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Kamarul Zaman, M. A., Kua, J. M., Jemuladin@Jamaludin, M. A., Shaharuddin, N. A., Mohd Sobri, M. Z., Abdullah, S. N. A., Amin, A. M., Suraninpong, P., and Azzeme, A. M. (2026). "Differential physiological and biochemical responses in oil palm seedlings exposed to single and combined flooding–salinity stress," BioResources 21(3), 5931–5953.

Abstract

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Differential Physiological and Biochemical Responses in Oil Palm Seedlings Exposed to Single and Combined Flooding–Salinity Stress

Increases in temperature, rainfall, and sea level associated with climate change have intensified flooding and saltwater intrusion, thereby posing a growing threat to oil palm cultivation. To evaluate the effects of these environmental stressors, 12-month-old oil palm seedlings were subjected to control, flooding, salinity, and combined flooding and salinity treatments. Physiological and biochemical parameters were measured, including total chlorophyll, antioxidant enzyme activities, lipid peroxidation, and proline content. Phytochemical profiles, such as total phenolics, flavonoids, alkaloids, terpenoids, and antioxidant activity, were also assessed. Combined stress caused the most severe reductions in chlorophyll and phytochemicals, with increased lipid peroxidation and visible symptoms such as leaf yellowing and adventitious root formation. Proline accumulation was markedly higher under combined stress, suggesting a protective role. In contrast, individual stress treatments induced antioxidant enzyme activity, contributing to reactive oxygen species mitigation. These findings highlight the distinct and synergistic impacts of flooding and salinity on oil palm seedling health. The results offer a foundation for identifying stress-resilient traits, which can support future breeding or management strategies to sustain oil palm productivity under changing climate conditions.


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Differential Physiological and Biochemical Responses in Oil Palm Seedlings Exposed to Single and Combined Flooding–Salinity Stress

Munirah Adibah Kamarul Zaman  ,a Kua Jay Mie  ,b Muhammad Amirul Jemuladin@Jamaludin  ,a Noor Azmi Shaharuddin  ,a Mohamad Zulfazli Mohd Sobri  ,Siti Nor Akmar Abdullah  ,d Adibah Mohd Amin  ,e Potjamarn Suraninpong  ,f and Azzreena Mohamad Azzeme  ,a,*

Increases in temperature, rainfall, and sea level associated with climate change have intensified flooding and saltwater intrusion, thereby posing a growing threat to oil palm cultivation. To evaluate the effects of these environmental stressors, 12-month-old oil palm seedlings were subjected to control, flooding, salinity, and combined flooding and salinity treatments. Physiological and biochemical parameters were measured, including total chlorophyll, antioxidant enzyme activities, lipid peroxidation, and proline content. Phytochemical profiles, such as total phenolics, flavonoids, alkaloids, terpenoids, and antioxidant activity, were also assessed. Combined stress caused the most severe reductions in chlorophyll and phytochemicals, with increased lipid peroxidation and visible symptoms such as leaf yellowing and adventitious root formation. Proline accumulation was markedly higher under combined stress, suggesting a protective role. In contrast, individual stress treatments induced antioxidant enzyme activity, contributing to reactive oxygen species mitigation. These findings highlight the distinct and synergistic impacts of flooding and salinity on oil palm seedling health. The results offer a foundation for identifying stress-resilient traits, which can support future breeding or management strategies to sustain oil palm productivity under changing climate conditions.

DOI: 10.15376/biores.21.3.5931-5953

Keywords: Oil palm; Physiological and biochemical responses; Combined stresses; Single stress; Flooding; Salinity

Contact information: a: Department of Biochemistry, Faculty of Biotechnology and Biomolecular Sciences, Universiti Putra Malaysia, 43400 UPM Serdang, Selangor, Malaysia; b: Department of Botany, Faculty of Science, The University of British Columbia, Vancouver, British Columbia V6T 1Z4, Canada; c: Department of Bioprocess Technology, Faculty of Biotechnology and Biomolecular Sciences, Universiti Putra Malaysia, 43400 UPM Serdang, Selangor, Malaysia; d: Institute of Plantation Studies, Universiti Putra Malaysia, 43400 UPM Serdang, Selangor, Malaysia; e: Department of Land Management, Faculty of Agriculture, Universiti Putra Malaysia, 43400 UPM, Serdang, Selangor, Malaysia; f: School of Agricultural Technology and Food Industry, Walailak University, Nakhon Si Thammarat 80161, Thailand; * Corresponding author: azzreena@upm.edu.my

Graphical Abstract

Graphic Summary:
Differential Physiological and Biochemical Responses in Oil Palm Seedlings Exposed to Single and Combined Flooding–Salinity Stress

INTRODUCTION

Oil palm plays a crucial role in ensuring food security. Global demand is rising due to its widespread use in the food industry and household cooking. Among oilseed crops, palm oil stands out for its high oil yield per unit area. According to Voora et al. (2023), palm oil is one of the leading sources of edible oils worldwide. The United States Department of Agriculture (USDA) reported that global palm oil consumption increased from 71 million metric tons in 2021/2022 to approximately 76 million metric tons in 2022/2023. In Malaysia, oil palm cultivation contributes significantly to the agricultural gross domestic product (GDP), accounting for RM 48.31 billion, or 56.8% of the total agricultural GDP in 2020. In the first quarter of 2022 alone, the sector contributed RM 9.5 billion, representing 51.8% of the agrocommodity sector (Siti-Dina et al. 2023). As of the third quarter of 2023, the total planted area reached 5.65 million hectares, contributing 2.85% to Malaysia’s national GDP (Ministry of Plantation and Commodities). The success of the Malaysian oil palm industry has been attributed to coordinated efforts among the government, industry stakeholders, and relevant agencies (Mohd Hanafiah et al. 2022).

