Abstract
The leaf area to sapwood area ratios of trees (A l:A S) can shift to maintain homeostatic gas exchange per unit leaf area in response to climate variability. We tested the hypothesis that trees alter their A l:A S ratios in response to long-term warming and reduced precipitation in order to maintain leaf-specific gas exchange rates under more stressful conditions. Whole-tree A l:A S was measured on mature piñon pine (Pinus edulis Engelm.) and one-seed juniper (Juniperus monosperma (Engelm.) Sarg.) trees after 5 years (2012-16) of chronic exposure to increased temperature (+4.8 °C), precipitation reduction (' '45%), or both simultaneously. No difference was found in A l:A s among treatments for either species. Associated with this lack of shift in A l:A s were large changes in pre-dawn leaf water potential and stomatal conductance, consistent with theoretical expectations of interactions between leaf and whole-tree hydraulic supply. Our results suggest that a lack of whole-tree acclimation in A l:A s results in the reductions in plant gas exchange and water status associated with long-term warming and reduced precipitation in semi-arid woodlands.
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McBranch, N. A., Grossiord, C., Adams, H., Borrego, I., Collins, A. D., Dickman, T., … McDowell, N. G. (2018). Lack of acclimation of leaf area:sapwood area ratios in piñon pine and juniper in response to precipitation reduction and warming. Tree Physiology, 39(1), 135–142. https://doi.org/10.1093/treephys/tpy066
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