Biology subjects

Bakken, L. R.

Publications and source records attributed to Bakken, L. R..

5 recordsLinked to original sources

bioRxiv2021

A novel dual enrichment strategy provides soil- and digestate- competent N2O-respiring bacteria for mitigating climate forcing in agriculture

Manipulating soil metabolism by heavy inoculation with microbes is deemed realistic if waste from anaerobic digestion (digestate) is utilized as substrate and vector, but requires organisms that can grow both in digestate and soil (=generalist). We designed a strategy to enrich and isolate such generalist N2O-respiring bacteria (NRB) in soil and digestate, to provide inoculum for reducing N2O-emissions from agricultural soil. Sequential anaerobic enrichment cultures were provided with a small dose of O2 and unlimited N2O, alternating between sterilized digestate and soil as substrates. The cultures were monitored for gas kinetics and community composition (16SrDNA), and cluster-analysis identified generalist-OTUs which became dominant, digestate/soil-specialists which did not, and a majority that were diluted out. Several NRBs circumscribed by generalist-OTUs were isolated, genome sequenced to screen for catabolic capacity, and phenotyped, to assess their capacity as N2O-sinks in soil. The two isolates Cloacibacterium sp., carrying only N2O-reductase (Clade-II) and Pseudomonas sp., with full-fledged denitrification-pathway, were both very effective N2O-sinks in soil, with Pseudomonas sp., showing a long-lasting sink effect, suggesting better survival in soil. This avenue for utilizing waste to bioengineer the soil microbiota holds promise to effectively combat N2O-emissions but could also be utilized for enhancing other metabolic functions in soil. Graphical abstract O_FIG_DISPLAY_L [Figure 1] M_FIG_DISPLAY C_FIG_DISPLAY

microbiology↗

bioRxiv2020

Soil Chemistry and Microbiome Determine N2O Emission Potential in Soils

Microbial nitrogen (N) transformations in soil, notably denitrification, result in the production of the potent greenhouse and ozone depleting gas nitrous oxide (N2O). Soil chemistry and microbiome composition impact N2O emission potential but the relative importance of these factors as determinants of N2O emission in denitrifying systems is rarely tested. In addition, previous linkages between microbiome composition and N2O emission potential rarely demonstrate causality. Here, we determined the relative impact of microbiome composition (i.e. soil extracted cells) and chemistry (i.e. water extractable chemicals) on N2O emission potential utilizing an anoxic cell based assay system. Cells and chemistry for assays were sourced from soils with contrasting N2O/N2O+N2 ratios, combined in various combinations and denitrification gas production was measured in response to nitrate addition. Average directionless effects of cell and chemical extract on N2O/N2O+N2 (Cell: {Delta}0.16, Chemical extract: {Delta}0.22) and total N2O hypothetically emitted (Cell: {Delta}2.62 mol-N, Chemical extract: {Delta}4.14 mol-N) indicated chemistry is the most important determinant of N2O emissions. Independent pH differences of just 0.6 points impacted N2O/N2O+N2 on par with independent chemical extract differences, supporting the dominance of this variable in previous studies. However, impacts on overall N2O hypothetically emitted were smaller suggesting that soil pH manipulation may not necessarily be a successful approach to mitigate emissions over a fixed time period. In addition, we observed increased N2O accumulation and emission potential at the end of incubations concomitant with predicted decreases in carbon availability suggesting that carbon limitation increases N2O emission transiently with the magnitude of emission dependent on the both chemical and microbiome controls.

microbiology↗

bioRxiv2020

Linking meta-omics to the kinetics of denitrification intermediates reveals pH-dependent causes of N2O emissions and nitrite accumulation in soil