However, climate change poses a significant threat to oil palm productivity. Fluctuations in global temperature and rainfall patterns are likely to disrupt oil palm production (Abdullah et al. 2017). Projected economic losses by 2099 are estimated to reach RM 341.29, RM 127.43, and RM 51.80 per hectare for Peninsular Malaysia, Sabah, and Sarawak, respectively (Abubakar and Ishak 2022). Malaysia’s equatorial climate, characterized by consistently high temperatures and rainfall, generally favors oil palm cultivation. However, climate-induced flooding events have become increasingly frequent, affecting both coastal and inland areas. Expansion of oil palm cultivation into coastal regions has contributed to mangrove deforestation, which further intensifies seawater intrusion (Bhowmik et al. 2022). Prolonged flooding under such conditions can expose oil palm to the combined stresses of waterlogging and salinity, severely hindering growth and reducing yield.

Combined salinity and flooding stress has been considered as a way to simulate conditions arising from typhoon- or monsoon-associated storm surges and seawater intrusion, in which saline water inundates plantations, leading to simultaneous root-zone hypoxia and ionic/osmotic stress. Such events have been reported in coastal oil palm-growing regions and are expected to increase with sea-level rise and climate change (Panggabean et al. 2025). In contrast, flooding without salinity represents inland or poorly drained plantations subjected to prolonged or intense monsoonal rainfall, river overflow, or high water tables (Asalam et al. 2023). By distinguishing among salinity, flooding and combined salinity–flooding treatments, this distinction enhances the ecological relevance of the experimental design and supports interpretation of oil palm stress regulation under field conditions.

Salinity stress adversely affects plant development by disrupting osmotic and ionic balance. It impedes water uptake by roots, leading to stomatal closure and inhibition of leaf expansion (Azzeme and Abdullah 2019; Ji et al. 2022). Ion toxicity resulting from salt accumulation further restricts nutrient absorption and induces oxidative damage. Excess sodium (Na⁺) interferes with the uptake and transport of essential ions, particularly potassium (K⁺), leading to impaired growth (Alharbi et al. 2022). Physiological symptoms, such as wilting, leaf senescence, and chlorophyll degradation are commonly observed. Similar physiological responses are also triggered by drought stress, which induces comparable metabolic and developmental changes (Azzeme et al. 2016, 2017; Suraninpong et al. 2023). Salt stress also leads to oxidative stress, disrupting metabolic activity and compromising membrane integrity (Alharbi et al. 2022).

In contrast, flooding induces hypoxia by restricting oxygen availability to the root system, thereby impairing overall plant growth and development. Flooding often results in reduced roots and shoots elongation, enhanced aerenchyma formation, and altered leaf morphology (Mozo et al. 2021). The shift towards anaerobic respiration under flooded conditions promotes the generation of reactive oxygen species (ROS) and inhibits photosynthesis by reducing stomatal conductance and carbon dioxide (CO₂) diffusion (Aslam et al. 2023; Jensen et al. 2024). Therefore, when flooding and salinity occur simultaneously, the stress effects intensify due to elevated accumulation Na⁺ and chloride (Cl⁻) disrupts nutrient uptake and exacerbates inhibition of K⁺ transport (Duan et al. 2018; Renziehausen et al. 2024).

The excessive accumulation of ROS under abiotic stress leads to lipid peroxidation, membrane damage, enzyme inhibition, and DNA disruption (Park and Lee 2019). Consequently, photosynthesis efficiency and plant growth decline, ultimately reducing crop productivity (Godoy et al. 2021). To counteract oxidative stress, plants activate antioxidant defense systems, including enzymatic antioxidants and the synthesis of protective compounds such as proline (Hasanuzzaman et al. 2020; Nadarajah 2020).

Proline is a key osmolyte that plays a vital role under numerous stress conditions. As an amino acid, proline functions in osmotic adjustment, stabilization of membrane and protein structure, as well as scavenging of free radicals (El-Beltagi et al. 2020). Stress-signaling molecules, particularly ABA, have been shown to stimulate the expression of the pyrroline-5-carboxylate synthase (P5CS) gene, thereby enhancing proline biosynthesis under salinity stress (Singh et al. 2022). Conversely, increased expression of proline dehydrogenase (PRODH) promotes proline catabolism in mitochondria, supporting respiration and energy production, hence contributing to plant growth maintenance under low water potential conditions (Launay et al. 2019). Therefore, proline accumulation is critical for mitigating ROS-induced damage under salinity and drought stresses. Proline is transported and accumulated in the cytoplasm, where it lowers osmotic potential, enhances water uptake, and maintains cellular osmotic balance (Yang et al. 2021). In addition, proline enhances antioxidant capacity by supporting the activities of key antioxidant enzymes, including peroxidase (POD), catalase (CAT), superoxide dismutase (SOD), polyphenol oxidase (PPO), and other ROS-scavenging enzymes (Yang et al. 2021). This enhancement may be explained by the ability of proline to stabilize protein structures and maintain cellular redox balance under stress conditions. By preserving enzyme conformation and preventing oxidative damage to proteins, proline helps sustain antioxidant enzyme functionality during salinity and flooding stress. Supporting this observation, Rho et al. (2025) reported that proline accumulation increased significantly under flooding stress across five Capsicum species during both summer and winter seasons.

While salinity and flooding often co-occur in coastal ecosystems, evaluating their impacts independently remains a significant experimental challenge. To address this issue, the present study employed a controlled hydroponic approach using a standardized Hoagland nutrient solution (Hoagland and Arnon 1950). This methodology allows precise decoupling of stressors by maintaining a constant and optimal nutrient baseline while independently manipulating NaCl concentration. Such an experimental framework ensures that the individual and combined effects of salinity and flooding can be monitored accurately. Similar approaches using Hoagland nutrient solution have been reported in studies on barley (Zeng et al. 2013), ryegrass (Yin et al. 2017), and ryegrass and alkaligrass (Isweiri et al. 2022).

In this study, it was hypothesized that combined flooding and salinity stresses would exert more detrimental effects on oil palm than single flooding or salinity stress. This hypothesis was based on the expectation that the synergistic interaction of flooding and salinity would impair plant health and development, which could be observed morphologically and physiologically. In particular, combined stress was anticipated to induce greater oxidative stress, thereby increasing reliance on osmoprotectants such as proline and antioxidant defense systems. To evaluate these responses, biochemical and antioxidant analyses were conducted to assess the effects of individual and combined stress treatments. Therefore, this study aimed to investigate the physiological and biochemical responses of oil palm seedlings to flooding and salinity, with particular emphasis on the differential responses of leaves and roots. The findings provide insights into key stress-responsive mechanisms and potential genetic targets for developing stress-resilient oil palm varieties.

