Skip to main content

Effect of ammonium stress on phosphorus solubilization of a novel marine mangrove microorganism Bacillus aryabhattai NM1-A2 as revealed by integrated omics analysis

Abstract

Background

Phosphorus is one of the essential nutrients for plant growth. Phosphate-solubilizing microorganisms (PSMs) can alleviate available P deficiency and enhance plant growth in an eco-friendly way. Although ammonium toxicity is widespread, there is little understanding about the effect of ammonium stress on phosphorus solubilization (PS) of PSMs.

Results

In this study, seven PSMs were isolated from mangrove sediments. The soluble phosphate concentration in culture supernatant of Bacillus aryabhattai NM1-A2 reached a maximum of 196.96 mg/L at 250 mM (NH4)2SO4. Whole-genome analysis showed that B. aryabhattai NM1-A2 contained various genes related to ammonium transporter (amt), ammonium assimilation (i.e., gdhA, gltB, and gltD), organic acid synthesis (i.e., ackA, fdhD, and idh), and phosphate transport (i.e., pstB and pstS). Transcriptome data showed that the expression levels of amt, gltB, gltD, ackA and idh were downregulated, while gdhA and fdhD were upregulated. The inhibition of ammonium transporter and glutamine synthetase/glutamate synthase (GS/GOGAT) pathway contributed to reducing energy loss. For ammonium assimilation under ammonium stress, accompanied by protons efflux, the glutamate dehydrogenase pathway was the main approach. More 2-oxoglutarate (2-OG) was induced to provide abundant carbon skeletons. The downregulation of formate dehydrogenase and high glycolytic rate resulted in the accumulation of formic acid and acetic acid, which played key roles in PS under ammonium stress.

Conclusions

The accumulation of 2-OG and the inhibition of GS/GOGAT pathway played a key role in ammonium detoxification. The secretion of protons, formic acid and acetic acid was related to PS. Our work provides new insights into the PS mechanism, which will provide theoretical guidance for the application of PSMs.

Peer Review reports

Background

Phosphorus (P) is essential to mangrove ecosystems, which is implicated as one of the most limiting nutrients for plant growth [1, 2]. Despite the high amount of total P in the soil, most of the P cannot be absorbed and utilized by plants [1, 3, 4]. Chemical fertilizers have been widely used to satisfy the demand for P to promote plant productivity [4]. However, the long-term application of chemical fertilizers has led to a series of problems limiting agricultural sustainable development, such as soil nutrient imbalance and water eutrophication [3, 4]. Consequently, it is urgent to find an eco-friendly and economically viable manner to maintain a continuous supply of P in plants. Phosphorus solubilization (PS) is a significant biochemical process in sediments, and plays important roles in alleviating P limitations of mangrove ecosystems [5]. Several microorganisms can transform insoluble inorganic P into soluble forms available to plants, which are known as phosphate-solubilizing microorganisms (PSMs) [1, 6]. Furthermore, PSMs can not only release the accumulated P left by P fertilizer but also promote plant growth without environmental hazards [1, 6]. PSMs mainly include phosphate-solubilizing bacteria (PSB) and phosphate-solubilizing fungi (PSF). PSB include various strains from the genera Pseudomonas, Bacillus, Agrobacterium Azotobacter, Xanthomonas, and Enterobacter [7, 8]. PSF include strains of Penicillium, Mucor, Aspergillus, Pichia, and Chaetomium [8, 9]. These microorganisms can serve as biofertilizers that improve the agricultural yield [10].

The secretion of low molecular weight organic acids is considered to be the principal mechanism for mineral phosphate dissolution [3, 11]. These organic acids can liberate P either by lowering the pH or chelating the cations bound to phosphate [10]. Gluconic acid produced by the direct oxidation of glucose is usually regarded as the main organic acid in the solubilization of mineral phosphate [3]. Accumulating evidence suggested that intermediates in the tricarboxylic acid cycle (TCA cycle), such as succinic acid, malic acid, and citric acid, were also the main organic acids secreted during the process of PS [11]. Other mechanisms such as the production of inorganic acids and chelating substances, are less effective than organic acids in releasing P [8]. PS conducted by PSMs is a complicated process. The efficiency of PS is affected by many factors such as nutrition, pH, and oxygen concentration [12, 13]. Since PSMs are heterotrophic, it is generally accepted that carbon (C) and nitrogen (N) are two of the limiting factors for the growth of PSMs [12]. It was reported that easily utilizable C source was deemed as a contributing factor to increase the PS efficiency of PSMs [14]. Besides, ammonium (NH4+) was also the best N source for PS, among various nutrients used by microorganisms [9].

NH4+ is a fundamental substrate for nucleic acid and amino acid synthesis [15, 16]. It has been proved that NH4+ played a positive role as a stress signal [16]. For instance, NH4+ nutrition enhanced salt stress resistance in citrus plants due to the induction of the antioxidant cellular machinery [17]. Moreover, increased alkaline phosphatase activity led to the solubilization of P under high NH4+ stress [18]. However, excessive NH4+ damages the growth of the living organism, which is widely known as NH4+ toxicity [19]. NH4+ toxicity is a significant ecological and agricultural issue [15]. Several hypotheses for the cause of toxicity have been proposed, including the futile transmembrane NH4+ cycle, the lack of inorganic cations and organic acids, the impairment of hormone homeostasis, and the disorder of pH regulation [20]. A previous study found that supplemented succinate effectively alleviated NH4+ toxicity [20]. Therefore, it was assumed that the production of organic acids in PS process performed a significant role in resisting NH4+ toxicity. Until now, few studies have focused on the influence of NH4+ stress on releasing precipitated inorganic P.

In our current work, an efficient PSM Bacillus aryabhattai NM1-A2 was isolated from the marine mangrove sediment. The effects of different C sources, N sources, C/N, (NH4)2SO4 concentrations, NaCl concentrations and initial pH of solution on the solubilization of insoluble phosphate were investigated to determine its PS characteristics. Then, the effect of NH4+ stress on PS was explored at the level of genome, transcriptome, and metabolite. Our work demonstrates the scientific basis for the application of PSMs, and it will promote environment-friendly agricultural development.

Results

Isolation and identification of PSMs

Seven PSMs were selectively obtained from the mangrove sediments based on the obvious phosphate-solubilizing halos around colonies on SRSM solid medium (the enrichment medium invented by Sundara Rao and Sinha specifically for the isolation of PSMs) (Fig. 1). The bromocresol purple indicator on the SRSM medium changed from purple to yellow (Fig. 1), which was a sign of pH drop. Thus, the seven PSMs might dissolve mineral phosphate by secreting organic acids or expelling protons.

