Integrative analysis of the salt stress response in cyanobacteria

Stephan Klähn; Stefan Mikkat; Matthias Riediger; Jens Georg; Wolfgang R Hess; Martin Hagemann

doi:10.1186/s13062-021-00316-4

. 2021 Dec 14;16:26. doi: 10.1186/s13062-021-00316-4

Integrative analysis of the salt stress response in cyanobacteria

Stephan Klähn ^1,^2,^#, Stefan Mikkat ^3,^#, Matthias Riediger ², Jens Georg ², Wolfgang R Hess ², Martin Hagemann ^4,^5,^✉

PMCID: PMC8670252 PMID: 34906211

Abstract

Microorganisms evolved specific acclimation strategies to thrive in environments of high or fluctuating salinities. Here, salt acclimation in the model cyanobacterium Synechocystis sp. PCC 6803 was analyzed by integrating transcriptomic, proteomic and metabolomic data. A dynamic reorganization of the transcriptome occurred during the first hours after salt shock, e.g. involving the upregulation of genes to activate compatible solute biochemistry balancing osmotic pressure. The massive accumulation of glucosylglycerol then had a measurable impact on the overall carbon and nitrogen metabolism. In addition, we observed the coordinated induction of putative regulatory RNAs and of several proteins known for their involvement in other stress responses. Overall, salt-induced changes in the proteome and transcriptome showed good correlations, especially among the stably up-regulated proteins and their transcripts. We define an extended salt stimulon comprising proteins directly or indirectly related to compatible solute metabolism, ion and water movements, and a distinct set of regulatory RNAs involved in post-transcriptional regulation. Our comprehensive data set provides the basis for engineering cyanobacterial salt tolerance and to further understand its regulation.

Supplementary Information

The online version contains supplementary material available at 10.1186/s13062-021-00316-4.

Keywords: Compatible solute, Ion transport, Regulatory RNAs, Transcriptome-proteome correlation, Salinity stress response

Background

Salinity is a prominent environmental factor determining the natural distribution of microorganisms, as approximately 97% of the water resources contain more than 30 g salt (mainly sodium chloride) per liter. Accordingly, the capability of microorganisms to cope with high or changing salinities is crucial, not only in aquatic environments but also in terrestrial habitats, in which the alternation between evaporation and rainfall can rapidly change salt concentrations. In a hypersaline environment, in which the external salt concentration exceeds the cellular ion content, microorganisms have to manage two major challenges: (i) the low external water potential results in water loss from the cell and collapse of turgor pressure, and (ii) inorganic ions permeate into cells along the electrochemical gradient, which could compromise the structure of critical macromolecules. Accordingly, most microorganisms feature acclimation strategies aiming at maintaining a high water and low inorganic ion content in the cell. This so-called “salt-out” strategy is based on the active extrusion of inorganic ions accompanied by the accumulation of compatible solutes, i.e. highly soluble, non-toxic, low molecular-mass organic compounds, for osmotic equilibrium [29].

Cyanobacteria are a morphologically and physiologically diverse group of photoautotrophic bacteria that are found in nearly all light-exposed habitats including environments with different salinities such as freshwaters, oceans, and hypersaline ponds or soil surfaces in temperate and arid climates [105]. Previous studies of cyanobacterial salt tolerance revealed that those with low salt tolerance, mainly freshwater and soil cyanobacteria, accumulate the sugars sucrose and/or trehalose, those with moderate tolerance (mainly marine strains) synthesize the heteroside glucosylglycerol (GG), whereas halophilic strains (found in hypersaline habitats) usually contain glycine betaine [29, 80]. Some deviations from these preferences have been documented as well [43, 67, 69].

Cyanobacterial salt acclimation has been investigated in great detail using the model strain Synechocystis sp. PCC 6803 (Synechocystis 6803). This unicellular strain was originally isolated from a freshwater pond [94]. Nevertheless, Synechocystis 6803 represents a truly euryhaline organism able to grow in freshwater but also in media containing salt concentrations twice as high as in seawater [79]. The early availability of both, genetic tools [24] and the complete genome sequence [37] established Synechocystis 6803 as photoautotrophic model organism. Using this strain, the molecular basis of salt-induced GG synthesis has been characterized, which is performed by the enzymes GG-phosphate synthase and GG-phosphate phosphatase, encoded by the genes ggpS (sll1566) and ggpP (stpA, slr0746), respectively [26, 57]. Today, Synechocystis 6803 is the best investigated photoautotrophic prokaryote represented by more than 3700 scientific publications, and has become popular as chassis for the introduction of pathways for the photosynthetic production of biofuels or chemical feedstock (e.g. [30, 55, 56]). Salt-tolerant cyanobacterial strains such as Synechocystis 6803 also permit large scale cultivations in saline waters making the process more sustainable by avoiding competition for limited freshwater resources [7].

Over the past two decades, omics technologies have been applied to study salt acclimation of cyanobacteria, particularly Synechocystis 6803. Genome-wide transcriptome analyses revealed the differential expression of hundreds of genes after sudden increases in the external salinity and allowed the identification of several potential regulatory proteins involved in their stress-induced expression [38, 59, 91]. However, most of these genes were only transiently induced or repressed. In long-term salt-acclimated cells, the expression of only 39 genes remained significantly enhanced [60]. Later on, 2D-gel-based proteomics displayed a snapshot of the salt-regulated proteome, which identified 45 stably salt-induced soluble proteins [15], while 20 proteins of the membrane fraction appeared to be salt-regulated [34]. In the meantime, advanced omics technologies such as different RNA-seq technologies were established, which, for example, revealed that also large numbers of non-protein-coding RNAs (ncRNAs) are transcribed in Synechocystis 6803 [4, 48, 64]. Among them, two classes can be differentiated, cis-encoded antisense RNAs (asRNAs) transcribed from the opposite strand within protein-coding genes, and trans-encoded small regulatory RNAs (sRNAs) [23, 49]. Some of the newly annotated asRNAs were demonstrated to act as regulators of their cognate mRNAs or sRNAs functioning in the acclimation response to changing environmental conditions [12, 21, 45, 85, 107]. Moreover, tremendous progress has been made in the investigation of cyanobacteria using gel-free technologies for proteomics [17, 93, 103] or metabolomics (reviewed by [87]).

Here, we combined transcriptomic with proteomic and metabolomic approaches for a comprehensive characterization of the salt acclimation process in Synechocystis 6803. Previous studies showed that salt acclimation is a highly dynamic process, in which many genes/proteins showed an early but mostly transient response before long-term salt acclimation leads to stable, physiological meaningful changes in the gene/protein expression pattern. Therefore, we sampled Synechocystis 6803 cells at different time points up to 7 days after transfer from NaCl-free into medium containing 684 mM NaCl (equal to 4% NaCl). In addition to many salt-regulated proteins and their corresponding mRNAs, we identified several potentially regulatory asRNAs and sRNAs to be salt-stimulated as well. Finally, metabolomics revealed that the massive accumulation of the compatible solute GG has a broader impact on the overall primary carbon and nitrogen metabolism.

Results

The response of Synechocystis 6803 to NaCl-induced hyperosmotic conditions (salt stress) was analyzed on transcriptome, proteome and metabolome levels at different time scales (Fig. 1). Changes in the expression profiles were first analyzed at a global scale. Then, selected examples were examined in a comprehensive way using all data sets.

Fig. 1 — Overview on the applied approaches and conditions. Samples for microarray, proteome, and metabolome analyses were taken from cultures sparked with CO₂-enriched air (5% [v/v]). Sampling points for each experiment are given in the panels. Further details about cultivation, salt treatment and sample processing are given in the “Materials and methods” section

Global transcriptome analysis

In the present study a microarray platform was used to detect RNA levels directly, without reverse transcription. This microarray contained probes for all protein-coding genes also covering so far non-annotated open reading frames as well as for ncRNAs such as cis-acting asRNAs and trans-acting sRNAs previously identified in Synechocystis 6803 [48, 64]. In total the microarray covered 3364 mRNAs, 1940 asRNAs and 602 sRNA candidates. Previous studies analyzing the salt transcriptome of Synechocystis 6803 used DNA microarrays only covering 3079 mRNAs and no ncRNAs [60]. Here, the microarray was hybridized with total RNA extracted from control cells (0% NaCl) and from cells exposed to 4% of NaCl for 0.5, 2, and 24 h. The time points were chosen to permit comparison with previously published microarray data [60]. Gene expression changes along the Synechocystis 6803 chromosome are shown in the Additional file 2: Genome Plots.

For the selection of differentially expressed genes, we applied the widely used cut-off criteria, i.e. log₂ fold change ≥ │1│, p-value < 0.05. As the transcriptome composition was highly dynamic at the different time points, we first focused on protein coding genes (mRNAs). Compared to control conditions (i.e., cells grown in NaCl-free BG11 medium), several hundred mRNAs showed a changed abundance 0.5 and 2 h after salt addition, while after 24 h only 87 were up- and 31 down-regulated (Table 1; volcano plots of transcriptional changes are displayed in Additional file 3: Fig. S1), consistent with the previous report [60]. Only a few mRNAs were significantly changed at all sampling points, i.e. 31 showed elevated levels and 19 were down-regulated.

