Research carried out in the southern sector of the Puna de Atacama, Argentina, enables taphonomic hypotheses concerning bone scattering and the fossil record to be tested. To that end, this study is based on bone samples from modern camelid (Lama sp.) carcasses. In the first stages of research I evaluated the role played by disarticulation and fluvial transport in relation to different skeletal elements. Subsequently, I tested the various sedimentary contexts where the bones were buried and their relative importance in the different topographic localities. In certain areas of the vega hydraulic transport power decreases in relation to certain topographic accidents and patches of vegetation that act as a retaining wall. The reduction of this form of transport produces bone sedimentation. As such, there is the possibility of elaborating certain expectations, when possible, for the formation of a future fossil record in some sectors of this environment. Without underestimating the importance of previously developed fluvial bone transport models, my research favours a model in which some skeletal parts are more affected by transport than others, allowing us to determine the existence of different patterns of bone scattering and fossil assemblage in this area. In brief, this article produces preliminary empirical evidence for fluvial transport of camelid bones in the high desert, evidence which could be used as an indicator of original conditions in environments where bones were accumulated and became fossilized.