Fig. 1
figure 1

Isolation of phosphorus-solubilizing microorganisms (PSMs). Seven PSMs screened in this study were labeled as NM1-A2, HM2, HM3, HM4, HM5, HM6 and HM7, respectively

We performed the PCR amplifications using specific primers [21] (Additional file 1: Table S1) for 16 S rDNA. 16 S rDNA sequences were subjected to agarose gel electrophoresis, and bright bands were detected at 1, 500 bp (Fig. 2a). The results showed that the seven PSMs were pure strains. The nucleotide sequences of 16 S rDNA were analyzed with the BLASTn search algorithm and aligned to their nearest neighbors (Table S2). A phylogenetic tree was created based on 16 S rDNA nucleotide sequences of the isolates and their nearest neighbors (Fig. 2b). It was found that NM1-A2 and HM3 were most closely related to B. aryabhattai. HM5 and HM6 were most closely related to B. licheniformis. HM2, HM4, and HM7 were most closely related to Metabacillus halosaccharovorans, B. haynesii, and B. velezensis, respectively.

Fig. 2
figure 2

Identification of seven PSMs screened in this study. (a) Evaluation of 16 S rDNA PCR products by agarose gel electrophoresis. (b) Neighbour-joining phylogenetic tree based on 16 S rDNA. Bootstrap analyses were made with 1000 cycles. M, 1, 2, 3, 4, 5, 6 and 7 indicate Marker, NM1-A2, HM2, HM3, HM4, HM5, HM6 and HM7, respectively

Determination of the soluble phosphate concentration in culture supernatant

The soluble phosphate concentration in culture supernatant of seven PSMs varied from 22.65 mg/L to 139.46 mg/L. Except for HM2 and HM7, the concentration of soluble phosphate decreased as time progressed. The soluble phosphate concentration in culture supernatant of B. aryabhattai NM1-A2 reached 139.46 mg/L at 48 h, which was much higher than those of other strains (Table 1).

Table 1 The concentration of soluble phosphate in culture supernatant when strain was cultured in SRSM medium for 12 h

The PS process of B. aryabhattai NM1-A2 on SRSM liquid medium containing different components was examined to better understand its PS characteristics. It was found that the solubilization of tricalcium phosphate (TCP) in the SRSM liquid medium was accompanied with the decrease of pH after 12 h (Fig. 3). The correlation analysis showed a significant negative correlation between the soluble phosphate concentration and pH in culture supernatant of B. aryabhattai NM1-A2 (Table 2). The results suggested that the secretion of organic acids or the release of protons might lead to a decrease in pH, which might be one of the PS mechanisms. The highest concentration of soluble phosphate reached 124.24 mg/L when B. aryabhattai NM1-A2 was cultivated with glucose as the sole C source, followed by sucrose, starch, fructose, and maltose (117, 73.07, 45.38 and 40.68 mg/L, p < 0.05) (Fig. 3a). As shown in Fig. 3b, the optimum N source for PS was (NH4)2SO4 (136.29 mg/L), followed by NH4Cl, CO(NH2)2, KNO3 (124.99, 87.51, and 56.08 mg/L, p < 0.05). The soluble phosphate concentration in culture supernatant of B. aryabhattai NM1-A2 decreased rapidly with the increase in C/N ratio in the SRSM lipid medium (Fig. 3c). In addition, the efficiency of PS was affected by the concentration of (NH4)2SO4. The highest soluble phosphate concentration of 196.96 mg/L was dissolved at 250 mM of (NH4)2SO4 concentration. in the range from 1 mM to 300 mM (Fig. 3d). And the production of soluble P could reach the highest when NaCl concentration was 2% in the range from 0 to 10% (Fig. 3e). Subsequently, the soluble phosphate concentration decreased continuously with the increase of NaCl concentration (Fig. 3e), which indicated that the process of PS was inhibited under salt stress. The change of pH value directly affected the survival and metabolism of microorganisms. As shown in Fig. 3f, B. aryabhattai NM1-A2 grew normally in the range of pH 5.0–10.0. The highest soluble phosphate concentration (142.79 mg/L) was detected when the initial pH value was 6.0, followed by 7.0, 5.0, 8.0, 9.0 and 10.0 (137.65, 132.87, 126.504, 114.74, and 65.37 mg/L).

Fig. 3
figure 3

(a) Effects of carbon sources, (b) nitrogen sources, (c) C/N, (d) (NH4)2SO4 concentrations, (e) NaCl concentrations, and (f) initial pH on the solubilization of tricalcium phosphate by B. aryabhattai NM1-A2. The least significant difference test based on the analysis of variance model was used to calculate statistical significance, as expressed in means ± standard error. And values significantly different from those of the control were represented by different lowercase letters

Table 2 Correlation coefficient between soluble phosphate concentration and pH while Bacillus aryabhattai NM1-A2 was cultured under different conditions

Effect of NH4 + stress on the types and concentrations of organic acids

As we know, PS process of PSMs was associated with the release of low molecular weight organic acids [3, 11]. High performance liquid chromatography (HPLC) analysis showed the presence of four organic acids in culture supernatant, namely formic acid, malic acid, acetic acid and succinic acid, while lactic acid and citric acid were not detected (Fig. S1 and Table S3). Among the four organic acids, formic acid showed the highest concentration, followed by malic acid, acetic acid and succinic acid (Fig. 4). As shown in Fig. 4, the concentrations of formic acid and acetic acid in the high-NH4+ group were 443.7 and 120.5 mg/L at 12 h, respectively. These concentrations were significantly higher than those in the low-NH4+ group (160.1 and 57.3 mg/L at 12 h, p < 0.001). As shown in Fig. 4, the concentrations of succinic acid in the high-NH4+ group was 7.5 mg/L at 12 h, which was lower than that in the low-NH4+ group (20.8 mg/L, p < 0.05). However, there was no significant difference in the concentration of malic acid between the low- and high-NH4+ group (Fig. 4). The increase of soluble phosphate concentration in culture supernatant of B. aryabhattai NM1-A2 could be potentially due to the production of organic acids. And the types and concentrations of secreted organic acids were influenced by (NH4)2SO4 concentration.

Fig. 4
figure 4

Kinds and concentrations of organic acids in the supernatants of B. aryabhattai NM1-A2 in the low- and high-NH4+ groups. Two independent-sample t-test was used to determine differences in organic acid concentration between the low- and high-NH4+ group. And values significantly different from those of the control were represented by asterisks, which “” and “” indicated p < 0.05 and p < 0.001, respectively, while “ns” indicated no significant difference

Whole-genome assembly and annotation of B. aryabhattai NM1-A2

NH4+ was a preferred N source for most bacteria [2]. The high-affinity NH4+ transporters AMTs (encoded by amt) were used to absorb NH4+ at low NH4+ concentrations, while some low-affinity transporters were responsible for NH4+ at high NH4+ concentrations [22]. The whole-genome of B. aryabhattai NM1-A2 (Table S4) contained genes coding for glutamine synthetase (GS, encoded by glnA), glutamate synthase (GOGAT, encoded by gltBD) and glutamate dehydrogenase (GDH, encoded by gdhA), which were key enzymes for NH4+ assimilation [23].

