The temporal response to drought in a Mediterranean evergreen tree: comparing a regional precipitation gradient and a throughfall exclusion experiment
Like many midlatitude ecosystems, Mediterranean forests will suffer longer and more intense droughts with the ongoing climate change. The responses to drought in long‐lived trees differ depending on the time scale considered, and short‐term responses are currently better understood than longer term...
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Published in | Global change biology Vol. 19; no. 8; pp. 2413 - 2426 |
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Main Authors | , , , , , , |
Format | Journal Article |
Language | English |
Published |
Oxford
Blackwell Publishing Ltd
01.08.2013
Wiley-Blackwell Wiley |
Subjects | |
Online Access | Get full text |
ISSN | 1354-1013 1365-2486 |
DOI | 10.1111/gcb.12215 |
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Summary: | Like many midlatitude ecosystems, Mediterranean forests will suffer longer and more intense droughts with the ongoing climate change. The responses to drought in long‐lived trees differ depending on the time scale considered, and short‐term responses are currently better understood than longer term acclimation. We assessed the temporal changes in trees facing a chronic reduction in water availability by comparing leaf‐scale physiological traits, branch‐scale hydraulic traits, and stand‐scale biomass partitioning in the evergreen Quercus ilex across a regional precipitation gradient (long‐term changes) and in a partial throughfall exclusion experiment (TEE, medium term changes). At the leaf scale, gas exchange, mass per unit area and nitrogen concentration showed homeostatic responses to drought as they did not change among the sites of the precipitation gradient or in the experimental treatments of the TEE. A similar homeostatic response was observed for the xylem vulnerability to cavitation at the branch scale. In contrast, the ratio of leaf area over sapwood area (LA/SA) in young branches exhibited a transient response to drought because it decreased in response to the TEE the first 4 years of treatment, but did not change among the sites of the gradient. At the stand scale, leaf area index (LAI) decreased, and the ratios of stem SA to LAI and of fine root area to LAI both increased in trees subjected to throughfall exclusion and from the wettest to the driest site of the gradient. Taken together, these results suggest that acclimation to chronic drought in long‐lived Q. ilex is mediated by changes in hydraulic allometry that shift progressively from low (branch) to high (stand) organizational levels, and act to maintain the leaf water potential within the range of xylem hydraulic function and leaf photosynthetic assimilation. |
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Bibliography: | istex:484E8BD0AD171AA4627E88B44B6FC8DA7E8C1C24 ArticleID:GCB12215 ark:/67375/WNG-C7B17K5K-R Appendix S1. Detailed description of hydraulic measurements. Table S1. Yearly allometric relationships between log (LA) and log (SA) of apical current-year shoots in both treatments of the TEE (Control and Dry). Table S2. Allometric relationships between log (LA) and log (SA) of branches sampled in 2009 at the proximal end growth unit 2004 in both treatments of the TEE (Control and Dry). Table S3. Allometric relationship between log (LA) and log (SA) of branches sampled in 2010 at the proximal end growth unit 2004 in all sites of the gradient (Mesic, Intermediate, and Xeric). Table S4. Allometric relationships between log (height) and log (DBH) of trees sampled in 2010 for all sites of the gradient (Mesic, Intermediate, and Xeric). French Research Agency - No. ANR-06-VULN-003-01 Agence de l'Environnement et de la Maîtrise de l'Energie SourceType-Scholarly Journals-1 ObjectType-Feature-1 content type line 14 ObjectType-Article-1 ObjectType-Feature-2 content type line 23 ObjectType-Article-2 |
ISSN: | 1354-1013 1365-2486 |
DOI: | 10.1111/gcb.12215 |