Table 1.

Global analysis of protein-coding genes showing altered transcript levels after salt shock of 684 mM NaCl

	Time after salt shock	Marin et al. [60]	Billis et al. [4]	This study
Up-regulated mRNAs	0.5 h	652	n.a	382
	2 h	477	n.a	458
	24 h	48	133	87
Down-regulated mRNAs	0.5 h	329	n.a	407
	2 h	268	n.a	574
	24 h	48	368	31

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A gene was regarded as induced or repressed if the log₂ fold change was higher or lower than 1 or − 1 (P value < 0.05; n.a.—not analyzed)

To evaluate the microarray data set systematically, a cluster analysis was performed using mfuzz [50]. Initially, 8538 transcript types were differentiated, including all mRNAs but also 5’UTRs, asRNAs, sRNAs and transcripts derived from start sites within genes; Additional file 1: Table S2). Two clusters (cluster 1 and 2) include transcripts that were induced and two other clusters (cluster 3 and 4) include transcripts that were repressed at specific time points after salt addition (Fig. 2A). Transcripts in cluster 1 and 3 peaked at 0.5 h, while transcripts in cluster 2 and 4 peaked at the 2 h time point. The majority of genes in all clusters, most pronounced in case of cluster 3, showed a clear tendency to return to the initial values at the end of the time course indicating that the short-term acclimation was complete.

Fig. 2 — Cluster analysis of the salt stress microarray time series. A Four major clusters of co-regulated transcripts were obtained. B Distribution of different transcript types over the different clusters (see Additional file 1: Table S2 for the precise values and assignments). C Functional enrichment analysis of proteins encoded by differentially regulated mRNAs according to KEGG Orthology (KO) terms for each cluster. Heatmap coloring represents the enrichment p-values (y axis = enriched KO terms, x axis = genes, see Additional file 1: Table S3 for detailed information)

Specific transcript types showed an uneven distribution in the different clusters, i.e. clusters 1 and 2 contain a significantly higher number of asRNAs and lower number of sRNAs while cluster 3 and 4 showed the opposite. Protein-coding transcripts are more present in the downregulated clusters (780 mRNAs) than in the upregulated clusters (690 mRNAs) (Fig. 2B). Functional enrichment analysis of the proteins encoded by mRNAs in each cluster was performed according to annotations from KEGG Orthology (KO) terms. On the one hand, mRNAs within the rapidly induced cluster 1 are enriched in proteins associated to replication and repair, cofactor biosynthesis, signaling, and transport, while the mRNAs of cluster 2 are enriched in protein families associated to transport, genetic information processing such as chaperones and folding catalysts, ribosome biogenesis, or transcription factors (Fig. 2C). On the other hand, transiently repressed mRNAs in the clusters 3 and 4 showed similar functionalities, and thus were analyzed jointly. The most pronounced functional enrichment could be seen for transcripts encoding proteins associated to energy and metabolism, such as oxidative phosphorylation, photosynthesis, nitrogen metabolism, or related metabolic functions, such as pathways of porphyrin and chlorophyll metabolism, lipid biosynthesis or pathways for carbon metabolism.

Salt-regulated asRNA:mRNA pairs

Most of the salt-induced changes of asRNA levels were transient, consistent with the observations for mRNAs. Our analysis considered only asRNAs that overlap on the opposite strand with the respective mRNAs, which led to the identification of 79 inversely regulated and 82 co-regulated asRNA/mRNA pairs (Fig. 3) at a Pearson correlation coefficient ≥ │0.65│ (details in Table S4). Previous work in Synechocystis 6803 showed that both modes of regulation can be functionally relevant [12, 13, 85].

Among the asRNA/mRNA pairs is sll1862 (Fig. 3D) encoding one of the most abundant salt shock proteins (see below). The massive accumulation of stress protein Sll1862 is correlated by the inversely related levels of its mRNA versus asRNA. Another asRNA seems to be involved in controlling the salt-stimulated expression of slr0082 (Fig. 3D), which encodes the ribosomal protein S12 methylthiotransferase RimO. This gene was early detected to be salt-induced by subtractive hybridization [101]. It is transcribed in an operon together with the RNA helicase CrhR, which has been shown to be involved in multiple stress responses and is regulated by redox changes [83]. Moreover, the mRNA level of sll0923 encoding the tyrosine kinase Wzc was less abundant after salt addition (Wzc protein level was lowered with a FC of 0.53), while the corresponding asRNA showed increased abundance (Fig. 3C). Wzc is involved in the synthesis of extracellular polysaccharides (EPS) [73], hence, the lowered expression of sll0923 is consistent with observation of reduced EPS synthesis in salt-acclimated Synechocystis 6803 cells [40]. Among the 56 mRNA/asRNA pairs showing similar induction patterns, the gene slr0953 encoding sucrose-phosphate phosphatase showed higher mRNA as well as asRNA levels (Fig. 3E). It could be assumed that in this case the asRNA supports the stability of the slr0953 mRNA contributing to the transiently elevated sucrose levels in salt-treated cells.

Moreover, we identified also not previously known salt-regulated transcripts, e.g. the sll1470 asRNA (Fig. 3). Although this asRNA originates from a TSS downstream of sll1470, it overlaps the 3’ end of the gene and a clear anti-correlation with the transcript accumulation of sll1470 during salt shock was detected (Fig. 3C). Gene sll1470 encodes the large subunit of 3-isopropylmalate dehydratase, an important enzyme connecting pyruvate metabolism with leucine/isoleucine/valine biosynthesis. Therefore, its lowered expression during early salt shock likely contributes to the metabolic reorganization towards synthesizing GG consistent with the lowered valine accumulation (see below).

Salt-regulated sRNAs

The used microarray also permitted to search for salt-induced changes in the abundance of sRNAs, which are in contrast to asRNAs encoded in trans. Interestingly, according to the cluster analysis (Fig. 2), both ncRNAs types responded differently to the salinity increase: asRNAs were mainly upregulated (cluster 1 and 2) while sRNAs were mainly downregulated (cluster 3 and 4). The salt-induced sRNA patterns, were again highly dynamic and mainly transient. For example, the sRNA IsaR1 was found to be transiently up-regulated in response to salt but returned to control levels in long-term salt acclimated cells (Additional file 1: Table S1). IsaR1 is a key player in the acclimation of the photosynthetic apparatus to iron starvation by targeting several mRNAs encoding Fe²⁺-containing proteins and enzymes involved in pigment and FeS cluster biosynthesis [22]. In addition to its role in iron acclimation, IsaR1 controls directly the synthesis of a key enzyme in GG synthesis, GgpS at the post-transcriptional level early during salt acclimation [84].

Altogether, eleven sRNA candidates were found to be differentially expressed at all-time points, three candidates were up- and 8 were down-regulated (Additional file 1: Table S5). Their potential roles in the salt acclimation process is an interesting topic for future research.

Global evaluation of the proteome in salt-acclimated cells

Proteome analyses using data-independent acquisition mass spectrometry (HDMS^E) were performed with extracts from cells cultivated at either 0% NaCl (control cultures) or 4% NaCl (7 days’ salt-acclimated cultures, Fig. 1). To improve coverage and to obtain additional information on cellular localization, the proteome of different fractions was analyzed: 1. Total protein extracts obtained without any centrifugation; 2. The debris fraction obtained after low speed centrifugation (yellowish brown pellet); 3. The soluble fraction representing the blueish supernatant after high-speed centrifugation; and, 4. The membrane-enriched fraction representing the washed green pellets after high-speed centrifugation (further details are described in the Additional file 3).

In total, 1816 proteins, approximately 52% of the entire proteome of Synechocystis 6803 in the UniProt database, were identified by at least two tryptic peptides per protein (Additional file 1: Table S6). In particular, 1253 proteins were found in the total extracts and 823 in the soluble fraction, while 1608 and 1421 proteins were identified in the membrane-enriched and debris fractions, respectively (Fig. 4). Similar to previous reports on the Synechocystis 6803 proteome [17], many proteins (79%) were found in both, the soluble as well as the membrane fractions, although the membrane pellet was washed with high salt and high pH buffers. The occurrence of proteins in different fractions clearly correlates with their numbers of transmembrane helices (Additional file 3: Fig. S2). In the present study, we also investigated the cell debris that is usually removed from proteome analyses if cellular fractionation is performed. The vast majority (96.3%) of proteins in this fraction was also identified in the membrane-enriched fraction. However, 29 proteins were exclusively found in the debris fraction, for example the large Slr1567 protein, a putative outer membrane protein (Additional file 1: Table S7). Many other proteins enriched in the debris fraction are annotated as components of the cell envelope or of the outer membrane-bound periplasmic space.

Salt-dependent changes in protein abundances were evaluated in total protein extracts as well as three subcellular fractions (Fig. 4). For the selection of differentially expressed proteins cut-off criteria were defined by a fold change of ≥ │1.5│ and a corresponding p-value < 0.05. However, for a large number of proteins less pronounced fold change values were also statistically significant. The volcano plots indicate that the group of stably up-regulated proteins (Additional file 3: Fig. S3) displayed larger fold changes than down-regulated proteins, resembling the observations made with the transcriptomic data (Additional file 3: Fig. S1).

