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. 2020 Jun 24;126(6):981–990. doi: 10.1093/aob/mcaa114

Fig. 2.

Fig. 2.

Boxplots showing the δ 13Cp difference between mature and young leaf dry matter as a function of phenology (A), and whether the trees grew in temperate or tropical climate zones (B). The δ 13C difference was calculated as mature leaf δ 13Cp minus young leaf δ 13Cp for the same species. Further details of the dataset are given in Table 1.