In addition, there were many types of PS-related genes, mainly including genes involved in organic acid synthesis and the phosphate regulatory system (Table S4). Inorganic phosphate (Pi) was mainly obtained through two independent uptake systems, inorganic phosphorus transporter (Pit) and phosphorus specific transporter (Pst) [24]. The Pst system was a typical ABC transporter composed of PstS, PstC, PstA, PstB and PhoU [24, 25]. Pi was transported by the Pst system under P starvation [25, 26]. B. aryabhattai NM1-A2 also had histidine kinase PhoR, response regulator PhoB for induction of PHO regulon under P-limiting conditions [27]. The main enzymes involved in TCA cycle and organic acid synthesis were found to be: isocitrate lyase, formate dehydrogenase, acetate kinase and isocitrate dehydrogenase, fumarate hydratase, and malate dehydrogenase, encoded by aceA, fdhD, ackA, idh, fumC and mdh, respectively.

Transcriptome sequencing of B. aryabhattai NM1-A2 and annotation analysis of DEGs

Transcriptome data results showed 2422 significantly differentially expressed genes (DEGs) between the low- and high-NH4+ groups. A total of 739 significantly upregulated genes and 1683 significantly downregulated genes were detected (Fig. 5a and b). KEGG enrichment results showed that the DEGs were mainly enriched in carbohydrate metabolism, amino acid metabolism, metabolism of cofactors and vitamins, and energy metabolism (Fig. 5c). C and N metabolism played an important role in response to NH4+ stress [22]. Moreover, the numbers of upregulated or downregulated DEGs of the top 20 most enriched KEGG pathways were displayed (Fig. 5d). The genes related to pyruvate metabolism, oxidative phosphorylation, glycolysis, and TCA cycle were mostly upregulated. The GO enrichment analysis of DEGs between the low- and high-NH4+ groups (Fig. 5e and f) showed that the main enriched biological processes were cellular process, single organization and metabolic processes. The main enriched cellular components were cell and cell part. The main enriched functions were binding, catalytic activity, and transporter activity. These results indicated that catalytic and transport activities in B. aryabhattai NM1-A2 were significantly affected by high NH4+ stress.

Fig. 5
figure 5

Effect of NH4+ stress on B. aryabhattai NM1-A2 gene transcription. (a) Numbers of upregulated and downregulated differentially expressed genes (DEGs). (b) Volcano plot presentation of overall scattered DEGs. (c) KEGG enrichment pathway of DEGs [1]. (d) Upregulated or downregulated expressions of DEGs of the top 20 most enriched KEGG pathways [1]. (e) GO annotation of DEGs. (f) Upregulated or downregulated expressions of the top 20 most enriched GO terms

The transcriptome data showed that the expression level of amt was downregulated by 3.52 fold, which indicated that the NH4+ transported by AMT was reduced (Table 3; Fig. 6). NH4+ assimilation was regulated by two PII proteins (GlnB and GlnK) [28]. GlnB and GlnK could be reversibly uridylylated by uridilyl-transferase/uridylyl-removase (UT/UR), controlling the bifunctional enzyme adenylyl-transferase/adenylyl-removase (AT/AR), which could reversibly adenylylate (inactivate) or deadenylylate (activate) GS [28, 29]. GlnK was commonly cotranscribed with the NH4+ transporter AMT and reversibly inhibited AMT’s transport activity [29]. The expression levels of glnB and glnK were downregulated by 2.779 and 2.323 folds, respectively (Table 3). AR enzymatic activity was promoted through the deuridylylation of GlnK-U and GlnB-U to rapidly inhibited the activity of GS. Then, GlnK binded to AMT to form a complex to inhibit NH4+ uptake.

Table 3 DEGs related to NH4+ assimilation, phosphate transport and metabolism in B. aryabhattai NM1-A2.
Fig. 6
figure 6

NH4+ tolerance mechanism of B. aryabhattai NM1-A2. “+” indicated that enzyme activity or substance content increases under NH4+ stress. “−“ indicated that enzyme activity or substance content reduces under NH4+ stress. Red letters indicated downregulation genes, and navy letters indicated upregulation genes. Purple letters indicated pathways, and orange ovals indicated transporters. Solid arrow corresponded to direct reaction, and dotted arrow corresponded to indirect reaction. The red line indicated that the process is inhibited. 2-OG, TCP, Pi, polyP, Pst, AMT, GLU, GLN, and GS indicated 2-oxoglutarate, tricalcium phosphate, inorganic phosphorus, polyphosphate, phosphorus specific transporter, ammonium transporter, glutamate, glutamine, and glutamine synthetase, respectively

The GS-GOGAT cycle was the most crucial pathway for primary N assimilation [30, 31]. NH4+ and glutamate (GLU) to form glutamine (GLN) under the catalysis of GS (GlnA) [29]. The large subunit (GltB) and small subunit (GltD) of GOGAT complete the metabolic pathway of GLU regeneration from GLN and 2-oxoglutarate (2-OG) [29]. The expression levels of gltB, and gltD were downregulated by 1.425, and 3.377 folds, respectively (Table 3), which revealed that the GS − GOGAT pathway was not the main approach for NH4+ assimilation in B. aryabhattai NM1-A2. GDH has been reported to incorporate excess NH4+ into GLU when exposed to NH4+ stress [23]. The expression level of gdhA was upregulated in the high-NH4+ group compared with that in the low-NH4+ group (Table 3). Therefore, the GDH pathway played a critical role in responding to NH4+ stress (Fig. 6). The assimilation of NH4+ was accompanied by the release of protons, which was one of the mechanisms of PS (Fig. 6).

The production of organic acids was the main mechanism for solubilizing insoluble P [9]. The transcriptome data showed that the expression level of ackA was upregulated, wheras fdhD was downregulated (Table 3; Fig. 6). This might lead to increased concentrations of acetic acid and formic acid in high-NH4+ group (Fig. 4). Therefore, formic acid and acetic acid played an important role in PS process of B. aryabhattai NM1-A2 under NH4+ stress (Fig. 6). In addition, idh was also upregulated by 1.256 fold. More 2-OG was produced under NH4+ stress, which provided sufficient C skeletons for the subsequent amino acid synthesis. The expression level of aceA was downregulated (Table 3), which might be the reason behind the decrease in succinic acid in the high-NH4+ group (Fig. 4). fumC and mdh were upregulated in the high-NH4+ group compared with those in the low-NH4+ group (Table 3). The catabolism of malic acid was greater than the synthesis, which led to the decrease in malic acid concentration under NH4+ stress.

The Pst system played an important role in transporting inorganic P under conditions of P limitation [27]. PstS and PstB were the key proteins in Pst system [24]. Genes related to the Pst system and PhoR were downregulated under NH4+ stress, especially pstS and pstB (downregulated by 5.29 and 5.71 folds). As shown in the Fig. 3d, the content of soluble phosphate in the high-NH4+ group (196.96 mg/L) was significantly higher than that in the low-NH4+ group (62.5 mg/L, p < 0.001). As a result, the Pst transporter was inhibited. The signal was transmitted from the Pst transporter to PhoR through PhoU, and inhibited the kinase function of PhoR, resulting in dephosphorylation of PhoB [27]. When Pi was abundant, excess P was stored as polyphosphate (PolyP) [32]. PolyP could be separated into two groups, pyrophosphates (two phosphate residues) and high molecular weight PolyP [33]. Pyrophosphates (PPi) was a metabolic product of biosynthetic reactions, and pyrophosphatase (PPaX) catalyzed the hydrolysis of PPi [33]. ppaX was upregulated in high-NH4+ group, which could maintain cellular PPi homeostasis and provide energy for the PPi-generating biosynthetic reactions (Table 3; Fig. 6).