Next, we analyzed whether or not particular proteins showed consistent salt-related changes in the different proteome fractions. For most proteins, well-matching values were found in the different fractions and in the total extract. However, in some cases the relative abundances showed an inverse relation in membrane and soluble fractions. For example, many ribosomal proteins occurred in lower amounts in the soluble fraction but were elevated in the membrane and debris fractions of salt-acclimated cells compared to control cells (Additional file 3: Fig. S4). Similar patterns were found, among others, for the subunits of the ATP synthase, the phycobilisome linker polypeptides, and the RNA polymerase. These results indicate cultivation-dependent differences in the distribution of proteins to the different cellular fractions as reported in other studies [18, 72]. In our case, some protein complexes such as ribosomes might be more stable under high salt conditions, resulting in their enrichment in the membrane fraction and depletion in the soluble fraction. To deal with this situation, we calculated a weighted fold change from the subcellular fractions data of each protein and showed that it was highly concordant with the corresponding fold change from the total protein extract (Additional file 3: Fig. S5; more detailed description is given in the Additional file 3). Finally, the mean value of the weighted fold change from the subcellular fractions and the fold change from the total protein extract was used. If only one of these two values was available, it was used directly as final fold change. This led to a list of 1803 proteins, to which two membrane proteins were appended that are known (Slr0531) or suspected (Sll1037) to be important for salt acclimation, but were identified by individual peptides only. As a final result, 190 proteins were up-regulated and 189 protein down-regulated 7 days after salt shock among the 1805 quantified proteins (Additional file 1: Table S6).

Correlation analysis of salt-stimulated transcriptome and proteome

A correlation analysis was performed to analyze the overall relation between transcriptomic (log₂ fold changes of mRNA after 24 h) and proteomic changes (log₂ fold changes of protein abundances after 7 d). 1749 transcript/protein pairs could be matched (Fig. 5; Additional file 1: Table S8). The Pearson correlation coefficient for the proteomic and transcriptomic data sets was r = 0.58 indicating a close relationship, especially taking into consideration that sampling was done in different laboratories and at different time points. To grade the correlation between the newly acquired transcriptomic and proteomic data sets, we also compared our proteome data to the previously published transcriptome data sets [4, 60]. In both cases, lower correlation coefficients of r = 0.41 and r = 0.42, respectively, were obtained. Next, we calculated the correlation coefficients between our transcriptome data and the previous transcriptome data [4, 60] using the same subset of mRNAs as for the comparison with the proteome. Surprisingly, the obtained coefficients of r = 0.49 and r = 0.50 showed a slightly lower correlation between different transcriptomic data sets than correlation between the proteomic and the present transcriptomic data set (Fig. 5C). These findings indicate that culture conditions significantly influence the comparability of different data. Nevertheless, in all cases a close correlation was observed for the expression of genes that are of direct importance for salt acclimation, while the expression of other genes can vary depending on small differences between the culture conditions leading to relatively low Pearson correlation coefficients.

Fig. 5 — Correlation between transcriptome (24 h) and proteome (7 d) dynamics in response to high salt conditions. A Data originate from the present study. B The newly obtained proteome data were compared with the previous transcriptomic study [60]. Scatterplots display the correlation of protein and transcript ratios. 1749 transcripts with reported fold changes could be mapped to corresponding changes in protein abundances. Matches with ratio differences below log₂ 1.5-fold changes were considered to be similar. C Table displaying Person’s correlation coefficients between the different data sets (data from this study and from previously reported data sets [4, 60]).

Detailed examination of specific processes

Compatible solute metabolism and transport constitutes a salt-specific stimulon

Central to salt acclimation of Synechocystis 6803 is the accumulation of the main compatible solute GG, because mutants affected in the genes ggpS and ggpP (stpA) encoding the GG synthesis enzymes showed the highest degree of salt sensitivity compared to wild type [26, 57]. As initially found [79], salt-acclimated cells accumulate high amounts of the compatible solute GG, which represents the by far largest pool of low molecular mass organic compounds. The amount of GG is approximately 2000times higher in salt-grown cells compared to the trace amounts of GG in control cells (Fig. 6C). The second compatible solute sucrose is approximately 1000-fold less abundant (0.28 nmol OD₇₅₀⁻¹ ml⁻¹) than GG in salt-acclimated cells (Additional file 1: Table S10), because it mainly plays a role as transiently accumulated osmolyte after salt shocks in Synechocystis 6803 [41].

Fig. 6 — Salt-dependent up-regulation of the GG synthesis key enzyme, GG-phosphate synthase (GgpS). A Northern-blot showing accumulation kinetics of the *ggpS* transcript in response to salt shock of 4% [w/v] NaCl. Relative abundances were calculated after densitometric evaluation of the blot signals (signal obtained for 6 h was set as maximum, 100%). B Western blot confirming increased GgpS abundance in cells acclimated to 4% NaCl. Relative abundance was calculated after densitometric evaluation of blot signals (signal from control cells was set as 1). Data are the mean ± SD of values obtained from three individual blots. C Intracellular accumulation of GG in cells acclimated for 7 days to 4% NaCl. Data are the mean ± SD of 6 replicates

Corresponding to the high GG accumulation, the GgpS and GgpP proteins and mRNAs showed significantly elevated levels (Table 2), which is supported for GgpS by Northern- and Western-blotting (Fig. 6A, B). The sucrose synthesis enzymes Sps and Spp also exceeded the threshold for significant protein changes (Table 2), whereas the sps mRNA was only transiently increased (Additional file 1: Table S1) consistent with the transient accumulation profile of sucrose [41]. The ggpS downstream gene glpD encoding glycerol 3-phosphate dehydrogenase, which is involved in the synthesis of the GG precursor glycerol 3-phosphate (G3P) from dihydroxyacetone phosphate, is also salt-stimulated. Overlapping with the ggpS promoter region exist the small ORF ssl3076 that encodes for the ggpS repressor GgpR [44], which could not be detected in the proteome. Upstream of ggpS on the opposite strand, the genes for the GG hydrolase (GghA) and glycerol kinase (GlpK), the latter is involved in synthesis of the GG precursor G3P from glycerol, are located. They show similar expression pattern as ggpS. In contrast to the salt induction of genes for G3P synthesis, the glgC gene encoding the enzyme for ADP-glucose synthesis, the second precursor for GG, is not salt-regulated on RNA or protein levels. However, we cannot rule that the protein is biochemical activated under salt conditions to match the possible elevated demand of ADP-glucose synthesis.

Table 2.

Expression of proteins involved in compatible solute metabolism and transport

Gene	Protein function	Proteome	Transcriptome	Cluster*
sll1566	Glucosylglycerol-phosphate synthase (GGPS)	2.92	3.85	2
slr0746	Glucosylglycerol-phosphate phosphatase (GGPP)	1.19	1.48	2
sll1085	Glycerol-3-phosphate dehydrogenase (GlpD)	2.55	0.71	2
slr1672	Glycerol kinase (GlpK)	2.14	2.71	2
slr0747	ATP-binding subunit of GG transporter (GgtA)	1.83	2.43	2
slr0529	Substrate-binding subunit of GG transporter (GgtB)	1.33	1.48	2
slr0531	Integral membrane protein of GG transporter (GgtD)	2.02	2.13	2
slr1670	Glucosylglycerol degrading enzyme (GghA)	1.89	2.95	2
sll0045	Sucrose-phosphate synthase (Sps)	1.22	0.46	2
slr0953	Sucrose-phosphate phosphatase (Spp)	1.04	1.26	2

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Given are log₂ fold changes of their levels in cells exposed for 7 d (proteome) or 24 h (transcriptome) to 684 mM NaCl versus control cells

*According to Cluster analysis shown in Fig. 2

Immediately downstream of ggpP, the salt-induced GgtA protein is encoded that acts as the ATP-binding subunit of the GG transporter (Ggt). The genes for the other Ggt subunits, GgtB, C and D (two of them were identified among the salt-stimulated proteins) form a separate salt-induced operon. The co-regulation of genes and proteins for GG synthesis and the ABC-type osmolyte transporter Ggt, which all belong to the cluster 2 (Table 2), indicates their functional cooperation in salt-acclimated cells, in which the transporter is mainly responsible for the avoidance of GG (and sucrose) leakage from the cells [63]. However, the GG hydrolase GghA (Slr1670), which degrades GG into glucose and glycerol after hypo-osmotic treatments [40], showed also enhanced expression on mRNA and protein level in salt-acclimated cells. It has been discussed that the GG synthesis and degradation are mainly regulated at enzyme activity level that are differentially affected by cellular ion contents; elevated internal ion content leads to biochemical activation of GG synthesis and inactivation of GG cleavage [41]. Hence, the increased amounts of putatively biochemically inactive GghA protein likely prepares Synechocystis 6803 cells for sudden decreases in osmolarity. It should be noted that the GgpP and GlpD proteins involved in GG synthesis were not detected in the soluble but exclusively in the membrane-associated fraction. This localization could indicate that these proteins might be involved in additional processes such as fatty acid (GlpD) or EPS (GgpP) syntheses [40].

