Introduction
Salinity is considered a significant factor that affects crop production in arid and semiarid regions of the world (Tester and Davenport, 2003). Depending on the cause, soil salinity is classified as primary (due to natural processes) and secondary or anthropic (due to human activity). In some regions, the main natural causes of salinity are the capillary rise of the phreatic layers with saline characteristics, where the source of salinity is the weathering of the original soil material of a saline nature and the constant contribution of salts received by the soils near the sea or the gradual withdrawal of the seas which leads these soils to salinization (Courel, 2019; Arulmathi and Porkodi, 2020). Among the main anthropic causes are irrigation with saline water, sudden changes in land use, and the misuse of irrigation and fertilizers (Courel, 2019).
Salinity can disrupt cell function, through the toxic effects of specific ions and by osmotic effects, or both (Munns, 2005). The detrimental effects of high salinity on plants can be seen at the whole plant level as plant death or decreased productivity. Most terrestrial plants, including agricultural crops, are glycophytes and cannot tolerate a high concentration of salt, such as the case of corn (Zea mays), wheat (Triticum aestivum), rice (Oryza sativa) and tomato (Solanum lycopersicum) (Majeed and Muhammad, 2019). Many plants develop mechanisms either to exclude salt from their cells or to tolerate its presence within the cells.
During the onset and development of salt stress within a plant, all the major processes such as photosynthesis, protein synthesis, and energy and lipid metabolism are affected. The earliest response is a reduction in plant leaf area and stomatal density, followed by growth interruption as stress intensifies, but growth resumes as salt stress decreases (Romero-Aranda, Soria and Cuartero, 2001).
Carbohydrates, among other substances, are necessary for cell growth and are supplied primarily through the process of photosynthesis. When plants are exposed to salt stress, especially NaCl, photosynthesis rates are usually lower and vary depending on the type of plant (glycophytes or halophytes) and the level of salinity to which they are exposed (Parida and Das, 2005; Hniličková, Kraus, Vachová and František 2021; Wang et al., 2022).
Salt tolerance in plants is a complex phenomenon that includes morphological changes and physiological and biochemical processes such as the elimination of salts by regulating the fall of leaves and in extreme cases of fruits (Del Amor-Saavedra, 2001), the elimination of excess salts through glands or specialized structures such as vesicular hairs, alteration in membrane structure (González, González and Ramírez, 2002), change in photosynthetic pathways, the accumulation or synthesis of proteins and amino acids that intervene in the osmotic adjustment (Ashraf and Harris, 2004), the selective accumulation or exclusion of ions at the root level and the retention of ions in the vacuoles of growing roots or in different organs (ElYacoubi et al., 2022), the accumulation of soluble carbohydrates to increase the osmotic potential (Murakeözy, Nagy, Duhazé, Bouchereau and Tuba, 2003).
To cultivate plants on salt-affected soils, tolerant plants with valued economic traits are required. Various investigations have identified halophytic plants of agroecological importance that grow well in coastal habitats, for example, Crithmum maritimum, Inula chritmoides, and Salicornia bigelovii (Ravindran, Venkatesan, Balakrishnan, Chellappan and Balasubramanian, 2007; Qadir et al., 2008; Rueda-Puente, López and Huez, 2012; González-Villaveces, 20221).
Coccoloba uvifera (L.) L. (Polygonaceae), also called sea grape, is a tree with branches at a low level that grows up to 15 m in height, it is widely distributed along the Atlantic, Caribbean, and Pacific coasts of the American tropics and subtropics (Parrotta, 2000). It is used as a fruit tree (edible fruit), an ornamental plant for exteriors, and as a windbreak along the beaches and roads of the Caribbean.
Sea grape is considered a woody plant, drought resistant and non-halophilous relatively salt tolerant, growing mainly in stands within well-drained sandy soils with a slightly alkaline pH (Parrotta, 2000; Larcher, 2003). Although several authors have reported that the sea grape is tolerant to salt stress, in the sources consulted, there is no information related to the physiological and biochemical mechanisms used by this plant to grow in environments with high salt content. However, Guzmán, Ramírez, Miller, Lodge and Baroni (2004), Bâ, McGuire and Diédhiou (2014) and Séne et al. (2018) reported that this tree is associated with ectomycorrhizal fungi of the genera Amanita, Inocybe, Cantharellus, Melanogaster, Cenococcum, Lactarius, Russula, Thelephoraceae, Xerocomus and Scleroderma, on the other hand, Bandou et al. (2006) and Bullaín et al. (2022) observed that the tolerance of sea grape to salt stress is considerably improved by S. bermudense.
