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Laureni, M.

Publications and source records attributed to Laureni, M..

12 recordsLinked to original sources

Long-term multi-meta-omics resolves the ecophysiological controls of seasonal N2O emissions

The potent greenhouse gas nitrous oxide (N2O) originates primarily from natural and engineered microbiomes. Emission seasonality is widely reported while the underlying metabolic controls remain largely unresolved, hindering effective mitigation. We use biological wastewater treatment as tractable model ecosystem over nearly two years. Long-term metagenomic-resolved metaproteomics is combined with ex situ kinetic and full-scale operational characterization. By leveraging the evidence independently obtained at multiple ecophysiological levels, from individual genetic potential to actual metabolism and emergent community phenotype, the cascade of environmental and operational triggers driving N2O emissions is resolved. We explain the dynamics in nitrite accumulation with the kinetic unbalance between ammonia and nitrite oxidisers, and identify nitrifier denitrification as the prime N2O-producing pathway. The dissolved O2 emerged as the key actionable parameter for emission control. This work exemplifies the yet-to-be-realized potential of multi-meta-omics approaches for the mechanistic understanding and ecological engineering of microbiomes, ultimately advancing sustainable biotechnological developments.

microbiology↗

A difficult coexistence: resolving the iron-induced nitrification delay in groundwater filters

Rapid sand filters (RSF) are an established and widely applied technology for the removal of dissolved iron (Fe2+) and ammonium (NH +) in groundwater treatment. Most often, biological NH + oxidation is delayed and starts only upon complete Fe2+ depletion. However, the mechanism(s) responsible for the inhibition of NH + oxidation by Fe2+ or its oxidation (by)products remains elusive, hindering further process control and optimization. We used batch assays, lab-scale columns, and full-scale filter characterizations to resolve the individual impact of the main Fe2+ oxidizing mechanisms and the resulting products on biological NH + oxidation. Modelling of the obtained datasets allowed to quantitatively assess the hydraulic implications of Fe2+ oxidation. Dissolved Fe2+ and the reactive oxygen species formed as byproducts during Fe2+ oxidation had no direct effect on nitrification. The Fe3+ oxides on the sand grain coating, commonly assumed to be the main cause for inhibited nitrification, seemed instead to enhance nitrification by providing additional surface area for biofilm growth. Modelling allowed to exclude mass transfer limitations induced by accumulation of iron flocs and consequent filter clogging as the cause for delayed nitrification. We unequivocally identify the inhibition of NH +oxidizing organisms by the Fe3+ flocs generated during Fe2+ oxidation as the main cause for the commonly observed nitrification delay. The addition of Fe3+ flocs inhibited NH + oxidation both in batch and column tests, and the removal of Fe3+ flocs by backwashing completely re-established the NH + removal capacity, suggesting that the inhibition is reversible. In conclusion, our findings not only identify the iron form that causes the inhibition, albeit the biological mechanism remains to be identified, but also highlight the ecological importance of iron cycling in nitrifying environments. Graphical abstract O_FIG O_LINKSMALLFIG WIDTH=200 HEIGHT=130 SRC="FIGDIR/small/581000v1_ufig1.gif" ALT="Figure 1"> View larger version (19K): org.highwire.dtl.DTLVardef@65ca28org.highwire.dtl.DTLVardef@bb3da3org.highwire.dtl.DTLVardef@cbd32dorg.highwire.dtl.DTLVardef@1956207_HPS_FORMAT_FIGEXP M_FIG C_FIG HighlightO_LIDissolved Fe2+ and reactive oxygen species do not affect NH + oxidation C_LIO_LIFe oxide coating aids sand grain colonization by NH +-oxidizing bacteria C_LIO_LIFe3+ flocs inhibit NH + oxidation by reducing the nitrifying capacity of AOB C_LIO_LIChanges in transport patterns due to clogging do not play a major role in NH + oxidation C_LIO_LIThe inhibition of NH4+ oxidation is reversible and reduced by backwashing C_LI

microbiology↗

Shifting to biology promotes highly efficient iron removal in groundwater filters

