Journal
NEW PHYTOLOGIST
Volume 231, Issue 1, Pages 285-296Publisher
WILEY
DOI: 10.1111/nph.17374
Keywords
air injection; bench dry; centrifuge; drought; embolism; xylem
Categories
Funding
- National Science Foundation [NSF IOS-1258186, 1656876]
- Direct For Biological Sciences [1656876] Funding Source: National Science Foundation
- Division Of Integrative Organismal Systems [1656876] Funding Source: National Science Foundation
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Different methods of measuring cavitation resistance in fern petioles can lead to variable results, depending on the species being tested. The anatomy of fern dictyostele structure affects air entry into the xylem, impacting the shape of the vulnerability curve. Validation of the curves with in situ measures of water potential and hydraulic data is important for generating realistic results.
Different methods of measuring cavitation resistance in fern petioles lead to variable results, particularly with respect to the P-50 metric. We hypothesised that the fern dictyostele structure affects air entry into the xylem, and therefore impacts the shape of the vulnerability curve. Our study examined this variation by comparing vulnerability curves constructed on petioles collected from evergreen and deciduous ferns in the field, with curves generated using the standard centrifuge, air-injection and bench-top dehydration methods. Additional experiments complemented the vulnerability curves to better understand how anatomy shapes estimates of cavitation resistance. Centrifugation and radial air injection generated acceptable vulnerability curves for the deciduous species, but overestimated drought resistance in the two evergreen ferns. In these hardy plants, axial air injection and bench-top dehydration produced results that most closely aligned with observations in nature. Additional experiments revealed that the dictyostele anatomy impedes air entry into the xylem during spinning and radial air injection. Each method produced acceptable vulnerability curves, depending on the species being tested. Therefore, we stress the importance of validating the curves with in situ measures of water potential and, if possible, hydraulic data to generate realistic results with any of the methods currently available.
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