The knowledge of the effect of salt stress on the morphological and physiological traits of plants is important for the selection of plant material tolerant to salinity and the management of crops in soils affected by high concentrations of salts and can be used as one of the most challenging strategies to help organisms under stress conditions (Vahdati and Leslie, 2013).
The objective of the study was to evaluate the effect of salt stress on morphological and physiological traits in C. uvifera seedlings from different edaphic conditions and to select traits whose behavior under salt stress can be used as an effective criterion of tolerance to salinity under greenhouse conditions.
Materials and Methods
Collection of sea grape fruits
Sea grape seeds from three representative origins were collected in the northern and southern coastal areas of Cuba based on the presence of 40-year-old sea grape populations. The geographic location, annual precipitation, mean annual temperature, pH, and electrical conductivity of the soil of the selected origins are given in Table 1. Samples of 20 sea grape trees were randomly taken from each origin. Ripe fruits without damage or malformations were collected from different positions in the crown and placed in labeled plastic bags.
The fresh fruits were transported to the laboratory and the pulp surrounding the seed was manually removed, washed with potable water, and dried at a room temperature of 32-35 °C for 72 hours on 50 × 30 cm cardboard trays.
Origin | Location and environmental conditions of the three origins | |||||
Latitude | Longitude | MAP | MAT | pH | EC | |
mm | °C | dS m-1 | ||||
Las Coloradas | 19° 56' 00'' | 77° 41' 00'' | 942 | 27.0 | 8.91 | 7.62 |
Guardalavaca | 21° 07' 30'' | 75° 49' 44'' | 974 | 26.4 | 8.84 | 7.31 |
Cayo Coco | 22° 32' 10.06'' | 78° 21' 19.44'' | 855 | 25.6 | 8.75 | 7.84 |
† MAP = mean annual precipitation; MAT = mean annual temperature; EC = electric conductivity.
Experimental design, plant material and environmental conditions
C. uvifera seedlings grew for sixteen weeks following a completely randomized design with a factorial arrangement, consisting of three origins (Cayo Coco, Guardalavaca, and Las Coloradas) and four salinity levels (0, 5, 15, and 25 dS m-1). A total of 12 treatments were compared, each with ten repetitions, and one plant per pot was established as the experimental unit.
To break dormancy, seeds were scarified in 95% sulfuric acid for 2 hours, and every 20 min the container was shaken to achieve the uniform action of the acid on the surface of the seeds (Bandou et al., 2006). Then, they were rinsed with abundant distilled water and then germinated in pots (20 × 12 cm) with 1 kg of river sand, collected from the banks of the Yao River (20°15’ 32.3” N, 76° 45’ 19.3” W) in Granma province, previously sterilized for one hour at 121 °C and 1.2 kg/cm2 pressure in a vertical autoclave (BK-75, T3MOИ, Ukraine). After germination, the seedlings were maintained under good irrigation conditions for eight weeks (50 ml of potable water every 48 hours).
The analysis of the substrate was carried out in the Soil Laboratory of the Ministry of Agriculture of the Granma Province (Cuba) and the following determinations were made following the methodology proposed by Paneque et al. (2010):
K and Na: by the flame photometry method.
Ca and Mg: by the volumetric method with EDTA.
Assimilable P in the soil: by the Olsen method.
pH (KCL): by the potentiometric method, in a ratio of substrate: solution 1:2.5.
% of organic matter (OM): by the wet combustion method.
Electrical Conductivity (EC): by the method of estimation of salinity by the electrical conductivity of the extract of saturation of the substrate, using a portable conductivity meter (HANNA. HI 9033. Romania).
The result of the analysis of the substrate showed the following composition (mg L-1): 67 K, 23.2 Na, 82.14 Ca, 28.12 Mg, 3.7 Olsen-P, pH (KCL) 7.2, 1.36% OM, and electrical conductivity (EC) 0.81 deciSiemens per meter.
