Unexpected Large Photosynthetic Thermal Plasticity of Montane Andean Trees.

In our study, although leaf nitrogen ( N a ) did not significantly differ overall among sites, it showed a decreasing trend in warmer (lower elevations) environments in both groups (Figure S8 ; Table S8 ).

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The upper leaf temperature threshold at which net photosynthesis rates become zero or the so‐called high temperature CO 2 compensation point ( T max ) (Figure 1a ) exhibited an increasing trend from high‐ to low‐elevation sites in both groups, but none of these shifts were significant in either group (Figure 3c,d ; Table 1 ; Table S3 ). 3.2.

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