“…Throughout the final Chalcolithic/early-Bronze Age and with the onset of the late-Holocene, a transition from climate-to human-dominated landscapes occurred (Balbo et al, 2018;Picornell-Gelabert and Carrion-Marco, 2017;Mensing et al, 2015;). This transition is likely to have been triggered by an enlarged LUC capacity aimed at adapting to the contemporary drier and warmer climate, further exacerbating aridification (El Ouahabi et al, 2018;Mazzini et al, 2016;Pustovoytov and Riehl, 2016). During that time, more complex adaptation measures were developed, such as storage systems, enlarged infrastructures, and extended trading networks, which raised pressures to the natural system (Fontana et al, 2017;Clarke et al, 2016;Flohr et al, 2016;Gogou et al, 2016;Morellón et al, 2016;Weiberg et al, 2016).…”