EXPERIMENTAL

Plant Materials

Twelve-month-old Calix-600 oil palm seedlings were obtained from SD Guthrie Seeds and Agricultural Services, Banting, Selangor, Malaysia. The seedlings were subsequently acclimatized in the greenhouse at the Institute of Plantation Studies, Universiti Putra Malaysia, Selangor. Both the acclimatization process and the application of abiotic stress treatments were conducted under ambient temperature conditions.

Salinity, Flooding, and Combined Stress Treatments

Four different treatments were applied to the 12-month-old seedlings: control, salinity, flooding, and combined flooding and salinity. The control group was maintained under normal conditions in Hoagland solution without the addition of sodium chloride (NaCl) or submergence. For the salinity treatment, seedlings were irrigated with Hoagland solution supplemented with NaCl. The salt concentration was gradually increased (50, 100, 150, 250, and 300 mM) every other day to avoid osmotic shock (Akbudak and Filiz 2018). Flooding stress was induced by submerging the seedlings in Hoagland solution (without added NaCl) until the aerial parts were fully covered (Chen et al. 2016). In the combined treatment, seedlings were submerged in Hoagland solution containing NaCl, with the salt concentration increased gradually as in the salinity treatment. All seedlings were maintained under their respective treatments for 12 days before being harvested for further analysis. Hoagland solution was used throughout the experiment to prevent nutrient deficiency in the seedlings.

Estimation of Chlorophyll Content

Chlorophyll content in control and treated oil palm leaves was determined following the method described by Azzeme et al. (2016). Approximately 0.5 g of leaf sample was extracted using 10 mL of 80% (v/v) acetone, and 0.5 mg of calcium carbonate (CaCO₃) was added to the mixture. The extract was then filtered using Whatman No. 1 filter paper. Excess sample residue was washed with acetone until it became colourless. All filtrates were combined, and the final volume was adjusted to 20 mL. Absorbance readings were taken at 645 nm (maximum absorption for chlorophyll b in acetone) and 663 nm (maximum absorption for chlorophyll a in acetone). The contents of chlorophyll a (Chla), chlorophyll b (Chlb), and total chlorophyll (TC) were calculated using Eqs. 1, 2, 3,

where A645 and A663 are the absorbances at 645 and 663 nm, V is the volume in mL, 𝛼 is the length of the light path in the cell (1 cm), and W is the fresh weight in g.

Estimation of Proline Content

Proline content was determined according to the method described by Bates et al. (1973). Approximately 0.5 g of leaf and root samples were extracted with 10 mL of 3% (w/v) sulfosalicylic acid. The homogenate was centrifuged at 11,200 × g for 30 min. A 2 mL aliquot of the clear supernatant was collected and reacted with 2 mL of ninhydrin solution and 2 mL of glacial acetic acid. The mixture was incubated at 100 °C for 1 h, after which the reaction was terminated by placing the tubes on ice for 5 min. Subsequently, 4 mL of toluene was added and mixed vigorously. The chromophore-containing toluene phase was separated from the aqueous phase and allowed to equilibrate at room temperature. Absorbance was measured at 520 nm using toluene as the blank. Proline concentration was determined from a standard curve and expressed on a fresh weight (FW) basis using Eq. 4:

Estimation of Catalase (CAT), Guaiacol Peroxidase (POD), and Ascorbate Peroxidase (APX) Assay

The activities of catalase (CAT; EC 1.11.1.6), peroxidase (POD; EC 1.11.1.7), and ascorbate peroxidase (APX; EC 1.11.1.11) were determined following the method described by Azzeme et al. (2016). For CAT analysis, crude protein was extracted in 50 mM potassium phosphate buffer (pH 7.5) containing 5 mM dithiothreitol (DTT) at 4 °C. The homogenate was centrifuged at 11,200 × g for 15 min at 4°C, and the supernatant was collected and centrifuged again under the same conditions. The assay mixture contained 50 μL of crude extract, 20 mM hydrogen peroxide (H₂O₂, 30%), and 52 mM potassium phosphate buffer (pH 7.5). The CAT activity was defined as the amount of enzyme catalyzing the decomposition of 1 μmol of H₂O₂ per minute for each mg of protein (μmolmin-1mg-1), with absorbance measured at 240 nm over 3 min.

For POD analysis, 0.5 g of frozen leaves and roots were homogenized separately in liquid nitrogen. The powdered samples were mixed with extraction buffer (0.1 M potassium phosphate buffer, pH 6.5, containing 0.5 M sodium chloride and 2% [w/v] polyvinylpyrrolidone, PVP) at 4 °C. The homogenate was gently mixed and centrifuged at 11,200 × g for 15 min at 4 °C, and the supernatant was collected and centrifuged again under the same conditions. A 50 μL aliquot of crude extract was added to 3 mL of substrate solution containing 0.1 M potassium phosphate buffer (pH 6.0), 15 mM guaiacol, and 7.5 mM H₂O₂ (30%). One unit of POD activity was defined as the amount of enzyme catalyzing the oxidation of 1 μmol of guaiacol per minute and for each mg of protein (μmolmin-1mg-1), measured at 470 nm over 3 min.

For APX analysis, 0.5 g of leaves or roots was ground in liquid nitrogen. The chilled powder was homogenized in 50 mM phosphate buffer (pH 7.8) containing 5 mM ascorbate, 2% PVP, 1 mM phenylmethylsulfonyl fluoride (PMSF), 10 mM DTT, and 0.1 mM ethylenediaminetetraacetic acid (EDTA). The homogenate was centrifuged at 11,200 × g for 15 min at 4 °C, and the supernatant was re-centrifuged under the same conditions. The APX activity was measured in a 3 mL reaction mixture containing 50 mM potassium phosphate buffer (pH 7.0), 50 μL crude extract, 0.1 mM H₂O₂, and 0.5 mM ascorbate. One unit of APX activity was defined as the amount of enzyme oxidizing 1 μmol of ascorbate per minute per mg of protein (μmolmin-1mg-1), with absorbance recorded at 290 nm for 3 min.

