Current views on the regulation of autotrophic carbon dioxide fixation via the Calvin cycle in bacteria

Enrichment and characterization of a nitric oxide-reducing microbial community in a continuous bioreactor

Nitric oxide (NO) is a highly reactive and climate-active molecule and a key intermediate in the microbial nitrogen cycle. Despite its role in the evolution of denitrification and aerobic respiration, high redox potential and capacity to sustain microbial growth, our understanding of NO-reducing microorganisms remains limited due to the absence of NO-reducing microbial cultures obtained directly from the environment using NO as a substrate. Here, using a continuous bioreactor and a constant supply of NO as the sole electron acceptor, we enriched and characterized a microbial community dominated by two previously unknown microorganisms that grow at nanomolar NO concentrations and survive high amounts (>6 µM) of this toxic gas, reducing it to N2 with little to non-detectable production of the greenhouse gas nitrous oxide. These results provide insight into the physiology of NO-reducing microorganisms, which have pivotal roles in the control of climate-active gases, waste removal, and evolution of nitrate and oxygen respiration.

Aerobic methanotrophy increases the net iron reduction in methanogenic lake sediments

In methane (CH4) generating sediments, methane oxidation coupled with iron reduction was suggested to be catalyzed by archaea and bacterial methanotrophs of the order Methylococcales. However, the co-existence of these aerobic and anaerobic microbes, the link between the processes, and the oxygen requirement for the bacterial methanotrophs have remained unclear. Here, we show how stimulation of aerobic methane oxidation at an energetically low experimental environment influences net iron reduction, accompanied by distinct microbial community changes and lipid biomarker patterns. We performed incubation experiments (between 30 and 120 days long) with methane generating lake sediments amended with 13C-labeled methane, following the additions of hematite and different oxygen levels in nitrogen headspace, and monitored methane turnover by 13C-DIC measurements. Increasing oxygen exposure (up to 1%) promoted aerobic methanotrophy, considerable net iron reduction, and the increase of microbes, such as Methylomonas, Geobacter, and Desulfuromonas, with the latter two being likely candidates for iron recycling. Amendments of 13C-labeled methanol as a potential substrate for the methanotrophs under hypoxia instead of methane indicate that this substrate primarily fuels methylotrophic methanogenesis, identified by high methane concentrations, strongly positive δ13CDIC values, and archaeal lipid stable isotope data. In contrast, the inhibition of methanogenesis by 2-bromoethanesulfonate (BES) led to increased methanol turnover, as suggested by similar 13C enrichment in DIC and high amounts of newly produced bacterial fatty acids, probably derived from heterotrophic bacteria. Our experiments show a complex link between aerobic methanotrophy and iron reduction, which indicates iron recycling as a survival mechanism for microbes under hypoxia.

Influence of Hydrogen Electron Donor, Alkaline pH, and High Nitrate Concentrations on Microbial Denitrification: A Review

Bacterial respiration of nitrate is a natural process of nitrate reduction, which has been industrialized to treat anthropic nitrate pollution. This process, also known as “microbial denitrification”, is widely documented from the fundamental and engineering points of view for the enhancement of the removal of nitrate in wastewater. For this purpose, experiments are generally conducted with heterotrophic microbial metabolism, neutral pH and moderate nitrate concentrations (<50 mM). The present review focuses on a different approach as it aims to understand the effects of hydrogenotrophy, alkaline pH and high nitrate concentration on microbial denitrification. Hydrogen has a high energy content but its low solubility, 0.74 mM (1 atm, 30 °C), in aqueous medium limits its bioavailability, putting it at a kinetic disadvantage compared to more soluble organic compounds. For most bacteria, the optimal pH varies between 7.5 and 9.5. Outside this range, denitrification is slowed down and nitrite (NO₂⁻) accumulates. Some alkaliphilic bacteria are able to express denitrifying activity at pH levels close to 12 thanks to specific adaptation and resistance mechanisms detailed in this manuscript, and some bacterial populations support nitrate concentrations in the range of several hundred mM to 1 M. A high concentration of nitrate generally leads to an accumulation of nitrite. Nitrite accumulation can inhibit bacterial activity and may be a cause of cell death.

