Publication: Denudation variability of the Sila Massif upland (Italy) from decades to millennia using 10Be and 239+240Pu
Denudation variability of the Sila Massif upland (Italy) from decades to millennia using 10Be and 239+240Pu
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Raab, G., Scarciglia, F., Norton, K., Dahms, D., Brandová, D., de Castro Portes, R., Christl, M., Ketterer, M. E., Ruppli, A., & Egli, M. (2018). Denudation variability of the Sila Massif upland (Italy) from decades to millennia using 10Be and 239+240Pu. Land Degradation & Development, 29(10), 3736–3752. https://doi.org/10.1002/ldr.3120
Abstract
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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 rate
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- Scarciglia, Fabio
- Norton, Kevin
- Dahms, Dennis
- Brandová, Dagmar
- de Castro Portes, Raquel
- Christl, Marcus
- Ketterer, Michael E
- Ruppli, Annina
- Egli, Markus
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Raab, G., Scarciglia, F., Norton, K., Dahms, D., Brandová, D., de Castro Portes, R., Christl, M., Ketterer, M. E., Ruppli, A., & Egli, M. (2018). Denudation variability of the Sila Massif upland (Italy) from decades to millennia using 10Be and 239+240Pu. Land Degradation & Development, 29(10), 3736–3752. https://doi.org/10.1002/ldr.3120