RT-qPCR of genes involved in PS of B. aryabhattai NM1-A2 under NH4 + stress

Quantitative real-time polymerase chain reaction (RT-qPCR). According to the abovemetioned results, eight genes (gltD, ackA, pstB, ppaX, pstB, amtB, phoR, and glnA) were selected for RT-qPCR analysis. The expression levels of ackA and ppaX were upregulated in the high-NH4+ group, whereas gltD, pstB, pstB, amtB, phoR, and glnA were downregulated (Fig. S2). The expression trends of eight genes were consistent with the RNA-seq data, which confirmed the reliability of the transcriptomic data.

Discussion

P is an essential nutrient element for plant growth and development [1, 2]. PSMs can promote the availability and absorption of P in soil [8]. The application of PSMs plays a very important role in the sustainable development of agriculture [1, 6].

In this study, TCP was selected as the sole P source on SRSM medium because it represented the vast majority of insoluble P [34]. Based on cultivation and observation, seven PSMs were screened from marine mangrove sediments (Fig. 1). According to 16 S rDNA sequence analysis, these strains were confirmed as members of Bacillus genus. Several studies have shown that Pseudomonas, Bacillus and Rhizobia were effective phosphate solubilizers [7, 8]. Bacillus spp. were preferred on account of lasting vitality [35]. The soluble phosphate concentrations in culture supernatant of these strains were evaluated by molybdenum blue colorimetric method [21]. Among them, the soluble phosphate concentration in culture supernatant of B. aryabhattai NM1-A2 reached a maximum of 139.46 mg/L at 48 h (Table 1). In addition, the soluble phosphate concentration in culture supernatant decreased as time progressed, which could probably be attributed to the utilization of P by bacteria [36]. Bacillus aryabhattai was widely distributed in various habitats owing to its strong stress resistance, and had great potential in nitrogen fixation, PS and the production of indole-3-acetic acid [36,37,38]. However, few studies have revealed the genomic potential of Bacillus aryabhattai on PS.

PSMs are heterotrophic microorganisms. The PS efficiency of PSMs depends on the provision of suitable C and N in a large extent [12]. Scervino et al. reported that glucose and (NH4)2SO4-based media showed the highest PS values [12], which was consistent with the results of this study (Fig. 3a and b). Glucose was the preferred C source for most bacterial growth [14]. However, Li’s report [6] showed that there was no correlation between cell growth and soluble P production [6]. Mineral phosphate could be solubilized by the direct oxidation of glucose to gluconic acid [8]. This condition might explain the maximum PS ability with glucose as C source (Fig. 3a). Among all N sources tested, the optimum N source for PS was (NH4)2SO4 (Fig. 3b). Bacterial growth was greatly enhanced with the increasing concentration of (NH4)2SO4, which led to the consumption of available P in the culture medium [6]. Interestingly, the soluble phosphate concentration in culture supernatant of B. aryabhattai NM1-A2 was continuously improved with the increase of (NH4)2SO4 concentration and reached the highest (196.96 mg/L) under 250 mM (NH4)2SO4 (Fig. 3d). NH4+ was the preferred N source for most bacteria, but it was toxic when reaching a certain concentration [37]. For example, Nitrobacter winogradskyi Nb-255 grew well under NH4+ concentrations below 25 mM, but it was inhibited under NH4+ concentrations higher than 35 mM [38]. It was reported that transcript degradation or gene repression was part of the NH4+-responsive stimulon [39]. Given its remarkable NH4+-tolerant survivability, the mechanism of PS and detoxification of B. aryabhattai NM1-A2 under NH4+ stress was revealed by multi-omics analysis.

Ammonium exists predominantly in the ionic form (NH4+) at neutral pH, and the minor gaseous species (NH3) can diffuse rapidly through the cell membrane. NH4+ could be transported into the cell via AMT under low ammonium conditions [40]. When bacteria encountered high concentration of NH4+, the passive diffusion of NH3 can provide enough N for optimal cell growth [41]. Transcriptome data showed that amt was downregulated, suggesting NH4+ transported via AMT was inhibited (Table 3). NH4+ assimilation was the main approach for NH4+ detoxification [22]. Under high-NH4+ condition, excess NH4+ could be assimilated into GLU mainly through GDH pathway, thereby reducing NH4+ accumulation (Table 3) [41, 42]. Downregulating the GS/GOGAT pathway under NH4+ stress was helpful to prevent the waste of energy (Table 3) [43]. Moreover, research shows that NH4+ assimilation by GS localized in the plastid rather than NH4+accumulation was a primary cause for toxicity [19]. In this study, GS enzyme activity of B. aryabhattai NM1-A2 was inhibited in the regulation of GlnB and GlnK under NH4+ stress, thereby preventing NH4+ toxicity (Fig. 6) [29]. Tian et al. reported that the sugar and starch contents of plants decreased under NH4+ treatment because of the depletion of C skeletons used for excess NH4+ assimilation [22]. In the present study, the overall upregulated glycolysis, pyruvate metabolism and TCA cycle could provide abundant C skeletons for excess NH4+ assimilation (Fig. 5d) [22]. Among them, the upregulated expression of idh indicated that more 2-OG was induced under NH4+ stress (Table 3) [44, 45]. It has been reported that supplemented 2-OG enhanced NH4+ assimilation [20]. That might be an important feature of B. aryabhattai NM1-A2 responded to NH4+ toxicity. The assimilation of NH4+ within microbial cells was accompanied by the release of protons resulting in the solubilization of P [3, 46].

The secretion of organic acids was an important phosphate-solubilizing way in PSMs, which could be produced from cells to facilitate the solubilization of P by supplying both protons and metal complexing organic acid anions [34]. Different PSMs would secrete the various types and concentrations of organic acids to solubilize P [3]. The production of succinic acid was related to PS activity of Bacillus megaterium, while oxalic acid and citric acid were the main organic acids released by Pseudomonas sp [3]. The secretion of organic acids was also influenced by the types and concentrations of P sources [47]. Arvind et al. found that the generation of formic acid was limited to the dissolution of TCP, and oxalic acid production to the solubilization of Mussoorie rock phosphate, Udaipur rock phosphate, and North Carolina rock phosphate [48]. In this study, transcriptome and HPLC analysis showed that formic acid and acetic acid played important roles in the improvement of available P fractions under NH4+ stress, and the concentrations of formic acid and acetic acid in the high-NH4+ group were generally higher, about 2.77 and 2.1 folds, respectively (Fig. 4; Table 3). It has been reported that acetate would accumulate when the glycolysis flux exceeded the catalytic capacity of the TCA cycle [49]. Therefore, high glycolysis rate might present in B. aryabhattai NM1-A2, which was responsible for the accumulation of acetic acid under NH4+ stress (Fig. 4). Furthermore, the PS process was affected by the properties of organic acids. Although formic acid and acetic acid were both mono-carboxylic acids, formic acid had a higher PS ability than acetic acid [50]. Isocitrate lyase was a key enzyme of the glyoxylate cycle that was the bypassed pathway of the TCA cycle [51]. As shown in Table 3, ackA was downregulated under NH4+ stress, which suggested that the transfer of energy metabolism to the glyoxylate cycle was inhibited. This might lead to a decrease in succinic acid concentration in the high-NH4+ group (Fig. 4).

