Publications

4855

Summary The C hlamydiae are a phylum of obligate intracellular bacteria comprising important human and animal pathogens, yet their occurrence in the environment, their phylogenetic diversity and their host range has been largely underestimated. We investigated the seasonality of environmental chlamydiae in a Tyrrhenian coastal lake. By catalysed reporter deposition fluorescence in situ hybridization, we quantified the small planktonic cells and detected a peak in the abundance of environmental chlamydiae in early autumn with up to 5.9 × 10 4 cells ml −1 . Super‐resolution microscopy improved the visualization and quantification of these bacteria and enabled the detection of pleomorphic chlamydial cells in their protist host directly in an environmental sample. To isolate environmental chlamydiae together with their host, we applied a high‐throughput limited dilution approach and successfully recovered a V exillifera sp., strain harbouring chlamydiae (93% 16 S r RNA sequence identity to S imkania negevensis ), tentatively named ‘ C andidatus   N eptunochlamydia vexilliferae’. Transmission electron microscopy in combination with fluorescence in situ hybridization was used to prove the intracellular location of these bacteria representing the first strain of marine chlamydiae stably maintained alongside with their host in a laboratory culture. Taken together, this study contributes to a better understanding of the distribution and diversity of environmental chlamydiae in previously neglected marine environments.

AbstractThe NC10 phylum is a candidate phylum of prokaryotes and is considered important in biogeochemical cycles and evolutionary history. NC10 members are as-yet-uncultured and are difficult to enrich and our knowledge regarding this phylum is largely limited to the first species ‘Candidatus Methylomirabilis oxyfera’ (M. oxyfera). Here, we enriched NC10 members from paddy soil and obtained a novel species of the NC10 phylum that mediates the anaerobic oxidation of methane (AOM) coupled to nitrite reduction. By comparing the new 16S rRNA gene sequences with those already in the database, this new species was found to be widely distributed in various habitats in China. Therefore, we tentatively named it ‘Candidatus Methylomirabilis sinica’ (M. sinica). Cells of M. sinica are roughly coccus-shaped (0.7–1.2 μm), distinct from M. oxyfera (rod-shaped; 0.25–0.5 × 0.8–1.1 μm). Notably, microscopic inspections revealed that M. sinica grew in honeycomb-shaped microcolonies, which was the first discovery of microcolony of the NC10 phylum. This finding opens the possibility to isolate NC10 members using microcolony-dependent isolation strategies.

Summary Although metabolic pathways and associated enzymes of anaerobic ammonium oxidation (anammox) of ‘ Ca . Kuenenia stuttgartiensis’ have been studied, those of other anammox bacteria are still poorly understood. reduction to NO is considered to be the first step in the anammox metabolism of ‘ Ca . K. stuttgartiensis’, however, ‘ Ca . Brocadia’ lacks the genes that encode canonical NO‐forming nitrite reductases (NirS or NirK) in its genome, which is different from ‘ Ca . K. stuttgartiensis’. Here, we studied the anammox metabolism of ‘ Ca . Brocadia sinica’. 15 N‐tracer experiments demonstrated that ‘ Ca . B. sinica’ cells could reduce to NH 2 OH, instead of NO, with as yet unidentified nitrite reductase(s). Furthermore, N 2 H 4 synthesis, downstream reaction of reduction, was investigated using a purified ‘ Ca . B. sinica' hydrazine synthase (Hzs) and intact cells. Both the ‘ Ca . B. sinica’ Hzs and cells utilized NH 2 OH and , but not NO and , for N 2 H 4 synthesis and further oxidized N 2 H 4 to N 2 gas. Taken together, the metabolic pathway of ‘ Ca . B. sinica’ is NH 2 OH‐dependent and different from the one of ‘ Ca . K. stuttgartiensis’, indicating metabolic diversity of anammox bacteria.

Summary The R ickettsiae comprise intracellular bacterial symbionts and pathogens infecting diverse eukaryotes. Here, we provide a detailed characterization of ‘ C andidatus   J idaibacter acanthamoeba’, a rickettsial symbiont of A canthamoeba . The bacterium establishes the infection in its amoeba host within 2 h where it replicates within vacuoles. Higher bacterial loads and accelerated spread of infection at elevated temperatures were observed. The infection had a negative impact on host growth rate, although no increased levels of host cell lysis were seen. Phylogenomic analysis identified this bacterium as member of the M idichloriaceae . Its 2.4 Mb genome represents the largest among R ickettsiales and is characterized by a moderate degree of pseudogenization and a high coding density. We found an unusually large number of genes encoding proteins with eukaryotic‐like domains such as ankyrins, leucine‐rich repeats and tetratricopeptide repeats, which likely function in host interaction. There are a total of three divergent, independently acquired type IV secretion systems, and 35 flagellar genes representing the most complete set found in an obligate intracellular A lphaproteobacterium . The deeply branching phylogenetic position of ‘ C andidatus   J idaibacter acanthamoeba’ together with its ancient features place it closely to the rickettsial ancestor and helps to better understand the transition from a free‐living to an intracellular lifestyle.

Summary The anaerobic oxidation of methane (AOM) is mediated by consortia of anaerobic methane‐oxidizing archaea (ANME) and their specific partner bacteria. In thermophilic AOM consortia enriched from Guaymas Basin, members of the ANME‐1 clade are associated with bacteria of the HotSeep‐1 cluster, which likely perform direct electron exchange via nanowires. The partner bacterium was enriched with hydrogen as sole electron donor and sulfate as electron acceptor. Based on phylogenetic, genomic and metabolic characteristics we propose to name this chemolithoautotrophic sulfate reducer Candidatus Desulfofervidus auxilii. Ca . D. auxilii grows on hydrogen at temperatures between 50°C and 70°C with an activity optimum at 60°C and doubling time of 4–6 days. Its genome draft encodes for canonical sulfate reduction, periplasmic and soluble hydrogenases and autotrophic carbon fixation via the reductive tricarboxylic acid cycle. The presence of genes for pili formation and cytochromes, and their similarity to genes of Geobacter spp., indicate a potential for syntrophic growth via direct interspecies electron transfer when the organism grows in consortia with ANME. This first ANME‐free enrichment of an AOM partner bacterium and its characterization opens the perspective for a deeper understanding of syntrophy in anaerobic methane oxidation.