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Assessment of O 2 diffusivity across the barrier to radial O 2 loss in adventitious roots of Hordeum marinum
Author(s) -
Garthwaite Alaina J.,
Armstrong William,
Colmer Timothy D.
Publication year - 2008
Publication title -
new phytologist
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 3.742
H-Index - 244
eISSN - 1469-8137
pISSN - 0028-646X
DOI - 10.1111/j.1469-8137.2008.02467.x
Subject(s) - suberin , biophysics , biology , cell wall , thermal diffusivity , respiration , botany , endodermis , anatomy , physics , quantum mechanics
Summary• The subapical regions of wetland plant roots can develop a barrier to radial O 2 loss (ROL), but barrier resistance has rarely been quantified in terms of its O 2 diffusivity. • Barrier resistance in adventitious roots of the waterlogging‐tolerant Hordeum marinum was assessed from measurements of ROL using cylindrical platinum electrodes while either varying shoot O 2 partial pressures or cooling the rooting medium. Anatomical features were examined using fluorescence microscopy. • When grown in stagnant agar nutrient solution, a barrier to ROL was induced over the basal half of 100–120‐mm‐long roots. Autofluorescence in hypodermal cell walls indicated that putative suberin deposition was coincident with barrier expression. Root cooling revealed a significant respiratory component in barrier resistance. Eliminating the respiration effect by manipulating shoot O 2 partial pressures revealed an O 2 diffusivity for the barrier of 5.96 × 10 −7 cm 2 s −1 , 96% less than that at the apex, which was ≥ 1.59 × 10 −5 cm 2 s −1 . • It is concluded that the ROL barrier is a manifestation of two components acting synergistically: a physical resistance caused principally by secondary cell‐wall deposits in the outer hypodermal layer; and respiratory activity in the hypodermal/epidermal layers; with physical resistance being the dominant component.