The seedlings grew in a climatic cabinet (Snijders Scientific. ECL02. Netherlands) (day/night temperatures of 35/25 °C, relative humidity of 80%, and photoperiod of 12 hours of day-length).
Experimental conditions and controlled variables
The NaCl concentration range was based on a field assessment of soil salinity in sea grape stands (Bojórquez et al., 2008; Herrera-Romero, Bojorquez, Can, Madueño and García, 2019). Over the course of four weeks, the seedlings were brought to the desired salinity level for each treatment by adding NaCl (PanReac, Reagent Grade) in the irrigation. To avoid osmotic shock, a volume of 50 ml of NaCl solution with an electrical conductivity of 2 dS m-1 was added to the substrate every 3 days. Upon reaching the desired salinity level for each treatment, exposure to salinity through irrigation was extended for sixteen weeks. The Na+ ions present in the substrate were leached with potable water every seven days to reduce salt accumulation. After each leaching, a volume of 50 ml of fresh saline solution was added to keep the NaCl concentration. The salinity was controlled weekly by the method of estimation of salinity by the electrical conductivity of the extract of saturation of the substrate (Torres, Camberato, Lopez and Mickelbart, 2010) using a portable conductivity meter (HANNA. HI 9033. Romania).
The chlorophyll fluorescence parameters, basal fluorescence (Fo), maximum fluorescence (Fm), variable fluorescence (Fv) the maximum quantum yield of photosystem II (Fv/Fm), the variable fluorescence initial fluorescence ratio (Fv/Fo), and performance index on absorption basis (PIabs) were measured with a portable chlorophyll fluorimeter (Hansatech Instruments, RS232, United Kingdom), only one measurement was made in the fourth fully expanded leaf of each plant (ten plants per treatment, n = 10) in the morning. Before taking the measurement, the leaves were dark-adapted for 30 min using the clips provided with the kit. A saturating pulse of radiation (3500 μmol m−2 s−1 with the help of three light-emitting diodes of 650 nm) was given for (from 10 μs to 1 s) allowing to determine these parameters related to the fluorescence of chlorophyll.
After harvest, root, and stem length were measured and leaf area was determined using a foliar area meter (ADC BioScientific, AM350, United Kingdom) (ten plants per treatment, n = 10). The excess of the substrate was removed from the roots gently with potable water, then the excess water was removed from the surface of the plant using absorbent paper and the fresh weight of the aerial parts (FWAP) and the roots were immediately determined (FWR) with an analytical laboratory balance (Denver Instrument, TP-214, USA). The dry weight of aerial parts (leaves and stem) (DWAP) and roots (DWR) was measured after drying the samples at 80 °C until reaching a constant weight in an oven with air recirculation (Memmert, UNB 200, Germany). Root shoot ratio (RSR) was calculated as the ratio of the dry weight of roots to the dry weight of aerial parts (DWR/DWAP = RSR) (Rogers, Zalesny, Hallett, Headlee and Wiese, 2019).
The specific leaf area (SLA) was calculated using the formula (SLA = Leaf area (cm2)/dry weight of leaves (g) (Nageswara, Talwar and Wright, 2001). The leaf water content (LWC) and root water content (RWC) were calculated following the methodology of Cuni, De Smedt, Haq and Samson (2011):
LWC = 100 * (fresh weight of leaves - dry weight of leaves)/fresh weight of leaves.
RWC= 100* (fresh weight of roots - dry weight of roots)/fresh weight of roots.
Statistical analysis
Prior to ANOVA analysis, the normality of the data and the homogeneity of the variances were verified using the Shapiro Wilk and Levene tests, respectively (P≥ 0.05), with the statistical software MINITAB Release 13.20 (Minitab, 2000). All data were subjected to a two-way (origin and salinity) analysis of variance, the mean values were compared using Tukey’s test (P ≤ 0.05). A simple linear regression analysis was performed and the Pearson’s correlation coefficient was determined with the InfoStat software version 2020 (Di Rienzo et al., 2020).
