Project description:This project aims to investigate the metabolic pathways expressed by the active microbial community occurring at the deep continental subsurface. Subsurface chemoLithoautotrophic Microbial Ecosystems (SLiMEs) under oligotrophic conditions are supported by H2; however, the overall ecological trophic structures of these communities are poorly understood. Some deep, fluid-filled fractures in the Witwatersrand Basin, South Africa appear to support inverted trophic pyramids wherein methanogens contributing <5% of the total DNA apparently produce CH4 that supports the rest of the community. Here we show the active metabolic relationships of one such trophic structure by combining metatranscriptomic assemblies, metaproteomic and stable isotopic data, and thermodynamic modeling. Four autotrophic β-proteobacteria genera that are capable of oxidizing sulfur by denitrification dominate. They co-occur with sulfate reducers, anaerobic methane oxidizers and methanogens, which each comprises <5% of the total community. Defining trophic levels of microbial chemolithoautotrophs by the number of transfers from the initial abiotic H2-driven CO2 fixation, we propose a top-down cascade influence of the metabolic consumers that enhances the fitness of the metabolic producers to explain the inverted biomass pyramid of a multitrophic SLiME. Symbiotic partnerships are pivotal in the deep biosphere on and potentially beyond the Earth.
Project description:To study long-term elevated CO2 and enriched N deposition interactive effects on microbial community and soil ecoprocess, here we investigated soil microbial community in a grassland ecosystem subjected to ambient CO2 (aCO2, 368 ppm), elevated CO2 (eCO2, 560 ppm), ambient nitrogen deposition (aN) or elevated nitrogen deposition (eN) treatments for a decade. There exist antagonistic CO2×N interactions on microbial functional genes associated with C, N, P S cycling processes. More strong antagonistic CO2×N interactions are observed on C degradation genes than other genes. Remarkably antagonistic CO2×N interactions on soil microbial communities could enhance soil C accumulation.
2018-05-01 | GSE98512 | GEO
Project description:Microbial Resilience in Flexible Ex Situ Biomethanation of H2/CO2
| PRJNA623376 | ENA
Project description:CO2 conversion to VFAs via microbial electrosynthesis
Project description:Background: Biological conversion of the surplus of renewable electricity to CH4 could support energy storage and strengthen the power grid. Biological methanation (BM) is closely linked to the activity of biogas-producing bacterial community and methanogenic Archaea in particular. During reactor operations, the microbiome is often subject to various changes whereby the microorganisms are challenged to adapt to the new conditions. In this study, a hydrogenotrophic-adapted microbial community in a laboratory-scale BM fermenter was monitored for its pH, gas production, conversion yields and composition. To investigate the robustness of BM regarding power oscillations, the biogas microbiome was exposed to five H2 starvations patterns for several hours.
Project description:Conversion of biomass-derived syngas (gaseous mixture of mainly H2, CO and CO2) to methane might be a sustainable alternative for the biofuel industry. Via the syngas route more methane can be produced from biomass than via conventional anaerobic digestion. Methanogenic archaea are key players in syngas conversion, but only a few are known to utilize CO (or syngas). Methanothermobacter thermoautotrophicus is one of the few hydrogenotrophic methanogens which has been observed to grow on CO. However, carboxydotrophic growth is slow and is reported to be readily inhibited above 50 kPa CO. The aim of this work was to get more insight of the CO metabolism in hydrogenotrophic archaea and to assess the potential toxic effects of CO towards these microorganisms. Archaeal genomic databases were searched for putative homologues of the Methanothermobacter thermoautotrophicus CODH alpha subunit (containing the catalytic site): the highest scores were for the CODH subunits of Methamothermobacter marburgensis (93% identity) and Methanococcus maripaludis (71%). M. thermoautotrophicus and the other two potential carboxydotrophic strains were incubated with CO and CO + H2 as sole substrates. In addition to M. thermoautotrophicus, M. marburgensis was able to grow methanogenically on CO alone and on CO + H2. In contrast to M. thermoautotrophicus, M. marburgensis was not as strongly inhibited when grown in presence of CO alone and was able to adapt its metabolism, shifting its lag phase from ~500 to ~100 hours. It was observed for both strains that presence of hydrogen stimulates the carbon monoxide metabolism. To gain further insight, the proteome of M. marburgensis culture grown on H2 + CO2 and H2 + CO2 + CO were analysed. Cultures grown with H2 + CO showed relative higher abundance of enzymes involved in CODH/ACS associated reactions and reactions involved in redox metabolism. Overall, the data suggests the strong reducing capacity of CO inhibits the hydrogenotrophic methanogen, making growth on CO as a sole substrate difficult for these organisms.
Project description:The synthetic microbial community used in this study was composed of the major functional guilds (cellulolytic fermenter, sulfate reducer, hydrogenotrophic methanogen and acetoclastic methanogen) that mediate the anaerobic conversion of cellulosic biomass to CH4 and CO2 in wetland soils. The choice of a facultative sulfate-reducing bacterium (Desulfovibrio vulgaris Hildenborough) introduced metabolic versatility and enabled investigations into the community response to sulfate intrusion. The growth status of these multi-species cultures was measured over a week by daily analysis of substrate consumption and product accumulation. The quad-cultures were analyzed with metaproteomics at the end of experiment to characterize the community structure and metabolic activities.
Project description:To study whether and how soil nitrogen conditions affect the ecological effects of long-term elevated CO2 on microbial community and soil ecoprocess, here we investigated soil microbial community in a grassland ecosystem subjected to ambient CO2 (aCO2, 368 ppm), elevated CO2 (eCO2, 560 ppm), ambient nitrogen deposition (aN) or elevated nitrogen deposition (eN) treatments for a decade. Under the aN condition, a majority of microbial function genes, as measured by GeoChip 4.0, were increased in relative abundance or remained unchanged by eCO2. Under the eN condition, most of functional genes associated with carbon, nitrogen and sulfur cycling, energy processes, organic remediation and stress responses were decreased or remained unchanged by eCO2, while genes associated with antibiotics and metal resistance were increased. The eCO2 effects on fungi and archaea were largely similar under both nitrogen conditions, but differed substantially for bacteria. Coupling of microbial carbon or nitrogen cycling genes, represented by positive percentage and density of gene interaction in association networks, was higher under the aN condition. In accordance, changes of soil CO2 flux, net N mineralization, ammonification and nitrification was higher under the aN condition. Collectively, these results demonstrated that eCO2 effects are contingent on nitrogen conditions, underscoring the difficulty toward predictive modeling of soil ecosystem and ecoprocesses under future climate scenarios and necessitating more detailed studies.