“…Traditional views of hydraulic limitation include (1) declines in leaf area-specific hydraulic conductance with increasing tree height; (2) declines in w leaf with tree height due to decreased whole-plant hydraulic conductance and increased gravitational potential; and (3) resulting decreases in average stomatal conductance (Ryan and Yoder 1997, Koch et al 2004, Ryan et al 2006, Hinckley et al 2011, Mencuccini et al 2011. Factors that might contribute to a tighter relationship of maximum tree height to P/E p than expected based on hydraulic limitation (and thus D) alone might include (4) increased allocation to leaves vs. roots or stems at a given height with increasing P/E p , or conditions correlated with higher P/E p (e.g., greater soil silt or nitrate content); (5) higher photosynthetic rates per unit leaf mass at higher P/E p or under conditions correlated therewith, independent of the degree of stomatal limitation; (6) higher leaf area-specific conductance at higher P/E p in trees of a given height, reflecting differences in wood density and xylem diameter and length (Thomas 1996b, Thomas and Bazzaz 1999, Zach et al 2010, Fan et al 2012, Gleason et al 2012; (7) variation across species in the rate at which mesophyll photosynthetic capacity declines with decreasing w leaf (Givnish 1986, Tezara et al 2003, Lawlor and Tezara 2009); (8) variation across sites in which the rate at which evaporation from sunlit leaves increases with relative height at the top of the canopy; and (9) greater uncertainties in measuring average D than average height. The preceding factors are all plausible ways in which resource allocation or modified hydraulic limitation effects could constrain tree height along the Victoria transect, in response to the increase in P/E p toward the Yarra Ranges, the reduced heat load and cloudier conditions at higher altitudes and latitudes there, and the increasingly fine-grained, more P-and Nrich soils there (see Eq.…”