Summary
Soil flooding is a severe abiotic stress for many plant species (e.g., most crops), whereas well adapted species (e.g., rice (Oryza sativa) and other wetland species) usually thrive. Flooded soils are usually anaerobic, so that internal O2 transport from shoot to roots is crucial for sustaining respiration in submerged organs. Formation of aerenchyma, together with a barrier impermeable to radial O2 loss in basal zones of roots, act synergistically to enhance O2 diffusion to the apex of the main axis of roots of many wetland species. In some situations the soil is not anoxic, but provides a restricted O2 supply to the roots. For roots with aerenchyma, O2 is usually much more readily available from the intercellular gas-filled pathway, than exogenously from the soil. In both types of situations some cells/tissues may become anoxic, especially the apical regions and the stele since these are at the ends of the longitudinal (gas phase) and radial (predominately liquid phase) diffusion paths, respectively. Anoxia in root tissues becomes even more likely when shoots of plants are submerged by floodwaters. The inhibition of oxidative phosphorylation due to anoxia causes a severe energy crisis. Tolerance of anoxia requires a carbohydrate supply to fuel anaerobic catabolism, and apportionment of the scarce available energy to processes essential to survival, whereas several energy-consuming processes typical for aerobic cells may be reduced. In addition to O2-deficiency, roots in waterlogged soils must also tolerate high CO2 partial pressures (e.g., up to 43 kPa); however, information on this topic is scant.
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Colmer, T.D., Greenway, H. (2005). Oxygen Transport, Respiration, and Anaerobic Carbohydrate Catabolism in Roots in Flooded Soils. In: Lambers, H., Ribas-Carbo, M. (eds) Plant Respiration. Advances in Photosynthesis and Respiration, vol 18. Springer, Dordrecht. https://doi.org/10.1007/1-4020-3589-6_8
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