The Altitudinal Patterns of Leaf C:N:P Stoichiometry Are Regulated by Plant Growth Form, Climate and Soil on Changbai Mountain, China

Understanding the geographic patterns and potential drivers of leaf stoichiometry is critical for modelling the nutrient fluxes of ecosystems and to predict the responses of ecosystems to global changes. This study aimed to explore the altitudinal patterns and potential drivers of leaf C:N:P stoichiometry. We measured the concentrations of leaf C, N and P in 175 plant species as well as soil nutrient concentrations along an altitudinal transect (500-2300 m) on the northern slope of Changbai Mountain, China to explore the response of leaf C: N: P stoichiometry to plant growth form (PGF), climate and soil. Leaf C, N, P and C: N: P ratios showed significant altitudinal trends. In general, leaf C and C: N: P ratios increased while leaf N and P decreased with elevation. Woody and herbaceous species showed different responses to altitudinal gradients. Trees had the largest variation in leaf C, C:N and C:P ratios, while herbs showed the largest variation in leaf N, P and N: P ratio. PGF, climate and soil jointly regulated leaf stoichiometry, explaining 17.6% to 52.1% of the variation in the six leaf stoichiometric traits. PGF was more important in explaining leaf stoichiometry variation than soil and climate. Our findings will help to elucidate the altitudinal patterns of leaf stoichiometry and to model ecosystem nutrient cycling.