Results and Discussion
Effects of NaCl on morphological traits
Salt stress had a negative effect on the morphological variables evaluated in C. uvifera seedlings. Significant differences (P ≤ 0.05) were observed in all traits as the salinity level increased. The highest level of salinity (25 dS m-1) caused the death of C. uvifera seedlings. The origin, salinity, and the interaction between origin and salinity had a significant influence on each of the traits analyzed (Table 2).
Origin | Salt level | Morphological traits | |||||||
Stem length | Root length | FWAP | FWR | DWAP | DWR | RSR | LA | ||
dS m-1 | - - - - cm - - - - | - - - - - - - - - - g - - - - - - - - - - | cm2 | ||||||
Cayo Coco | 0 | 15.62 a | 10.20 a | 0.78 a | 0.14 a | 0.53 a | 0.12 a | 0.22 cd | 127.15 a |
5 | 10.42 d | 7.66 d | 0.61 b | 0.13 b | 0.32 d | 0.12 a | 0.37 b | 60.18 d | |
15 | 5.92 g | 3.70 g | 0.44 d | 0.12 c | 0.1 6g | 0.08 b | 0.49 a | 27.20 g | |
25 | 0.00 j | 0.00 j | 0.00 g | 0.00 f | 0.00 j | 0.00 e | 0.00 e | 0.00 j | |
Guardalavaca | 0 | 14.92 b | 9.80 b | 0.76 a | 0.12 c | 0.51 b | 0.08 b | 0.15 cd | 125.25 b |
5 | 9.66 e | 7.36 e | 0.58 c | 0.07 e | 0.31 e | 0.07 bc | 0.23 cd | 58.27 e | |
15 | 5.24 h | 3.18 h | 0.22 f | 0.07 e | 0.14 h | 0.06 bc | 0.42 ab | 25.09 h | |
25 | 0.00 j | 0.00 j | 0.00 g | 0.00 f | 0.00 j | 0.00 e | 0.00 e | 0.00 j | |
Las Coloradas | 0 | 13.38 c | 8.86 c | 0.62 b | 0.13 b | 0.49 c | 0.07 bc | 0.14 d | 122.22 c |
5 | 8.26 f | 6.40 f | 0.45 d | 0.09 d | 0.28 f | 0.05 cd | 0.19 cd | 55.22 f | |
15 | 3.74 i | 2.34 i | 0.27 e | 0.06 e | 0.12 i | 0.03 d | 0.25 c | 22.04 i | |
25 | 0.00 j | 0.00 j | 0.00 g | 0.00 f | 0.00 j | 0.00 e | 0.00 e | 0.00 j | |
Origin | S | S | S | S | S | S | S | S | |
Salinity | S | S | S | S | S | S | S | S | |
Origin × Salinity | S | S | S | S | S | S | S | S | |
C.V. (%) | 0.25 | 0.46 | 5.46 | 2.77 | 0.79 | 19.83 | 26.42 | 0.06 |
† Distinct letters in the same column indicate significant differences (Tukey, P ≤ 0.05). Values are the means (n = 10). C.V.= Coefficient of variation. S = significant (P ≤ 0.05); FWAP = fresh weight of the aerial parts; FWR = fresh weight of roots; DWAP = dry weight of aerial parts; DWR = dry weight of roots; RSR = root shoot ratio; LA = leaf area.
In the seedlings from the three locations, the growth parameters evaluated, stem length and root length, FWAP, FWR, DWAP, RSR, and the leaf area were negatively and significantly affected as the salinity level increased from 0 to 25 dS m-1. On the other hand, the DWR of the seedlings of the three localities did not show severe affections due to exposure to increased levels of salinity from 0 to 5 dS m-1 and only seedlings from Cayo Coco showed significant differences between 5 and 15 dS m-1. The RSR showed that at 15 dS m-1 the seedlings presented a significantly higher amount of biomass in the root system (Table 2).
The values of the morphological traits evaluated were significantly higher in the seedlings from Cayo Coco, while the lower values were observed in the seedlings from Las Coloradas (Table 2).
Salt stress affected the vegetative growth and leaf development of C. uvifera seedlings from the three origins. Stem length, root length, and leaf area of seedlings decreased as the salinity level increased from 0 to 25 dS m-1, although growth continued at 15 dS m-1 (Table 2).
