Using robust, pairwise comparisons and a global dataset, we show that nitrogen concentration per unit leaf mass for nitrogen-fixing plants (N 2 FP; mainly legumes plus some actinorhizal species) in nonagricultural ecosystems is universally greater (43-100%) than that for other plants (OP). This difference is maintained across Koppen climate zones and growth forms and strongest in the wet tropics and within deciduous angiosperms. N 2 FP mostly show a similar advantage over OP in nitrogen per leaf area (N area ), even in arid climates, despite diazotrophy being sensitive to drought. We also show that, for most N 2 FP, carbon fixation by photosynthesis (A sat ) and stomatal conductance (g s ) are not related to N area -in distinct challenge to current theories that place the leaf nitrogen-A sat relationship at the center of explanations of plant fitness and competitive ability. Among N 2 FP, only forbs displayed an N area -g s relationship similar to that for OP, whereas intrinsic water use efficiency (WUE i ; A sat /g s ) was positively related to N area for woody N 2 FP. Enhanced foliar nitrogen (relative to OP) contributes strongly to other evolutionarily advantageous attributes of legumes, such as seed nitrogen and herbivore defense. These alternate explanations of clear differences in leaf N between N 2 FP and OP have significant implications (e.g., for global models of carbon fluxes based on relationships between leaf N and A sat ). Combined, greater WUE and leaf nitrogen-in a variety of forms-enhance fitness and survival of genomes of N 2 FP, particularly in arid and semiarid climates.legume | actinorhizal species | nitrogen | photosynthesis | water use efficiency T hrough symbioses with diazotrophic bacteria, legumes and other N 2 -fixing plants (N 2 FP) acquire atmospheric dinitrogen (N 2 ) and are widely expected to maintain greater leaf nitrogen than nonfixing or other plants (OP) (1). N 2 FP can profoundly influence both ecosystem development and responses to changing climate by alleviating nitrogen shortages that limit capacity of ecosystems to fix and sequester CO 2 (2-4). A central tenet of traitbased ecology (5, 6) is that carbon fixation and transpiration are directly related to leaf nitrogen; in turn, leaf nitrogen is used to drive global models of carbon (and water) exchanges between plants and the atmosphere (7).The distribution, abundance, and activity of N 2 FP in terrestrial ecosystems have remained unexplained, even "paradoxical" (8, 9), especially in relation to local and global nitrogen cycles. For the northern hemisphere, one recent explanation of the distribution of N 2 FP (2) and their dominance in wet tropical forests relied on their greater ability to acquire phosphorus from old tropical soils and temperature maxima for N 2 fixation of around 25°C (i.e., similar to prevailing temperatures in the tropics). Menge et al. (8) subsequently noted that the diazotrophic symbioses are typically rhizobial and facultative toward the tropics but actinorhizal and obligate north of about 35°N. Fac...