Publications by authors named "Marc Mussmann"

Electromicrobiology can be used to understand extracellular electron uptake in previously undescribed chemolithotrophs. Enrichment and characterization of the uncultivated electroautotroph " Tenderia electrophaga" using electromicrobiology led to the designation of the order Representative metagenome-assembled genomes (MAGs) have been identified in a number of environmental surveys, yet a comprehensive characterization of conserved genes for extracellular electron uptake has thus far not been conducted. Using comparative genomics, we identified conserved orthologous genes within the and nearest-neighbor orders important for extracellular electron uptake based on a previously proposed pathway from " Tenderia electrophaga.

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Bivalves from the family Lucinidae host sulfur-oxidizing bacterial symbionts, which are housed inside specialized gill epithelial cells and are assumed to be acquired from the environment. However, little is known about the Lucinidae life cycle and symbiont acquisition in the wild. Some lucinid species broadcast their gametes into the surrounding water column, however, a few have been found to externally brood their offspring by the forming gelatinous egg masses.

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Molecular surveys of low temperature deep-sea hydrothermal vent fluids have shown that (previously ) often dominate the microbial community and that three genera, , , and , frequently coexist. In this study, we used replicated radiocarbon incubations of deep-sea hydrothermal fluids to investigate activity of each genus under three experimental conditions. To quantify genus-specific radiocarbon incorporation, we used newly designed oligonucleotide probes for , , and to quantify their activity using catalyzed-reporter deposition fluorescence hybridization (CARD-FISH) combined with fluorescence-activated cell sorting.

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Sulphide-driven anoxygenic photosynthesis is an ancient microbial metabolism that contributes significantly to inorganic carbon fixation in stratified, sulphidic water bodies. Methods commonly applied to quantify inorganic carbon fixation by anoxygenic phototrophs, however, cannot resolve the contributions of distinct microbial populations to the overall process. We implemented a straightforward workflow, consisting of radioisotope labelling and flow cytometric cell sorting based on the distinct autofluorescence of bacterial photopigments, to discriminate and quantify contributions of co-occurring anoxygenic phototrophic populations to in situ inorganic carbon fixation in environmental samples.

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Acetate is a key intermediate in anaerobic mineralization of organic matter in marine sediments. Its turnover is central to carbon cycling, however, the relative contribution of different microbial populations to acetate assimilation in marine sediments is unknown. To quantify acetate assimilation by abundant bacterial populations, we incubated coastal marine sediments with C-labeled acetate and flow-sorted cells that had been labeled and identified by fluorescence hybridization.

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Chemoautotrophic bacteria belonging to the genus Sulfurimonas (class Campylobacteria) were previously identified as key players in the turnover of zero-valence sulfur, a central intermediate in the marine sulfur cycle. S. denitrificans was further shown to be able to oxidize cyclooctasulfur (S ).

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Article Synopsis
  • Coastal oceans are impacted by human-caused nitrogen inputs, which are often denitrified in sandy sediments before they reach the open ocean.
  • Sandy sediments facilitate this process through porewater transport, impacting organic matter and oxygen levels, but how denitrifying microorganisms adapt to these changes is not fully understood.
  • Research from the Wadden Sea shows that different microorganisms are responsible for denitrification, producing nitrous oxide (N2O) that is released into the atmosphere, which may have implications for other coastal environments as well.
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In this Article, the completeness and number of contigs for draft genomes from two individuals of Laxus oneistus are incorrect in the main text, although the correct information is included in Table 1. The original and corrected versions of the relevant sentence are shown in the correction notice.

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Molecular hydrogen (H ) is the key intermediate in the anaerobic degradation of organic matter. Its removal by H -oxidizing microorganisms is essential to keep anaerobic degradation energetically favourable. Sulfate-reducing microorganisms (SRM) are known as the main H scavengers in anoxic marine sediments.

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Article Synopsis
  • Chlamydiae are specialized bacteria that can be harmful or help other organisms, with many species likely existing in diverse marine environments, though most research focuses on land-based types.
  • Recent studies of marine chlamydiae have uncovered unique genetic traits, including a complete flagellar system, suggesting these bacteria can move and may have evolved differently compared to their land relatives.
  • The findings imply that marine chlamydiae have greater adaptability and may play a significant role in host interactions, expanding our understanding of their biology and ecological impact.
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Almost the entire seafloor is covered with sediments that can be more than 10 000 m thick and represent a vast microbial ecosystem that is a major component of Earth's element and energy cycles. Notably, a significant proportion of microbial life in marine sediments can exploit energy conserved during transformations of sulfur compounds among different redox states. Sulfur cycling, which is primarily driven by sulfate reduction, is tightly interwoven with other important element cycles (carbon, nitrogen, iron, manganese) and therefore has profound implications for both cellular- and ecosystem-level processes.

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To date, very little is known about the bacterial core community of marine sediments. Here we study the environmental distribution, abundance and ecogenomics of the gammaproteobacterial Woeseiaceae/JTB255 marine benthic group. A meta-analysis of published work shows that the Woeseiaceae/JTB255 are ubiquitous and consistently rank among the most abundant 16S rRNA gene sequences in diverse marine sediments.

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Chemosynthetic symbioses are partnerships between invertebrate animals and chemosynthetic bacteria. The latter are the primary producers, providing most of the organic carbon needed for the animal host's nutrition. We sequenced genomes of the chemosynthetic symbionts from the lucinid bivalve Loripes lucinalis and the stilbonematid nematode Laxus oneistus.