Finally, the salt-induced proteins involved in GG metabolism and transport as well as in G3P synthesis are obviously part of a larger group of salt-induced genes/proteins in Synechocystis 6803, which presumably can form a salt-regulon. Using ggpS as search string in the CyanoExpress database, which compiles gene expression data sets from Synechocystis 6803 [33], revealed more than 30 genes showing similar expression pattern under different environmental stimuli (Additional file 3: Fig. S6). The occurrence of all genes related to GG biochemistry, which are proven to be involved in salt acclimation, make it very probable that several of the co-regulated genes encode proteins also specific for this stress acclimation. This assumption is supported by our finding that many of these proteins also accumulated to higher levels in salt-acclimated cells. In cases where the protein levels were not significantly elevated, the corresponding gene showed only transient stimulation at the earliest time points after salt addition (Additional file 3: Fig. S6).

Transporters and channels belonging to the salt-specific stimulon

Clustering and functional enrichment analyses clearly indicated that differential regulation of proteins related to membrane transport is generally an important mechanism for salt acclimation (Additional file 1: Table S9). Among them, the mechanosensitive channel protein of small conductance (MscS) Slr0639 accumulated to the highest level, fold change of 14.3 (RNA approximately twofold) (Additional file 1: Table S6; Fig. 7). Two other MscS proteins, Slr0765 and Sll1040 were identified at elevated protein and RNA levels as well. Msc proteins are important for proper acclimation to hypo-osmotic treatments to facilitate quick release of compatible solutes and to prevent burst of cells [51]. Hence, similar to elevated GghA, the MscS accumulation likely prepares the cell for upcoming events of lower osmotic pressure as safety valves as has been also shown in many heterotrophic bacteria [74, 95]. In contrast, the abundance of MscL (Slr0875), which is involved in water movements after sudden osmotic shocks on Synechocystis 6803 [2, 88], did not change in long-term salt-acclimated cells.

Na⁺/H⁺ antiporters are considered as main exporters of excess Na⁺ and, therefore, play a crucial role for salt acclimation [29]. The Synechocystis 6803 genome codes for six Na⁺/H⁺ antiporters, five of them were identified in the proteome. Among them, the protein abundance of NhaS2 and NhaS5 was significantly enhanced in salt-acclimated cells (Fig. 7), whereas the amount of NhaS3, which is essential for cell viability and was discussed to be mainly responsible for Na⁺ export [14, 104], remained unchanged (Additional file 1: Table S6). However, the fact that the abundance of a protein remains unchanged does not exclude an essential function of this protein for salt acclimation, because it could be regulated on biochemical level according to cellular demands. While crucial roles were assigned to NhaS2 under low Na⁺/K⁺ ratios [62] or growth at different pH values, the nhaS5 mutant did not show any changes compared to wild type [14, 104]. Unfortunately, none of the previously discussed candidates for chloride exporters (Sll1864, Slr0753, Sll0855) [29] could be identified in our proteome data set. Among them, only the gene sll1864 was transiently stronger expressed on mRNA level in salt-shocked cells (Additional file 1: Table S1).

In addition, several other proteins potentially involved in ion transport were found in higher abundances in salt-acclimated cells (Fig. 7). For example, two of the 7 annotated cation-transporting ATPases [104] were elevated in the proteome (Slr1950 with FC 1.8 and Sll1614 with FC 1.68) and two hours after salt shock in the transcriptome as well. Furthermore, the amount of the protein Slr1257, which comprises a ligand-gated ion channel domain, increased fourfold, whereas the corresponding mRNA was slightly below the threshold of twofold in salt-acclimated cells. Many other transport proteins such as Slr0798 (Zinc-transporting ATPase, FC 1.64), Sll0615 (GDT1-like, possible Ca²⁺/H⁺ antiporter, FC 1.59) or those involved in uptake of nutrients such as nitrate, phosphate, or magnesium were also present in higher amounts in salt-acclimated cells (Additional file 1: Tables S6, S9). Finally, several transporters involved in iron uptake are transiently up-regulated at mRNA level, which indicates that the transient influx of high NaCl amounts in the cells somehow interferes with the general ion homeostasis including iron availability. However, their expression returned to control mRNA as well as protein levels after long-term salt acclimation (Fig. 7).

Many salt-induced proteins are involved in general stress response

Two proteins of unknown function, Sll1862 and Sll1863 showed 9.9- and 13.3-fold, respectively, higher abundances in salt-acclimated cells (Table 3). Searches using CyanoExpress [33] revealed that these proteins are induced on mRNA level not only after salt stress but also in response to many other stress treatments, hence, they belong to the group of general stress proteins. The Sll1863 protein was previously identified as the top salt-induced gene/protein [15], while in the present study it shares the top four positions with Sll1862 and two MscS proteins, which were not previously quantified. The induction of Sll1862 and Sll1863 also led to high total protein amounts in salt-acclimated cells, both of them belong to the 60 most abundant proteins. However, their inactivation by interposon mutagenesis did not result in a salt-sensitive phenotype (unpublished results of Hagemann group).

Table 3.

Salt-regulated proteins that are involved in general stress tolerance

Gene	Protein function	Proteome	Transcriptome
Gene	Protein function	7 d	24 h	2 h	0.5 h
sll1863	Unknown protein	3.73	5.18	7.47	7.49
sll1862	Unknown function	3.30	4.00	5.28	5.30
sll1037	Putative component of TRAP transporter	3.01	0.63	0.17	0.38
slr0750	Light-independent protochlorophyllide reductase subunit N	3.00	1.29	− 1.88	− 0.86
slr0786	Methionine aminopeptidase B	2.83	4.77	5.32	0.95
slr0967	Hypothetical protein, involved in stress responses	2.43	3.00	3.28	0.27
Sll0528	Putative zinc metalloprotease	2.43	4.19	6.22	1.61
sll7064	CRISPR-Cas system 2	2.18	0.57	− 2.56	− 1.00
sll0248	Flavodoxin (IsiB)	2.15	1.15	4.27	0.89
sll1988	33 kDa chaperonin (HSP33)	2.06	0.42	0.21	0.35
sll0947	Light-repressed protein A, LrpA	1.83	− 1.69	− 2.54	0.84
slr2019	Putative ATP binding subunit of ABC transporter	1.79	2.13	− 0.33	− 0.11
slr1894	General stress protein MrgA/Dps	0.94	1.06	2.09	1.16
sll1514	16.6 kDa small heat shock protein, molecular chaperon	− 1.68	0.91	5.85	4.25

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Given are log₂ fold changes of their protein and corresponding mRNA levels in cells exposed for different times to 684 mM NaCl versus control cells

Several heat-shock proteins that are involved in protein folding and repair have been previously identified among the salt-induced, general stress proteins [15]. In the present study, only the 33 kDa chaperone (Sll1988) was more than twofold accumulated while its mRNA showed only a slight increase, whereas the amounts of DnaK, GroEL, or DnaJ proteins were not significantly changed. Moreover, the small, 16.6 kDa heat shock protein (Sll1514) was decreased despite its RNA accumulated after the salt addition (Table 3), whereas it was found before in significant enhanced amounts in salt-acclimated cells [15]. These differences most probably result from different cultivation conditions and sampling times in the different studies. Many other salt-stimulated proteins have no functional annotations, however, the proteins Slr0967, Slr2019, Sll0528, and Sll0947 were all also implicated in multiple stress responses of Synechocystis 6803 [16, 52, 61, 100].

Moreover, an overlap between salt stress and iron-starvation response has been often observed, because in previous studies many genes/proteins serving as markers for iron-starvation have been observed in elevated amounts in salt-stressed cells as well [15, 60]. In the present study, many proteins related to iron transport are found at higher mRNA levels in the early time points (Fig. 7, Additional file 1: Table S1). However, in long-term acclimated cells only two iron-regulated proteins are significantly elevated (Table 3). The general stress protein Slr1894, which is annotated as MrgA or Dps like protein, was found in higher abundances in salt-acclimated cells. It has been shown to be involved in oxidative stress response [53] or in the mobilization of iron-storage after transfer from iron-replete into iron-deplete conditions [89]. Furthermore, flavodoxin (isiB) is clearly accumulated, which plays an important role in the salt-stimulated photosynthetic cyclic electron transport [27].

