Limoniastrum guyonianum behavior under seasonal conditions fluctuations of Sabkha Aïn Maïder (Tunisia)
Introduction
The Mediterranean region, especially the southern basin, is characterized by a large fluctuation of precipitation in terms of quantity and distribution throughout the year, severe drought, and high temperatures associated with a significant evapo-transpiration favouring the accumulation of salts in the soil. This situation has become more complex with the tangible impact of climate change which increases desertification and soil salinization leading to the restriction of cultivated areas (Abdel Latef, 2010; Rozema and Flowers, 2008). Besides this stressful condition, the overgrazing aggravates the situation of wild plants, some species have disappeared, and others are threatened, growing genetic erosion leading to a huge forage deficit which accentuated desertification phenomenon (Abdellaoui et al., 2017; Aïdoud et al., 2006). These environmental changes have increased marginalized lands generally characterized by low yield and reduced economic income. Currently, the exploitation of these areas has become a necessity (Munns and Tester, 2008). The sustainable and equitable management of these vulnerable ecosystems with high added value can be achieved by valuing plant species chosen according to their degree of adaptation and their ecological and economic importance.
Halophytes have a high tolerance to salinity and could potentially be exploited due to their ecological and economic interests (Abdelly et al., 2006; Laudadio et al., 2009; Nedjimi, 2011) seem to constitute a valuable tool for the creation of productive systems under extreme environmental conditions. Generally, the halophytes dominate the marginal saline areas thanks to their ability to tolerate very high soil salinity and to achieve their life cycle independent of the salt effects, which gives these plants a great important role in the restoration, rehabilitation, and protection of saline biotope (Flowers and Colmer, 2008). Besides, the saline agriculture of many forages and edible halophytes is more and more recommended in recent years (Rozema and Schat, 2013; Salem et al., 2010; Ventura et al., 2015). In saline biotope of arid regions, halophytes are exposed to a set of environmental factors such as severe salinity, drought, high temperature, low precipitation, and high UV-radiation (Chaves et al., 2002; Elnaggar et al., 2020; Souid et al., 2018), which can lead to various abiotic stresses. To counteract the stressful conditions, these plants exhibit a series of complementary potent adequate and effective tolerance mechanisms such as physiological, biochemical, and morpho-anatomical adaptation.
Among the main mechanisms used to cope with saline stress, these can be mentioned: control of Na+ and Cl− fluxes, salt vacuolar compartmentalization, salt secretion (secretary glands or hairs) and/or the excretion of excess salt, succulence, the accumulation of compatible osmolytes and organic acids, activation of antioxidant enzymes and the biosynthesis of effective antioxidant compounds (Flowers and Colmer, 2008; He et al., 2019; Yamamoto et al., 2015). Under stressful conditions, osmotic adjustment is a vital strategy for the plant to control osmotic homeostasis between vacuole and cytoplasm, helping to maintain tissue hydration. This osmoregulation is related to the ability of plants to accumulate certain inorganic ions (Na+ and Cl−) and organic compounds (such as proline, glycine betaine, sugars, and organic acids) to regulate the osmotic potential (Raven, 1985; Shabala and Shabala, 2011; Slama et al., 2015). The stressful environmental conditions also can cause oxidative stress by promoting the reactive oxygen species (ROS) generation (Munns, 2002; Yang and Guo, 2018). To mitigate the oxidative damage (lipids peroxidation, proteins, and DNA degradation) induced by abiotic stress, plants have developed an effective antioxidant defence system that can be of enzymatic nature through the activation of several antioxidant enzymes and/or the accumulation of secondary metabolites (Boughalleb et al., 2020; Isayenkov and Maathuis, 2019). Phenolic compounds like phenolic acids and flavonoids are classified among the most important secondary metabolites that can play an antioxidant role in minimizing the harmful effects of abiotic stress (Falleh et al., 2013; Ksouri et al., 2008; Shafeiee and Ehsanzadeh, 2019). In addition to their role in osmotic adjustment and the protection of plasma membrane integrity, many osmolytes such as proline, glycine betaine, soluble sugars, play a role in scavenging reactive oxygen species (ROS) (Abd El-Maboud and Abd Elbar, 2020; Slama et al., 2015; Szabados and Savouré, 2010).
