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- W1536087908 abstract "The variability of Late Holocene fluvial dynamics in the Swiss Alps is traced from fan delta deposits using a multi-proxy approach. The spatial coexistence of wetland, alluvial and fluvial environments on the low-gradient Lutschine fan delta provides a high-resolution fluvial record. The sedimentary record shows seven major aggradation pulses from 3600 cal year BP to the present. Furthermore, 19 minor burial episodes occur between 3600 and 1050 cal year BP at intervals of between 100 and 130 years, suggesting that aggradation during the period of interest was triggered by centennial flood events. Nine coarse-grained flood layers, deposited at a recurrence interval of between 200 and 600 years, coincide with positive radiocarbon anomalies and cold phases in the Alps. The solar influence on the regional hydrological regime is proposed as the main factor triggering the flooding events." @default.
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- W1536087908 date "2008-01-01" @default.
- W1536087908 modified "2023-10-12" @default.
- W1536087908 title "Sensitivity of Alpine fluvial environments in the Swiss Alps to climate forcing during the Late Holocene" @default.
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