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Jorgensen, B. B.

Publications and source records attributed to Jorgensen, B. B..

3 recordsLinked to original sources

Genome-centric metagenomics reveals novel electroactive syntrophs in a conductive particle-dependent consortium from coastal sediments

Conductive particles are abundant in coastal sediments, yet the organisms and pathways that use them for methane production remain unclear. We applied long-read, genome-resolved metagenomics to a sediment-derived consortium that remained dependent on granular activated carbon (GAC) for a decade. We identified a particle-obligate food web of electrogenic syntrophic acetate oxidizers (SAO), an electrotrophic methanogen, and necromass recyclers. The dominant SAO electrogen was a new genus, Candidatus Geosyntrophus acetoxidans (<70% ANI/AAI to described taxa), encoding a streamlined extracellular electron-transfer system: one porin-cytochrome conduit (PCC), 47 multiheme cytochromes, conductive pili, and acetate uptake/utilization genes. A second SAO electrogen, Lentimicrobium sp., carried two giant PCC-like clusters, suggesting an alternative acetate-oxidation route. Electrons flowed via GAC to a Methanosarcina (<89% ANI/AAI to described taxa) equipped with the multiheme cytochrome MmcA and a Rnf/Fpo/HdrDE circuit for EET-driven CO2-reducing methanogenesis. Particle-free lines lost both partners and methanogenic activity, establishing particles as the determinant of persistence. This first genomic blueprint of a natural CIET-SAO consortium identifies potential genomic markers (distinct PCCs, MmcA) for in-situ detection and reveals a particle-bound route from acetate to methane likely operating as a fundamental electron-transfer unit in geoconductor-rich anoxic sediments.

microbiology↗

Drivers of methane-cycling archaeal abundances, community structure, and catabolic pathways in continental margin sediments

Marine sediments contain Earths largest reservoir of methane, with most of this methane being produced and consumed in situ by methane-cycling archaea. While numerous studies have investigated communities of methane-cycling archaea in hydrocarbon seeps and sulfate-methane transition zones, little is known about how these archaea change from the seafloor downward in the far more common diffusion-dominated marine sediments. Focusing on four continental margin sites of the North Sea-Baltic Sea transition, we here investigate the in situ drivers of methane-cycling archaeal community structure and metabolism based on geochemical and stable carbon-isotopic gradients, functional gene (mcrA) copy numbers and phylogenetic compositions, as well as thermodynamic calculations. We observe major vertical and lateral changes in community structure that largely follow changes in organic matter reactivity and content, sulfate concentration, and bioturbation activity. While methane-cycling archaeal communities in bioturbation and sulfate reduction zones are dominated by known methyl-dismutating taxa within the Methanosarcinaceae and putatively CO2-reducing Methanomicrobiaceae, the communities change toward dominance of known methane-oxidizing taxa (ANME-2a-b, ANME-2c, ANME-1a-b) in sulfate-methane transitions. Underlying methanogenesis zones were characterized by a change toward mainly physiologically uncharacterized groups, including ANME-1d and several new genus-level groups of putatively CO2-reducing Methanomicrobiaceae and methyl-reducing Methanomassiliicoccales. Notably, group-specific increases in mcrA copy numbers by 2 to 4 orders of magnitude from the sulfate reduction zone into the sulfate-methane transitions or methanogenesis zones indicate the thriving of several major methane-cycling archaeal taxa. Together our study provides insights into the community and pathway shifts vertically along the geochemical gradients and horizontally along the different sedimentary settings and their underlying drivers in continental margin sediments.

ecology↗

Marine deep biosphere microbial communities assemble in near-surface sediments in Aarhus Bay

Analyses of microbial diversity in marine sediments have identified a core set of taxa unique to the marine deep biosphere. Previous studies have suggested that these specialized communities are shaped by processes in the surface seabed, in particular that their assembly is associated with the transition from the bioturbated upper zone to the nonbioturbated zone below. To test this hypothesis, we performed a fine-scale analysis of the distribution and activity of microbial populations within the upper 50 cm of sediment from Aarhus Bay (Denmark). Sequencing and qPCR were combined to determine the depth distributions of bacterial and archaeal taxa (16S rRNA genes) and sulfate-reducing microorganisms (dsrB gene). Mapping of radionuclides throughout the sediment revealed a region of intense bioturbation at 0-6 cm depth. The transition from bioturbated sediment to the subsurface below (7 cm depth) was marked by a shift from dominant surface populations to common deep biosphere taxa (e.g. Chloroflexi & Atribacteria). Changes in community composition occurred in parallel to drops in microbial activity and abundance caused by reduced energy availability below the mixed sediment surface. These results offer direct evidence for the hypothesis that deep subsurface microbial communities present in Aarhus Bay mainly assemble already centimeters below the sediment surface, below the bioturbation zone.

microbiology↗