Conclusion

B. aryabhattai NM1-A2 was screened from marine mangrove sediments. The soluble phosphate concentration in culture supernatant of B. aryabhattai NM1-A2 was continuously improved with the increase of (NH4)2SO4 concentration. Integrated omics technology was used to reveal the effects of NH4+ stress on PS of B. aryabhattai NM1-A2 for the first time. The inhibitions of AMT and GS/GOGAT were helpful to prevent the waste of energy. The GDH pathway was the main approach for NH4+ assimilation, in which glycolysis and TCA cycle could provide abundant C skeletons. The secretion of protons, formic acid, and acetic acid played a key role in PS of B. aryabhattai NM1-A2 under NH4+ stress. This study demonstrated a scientific basis for the development of biofertilizers.

Methods

Samples and media

The sediment samples were isolated from the National Shankou Natural Reserve of Mangrove in Beihai, Guangxi, China (21°29′25.74′′N, 109°45′49.43′′E) using the methods described in a previous study [52].

The following media were used in this study: Luria–Bertani medium (LB) containing (g/L) tryptone (10 g), yeast extract (5 g) and NaCl (10 g); SRSM enrichment medium [53] containing (g/L) glucose (10 g), (NH4)2SO4 (0.5 g), NaCl (20 g), KCl (0.2 g), FeSO4·7H2O (0.004 g), MgSO4·7H2O (0.3 g), MnSO4·H2O (0.0045 g), yeast extract (0.5 g), Ca3(PO4)2 (5 g). The initial pH of the medium for both groups was adjusted to 7.0 by adding NaOH or HCl.

Screening for PSMs

The sediment (5.0 g) was mixed with LB medium (10 mL), followed by shaking for 1 h in a biochemical incubator at 37 °C, 200 rpm. Then serial dilutions (100–10− 3) were spread-plated onto LB medium plates. After incubation for 12 h at 37 °C, colonies were selected from the plates. Then, these isolates were purified by the streak plate method. Each isolate was added to the SRSM medium plates to verify its PS ability by the presence of a clear halo around colonies.

Identification of the isolated strains

All strains were cultured in 100 mL Erlenmeyer flasks containing 50 mL LB at 37 °C with continuous rocking on a shaker at 200 rpm for 12 h. Total genomic DNA was extracted using a TIANamp bacterial DNA kit (TIANGEN) according to the instructions of the manufacturer. The quality of the extracted DNA was measured by 1% agarose gel electrophoresis and analyzed using a NanoDrop™ 2000 spectrophotometer [5] (Thermo Scientific, USA). The amplified products of 16 S rDNA were obtained with specific primers [21] (Table S1) under the following reaction conditions: 95 ℃, 5 min; [95 °C for 30 s; 54 °C for 30 s; and 72 °C for 1 min] × 35 cycles; and 72 °C, 7 min. The PCR products were verified by 1% agarose gel electrophoresis, and they were sequenced using the Sanger sequencing platform (BGI: https://www.bgi.com/). The nucleotide sequences of 16 S rDNA were compared with sequences in NCBI (http://www.ncbi.nlm.nih.gov/GenBank) to identify close phylogenetic relatives. And the 16 S rDNA phylogenetic tree was constructed by using the neighbor-joining method supported by 1,000 bootstrap replicates in MEGA 7.0 [54].

Determination of the soluble phosphate concentration in culture supernatant

The seven strains were cultured on SRSM medium for 48, 72, 96, and 120 h, and then centrifuged at 6, 000 rpm for 5 min. Then, the concentration of soluble phosphate in culture supernatant was determined by molybdenum blue colorimetric method [21]. A separate SRSM medium inoculated with sterile double-distilled water served as the control.

For optimization purpose, B. aryabhattai NM1-A2 was cultured for 12 h on SRSM medium containing C sources (glucose, sucrose, starch, fructose, and maltose), N sources ((NH4)2SO4, NH4Cl, CO(NH2)2, and KNO3), C/N (5, 20, and 40), initial solution pH (5.0, 6.0, 7.0, 8.0, 9.0, and 10.0), NaCl concentrations (0%, 2%, 4%, 6%, 8%, and 10%) and (NH4)2SO4 concentrations (1-300 mM). Then the concentration of soluble phosphate in culture supernatant of B. aryabhattai NM1-A2 was detected by the same method as described above. The final solution pH was determined using a pH meter (PHS-3 C, China Sanxin).

Organic acids production of B. aryabhattai NM1-A2 under NH4 + stress

The types and concentrations of organic acid in the supernatants of the low- and high-NH4+ groups were analyzed using HPLC method [6]. The following organic acids (i.e., formic acid, malic acid, lactic acid, acetic acid, citric acid, and succinic acid) were measured using an Alliance liquid chromatograph (Waters E2695, United States). The liquid chromatograph column was Poroshell120 SB-Aq 4.6×250 mm, 4 μm (Agilent Technologies Inc., America), with a column temperature of 25 ℃. The detection wavelength was 210 nm.

Whole-genome sequencing and assembly of B. aryabhattai NM1-A2

The whole-genome sequencing and assembly were performed by PFOMIC Bioinformatics Company (Nanning, China) with the Illumina NovaSeq 6000 PE150, Oxford Nanopore Technologies PromethION [54]. The whole genome data of B. aryabhattai NM1-A2 have been deposited in NCBI GeneBank with the accession number PRJNA760884. The MinKNOW software was used for filtering the low-quality reads. Then, the filtered reads were assembled by using the Unicycler (0.4.8) software. Moreover, Pilon software was used to obtain more accurate genome. Finally, DIAMOND was used to align the predicted protein sequence with the Kyoto Encyclopedia of Genes and Genomes (KEGG) [55]. For the alignment of each protein sequence, the match with the highest score (default identity ≥ 30%) was used to select the functional annotation.

Transcriptome sequencing analysis of B. aryabhattai NM1-A2

We analyzed the transcriptome of B. aryabhattai NM1-A2 in the low- and high-NH4+ groups to study the transcriptional expression changes between the N deficient and the NH4+-stressed environment. The RNA of B. aryabhattai NM1-A2 was extracted using the TRIzol method [56]. Qualified libraries were sequenced on the Illumina Novaseq sequencing platform using the paired-end sequencing method (PE150). FastQC_v0.11.3 was used for quality control of the raw sequencing data [57]. The filtered sequence was aligned with the rRNA database using Bowtie2 to remove the rRNA sequence. Qualified sequencing data were aligned to the B. aryabhattai NM1-A2 genome using Hisat2, and the count value and the Fragments Per Kilobase of transcript per Million mapped reads (FPKM) values of the genes were calculated using HTseq-count and AWK script. EdgeR was used to calculate the differentially expressed genes (DEGs) [p < 0.05 and |Log2(fold change) | > 1]. Then, Gene Ontology (GO) and KEGG databases were used for functional enrichment of DEGs [55].