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Large, colorless sulfur-oxidizing bacteria (LSB) of the family Beggiatoaceae form thick mats at sulfidic sediment surfaces, where they efficiently detoxify sulfide before it enters the water column. The genus Thiomargarita harbors the largest known free-living bacteria with cell sizes of up to 750 μm in diameter. In addition to their ability to oxidize reduced sulfur compounds, some Thiomargarita spp.

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The genus Thiomargarita includes the world's largest bacteria. But as uncultured organisms, their physiology, metabolism, and basis for their gigantism are not well understood. Thus, a genomics approach, applied to a single Candidatus Thiomargarita nelsonii cell was employed to explore the genetic potential of one of these enigmatic giant bacteria.

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Marine sediments are the largest carbon sink on earth. Nearly half of dark carbon fixation in the oceans occurs in coastal sediments, but the microorganisms responsible are largely unknown. By integrating the 16S rRNA approach, single-cell genomics, metagenomics and transcriptomics with (14)C-carbon assimilation experiments, we show that uncultured Gammaproteobacteria account for 70-86% of dark carbon fixation in coastal sediments.

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Article Synopsis
  • Diffuse hydrothermal fluids contain various organic compounds, and the study aimed to identify heterotrophic microorganisms consuming these compounds without prior cultivation methods.
  • Researchers used microbial community analysis and short-term (13)C-labeled acetate incubations at two hydrothermal systems: Menez Gwen (55 °C) and Manus Basin (37 °C) to track cell growth and acetate assimilation.
  • Findings revealed a novel epsilonproteobacterial group as the primary acetate consumer at Menez Gwen, while Gammaproteobacteria dominated in Manus Basin, showcasing the opportunistic nature of these microorganisms to utilize available energy sources in fluctuating environments.
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Zero-valence sulfur (S°) is a central intermediate in the marine sulfur cycle and forms conspicuous accumulations at sediment surfaces, hydrothermal vents and in oxygen minimum zones. Diverse microorganisms can utilize S°, but those consuming S° in the environment are largely unknown. We identified possible key players in S° turnover on native or introduced S° in benthic coastal and deep-sea habitats using the 16S ribosomal RNA approach, (in situ) growth experiments and activity measurements.

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Hydrothermal sediments in the Guaymas Basin are covered by microbial mats that are dominated by nitrate-respiring and sulphide-oxidizing Beggiatoa. The presence of these mats strongly correlates with sulphide- and ammonium-rich fluids venting from the subsurface. Because ammonium and oxygen form opposed gradients at the sediment surface, we hypothesized that nitrification is an active process in these Beggiatoa mats.

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Desulfocapsa sulfexigens SB164P1 (DSM 10523) belongs to the deltaproteobacterial family Desulfobulbaceae and is one of two validly described members of its genus. This strain was selected for genome sequencing, because it is the first marine bacterium reported to thrive on the disproportionation of elemental sulfur, a process with a unresolved enzymatic pathway in which elemental sulfur serves both as electron donor and electron acceptor. Furthermore, in contrast to its phylogenetically closest relatives, which are dissimilatory sulfate-reducers, D.

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Effluents from wastewater treatment plants (WWTPs) containing micro-organisms and residual nitrogen can stimulate nitrification in freshwater streams. We hypothesized that different ammonia-oxidizing (AOB) and nitrite-oxidizing (NOB) bacteria present in WWTP effluents differ in their potential to colonize biofilms in the receiving streams. In an experimental approach, we monitored biofilm colonization by nitrifiers in ammonium- or nitrite-fed microcosm flumes after inoculation with activated sludge.

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Among the dominant deltaproteobacterial sulfate-reducing bacteria (SRB), members of the genus Desulfobacula are not only present in (hydrocarbon-rich) marine sediments, but occur also frequently in the anoxic water bodies encountered in marine upwelling areas. Here, we present the 5.2 Mbp genome of Desulfobacula toluolica Tol2, which is the first of an aromatic compound-degrading, marine SRB.

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Article Synopsis
  • The bacterium Candidatus Allobeggiatoa halophila has a specialized vacuole that contains an electron transport chain (ETC) responsible for creating a proton motive force (PMF) for energy conservation.
  • Immunostaining confirmed the presence of key proteins like cytochrome c oxidase and vacuolar ATPase in the vacuolar membrane, which are essential for maintaining vacuolar pH and generating ATP.
  • The study findings indicate that nitrate respiration boosts the proton concentration in the vacuole, demonstrating its role in enhancing the PMF necessary for the bacterium's energy needs.
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A novel fluorescence in situ hybridisation (FISH) method is presented that allows the combination of epifluorescence and scanning electron microscopy (SEM) to identify single microbial cells. First, the rRNA of whole cells is hybridised with horseradish peroxidase-labelled oligonucleotide probes and this is followed by catalysed reporter deposition (CARD) of biotinylated tyramides. This facilitates an amplification of binding sites for streptavidin conjugates covalently labelled with both fluorophores and nanogold particles.

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Roseobacter clade bacteria (RCB) are abundant in marine bacterioplankton worldwide and central to pelagic sulfur cycling. Very little is known about their abundance and function in marine sediments. We investigated the abundance, diversity and sulfur oxidation potential of RCB in surface sediments of two tidal flats.

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