Rapid sand filters are established and widely applied technologies for groundwater treatment. Conventionally, intensive aeration is employed to provide oxygen for the oxidation and removal of the main groundwater contaminants. While effective, intensive aeration promotes flocculent iron removal, which results in iron flocs that rapidly clog the filter. In this study, we operated two parallel full-scale sand filters at different aeration intensities to resolve the relative contribution of homogeneous, heterogeneous and biological iron removal pathways, and identify their operational controls. Our results show that mild aeration in the LOW filter (5 mg/L O2pH 6.9) promoted biological iron removal and enabled iron oxidation at twice the rate compared to the intensively aerated HIGH filter (>10mg/L O2,pH 7.4). ESEM images showed distinctive twisted stalk-like Fe solids, biosignatures of Gallionella ferruginea, both in the LOW filter sand coatings as well as in its backwash solids. In accordance, 10 times higher DNA copy numbers of G. ferruginea were found in the LOW filter effluent. Clogging by biogenic FeOx was slower than by chemical FeOx flocs, resulting in lower backwash frequencies and yielding four times more water per run. Ultimately, our results reveal that biological Fe2+ oxidation can be actively controlled and favoured over competing physico-chemical routes. The resulting operational benefits are only starting to be appreciated, with the counterintuitive higher oxidation rates and water yields at lower aeration regimes, and the production of more compact and practically valuable FeOx solids being of outmost interest.

microbiology↗

Selective enrichment of high-affinity clade II N2O-reducers in a mixed culture

Microorganisms encoding for the N2O reductase (NosZ) are the only known biological sink of the potent greenhouse gas N2O, and are central to global N2O mitigation efforts. Yet, the ecological constraints selecting for different N2O-reducers strains and controlling the assembly of N2O-respiring communities remain largely unknown. Of particular biotechnological interest are clade II NosZ populations, which usually feature high N2O affinities and often lack other denitrification genes. Two planktonic N2O-respiring mixed cultures were enriched under limiting and excess dissolved N2O availability to assess the impact of substrate affinity and N2O cytotoxicity, respectively. Genome-resolved metaproteomics was used to infer the metabolism of the enriched populations. We show that clade II N2O-reducers outcompete clade I affiliates for N2O at sufficiently low sludge dilution rates (0.006 h-1), a scenario previously only theorized based on pure-cultures. Under N2O limitation, all enriched N2O-reducers encoded and expressed only clade II NosZ, while also possessing other denitrification genes. Two Azonexus and Thauera genera affiliates dominated the culture. We explain their coexistence with the genome-inferred metabolic exchange of cobalamin intermediates. Conversely, under excess N2O, clade I and II populations coexisted. Notably, the single dominant N2O-reducer (genus Azonexus) expressed most cobalamin biosynthesis marker genes, likely to contrast the continuous cobalamin inactivation by dissolved cytotoxic N2O concentrations (400 {micro}M). Ultimately, we demonstrate that the solids dilution rate controls the selection among NosZ clades, albeit the conditions selecting for genomes possessing the sole nosZ remain elusive. Additionally, we suggest the significance of N2O-cobalamin interactions in shaping the composition of N2O-respiring microbiomes.

systems biology↗

"Candidatus Siderophilus nitratireducens": a psychrophilic, nap-dependent nitrate-reducing iron oxidizer within the new order Siderophiliales

Nitrate leaching from agricultural soils is increasingly found in groundwater, a primary source of drinking water worldwide. This nitrate influx can potentially stimulate the biological oxidation of iron in anoxic groundwater reservoirs. Nitrate-reducing iron-oxidizing (NRFO) bacteria have been extensively studied in laboratory settings, yet their ecophysiology in natural environments remains largely unknown. To this end, we established a pilot-scale filter on nitrate-rich groundwater to elucidate the structure and metabolism of nitrate-reducing iron-oxidizing microbiomes under oligotrophic conditions mimicking natural groundwaters. The enriched community stoichiometrically removed iron and nitrate consistently with NRFO metabolism. Genome-resolved metagenomics revealed the underlying metabolic network between the dominant iron-dependent denitrifying autotrophs and the less abundant organoheterotrophs. The most abundant genome belonged to a new Candidate order, named Siderophiliales. This new species, "Candidatus Siderophilus nitratireducens", carries central genes to iron oxidation (cytochrome c cyc2), carbon fixation (rbc), and for the sole periplasmic nitrate reductase (nap). To our knowledge, this is the first report of nap-based lithoautotrophic growth, and we demonstrate that iron oxidation coupled to dissimilatory reduction of nitrate to nitrite is thermodynamically favourable under realistic Fe3+/Fe2+ and [Formula] concentration ratios. Ultimately, by bridging the gap between laboratory investigations and real-world conditions, this study provides insights into the intricate interplay between nitrate and iron in groundwater ecosystems, and expands our understanding of NRFOs taxonomic diversity and ecological role.