Estimation of Lipid Peroxidation Activity

Lipid peroxidation in control and treated oil palm leaves and roots was assessed by measuring malondialdehyde (MDA) content using the thiobarbituric acid (TBA) method, as described by Heath and Packer (1968). Approximately 250 mg of fresh tissue was homogenized in 5 mL of 0.1% trichloroacetic acid (TCA) and centrifuged at 10,000 × g for 5 min at 4 °C. Subsequently, 1 mL of the supernatant was mixed with 4 mL of 20% TCA containing 0.5% TBA and incubated at 95 °C for 30 min. The reaction mixture was rapidly cooled in crushed ice and centrifuged again at 10,000 × g for 10 min at 4 °C. Absorbance was measured at 532 nm and 600 nm using a spectrophotometer. The MDA concentration was calculated using a standard calibration curve and expressed as mmol MDA per gram fresh weight (mmolMDAg-1FW).

Preparation of Crude Extract for Phytochemical Analysis

Control and treated oil palm leaves and roots were extracted following the method described by Kamarul Zaman et al. (2020a). Approximately 1 g of leaf and root tissue was ground into a fine powder and extracted with 100 mL of methanol. The mixture was kept at room temperature under continuous shaking at 150 rpm for 24 h. After incubation, the extract was filtered using Whatman No. 1 filter paper. The resulting supernatant was collected and stored at 4 °C for subsequent phytochemical analysis.

Estimation of Total Phenolic Content

The total phenolic content (TPC) of oil palm leaves and roots was determined using the Folin–Ciocalteu method. Methanolic extracts prepared as described earlier were used. Approximately 1 mL of each extract was transferred into a test tube, followed by the addition of 0.5 mL of 10-fold diluted Folin–Ciocalteu reagent and 7 mL of distilled water. The mixture was incubated for 5 min, after which 1.5 mL of 7.5% (w/v) sodium carbonate (Na₂CO₃) was added and mixed thoroughly. The reaction mixture was then incubated in the dark for 2 h. Absorbance was measured at 765 nm using a spectrophotometer. TPC was expressed as milligrams of gallic acid equivalents per gram of fresh weight (mgGAEg-1 FW) (Kamarul Zaman et al. 2020b).

Estimation of Total Flavonoid Content

The total flavonoid content (TFC) of oil palm leaves and roots was determined using the aluminum chloride colorimetric assay, as described by Kamarul Zaman et al. (2020b). A total of 1 mL of each methanolic extract (prepared as described earlier) was added to a reaction mixture containing 4 mL of distilled water. Then, 0.3 mL of 5% (w/v) sodium nitrite (NaNO₂) was added, and the mixture was allowed to react for 5 min. Subsequently, 0.3 mL of 10% (w/v) aluminum chloride (AlCl₃) and 2 mL of 1 M sodium hydroxide (NaOH) were added. The final volume was adjusted to 10 mL with distilled water. Absorbance was measured at 510 nm using a spectrophotometer. The TFC was expressed as milligrams of quercetin equivalents per gram of fresh weight (mgQEg-1 FW).

Estimation of Total Terpenoid Content

The total terpenoid content (TTC) of oil palm leaves and roots was determined using a sulfuric acid colorimetric assay. A total of 3 mL of chloroform were added to 1 mL of each methanolic extract. The mixture was vortexed and left to stand for 3 min. Then, 200 μL of concentrated sulfuric acid (H₂SO₄) was added, and the reaction mixture was incubated at room temperature for 1.5 h in the dark until a reddish-brown precipitate formed. The supernatant was carefully decanted without disturbing the precipitate. Subsequently, 3 mL of 95% (v/v) methanol was added and vortexed thoroughly until the precipitate was completely dissolved. Absorbance was measured at 538 nm using a spectrophotometer. The TTC was expressed as milligrams of linalool equivalents per gram of fresh weight (mgLEg-1 FW) (Kamarul Zaman et al. 2020b).

Estimation of Total Alkaloid Content

The total alkaloid content (TAC) of oil palm leaves and roots was determined using Dragendorff’s precipitation method, as described by Mishra et al. (2018). Methanolic extracts were transferred into test tubes, and the pH was adjusted to 2.3 using a few drops of 1 M hydrochloric acid (HCl). Subsequently, 400 μL of Dragendorff’s reagent (DR) was added to 1 mL of extract. The mixture was centrifuged at 1,844 × g for 10 min at 24 °C. To confirm complete precipitation, another 400 μL of DR was added to the supernatant. After centrifugation, the supernatant was discarded, and the resulting precipitate was washed twice with 1 mL of methanol. The aqueous phase was removed, and the residue was treated with 400 μL of 1% (w/v) disodium sulfide solution (Na₂S). The brownish-black precipitate was then centrifuged again at 1,844 × g for 10 min at 24 °C. Two drops of 1% (w/v) Na₂S solution were added to confirm the completion of the reaction, indicated by the formation of an intense brownish-black precipitate, followed by re-centrifugation. The final supernatant was discarded, and the pellet was dissolved in 400 μL of concentrated nitric acid (HNO₃) by gentle warming at 25 °C. The resulting solution was then diluted with 1.6 mL of autoclaved distilled water. A total of 1 mL of this solution was further reacted with 5 mL of 3% (w/v) thiourea solution. Absorbance was measured at 430 nm against a blank containing concentrated HNO₃ and 3% (w/v) thiourea. Alkaloid content was expressed as mg per gram of fresh weight (mgg-1 FW) and calculated using Eq. 5:

Estimation of Antioxidant Activity

Antioxidant activity was determined using the 2,2-diphenyl-1-picryl-hydrazyl (DPPH) free radical scavenging assay, as described by Kamarul Zaman et al. (2020b). The initial absorbance of the DPPH solution (without sample) was measured at 517 nm. Approximately 0.2 mL of each sample extract was mixed with 3 mL of 0.1 mM DPPH solution. The mixture was incubated at room temperature in the dark for 30 min. After incubation, the absorbance was measured again at 517 nm. The antioxidant activity was calculated and expressed as the percentage of DPPH free radical scavenging activity using the following Eq. 6,

where A control is the absorbance of DPPH solution without sample and A sample is the absorbance of sample with DPPH solution.