Salt effects on proteins involved in the basic cell physiology

Previous transcriptome analysis revealed that genes encoding subunits of protein complexes are co-regulated in salt-stressed cells [60]. The evaluation of the proteome data showed that the abundances of most proteins belonging to the photosystem (PS) I and II, phycobilisomes, ribosomes, or enzymes of the tricarboxylic acid (TCA) cycle were slightly lower after long-term salt acclimation (Fig. 8). Only a few exceptions were found. The Psb28 protein of PSII was elevated (FC 1.8). This subunit is involved in PSII assembly and repair [66], thus its higher amount could indicate that the PSII is less stable in salt-acclimated cells. As another example, the transcript levels of sll1471 encoding the CpcG2 phycobilisome rod-core linker polypeptide was strongly reduced in the microarray dataset upon short term salt stress and exhibited a lowered protein level (log₂ FC of -0.42) as well. CpcG2 is the rod core linker of the smaller CpcL-phycobilisome type [47, 55, 56], which has been implicated in the formation of a PSI/NDH supercomplex in Synechocystis 6803 [19]. Furthermore, alpha phycocyanobilin lyase (CpcF, sll1051), a protein involved in phycobiliprotein assembly into phycobilisomes, increased 1.7-fold. Another phycocyanobilin lyase (CpcE, slr1878) was also increased. Finally, many ribosomal proteins showed a tendency to slightly lowered amounts (Fig. 8), which correlates with the slower growth of salt-acclimated cells [25]. The results show that cells acclimated to 684 mM NaCl for 7 days have reached a new steady state, in which many basic physiological processes differ from the control cultures. Regarding basic cellular processes our current transcriptome data of salt-shocked cells after 24 h showed a high agreement with the proteome data.

Fig. 8 — Influence of the salinity on basic cellular processes. Log₂ fold change values (salt-acclimated/control) from the identified protein components of the indicated processes are plotted vertically aligned

The potential impact of high salinity on the cell surface of Synechocystis 6803 cells is indicated by the observation that 8 salt-induced proteins were found among the 19 identified proteins of the functional category „Murein sacculus and peptidoglycan “. These proteins include MurF (Slr1351), DacB (Slr0804), MurA (Slr0017), MurG (slr1656) and MltA (Sll0016), which all are enzymes probably involved in cell wall or cell envelope biogenesis (Additional file 1: Table S6). Their coordinated up-regulation indicates that salt stress induces a reorganization of cell wall structures, which possibly decrease its permeability for inorganic ions. Changed abundances of several further proteins involved in the reorganization of the cell surface support this assumption. The lowered abundance of Wzc (Sll0923) is consistent with the lowered amount of EPS of salt-acclimated cells [40]. Some of the most giant proteins encoded in the Synechocystis 6803 genome that are believed to have functions in the cell envelope, such as the 192 kDa protein Sll0723 (FC 3.9) and the 214 kDa protein Sll1265 (FC 1.6) accumulated in salt-acclimated cells. However, in contrast to the proteins participating in salt-regulated compatible solute synthesis or ion transport, a lower correlation between mRNA and protein abundances was found for the proteins involved cell envelope related processes.

Differential expression of regulator proteins

Regulatory proteins are highly important for stress acclimation, but were underrepresented in the proteome data. Only three out of 86 identified regulatory proteins showed significantly elevated protein but not increased mRNA levels in our study. All three represent different members of two-component regulatory systems (Sll1624—Rre18, Slr1324—Hik 23, Slr6110—Rre on plasmid pSYSX). However, none of them is functionally characterized and none of the previously identified salt-stress-associated two-component regulators [58, 91] showed higher protein amounts here. Further 15 proteins among the 86 identified regulatory proteins were found with lower abundances in salt-acclimated cells, mostly in concordance to their mRNAs.

The list of genes co-regulated with ggpS and other genes/proteins for the GG biochemistry included one transcription factor, PrqR (Slr0895; Additional file 3: Fig. S6). Hence, it is tempting to speculate that PrqR might be involved in the salt-stimulated expression of ggpS and other genes in this putative regulon. PrqR was reported as repressor for genes involved in glucose metabolism and oxidative stress acclimation [39]. The LexA protein, which is not changed on protein level but became significantly decreased on RNA level (Additional file 3: Fig. S7), has been shown to act as negative regulator of GgpS and GgpP expression [97]. However, the fact that the abundance of a protein remains unchanged does not exclude an important function of this protein for salt acclimation, because especially regulatory proteins are often activated/inactivated upon association with other proteins or metabolic signals. Moreover, the expression of genes for other annotated transcription factor changed. For example, the gene sll0998 encoding the transcription factor RbcR, which regulates the expression of the key CO₂-fixing enzyme ribulose 1,5 bisphosphate carboxylase/oxygenase (RubisCO), showed lower abundances on protein and RNA levels in salt-acclimated cells. Albeit not passing our significance criteria, both the large and small subunit of RubisCO were reduced by 20–30% that could indeed result in lower CO₂-fixing activity given the high amount of RubisCO protein per cell.

Finally, sigma factor cascades have been implicated in the stress acclimation of bacteria. Among the down-regulated genes as well as proteins is the anti-sigma F factor antagonist Slr1859 (Additional file 3: Fig. S7), whose homolog in Bacillus subtilis is involved in posttranslational regulation of Sigma factor F [8]. Interestingly, the Sigma F (Slr1564), which itself showed an unchanged protein abundance, is one of the candidate factors involved in mediating the salt-dependent expression of ggpS [58]. Other sigma factors, particularly the genes encoding SigB and SigC were transiently induced after salt addition, while the amount of SigC slightly decreased in the proteome (SigB not identified) (Additional file 3: Fig. S7). Mutations of these group 2 sigma factors have been shown to reduce the stress tolerance including salt resistance of Synechocystis 6803 [99]. Hence, the salt-dependent activity of different sigma factors might significantly contribute to the observed salt-induced expression changes on transcript and protein levels.

Salt stress differentially affects chromosome regions

Most salt-regulated proteins are encoded by single genes or in small operons that are spread on the Synechocystis 6803 chromosome. However, some salt-regulated genes are clustered on specific chromosomal regions. The most remarkable examples are clusters including the genes ggpS and ggpP, which were found in regions on the chromosome comprising several genes/proteins with salt-stimulated expression. The ggpS cluster comprises 9 salt-regulated genes, which are at least transiently stronger expressed in salt-grown cells than in control cells (Additional file 3: Fig. S8). Upstream of the ggpS/glpD operon, on the opposite strand, a salt-regulated gene cluster of at least 7 genes (slr1670-1677) is found. This gene organization is widely conserved in the genomes of many GG-accumulating cyanobacteria [40]. A second salt-stimulated gene cluster can be found downstream of ggpP and ggtA, which comprises 5 different genes (Additional file 3: Fig. S9). In addition to glpK four other genes (three encode subunits of protochlorophyllide synthase, e.g. ChlN, slr0750; see Table 3) are at least transiently salt-regulated but have not yet shown to code for proteins directly involved in salt acclimation.

Another salt-stimulated gene cluster was found on the plasmid pSYSA. The genes sll7063-sll7067 (for one example see Table 3) are cas genes that encode structural proteins of one of the three CRISPR-Cas systems in Synechocystis 6803, called CRISPR2 [86]. The five proteins were significantly up-regulated whereas the transcripts were transiently down-regulated and then slightly up-regulated after 24 h of salt acclimation. In contrast, the CRISPR3 system (sll7085-sll7090) on the same plasmid was consistently down-regulated at RNA and protein level. Recently, it has been shown that these proteins form a stable protein complex together with their cognate crRNAs [82].

There are also some examples of coordinately down-regulated genes/proteins in salt-acclimated cells. One example is the large region (chromosome positions 1181250–1200000) comprising 22 genes, which are forming three operons (Additional file 3: Fig. S10). The first operon slr1406-1410 encodes proteins of unknown function. The second salt-repressed operon is situated on the opposite strand (sll1307-1304 and sll1784-1785) and also mostly encodes not functionally annotated proteins; however, the protein Sll1305 resembles ketose 3-epimerases while Sll1307 and Sll1784 are predicted outer membrane-bound periplasmic proteins. Hence it can be speculated that these proteins are somehow involved in cell wall synthesis/reorganization. The third salt-repressed operon in this region comprises the genes slr1852-1862. This cluster contains several annotated genes (Slr1855 N-acetylglucosamine 2-epimerase, Slr1856—anti-sigma factor antagonist, GlgX1—glycogen branching enzyme 1, IcfG—carbon metabolism regulator), which play important roles in the primary carbon metabolism and, particularly, its regulation [3, 90]. Another example of coordinated down-regulated genes/proteins represents the large operon slr0144-0152, which has been noted before as one of the highly coordinated expressed regions on the chromosome of Synechocystis 6803 (e.g., [96]) that is controlled by the redox-responsive transcription factor RpaB [81].

Metabolome analysis of salt-acclimated cells

The presence of high NaCl amounts in the medium induces a massive GG accumulation (Fig. 6C), which likely triggers a strong redistribution of organic carbon in Synechocystis 6803. The large impact of GG synthesis on overall carbon metabolism is also consistent with the observation that many proteins (and their genes) involved in glycogen metabolism as well as glycolysis showed significant changes in their abundances (Table 4). For example, the neopullulanase, glycogen phosphorylase GlgP2 (Slr1367) and one debranching enzyme GlgX1 (Slr0237, the other one Sll1857 is decreased) showed higher abundances on protein as well as RNA levels in salt-acclimated cells. The different response of the two GlgX proteins towards salt stress has been previously shown with Western-blotting [35]. Hence, the demand of organic carbon for the synthesis of GG precursors is at least partly supported by an enhanced glycogen breakdown and reduced glycogen build up, because glycogen and GG synthesis are competing for the same precursor, ADP glucose. The relatively low carbon/nitrogen state in salt-acclimated cells is also reflected by the lowered amount of 2-oxoglutarate (2OG, Fig. 9), which is the key metabolic signal reporting changes of the cellular carbon/nitrogen ratio in cyanobacteria [31].