microbiology↗

Aerobic denitrification as N2O source in microbial communities

Nitrous oxide (N2O) is a potent greenhouse gas of primarily microbial origin. Aerobic and anoxic emissions are commonly ascribed to nitrification and denitrification, respectively. Beyond this established dichotomy, we quantitatively prove that heterotrophic denitrification can significantly contribute to aerobic nitrogen turnover and N2O emissions in complex microbiomes exposed to frequent oxic/anoxic transitions. Planktonic, nitrification-inhibited denitrifying enrichments respired over a third of the influent organic substrate with nitrate at high oxygen concentrations. N2O accounted for up to one quarter of the aerobically respired nitrate. The constitutive detection of all denitrification enzymes in both anoxic and oxic periods highlight the selective advantage offered by metabolic preparedness in dynamic environments. We posit that aerobic denitrification and associated N2O formation is currently underestimated in dynamic microbial ecosystems.

microbiology↗

Microbiome, resistome and mobilome of chlorine-free drinking water treatment systems

Drinking water treatment plants (DWTPs) are designed to remove physical, chemical, and biological contaminants. However, until recently, the role of DWTPs in minimizing the cycling of antibiotic resistance determinants has got limited attention. In particular, the risk of selecting antibiotic-resistant bacteria (ARB) is largely overlooked in chlorine-free DWTPs where biological processes are applied. Here, we combined high-throughput quantitative PCR and metagenomics to analyze the abundance and dynamics of microbial communities, antibiotic resistance genes (ARGs), and mobile genetic elements (MGEs) across the treatment trains of two chlorine-free DWTPs involving dune-based and reservoir-based systems. The microbial diversity of the water being treated increased after all biological unit operations, namely rapid and slow sand filtration (SSF), and granular activated carbon filtration. Both DWTPs reduced the concentration of ARGs and MGEs in the water by about 2.5 log gene copies mL-1, despite their relative increase in the disinfection sub-units (SSF in dune-based and UV treatment in reservoir-based DWTPs). The total microbial concentration was also reduced (2.5 log units), and none of the DWTPs were enriched for antibiotic resistant bacteria. Our findings highlight the effectiveness of chlorine-free DWTPs in supplying safe drinking water while reducing the concentration of antibiotic resistance determinants. To the best of our knowledge, this is the first study that monitors the presence and dynamics of antibiotic resistance determinants in chlorine-free DWTPs.

microbiology↗

Meta-omics profiling of full-scale groundwater rapid sand filters explains stratification of iron, ammonium and manganese removals

Rapid sand filters (RSF) are an established and widely applied technology for groundwater treatment. Yet, the underlying interwoven biological and physical-chemical reactions controlling the sequential removal of iron, ammonia and manganese remain poorly understood. To resolve the contribution and interactions between the individual reactions, we studied two full-scale drinking water treatment plant configurations, namely (i) one dual-media (anthracite and quartz sand) filter and (ii) two single-media (quartz sand) filters in series. In situ and ex situ activity tests were combined with mineral coating characterization and metagenome-guided metaproteomics along the depth of each filter. Both plants exhibited comparable performances and process compartmentalization, with most of ammonium and manganese removal occurring only after complete iron depletion. Within each compartment, the homogeneity of the media coating and genome-based microbial composition highlighted the effect of backwashing on filter media mixing. In stark contrast, intra-compartment contaminant removal was highly stratified following decreasing substrate availability along the filter height. This apparent and long-standing conflict was resolved by quantifying the expressed proteome at different filter heights, revealing a consistent stratification of proteins catalysing ammonia oxidation and protein-based relative abundances of nitrifying genera. This implies that microorganisms adapt their protein pool to the available nutrient load at a faster rate than the backwash mixing frequency. Ultimately, these results show the unique and complementary potential of metaproteomics to understand metabolic adaptations and interactions in highly dynamic ecosystems.

microbiology↗

Adaptation of anammox bacteria to low temperature via gradual acclimation and cold shocks: distinctions in protein expression, membrane composition and activities

