Abstract
We established a syntrophic coculture of Syntrophobacter fumaroxidans MPOBT (SF) and Geobacter sulfurreducens PCAT (GS) growing on propionate and Fe(III). Neither of the bacteria was capable of growth on propionate and Fe(III) in pure culture. Propionate degradation by SF provides acetate, hydrogen, and/or formate that can be used as electron donors by GS with Fe(III) citrate as electron acceptor. Proteomic analyses of the SF-GS coculture revealed propionate conversion via the methylmalonyl-CoA (MMC) pathway by SF. The possibility of interspecies electron transfer (IET) via direct (DIET) and/or hydrogen/formate transfer (HFIT) was investigated by comparing the differential abundance of associated proteins in SF-GS coculture against (i) SF coculture with Methanospirillum hungatei (SF-MH), which relies on HFIT, (ii) GS pure culture growing on acetate, formate, hydrogen as propionate products, and Fe(III). We noted some evidence for DIET in the SF-GS coculture, i.e., GS in the coculture showed significantly lower abundance of uptake hydrogenase (43-fold) and formate dehydrogenase (45-fold) and significantly higher abundance of proteins related to acetate metabolism (i.e., GltA; 62-fold) compared to GS pure culture. Moreover, SF in the SF-GS coculture showed significantly lower abundance of IET-related formate dehydrogenases, Fdh3 (51-fold) and Fdh5 (29-fold), and the rate of propionate conversion in SF-GS was 8-fold lower than in the SF-MH coculture. In contrast, compared to GS pure culture, we found lower abundance of pilus-associated cytochrome OmcS (2-fold) and piliA (5-fold) in the SF-GS coculture that is suggested to be necessary for DIET. Furthermore, neither visible aggregates formed in the SF-GS coculture, nor the pili-E of SF (suggested as e-pili) were detected. These findings suggest that the IET mechanism is complex in the SF-GS coculture and can be mediated by several mechanisms rather than one discrete pathway. Our study can be further useful in understanding syntrophic propionate degradation in bioelectrochemical and anaerobic digestion systems.
Introduction
Geobacter bacteria are important in soils and sediments containing available organic matter and amorphous Fe(III) (; ). Geobacter species play a key role in syntrophic interactions by the removal of fermentation products, such as acetate, formate, and hydrogen, and mitigating the thermodynamic barrier that would otherwise inhibit organic compound decomposition. In these Fe(III)-dependent syntrophic partnerships, Geobacter species reduce Fe(III) (hydroxy)oxides by electrons derived from the oxidation of organic matter. Accordingly, several syntrophic interactions involving Geobacter species have been documented (; ; ) and more might be possible where Geobacter could drive other microorganisms degrading organic substrates.
Propionate is an important intermediate in anaerobic degradation of organic matter. However, anaerobic oxidization of propionate is thermodynamically more difficult than other intermediates such as butyrate, lactate, and ethanol. Hence, it can accumulate in anaerobic environments such as digesters (; ; ; ; ) and inhibit efficient anaerobic digestion. Therefore, anaerobic conversion of propionate is a prime example of a syntrophic relationship between propionate-oxidizing bacteria and downstream partners, usually methanogens (Worm et al., 2011).
Syntrophobacter fumaroxidans (SF) is a propionate-oxidizing bacterium that degrades propionate in pure culture using sulfate or fumarate as an electron acceptor (; ; ), or in syntrophic associations with methanogens such as Methanospirillum hungatei (MH) or Methanobacterium formicicum (MF) that utilize hydrogen and formate to make propionate oxidation an exergonic process (). Therefore, propionate degradation requires hydrogen and formate scavengers such as methanogens to keep these concentrations sufficiently low (1 Pa and 10 μM, respectively) and make the reaction energetically feasible (; ). SF metabolizes propionate using the methylmalonyl-CoA (MMC) pathway (Figure 1) (). In this pathway, succinate oxidation via menaquinone is highly endergonic since the midpoint potential of succinate is much more positive (+30 mV) than the menaquinone (−80 mV) (). Therefore, this reaction requires a transmembrane proton gradient to function (). To make the endergonic oxidation of succinate possible, involvement of a periplasmic formate dehydrogenase, cytochrome b:quinone oxidoreductases, the menaquinone loop, and a cytoplasmic fumarate reductase has been proposed (). In the MMC, electrons are produced in three oxidation steps: (i) succinate to fumarate, (ii) malate to oxaloacetate, and (iii) pyruvate to acetyl-CoA plus CO2 (red arrows, Figure 1). Consequently, these electrons reduce protons to hydrogen or protons plus CO2 to formate. Subsequently, hydrogen and formate are transferred to the methanogenic partner.
FIGURE 1
Besides methanogens, the syntrophic partner could be any other microbe capable of effective hydrogen and formate removal to facilitate propionate oxidation. G. sulfurreducens PCA (GS) can engage in a cooperative partnership with other microbes using different mechanisms for interspecies electron transfer (IET) via direct (DIET) and/or hydrogen/formate transfer (HFIT). For instance, HFIT has been identified in cocultures between Pelobacter carbinolicus and GS (PC-GS) where ethanol fermentation by P. carbinolicus produces hydrogen and formate to support the growth of GS (). Furthermore, DIET has been reported in an evolved syntrophic coculture of the ethanol-oxidizing G. metallireducens and GS (GM-GS) mediated by extracellular c-type cytochromes (). GS can grow using a range of fermentation products such as acetate, formate, and hydrogen. However, fatty acids like propionate and butyrate that are key intermediates in the mineralization of complex organic matter are not used by this bacterium.
A coculture of SF and GS might also overcome the energetic barrier of propionate oxidation. In such a partnership, SF cannot reduce Fe (III) and GS cannot oxidize propionate. Hence, we hypothesized that a coculture benefiting from metabolic interactions between SF and GS might be an alternative strategy for propionate oxidation coupled to Fe(III) by GS. Accordingly, a recent study reported syntrophic propionate degradation by a coculture of SF-GS in the anode of a microbial fuel cell (). Here, we report syntrophic growth of SF-GS cocultures on propionate and Fe(III) followed by proteomic analyses of the coculture to gain insight into the underlying mechanisms of propionate degradation and associated syntrophic interactions.
Materials and Methods
Microorganism and Cultivation
Syntrophobacter fumaroxidans MPOB (DSM10017) and G. sulfurreducens strain PCA (DSM 12127; ATCC 51573) were grown under strict anoxic conditions at 35°C in 120-ml serum bottles with 50 ml of bicarbonate-buffered medium as described previously (). For the pure culture experiments, SF was grown on propionate (20 mM) plus fumarate (60 mM) with N2/CO2 (80:20, v/v) as the headspace, while GS was grown on a mixture of acetate (5 mM), formate (20 mM), and hydrogen (10 mM) plus Fe(III) citrate (80 mM). Propionate, fumarate, acetate, and formate (all sodium salts) were added from 1 M sterile anoxic stock solutions. To reach 10 mmol hydrogen per liter of liquid medium, 18% of the headspace was filled with pure hydrogen (18.1 kPa). Both bacteria were adapted to their growth conditions by at least five subsequent transfers (10% v/v) to fresh media containing respective electron donors and acceptors.