Prokaryotic Responses to Ammonium and Organic Carbon Reveal Alternative CO2 Fixation Pathways and Importance of Alkaline Phosphatase in the Mesopelagic North Atlantic

To decipher the response of mesopelagic prokaryotic communities to input of nutrients, we tracked changes in prokaryotic abundance, extracellular enzymatic activities, heterotrophic production, dark dissolved inorganic carbon (DIC) fixation, community composition (16S rRNA sequencing) and community gene expression (metatranscriptomics) in 3 microcosm experiments with water from the mesopelagic North Atlantic. Responses in 3 different treatments amended with thiosulfate, ammonium or organic matter (i.e., pyruvate plus acetate) were compared to unamended controls. The strongest stimulation was found in the organic matter enrichments, where all measured rates increased >10-fold. Strikingly, in the organic matter treatment, the dark DIC fixation rates-assumed to be related to autotrophic metabolisms-were equally stimulated as all the other heterotrophic-related parameters. This increase in DIC fixation rates was paralleled by an up-regulation of genes involved in DIC assimilation via anaplerotic pathways. Alkaline phosphatase was the metabolic rate most strongly stimulated and its activity seemed to be related to cross-activation by nonpartner histidine kinases, and/or the activation of genes involved in the regulation of elemental balance during catabolic processes. These findings suggest that episodic events such as strong sedimentation of organic matter into the mesopelagic might trigger rapid increases of originally rare members of the prokaryotic community, enhancing heterotrophic and autotrophic carbon uptake rates, ultimately affecting carbon cycling. Our experiments highlight a number of fairly unstudied microbial processes of potential importance in mesopelagic waters that require future attention.

Assembly and catalysis of molybdenum or tungsten-containing formate dehydrogenases from bacteria

The global carbon cycle depends on the biological transformations of C1 compounds, which include the reductive incorporation of CO₂into organic molecules (e.g. in photosynthesis and other autotrophic pathways), in addition to the production of CO₂from formate, a reaction that is catalyzed by formate dehydrogenases (FDHs). FDHs catalyze, in general, the oxidation of formate to CO₂and H⁺. However, selected enzymes were identified to act as CO₂reductases, which are able to reduce CO₂to formate under physiological conditions. This reaction is of interest for the generation of formate as a convenient storage form of H₂for future applications. Cofactor-containing FDHs are found in anaerobic bacteria and archaea, in addition to facultative anaerobic or aerobic bacteria. These enzymes are highly diverse and employ different cofactors such as the molybdenum cofactor (Moco), FeS clusters and flavins, or cytochromes. Some enzymes include tungsten (W) in place of molybdenum (Mo) at the active site. For catalytic activity, a selenocysteine (SeCys) or cysteine (Cys) ligand at the Mo atom in the active site is essential for the reaction. This review will focus on the characterization of Mo- and W-containing FDHs from bacteria, their active site structure, subunit compositions and its proposed catalytic mechanism. We will give an overview on the different mechanisms of substrate conversion available so far, in addition to providing an outlook on bio-applications of FDHs. This article is part of a Special Issue entitled: Cofactor-dependent proteins: evolution, chemical diversity and bio-applications.