Anammox bacteria enable an efficient removal of nitrogen from sewage in processes involving partial nitritation and anammox (PN/A) or nitrification, partial denitrification, and anammox (N-PdN/A). In mild climates, anammox bacteria must be adapted to [≤]15 {degrees}C, typically by gradual temperature decrease; however, this takes months or years. To reduce the time necessary for the adaptation, an unconventional method of cold shocks is promising, involving hours-long exposure of anammox biomass to extremely low temperatures. We compared the efficacies of gradual temperature decrease and cold shocks to increase the metabolic activity of anammox (fed batch reactor, planktonic "Ca. Kuenenia"). We assessed the cold shock mechanism on the level of protein expression (quantitative shot-gun proteomics, LC-HRMS/MS) and structure of membrane lipids (UPLC-HRMS/MS). The shocked culture was more active (0.66{+/-}0.06 vs 0.48{+/-}0.06 kg-N/kg-VSS/d) and maintained the relative content of N-respiration proteins at levels consistent levels with the initial state, whereas the content of these proteins decreased in gradually acclimated culture. Cold shocks also induced a more efficient up-regulation of cold shock proteins (e.g. CspB, TypA, ppiD). Ladderane lipids characteristic for anammox evolved to a similar end-point in both cultures which confirms their role in anammox bacteria adaptation to cold and indicates a three-pronged adaptation mechanism involving ladderane lipids (ladderane alkyl length, introduction of shorter non-ladderane alkyls, polar headgroup). Overall, we show the outstanding potential of cold shocks for low-temperature adaptation of anammox bacteria and provide yet unreported detailed mechanisms of anammox adaptation to low temperatures. HighlightsO_LIAnammox bacteria were adapted to low T by gradual acclimation and cold shocks C_LIO_LIThe shocked culture was more active (0.66{+/-}0.06 vs 0.48{+/-}0.06 kg-N/kg-VSS/d) C_LIO_LIN-respiration proteins content decreased in gradually acclimated bacteria C_LIO_LISeveral cold shock proteins were upregulated more efficiently by cold shocks C_LIO_LIAt {downarrow}T, anammox adjusted ladderane membrane lipid composition in three aspects C_LI Graphical abstract O_FIG_DISPLAY_L [Figure 1] M_FIG_DISPLAY C_FIG_DISPLAY

bioengineering↗

A general approach to explore prokaryotic protein glycosylation reveals the unique surface layer modulation of an anammox bacterium.

The enormous chemical diversity and strain variability of prokaryotic protein glycosylation makes a large-scale exploration exceptionally challenging. Therefore, despite the universal relevance of protein glycosylation across all domains of life, the understanding of their biological significance and the evolutionary forces shaping oligosaccharide structures remains highly limited. Here, we report on a newly established mass binning glycoproteomics approach that establishes the chemical identity of the carbohydrate components and performs untargeted exploration of prokaryotic oligosaccharides from large-scale proteomics data directly. We demonstrate our approach by exploring an enrichment culture of the globally relevant anaerobic ammonium-oxidizing bacterium Ca. Kuenenia stuttgartiensis. By doing so we resolved a remarkable array of oligosaccharides, produced by two entirely unrelated glycosylation machineries targeting the same surface-layer protein (SLP) simultaneously. More intriguingly, the investigated strain also accomplished modulation of highly specialized sugars, supposedly in response to its energy metabolism--the anaerobic oxidation of ammonium --which depends on the acquisition of substrates of opposite charge. Ultimately, we provide a systematic approach for the compositional exploration of prokaryotic protein glycosylation, and reveal for the first time a remarkable balance between maximising cellular protection through a complex array of oligosaccharides and adhering to the requirements of the metabolic lifestyle.

systems biology↗

On anammox activity at low temperature: effect of ladderane composition, process conditions and dominant anammox population

The application of partial nitritation-anammox (PN/A) under mainstream conditions can enable substantial cost savings at wastewater treatment plants (WWTPs), but how process conditions and cell physiology affect anammox performance at psychrophilic temperatures below 15 {degrees}C remains poorly understood. We tested 14 anammox communities, including 8 from globally-installed PN/A processes, for (i) specific activity at 10-30 {degrees}C (batch assays), (ii) composition of membrane lipids (U-HPLC-HRMS/MS), and (iii) microbial community structure (16S rRNA gene amplicon sequencing). Crucially, the key parameters impacting anammox activity were the membrane lipid composition and cultivation temperature. The size of ladderane lipids and the content of bacteriohopanoids were key physiological drivers of anammox performance at low temperatures. Higher contents of (i) short C18 [3]-ladderane alkyl and (ii) large phosphatidylcholine headgroup were determined in anammox more active at 15-30 {degrees}C and 10-15 {degrees}C, respectively. At below 15 {degrees}C, the activation energies of most mesophilic cultures severely increased while those of the psychrophilic cultures remained stable; this indicates that the adaptation of mesophilic cultures to psychrophilic regime necessitates months, but in some cases can take up to 5 years. Interestingly, biomass enriched in the marine genus "Candidatus Scalindua" displayed exceptionally highest activity at 10-20 {degrees}C (0.50 kg-N.kg-VSS-1.d-1 at 10 {degrees}C, Ea10-30 {degrees}C = 51{+/-}16 kJ.mol-1), indicating outstanding potential for nitrogen removal from cold streams. Collectively, our comprehensive study provides essential knowledge of cold adaptation mechanism, will enable more accurate modelling and suggests highly promising target anammox genera for inoculation and set-up of anammox reactors, in particular for mainstream WWTPs. HighlightsO_LILadderane size and cold exposure affected anammox activation energy (Ea). C_LIO_LIEa improved with more C18 [3]-ladderanes over C20 and larger polar headgroup. C_LIO_LILong-term cold exposure reduced Ea at 10-15 {degrees}C, not activity per se. C_LIO_LIMarine "Ca. Scalindua" was exceptionally suitable for cold streams. C_LIO_LIAnammox Ea at 15-30 {degrees}C was 79{+/-}18 kJ.mol-1. C_LI Graphical abstract O_FIG O_LINKSMALLFIG WIDTH=200 HEIGHT=121 SRC="FIGDIR/small/873869v1_ufig1.gif" ALT="Figure 1"> View larger version (25K): org.highwire.dtl.DTLVardef@1c5c3aborg.highwire.dtl.DTLVardef@b11ed2org.highwire.dtl.DTLVardef@5e7ec9org.highwire.dtl.DTLVardef@1d5cba5_HPS_FORMAT_FIGEXP M_FIG C_FIG

