Leaves as bottlenecks: The contribution of tree leaves to hydraulic resistance within the soil−plant−atmosphere continuum. (6th January 2023)

• Record Type: Journal Article
• Authors: Wolfe, Brett T.; Detto, Matteo; Zhang, Yong‐Jiang; Anderson‐Teixeira, Kristina J.; Brodribb, Tim; Collins, Adam D.; Crawford, Chloe; Dickman, L. Turin; Ely, Kim S.; Francisco, Jessica; Gurry, Preston D.; Hancock, Haigan; King, Christopher T.; Majekobaje, Adelodun R.; Mallett, Christian J.; McDowell, Nate G.; Mendheim, Zachary; Michaletz, Sean T.; Myers, Daniel B.; Price, Ty J.; Rogers, Alistair; Sack, Lawren; Serbin, Shawn P.; Siddiq, Zafar; Willis, David; Wu, Jin; Zailaa, Joseph; Wright, S. Joseph
• Is Part Of: Plant, cell and environment. Volume 46:Number 3(2023)
• Page Start: 736
• Page End: 746
• Publication Date: 2023-01-06
• Subjects: drought response -- hydrodynamic modelling -- leaf hydraulic conductivity -- plant hydraulics -- plant water relations -- whole‐tree hydraulic conductance; Plant physiology -- Periodicals; Plant cells and tissues -- Periodicals; Plant communities -- Periodicals; 581.105
• DOI: 10.1111/pce.14524
• Languages: English
• ISSNs: 0140-7791

Abstract

Abstract: Within vascular plants, the partitioning of hydraulic resistance along the soil‐to‐leaf continuum affects transpiration and its response to environmental conditions. In trees, the fractional contribution of leaf hydraulic resistance (Rleaf ) to total soil‐to‐leaf hydraulic resistance (Rtotal ), or fRleaf (=Rleaf /Rtotal ), is thought to be large, but this has not been tested comprehensively. We compiled a multibiome data set of fRleaf using new and previously published measurements of pressure differences within trees in situ. Across 80 samples, fRleaf averaged 0.51 (95% confidence interval [CI] = 0.46−0.57) and it declined with tree height. We also used the allometric relationship between field‐based measurements of soil‐to‐leaf hydraulic conductance and laboratory‐based measurements of leaf hydraulic conductance to compute the average fRleaf for 19 tree samples, which was 0.40 (95% CI = 0.29−0.56). The in situ technique produces a more accurate descriptor of fRleaf because it accounts for dynamic leaf hydraulic conductance. Both approaches demonstrate the outsized role of leaves in controlling tree hydrodynamics. A larger fRleaf may help stems from loss of hydraulic conductance. Thus, the decline in fRleaf with tree height would contribute to greater drought vulnerability in taller trees and potentially to their observed disproportionate drought mortality. Summary Statement: In trees, we found that leaves contribute a large and varying fraction of the total hydraulic resistance within the soil‐to‐leaf continuum that feeds the transpiration stream.