To construct the coculture, SF and GS were grown on propionate (10 mM) and Fe(III) citrate (80 mM) as electron acceptor in the same medium as the pure cultures. The coculture was adapted to the growth condition by at least five subsequent transfers (10% v/v) in the corresponding media. Growth was determined by analyzing depletion of propionate, production of Fe(II), and increase in volatile suspended solids (VSS) contents. The Fe (III) media were reduced with FeCl2 (1.3 mM), and no other reducing agent (e.g., cysteine and sulfide) was used.
Analytical Methods
Short-chain fatty acids (SCFA) were analyzed using high-performance liquid chromatography (HPLC) using a Dionex UHPLC system (). Fe(II) and Fe(III) were quantified with the ferrozine colorimetric method () with absorbance at 562 nm using a U-1500 spectrophotometer (Hitachi, Chiyoda, Tokyo, Japan). The biomass at time zero and at the end of the experiment was analyzed by VSS contents according to standard methods ().
Scanning Electron Microscopy
Biomass samples of the SF-GS coculture were fixed in 2.5% (w/v) glutaraldehyde overnight at 4°C. The fixed samples were washed twice with carbonate/bicarbonate buffer (pH 9, 1.5 M Na+) and then dehydrated in a series of ethanol solutions (10, 25, 50, 75, 90, and twice 100%) with 20-min incubations in each step. The slides were dried in a desiccator, coated with gold, and analyzed in a JEOL JSM-6480LV Scanning Electron Microscope. Energy-dispersive X-ray spectroscopy (EDX) analysis was performed using a NORAN Systems SIX (Thermo Scientific, United States).
Proteomic Analyses
The SF-GS cocultures were used for whole-cell proteomic analyses. Cells from triplicate cultures were harvested at the end of the exponential growth phase by centrifugation at 16,000 g for 20 min at 4°C. Cell pellets were washed twice with 20 mM Tris-HCl (pH 7.5) and stored at −80°C until further use. For protein extraction, cell pellets were resuspended in 0.5 ml of SDT-lysis buffer composed of 100 mM Tris/HCl, pH 7.5, 4% w/v sodium dodecyl sulfate (SDS), SIGMAFAST™, Protease Inhibitor Cocktail Tablet (Sigma-Aldrich, Missouri), and 0.1 M dithiothreitol (DTT). Protein extractions, separation, tryptic digestion, and analysis were performed as described previously (). The proteins of SF and GS were downloaded from UniProt1. An additional database with protein sequences of common contaminants (trypsin, human keratins, and bovine serum albumin) was also included in the database search. False discovery rate (FDR) of less than 1% were set at both peptide and protein levels. The proteomics result contained proteins with at least two identified peptides of which at least one is unique and at least one is unmodified. The natural logarithm was taken from protein label-free quantitation (LFQ; normalized with respect to the total amount of protein and all of its identified peptides) intensities. The non-existing LFQ intensity values were replaced with values obtained by applying a normal distribution down shift of 1.8 and a width of 0.3 (Perseus default values). Relative protein quantification of sample to control was conducted with PERSEUS v.1.6.2.1. by applying two-sample t tests using the “log LFQ intensity” columns obtained with an FDR threshold set to 0.05 and S0 = 1. Proteins significantly (p < 0.05) present under the given condition were mentioned throughout the text. To determine the proteins’ fold change between two conditions, the log protein abundance ratio of those conditions was considered. Further statistical analyses were performed using R () and the Venn Diagram package () as described previously (). The proteins SF and GS are listed in the Supplementary Files 1, 2. The mass spectrometry proteomics data have been deposited to the ProteomeXchange Consortium via the PRIDE () partner repository with the dataset identifier PXD027104.
Results and Discussion
Propionate Oxidation and Fe(III) Reduction by the SF-GS Coculture
A syntrophic coculture of the propionate-oxidizing bacterium SF with the Fe(III)-reducing GS was established. Both bacteria are important in anaerobic environments and are known to establish syntrophic interactions with other microbes. Recently, syntrophic propionate degradation using a coculture of SF-GS was reported in a microbial fuel cell (). In our study, we established syntrophic propionate degradation coupled to Fe(III) reduction using a SF-GS coculture. Whereas anaerobic propionate degradation is an endergonic reaction, removal of acetate, formate, and hydrogen by GS coupled to Fe(III) reduction would make the reaction exergonic (Table 1). Our recent physiological and proteomic analyses indeed verified degradation of acetate, formate, and hydrogen by a pure culture of GS (Figure 2A) ().
TABLE 1
| Reactions | ΔG0 (kJ/mol) |
| Propionate degradation by SF | |
| Propionate– + 3H2O → acetate– + HCO3– + H+ + 3H2 | +76.5 |
| Propionate– + 2HCO3– → acetate– + H+ + 3HCOO– | +72.4 |
| Acetate, hydrogen, and formate consumption by GS | |
| Acetate– + 4H2O + 8 Fe3+ → 2HCO3– + 8Fe2+ + 9H+ | −808.6 |
| H2 + 2Fe3+ → 2H+ + 2 Fe2+ | −228.3 |
| Formate– + H2O + 2Fe3+ → HCO3– + 2Fe2+ + 2H+ | −226.9 |
| Syntrophic propionate degradation with removal of acetate (a), hydrogen (b), or formate (c) | |
| (a) Propionate– + 7H2O + 8Fe3+ → 3HCO3– + 10H+ + 3H2 + 8Fe2+ | −733.3 |
| (b) Propionate– + 3H2O + 6Fe3+ → acetate– + HCO3– + 7H+ + 6Fe2+ | −609.4 |
| (c) Propionate– + 3H2O + 6Fe3+ → acetate– + HCO3– + 7H+ + 6Fe2+ | −609.2 |
| Complete propionate degradation | |
| Propionate– + 7H2O + 14Fe3+ → 3HCO3– + 16 H+ + 14Fe2+ | −733.3 |
Potential reactions during syntrophic growth of SF-GS coculture based on Gibbs free energy changes.
Data were obtained from and .
