Correlations with climate and physiological constraints have been proposed to explain the staggering diversity of leaf shapes and sizes. Just over a century ago, large, entire leaves were first observed to predominate in the tropics, while smaller, more dissected leaves are more commonly found in temperate regions Sinnott, 1915, 1916). The correlation between leaf serrations and present climate conditions can be used as indicators of ancient climates (Wolfe, 1978;Wilf, 1997;Peppe et al., 2011). Beyond serration correlations, scaling relationships constrain the relationship between blade and vein area across evolution. In mature, larger leaves, primary and secondary veins are wider but with less vein density compared to smaller leaves (Sack et al., 2012). These scaling laws have implications for leaf physiology, especially with respect to leaf hydraulic conductance, that offer a framework for the relationship between form and function in leaves and possibly explain major shifts in the evolutionary history of plants (Scoffoni et al., 2011;Sack and Scoffoni, 2013).To understand how broad patterns across plant evolution and geological time arise, ultimately, we must consider how leaves develop and how individual plants respond to the environment over a lifetime of growth. Distinguishing genetic, environmental, and interaction effects are critical to explain patterns in leaf shape and size observed from individual to global scales. Hypotheses about the mechanisms underlying plasticity in leaf shape have long been proposed (Goebel, 1908), but only careful work disentangling distinct processes-such as leaf ontogeny from the heteroblastic series-can inform as to when during development and how plasticity arises (Jones, 1995). Ontogenetic contingency-how the developmental program of an individual plant responds to changes in the environment during different phases of its life-can lead to disparate morphological outcomes in the same genotype or individual exposed to different environments (