Limoniastrum guyonianum Boiss belonging to the Plumbaginaceae family growing in the deserts of North Africa especially in Northern Sahara (Algeria, Tunisia) in the salty soils of the great chotts (Quezel and Santa, 1963). This halophyte is characterized by the presence of salt glands that contribute to salt excess excretion (Ding et al., 2010; Yuan et al., 2016). Commonly used for dune stabilization and landscaping (Zouhaier et al., 2015b) also used in folk medicine as anti-dysenteric, antibacterial, antidiabitic (Hammami et al., 2011; Telli et al., 2016). Photochemical studies have shown that this species presents anti-inflammatory and antitumor proprieties (Krifa et al., 2015; Trabelsi et al., 2013). However, no study has been carried out on the impacts of environmental condition changes on L. guyonianum grown in their natural habitats yet. Saline habitats could be subjected; in addition to salinity; to high temperature, drought, flooding, active deflation depending on site and seasons (Al Hassan et al., 2017b; Souid et al., 2018)). Thus, halophytes behavior to their habitats environmental conditions is complex. In our study, L. guyonianum grows in the shott of Sebkha of Aïn Maider – (Boughrara- Medenine, Tunisia), a salt-encrusted plain subjected to periodic flooding (Oueslati, 1992). Consequently, this study aimed to evaluate the monthly physiological and biochemical behavior of L. guyonianum in relation to the environmental conditions of the Sabkha of Aïn Maïder by modeling its response to seasonal climatic conditions over a year and examining the possible relationship between responses changes and the metrolo-edaphic conditions in its natural biotope.
Section snippets
Plant material sampling
Limoniastrum guyonianum shoots were used as the plant material in this work. The plant harvested from its natural habitat, the shott of Sebkha of Aïn Maider – Boughrara, a south-eastern coastal area, located at 33°27′52″N, 10°43′31″E, with 35 km distance from the city of Medenine, Tunisia. The climate of the region is arid continental characterized by an annual precipitation not exceeding 150 mm with a long period of water deficit. The average minimum and maximum temperatures are around 15 and
Meteorological and soil physicochemical measurements
Monthly climatic conditions of the study site are shown in T able 1. Our results showed the presence of two seasons, a dry period extending from April to August and a wet period from September to March. The temperature varies between 10.7 °C and 30.9 °C in January and August respectively. The rainfall is zero in summer while it varies between 6 mm in May and 51.4 mm in October (Table 1). An exponential model (Eq. (3), R2 > 0.90) could quantify well the variation in the soil parameters (Table 2
Discussion
Based on our results, a moderate salinity (rainy period) did not affect the RWC of L. guyonianum shoots, while at a high salinity (dry period), the RWC moderately decreased (≤10.5% in August); indicating that despite the combined effects of salinity, drought and temperature, L. guyonianum was able to maintain tissue hydration. Similarly, Maaloul et al. (2021) showed a moderate decrease of RWC (≤24%) of Limonium pruinosum and Limonium tunetanum during the dry season in the Sabkha biotope. In
Conclusion
Our work showed that Na + accumulation in L. guyonianum shoots was positively correlated to EC and soil Na + contrarily to the other plant nutrients (i.e., K+, Ca2+, and Mg2+), which showed a decrease in their content with increasing EC and soil Na+. Similar trend was observed when correlating shoots Na+ and plant nutrients (i.e., K+, Ca2+, and Mg2+) with temperature. As a result, to deficit in nutrients especially K+ and Mg2+ and to a lesser degree Ca2+, the Ψw, photosynthetic pigments and
Author contribution statement
Fayçal Boughalleb and Raoudha Aabdellaoui conceived and designed the experiments. Sameh Maaloul, Mmaher Mahmoudi and Mahmoud Mabrouk conducted experiments; Esmaeil Bakhshandeh conducted the modeling and interpreted the data. Fayçal Boughalleb, Esmaeil Bakhshandeh and Raoudha Aabdellaoui co-wrote all drafts of the paper and also approved the final draft for submission. Fayçal Boughalleb supervised the work.
Funding
Tunisian Ministry of Higher Education and Scientific Research (LR16IRA03) and the Genetics and Agricultural Biotechnology Institute of Tabarestan (GABIT), and Sari Agricultural Sciences and Natural Resources University (SANRU).
Declaration of competing interest
The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.
Acknowledgment
This study was supported by the Tunisian Ministry of Higher Education and Scientific Research (LR16IRA03) and the Genetics and Agricultural Biotechnology Institute of Tabarestan (GABIT), and Sari Agricultural Sciences and Natural Resources University (SANRU), Iran based on the joint research project agreement between IRA-Medenine and GABIT in March 2020.
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