FIGURE 2
Propionate consumption and Fe(III) reduction indicated a successful syntrophic relationship between these two partners (Figure 2C). However, the rate of propionate consumption by the SF-GS coculture (0.14 mM/day) (Figure 2C) was considerably lower than the SF pure culture growing on propionate and fumarate (1.05 mM/day) (Figure 2B) and a SF-MH coculture growing on propionate (1.08 mM/day) (
The Fe(II) produced (39.1 ± 2.4 mmol; mean ± SD, n = 3) from 4.3 ± 0.2 mmol propionate consumed (Figure 2C) corresponded to a molar yield of Fe(II) production on propionate of 9.2 ± 0.9. This is consistent with the stoichiometry for the oxidation of propionate to acetate by SF and Fe (III) reduction of acetate by GS (Table 1). Acetate production from propionate by a SF-GS coculture in a microbial fuel cell was also shown by
Proteomic Analyses of the SF-GS Coculture
To gain further insights into the metabolism of the SF-GS coculture and to evaluate electron transfer mechanisms, we performed proteomic analyses. Three biological replicates of cocultures were prepared in batch culture. These replicates were harvested when ∼50% of Fe(III)-citrate (80 mM) had been reduced to Fe(II). The proteome of the SF-GS coculture was compared with the previously published proteome of (i) the SF pure culture growing on propionate and fumarate (
The genome of S. fumaroxidans contains 4,098 protein coding genes (PCGs) (
Proteome of SF in SF-GS Coculture vs. SF Pure Culture and SF-MH Coculture
Enzymes of the Methylmalonyl CoA Pathway
Previous genomic analyses of SF predicted several genes coding for proteins involved in the MMC pathway (
FIGURE 3

Relative abundance of the detected proteins in the methylmalonyl-CoA pathway of SF in the SF-GS coculture versus the SF pure culture and the SF-MH coculture. Protein abundance levels are shown after Z-score normalization. The colour intensity indicates the degree of protein presence, where high relative abundance is indicated in red and low relative abundance in blue. The rows in the heat map show the detected proteins in the SF-GS coculture, the SF pure culture and the SF-MH coculture. The columns show the cultures in triplicates. Clustering shows that samples grouped according to treatments even when only enzymes in this set are considered (Supplementary Figure 6).
Succinate oxidation to fumarate by a membrane-bound succinate dehydrogenase/fumarate reductase and via a menaquinone is the most energy-dependent reaction in the MMC pathway (
During SF growth on propionate with fumarate, propionate is converted to succinate (black arrows, Figure 1), and then, fumarate is partially oxidized to acetate (blue arrows, Figure 1). This conversion is energy demanding and produces reducing equivalents during malate oxidation, and pyruvate decarboxylation, and is only possible by its coupling to the energy-yielding reduction of fumarate to succinate. In line with this, three subunits of the fumarate reductase complex, FrdABEF (Sfum_4093–95), were detected in significantly higher abundance (11-, 45-, and 15-fold, respectively) in the SF pure culture versus the SF-GS coculture (Figure 3). Yet, the FrdABEF complex showed slightly higher abundance in the SF-GS coculture compared to the SF-MH coculture (2-, 2-, and 1-fold, respectively) (Figure 3). In line with the former, transcription analyses of the SF pure culture grown with fumarate also reported upregulation of FrdABEF (>2 log ratio) and downregulation in SF cells cocultured with MH (
Fumarase converts fumarate to malate and maintains the level of fumarate low to pull the oxidation of succinate to fumarate. The predicted fumarase in the gene cluster (Sfum_2101–2102) was not detected in the coculture of SF-GS. Instead, a second fumarase from a non-clustered gene (Sfum_2336) was detected in our study with significantly lower abundance compared to SF-MH coculture (10-fold) and SF pure culture (4-fold) (Figure 3).
The remaining enzymes of the MMC pathway such as methylmalonyl-CoA epimerase (Sfum_0455–0456), methylmalonyl-CoA mutase (Sfum_0457–0458), and pyruvate carboxyltransferase (Sfum_0461 and Sfum_0676) showed lower abundance in the SF-GS coculture compared to the SF-MH coculture and the SF culture (Figure 3). Two enzymes showed significantly lower abundance in the SF-GS coculture, i.e., pyruvate ferredoxin oxidoreductase (Sfum_2792–95) and carboxyl transferase (Sfum_1223) (Figure 3). In contrast, two enzymes showed slightly higher abundance in the SF-GS compared to SF-MH and SF, i.e., malate dehydrogenase (Sfum_2777) (8-fold higher vs. SF-MH, and 1-fold higher vs. SF) and two subunits of acetyl-CoA synthase/COdh complex (Sfum_2564-65) (19- and 15-fold higher vs. SF-MH, and 3- and 7-fold higher vs. SF, respectively) (Figure 3).
Potential Involvement of Hydrogenases and Formate Dehydrogenases, Pilin, and Cytochromes of SF in Interspecies Electron Transfer
The genome of SF contains eight hydrogenases and six formate dehydrogenases (Supplementary File 2 and Supplementary Table 6). Of the eight predicted hydrogenases, seven were detected in the present study (Figure 4). The three important cytoplasmic hydrogenases, i.e., Hyd1 (Sfum_0844–0846), Hox (Sfum_2712–2716), and Fhl-h (Sfum_1791–94) detected in this study showed significantly lower abundance in the SF-GS coculture (Figure 4). Other cytoplasmic hydrogenases, Mvh1 (Sfum_3535–3537), Mvh2 (Sfum_3954–3957), and Frh (Sfum_2221–2224), were not found in our study except one subunits of Frh (Sfum_2221) (Figure 4). Sfum_2221 subunit in SF-GS showed slightly higher abundance (2 vs. SF and 3-fold vs. SF-MH) (Figure 4).
FIGURE 4

Relative abundance levels of detected hydrogenases and formate dehydrogenases of SF in the SF-GS coculture versus the SF pure culture and the SF-MH coluture. Protein abundance levels are shown after Z-score normalization. Protein abundance levels are shown after Z-score normalization. The colour intensity indicates the degree of protein presence, where high relative abundance is indicated in red and low relative abundance in blue. The rows in the heat map show the detected proteins in the SF-GS coculture, the SF pure culture and the SF-MH coulture. The columns show the cultures in triplicates. Clustering shows that samples grouped according to treatments even when only enzymes in this set are considered (Supplementary Figure 6).
