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At least it is a dry cold: the global distribution of freeze-thaw and drought stress and the traits that may impart poly-tolerance in conifers

Journal

TREE PHYSIOLOGY
Volume 43, Issue 1, Pages 1-15

Publisher

OXFORD UNIV PRESS
DOI: 10.1093/treephys/tpac102

Keywords

abiotic stress; conifers; distributions; drought; freeze-thaw; poly-tolerance

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Conifers are able to tolerate multiple abiotic stressors, such as aridity and freezing temperatures. The study finds that conifer distribution is mainly concentrated in areas with moderate poly-stress, where both moderate drought and freeze-thaw cycles occur. The response of conifers to these stressors varies among different traits. The study also highlights the need for further research to understand the prevalence and plasticity of traits related to freeze-thaw and drought stress across different species and geographic scales.
Conifers inhabit some of the most challenging landscapes where multiple abiotic stressors (e.g., aridity, freezing temperatures) often co-occur. Physiological tolerance to multiple stressors ('poly-tolerance') is thought to be rare because exposure to one stress generally limits responses to another through functional trade-offs. However, the capacity to exhibit poly-tolerance may be greater when combined abiotic stressors have similar physiological impacts, such as the disruption of hydraulic function imposed by drought or freezing. Here, we reviewed empirical data in light of theoretical expectations for conifer adaptations to drought and freeze-thaw cycles with particular attention to hydraulic traits of the stem and leaf. Additionally, we examined the commonality and spatial distribution of poly-stress along indices of these combined stressors. We found that locations with the highest values of our poly-stress index (PSi) are characterized by moderate drought and moderate freeze-thaw, and most of the global conifer distribution occupies areas of moderate poly-stress. Among traits examined, we found diverse responses to the stressors. Turgor loss point did not correlate with freeze-thaw or drought stress individually, but did with the PSi, albeit inverse to what was hypothesized. Leaf mass per area was more strongly linked with drought stress than the poly-stress and not at all with freeze-thaw stress. In stems, the water potential causing 50% loss of hydraulic conductivity became more negative with increasing drought stress and poly-stress but did not correlate with freeze-thaw stress. For these traits, we identified a striking lack of coverage for substantial portions of species ranges, particularly at the upper boundaries of their respective PSis, demonstrating a critical gap in our understanding of trait prevalence and plasticity along these stress gradients. Future research should investigate traits that confer tolerance to both freeze-thaw and drought stress in a wide range of species across broad geographic scales. Majority of conifer extent subjected to moderate poly-stress. Traits that correlated with drought stress also correlated with poly-stress. Paucity of trait data reflects a need for range-wide sampling.

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