The reduction in the values of the controlled variables as the salinity level increased coincides with the results obtained by Bullaín et al. (2022) in C. uvifera seedlings from Las Coloradas beach, but they differ in that in this study the seedlings did not survive a salinity level of 25 dS m-1, which may be the result of a longer exposure time to saline stress.
El-Juhany, Ali, Basalah and Shehatah (2014) mentioned that the reduction of the leaf area in plants under the effect of salt stress is due to the decrease in the number of leaves. Also, Chamekh et al. (2014) observed a significant reduction in leaf area as salinity level increased in 17 of 25 genotypes of Triticum turgidum ssp. durum. On the other hand, Rahneshan, Nasibi and Moghadam (2018) reported that exposure to moderate and high salinities (0, 4.5, 9.1, and 13.7 dS m-1) negatively affected stem and root length in two cultivars of Pistacia vera L.
Ahanger, Aziz, Alsahli, Alyemeni and Ahmad (2019) and Zhao, Zhang, Song, Zhu and Shabala (2020) observed that under salt stress conditions, the reduction of the values of the traits evaluated is due to the high osmotic pressure caused by the excessive accumulation of NaCl that interferes with the absorption of water and nutrients by the roots, this reduces growth and affects physiological processes such as photosynthetic rate, stomatal conductance, and transpiration rate.
Similar damage showed the FWAP, FWR, and DWAP. The values of FWAP and DWAP were higher in comparison to the FWR and DWR (Table 2), this coincides with the results obtained by Demir-Kaya, Ipek and Öztürk (2003) in which root biomass rarely overcomes stem biomass.
Plant growth is an important character in determining the salt tolerance capacity of plants. Although plant length is genetically controlled, environmental factors also have a strong influence on gene expression (Deinlein et al., 2014). The main cause of decreased plant growth based on salinity stress is reduced photosynthesis (Chartzoulakis, Loupassaki, Bertaki and Androulakis, 2002; Sivritepe, Sivritepe, Çelik and Katkat, 2010). Also, under saline stress, competition is generated between the aerial organs and the roots for the absorption of photosynthetic materials and this affects these organs (Chookhampaeng, 2011; Hsiao & Xu, 2000).
Effects of NaCl on physiological traits
Salt stress also had a significant negative effect on controlled physiological traits in C. uvifera seedlings. Under salt stress, the reduction in LWC was 15.5% at 5 dS m-1 and 36.34-36.35% at 15 dS m-1. While the RWC showed the same behavior, the reduction due to salt stress was 17.02-17.2% at 5 dS m-1 and 25.7-32.52% at 15 dS m-1 (Table 3).
Origin | Salt level | Physiological traits | ||
LWC | RWC | SLA | ||
dS m-1 | - - - - - - % - - - - - - - | cm2 g-1 | ||
Cayo Coco | 0 | 81.12a | 79.22a | 253.22a |
5 | 65.62d | 62.20d | 202.18d | |
15 | 44.77g | 46.52h | 188.28g | |
25 | 0.00j | 0.00j | 0.00j | |
Guardalavaca | 0 | 79.32b | 75.62b | 252.27b |
5 | 63.82e | 58.42e | 200.24e | |
15 | 42.97h | 49.92g | 187.14h | |
25 | 0.00j | 0.00j | 0.00j | |
Las Coloradas | 0 | 77.72c | 72.72c | 249.28c |
5 | 62.22f | 55.52f | 197.24f | |
15 | 41.38i | 40.20i | 184.14i | |
25 | 0.00j | 0.00j | 0.00j | |
Origin | S | S | S | |
Salinity | S | S | S | |
Origin × Salinity | S | S | S | |
C.V. (%) | 0.04 | 0.06 | 0.06 |
† Distinct letters in the same column indicate significant differences (Tukey, P ≤ 0.05). Values are the means (n = 10). C.V.= Coefficient of variation. S = significant (P ≤ 0.05). LWC = leaf water content; RWC = root water content; SLA = specific leaf area.
The origin, salinity, and interaction between these two experimental factors had a significant influence on the water content and the SLA of the seedlings of the three origins.