The two predicted periplasmic hydrogenases [Hyd2 (Sfum_0847–0848) and Hyn (Sfum_2952–2953)] detected in this study showed significantly lower abundance in the SF-GS coculture compared to the other conditions (Figure 4). Hyd1 might be involved in energy conservation as a confurcating hydrogenase, and Hyn has been suggested to be involved in reverse electron transport (RET) coupled with FrdABEF for fumarate reduction or with SdhABC for succinate oxidation (Worm et al., 2011;
Among the cytoplasmic formate dehydrogenases, Fdh1 (Sfum_2703–2706) and Fdh4 (Sfum_0030–0031) were detected in significantly lower abundance in the SF-GS coculture versus SF-MH. Compared to the SF culture, Fdh1 (Sfum_2703) (7-fold) and Fdh4 (Sfum_0030–0031) (2- and 1-fold, respectively) were more abundant in the SF-GS cocultures whereas the rest of subunits were lower (Figure 4). The three periplasmic formate dehydrogenases of SF, Fdh2 (Sfum_1273–1275), Fdh3 (Sfum_3510-11), and Fdh5 (Sfum_0035-37), detected in our study showed significantly lower abundance in the SF-GS cocultures than SF-MH (Figure 4). However, compared to SF, Fdh2 (Sfum_1274; 8-fold), Fdh3 (Sfum_3510; 2-fold), and Fdh5 (4-, 2-, and 7-fold, respectively) showed higher abundance in the SF-GS coculture. It was proposed that Fdh3 and Fdh5 are specialized in transferring formate to the methanogenic partner, whereas Fdh2 is used for energy conservation as part of the reverse electron transport mechanism associated with succinate oxidation, possibly coupled to SdhABC or FrdABEF (
From the membrane-bound Fhl-f (Sfum_1795–1806), seven subunits (1795–1797, 1801, and 1804–1806) were found with significantly lower abundance in the SF-GS compared to the SF-MH coculture. Compared to the SF pure culture, Fhl-f (Sfum_1795–1796 and 1805–1806) showed (7-, 2-, 3-, and 9-fold, respectively) higher abundance in the SF-GS coculture (Figure 4). A possible role for Fhl-f was suggested in hydrogen-formate interconversion during syntrophic growth (
SF has not been observed to grow syntrophically by DIET. In order to provide insight into the potential role of pili and c-type cytochromes of SF in DIET (Supplementary File 2 and Supplementary Table 2), the differential abundance levels of detected ones in SF-GS cocultures were compared against SF-MH that relies on HFIT. PilE (suggested as e-pili) was not detected. PilQ (Sfum_0540) in SF-GS coculture showed slightly lower abundance (1-fold) compared to the SF-MH coculture, but higher abundance (5-fold) compared to the SF pure culture. This may not necessarily indicate a role of PilQ in IET. PilQ might also be produced for adhesion of the cells. Cytc3 (Sfum_4047) showed lower abundance in the SF-GS coculture (25-fold vs. SF-MH, 8-fold vs. SF) which indicates that its function is not related to electron transfer between SF and GS. Further physiological and gene knockout studies are required to determine if cytochromes/pilin directly contribute to DIET. For instance, PilE/PilQ-deficient mutant of SF cocultures with GS could reveal whether it is associated with DIET.
Proteome of GS in the SF-GS Coculture vs. GS Pure Culture Grown on Products of Propionate Conversion
The growth of GS pure culture on products of propionate oxidation (acetate, formate, and hydrogen) revealed that when all three substrates are available, formate and hydrogen were the preferred substrates than acetate (Figure 2A, till day 6) (
Proteins Related to Acetate Metabolism in GS
In SF-GS cocultures, GS has the option to use acetate derived from propionate conversion. Our proteomic analyses of acetate uptake, acetate activation, and citric acid cycle (CAC) proteins indicated that GS was actively metabolizing acetate in the SF-GS coculture. Among the acetate uptake proteins of GS (AplA; GSU1068, AplB; GSU1070, AplC; GSU2352), AplB and AplC were more abundant in the SF-GS coculture (11- and 3-fold, respectively), whereas AplA was more abundant in the GS pure culture (5-fold) (Figure 5). Presence of at least two of these proteins is necessary for acetate uptake (
FIGURE 5

Relative abundance of the detected proteins in the central metabolic network of GS in the SF-GS coculture versus the GS pure culture. Protein abundance levels are shown after Z-score normalization. The color intensity indicates the degree of protein presence, where high relative abundance is indicated in red and low relative abundance is indicated in blue. The rows in the heat map show the detected proteins in the SF-GS coculture and the GS pure culture. The columns show the cultures in replicates. The abbreviations of the proteins are as follows: sodium/solute symporter family protein (AplA, AplB, AplC, and AplD), citrate synthase (GltA), aconitate hydratase 1 (AcnA), aconitate hydratase 2 (AcnB), aconitate hydratase, putative (GSU2445), isocitrate dehydrogenase, NADP-dependent (Icd), 2-oxoglutarate:ferredoxin oxidoreductase, ferredoxin subunit (KorD), 2-oxoglutarate:ferredoxin oxidoreductase, alpha subunit (KorA), 2-oxoglutarate:ferredoxin oxidoreductase, thiamin diphosphate-binding subunit (KorB), 2-oxoglutarate:ferredoxin oxidoreductase, gamma subunit (KorC), 2-oxoglutarate dehydrogenase, E1 protein (SucA), 2-oxoglutarate dehydrogenase, E2 protein, dihydrolipoamide succinyltransferase (SucB), succinyl-CoA synthetase, beta subunit (SucC), succinyl-CoA synthetase, alpha subunit (SucD), succinate dehydrogenase/fumarate reductase, iron-sulfur protein (FrdB), succinate dehydrogenase/fumarate reductase, flavoprotein subunit (FrdA), succinate dehydrogenase/fumarate reductase, cytochrome b558 subunit (FrdC), fumarate hydratase, class I (FumB), malate dehydrogenase, NAD-dependent (Mdh), acetate kinase (AckA), chaperonin Hsp33 (HslO), phosphate acetyltransferase (Pta), succinyl:acetate coenzyme A transferase (Ato-2), succinyl:acetate coenzyme A transferase (Ato-1), pyruvate:ferredoxin/flavodoxin oxidoreductase (Por), pyruvate dehydrogenase E1 component subunit alpha (PdhA), pyruvate dehydrogenase E1 component subunit beta (PdhB), formate acetyltransferase/glycerol dehydratase, putative (GSU2101), NADP-dependent malic enzyme (MaeB), pyruvate kinase (Pyk), phosphoenolpyruvate synthase (PpsA), pyruvate phosphate dikinase (PpdK), phosphoenolpyruvate carboxykinase, GTP-dependent (PckA), pyruvate carboxylase (Pyc), enolase (Eno), phosphoglycerate mutase family protein (GSU1818), phosphoglycerate mutase, 2,3-bisphosphoglycerate-independent (GpmI), phosphoglycerate kinase (Pgk), glyceraldehyde-3-phosphate dehydrogenase, type I (GapA), aldehyde dehydrogenase (GSU1108), ketose-1,6-bisphosphate aldolase, class II, putative (GSU1193), ketose-1,6-bisphosphate aldolase, class II, putative (GSU1245), 6-phosphofructokinase (Pfk-1), 6-phosphofructokinase, ATP-dependent (Pfk-2), fructose-1,6-bisphosphatase (Fbp), glucose-6-phosphate isomerase (Pgi), acetolactate synthase (IlvB), ketol-acid reductoisomerase (IlvC), 2-isopropylmalate synthase (CimA), triose-phosphate isomerase (GSU1628), transketolase, C-terminal subunit (GSU2918), transketolase, N-terminal subunit (GSU2919), transaldolase (Tal), aspartate transaminase (GSU1061), threonine synthase (ThrC), (TdcB), 3-isopropylmalate dehydrogenase (LeuB), (GlyA), NADH oxidase, putative or FAD-dependent pyridine nucleotide-disulfide oxidoreductase family protein (FNOR), carbon monoxide dehydrogenase-associated iron-sulfur cluster-binding oxidoreductase (CooF), carbon monoxide dehydrogenase accessory protein (CooC), carbon monoxide dehydrogenase, catalytic subunit (CooS), sensory box protein (RcoM), bifunctional protein FolD 1 (FolD1), and 5-methyltetrahydrofolate-homocysteine S-methyltransferase and 5,10-methylenetetrahydrofolate reductase (MetF-2). Clustering shows that samples grouped according to treatments even when only enzymes in this set are considered (Supplementary Figure 6).