Statistical Analysis

Abiotic stress treatments were arranged in a completely randomized design (CRD), with seven replicates per treatment. For biochemical analysis, three individual plants were randomly selected from each treatment. Data for all measured parameters were subjected to one-way analysis of variance (ANOVA), and differences between means were determined using Tukey’s multiple range test at p ≤ 0.05. Statistical analyses were performed using SAS 9.4 software (Cary, NC, USA). Results are presented as means ± standard error (SE) from triplicate determinations. Different letters indicate statistically significant differences among treatments.

RESULTS AND DISCUSSION

Morphological Changes of Oil Palm Seedlings

Oil palm seedlings exhibited distinct morphological responses to individual and combined stresses of flooding and salinity, revealing key aspects of their resilience mechanisms. Control seedlings displayed healthy, verdant foliage (Fig. 1A), whereas those exposed to salinity, flooding, and combined stresses showed evident yellowing symptoms (Fig. 1B, 1C, and 1D), with the most pronounced effects observed under salinity and combined stress conditions. In terms of root response, flooding treatment (Fig. 2C) notably induced the development of numerous adventitious roots with aerenchyma formation, a feature not observed in seedlings from other treatments (Fig. 2A, 2B, and 2D).

Morphological changes in oil palm seedlings under (A) control, (B) salinity, (C) flooding, and (D) combined flooding and salinity treatments after twelve days of exposure

Fig. 1. Morphological changes in oil palm seedlings under (A) control, (B) salinity, (C) flooding, and (D) combined flooding and salinity treatments after twelve days of exposure

Under salinity and combined stresses, notable leaf yellowing indicated the severe impact of high sodium (Na⁺) and chloride (Cl⁻) accumulation in oil palm leaves. This striking foliage transformation may result from the deleterious effects of Na⁺ and Cl⁻ ions, which trigger the degradation of vital pigments, particularly chlorophyll, and other essential chloroplast components under abiotic stress. Alharbi et al. (2022) reported that Na⁺ and Cl⁻ accumulation impairs chlorophyll biosynthesis and disrupts the photosynthetic machinery by inhibiting pigment-producing enzymes, thereby reducing carotenoid and chlorophyll synthesis and leading to chlorosis. Additionally, salt stress may damage cell wall structure, exacerbate dehydration, and impede overall plant growth and development. Ma et al. (2020) and Raju et al. (2020) highlighted that salinity-induced dehydration and ionic toxicity promote leaf senescence and reduce photosynthetic activity.

Morphological changes of oil palm roots under (A) control, (B) salinity, (C) flooding, and (D) combined flooding and salinity stress treatments after twelve days of exposure

Fig. 2. Morphological changes of oil palm roots under (A) control, (B) salinity, (C) flooding, and (D) combined flooding and salinity stress treatments after twelve days of exposure

Maintaining the negative charge of cell walls is crucial for calcium (Ca²⁺) binding and pectin cross-linking, which reinforce cell wall integrity. However, excess Na⁺ may displace Ca²⁺, thereby hindering pectin cross-linking and reducing cell elongation (Dabravolski and Isayenkov 2023). The synergy of flooding and salinity may intensify leaf yellowing, potentially due to reduced oxygen (O₂) availability, which promotes toxic Na⁺ accumulation in leaves. Oxygen deficiency may impair energy-dependent Na⁺ exclusion from the xylem, mediated by high-affinity potassium transporters (HKT) and salt overly sensitive (SOS) transporters, thereby increasing Na⁺ levels in mesophyll cells and suppressing photosynthesis (Renziehausen et al. 2024).

Roots, being the primary sensors of soil moisture changes, perceive flooding-induced limitations in gas diffusion, leading to elevated ethylene levels and O₂ depletion (Verslues et al. 2023). Aerenchyma formation facilitates gas exchange between roots and shoots during submergence, while adventitious roots replace damaged primary roots under O₂ deficiency, ensuring continued oxygen uptake and transport (Aslam et al. 2023). Studies by Nuanlaong et al. (2021) and Rivera-Mendes et al. (2016) reported the development of aerenchyma and pneumatophores in oil palm seedlings under waterlogging stress, demonstrating adaptive strategies to cope with flooding.

In contrast, salinity and combined stress treatments (Fig. 2B and 2D) failed to induce adventitious root formation, potentially due to disrupted Na⁺ and Cl⁻ dynamics that impede root development. Salinity-induced reductions in plant cell water potentially result in dehydration, further aggravated by excess NaCl, which restricts water availability and induces physiological drought (Hannachi et al. 2022).

Under combined flooding and salinity stress, low water potential, oxygen deficiency, and ionic toxicity likely compound root growth inhibition. Oxygen deprivation disrupts O₂-dependent ion transporters responsible for Na⁺ exclusion and ion homeostasis. Tahjib-Ul-Arif et al. (2023) reported that salinity-induced membrane depolarization, coupled with root O₂ deficiency, diminishes ATP production and impairs SOS1 Na⁺/H⁺ antiporter activity, leading to reduced Na⁺ exclusion and K⁺ retention. As a result, an unfavorable Na⁺/K⁺ ratio impairs plant metabolism and hinders both root and shoot development. In a study by Chakraborty et al. (2021), aerenchyma formation in the rice variety Varshadhan was inhibited under saline flooding due to suppression of reactive oxygen species (ROS) signaling by metallothioneins.

Estimation of Chlorophyll Content

A reduction in chlorophyll a (Chla), chlorophyll b (Chlb), and total chlorophyll (TC) was observed in treated oil palm leaves compared to the control (Table 1). The combined stress treatment had the most severe effect, with Chla, Chlb, and TC levels reduced 5.92-, 5.88-, and 5.93-fold, respectively, relative to the control. However, no significant differences were observed between the effects of single and combined stresses on Chla, Chlb, and TC, indicating that salinity, flooding, and their combination elicited comparable impacts on chlorophyll content. Among all treatments, the combined stress resulted in the lowest levels of Chla, Chlb, and TC. These reductions are consistent with the yellowing symptoms observed in oil palm leaves under combined stress, as illustrated in Fig. 1D.

