All models were highly significant, suggesting that height and PAR, or the interaction of both, as well as %N, %C and tree species have significant effects on δ 13 C, δ 18 O and δ 15 N values and LMA (Table 2 , see Table S2 for detailed model results).
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Stratigraphy of stable isotope ratios and leaf structure within an African rainforest canopy with implications for primate isotope ecology.
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