Heterotrophic bicarbonate assimilation is the main process of de novo organic carbon synthesis in hadal zone of the Hellenic Trench, the deepest part of Mediterranean Sea

Ammonium-oxidizing chemoautotrophic members of Thaumarchaea are proposed to be the key players in the assimilation of bicarbonate in the dark (ABD). However, this process may also involve heterotrophic metabolic pathways, such as fixation of carbon dioxide (CO2) via various anaplerotic reactions. We collected samples from the depth of 4900 m at the Matapan-Vavilov Deep (MVD) station (Hellenic Trench, Eastern Mediterranean) and used the multiphasic approach to study the ABD mediators in this deep-sea ecosystem. At this depth, our analysis indicated the occurrence of actively CO2-fixing heterotrophic microbial assemblages dominated by Gammaproteobacteria with virtually no Thaumarchaea present. [14C]-bicarbonate incorporation experiments combined with shotgun [14C]-proteomic analysis identified a series of proteins of gammaproteobacterial origin. More than quarter of them were closely related with Alteromonas macleodii ‘deep ecotype’ AltDE, the predominant organism in the microbial community of MVD. The present study demonstrated that in the aphotic/hadal zone of the Mediterranean Sea, the assimilation of bicarbonate is associated with both chemolithoauto- and heterotrophic ABD. In some deep-sea areas, the latter may predominantly contribute to the de novo synthesis of organic carbon which points at the important and yet underestimated role heterotrophic bacterial populations can play the in global carbon cycle/sink in the ocean interior.

Dynamics of metabolic activities and gene expression in the Roseobacter clade bacterium Phaeobacter sp. strain MED193 during growth with thiosulfate

Metagenomic analyses of surface seawater reveal that genes for sulfur oxidation are widespread in bacterioplankton communities. However, little is known about the metabolic processes used to exploit the energy potentially gained from inorganic sulfur oxidation in oxic seawater. We therefore studied the sox gene system containing Roseobacter clade isolate Phaeobacter sp. strain MED193 in acetate minimal medium with and without thiosulfate. The addition of thiosulfate enhanced the bacterial growth yields up to 40% in this strain. Concomitantly, soxB and soxY gene expression increased about 8-fold with thiosulfate and remained 11-fold higher than that in controls through stationary phase. At stationary phase, thiosulfate stimulated protein synthesis and anaplerotic CO2 fixation rates up to 5- and 35-fold, respectively. Several genes involved in anaplerotic CO2 fixation (i.e., pyruvate carboxylase, propionyl coenzyme A [CoA], and crotonyl-CoA carboxylase) were highly expressed during active growth, coinciding with high CO2 fixation rates. The high expression of key genes in the ethylmalonyl-CoA pathway suggests that this is an important pathway for the utilization of two-carbon compounds in Phaeobacter sp. MED193. Overall, our findings imply that Roseobacter clade bacteria carrying sox genes can use their lithotrophic potential to gain additional energy from sulfur oxidation for both increasing their growth capacity and improving their long-term survival.

Dark carbon fixation: an important process in lake sediments

Close to redox boundaries, dark carbon fixation by chemoautotrophic bacteria may be a large contributor to overall carbon fixation. Still, little is known about the relative importance of this process in lake systems, in spite the potentially high chemoautotrophic potential of lake sediments. We compared rates of dark carbon fixation, bacterial production and oxygen consumption in sediments from four Swedish boreal and seven tropical Brazilian lakes. Rates were highly variable and dark carbon fixation amounted up to 80% of the total heterotrophic bacterial production. The results indicate that non-photosynthetic carbon fixation can represent a substantial contribution to bacterial biomass production, especially in sediments with low organic matter content.

Contribution of Crenarchaeota and Bacteria to autotrophy in the North Atlantic interior