Verification experiment

RT-qPCR was used to validate the transcriptomic data. A two-step method was used for the RT-qPCR of key genes with specific primers (Table S2) [21]. GAPDH was used as a reference gene for the normalization. The expression levels of selected genes were evaluated using the 2−ΔΔCt method.

Statistical analyses

All experimental treatments were conducted in triplicate, and the results are expressed as the means ± standard error. Data were processed with SPSS 24 and Diamond software. The relevant query databases were KEGG and NCBI. The least significant difference test based on the analysis of variance model was used for multiple comparisons among treatments groups for soluble phosphate concentration or pH value. And two independent-sample t-test was used to determine differences in organic acid concentration between the low- and high-NH4+ group. All figures were made with GraphPad Prism 8.0.2 (263) and Adobe Illustrator (2020).

Data availability

The datasets presented in this study can be found in online repositories. The whole genome sequences are available from the NCBI nucleotides database under accessions NZ_CP083269 − NZ_CP083272. The transcriptome data has been uploaded to the SRA database of the NCBI database, the accession numbers are SRX18707345 − SRX18707349.

References

  1. Wang ZH, Zhang HH, Liu L, Li SJ, Xie JF, Xue X, et al. Screening of phosphate-solubilizingbacteria and their abilities of phosphorus solubilization and wheat growth promotion. BMC Microbiol. 2022;22(1):296.

    PubMed  PubMed Central  Google Scholar 

  2. Reef R, Feller IC, Lovelock CE. Nutrition of mangroves. Tree Physiol. 2010;30(9):1148–60.

    PubMed  CAS  Google Scholar 

  3. Zeng QW, Ding XL, Wang JC, Han XJ, Iqbal HM, Bilal M. Insight into soil nitrogen and phosphorus availability and agricultural sustainability by plant growth-promoting rhizobacteria. Environ Sci Pollut Res. 2022;29(30):45089–106.

    CAS  Google Scholar 

  4. Liu YQ, Wang YH, Kong WL, Liu WH, Xie XL, Wu XQ. Identification, cloning and expression patterns of the genes related to phosphate solubilization in Burkholderia multivorans WS-FJ9 under different soluble phosphate levels. AMB Express. 2020;10(1):108.

    PubMed  PubMed Central  CAS  Google Scholar 

  5. Zhang ZF, Nie SQ, Sang YM, Mo SM, Li JH, Kashif M, et al. Effects of Spartina alterniflora invasion on nitrogen fixation and phosphorus solubilization in a subtropical marine mangrove ecosystem. Microbiol spectr. 2022;10(3):e0068221.

    PubMed  Google Scholar 

  6. Li LL, Chen RB, Zuo ZY, Lv ZS, Yang ZH, Mao W, et al. Evaluation and improvement of phosphate solubilization by an isolated bacterium Pantoea agglomerans ZB. World J Microbiol Biotechnol. 2020;36(2):27.

    PubMed  CAS  Google Scholar 

  7. Behera BC, Singdevsachan SK, Mishra RR, Dutta SK, Thatoi HN. Diversity, mechanism and biotechnology of phosphate solubilising microorganism in mangrove—a review. Biocatal Agric Biotechnol. 2014;3(2):97–110.

    Google Scholar 

  8. Alori ET, Glick BR, Babalola OO. Microbial phosphorus solubilization and its potential for use in sustainable agriculture. Front Microbiol. 2017;8:971.

    PubMed  PubMed Central  Google Scholar 

  9. Sharma SB, Sayyed RZ, Trivedi MH, Gobi TA. Phosphate solubilizing microbes: sustainable approach for managing phosphorus deficiency in agricultural soils. Springerplus. 2013;2(1):587.

    PubMed  PubMed Central  Google Scholar 

  10. Rawat P, Das S, Shankhdhar D, Shankhdhar SC. Phosphate-solubilizing microorganisms: mechanism and their role in phosphate solubilization and uptake. J Soil Sci Plant Nutr. 2021;21(1):49–68.

    CAS  Google Scholar 

  11. Ding YQ, Yi ZL, Fang Y, He SL, Li YM, He KZ, et al. Multi-omics reveal the efficient phosphate-solubilizing mechanism of bacteria on rocky soil. Front Microbiol. 2021;12:761972.

    PubMed  PubMed Central  Google Scholar 

  12. Scervino JM, Papinutti VL, Godoy MS, Rodriguez MA, Monica DI, Recchi M, et al. Medium pH, carbon and nitrogen concentrations modulate the phosphate solubilization efficiency of Penicillium purpurogenum through organic acid production. J Appl Microbiol. 2011;110(5):1215–23.

    PubMed  CAS  Google Scholar 

  13. Sarikhani MR, Khoshru B, Greiner R. Isolation and identification of temperature tolerant phosphate solubilizing bacteria as a potential microbial fertilizer. World J Microbiol Biotechnol. 2019;35(8):126.

    PubMed  Google Scholar 

  14. An R, Moe LA. Regulation of pyrroloquinoline quinone-dependent glucose dehydrogenase activity in the model rhizosphere-dwelling bacterium Pseudomonas putida KT2440. Appl Environ Microbiol. 2016;82(16):4955–64.

    PubMed  PubMed Central  CAS  Google Scholar 

  15. Li BH, Li GJ, Kronzucker HJ, Baluska F, Shi WM. Ammonium stress in Arabidopsis: signaling, genetic loci, and physiological targets. Trends Plant Sci. 2014;19(2):107–14.

    PubMed  CAS  Google Scholar 

  16. Zhu XF, Dong XY, Wu Q, Shen RF. Ammonium regulates Fe deficiency responses by enhancing nitric oxide signaling in Arabidopsis thaliana. Planta. 2019;250(4):1089–102.

    PubMed  CAS  Google Scholar 

  17. Emma FC, Gemma C, Pilar GA. Ammonium enhances resistance to salinity stress in citrus plants. J Plant Physiol. 2012;169(12):1183–91.

    Google Scholar 

  18. Ma SN, Wang HJ, Wang HZ, Li Y, Liu M, Liang XM, et al. High ammonium loading can increase alkaline phosphatase activity and promote sediment phosphorus release: a two-month mesocosm experiment. Water Res. 2018;145:388–97.

    PubMed  CAS  Google Scholar 

  19. Hachiya T, Inaba J, Wakazaki M, Sato M, Toyooka K, Miyagi A, et al. Excessive ammonium assimilation by plastidic glutamine synthetase causes ammonium toxicity in Arabidopsis thaliana. Nat Commun. 2021;12(1):4944.

    PubMed  PubMed Central  CAS  Google Scholar 

  20. Hachiya T, Watanabe CK, Fujimoto M, Ishikawa T, Takahara K, Kawai-Yamada M, et al. Nitrate addition alleviates ammonium toxicity without lessening ammonium accumulation, organic acid depletion and inorganic cation depletion in Arabidopsis thaliana shoots. Plant Cell Physiol. 2012;53(3):577–91.

