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对滨海大麦不定根中径向氧气损失屏障的氧气扩散率的评估。

Assessment of O2 diffusivity across the barrier to radial O2 loss in adventitious roots of Hordeum marinum.

作者信息

Garthwaite Alaina J, Armstrong William, Colmer Timothy D

机构信息

School of Plant Biology and.

Future Farm Industries CRC, Faculty of Natural and Agricultural Sciences, The University of Western Australia, Crawley, 6009 Western Australia.

出版信息

New Phytol. 2008 Jul;179(2):405-416. doi: 10.1111/j.1469-8137.2008.02467.x.

DOI:10.1111/j.1469-8137.2008.02467.x
PMID:19086178
Abstract

The subapical regions of wetland plant roots can develop a barrier to radial O2 loss (ROL), but barrier resistance has rarely been quantified in terms of its O2 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 O2 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 O2 partial pressures revealed an O2 diffusivity for the barrier of 5.96 x 10(-7) cm2 s(-1), 96% less than that at the apex, which was > or = 1.59 x 10(-5) cm2 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.

摘要

湿地植物根系的根尖下区域能够形成一道阻止径向氧气损失(ROL)的屏障,但屏障阻力很少根据其氧气扩散率进行量化。通过使用圆柱形铂电极测量ROL,同时改变地上部氧气分压或冷却生根介质,评估了耐涝植物海大麦不定根中的屏障阻力。使用荧光显微镜检查解剖特征。当在静止的琼脂营养液中生长时,在100 - 120毫米长的根的基部一半区域诱导形成了一道ROL屏障。皮下细胞壁中的自发荧光表明,假定的木栓质沉积与屏障表达一致。根系冷却揭示了屏障阻力中存在显著的呼吸成分。通过操纵地上部氧气分压消除呼吸作用后,屏障的氧气扩散率为5.96×10⁻⁷平方厘米每秒,比根尖处的氧气扩散率低96%,根尖处的氧气扩散率≥1.59×10⁻⁵平方厘米每秒。得出的结论是,ROL屏障是两种成分协同作用 的表现:一种主要由外部皮下层的次生细胞壁沉积物引起的物理阻力;以及皮下 / 表皮层中的呼吸活动;其中物理阻力是主要成分。

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