Rates of microbial hydrogen oxidation and sulfate reduction in Opalinus Clay rock

Hydrogen gas (H2) may be produced by the anoxic corrosion of steel components in underground structures, such as geological repositories for radioactive waste. In such environments, hydrogen was shown to serve as an electron donor for autotrophic bacteria. High gas overpressures are to be avoided in radioactive waste repositories and, thus, microbial consumption of H2 is generally viewed as beneficial. However, to fully consider this biological process in models of repository evolution over time, it is crucial to determine the in situ rates of microbial hydrogen oxidation and sulfate reduction. These rates were estimated through two distinct in situ experiments, using several measurement and calculation methods. Volumetric consumption rates were calculated to be between 1.13 and 1.93 μmol cm−3 day−1 for H2, and 0.14 and 0.20 μmol cm−3 day−1 for sulfate. Based on the stoichiometry of the reaction, there is an excess of H2 consumed, suggesting that it serves as an electron donor to reduce electron acceptors other than sulfate, and/or that some H2 is lost via diffusion. These rate estimates are critical to evaluate whether biological H2 consumption can negate H2 production in repositories, and to determine whether sulfate reduction can consume sulfate faster than it is replenished by diffusion, which could lead to methanogenic conditions.

H2-fuelled microbial metabolism in Opalinus Clay

Rizlan Bernier-Latmani, Aislinn Ann Boylan, Niels Burzan, Luca Loreggian, Carla Perez Mon

In Switzerland, the Opalinus Clay formation is considered the most likely host rock for a deep geological repository for nuclear waste. In deep geological repositories, H2 is expected to be the most abundant gas formed from the degradation of waste and from metal corrosion. The microbial community present in Opalinus Clay is capable of utilizing H2 as an electron donor and sulfate as an electron acceptor to produce hydrogen sulfide. This could be problematic due to its potential for increasing the corrosion of metal waste canisters containing radioactive waste, however, the possible impacts of these processes on the clay rock have not been fully investigated. In this study, a series of microcosm experiments were set-up containing Opalinus Clay and porewater from the Mont Terri underground research laboratory (Switzerland) as an inoculum. Uninoculated microcosms were established to investigate abiotic processes. In the presence of clay, a higher aqueous sulfate concentration was detected than in those with only porewater present and this concentration decreased over time in the inoculated experiments. However, there was no evidence of hydrogen sulfide production in the aqueous phase. In all experiments with clay, there was an increase in aqueous Fe2+ concentrations with the highest concentrations found in uninoculated experiments. The sulfur speciation of the Opalinus Clay was analysed and the results of the inoculated sample suggested that hydrogen sulfide reacted with Fe2+, precipitating iron sulfide minerals. After the incubation period, the microbial community was dominated by the sulfate-reducing Desulfobulbaceae family. The study suggests that H2-fuelled, microbially-mediated sulfate reduction can affect the mineral composition within the Opalinus Clay due to the precipitation of iron sulfide minerals. These precipitation reactions may enhance the long-term integrity of the repository by removing corrosive hydrogen sulfide from solution when sufficient Fe2+ is available and so protecting the canisters containing the nuclear waste.

2019

Identification and characterization of proteins supporting dehalorespiration in Desulfitobacterium hafniense strain TCE1