Table 1. The Chla, Chlb, and TC Contents in Leaf Tissues of Oil Palm Seedlings Subjected to Control, Flooding, Salinity, and Combined Flooding and Salinity Stress Treatments

The effects of combined salinity and flooding stress on oil palm seedlings reveal intricate physiological and biochemical responses, particularly related to oxidative stress and antioxidant defense mechanisms. Unlike individual stresses, combined stress conditions often lead to more complex interactions that can either intensify damage or trigger distinct adaptive responses. A prominent negative effect observed under combined stress was the reduction in chlorophyll content in oil palm leaves. Similar reductions in chlorophyll under combined stress conditions have also been reported in maize, alfalfa, and barley (Zeng et al. 2013; Sghaier et al. 2020; Mahmood et al. 2021).

This chlorophyll decline is likely associated with ion imbalance, particularly the disruption of sodium (Na⁺) and potassium (K⁺) uptake. Under combined stresses, low oxygen levels caused by flooding impair root respiration and reduce the efficiency of selective ion transporters, leading to excessive Na⁺ accumulation (Tahjib-Ul-Arif et al. 2023). This ion toxicity is further exacerbated by competition between Na⁺ and K⁺ for uptake, resulting in K⁺ deficiency. Potassium plays a critical role in stomatal regulation, enzyme activation, and photosynthetic function; therefore, its deficiency compromises the structural and functional integrity of the chloroplasts.

The destabilization of chloroplast membranes and disruption of pigment–protein complexes (Renziehausen et al. 2024) contribute to accelerated chlorophyll degradation. This process is not only driven by Na⁺ toxicity but also by the induction of chlorophyll-degrading enzymes such as chlorophyllase. Activation of chlorophyllase under stress conditions (Guyer et al. 2018; Wang et al. 2018), along with thylakoid shrinkage within chloroplasts, likely contributes to visible chlorosis, leaf necrosis, and impaired plant development (Mohsin et al. 2020; Hannachi et al. 2022). The plant’s inability to maintain cellular homeostasis under combined salinity and flooding stress ultimately accelerates chlorophyll loss, reducing photosynthetic efficiency and overall growth.

Estimation of Catalase, Guaiacol Peroxidase, and Ascorbate Peroxidase

The present study revealed that the antioxidant enzymes catalase (CAT), peroxidase (POD), and ascorbate peroxidase (APX) exhibited tissue-specific responses to the imposed stress treatments (Fig. 3). In roots, combined salinity and flooding stress had a markedly negative impact on antioxidant enzyme activities. No CAT (Fig. 3A) or APX (Fig. 3C) activity was detected, while POD activity (Fig. 3B) was significantly reduced by 3.90-fold compared to the control. In contrast, oil palm leaves demonstrated an increase in CAT and POD activities under combined stress, with 5.09-fold and 1.15-fold increases, respectively, compared to the control. However, APX activity in leaves decreased 1.85-fold. When compared to the effects of individual salinity or flooding stress, the combined stress treatment resulted in the lowest CAT, POD, and APX activities in roots, indicating a compounded inhibitory effect. In leaves, only POD and APX showed increased activity under combined stress, suggesting a partial compensatory antioxidant response. These findings indicate that combined salinity and flooding stress exerts a strong negative influence on the antioxidant defense system of oil palm seedlings, particularly in the roots, where enzymatic activity was largely suppressed.

Effect of single and combined flooding and salinity stresses on the activities of antioxidant enzymes: (a) catalase (CAT), (b) guaiacol peroxidase (POD), and (c) ascorbate peroxidase (APX). Data are presented as mean ± standard error (SE) of three replicates. Different letters indicate statistically significant differences at p ≤ 0.05 according to Tukey’s multiple range test.

Fig. 3. Effect of single and combined flooding and salinity stresses on the activities of antioxidant enzymes: (a) catalase (CAT), (b) guaiacol peroxidase (POD), and (c) ascorbate peroxidase (APX). Data are presented as mean ± standard error (SE) of three replicates. Different letters indicate statistically significant differences at p ≤ 0.05 according to Tukey’s multiple range test.

Combined salinity and flooding stresses also trigger oxidative stress, primarily due to the overproduction of reactive oxygen species (ROS) such as hydrogen peroxide (H₂O₂), superoxide (O₂⁻), and hydroxyl radicals (OH⁻). These ROS can damage cellular structures, including membranes, proteins, and nucleic acids, and their accumulation is exacerbated under dual stress conditions due to Na⁺ toxicity and low oxygen availability.

In this study, antioxidant enzyme activities showed distinct tissue-specific patterns in response to combined stresses. While catalase (CAT) and guaiacol peroxidase (POD) activities were slightly elevated in leaves, their activities were markedly reduced in roots. The increased CAT and POD activities in leaves suggest that oil palm seedlings retain some capacity to mitigate oxidative damage in aerial tissues. These enzymes function synergistically to decompose H₂O₂, a major by-product of ROS accumulation, thereby playing a protective role in photosynthetically active tissues (Xiong et al. 2020).

In contrast, the decline in antioxidant enzyme activity in roots indicates severe physiological impairment under combined stress. This may be attributed to the dysfunction of key ion transporters, such as salt overly sensitive (SOS) and high-affinity potassium transporter (HKT), which are energy-dependent and adversely affected by low oxygen levels. Impaired transporter function reduces the exclusion of Na⁺ from root cells, leading to its toxic accumulation. Excessive Na⁺ and Cl⁻ disrupt root enzymatic function, destabilize antioxidant proteins, and reduce the plant’s ability to detoxify ROS. As suggested by López-Cristoffanini et al. (2020), excessive ionic accumulation can overwhelm enzymatic defense systems, resulting in reduced scavenging capacity and heightened oxidative damage.

