Vick, S. H. | Search bioRxiv

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

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↗