Laure Prat

Respiration is a fundamental catalytic process in the aerobic and anaerobic energy metabolism of many prokaryotic and most eukaryotic organisms. The major difference between these organisms is that various organic and inorganic substrates can be used to donate or accept electrons in the bacterial and archaeal kingdoms, in various ranges of redox potentials in order to drive aerobic (with oxygen as electron acceptor) and anaerobic respiratory pathways. During the last few decades, several bacterial strains have been reported to use chlorinated compounds as terminal electron acceptor under anaerobic conditions, in a process called dehalorespiration. Among more than thirty dehalorespiring bacterial strains isolated to date, the Dehalococcoides group and the Gram-positive genus Desulfitobacterium comprise the largest number of reductively dehalogenating pure cultures. While most Dehalococcoides isolates appeared as highly specialized bacteria that depend strictly on dehalorespiration for growth, members of the genus Desulfitobacterium are very versatile microorganisms with regards to the electron donors and acceptors utilized. Globally, this remarkable prokaryotic respiratory flexibility is guaranteed by an elaborate reservoir of complex redox enzymes. Regarding the specific electron transport chain involved in dehalorespiration, rather little knowledge has been obtained so far with the exception of the key enzyme, the reductive dehalogenase, well described in several dehalorespiring bacteria, and of little information on b-type cytochromes and menaquinones. The overall objective of this thesis was to identify new possible components of the electron transport chain by comparative proteomic analysis, to investigate the presence/absence of a regulatory pathway leading to the biosynthesis of the reductive dehalogenase, and finally to characterize newly identified proteins that might support the dehalorespiration process. A comparative 2D proteomic analysis was performed on Desulfitobacterium hafniense strain TCE1, a bacterium capable of using tetrachloroethene (PCE) as electron acceptor. Soluble and membrane-associated proteins were analyzed from cells cultivated on different couples of electron donors and acceptors, lactate – fumarate (LF), lactate – PCE (LP), hydrogen – fumarate (HF), and hydrogen – PCE (HP). Cells growing on LP or HP revealed 72 and 93 protein spots in membrane fraction, and 49 and 12 spots in soluble fraction that correspond to increasingly expressed proteins compared to their fumarate-grown counterparts. More than 80 proteins were identified by mass spectrometry analysis, among which the key enzyme in the dehalorespiration process, the PCE reductive dehalogenase (PceA), as well as interesting candidates which could support dehalorespiration. The possible role of these proteins was analyzed in further details. Involved in energy and carbon metabolisms, electron transfer flavoproteins (ETF) and proteins related to the Wood-Ljungdahl pathway of CO2 fixation were identified in HP growth conditions. Proteins associated to stress response such as the phage shock protein PspA, and to regulatory pathways, the transcriptional repressor CodY, were also observed and discussed. Although only slightly induced by PCE, an additional protein displaying homology to sulfur-transferases was found in a large abundance in the fraction of membrane-associated proteins. This protein was named PhsE, as the corresponding gene belongs to a gene operon with homology to the molybdoenzyme thiosulfate/polysulfide reductase operons (phs/psr) found in Salmonella typhimurium or Wolinella succinogenes. PhsE protein architecture resembles to the class of tandem-domain rhodaneses, with the particularity to contain two active-site cysteines. It is also characterized by the presence of a typical lipoprotein signal peptide (LSP), which anchors PhsE on the outside of the cytoplasmic membrane. In the genome sequence of D. hafniense strain Y51, phsE (DSY3892) is part of an apparent operon encoding one out of about sixty different members of the complex iron-sulfur molybdoenzyme (CISM) family. PhsA, the catalytic molybdoenzyme, displays significant sequence homology with the thiosulfate/polysulfide reductase (PhsA/PsrA) subfamily. So far no other CISM operon has been described with a sulfur-transferase encoding gene. Despite the numerous functions proposed for rhodanese in cyanide detoxification, Fe/S cluster formation, oxidative stress protection, sulfur mobilization and involvement in general sulfur metabolism, the question of the physiological role of PhsE remains open. The expression of the Phs complex appeared to be influenced by the addition of sulfide in the culture medium, generally used as reducing agent in anaerobic cultures. Sulfide is known to affect the intracellular redox status. Therefore, it is hypothesized that PhsE might be involved in the control of the redox balance of the cell, notably by scavenging potentially toxic reduced sulfur species. To support data obtained at the protein level during proteomic analysis, genes and the corresponding messenger RNA from D. hafniense strain TCE1 were studied. While in silico DNA sequence analysis did not reveal any obvious features regulating the transcription of pceA, puzzling results were obtained in proteomic analysis showing an almost complete absence of PceA in cells grown on fumarate. To characterize this phenomenon, starting from a routinely PCE-grown inoculum, strain TCE1 was repeatedly transferred on medium containing fumarate as electron acceptor. The pool of pceA gene in the total culture DNA decreased significantly already after fifteen successive sub-cultures on fumarate, suggesting a shift in strain TCE1 population upon relief of the PCE selection pressure. Consequently the level of pceA mRNA and PceA protein also followed the same trend. Secondly, a PCE pulse experiment was performed in an anaerobic continuous culture of strain TCE1 on fumarate. It revealed that PCE itself has no power of induction on genetic level, except for the positive effect observed on pspA transcripts which encodes a protein involved in cell membrane integrity. Finally the expression study of the phsFABCDE gene cluster revealed that all phs genes are co-transcribed, and most likely build an operon. Thus phsE seemed to be strictly coregulated with the phs operon, and not under the influence of another promoter. In conclusion, proteomic analysis enabled to investigate the general physiological status of Desulfitobacterium hafniense strain TCE1 during dehalorespiration. A tentative model of the dehalorespiration pathway is proposed in summarizing recent data obtained on the topology of the PCE reductive dehalogenase and on sequence similarity with proteins involved in other anaerobic respiratory pathways. Regarding the possible support of PhsE towards the dehalorespiration, the complicated chemistry of sulfur does not allow to clearly attribute a function to the Phs complex, but there are indications that it might build a 'sulfur' oxidoreductase which could catalyze the conversion of sulfide to polysulfide with concomitant electron transfer to the quinone pool. The sulfide oxidation activity might be useful to D. hafniense to scavenge toxic sulfur species, avoiding that they disturb the redox balance of the cell, and redox-sensitive enzymatic complexes.