Estimation of Proline Content

A notable aspect of the response to combined salinity and flooding stresses in oil palm seedlings is the accumulation of proline, a key osmoprotectant and antioxidant molecule. In this study, proline content increased significantly in both leaves and roots under combined stress compared to the control and single stress treatments (Fig. 4). In leaves, proline levels increased 1.74-fold, 1.80-fold, and 2.35-fold relative to the control, salinity, and flooding treatments, respectively. Similarly, in roots, proline content increased 1.46-fold, 1.35-fold, and 1.40-fold compared to the control, salinity, and flooding treatments, respectively.

Interestingly, flooding alone led to a significant reduction in proline content in leaves, with a 1.35-fold decrease compared to the control. In contrast, salinity caused a slight but non-significant increase in proline levels in both leaves and roots, while flooding slightly elevated proline in roots only. However, the changes in proline content under single salinity and flooding stresses were not statistically significant when compared to the control.

Proline serves as a critical component in maintaining cellular homeostasis and mitigating damage caused by reactive oxygen species (ROS). The elevated proline content observed in oil palm seedlings under combined stress conditions suggests that proline plays a compensatory role when enzymatic antioxidant activity is insufficient. As noted by Badrulzaman et al. (2021), proline may also function as a non-enzymatic antioxidant, protecting cells from oxidative injury associated with excessive ROS accumulation. This supports the hypothesis that non-enzymatic antioxidants, such as proline, become especially important under complex environmental conditions, such as the concurrent occurrence of salinity and flooding.

This finding is consistent with the work of Sghaier et al. (2020) and Urmi et al. (2023), who reported that proline biosynthesis is a direct response to disrupted cellular homeostasis, aiding in the maintenance of turgor pressure and ROS detoxification. Notably, the current study revealed a reduction in proline content under individual stress treatments (salinity or flooding alone), which coincided with higher enzymatic antioxidant activities, such as those of catalase (CAT) and peroxidase (POD). This suggests a potential inverse relationship between proline accumulation and enzymatic antioxidant activity under single-stress conditions.

The decrease in proline under salinity or flooding alone may be attributed to the plant’s capacity to manage oxidative stress primarily through its enzymatic defense systems, reducing the need for non-enzymatic antioxidants. However, under combined stresses, the simultaneous presence of multiple stressors may overwhelm the enzymatic antioxidant system, thereby necessitating greater proline accumulation to compensate for reduced enzymatic efficacy.

Proline content in the leaves and roots of oil palm seedlings subjected to single and combined flooding and salinity stress treatments. Data are presented as mean ± SE of three replicates. Different letters indicate statistically significant differences at p ≤ 0.05 according to Tukey’s multiple range test.

Fig. 4. Proline content in the leaves and roots of oil palm seedlings subjected to single and combined flooding and salinity stress treatments. Data are presented as mean ± SE of three replicates. Different letters indicate statistically significant differences at p ≤ 0.05 according to Tukey’s multiple range test.

Estimation of Lipid Peroxidation Activity

This study also provides insight into lipid peroxidation activity, assessed through malondialdehyde (MDA) content, a widely recognized indicator of oxidative damage to cellular membranes. The MDA levels were significantly elevated under both single and combined stress treatments compared to the control (Fig. 5). Under combined salinity and flooding stress, oil palm leaves and roots exhibited markedly higher MDA contents, with 2.51-fold and 1.38-fold increases, respectively, relative to the control. Similarly, exposure to either salinity or flooding alone also resulted in significant increases in MDA content in both tissues compared to the control.

MDA content in the leaves and roots of oil palm seedlings subjected to control, flooding, salinity, and combined flooding and salinity stress treatments. Data are presented as mean ± SE of three replicates. Different letters indicate statistically significant differences at p ≤ 0.05 according to Tukey’s multiple range test.

Fig. 5. MDA content in the leaves and roots of oil palm seedlings subjected to control, flooding, salinity, and combined flooding and salinity stress treatments. Data are presented as mean ± SE of three replicates. Different letters indicate statistically significant differences at p ≤ 0.05 according to Tukey’s multiple range test.

The significant increase in MDA content under combined stress conditions suggests that oil palm seedlings experienced higher levels of oxidative stress compared to single-stress treatments. This observation aligns with the findings of Wang et al. (2019), who reported that combined abiotic stresses can exacerbate oxidative damage due to the excessive accumulation of reactive oxygen species (ROS), leading to increased lipid peroxidation. For example, the combination of salinity and waterlogging disrupts ion homeostasis, particularly through elevated Na⁺ and Cl⁻ accumulation, which contributes to both ionic and osmotic stress and subsequently enhances ROS production.

Additionally, oxygen deprivation under waterlogged conditions may impair the plant’s capacity to maintain ion selectivity, resulting in increased Na⁺ uptake and reduced K⁺ transport to the shoots, further aggravating oxidative stress (Duan et al. 2019). In contrast, a study by Liu et al. (2020) on Elaeagnus angustifolia reported lower MDA levels under combined waterlogging and 0.6% NaCl stress, indicating reduced membrane lipid peroxidation, greater membrane stability, and lower relative membrane conductivity. This discrepancy may be attributed to species-specific stress tolerance mechanisms or differences in stress intensity and duration.

In oil palm seedlings, the elevated MDA levels likely reflect more severe oxidative damage, possibly due to prolonged exposure to both salinity and flooding, or a limited capacity to activate sufficient defense mechanisms against the compounded stress effects.

Estimation of Total Phenolic Content, Total Flavonoid Content, Total Terpenoid Content, and Total Alkaloid Content

Total phenolic content (TPC), total flavonoid content (TFC), total terpenoid content (TTC), and total alkaloid content (TAC) were measured to evaluate the effects of single and combined salinity and flooding stresses on non-enzymatic antioxidant activity in oil palm leaves and roots (Fig. 6). Among the four phytochemical classes, TTC (Fig. 6C) exhibited the highest concentrations overall, compared to TPC (Fig. 6A), TFC (Fig. 6B), and TAC (Fig. 6D).