Salinity generates both water stress and osmotic stress in plants by decreasing water potential within the cells, and ionic stress due to the inhibition of specific metabolic processes such as the transport and elimination of ions, (mainly Na+, Cl−, and SO42−), (Heidari, 2012; Hniličková, Hnilička, Martinková and Kraus, 2017). The reduction of water uptake inhibits stomatal conductance, protein synthesis, and photosynthetic activity (Munns and Tester, 2008). Osmotic regulation is evidence of response to osmotic stress and in the conditions of water scarcity due to any stress, the osmotic potential decreases, and thus the relative water content of the leaves decreases (Karimi and Yusef-Zadeh, 2013). Osmotic regulation capacity is important for plants and the reduction of water potential is one of the mechanisms of resistance to salinity to maintain the higher relative water content of the leaf. The RWC is mostly correlated with the leaf area, dry weight of the leaf, amount of chlorophyll, and other growth rates indicators such as root and stem length (Kafi and Mahdavi, 2003).
The SLA is reduced under saline stress conditions and constitutes a way to improve Water-use efficiency (Bayuelo-Jiménez, Debouck and Lynch, 2003) This trait has a relation with leaf area and photosynthesis due to the sensitivity of photosynthesis and the reduction of leaf area under salt stress (El-juhany, Aref and Ahmed, 2008). Similar results were obtained by Ziaf et al. (2009) in plants of Capsicum annuum L. exposed to 2, 4, 6, and 8 dS m-1 and Elfeel and Bakhashwain (2012) in plants of Acacia saligna (Labill.) H. Wendl subjected to 1.5, 7, 9 and 12 deciSiemens per meter.
The origin, the salinity, and the interaction between these two factors significantly influenced the parameters of chlorophyll fluorescence evaluated (Table 4).
Origin | Salt level | Chlorophyll fluorescence parameters | ||||
Fo | Fm | Fv/Fm | Fv/Fo | PIabs | ||
dS m-1 | - - - - - - - - - - - - - bits - - - - - - - - - - - | |||||
Cayo Coco | 0 | 262.00c | 1806.80a | 0.86a | 5.91a | 2.04a |
5 | 281.80bc | 1644.20b | 0.83ab | 4.85b | 1.29b | |
15 | 286.60bc | 1501.80c | 0.81bc | 4.25bc | 1.00c | |
25 | 0.00d | 0.00e | 0.00e | 0.00e | 0.00g | |
Guardalavaca | 0 | 270.20c | 1809.60a | 0.85a | 5.71a | 2.04a |
5 | 284.80bc | 1649.00b | 0.83ab | 4.81b | 1.29b | |
15 | 288.40bc | 1509.20c | 0.81bc | 4.24bc | 1.00c | |
25 | 0.00d | 0.00e | 0.00e | 0.00e | 0.00g | |
Las Coloradas | 0 | 310.40b | 1496.00c | 0.79c | 3.84c | 0.28d |
5 | 374.20a | 1442.80cd | 0.74d | 2.88d | 0.20e | |
15 | 378.60a | 1341.60d | 0.72d | 2.57d | 0.14f | |
25 | 0.00d | 0.00e | 0.00e | 0.00e | 0.00g | |
Origin | S | S | S | S | S | |
Salinity | S | S | S | S | S | |
Origin × Salinity | S | S | S | S | S | |
C.V. (%) | 7.46 | 4.74 | 2.63 | 12.03 | 6.88 |
† Distinct letters in the same column indicate significant differences (Tukey, P ≤ 0.05). Values are the means (n = 10). C.V.= Coefficient of variation. S = significant (P ≤ 0.05). Fo = basal fluorescence; Fm = maximum fluorescence; Fv/Fm = maximum quantum yield of photosystem II; PIabs = performance index on absorption basis.
As the salinity level increased, a negative effect on photochemical processes was observed. The values of Fo increased and the values of Fm, Fv/Fm, Fv/Fo, and PIabs decreased in the seedlings of the three origins. The most critical values of the four parameters evaluated were observed in the seedlings from Las Coloradas.
