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of the Holocene is not closed. OLIVEIRA et al. (2008-this issue) attributes the variability in the stratigraphy of near-valley head deposits (including the Holocene) to climatic forcing. The archaeological site of Axum offers the opportunity to link human
activities such as ploughing and the induced soil loss (CIAMPALINI et al., 2008), to the age of human occupation and the land-use changes that have occurred ever since (SCHMID et al., 2008). Here, VAN DE WAUW et al. (2008)) could also demonstrate
of the major processes resulting in this rejuvenation of parent material in many tropical areas is the presence of ancient and active lanslide bodies (MOEYERSONS et al., 2008). TURKELBOOM et al. (2008) demonstrate the negative impacts of current land-use
intensification on the natural hydrological equilibrium. In contrast to this is the situation in north Ethiopia, where MUNRO et al.(2008) with repeat photography over a period of 30 years found decreased soil loss rates, which they link to the introduction of soil
NYSSEN, J., (Editeur scientifique)[a1]
2008

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