1. Water is the most limiting resource for plant survival and growth in arid environments, but the diversity of water-use strategies among coexisting species in dryland communities is not well understood. There is also growing interest in assessing whether a whole-plant coordination exists between traits related to water-use and the leaf economic spectrum (LES).2. We used water stable isotopes (δ 2 H, δ 18 O) to quantify water uptake proportions from different soil depths by 24 species in a Mediterranean shrubland. Leaf traits associated with water-use efficiency, stomatal regulation (δ 13 C, δ 18 O) and the LES (SLA, N, P, K concentrations) were also measured. We assessed potential trade-offs between the above-mentioned leaf traits, water uptake depth and their relationship with species abundance.3. We found distinct ecohydrological niche segregation among coexisting species.Bayesian models showed that our shrubland species used a median of 37% of shallow soil water (0-30 cm) and 63% of deep water (30-100 cm). Still, water source proportions varied considerably among species, as shallow soil water-use ranged from a minimum of 6.4% to a maximum of 68%. Interspecific variability in foliar carbon investment (SLA) and nutrient concentrations was remarkably high, indicating diverse nutrient-use strategies along the LES. Leaf δ 18 O, δ 13 C and δ 15 N values also differed widely among species, revealing differences in stomatal regulation, water-use efficiency and nitrogen acquisition mechanisms.After accounting for evolutionary history effects, water uptake depth was coordinated with the LES: species using shallower soil water from fertile topsoil layers exhibited a more acquisitive carbon-and nutrient-use strategy, whereas water uptake from deeper but less fertile soil layers was linked to a more conservative nutrient-use strategy. Leaf-level water-use traits significantly influenced species abundance, as water-savers with tight stomatal regulation and high water-use efficiency were dominant.
Synthesis.Greater utilisation of water stored in nutrient-rich topsoil layers favoured a more acquisitive nutrient-use strategy, whereas a deeper water uptake