In the oxidation route of acetate, the abundance of CAC enzymes (
Succinyl-CoA synthetase subunits (SucA; GSU2449, SucB; GSU2448, SucC; GSU1058, and SucD; GSU1059) were mostly more abundant in the SF-GS coculture (2-, 2-, 31-, and 58-fold, respectively) compared to the GS pure culture (Figure 5). In the previous studies, GS in both types of cocultures (PC-GS and GM-GS) showed low expression of succinyl-CoA synthetase genes compared to the other enzymes of the CAC (
Hydrogenases and Formate Dehydrogenases of GS
GS has only one hydrogenase, a membrane-bound respiratory Hyb hydrogenase with a periplasmic-oriented active site that functions as uptake hydrogenase (
FIGURE 6

Relative abundance of the detected hydrogenases of GS in the SF-GS coculture versus the GS pure culture. Protein abundance levels are shown after Z-score normalization. The color intensity indicates the degree of protein presence, where high relative abundance is indicated in red and low relative abundance is indicated in blue. The rows in the heat map show the detected proteins in the SF-GS coculture and the GS pure culture. The columns show the cultures in replicates. The abbreviations of the proteins are as follows: Hyb: periplasmically oriented, membrane-bound [NiFe]-hydrogenase, small subunit (HybS), periplasmically oriented, membrane-bound [NiFe]-hydrogenase, iron-sulfur cluster-binding subunit (HybA), periplasmically oriented, membrane-bound [NiFe]-hydrogenase, cytochrome b subunit (HybB), periplasmically oriented, membrane-bound [NiFe]-hydrogenase, large subunit (HybL). Hya: periplasmically oriented, membrane-bound [NiFe]-hydrogenase, large subunit (HyaL). Hyp: hydrogenase accessory protein (HypB), hydrogenase maturation protein (HypF), hydrogenase expression/formation protein (HypD), hydrogenase expression/formation protein (HypE). Ehr: Ech-hydrogenase-related complex, NuoL-like integral membrane subunit (EhrA-1), Ech-hydrogenase-related complex, HyfE-like integral membrane subunit (EhrC), Ech-hydrogenase-related complex, large subunit (EhrL), Ech-hydrogenase-related complex, small subunit (EhrS). Hox: bidirectional NAD-reducing hydrogenase, small subunit (HoxS), bidirectional NAD-reducing hydrogenase, large subunit (HoxL). Mvh: methyl-accepting chemotaxis sensory transducer (MvhV). Hdr: heterodisulfide oxidoreductase, NAD(P)H oxidoreductase subunit F (HdrF), heterodisulfide oxidoreductase, iron-sulfur cluster-binding subunit E (HdrE), heterodisulfide oxidoreductase, iron-sulfur cluster-binding subunit D (HdrD), heterodisulfide oxidoreductase, iron-sulfur cluster-binding subunit G (HdrG), heterodisulfide oxidoreductase, FAD-binding and iron-sulfur cluster-binding subunit A (HdrA), heterodisulfide oxidoreductase subunit B (HdrB), heterodisulfide oxidoreductase, iron-sulfur cluster-binding subunit C (HdrC), Periplasmically oriented, membrane-bound formate dehydrogenase, major subunit, selenocysteine-containing (FdnG), periplasmically oriented, membrane-bound formate dehydrogenase, iron-sulfur cluster-binding subunit (FdnH), periplasmically oriented, membrane-bound formate dehydrogenase, cytochrome b subunit (FdnI). Clustering shows that samples grouped according to treatments even when only enzymes in this set are considered (Supplementary Figure 6).
Other hydrogenases such as Hya (GSU0120–0123), Hyp (GSU0305–0309 and GSU0374), Hox (GSU2717–2722), Mvh (GSU2416–2423), Hdr (GSU0085–0092), and Ehr (GSU0739–0745) that might be involved in hydrogen metabolism and not in hydrogen uptake (
To investigate if formate can function as an alternative interspecies electron carrier or together with hydrogen in the SF-GS coculture, protein abundance of all four formate dehydrogenase subunits (FdnG; GSU0777, FdnH; GSU0778, FdnI; GSU0779, and FdhD/mobA-2; GSU0780) was evaluated in this study. Interestingly, the abundance of formate dehydrogenase subunits was also significantly lower (45-, 20-, and 2-fold, respectively) in the SF-GS coculture compared to the GS pure culture, and FdhD/mobA-2 was not even detected in the SF-GS coculture (Figure 6). This further indicates that formate was unlikely an important carrier in interspecies electron transfer in the SF-GS coculture. In line with this, transcript abundance of formate dehydrogenase genes was also low in the GM-GS coculture versus the PC-GS coculture (
Electron Transport Proteins of GS
To reduce Fe(III) in the propionate-fed syntrophic coculture of SF-GS, electrons from propionate should be first transported, directly or through electron carriers (formate and hydrogen), to GS and then to Fe(III). This is likely mediated by respiratory chains consisting of c-type cytochromes of the inner membrane (e.g., MacA), periplasmic c-type cytochromes (e.g., PpcA and PpcB), outer membrane cytochromes (e.g., OmcB and OmcS), and menaquinone (MQ) that finally delivers electrons to Fe(III). Formate and hydrogen oxidation likely directly contribute to the proton motive force and electron flow to the MQ pool in the inner membrane of GS (
MacA (GSU0466), an inner membrane c-type cytochrome of GS, was detected with higher abundance (7-fold) in the SF-GS coculture compared to the GS pure culture (Figure 7). This may indicate the cytoplasmic oxidation of electron donors in GS (mainly acetate due to much higher abundance of enzymes involved in the acetate oxidation than those of formate and hydrogen in the SF-GS coculture), and extracellular electron transport from the inner membrane.
