Although environmental stimuli are known to affect the structure and function of microbial communities, their impact on the metabolic network of microorganisms has not been well investigated. Here, geochemical analyses, high-throughput sequencing of 16S rRNA genes and transcripts, and isolation of potentially relevant bacteria were carried out to elucidate the anaerobic respiration processes stimulated by nitrate (20 mM) amendment of marine sediments. Marine sediments deposited by the Great East Japan Earthquake in 2011 were incubated anaerobically in the dark at 25∘C for 5 days. Nitrate in slurry water decreased gradually for 2 days, then more rapidly until its complete depletion at day 5; production of N2O followed the same pattern. From day 2 to 5, the sulfate concentration significantly increased and the sulfur content in solid-phase sediments significantly decreased. These results indicated that denitrification and sulfur oxidation occurred simultaneously. Illumina sequencing revealed the proliferation of known sulfur oxidizers, i.e., Sulfurimonas sp. and Chromatiales bacteria, which accounted for approximately 43.5% and 14.8% of the total population at day 5, respectively. These oxidizers also expressed 16S rRNA to a considerable extent, whereas the other microorganisms, e.g., iron(III) reducers and methanogens, became metabolically active at the end of the incubation. Extinction dilution culture in a basal-salts medium supplemented with sulfur compounds and nitrate successfully isolated the predominant sulfur oxidizers: Sulfurimonas sp. strain HDS01 and Thioalkalispira sp. strain HDS22. Their 16S rRNA genes showed 95.2–96.7% sequence similarity to the closest cultured relatives and they grew chemolithotrophically on nitrate and sulfur. Novel sulfur-oxidizing bacteria were thus directly involved in carbon fixation under nitrate-reducing conditions, activating anaerobic respiration processes and the reorganization of microbial communities in the deposited marine sediments.

Reduction of crystalline Fe(III) oxides is one of the most important electron sinks for organic compound oxidation in natural environments. Yet the limited number of isolates makes it difficult to understand the physiology and ecological impact of the microorganisms involved. Here, two-stage cultivation was implemented to selectively enrich and isolate crystalline iron(III) oxide reducing microorganisms in soils and sediments. Firstly, iron reducers were enriched and other untargeted eutrophs were depleted by 2-years successive culture on a crystalline ferric iron oxide (i.e., goethite, lepidocrocite, hematite, or magnetite) as electron acceptor. Fifty-eight out of 136 incubation conditions allowed the continued existence of microorganisms as confirmed by PCR amplification. High-throughput Illumina sequencing and clone library analysis based on 16S rRNA genes revealed that the enrichment cultures on each of the ferric iron oxides contained bacteria belonging to the Deltaproteobacteria (mainly Geobacteraceae), followed by Firmicutes and Chloroflexi, which also comprised most of the operational taxonomic units (OTUs) identified. Venn diagrams indicated that the core OTUs enriched with all of the iron oxides were dominant in the Geobacteraceae while each type of iron oxides supplemented selectively enriched specific OTUs in the other phylogenetic groups. Secondly, 38 enrichment cultures including novel microorganisms were transferred to soluble-iron(III) containing media in order to stimulate the proliferation of the enriched iron reducers. Through extinction dilution-culture and single colony isolation, six strains within the Deltaproteobacteria were finally obtained; five strains belonged to the genus Geobacter and one strain to Pelobacter. The 16S rRNA genes of these isolates were 94.8–98.1% identical in sequence to cultured relatives. All the isolates were able to grow on acetate and ferric iron but their physiological characteristics differed considerably in terms of growth rate. Thus, the novel strategy allowed to enrich and isolate novel iron(III) reducers that were able to thrive by reducing crystalline ferric iron oxides.

Stable isotope probing (SIP) of rRNA directly identifies microorganisms assimilating an isotopically labelled substrate. High-throughput DNA sequencing is available for label screening at high resolution and high sensitivity, yet its effectiveness and validity remain to be clarified. Here, we investigated whether the detection sensitivity of rRNA-SIP could be improved by using Illumina sequencing in place of terminal restriction fragment length polymorphism (T-RFLP) analysis. A dilution series of (13) C-labelled RNA from Escherichia coli (1-0.0001%) and unlabelled RNA from Bacillus subtilis was density separated and fractionated. Illumina sequencing of isopycnic centrifugation gradients was able to detect (13) C-labelled RNA in the heaviest fraction with a buoyant density of 1.798 g ml(-1) even at the mixing ratio of 0.001%, whereas the detection ability of T-RFLP was not lower than 0.5%. Quantitative reverse transcription polymerase chain reaction of the density-separated RNAs showed that (13) C-labelled RNAs at mixing ratios of 0.05-0.001% had definitely accumulated in the heaviest fraction. Consequently, high-throughput sequencing provided up to 500-fold higher sensitivity for screening of (13) C-labelled RNA than T-RFLP. Ultra-high-sensitivity rRNA-SIP represents a clear advance towards a more complete understanding of microbial ecosystem function, including the ecophysiology of rare microorganisms in various natural environments.

Organically enriched sediment has been found in water environments. The tsunami originating from the Great East Japan Earthquake in 2011 deposited large amount of sediment, thus providing evidence about its huge accumulation in coastal marine areas possibly due to human activities such as fish culture and marine product processing of industries. Here, degradation potential of organically enriched sediment deposited on a coastal site at Higashi-Matsushima, Miyagi, Japan was investigated under both sulfate-and iron-reducing conditions. Sediment slurry was prepared by mixing the sediment with artificial seawater. The effects of supplementation with sulfate and lepidocrocite (a crystalline Fe[III] oxide) on the structure and activity of the slurry microorganisms were examined by the combined physicochemical analyses and 16S rRNA deep sequencing. The sediment slurry was incubated for 5 days, during which the concentrations of TOC, sulfate, and ferrous iron remained at constant levels and the TG-DTA patterns did not change. The composition of dominant members of the microbial communities was stable, although the rare microbial populations slightly changed. The result in this study revealed that the organically enriched sediment was resistant to biodegradation under the sulfateand iron-reducing conditions.

A large amount of marine sediment was launched on land by the Great East Japan earthquake. Here, we employed both on-site and laboratory studies on the launched marine sediment to investigate the succession of microbial communities and its effects on geochemical properties of the sediment. Twenty-two-month on-site survey showed that microbial communities at the uppermost layer (0–2 mm depth) of the sediment changed significantly with time, whereas those at the deeper layer (20–40 mm depth) remained nearly unchanged and kept anaerobic microbial communities. Nine months after the incidence, various sulfur-oxidizing bacteria (SOB) prevailed in the uppermost layer, in which afterwards diverse chemoorganotrophic bacteria predominated. Geochemical analyses indicated that the concentration of metals other than Fe was lower in the uppermost layer than that in the deeper layer. Laboratory study was carried out by incubating the sediment for 57 days, and clearly indicated the dynamic transition of microbial communities in the uppermost layer exposed to atmosphere. SOB affiliated in the class Epsilonproteobacteria rapidly proliferated and dominated at the uppermost layer during the first 3 days, after that Fe(II)-oxidizing bacteria and chemoorganotrophic bacteria were sequentially dominant. Furthermore, the concentration of sulfate ion increased and the pH decreased. Consequently, SOB may have influenced the mobilization of heavy metals in the sediment by metal-bound sulfide oxidation and/or sediment acidification. These results demonstrate that SOB initiated the dynamic shift from the anaerobic to aerobic microbial communities, thereby playing a critical role in element cycling in the marine sediment.