A behavior similar to Fo was observed by De Lucena, Lopez, Prieto and Cecon (2012) and (Hniličková et al. (2017). This could be related to a decrease in the capacity to channel solar energy through photochemical pathways due to damage to the PSII reaction center or a reduction in the capacity to transfer excitation energy from the antenna to the reaction center as a result of exposure to salt stress (Baker, 2008; Jiménez-Suancha, Alvarado and Balaguera, 2015).
The reduction of Fm values with increasing salinity was observed by Erdal & Çakirlar (2014) and (Hniličková et al. (2017). This reduction may be the result of decreased chlorophyll levels, reduction in the number or severe damage to the antenna complex, accumulation of inactive reaction centers of photosystem II, and low efficiency in the photoreduction of quinone A and in the flow of electrons between the photosystems (Dan-Tatagiba, Kling, Telles and de Figueiredo 2014; de Melo, de Souza and Cunha, 2017; Tsai et al., 2019).
The reduction of Fv/Fm in plants subjected to increasing levels of salinity has been reported by several investigations (Kalaji, Govindjee, Karolina, Kościelniak and Żuk-Gołaszewska, 2011; Casierra-Posada, Peña and Vaughan, 2013; Tsai et al., 2019). The presence of (Fv/Fm) values below 0.85 suggest exposure to some type of biotic or abiotic stress (Hansatech Instruments, 20062). However, a value of 0.83 is considered acceptable for most plants (Maxwell and Johnson, 2000).
A sensitive indicator of photosynthetic activity in healthy and stressed plants is Fv/Fo (Li et al., 2010). The significant differences in the values of Fv/Fo between 0 and 5 dS m-1 in the seedlings of the three locations suggest that photosynthetic activity was affected by a slight increase in salinity, considering the high levels of salinity of the medium in which this species normally develops. The reduction of the value of Fv/Fo with the increase in the salinity level coincides with that observed by Kalaji et al. (2011), Khalid et al. (2015), Killi and Haworth (2017) and Pereira, de Siqueira, Martínez and Puiatti (2000) indicated that the reduction of Fv/Fo is a manifestation of structural damage in the photosynthetic apparatus, this causes damage to the efficiency of the photochemical processes and in the electron transport chain.
Plant vitality could be characterized by PIabs it reflects the functionality of both photosystems I and II and provides quantitative information related to the current state of plant performance under stress conditions Strasser, Srivastava and Tsimilli-Michael, 2000; Strasser, Tsimilli-Michael and Srivastava, 2004) The decrease in PIabs values and the presence of significant differences between treatments as the salinity level increased in the seedlings of the three origins coincides with a similar behavior previously observed by Kalaji et al. (2011), Sayyad-Amin, Jahansooz, Borzouei and Ajili (2016), Yasmeen and Siddiqui (2017) and Estaji, Kalaji, Karimi, Roosta and Moosavi, 2019)
The correlation analysis between the traits evaluated and the saline stress levels (Table 5) showed that the correlation coefficient was highly significant and negative in all cases, therefore, the increase in the level of salinity will decrease the values of the variables evaluated. Except for RSR where the correlation coefficient between the evaluated traits and the salinity level was between -0.68 and -0.99.
Controlled variables | Equation | r | R2 |
Stem length (cm) | y = -0.5561x + 13.519 | -0.98** | 0.95 |
Root length (cm) | y = -0.3833x + 9.2703 | -0.99** | 0.97 |
FWAP (g) | y = -0.028x + 0.7076 | -0.96** | 0.93 |
FWR (g) | y = -0.0048x + 0.1317 | -0.88** | 0.77 |
DWAP (g) | y = -0.0192x + 0.4532 | -0.97** | 0.94 |
DWR (g) | y = -0.0034x + 0.0939 | -0.78** | 0.61 |
RSR | y = -0.0057x + 0.2684 | -0.32** | 0.10 |
Leaf area (cm2) | y = -4.5389x + 102.95 | -0.93** | 0.86 |
LWC (%) | y = -3.0672x + 81.085 | -0.99** | 0.97 |
RWC (%) | y = -2.8461x + 77.046 | -0.97** | 0.93 |
SLA (cm2.g-1) | y = -9.1667x + 262.62 | -0.92** | 0.85 |
Fo (bits) | y = -10.652x + 347.91 | -0.75** | 0.56 |
Fm (bits) | y = -63.993x + 1903.3 | -0.88** | 0.78 |
Fv/Fm (bits) | y = -0.031x + 0.9511 | -0.85** | 0.72 |
Fv/Fo (bits) | y = -0.1907x + 5.4005 | -0.86** | 0.74 |
PIabs | y = -0.0528x + 1.3673 | -0.68** | 0.47 |
† R2=determination coefficient; r = correlation coefficient; ** = highly significant (P ≤ 0.01); FWAP = fresh weight of the aerial parts; FWR = fresh weight of roots; DWAP = dry weight of aerial parts; DWR = dry weight of roots; RSR = root shoot ratio; LWC = leaf water content; RWC = root water content; SLA = specific leaf area; Fo = basal fluorescence; Fm = maximum fluorescence; Fv/Fm = maximum quantum yield of photosystem II; PIabs = performance index on absorption basis.