FIGURE 7

Abundance levels of the detected C-type cytochrome of GS in the SF-GS coculture versus the GS pure culture. Protein abundance levels are shown after Z-score normalization. The color intensity indicates the degree of protein presence, where high relative abundance is indicated in red and low relative abundance in blue. The rows in the heat map show the detected proteins in the SF-GS coculture and the GS pure culture. The columns show the cultures in replicates. Protein abbreviations are as follows: cytochrome c oxidase, coo3-type, synthesis factor (Sco), cytochrome c/cytochrome b (GSU0274), cytochrome c nitrite reductase (GSU0357), cytochrome c (PpcB), cytochrome c peroxidase (MacA), cytochrome c (GSU0591), lipoprotein cytochrome c (OmcQ), cytochrome c (GSU0594), ResB-like family cytochrome c biogenesis protein (GSU0613), ResC/HemX-like cytochrome c biogenesis membrane protein (GSU0614), cytochrome c (OmcE), lipoprotein cytochrome c (OmcX), lipoprotein cytochrome c (GSU0702), apocytochrome c disulfide reductase lipoprotein ResA (ResA), cytochrome c (GSU1334), cytochrome c (GSU1538), cytochrome c (GSU1648), cytochrome c, 1 heme-binding site (GSU1740), cytochrome c (GSU1996), cytochrome c (OmcS), lipoprotein cytochrome c, 1 heme-binding site (GSU2513), cytochrome c (GSU2724), lipoprotein cytochrome c (OmcC), lipoprotein cytochrome c (OmcB), cytochrome c, 1 heme-binding site (GSU2743), cytochrome c (GSU2801), lipoprotein cytochrome c (GSU2808), cytochrome c (GSU2811), cytochrome c peroxidase (CcpA), cytochrome c (OmcG), cytochrome c (GSU3615), lipoprotein cytochrome c (GSU2887), ResB-like family cytochrome c biogenesis protein (GSU2891), lipoprotein cytochrome c (OmcN), lipoprotein cytochrome c (GSU2899), cytochrome c (OmcO), cytochrome c (Dhc2), cytochrome c nitrite and sulfite reductase, catalytic subunit lipoprotein (NrfA), cytochrome c (GSU3259), and ResC/HemX-like cytochrome c biogenesis membrane protein (GSU3283). Clustering shows that samples grouped according to treatments even when only enzymes in this set are considered (Supplementary Figure 6).
To transfer electrons across the periplasm from electron donors that are metabolized in the cytoplasm, several small periplasmic cytochromes (Ppc) are involved. Of the five closely related periplasmic c-type cytochromes of GS (PpcA-E) (
Among the outer membrane cytochromes, OmcS (GSU2504) was reported to be essential for DIET in the adapted coculture of GM-GS (
OmcB (GSU2737), another outer membrane multiheme c-type cytochrome that is required for optimal Fe(III) reduction in GS, had lower abundance in the SF-GS coculture (5-fold) compared to the GS culture (Figure 7). This is consistent with lower expression of OmcB in GM-GS versus PC-GS (
Based on the genetic evidence, cytochromes are more likely than pili to mediate DIET in syntrophic interactions of Geobacter and methanogens (
Overall, the knowledge about DIET is still expanding and the mere presence of DIET-associated proteins cannot guarantee occurrence of DIET (
Conclusion
Here, we report a successful coculture of SF-GS on propionate and Fe(III). Neither of the two bacteria was capable of growth on propionate and Fe(III), indicating a syntrophic interaction. Using proteomic analyses, we detected low abundance of outer-surface c-type cytochromes and electrically conductive pili (e-pili) of GS that act as a Fe(III) reductase and as an electron carrier to other acceptors or to syntrophic partner bacteria respectively (
Publisher’s Note
All claims expressed in this article are solely those of the authors and do not necessarily represent those of their affiliated organizations, or those of the publisher, the editors and the reviewers. Any product that may be evaluated in this article, or claim that may be made by its manufacturer, is not guaranteed or endorsed by the publisher.
Statements
Data availability statement
The original contributions presented in the study are included in the article/Supplementary Material, further inquiries can be directed to the corresponding author.
Author contributions
MM, CP, and AS conceptualized and designed the experiments. MM, VS-N, and SB performed the experiments. MM, MS-D, and SB analyzed the data. All authors wrote the manuscript.
Funding
This work was performed in the TTIW-cooperation framework of Wetsus, European Centre of Excellence for Sustainable Water Technology (www.wetsus.nl). Wetsus was funded by the Dutch Ministry of Economic Affairs, the European Union Regional Development Fund, the Province of Fryslân, the City of Leeuwarden, and the EZ/Kompas program of the “Samenwerkingsverband Noord-Nederland”. Research of AJMS was financed by an advanced grant of the European Research Council under the European Union’s Seventh Framework Programme (FP/2007e2013)/ERC Grant Agreement (project 323009) and a Gravitation grant (project 024.002.002) of the Netherlands Ministry of Education, Culture and Science.
Acknowledgments
The authors thank the participants of the research theme “Resource Recovery” for fruitful discussions and their financial support.
Conflict of interest
The authors declare that the research was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest.
Supplementary material
The Supplementary Material for this article can be found online at: https://www.frontiersin.org/articles/10.3389/fmicb.2021.708911/full#supplementary-material
Footnotes
References
1
BaekG.KimJ.LeeC. (2019). A review of the effects of iron compounds on methanogenesis in anaerobic environments.Renewable Sustain. Energy Rev.113:109282. 10.1016/j.scitotenv.2019.133876
2
ButlerJ. E.YoungN. D.AklujkarM.LovleyD. R. (2012). Comparative genomic analysis of Geobacter sulfurreducens KN400, a strain with enhanced capacity for extracellular electron transfer and electricity production.BMC Genomics13:471. 10.1186/1471-2164-13-471
3
ChenH.BoutrosP. C. (2011). VennDiagram: a package for the generation of highly-customizable Venn and Euler diagrams in R.BMC Bioinform.12:35. 10.1186/1471-2105-12-35
4
ClesceriL. S.GreenbergA. E.TrusselR. R.(eds). (1995). Standard Methods for the Examination of Water and Wastewater, 19th Edn. Washington, DC: APHA-AWWA-WEF.
5
CoppiM. V.O’neilR. A.LovleyD. R. (2004). Identification of an uptake hydrogenase required for hydrogen-dependent reduction of Fe (III) and other electron acceptors by Geobacter sulfurreducens.J. Bacteriol.1863022–3028. 10.1128/JB.186.10.3022-3028.2004
6
Cord-RuwischR.LovleyD. R.SchinkB. (1998). Growth of Geobacter sulfurreducens with acetate in syntrophic cooperation with hydrogen-oxidizing anaerobic partners.Appl. Environ. Microbiol.642232–2236. 10.1128/AEM.64.6.2232-2236.1998
7
DongX.PluggeC. M.StamsA. J. (1994). Anaerobic degradation of propionate by a mesophilic acetogenic bacterium in coculture and triculture with different methanogens.Appl. Environ. Microbiol.602834–2838. 10.1128/aem.60.8.2834-2838.1994
8
DongX.StamsA. J. (1995). Evidence for H2 and formate formation during syntrophic butyrate and propionate degradation.Anaerobe135–39. 10.1016/s1075-9964(95)80405-6
9
GalushkoA. S.SchinkB. (2000). Oxidation of acetate through reactions of the citric acid cycle by Geobacter sulfurreducens in pure culture and in syntrophic coculture.Arch. Microbiol.174314–321. 10.1007/s002030000208
10
GhasimiS.IdrisA.ChuahT.TeyB. (2009). The Effect of C: N: P ratio, volatile fatty acids and Na levels on the performance of an anaerobic treatment of fresh leachate from municipal solid waste transfer station.Afr. J. Biotechnol.84572–4581.