EPFL2009

Microbial metabolism in the deep subsurface

Alexandre Bagnoud

Microbes have successfully colonized the deep subsurface, thanks to their small size and their diverse metabolic activities. This part of the biosphere remains a terra incognita for microbiologists, containing innumerable unknown microbial species and processes. We depend on it for many things, i. e. water supply, oil extraction and nuclear waste disposal. In Switzerland, Opalinus Clay will be used for deep geological repositories, because of its very low permeability. This rock has been studied for 20 years, however, the potential role of microbes has long been overlooked, even though they could play a major role in controlling geochemical conditions. It was showed that they were present in pristine rock, but were not active due to the lack of space. The potential for microbial activity in disturbed rock, under repository relevant conditions, remains unexplored. This is the focus of this thesis. The first condition tested was the presence of space alone. This will occur when the rock is excavated to build the repository. The digging creates a network of large fractures in the rock zones near the galleries. This change is enough to promote microbial activity in a system, mainly composed of two species. The first one, a Peptococcaceae, oxidizes organic carbon to dioxide carbon, by reducing sulfate. The second organism is a Pseudomonas that seems to grow by fermenting organic carbon. From this model, it appears that the Peptococcaceae feeds on low molecular organic acids present in the Opalinus Clay, but also on fermentation products from Pseudomonas. What is less clear is the source of organic carbon for the latter. Is it only feeding on dead microbial cells, or is it also able to feed on reactive fossilized carbon contained in Opalinus Clay? The second case study included an additional energy source, hydrogen. This gas will be produced by anoxic steel corrosion and could damage the repository if the pressure increases significantly. However, it can be oxidized in situ by autotrophic microbial species. The dominating microbe in this system is a sulfate-reducing Desulfobulbaceae. It produces organic carbon from carbon dioxide, which can later feed heterotrophic bacteria, which are also sulfate-reducing and that release carbon dioxide. A carbon loop was thus reconstructed for the first time in the deep subsurface. It includes a fermentation step that releases the organic substrate for heterotrophic sulfate-reducing bacteria that completely oxidize simple organic carbon molecules, i.e., acetate, to carbon dioxide. In this system, hydrogen and sulfate consumption rates are 1.5 and 0.2 µmol·cm-3·day-1, respectively. This means that electrons derived from hydrogen reduce electron acceptors other than sulfate, confirming carbon fixation. These projects highlight the role that microbes can play for the safety of nuclear waste disposal. Hydrogen consumption is a beneficial process, but the overall impact of microbial activity can be negative, because it can promote corrosion and weathering of the different barriers surrounding the waste. Further work is needed in order to obtain a more complete picture of the role played by bacteria in a deep geological repository. Nonetheless, the results presented here represent a large improvement in our understanding of deep subsurface microbiology. Microbial processes were never described in this much detail in these environments, as is done here: from the metabolic pathway level, up to the ecosystem level.

EPFL2015