Table 4.

Salt effects on proteins involved in central carbon metabolism

Gene	Protein function	Proteome	Transcriptome
slr0394	Phosphoglycerate kinase	0.76	0.58
slr0884	Glyceraldehyde-3-phosphate dehydrogenase 1, Gap1	0.75	1.35
sll0842	Neopullulanase, NplT	1.28	0.83
slr0237	Glycogen debranching enzyme 1, GlgX1	1.16	1.13
slr1857	Glycogen debranching enzyme 2, GlgX2	− 1.12	− 1.12
slr1367	Alpha-1,4 glucan phosphorylase	0.61	0.81
sll1356	Glycogen phosphorylase 2, GlgP2	0.08	0.53
sll0587	Pyruvate kinase 1 (PK 1)	0.76	0.60
sll1275	Pyruvate kinase 2 (PK 2)	− 0.45	− 0.78
slr0301	Phosphoenolpyruvate synthase	− 1.19	− 0.97

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Given are log₂ fold changes of their levels in cells exposed for 7 d (proteome) or 24 h (transcriptome) to 684 mM NaCl versus control cells

Fig. 9 — Alterations in the central carbon and nitrogen metabolism. Low molecular mass compounds were isolated from cells of *Synechocystis* 6803 grown in NaCl-free BG11 medium or medium supplemented with 4% NaCl for 7 days. LC–MS/MS was used to estimate the relative levels (Y axis show fold changes, amount in cells from 0% NaCl cultivation (-) set to 1 and relative level at 4% NaCl ( +) is shown) of central metabolites as part of primary carbon and nitrogen metabolism. Shown are mean values from three biological replicates (details in Additional file 1: Table S10). Dotted arrows indicate that several enzymes are necessary to convert one metabolite into the other. The alteration in the compatible solute GG is shown in Fig. 6

To obtain a snapshot on metabolites of the central carbon and nitrogen metabolism, LC–MS/MS was used (Additional file 1: Table S10). The relative levels of the RubisCO carboxylation and oxygenation products 3PGA and 2PG, respectively, showed opposite behavior (Fig. 9). 3PGA accumulated approximately threefold less in salt-acclimated cells, while 2PG was clearly enhanced. This could indicate a decreased CO₂/O₂ ratio at the active site of Rubisco, since the amounts of these gasses mainly regulate its relative carboxylation/oxygenation activity. For example, it might be possible that due to the higher content of inorganic ions inside the salt-exposed cells carboxysomes are less gas tight in high salt-grown cells, thereby promoting a better diffusion of oxygen into carboxysomes reducing the CO₂/O₂ ratio. The observed changes in the 3PGA and 2PG levels are consistent with the reported lower photosynthetic activity and growth rate in salt-acclimated cells of Synechocystis 6803 [25], which certainly also reduce Calvin-Benson-cycle activity. Consistently, the protein abundances of photosynthetic complexes, Calvin-Benson-cycle enzymes including RubisCO and components of the cyanobacterial inorganic carbon-concentrating mechanism were found at 10–40% lower levels, which is below our significance threshold but might contribute to lower photosynthetic activity in salt-acclimated cells. Furthermore, more organic carbon could be taken out from the Calvin-Benson-cycle, which is for example seen in the increased amount of pyruvate and organic acids in the reductive branch of the TCA cycle, such as malate and fumarate. This interpretation is also supported by the finding that Gap1, the glyceraldehyde dehydrogenase 1 (Slr0884) involved in sugar catabolism [46] is also up-regulated (Table 4), while Gap2 involved in photosynthetic carbon assimilation did not change (Additional file 1: Table S1).

In addition to the carbon fixation and allocation, nitrogen assimilation is altered in salt-acclimated cells, which is reflected by enhanced glutamine and glutamate levels while 2OG, the carbon skeleton used for ammonia assimilation decreased (Fig. 9). Increased glutamate levels have been often reported in salt-exposed bacteria [29], because this negatively charged amino acid is compensating the positive charge of cations, especially K⁺. The enzymes involved in the GS/GOGAT cycle for assimilation of NH₄⁺ into 2OG did not significantly change their expression in long-term salt acclimated cells, but were significantly lowered immediately after salt addition. However, the glutamate decarboxylase Gad (Sll1641) showed increased expression in salt-grown cells. Proline, which is often used in heterotrophic bacteria as compatible solute and can be synthesized from glutamate, is not changed during salt acclimation of Synechocystis 6803 (Fig. 9). Moreover, aspartate and arginine levels decreased. These amino acids serve as precursors for cyanophycin, the nitrogen storage compound of Synechocystis 6803. In this regard it is interesting to note that cyanophycin synthetase (Slr2002, FC 0.64) was decreased on protein level while the mRNA did not change. Furthermore, the mutation of a gene presumably involved in cyanophycin turnover resulted in a salt-sensitive phenotype of Synechocystis 6803 [108]. These observations also add to the assumption of altered nitrogen assimilation in salt-loaded cells. Marked changes in the amino acid composition had been also reported for Synechocystis 6803 cells when grown in artificial seawater medium compared to BG11 [36]. Similarly, global changes in the carbon- and nitrogen metabolism have been noticed in Synechococcus sp. PCC 7002 [1].

Discussion

Overall correlation of omics data

Our proteomic and transcriptomic data showed a good relationship (Pearson correlation coefficient, 0.58) especially taking into consideration that sampling was done in different laboratories and at different time periods after salt treatment. This finding indicates that in most cases transcriptional activation/repression leads to enhanced/diminished protein amounts, whereas the differential regulated ncRNAs rather regulate single genes/proteins. Generally, relationships between the transcript and corresponding protein amounts are influenced by several processes, such as (1) impact of mRNA processing or ncRNAs on translation rates, (2) protein´s half-life, and (3) protein synthesis delay [54]. Other studies found widely differing correlation coefficients between cyanobacterial transcriptomes and proteomes depending on the conditions examined. For example, experiments with Synechocystis 6803 cells shifted from high to low CO₂ conditions showed also a good correspondence between transcriptomics and proteomics [93], whereas a rather low correlation between transcriptomics and proteomics in Synechocystis 6803 cells grown under phototrophic, mixotrophic or heterotrophic conditions has been reported [98]. Similarly, a very low correlation was reported from an integrated proteomic and transcriptomic analysis of salt stress responses in Synechocystis 6803 [77].

Moreover, the comparison of proteome and transcriptome data from different studies, despite the varying degree of correspondence, offers the possibility to filter out regularly, truly salt-regulated proteins. To this end, we compared three transcriptomic with our proteomic data sets to identify further proteins potentially involved with unknown function in salt acclimation. Filtering the four datasets for features that were at least 1.5-fold increased (log₂ > 0.58) in the three transcriptome data sets and at least 1.3-fold increased (log₂ > 0.38) in the proteome data set produced a list of 44 genes, for which in 25 cases the corresponding proteins were identified (Additional file 1: Table S11). This group of genes/proteins includes 11 that are involved in GG metabolism and ion transport. Among the rather general stress proteins with unknown function are the Sll1862 and Sll1863 proteins as well as the putative zinc metalloprotease Sll0528 and the Slr1894 protein, which all have been discussed before. Other proteins with unknown function in salt acclimation such as the methionine aminopeptidase B (MAP B, Slr0786; co-expressed with ggpS, Additional file 3: Fig. S6), Sll0723 and Slr0001 are candidate proteins for further studies. Among the 19 salt-induced genes, whose proteins were not identified in our study, only the slr0530 gene product as component of the GG transporter is functionally related to known processes in salt acclimation.

The good correlation of transcriptomic and proteomic changes extends to the alterations on the metabolome level. Basic alterations in the central carbon and nitrogen metabolism are also supported by expression changes. However, biochemical alteration due to changed metabolite and ion levels on key enzyme activities certainly contribute to the novel metabolic homeostasis in salt-acclimated cells as has been recently discussed for the metabolic acclimation of Synechocystis 6803 towards different CO₂ availability [36].

Salt shock leads to a temporally staggered reshaping of the transcriptome composition

The salt acclimation response goes way beyond the induction of gene expression required for the compatible solute machinery, it has clearly a great impact on general metabolism. Along the temporal axis, the reprogramming of gene expression can be differentiated between an early response with the respective minima and maxima leading to the four different clusters (Fig. 2). The metabolic response included the rapid repression of the ammonia assimilation system, detected by decreased transcript abundances for amt1 and glnA encoding the ammonium transporter and the primary enzyme for ammonium incorporation, glutamine synthetase (GS). Consistently, increased transcript levels were found for genes gifA and gifB, which encode inhibitory proteins for GS, thereby blocking ammonium assimilation (for an overview see [5]). After 24 h the transcript levels of these genes were at the initial levels.