11
HarmsenH. J.Van KuijkB. L.PluggeC. M.AkkermansA. D.De VosW. M.StamsA. J. (1998). Syntrophobacter fumaroxidans sp. nov., a syntrophic propionate-degrading sulfate-reducing bacterium.Int. J. Syst. Evolutionary Microbiol.481383–1387. 10.1099/00207713-48-4-1383
12
JuárezK.KimB.-C.NevinK.OlveraL.RegueraG.LovleyD. R.et al (2009). PilR, a transcriptional regulator for pilin and other genes required for Fe (III) reduction in Geobacter sulfurreducens.J. Mol. Microbiol. Biotechnol.16146–158. 10.1159/000115849
13
KasparH. F.WuhrmannK. (1977). Product inhibition in sludge digestion.Microb. Ecol.4241–248.
14
LiY.YuS.StrongJ.WangH. (2012). Are the biogeochemical cycles of carbon, nitrogen, sulfur, and phosphorus driven by the “Fe III–Fe II redox wheel” in dynamic redox environments?J. Soils Sediments12683–693. 10.1007/s11368-012-0507-z
15
LiuR.TianQ.YangB.ChenJ. (2010). Hybrid anaerobic baffled reactor for treatment of desizing wastewater.Int. J. Environ. Sci. Technol.7111–118. 10.1007/bf03326122
16
LiuX.ZhuoS.RensingC.ZhouS. (2018). Syntrophic growth with direct interspecies electron transfer between pili-free Geobacter species.ISME J.122142–2151. 10.1038/s41396-018-0193-y
17
MahadevanR.BondD. R.ButlerJ. E.Esteve-NunezA.CoppiM. V.PalssonB. O.et al (2006). Characterization of metabolism in the Fe (III)-reducing organism Geobacter sulfurreducens by constraint-based modeling.Appl. Environ. Microbiol.721558–1568. 10.1128/AEM.72.2.1558-1568.2006
18
MahadevanR.PalssonB. O.LovleyD. R. (2011). In situ to in silico and back: elucidating the physiology and ecology of Geobacter spp. using genome-scale modelling.Nat. Rev. Microbiol.939–50. 10.1038/nrmicro2456
19
MalvankarN. S.VargasM.NevinK. P.FranksA. E.LeangC.KimB.-C.et al (2011). Tunable metallic-like conductivity in microbial nanowire networks.Nat. Nanotechnol.6573–579. 10.1038/nnano.2011.119
20
MetheB.NelsonK. E.EisenJ. A.PaulsenI. T.NelsonW.HeidelbergJ.et al (2003). Genome of Geobacter sulfurreducens: metal reduction in subsurface environments. Science302, 1967–1969. 10.1126/science.1088727
21
MolenaarS. D.ElzingaM.WillemseS. G.SleutelsT.Ter HeijneA.BuismanC. J. (2019). Comparison of two sustainable counter electrodes for energy storage in the microbial rechargeable battery.ChemElectroChem62464–2473. 10.1002/celc.201900470
22
MollaeiM.TimmersP. H.Suarez-DiezM.BoerenS.Van GelderA. H.StamsA. J.et al (2021). Comparative proteomics of Geobacter sulfurreducens PCAT in response to acetate, formate and/or hydrogen as electron donor.Environ. Microbiol.23299–315. 10.1111/1462-2920.15311
23
MüllerN.WormP.SchinkB.StamsA. J.PluggeC. M. (2010). Syntrophic butyrate and propionate oxidation processes: from genomes to reaction mechanisms.Environ. Microbiol. Rep.2489–499. 10.1111/j.1758-2229.2010.00147.x
24
OtwellA. E.CallisterS. J.SherwoodR. W.ZhangS.GoldmanA. R.SmithR. D.et al (2018). Physiological and proteomic analyses of Fe (III)-reducing co-cultures of Desulfotomaculum reducens MI-1 and Geobacter sulfurreducens PCA.Geobiology161–18. 10.1111/gbi.12295
25
PluggeC. M.DijkemaC.StamsA. J. (1993). Acetyl-CoA cleavage pathway in a syntrophic propionate oxidizing bacterium growing on fumarate in the absence of methanogens.FEMS Microbiol. Lett.11071–76. 10.1111/j.1574-6968.1993.tb06297.x
26
PluggeC. M.HenstraA. M.WormP.SwartsD. C.Paulitsch-FuchsA. H.ScholtenJ. C.et al (2012). Complete genome sequence of Syntrophobacter fumaroxidans strain (MPOB T).Standards Genomic Sci.791–106. 10.4056/sigs.2996379
27
R Core Team. (2016). R: A Language and Environment for Statistical Computing.Vienna: R Core Team.