    PubMed  CAS  Google Scholar 

  21. Aliyat FZ, Maldani M, Guilli ME, Nassiri L, Ibijbijen J. Phosphate-solubilizing bacteria isolated from phosphate solid sludge and their ability to solubilize three inorganic phosphate forms: aalcium, iron, and aluminum phosphates. Microorganisms. 2022;10(5):980.

    PubMed  PubMed Central  CAS  Google Scholar 

  22. Tian XP, Fang Y, Jin YL, Yi ZL, Li JM, Du AP, et al. Ammonium detoxification mechanism of ammonium-tolerant duckweed (Landoltia punctata) revealed by carbon and nitrogen metabolism under ammonium stress. Environ Pollut. 2021;277:116834.

    PubMed  CAS  Google Scholar 

  23. Meng S, Su L, Li YM, Wang YJ, Zhang CX, Zhao Z. Nitrate and ammonium contribute to the distinct nitrogen metabolism of Populus simonii during moderate salt stress. PLoS ONE. 2016;11(3):e0150354.

    PubMed  PubMed Central  Google Scholar 

  24. Luz DE, Nepomuceno RS, Spira B, Ferreira RC. The pst system of Streptococcus mutans is important for phosphate transport and adhesion to abiotic surfaces. Mol Oral Microbiol. 2012;27(3):172–81.

    PubMed  CAS  Google Scholar 

  25. Grafe M, Goers M, Tucher SV, Baum C, Zimmer D, Leinweber P, et al. Bacterial potentials for uptake, solubilization and mineralization of extracellular phosphorus in agricultural soils are highly stable under different fertilization regimes. Environ Microbiol Rep. 2018;10(3):320–27.

    PubMed  CAS  Google Scholar 

  26. Yuan ZC, Zaheer R, Finan TM. Regulation and properties of PstSCAB, a high-affinity, high-velocity phosphate transport system of Sinorhizobium meliloti. J Bacteriol. 2006;188(3):1089–102.

    PubMed  PubMed Central  CAS  Google Scholar 

  27. Luttmann D, Gopel Y, Gorke B. The phosphotransferase protein EIIANtr modulates the phosphate starvation response through interaction with histidine kinase PhoR in Escherichia coli. Mol Microbiol. 2012;86(1):96–110.

    PubMed  Google Scholar 

  28. Gosztolai A, Schumacher J, Behrends V, Bundy JG, Heydenreich F, Bennett MH, et al. GlnK facilitates the dynamic regulation of bacterial nitrogen assimilation. Biophys J. 2017;112(10):2219–30.

    PubMed  PubMed Central  CAS  Google Scholar 

  29. Smith DP, Thrash JC, Nicora CD, Lipton MS, Burnum-Johnson KE, Carini P, et al. Proteomic and transcriptomic analyses of “Candidatus Pelagibacter ubique” describe the first PII-independent response to nitrogen limitation in a free-living Alphaproteobacterium. mBio. 2013;4(6):e00133–12.

    PubMed  PubMed Central  Google Scholar 

  30. Bernard SM, Habash DZ. The importance of cytosolic glutamine synthetase in nitrogen assimilation and recycling. New Phytol. 2009;182(3):608–20.

    PubMed  CAS  Google Scholar 

  31. Wang F, Wang Q, Yu QG, Ye J, Gao J, Liu HT, et al. Is the NH4+-induced growth inhibition caused by the NH4+ form of the nitrogen source or by soil acidification? Front Plant Sci. 2022;13:968707.

    PubMed  PubMed Central  Google Scholar 

  32. Martin P, Dyhrman ST, Lomas MW, Poulton NJ, Van Mooy BAS. Accumulation and enhanced cycling of polyphosphate by Sargasso Sea plankton in response to low phosphorus. Proc Nat Acad Sci. 2014;111(22):8089–94.

    PubMed  PubMed Central  CAS  Google Scholar 

  33. Mirra B, Carvalho K, Curitiba B, Ribeiro L, Moraes J, da Silva JR, et al. Inorganic pyrophosphatase from the red flour beetle (Tribolium castaneum) modulates mitochondrial polyphosphate metabolism. Arch Insect Biochem Physiol. 2019;102(4):e21606.

    PubMed  CAS  Google Scholar 

  34. Wei YQ, Zhao Y, Shi MZ, Cao ZY, Lu Q, Yang TX, et al. Effect of organic acids production and bacterial community on the possible mechanism of phosphorus solubilization during composting with enriched phosphate-solubilizing bacteria inoculation. Bioresour Technol. 2018;247:190–9.

    PubMed  CAS  Google Scholar 

  35. Bhattacharyya C, Bakshi U, Mallick I, Mukherji S, Bera B, Ghosh A. Genome-guided insights into the plant growth promotion capabilities of the physiologically versatile Bacillus aryabhattai strain AB211. Front Microbiol. 2017;8:411.

    PubMed  PubMed Central  Google Scholar 

  36. Nelofer R, Syed Q, Nadeem M, Bashir F, Mazhar S, Hassan A. Isolation of phosphorus-solubilizing fungus from soil to supplement biofertilizer. Arab J Sci Eng. 2016;41(6):2131–8.

    CAS  Google Scholar 

  37. Chen HY, Chen YN, Wang HY, Liu ZT, Frommer WB, Ho CH. Feedback inhibition of AMT1 NH4+-transporters mediated by CIPK15 kinase. BMC Biol. 2020;18(1):196.

    PubMed  PubMed Central  Google Scholar 

  38. Sayavedra-Soto L, Ferrell R, Dobie M, Mellbye B, Chaplen F, Buchanan A, et al. Nitrobacter winogradskyi transcriptomic response to low and high ammonium concentrations. FEMS Microbiol Lett. 2015;362(3):1–7.

    PubMed  CAS  Google Scholar 

  39. Stein LY, Campbell MA, Klotz MG. Energy-mediated vs. ammonium-regulated gene expression in the obligate ammonia-oxidizing bacterium, Nitrosococcus oceani. Front Microbiol. 2013;4:277.

    PubMed  PubMed Central  Google Scholar 

  40. Hess DC, Lu W, Rabinowitz JD, Botstein D. Ammonium toxicity and potassium limitation in yeast. PLoS Biol. 2006;4(11):e351.

    PubMed  PubMed Central  Google Scholar 

  41. Kim M, Zhang ZG, Okano H, Yan DL, Groisman A, Hwa T. Need-based activation of ammonium uptake in Escherichia coli. Mol Syst biol. 2012;8:616.

    PubMed  PubMed Central  Google Scholar 

  42. Sathee L, Jha SK, Rajput OS, Singh D, Kumar S, Kumar A. Expression dynamics of genes encoding nitrate and ammonium assimilation enzymes in rice genotypes exposed to reproductive stage salinity stress. Plant Physiol Biochem. 2021;165:161–72.

    PubMed  CAS  Google Scholar 

  43. Burkovski A. Ammonium assimilation and nitrogen control in Corynebacterium glutamicum and its relatives: an example for new regulatory mechanisms in actinomycetes. FEMS Microbiol Rev. 2003;27(5):617–28.

