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On the mechanism of salt tolerance in olive (Olea europaea L.) under low- or high-Ca2+ supply
Authors:Massimiliano Tattini  Maria Laura Traversi
Institution:2. School of Chemical, Biological and Environmental Engineering, 102 Gleeson Hall, Oregon State University, Corvallis, OR 97331-2702, United States;1. Key Laboratory of Horticultural Plant Biology, Ministry of Education, Huazhong Agricultural University, No. 1, Shizishan Street, Hongshan District, Wuhan, Hubei 430070, China;2. Key Laboratory of Biology and Genetic Resources of Rubber Tree, Ministry of Agriculture, Rubber Research Institute, Chinese Academy of Tropical Agricultural Sciences, Danzhou 571737, China;1. Beijing Key Laboratory of Materials Utilization of Nonmetallic Minerals and Solid Wastes, National Laboratory of Mineral Materials, School of Materials Science and Technology, China University of Geosciences, Beijing, 29 Xueyuan Road, Beijing 100083, China;2. Geosciences Department, University of Wisconsin-Parkside, Kenosha, WI 53144, USA;3. Department of Earth Science, National Cheng Kung University, Tainan 70101, Taiwan;1. BioLabs, Institute of Life Sciences, Scuola Superiore Sant’Anna, Pisa, Italy;2. Instituto de la Grasa (CSIC), Campus Universitario Pablo de Olavide, Sevilla, Spain;1. Olive Institute, University of Sfax, PO Box 1087, 3000, Sfax, Tunisia;2. National Engineering School of Sfax, University of Sfax, Route de la Soukra km, 4 - 3038 Sfax, Tunisia;3. Research Centre for Plant Growth and Development, School of Life Sciences, University of KwaZulu-Natal Pietermaritzburg, Private Bag X01, Scottsville, 3209, South Africa;1. Key Laboratory of Conservation and Utilization for Bioresources and Key Laboratory of Microbial Diversity in Southwest China, Ministry of Education, Yunnan University, Kunming 650091, Yunnan, China;2. School of Agriculture, Yunnan University, Kunming 650091, Yunnan, China
Abstract:The effect of changes in Ca2+/Na+ ratios at the root zone has been reported in Olea europaea, a species mostly cultivated in calcareous soils. Plants were exposed to low (2.0 mM, low-Ca) or high-Ca2+ supply (9.0 mM, high-Ca) and supplied with 0 or 200 mM NaCl. Measurements were performed on water relations, gas exchange and photosynthetic performances, ion fluxes at whole-plant and leaf level, Na+ allocation at organismal level, the elemental and soluble carbohydrate concentration in the leaf. Most parameters were also measured during a period of relief from salinity stress, as Olea europaea suffers from fluctuating root zone NaCl concentrations over the whole growing season. High-Ca2+ supply decreased stomatal conductance, especially during the first two weeks of treatment. In response to salinity stress (i) leaf turgor potential was more severely depressed in high-Ca than in low-Ca plants, whereas net CO2 assimilation rate and relative growth rate were unaffected by root zone Ca2+ concentrations (ii) high-Ca plants had a markedly superior ability to both exclude Na+ from the shoot and to selectively transport K+ over Na+ than low-Ca plants; (iii) both CO2 carboxylation efficiency and maximal efficiency of PSII photochemistry (Fv/Fm) were significantly smaller in low-Ca than in high-Ca plants, likely as a result of a greater accumulation of toxic ions. Consistently, when osmotic stress was relieved by supplying plants with good quality water (relief period), both photosynthetic (+44%) and growth rates (+65%) recovered to a markedly superior degree in high-Ca than in low-Ca plants which had been previously treated with 200 mM NaCl. We conclude that (1) high-Ca2+ supply expose olive leaves to a more severe dehydration, but allowed to restrict both the entry and the allocation of potentially toxic ions to sensitive shoot organs; (2) a transient restriction of water-mass flow to the shoot during salinization may be of relatively minor significance in Olea europaea, which is very tolerant to drought; (3) overall salt tolerance in Olea europaea, as in most evergreen sclerophylls inhabiting Mediterranean areas, tightly depends upon the ability to reduce water uptake and transpiration during the dry/warm period and to recover photosynthetic and growth rates when low-salinity flood water is available. Therefore, data from the present experiment allow conclude that an increase in root zone Ca2+ concentration enhances tolerance to salinity stress in olive plants.
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