Marine Crenarchaeota are among the most abundant groups of prokaryotes in the ocean and recent reports suggest that they oxidize ammonia as an energy source and inorganic carbon as carbon source, while other studies indicate that Crenarchaeota use organic carbon and hence, live heterotrophically. We used catalysed reporter deposition fluorescence in situ hybridization (CARD-FISH) to determine the crenarchaeal and bacterial contribution to total prokaryotic abundance in the (sub)tropical Atlantic. Bacteria contributed ~ 50% to total prokaryotes throughout the water column. Marine Crenarchaeota Group I (MCGI) accounted for ~ 5% of the prokaryotes in subsurface waters (100 m depth) and between 10 and 20% in the oxygen minimum layer (250-500 m depth) and deep waters (North East Atlantic Deep Water). The fraction of both MCGI and Bacteria fixing inorganic carbon, determined by combining microautoradiography with CARD-FISH (MICRO-CARD-FISH), decreased with depth, ranging from ~ 30% in the oxygen minimum zone to < 10% in the intermediate waters (Mediterranean Sea Outflow Water, Antarctic Intermediate Water). In the deeper water masses, however, MCGI were not taking up inorganic carbon. Using quantitative MICRO-CARD-FISH to determine autotrophy activity on a single cell level revealed that MCGI are incorporating inorganic carbon (0.002-0.1 fmol C cell⁻¹ day⁻¹) at a significantly lower rate than Bacteria (0.01-0.6 fmol C cell⁻¹ day⁻¹). Hence, it appears that MCGI contribute substantially less to autotrophy than Bacteria. Taking the stoichiometry of nitrification together with our findings suggests that MCGI might not dominate the ammonia oxidation step in the mesopelagic waters of the ocean to that extent as the reported dominance of archaeal over bacterial amoA would suggest.

Metabolic signals that lead to control of CBB gene expression in Rhodobacter capsulatus

Various mutant strains were used to examine the regulation and metabolic control of the Calvin-Benson-Bassham (CBB) reductive pentose phosphate pathway in Rhodobacter capsulatus. Previously, a ribulose 1,5-bisphosphate carboxylase/oxygenase (RubisCO)-deficient strain (strain SBI/II) was found to show enhanced levels of cbb(I) and cbb(II) promoter activities during photoheterotrophic growth in the presence of dimethyl sulfoxide. With this strain as the starting point, additional mutations were made in genes encoding phosphoribulokinase and transketolase and in the gene encoding the LysR-type transcriptional activator, CbbR(II). These strains revealed that a product generated by phosphoribulokinase was involved in control of CbbR-mediated cbb gene expression in SBI/II. Additionally, heterologous expression experiments indicated that Rhodobacter sphaeroides CbbR responded to the same metabolic signal in R. capsulatus SBI/II and mutant strain backgrounds.

Xanthobacter flavus employs a single triosephosphate isomerase for heterotrophic and autotrophic metabolism

The expression of the cbb and gap-pgk operons of Xanthobacter flavus encoding enzymes of the Calvin cycle is regulated by the transcriptional regulator CbbR. In order to identify other genes involved in the regulation of these operons, a mutant was isolated with a lowered activity of a fusion between the promoter of the cbb operon and the reporter gene lacZ. This mutant was unable to grow autotrophically and had a reduced growth rate on medium supplemented with gluconate or succinate. The regulation of the gap-pgk operon in the mutant was indistinguishable from the wild-type strain, but induction of the cbb operon upon transition to autotrophic growth conditions was delayed. Complementation of the mutant with a genomic library of X. flavus resulted in the isolation of a 1.1 kb ApaI fragment which restored autotrophic growth of the mutant. One open reading frame (ORF) was present on the ApaI fragment, which could encode a protein highly similar to triosephosphate isomerase proteins from other bacteria. Cell extracts of the mutant grown under glycolytic or gluconeogenic conditions had severely reduced triosephosphate isomerase activities. The ORF was therefore identified as tpi, encoding triosephosphate isomerase. The tpi gene is not linked to the previously identified operons encoding Calvin cycle enzymes and therefore represents a third transcriptional unit required for autotrophic metabolism.