Denitrifier community phenotypes often result in transient accumulation of denitrification (NO3-[->]NO2-[->]NO[->]N2O[->]N2) intermediates. Consequently, anoxic spells drive NO-, N2O- and possibly HONO-emissions to the atmosphere, affecting both climate and tropospheric chemistry. Soil pH is a key controller of intermediate levels, and while there is a clear negative correlation between pH and emission of N2O, NO2- concentrations instead increase with pH. These divergent trends are probably a combination of direct effects of pH on the expression/activity of denitrification enzymes, and an indirect effect via altered community composition. This was studied by analyzing metagenomics/transcriptomics and phenomics of two soil denitrifier communities, one of pH 3.8 (Soil3.8) and the other 6.8 (Soil6.8). Soil3.8 had severely delayed N2O reduction despite early transcription of nosZ, encoding N2O reductase, by diverse denitrifiers, and of several nosZ accessory genes. This lends support to a post-transcriptional, pH-dependent mechanism acting on the NosZ apo-protein or on enzymes involved in its maturation. Metagenome/metatranscriptome reads of nosZ were almost exclusively clade I in Soil3.8 while clade II dominated in Soil6.8. Reads of genes and transcripts for NO2--reductase were dominated by nirK over nirS in both soils, while qPCR-based determinations showed the opposite, demonstrating that standard primer pairs only capture a fraction of the nirK community. The -omics results suggested that low NO2- concentrations in acidic soils, often ascribed to abiotic degradation, are primarily due to enzymatic activity. The NO reductase gene qnor was strongly expressed in Soil3.8, suggesting an important role in controlling NO. Production of HONO, for which some studies claim higher, others lower, emissions from NO2- accumulating soil, was estimated to be ten times higher from Soil3.8 than from Soil6.8. The study extends our understanding of denitrification-driven gas emissions and the diversity of bacteria involved and demonstrates that gene and transcript quantifications cannot always reliably predict community phenotypes.

microbiology↗

bioRxiv2020

Bacteria in biogas digestates for reduced climate forcing

Inoculating agricultural soils with N2O-respiring bacteria (NRB) can reduce N2O-emissions, but would be impractical as a standalone operation. Here we demonstrate that digestates obtained after biogas production are suitable substrates and vectors for NRB. We show that indigenous NRB in digestates grew to high abundance during anaerobic enrichment under N2O. Gas-kinetics and meta-omic analyses showed that these NRB's, recovered as metagenome-assembled genomes (MAGs), grew by harvesting fermentation intermediates of the methanogenic consortium. Three NRB's were isolated, one of which matched the recovered MAG of a Dechloromonas, deemed by proteomics to be the dominant producer of N2O-reductase in the enrichment. While the isolates harbored genes required for a full denitrification pathway and could thus both produce and sequester N2O, their regulatory traits predicted that they act as N2O sinks in soil, which was confirmed experimentally. The isolates were grown by aerobic respiration in digestates, and fertilization with these NRB-enriched digestates reduced N2O emissions from soil. Our use of digestates for low-cost and large-scale inoculation with NRB in soil can be taken as a blueprint for future applications of this powerful instrument to engineer the soil microbiome, be it for enhancing plant growth, bioremediation, or any other desirable function.

microbiology↗

bioRxiv2020

Competition for electrons favors N2O reduction in denitrifying Bradyrhizobium isolates

Bradyrhizobia are common members of soil microbiomes and known as N2-fixing symbionts of economically important legumes. Many are also denitrifiers, which can act as sinks or sources for N2O. Inoculation with compatible rhizobia is often needed for optimal N2-fixation, but the choice of inoculant may also have consequences for N2O emission. Here, we analyzed the phylogeny and denitrification capacity of Bradyrhizobium strains, most of them isolated from peanut-nodules. All were dinitrifiers, but only ~1/3 could reduce N2O while most others were net N2O producers. The N2O-reducing isolates showed strong preference for N2O- over NO3--reduction. Such preference was also observed in a study of other bradyrhizobia and tentatively ascribed to competition between the electron pathways to Nap (periplasmic NO3- reductase) and Nos (N2O reductase). Another possible explanation is lower abundance of Nap than Nos. Here, proteomics revealed that Nap was instead more abundant than Nos, supporting the hypothesis that the electron pathway to Nos outcompetes that to Nap. In contrast, Paracoccus denitrificans, which has membrane-bond NO3- reductase (Nar), reduced N2O and NO3- simultaneously. We propose that the control at the metabolic level, favoring N2O reduction over NO3- reduction, applies also to other denitrifiers carrying Nos and Nap but lacking Nar. Originality-Significance StatementThis study extends the current knowledge on denitrification in bradyrhizobia, which mostly originates from studies of one model strain, by investigating the denitrification phenotypes of a diverse collection of Bradyrhizobium isolates. Only 1/3 of them could reduce N2O while the others were net sources for this potent greenhouse gas. All N2O-reducers showed strong preference for N2O over NO3-. We revealed by proteomics that this was not explained by differences in the abundances of Nap (periplasmic nitrate reductase) and Nos (N2O reductase), which strengthens our hypothesis (Mania et al., 2020) of a metabolic control mechanism by which Nos competes efficiently with Nap for electrons, making these organisms strong sinks for N2O. The findings highlight the potential importance of these organisms as N2O sinks in natural and agricultural ecosystems and pinpoint the need to take N2O reduction into account, along with N2-fixation effectiveness, when searching for strains suitable for production of inoculants.

microbiology↗