The question arises, which processes are responsible for the staggered reshaping of the transcriptome. It has been shown that shortly after salt addition the cytoplasmic composition underwent rapid changes due to ion and water movements, whereby the early high internal ion contents, especially of Na⁺ are discussed to inhibit metabolic activities but also to trigger acclimation responses such as GG synthesis activation (reviewed in [29]. The transporters responsible for the rapid ion movements are largely unknown, especially verified candidates for Cl⁻ export are still missing. In the present study we did not find marked expression changes for genes encoding potential anion exporters. It can be assumed that these transporters are mainly regulated on their activity levels to manage the ion regulation within the first minutes to hours after salt shock, because de novo protein synthesis is one process clearly down-regulated after salt shock [25]. However, we found that especially in the early time points after salt shock multiple ncRNAs become up- or down-regulated, which were not covered in the previous transcriptomic datasets. These small RNAs likely reshape mainly the translational efficiency of specific target mRNAs. Hence, it is well possible that many of the identified asRNAs and sRNAs are important to fine tune the translational response in the acute stress situation. Further work is necessary to identify the specific targets of the sRNAs and to verify the action of the ncRNAs during salt acclimation in cyanobacteria.

Impact of salt on DNA structure

The identification of chromosomal regions in the Synechocystis 6803 genome with coordinately up- or down-regulated genes under high salt conditions indicates that the DNA structure likely differs between distinct chromosomal regions (Additional file 3: Figs. S8–10). Similar observations were made when the impact of antibiotics that affect DNA supercoiling was analyzed on global gene expression patterns in E. coli and Synechocystis 6803. Interestingly, a large overlap has been observed between the antibiotic-induced gene expression changes and the salt and osmostress responses [6, 76]. Hence, the salt-stimulated expression of genes in some chromosomal regions could be related to a relaxed DNA topology permitting easier access of the transcription machinery and vice versa. In this regard it is interesting to note that the gene slr2058 encoding the DNA topisomerase I is higher transcribed in the first hours after salt shock (Additional file 1: Tables S1 and S2). The ATP-dependent DNA topoisomerases relax negative supercoils and are specifically involved in chromosome partitioning, which has been shown to be of fundamental importance for bacterial gene expression [11]. Recently, another subunit of DNA toposiomerase has been suggested to be involved in the regulation of DNA replication in a mutant defective in one of the dominating DNA methylation activities in Synechocystis 6803 [20]. It might be possible that differences in DNA methylation and thereby induced changes in the DNA/protein association are at least partly responsible for the different accessibility of specific chromosomal regions under different salt conditions. Finally, the interaction of chromosomal DNA with the GG synthesizing enzyme GgpS has been shown to be central for the ion-mediated activation/inactivation of its biochemical activity [65]. Collectively, our data support the notion that changes in DNA structure and DNA/protein interactions due to altered ionic and electrostatic relations play an important role in microbial salt acclimation.

Future developments: regulation and application

One still open question is how salt stress is sensed and transduced to the cellular gene expression machinery. Despite several efforts, specific salt-sensing proteins have not been identified in cyanobacteria. The screening of mutant collections defective in histidine kinases and cooperating response regulators identified some two-component systems that are involved in the salt-induced regulation of different general stress proteins, however, the induction of salt-specific proteins including ggpS remained unchanged [58, 91]. Two proteins were identified as repressors for ggpS, the small GgpR protein [44] and the transcriptional factor LexA have been shown to bind specifically the ggpS promoter [97]. However, the role of LexA as specific salt-sensing transcription factor is unlikely, because it is also involved in the regulation of many other processes in Synechocystis 6803, for example a verified role in fatty acid accumulation [42], and the lexA mutant has no reported salt-sensitive phenotype or changed GG accumulation. The present study identified two other likely candidates for a salt-stress specific gene regulation. First, the transcription factor PrqR (Slr0895) represents an interesting candidate, because the gene sl0895 is clearly co-regulated with many genes coding proteins involved on GG metabolism (Additional file 3: Fig. S6). It has been recently shown that PrqR is involved in the acclimation to oxidative stress in Synechocystis 6803 [39]. Salt stress is also inducing oxidative stress in cyanobacterial cells, hence, the finding of the role of PrqR in this stress acclimation process might of secondary importance. Second, the gene ssl1326 that possibly encodes a CopG family transcription factor has been found strongly induced after salt shock in the DNA microarray data set (Additional file 1: Table S1). Further work is necessary to validate whether PrqR or CopG are somehow acting as salt-specific gene expression regulators. In the moment, it might well be possible that ion-mediated changes in the DNA structure, RNA-polymerase affinity, and enzyme activities might be the main and sufficient mechanism to acclimate towards different salt conditions in euryhaline bacteria such as Synechocystis 6803.

Furthermore, salt acclimation is becoming more important for applied research with cyanobacteria regarding the direct use of compatible solutes as well as mass cultivation in sea water to make the process more sustainable [9, 68]. For example, the cyanobacterial production of mannitol [106] and trehalose [78] has been promoted by cultivation at enhanced salinities. Moreover, a more salt-tolerant version of the fast-growing Synechococcus elongatus strain UTEX2973 has been engineered by the expression of GG synthesis genes, which can be used for biotechnological purposes in full marine waters [10]. However, saline conditions might also negatively affect the production titer. The large impact of GG accumulation on the overall carbon metabolism also negatively influenced the ethanol production with Synechocystis 6803 at 4% NaCl while 2% NaCl were slightly stimulatory [70]. Salt-regulated, strong promoters might be an option to improve transgene expression in salt-grown cyanobacteria. Hence, a deeper knowledge on salt acclimation will promote future biotechnological applications with cyanobacteria.

Materials and methods

Cultivation and sampling

Synechocystis sp. 6803 substrain PCC-M was used in all experiments. Axenic cells were maintained on agar plates with BG11 mineral medium at 30 °C under constant illumination. For salt stress experiments, axenic cells were grown photoautotrophically in glass tubes containing liquid BG11 medium (TES-buffered at pH 8) at 29 °C in the cooperating laboratories. If not stated differently, cultures were aerated with CO₂-enriched air (5% CO₂ [v/v]) and kept under continuous illumination of 150 µmol photons m⁻² s⁻¹ (warm light, Osram L58 W32/3). Control cells were cultured in NaCl-free BG11 medium, whereas salt-acclimated cultures were obtained after long-term growth (up to one week) in BG11 medium supplemented with 684 mM NaCl (4% NaCl [w/v]). For this, cells were transferred daily to fresh media with 4% NaCl. Short-term salt shock experiments were performed by adding crystalline NaCl to a final amount of 4% into control cultures at time point zero. Subsequently, cells were harvested at defined time points.

For proteomics, cells were harvested by centrifugation at 14,000g and 4 °C for 5 min. The cell pellets were frozen in liquid nitrogen and stored at − 80 °C. For metabolomics, cells were harvested by quick filtration on nitrocellulose filters (0.45 µm pore size) in growth light within 30 s. Cells on filters were then frozen in liquid nitrogen and stored at − 80 °C. For transcriptomics, cells from 40 ml culture were harvested by quick filtration on hydrophilic polyethersulfone filters (Pall Supor-800, 0.8 µm), immediately immersed in 1 ml of cold PGTX solution [75] and frozen in liquid nitrogen.

Transcriptomic methods

RNA extraction

Total RNA was extracted as described previously [32]. Prior to the microarray analysis, 10 µg of total RNA were treated with Turbo DNase (Invitrogen) according to the manufacturer's protocol and precipitated with ethanol/sodium acetate. RNA quality was verified by electrophoresis on MEN-buffered 1.5% agarose gels supplemented with 6% formaldehyde.

Microarray analysis

To enable the comparison with a previous microarray analysis [60], we analyzed similar time points after salt shock: 0, 0.5, 2 and 24 h. Labeling and hybridization were performed as described [45]. Three µg of RNA were used for the labeling reaction and 1.65 µg of labeled RNA for the hybridization. The microarray hybridization was performed in duplicates for each sampling point. Almost all features on the microarray chip were covered by several independent probes. In addition, it contained technical replicates for each single probe. Hence, mean values for all probes of a given feature were used for the final calculation of fold changes. Data processing and statistical evaluation was performed using the R software as described [45]. The full dataset is accessible from the GEO database with the accession number GSE174316 (accession for Reviewers via: izupwswenzelfkv).

In Additional file 1: Table S1 transcripts are separated into mRNAs, asRNAs, other ncRNAs, 5'UTRs and transcripts derived from internal TSSs, i.e. within CDS (int). However, it should be noted that for every category overlaps are possible, i.e. the annotation as well as microarray detection of ncRNAs is often ambiguous since they can overlap with UTRs. Thus, all features labeled with the systematic term “NC-#” are referred as “potentially” trans-acting ncRNAs. For the evaluation presented in the text only ncRNAs with an annotation based on reference [64] were considered.