Characterisation of carbon dioxide-inducible genes of the marine bacterium, Pseudomonas sp. S91

Characterisation of two genes in Pseudomonas sp. S91 that are responsive to carbon dioxide is reported. These were identified by random transposon mutagenesis leading to fusion of the Escherichia coli lacZ reporter gene to the genes of interest. Expression of the genes' promoters was quantified by measuring the reporter gene product, beta-galactosidase. beta-Galactosidase synthesis was induced when cells were exposed to 10% CO2 on solid media or during growth in aqueous phase when the culture density was greater than 1 at 610 nm, in either rich or minimal media. Induction of beta-galactosidase synthesis was not due to: increased alkalinity, onset of stationary phase, build up of soluble metabolites in the culture supernatant, or cell density-dependent signalling. The CO2-inducible gene fusions were not induced by other environmental conditions that are known to stimulate global regulators of environmental gene expression. Benzoic acid (2 mM) induced beta-galactosidase synthesis in one of the mutants indicating the Co2 response may involve the intracellular CO2 partial pressure/bicarbonate ion concentration/pH equilibrium.

The Calvin cycle enzyme phosphoglycerate kinase of Xanthobacter flavus required for autotrophic CO2 fixation is not encoded by the cbb operon

During autotrophic growth of Xanthobacter flavus, energy derived from the oxidation of hydrogen methanol or formate is used to drive the assimilation of CO2 via the Calvin cycle. The genes encoding the Calvin cycle enzymes are organized in the cbb operon, which is expressed only during autotrophic growth. Although it has been established that the transcriptional activator CbbR is required for the expression of the cbb operon, it is unclear whether CbbR is the only factor contributing to the regulation of the cbb operon. This paper describes the isolation of X. flavus mutants which were affected in the regulation of the cbb operon. One of the mutant strains was subject to an enhanced repression of the cbb operon promoter by the gluconeogenic substrate succinate and in addition failed to grow autotrophically. The rate of growth of the X. flavus mutant on succinate-containing medium was lower than that of the wild-type strain, but rates of growth on medium supplemented with gluconate were identical. A genomic library of X. flavus was constructed and was used to complement the mutant strain. The nucleotide sequence of the DNA fragment required to restore autotrophic growth of the X. flavus mutant was determined. One open reading frame that displayed extensive similarities to phosphoglycerate kinase-encoding genes (pgk) was identified. The X. flavus mutant lacked phosphoglycerate kinase activity following growth on gluconate or succinate. Introduction of the pgk gene into the X. flavus mutant partially restored the activity of phosphoglycerate kinase. Induction of the cbb operon of the X. flavus wild-type strain resulted in a simultaneous and parallel increase in the activities of ribulose-1,5-biphosphate carboxylase and phosphoglycerate kinase, whereas the latter activity remained absent in the X. flavus pgk mutant. It is concluded that X. flavus employees a single phosphoglycerate kinase enzyme and this is not encoded within the cbb operon.

Characterization of Xanthobacter strains H4-14 and 25a and enzyme profiles after growth under autotrophic and heterotrophic conditions

All Xanthobacter strains studied are versatile autotrophic bacteria, able to grow on methanol and other substrates. Strain 25a, a yellow-pigmented, pleomorphic, Gram-negative bacterium, capable of autotrophic growth on methanol, formate, thiosulfate, and molecular hydrogen, was isolated from an enrichment culture inoculated with soil from a subtropical greenhouse. Subsequent studies showed that the organism also grows on a wide range of multicarbon substrates. Ammonia, nitrate and molecular nitrogen were used as nitrogen sources. The taxonomic relationship of strains H4-14 and 25a with previously described Xanthobacter strains was studied by numerical classification. Strain H4-14 was identified as a X. flavus strain, but the precise position of strain 25a remained uncertain. It probably belongs to a new species of the genus Xanthobacter. The levels of various enzymes involved in autotrophic and heterotrophic metabolism were determined following growth of strains H4-14 and 25a in batch and continuous cultures. The mechanisms involved in controlling ribulose-1,5-bisphosphate carboxylase/oxygenase synthesis in Xanthobacter strains appear to be comparable to those observed for other autotrophic bacteria, namely repression by organic compounds and derepression by autotrophic energy sources, such as methanol and hydrogen.

Molecular and cellular regulation of autotrophic carbon dioxide fixation in microorganisms

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