The variation of stem length, root length, FWAP, DWAP, LWC, and RWC were determined by more than 90% by the linear relationship between the salinity level and these traits. This suggests that in C. uvifera seedlings these were the variables most sensitive to salt stress. The variation of the FWR, DWR, Leaf area, SLA, Fo, Fm, Fv/Fm, and Fv/Fo was determined by more than 50% by the relationship between these with the level of salinity. The RSR and the PIabs were the traits whose variation was less determined by the salinity level, with a coefficient of determination of 0.10 and 0.47, respectively, it is then inferred that these were the variables least affected by exposure to this type of stress.
These results coincide with those obtained by Bandou et al. (2006) who reported the reduction of stem length, leaf area, DWAP, DWR, and leaf water potential in C. uvifera seedlings subjected to increasing levels of salinity (0, 18, 30, and 45 dS m-1). This may be related to the fact that under salinity conditions macroscopic changes are observed, such as the reduction of leaf area and RSR (Leidi and Pardo, 2002). Hasan, Kawasaki, Taniguchi and Miyake (2018) indicated that the osmotic stress caused by salt accumulation within cells and tissues contributes to cell distortion and acceleration of cell death. On the other hand, it is widely reported that salt stress inhibits plant growth (Sam, 2007; Martínez-Villavicencio, López, Pérez and Basurto, 2011; Zhao et al., 2020).
Under saline stress, seedlings from Cayo Coco showed higher morphological and physiological values than those from other origins, the tolerance of salt stress was more evident indicating a better ability to grow with salt stress. The differences in the response to salt stress between sea grape seedlings from different origins are related to the ecological conditions where these tree populations are established (Gilman et al., 2014). The seedlings from Las Coloradas showed greater susceptibility to saline stress, apparently, the presence of mean annual precipitation of 942 mm, a mean annual temperature of 27.0 °C and a pH of 8.91 and an electrical conductivity of 7.62 dS m-1 in the soil solution, or the synergy of these variables, makes the environmental conditions on the southeastern coast of Cuba more favorable for the growth and development of C. uvifera seedlings compared to the eastern and central north coast.
Conclusions
Exposure to increasing levels of salinity, the origin of the seedlings, and the interaction between these two factors had a significant effect on all the morphological and physiological traits controlled. RSR and PIabs are not good markers of salt tolerance in C. uvifera seedlings, since their variation was the least influenced by the salinity level. The fact that more than 90% of the variation of stem and root length, FWAP, DWAP, LWC, and RWC is determined by the salinity level would allow using the behavior of these traits under salt stress as an effective criterion for salinity tolerance.
Availability of Supporting Data
The sets of data used or analyzed during this study are available through the corresponding author upon reasonable request.
Authors’ Contributions
Conceptualization: R.L.S., A.B., and M.B.G. Methodology: R.L.S., A.B., and M.B.G. Validation: M.B.G., and L.P. Formal analysis: M.B.G., B.E.L., R.C.P., G.C.P. and L.P. Investigation: M.B.G. and R.L.S. Data curation: M.B.G., R.L.S. and B.E.L. Writing-original draft preparation: M.B.G. and R.L.S. Writing-review and editing: M.B.G., R.L.S., A.B. and B.E.L. Statistical analysis: M.B.G. Supervision: R.L.S., A.B. and M.B.G. Funding acquisition: R.L.S.