Cluster analysis

Clustering analysis for the microarray time series was performed using the mfuzz R package [50]. To reduce noise and false positives, only 3831 transcripts entered the clustering analysis that had a difference in their absolute expression values higher than log₂ ≥ │1│in at least one of these comparisons. The optimal cluster number was determined with the Elbow method using the minimum centroid distance and an estimated “fuzzifier” parameter of m = 2.53, yielding four clusters. Transcripts with low membership values < 0.5 were removed. However, those transcripts were still included if the combined membership values for two similar clusters (e.g. cluster 1 + 2 and 3 + 4) exceeded > 0.6.

Proteomic methods

Cells from four biological replicates of salt-acclimated and control cultures, respectively, were broken with glass beads using Precellys 24 homogenizer (peqLab Biotechnologie GmbH, Erlangen, Germany) in non-denaturing buffer containing 10 mM Tris/HCl, pH 7.4, 138 mM NaCl, 2.7 mM KCl, 1 mM MgCl₂. After withdrawing an aliquot of each cell extract as total protein the remaining cell extracts were fractionated into debris, soluble, and membrane-enriched fractions. Protein samples were reduced with dithiothreitol, alkylated with iodoacetamide and digested with trypsin in sodium deoxycholate-containing buffer solution [71].

LC-HDMS^E analyses of desalted peptide samples supplemented with 40 fmol of Hi3 Phos B standard for protein absolute quantification (Waters) were carried out using a nanoAcquity UPLC system (Waters) coupled to a Waters Synapt G2-S mass spectrometer [70]. The Synapt G2-S instrument was operated in data-independent mode with ion-mobility separation as an additional dimension of separation (referred to as HDMS^E). Single measurements of the four biological replicates of the total extract, soluble fraction and membrane-enriched fraction were carried out, while pooled samples of the debris fraction were measured in triplicate.

Progenesis QI for Proteomics version 4.1 (Nonlinear Dynamics, Newcastle upon Tyne, UK) was used for raw data processing, protein identification and label free quantification. Proteins were quantified by the absolute quantification Hi3 method using Hi3 Phos B Standard (Waters) [92]. Results were given as fmol on column. Proteins identified in one fraction by at least two unique peptides were included in the quantitative analysis. Protein abundance changes between salt-acclimated and control cells by a factor of at least 1.5, accompanied by ANOVA p-values < 0.05 were regarded as significant. To determine a combined fold change value for the total extract and the three subcellular fractions, first a weighted fold change value for the three subcellular fractions was calculated by summing up the corresponding protein amounts (measured as fmol on column) and dividing the value from salt-acclimated cells by the value from controls. Since the debris fraction contained only a minor part of about 10% of the total protein, the protein amounts of the debris fraction were divided by ten. In a second step, the final combined fold change value was calculated as the average of the weighted fold change from the subcellular fractions and the fold change of the total extract.

A detailed description of the proteome method can be found in the Additional file 3. The mass spectrometry proteomics data have been deposited to the ProteomeXchange Consortium via the PRIDE [102] partner repository with the dataset identifier PXD026118 and 10.6019/PXD026118.

Metabolomic methods

Low molecular mass compounds were extracted from cells with ethanol (80%, HPLC grade, Roth, Germany) at 65ºC for 2 h. The soluble sugars were analyzed by gas–liquid chromatography using a defined amount of sorbitol as internal standard [28]. Other metabolites were analyzed by LC–MS/MS using the high-performance liquid chromatograph mass spectrometer system LCMS-8050 (Shimadzu, Japan). One microgram of carnitine was added per sample as internal standard for LC–MS/MS analyses. The dry extracts were dissolved in 200 µl MS-grade water and filtered through 0.2 µm filters (Omnifix®-F, Braun, Germany). The cleared supernatants were separated on a pentafluorophenylpropyl (PFPP) column (Supelco Discovery HS FS, 3 µm, 150 × 2.1 mm) with a mobile phase containing 0.1% formic acid. The compounds were eluted at a rate of 0.25 ml min⁻¹ using the following gradient: 1 min 0.1% formic acid, 95% water, 5% acetonitrile, within 15 min linear gradient to 0.1% formic acid, 5% distilled water, 95% acetonitrile, 10 min 0.1% formic acid, 5% distilled water, 95% acetonitrile. Aliquots were continuously injected in the MS/MS part and ionized via electrospray ionization (ESI). The compounds were identified and quantified using the multiple reaction monitoring (MRM) values given in the LC–MS/MS method package and the LabSolutions software package (Shimadzu, Japan). The metabolites were determined as relative metabolite abundances (fold changes), which were calculated after normalization of signal intensity to that of the internal standard carnitine.

Supplementary Information

13062_2021_316_MOESM1_ESM.xlsx^{(4.8MB, xlsx)}

Additional file 1. Excel sheets displaying selected data from the transcriptomic, proteomic, and metabolomic data as well as meta-analyses.

13062_2021_316_MOESM2_ESM.pdf^{(11.1MB, pdf)}

Additional file 2. Genome plot of Synechocystis sp. PCC 6803 chromosome displaying the microarray data for each single probe.

13062_2021_316_MOESM3_ESM.docx^{(4.8MB, docx)}

Additional file 3. Details on methodology as well as additional figures.

Acknowledgements

The technical assistance of Klaudia Michl (University of Rostock) is acknowledged.

Authors' contributions

MH designed the study. SK, MR, JG & WRH performed and evaluated the transcriptomic analyses. SM performed and evaluated the proteome experiments. MH performed and evaluated the metabolome analyses. MH, WRH, SK & SM wrote the manuscript. All authors read and approved the final manuscript.

Funding

Open Access funding enabled and organized by Projekt DEAL. Funded by the German research Foundation (DFG) - “SCyCode” research group FOR 2816 (DFG ID 397695561) to MH (HA 2002/23-1) and WRH (HE 2544/15-1), individual grant KL 3114/2-1 to SK, and the Research Training Group “MeInBio” GRK2344 (DFG ID 322977937) to MR. The LC–MS/MS equipment at University of Rostock was financed through the HBFG program (GZ: INST 264/125- FUGG).

Availability of data and materials

The transcriptomic and proteomic datasets generated and analyzed during the current study are available in the GEO or PRIDE repository, [web links given in the M&M section]. Most of the other data generated or analyzed during this study are included in the Additional file 3 of this article.

Declarations

Consent for publication

All authors agree to the submission.

Competing interests

The authors declare no competing interests.

Footnotes

Publisher's Note

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

Stephan Klähn and Stefan Mikkat contributed equally to this study

Contributor Information

Stephan Klähn, Email: stephan.klaehn@ufz.de.

Stefan Mikkat, Email: stefan.mikkat@med.uni-rostock.de.

Matthias Riediger, Email: matthias.riediger@biologie.uni-freiburg.de.

Jens Georg, Email: jens.georg@biologie.uni-freiburg.de.

Wolfgang R. Hess, Email: wolfgang.hess@biologie.uni-freiburg.de

Martin Hagemann, Email: martin.hagemann@uni-rostock.de.

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Associated Data

This section collects any data citations, data availability statements, or supplementary materials included in this article.

Supplementary Materials

13062_2021_316_MOESM1_ESM.xlsx^{(4.8MB, xlsx)}

Additional file 1. Excel sheets displaying selected data from the transcriptomic, proteomic, and metabolomic data as well as meta-analyses.

13062_2021_316_MOESM2_ESM.pdf^{(11.1MB, pdf)}

Additional file 2. Genome plot of Synechocystis sp. PCC 6803 chromosome displaying the microarray data for each single probe.

13062_2021_316_MOESM3_ESM.docx^{(4.8MB, docx)}

Additional file 3. Details on methodology as well as additional figures.

Data Availability Statement

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PERMALINK

Integrative analysis of the salt stress response in cyanobacteria

Stephan Klähn

Stefan Mikkat

Matthias Riediger

Jens Georg

Wolfgang R Hess

Martin Hagemann

Abstract

Supplementary Information

Background

Results

Fig. 1.

Global transcriptome analysis

Table 1.

Fig. 2.

Salt-regulated asRNA:mRNA pairs

Fig. 3.

Salt-regulated sRNAs

Global evaluation of the proteome in salt-acclimated cells

Fig. 4.

Correlation analysis of salt-stimulated transcriptome and proteome

Fig. 5.

Detailed examination of specific processes

Compatible solute metabolism and transport constitutes a salt-specific stimulon

Fig. 6.

Table 2.

Transporters and channels belonging to the salt-specific stimulon

Fig. 7.

Many salt-induced proteins are involved in general stress response

Table 3.

Salt effects on proteins involved in the basic cell physiology

Fig. 8.

Differential expression of regulator proteins

Salt stress differentially affects chromosome regions

Metabolome analysis of salt-acclimated cells

Table 4.

Fig. 9.

Discussion

Overall correlation of omics data

Salt shock leads to a temporally staggered reshaping of the transcriptome composition

Impact of salt on DNA structure

Future developments: regulation and application

Materials and methods

Cultivation and sampling

Transcriptomic methods

RNA extraction

Microarray analysis

Cluster analysis

Proteomic methods

Metabolomic methods

Supplementary Information

Acknowledgements

Authors' contributions

Funding

Availability of data and materials

Declarations

Consent for publication

Competing interests

Footnotes

Contributor Information

References

Associated Data

Supplementary Materials

Data Availability Statement

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