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Three phases of landscape alteration are distinguished.
Several calcretes, buried surfaces and initial soil horizons indicate phases of landscape stability and potentially moister climatic conditions than today.
Pollen, NPP and charcoal particles analyses evidenced seven phases of landscape change, resulting from different agricultural and pastoral practices and the use of fire probably to manage vegetation.
Furthermore, colluvial slope deposits and erosional discordances provide information on distinct phases of landscape instability that are linked to interglacial periods and the transition to glacial conditions.
By using luminescence and radiocarbon dating, phases of landscape change, indicated by soil formation, occurred mainly at around 6.5 6 ka.
Results from regolith samples relate to different phases of landscape activation and stability from the late 6th millennium BC to the Roman conquest.
Similar(51)
Evidence of a phase of landscape stability is seen corresponding to the interval 11 9 ka.
Collectively, these characteristics indicate the catchment is undergoing a phase of landscape recovery.
The post-glacial to early Holocene was a phase of landscape stability (subdued tectonics) which persisted until around 7.1 ka.
The record casts light on a previously undocumented phase of landscape instability in the dynamic setting of the Assif n'Imserdane valley, and highlights the potential for further exploration of small infilled basins in the High Atlas to illuminate the geoecological history of the region.
Conversely, several phases of homogeneous landscape management are distinguishable during the early Neolithic, and from the late Bronze to the late Iron Age.
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