    PubMed  CAS  Google Scholar 

  44. Hodges M. Enzyme redundancy and the importance of 2-oxoglutarate in plant ammonium assimilation. J Exp Bot. 2002;53(370):905–16.

    PubMed  CAS  Google Scholar 

  45. Gunka K, Commichau FM. Control of glutamate homeostasis in Bacillus subtilis: a complex interplay between ammonium assimilation, glutamate biosynthesis and degradation. Mol Microbiol. 2012;85(2):213–24.

    PubMed  CAS  Google Scholar 

  46. Rubio PJ, Godoy MS, Monica IF, Pettinari MJ, Godeas AM, Scervino JM. Carbon and nitrogen sources influence tricalcium phosphate solubilization and extracellular phosphatase activity by Talaromyces flavus. Curr Microbiol. 2016;72(1):41–7.

    Google Scholar 

  47. Wang SB, Li Y, Zhang J, Wang XY, Hong JP, Qiu C, et al. Transcriptome profiling analysis of phosphate-solubilizing mechanism of Pseudomonas strain W134. Microorganisms. 2022;10(10):1998.

    PubMed  PubMed Central  CAS  Google Scholar 

  48. Gulati A, Sharma N, Vyas P, Sood S, Rahi P, Pathania V, et al. Organic acid production and plant growth promotion as a function of phosphate solubilization by Acinetobacter rhizosphaerae strain BIHB 723 isolated from the cold deserts of the trans-himalayas. Arch Microbiol. 2010;192(11):975–83.

    PubMed  CAS  Google Scholar 

  49. Chiang CJ, Hu RC, Huang ZC, Chao YP. Production of succinic acid from amino acids in Escherichia coli. J Agric Food Chem. 2021;69(29):8172–8.

    PubMed  CAS  Google Scholar 

  50. Basak BB. Phosphorus release by low molecular weight organic acids from low-grade indian rock phosphate. Waste Biomass Valorization. 2019;10(11):3225–33.

    CAS  Google Scholar 

  51. Yuenyong W, Sirikantaramas S, Qu LJ, Buaboocha T. Isocitrate lyase plays important roles in plant salt tolerance. BMC Plant Biol. 2019;19(1):472.

    PubMed  PubMed Central  Google Scholar 

  52. Nie SQ, Zhang ZF, Mo SM, Li JH, He S, Kashif M, et al. Desulfobacterales stimulates nitrate reduction in the mangrove ecosystem of a subtropical gulf. Sci Total Environ. 2021;769:144562.

    PubMed  CAS  Google Scholar 

  53. Vazquez P, Holguin G, Puente ME, Lopez-Cortes A, Bashan Y. Phosphate-solubilizing microorganisms associated with the rhizosphere of mangroves in a semiarid coastal lagoon. Biol Fertil Soils. 2000;30(5–6):460–8.

    CAS  Google Scholar 

  54. Kashif M, Lu ZM, Sang YM, Yan B, Shah SJ, Khan S, et al. Whole-genome and transcriptome sequencing-based characterization of Bacillus Cereus NR1 from subtropical marine mangrove and its potential role in sulfur metabolism. Front Microbiol. 2022;13:856092.

    PubMed  PubMed Central  Google Scholar 

  55. Kanehisa M, Furumichi M, Sato Y, Kawashima M, Ishiguro-Watanabe M. KEGG for taxonomy-based analysis of pathways and genomes. Nucleic Acids Res. 2023;51(D1):D587–92.

    PubMed  CAS  Google Scholar 

  56. Kashif M, Sang YM, Mo SM, Rehman SE, Khan S, Khan MR, et al. Deciphering the biodesulfurization pathway employing marine mangrove Bacillus aryabhattai strain NM1-A2 according to whole genome sequencing and transcriptome analyses. Genomics. 2023;115(3):110635.

    PubMed  CAS  Google Scholar 

  57. Chen SF, Zhou YQ, Chen YR, Gu J. Fastp: an ultra-fast all-in-one FASTQ preprocessor. Bioinformatics. 2018;34(17):i884–90.

    PubMed  PubMed Central  Google Scholar 

Download references

Acknowledgements

The author expresses their special gratitude to all the funding sources for the financial assistance. The sediment samples in this study were obtained from the National Shankou Natural Reserve of Mangrove in Beihai, Guangxi, China, with permission from the National Shankou Natural Reserve of Mangrove.

Funding

This research was supported by the Natural Science Fund for Distinguished Young Scholars of Guangxi Zhuang Autonomous Region of China (Grant No. 2019GXNSFFA245011), the Fund Project of Chinese Central Government Guiding to the Guangxi Local Science and Technology Development (Grant No. GUIKEZY21195021), the Fund Project of Chinese Central Government Guiding to Nanning Local Science and Technology Development (Grant No. 20231012), the Fund Project of Technological Development from Angel Yeast (Chongzuo) Co. Ltd., and the Basic Research Fund of Guangxi Academy of Sciences (Grant No. CQ-C-202202).

Author information

Authors and Affiliations

Authors

Contributions

LZ and HS conceived and designed these experiments. HS, DL, and JC provided technical advice on the experiments, and LZ performed the experiments, analysed the sequencing data and wrote this manuscript. KM, ZZ, MS, and SG contributed to valuable discussions. Final manuscript read and endorsed by all authors.

Corresponding authors

Correspondence to Linfang Du or Chengjian Jiang.

Ethics declarations

Ethics approval and consent to participate

Not applicable.

Consent for publication

Not applicable.

Competing interests

The authors declare that they have no competing interests.

Additional information

Publisher’s Note

Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.

Electronic supplementary material

Below is the link to the electronic supplementary material.

Figure S1

: Chromatograms of six organic acids mixed standard solutions. The numbers 1, 2, 3, 4, 5 and 6 represent formic acid, malic acid, lactic acid, acetic acid, citric acid and succinic acid, respectively. Figure S2: Validation of key genes related to NH4+ assimilation and phosphate transport and metabolism by RT-qPCR. Table S1 Primers used for the amplification of 16S DNA of seven PSMs screened in this study [1]. Table S2 16S rDNA comparison results of seven PSMs screened in this study. Table S3 Chromatographic retention time, standard curve equation, and correlation coefficient of six organic acid mixed standard solutions. Table S4 The KEGG annotation results of genes relevant to NH4+ assimilation and phosphate transport and metabolism in B. aryabhattai NM1-A2 [2]. Table S5 Primers used in RT-qPCR.

Rights and permissions

Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/. The Creative Commons Public Domain Dedication waiver (http://creativecommons.org/publicdomain/zero/1.0/) applies to the data made available in this article, unless otherwise stated in a credit line to the data.

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Lu, Z., He, S., Kashif, M. et al. Effect of ammonium stress on phosphorus solubilization of a novel marine mangrove microorganism Bacillus aryabhattai NM1-A2 as revealed by integrated omics analysis. BMC Genomics 24, 550 (2023). https://doi.org/10.1186/s12864-023-09559-z

Download citation

  • Received:

  • Accepted:

  • Published:

  • DOI: https://doi.org/10.1186/s12864-023-09559-z

Keywords