erosion histories over geologic and human timescales and made a new archive to soil science and geomorphology accessible.

Original languageEnglish (US)
Pages (from-to)3736-3752
Number of pages17
JournalLand Degradation and Development
Volume29
Issue number10
DOIs
StatePublished - Oct 1 2018

Fingerprint

denudation
erosion
highlands
Italy
Soils
soil
soil formation
erosion rate
Erosion
radionuclides
redistribution
Last Glacial Maximum
Radioisotopes
geomorphology
cosmogenic radionuclide
soil science
history
science
anthropogenic activities
Geomorphology

Keywords

  • cosmogenic nuclides
  • fallout radionuclides
  • landscape evolution
  • soil erosion rates
  • tor formation

ASJC Scopus subject areas

  • Environmental Chemistry
  • Development
  • Environmental Science(all)
  • Soil Science

Cite this

Raab, G., Scarciglia, F., Norton, K., Dahms, D., Brandová, D., de Castro Portes, R., ... Egli, M. (2018). Denudation variability of the Sila Massif upland (Italy) from decades to millennia using 10Be and 239+240Pu. Land Degradation and Development, 29(10), 3736-3752. https://doi.org/10.1002/ldr.3120

Denudation variability of the Sila Massif upland (Italy) from decades to millennia using 10Be and 239+240Pu. / Raab, Gerald; Scarciglia, Fabio; Norton, Kevin; Dahms, Dennis; Brandová, Dagmar; de Castro Portes, Raquel; Christl, Marcus; Ketterer, Michael E; Ruppli, Annina; Egli, Markus.

In: Land Degradation and Development, Vol. 29, No. 10, 01.10.2018, p. 3736-3752.

Research output: Contribution to journalArticle

Raab, G, Scarciglia, F, Norton, K, Dahms, D, Brandová, D, de Castro Portes, R, Christl, M, Ketterer, ME, Ruppli, A & Egli, M 2018, 'Denudation variability of the Sila Massif upland (Italy) from decades to millennia using 10Be and 239+240Pu', Land Degradation and Development, vol. 29, no. 10, pp. 3736-3752. https://doi.org/10.1002/ldr.3120
Raab, Gerald ; Scarciglia, Fabio ; Norton, Kevin ; Dahms, Dennis ; Brandová, Dagmar ; de Castro Portes, Raquel ; Christl, Marcus ; Ketterer, Michael E ; Ruppli, Annina ; Egli, Markus. / Denudation variability of the Sila Massif upland (Italy) from decades to millennia using 10Be and 239+240Pu. In: Land Degradation and Development. 2018 ; Vol. 29, No. 10. pp. 3736-3752.
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abstract = "Landscapes and soils evolve in non-linear ways over millennia. Current knowledge is incomplete as only average denudation (or erosion) rates are normally estimated, neglecting the temporal discontinuities of these processes. The determination of regressive and progressive phases of soil evolution is important to our understanding of how soils and landscapes respond to environmental changes. The Sila Massif (Italy) provides a well-defined geomorphological and geological setting to unravel temporal variations in soil redistribution rates. We used a combination of in situ cosmogenic radionuclide measurements (10Be) along tor (residual rock) height profiles, coupled with fallout radionuclides (239+240Pu) in soils, to model soil denudation rates over the last 100 ka. We measured rates prior to the Last Glacial Maximum (LGM) of ≤30 t km−2 yr−1 (~0.036 mm yr−1). Following the LGM, during the transition from the Pleistocene to the Holocene, these rates increased to ~150–200 t km−2 yr−1 and appeared to be above soil production rates, causing regressive soil evolution. For the last ~50 years, we even describe erosion rates of ≥1,000 t km−2 yr−1 (~1.23 mm yr−1) and consider human impact as the decisive factor for this development. Consequently, the natural soil production rates cannot cope with the current erosion rates. Thus, a distinct regressive phase of soil formation exists, which will give rise to shallowing of soils over time. Overall, our multimethod approach traced denudation and erosion histories over geologic and human timescales and made a new archive to soil science and geomorphology accessible.",
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