Abstract
Higher plants (for the most part of their life cycle strict aerobes) are often challenged by environmental conditions (flooding, ice crusts sealing soil surface etc.) that deprive them of oxygen. In water-filled soil pores the diffusional resistance for gases is several orders of magnitude higher than in air-filled pores (Armstrong 1979). As a result, the oxygen concentration at the root surface drops dramatically, which inhibits mitochondrial respiration in root cells, since the requirement for oxygen as terminal electron acceptor is absolute (Aldrich et al. 1985; Andreev et al. 1991). Even the so-called flood-tolerant species (Oryza sativa, Erythrina caffra, Trapa nutans, Echinochloa crus-galli etc.) could tolerate anaerobiosis for only a short time (Kennedy et al. 1992). Consequently, hypoxic/anoxic conditions often cause severe losses in crop production (an important practical problem in agriculture). Tolerance by plant roots of phases of partial or complete oxygen deficiency indeed differs greatly with plant species, but also with other environmental factors. Among the latter, the type of nitrogen source (nitrate or ammonium) appears to affect plant tolerance to hypoxia or anoxia, as already noticed by Arnon (1937):
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Stoimenova, M., Kaiser, W.M. (2004). The Role of Nitrate Reduction in Plant Flooding Survival. In: Esser, K., Lüttge, U., Beyschlag, W., Murata, J. (eds) Progress in Botany. Progress in Botany, vol 65. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-18819-0_14
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DOI: https://doi.org/10.1007/978-3-642-18819-0_14
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