Plants synthesize secondary metabolites, such as phenolics, flavonoids, terpenoids, and alkaloids, as part of their antioxidant defense mechanisms. These compounds play essential roles in neutralizing reactive oxygen species (ROS) and enabling plants to adapt to environmental stressors (Li et al. 2020). In the present study, combined salinity and flooding stresses elicited variable effects on the production of these secondary metabolites. Among the metabolites evaluated, terpenoids exhibited the highest accumulation under both single and combined stress conditions. Given their known roles in membrane stabilization and antioxidant activity, the elevated levels of terpenoids suggest a potential protective function in enhancing membrane integrity under abiotic stress.

However, the absence of significant differences in terpenoid content across treatments indicates that their accumulation may not be a primary or specific response to the combined stress of flooding and salinity. In contrast, the reduced accumulation of phenolics, flavonoids, and alkaloids under combined stress conditions suggests that oil palm seedlings may not rely extensively on these compounds for ROS scavenging when facing multiple concurrent stressors. This implies a potential shift in the antioxidant defense strategy under combined stresses, where non-enzymatic antioxidants, such as proline or other physiological adaptations, may play a more dominant role.

Effect of single and combined flooding and salinity stresses on (a) total phenolic content (TPC), (b) total flavonoid content (TFC), (c) total terpenoid content (TTC), and (d) total alkaloid content (TAC) in the leaf and root tissues of oil palm seedlings. Data are presented as mean ± SE of three replicates. Different letters indicate statistically significant differences at p ≤ 0.05 according to Tukey’s multiple range test.

Fig. 6. Effect of single and combined flooding and salinity stresses on (a) total phenolic content (TPC), (b) total flavonoid content (TFC), (c) total terpenoid content (TTC), and (d) total alkaloid content (TAC) in the leaf and root tissues of oil palm seedlings. Data are presented as mean ± SE of three replicates. Different letters indicate statistically significant differences at p ≤ 0.05 according to Tukey’s multiple range test.

Estimation of Antioxidant Activity

Antioxidant activity in oil palm leaves and roots was assessed using the DPPH free radical scavenging assay. In roots, DPPH scavenging activity increased under single salinity and flooding treatments by 1.48-fold and 1.19-fold, respectively, compared to the control (Fig. 7). However, under combined salinity and flooding stress, a reduction in DPPH activity was observed in both leaves and roots, by 1.70-fold and 1.13-fold, respectively, relative to the control.

A similar decline was also recorded in leaves under individual stress treatments, with a 1.76-fold decrease under salinity and a 1.28-fold decrease under flooding. Among all treatments, the highest DPPH activity in leaves was recorded in the control group (58.68 ± 1.08%), while in roots, the highest activity was observed under salinity stress (49.96 ± 5.21%).

The antioxidant capacity of oil palm seedlings, as indicated by DPPH scavenging activity, was highest under flooding in leaves and under salinity in roots. This suggests that different tissues may employ distinct defense strategies depending on the type of stress imposed. The elevated antioxidant activity in roots under salinity stress may be attributed to the enhanced production of phenolics, flavonoids, and alkaloids, which are known to scavenge ROS generated during salt stress.

DPPH free radical scavenging activity in the leaf and root tissues of oil palm seedlings subjected to control, flooding, salinity, and combined flooding and salinity stress treatments. Data are presented as mean ± SE of three replicates. Different letters indicate statistically significant differences at p ≤ 0.05 according to Tukey’s multiple range test.

Fig. 7. DPPH free radical scavenging activity in the leaf and root tissues of oil palm seedlings subjected to control, flooding, salinity, and combined flooding and salinity stress treatments. Data are presented as mean ± SE of three replicates. Different letters indicate statistically significant differences at p ≤ 0.05 according to Tukey’s multiple range test.

In contrast, under combined salinity and flooding stress, the lowest antioxidant activity was recorded in both leaves and roots. This decline may reflect either the depletion of antioxidant compounds or the suppression of their biosynthetic pathways, which is likely due to the severe physiological damage induced by the dual stress. Simultaneous exposure to salinity and flooding may also disrupt the plant’s energy balance, thereby limiting its ability to sustain the synthesis of antioxidant metabolites required for effective ROS detoxification.

CONCLUSIONS

  1. Oil palm seedlings exhibited distinct physiological and biochemical responses when subjected to single and combined flooding and salinity stress, confirming that stress interactions produce unique effects not predictable from individual stress responses alone.
  2. Combined stress led to a more pronounced reduction in chlorophyll content and photosynthetic capacity, as reflected by visible leaf chlorosis and significant decreases in chlorophyll ab, and total chlorophyll, compared to single-stress treatments.
  3. Lipid peroxidation, indicated by elevated malondialdehyde (MDA) content, was highest under combined stress, signifying enhanced oxidative damage in both leaves and roots due to the overaccumulation of reactive oxygen species (ROS).
  4. While catalase (CAT) and peroxidase (POD) activities increased in leaves under combined stress, all antioxidant enzyme activities were significantly suppressed in roots, indicating tissue-specific limitations in enzymatic ROS detoxification.
  5. Proline levels increased substantially in both leaves and roots under combined stress, highlighting its role as a key osmoprotectant and non-enzymatic antioxidant when enzymatic defenses are insufficient.
  6. The content of secondary metabolites, including phenolics, flavonoids, terpenoids, and alkaloids, generally declined under combined stress, suggesting compromised biosynthetic capacity or diversion of metabolic resources under severe physiological strain.
  7. Collectively, these results demonstrate that combined flooding and salinity stress overwhelms the antioxidant defense system in oil palm seedlings, especially in roots, underscoring the need for stress-resilient varieties and adaptive management strategies for areas exposed to multiple abiotic stressors.

ACKNOWLEDGMENTS

This work is supported by the Ministry of Higher Education Malaysia under the Fundamental Research Grant Scheme (FRGS) (FRGS/1/2019/STG04/UPM/02/1).

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Article submitted: June 14, 2025; Peer review completed: January 8, 2026; Revised version received: February 28, 2026; Accepted: March 8, 2026; Published: May 15, 2026.

DOI: 10.15376/biores.21.3.5931-5953