microbiology↗

Biomass segregation between biofilm and flocs improves the control of nitrite-oxidizing bacteria in mainstream partial nitritation and anammox processes

The control of nitrite-oxidizing bacteria (NOB) challenges the implementation of partial nitritation and anammox (PN/A) processes under mainstream conditions. The aim of the present study was to understand how operating conditions impact microbial competition and the control of NOB in hybrid PN/A systems, where biofilm and flocs coexist. A hybrid PN/A moving-bed biofilm reactor (MBBR; also referred to as integrated fixed film activated sludge or IFAS) was operated at 15 {degrees}C on aerobically pre-treated municipal wastewater (23 mgNH4-N{middle dot}L-1). Ammonium-oxidizing bacteria (AOB) and NOB were enriched primarily in the flocs, and anammox bacteria (AMX) in the biofilm. After decreasing the dissolved oxygen concentration (DO) from 1.2 to 0.17 mgO2{middle dot}L-1 - with all other operating conditions unchanged - washout of NOB from the flocs was observed. The activity of the minor NOB fraction remaining in the biofilm was suppressed at low DO. As a result, low effluent NO3- concentrations (0.5 mgN{middle dot}L-1) were consistently achieved at aerobic nitrogen removal rates (80 mgN{middle dot}L-1{middle dot}d-1) comparable to those of conventional treatment plants. A simple dynamic mathematical model, assuming perfect biomass segregation with AOB and NOB in the flocs and AMX in the biofilm, was able to qualitatively reproduce the selective washout of NOB from the flocs in response to the decrease in DO-setpoint. Similarly, numerical simulations indicated that flocs removal is an effective operational strategy to achieve the selective washout of NOB. The direct competition for NO2- between NOB and AMX - the latter retained in the biofilm and acting as a \"NO2-sink\" - was identified by the model as key mechanism leading to a difference in the actual growth rates of AOB and NOB (i.e., NOB < AOB in flocs) and allowing for the selective NOB washout. Experimental results and model predictions demonstrate the increased operational flexibility, in terms of variables that can be easily controlled by operators, offered by hybrid systems as compared to solely biofilm systems for the control of NOB in mainstream PN/A applications.\n\nHighlightsO_LIHybrid PN/A systems provide increased operational flexibility for NOB control\nC_LIO_LIAOB and NOB enrich primarily in the flocs, and AMX in the biofilm (\"NO2-sink\")\nC_LIO_LIAMX use NO2- allowing to differentiate AOB and NOB growth rates\nC_LIO_LIA decrease in DO or an increase in floc removal leads to selective NOB washout from flocs\nC_LIO_LIThe activity of the minor NOB fraction in the biofilm is suppressed at limiting DO\nC_LI\n\n\n\nO_FIG O_LINKSMALLFIG WIDTH=200 HEIGHT=63 SRC=\"FIGDIR/small/480780v2_ufig1.gif\" ALT=\"Figure 1\">\nView larger version (21K):\norg.highwire.dtl.DTLVardef@cad5deorg.highwire.dtl.DTLVardef@9efef3org.highwire.dtl.DTLVardef@7409feorg.highwire.dtl.DTLVardef@3c1043_HPS_FORMAT_FIGEXP M_FIG C_FIG

systems biology↗