28
RegueraG.KashefiK. (2019). The electrifying physiology of Geobacter bacteria, 30 years on.Adv. Microb. Physiol.741–96. 10.1016/bs.ampbs.2019.02.007
29
RissoC.MetheB. A.ElifantzH.HolmesD. E.LovleyD. R. (2008). Highly conserved genes in Geobacter species with expression patterns indicative of acetate limitation.Microbiology1542589–2599. 10.1099/mic.0.2008/017244-0
30
RotaruA.-E.ShresthaP. M.LiuF.ShresthaM.ShresthaD.EmbreeM.et al (2014b). A new model for electron flow during anaerobic digestion: direct interspecies electron transfer to Methanosaeta for the reduction of carbon dioxide to methane.Energy Environ. Sci.7408–415. 10.1039/c3ee42189a
31
RotaruA.-E.ShresthaP. M.LiuF.MarkovaiteB.ChenS.NevinK. P.et al (2014a). Direct interspecies electron transfer between Geobacter metallireducens and Methanosarcina barkeri.Appl. Environ. Microbiol.804599–4605. 10.1128/AEM.00895-14
32
RotaruA.-E.ShresthaP. M.LiuF.UekiT.NevinK.SummersZ. M.et al (2012). Interspecies electron transfer via hydrogen and formate rather than direct electrical connections in cocultures of Pelobacter carbinolicus and Geobacter sulfurreducens.Appl. Environ. Microbiol.787645–7651. 10.1128/AEM.01946-12
33
RotaruA.-E.WoodardT. L.NevinK. P.LovleyD. R. (2015). Link between capacity for current production and syntrophic growth in Geobacter species.Front. Microbiol.6:744. 10.3389/fmicb.2015.00744
34
SchinkB.StamsA. J. (2006). Syntrophism among prokaryotes.Prokaryotes2309–335. 10.1007/0-387-30742-7_11
35
Sedano-NúñezV. T.BoerenS.StamsA. J.PluggeC. M. (2018). Comparative proteome analysis of propionate degradation by Syntrophobacter fumaroxidans in pure culture and in coculture with methanogens.Environ. Microbiol.201842–1856. 10.1111/1462-2920.14119
36
SeguraD.MahadevanR.JuárezK.LovleyD. R. (2008). Computational and experimental analysis of redundancy in the central metabolism of Geobacter sulfurreducens.PLoS Computat. Biol.4:e36. 10.1371/journal.pcbi.0040036
37
ShahB.ShahA.SinghR. (2009). Sorption isotherms and kinetics of chromium uptake from wastewater using natural sorbent material.Int. J. Environ. Sci. Technol.677–90. 10.1007/bf03326062
38
ShresthaP. M.RotaruA.-E. (2014). Plugging in or going wireless: strategies for interspecies electron transfer.Front. Microbiol.5:237. 10.3389/fmicb.2014.00237
39
ShresthaP. M.RotaruA.-E.SummersZ. M.ShresthaM.LiuF.LovleyD. R. (2013). Transcriptomic and genetic analysis of direct interspecies electron transfer.Appl. Environ. Microbiol.792397–2404. 10.1128/AEM.03837-12
40
StamsA. J.Van DijkJ. B.DijkemaC.PluggeC. M. (1993). Growth of syntrophic propionate-oxidizing bacteria with fumarate in the absence of methanogenic bacteria.Appl. Environ. Microbiol.591114–1119. 10.1128/aem.59.4.1114-1119.1993
41
StookeyL. L. (1970). Ferrozine—a new spectrophotometric reagent for iron.Analytical Chem.42779–781. 10.1021/ac60289a016
42
SummersZ. M.FogartyH. E.LeangC.FranksA. E.MalvankarN. S.LovleyD. R. (2010). Direct exchange of electrons within aggregates of an evolved syntrophic coculture of anaerobic bacteria.Science3301413–1415. 10.1126/science.1196526
43
ThauerR. K.JungermannK.DeckerK. (1977). Energy conservation in chemotrophic anaerobic bacteria.Bacteriol. Rev.41100–180. 10.1128/mmbr.41.1.100-180.1977
44
TremblayP.-L.LovleyD. R. (2012). Role of the NiFe hydrogenase Hya in oxidative stress defense in Geobacter sulfurreducens.J. Bacteriol.1942248–2253. 10.1128/JB.00044-12
45
UekiT.LovleyD. R. (2010). Genome-wide gene regulation of biosynthesis and energy generation by a novel transcriptional repressor in Geobacter species.Nucleic Acids Res.38810–821. 10.1093/nar/gkp1085
46
UekiT.NevinK. P.RotaruA.-E.WangL.-Y.WardJ. E.WoodardT. L.et al (2018). Geobacter strains expressing poorly conductive pili reveal constraints on direct interspecies electron transfer mechanisms.MBio9e1273–e1218. 10.1128/mBio.01273-18
47
Van KuijkB. L.HagenW. R.StamsA. J. (1998). Isolation and Properties of the Oxygen-Sensitive Fumarate Reductase of the Syntrophic Propionate-Oxidizing Bacterium Strain MPOB. Ph. D. thesis.Wageningen: Wageningen University. 71–88.
48
Van KuijkB. L.StamsA. J. (1995). Sulfate reduction by a syntrophic propionate-oxidizing bacterium.Antonie van Leeuwenhoek68293–296. 10.1007/bf00874139
49
Van LierJ. B.MartinJ. L. S.LettingaG. (1996). Effect of temperature on the anaerobic thermophilic conversion of volatile fatty acids by dispersed and granular sludge.Water Res.30199–207. 10.1016/0043-1354(95)00107-v
50
Van SteendamC.SmetsI.SkerlosS.RaskinL. (2019). Improving anaerobic digestion via direct interspecies electron transfer requires development of suitable characterization methods.Curr. Opin. Biotechnol.57183–190. 10.1016/j.copbio.2019.03.018
51
VizcaínoJ. A.CsordasA.Del-ToroN.DianesJ. A.GrissJ.LavidasI.et al (2016). 2016 update of the PRIDE database and its related tools.Nucleic Acids Res.44D447–D456.
52
WangT.ZhuG.KuangB.JiaJ.LiuC.CaiG.et al (2021). Novel insights into the anaerobic digestion of propionate via Syntrophobacter fumaroxidans and Geobacter sulfurreducens: process and mechanism.Water Res.200117270. 10.1016/j.watres.2021.117270
53
WormP. (2010). Formate Dehydrogenases and Hydrogenases in Syntrophic Propionate-Oxidizing Communities: Gene Analysis and Transcritional Profiling.Wageningen: Wageningen University.
54
WormP.StamsA. J.ChengX.PluggeC. M. (2011). Growth-and substrate-dependent transcription of formate dehydrogenase and hydrogenase coding genes in Syntrophobacter fumaroxidans and Methanospirillum hungatei.Microbiology157280–289. 10.1099/mic.0.043927-0
55
ZhangT.ShiX.-C.DingR.XuK.TremblayP.-L. (2020). The hidden chemolithoautotrophic metabolism of Geobacter sulfurreducens uncovered by adaptation to formate.ISME J.142078–2089. 10.1038/s41396-020-0673-8
Summary
Keywords
Syntrophobacter fumaroxidans, Geobacter sulfurreducens, coculture, interspecies electron transfer, propionate, proteomics
Citation
Mollaei M, Suarez-Diez M, Sedano-Nunez VT, Boeren S, Stams AJM and Plugge CM (2021) Proteomic Analysis of a Syntrophic Coculture of Syntrophobacter fumaroxidans MPOBT and Geobacter sulfurreducens PCAT. Front. Microbiol. 12:708911. doi: 10.3389/fmicb.2021.708911
Received
12 May 2021
Accepted
04 November 2021
Published
30 November 2021
Volume
12 - 2021
Edited by
Matthias Boll, University of Freiburg, Germany
Reviewed by
Pengfei Liu, Lanzhou University, China; Ivan A. Berg, University of Münster, Germany
Updates

Check for updates
Copyright
© 2021 Mollaei, Suarez-Diez, Sedano-Nunez, Boeren, Stams and Plugge.
This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.
*Correspondence: Caroline M. Plugge, caroline.plugge@wur.nl
†Present address: Vicente T. Sedano-Nunez, Chr. Hansen A/S, Hørsholm, Denmark
This article was submitted to Microbial Physiology and Metabolism, a section of the journal Frontiers in Microbiology
Disclaimer
All claims expressed in this article are solely those of the authors and do not necessarily represent those of their affiliated organizations, or those of the publisher, the editors and the reviewers. Any product that may be evaluated in this article or claim that may be made by its manufacturer is not guaranteed or endorsed by the publisher.