Search

A Nonomuraea sp. strain MM565M-173N2 was isolated from deep-sea sediment off the Sanriku coast, and new antibiotics were evaluated against carbapenem-resistant Enterobacteriaceae (CRE), which is a problematic group of bacteria because of their antimicrobial resistance. From 220 l of fermented broth from strain MM565M-173N2, we isolated four new antibiotics by gel filtration and HPLC, designated as sealutomicins A (1.8 mg), B (1.5 mg), C (0.8 mg), and D (0.8 mg). Their structures were determined from MS, NMR, and CD spectra. Sealutomicin A was found to be a new enediyne antibiotic, while sealutomicins B-D were aromatized products from sealutomicin A. Sealutomicin A showed strong antibacterial activity (MIC 0.05-0.2 μg ml-1) against CRE.

Deep-sea bacteria can produce various biotechnologically relevant enzymes due to their adaptations to high pressures and low temperatures. To identify such enzymes, we have sequenced the genome of the polycaprolactone-degrading bacterium Moritella sp. JT01, isolated from sediment samples from Japan Trench (6957 m depth), using a Illumina HiSeq2000 sequencer (12.1 million paired-end reads) and CLC Genomics Workbench (version 6.5.1) for the assembly, resulting in a 4.83-Mb genome (42 scaffolds). The genome was annotated using Rapid Annotation using Subsystem Technology (RAST), Protein Homology/analogY Recognition Engine V 2.0 (PHYRE2), and BLAST2Go, revealing 4439 protein coding sequences and 101 RNAs. Gene products with industrial relevance, such as lipases (three) and esterases (four), were identified and are related to bacterium's ability to degrade polycaprolactone. The annotation revealed proteins related to deep-sea survival, such as cold-shock proteins (six) and desaturases (three). The presence of secondary metabolite biosynthetic gene clusters suggests that this bacterium could produce nonribosomal peptides, polyunsaturated fatty acids, and bacteriocins. To demonstrate the potential of this genome, a lipase was cloned an introduced into Escherichia coli. The lipase was purified and characterized, showing activity over a wide temperature range (over 50% at 20-60 °C) and pH range (over 80% at pH 6.3 to 9). This enzyme has tolerance to the surfactant action of sodium dodecyl sulfate and shows 30% increased activity when subjected to a working pressure of 200 MPa. The genomic characterization of Moritella sp. JT01 reveals traits associated with survival in the deep-sea and their potential uses in biotechnology, as exemplified by the characterized lipase.

The deep-sea denitrifier Pseudomonas sp. MT-1 has two gene clusters encoding dissimilatory nitrate reductases, periplasmic nitrate reductase (Nap) and membrane-bound nitrate reductase (Nar). In order to investigate the physiological role of these enzymes, we constructed the disrupted mutants of napA, narG, and narK (encoding the catalytic subunits of Nap and Nar, as well as the nitrate transporter, respectively). The napA mutant showed almost the same growth rate as the wild-type under both atmospheric and high pressure of 30 MPa. On the other hand, the narG and narK mutants showed growth deficiencies under atmospheric pressure which were more pronounced at a pressure of 30 MPa. Thus, Nar was shown to be the dominant dissimilatory nitrate reductase in MT-1, especially under high pressure, whereas Nap can support the growth with denitrification to some extent. Further, nitrate reductase activity of the soluble and membrane fractions of MT-1 was measured under high pressure. Both activities were highly piezotolerant even under a pressure of 150 MPa. Therefore, the stability of nitrate reductases under high pressure is not a limiting step for the growth of MT-1 under these conditions. Although the reason why Nar rather than Nap is dominant and the physiological role of Nap in MT-1 are still unclear, we have demonstrated the mechanisms of the denitrification system in the environment of the deep-sea.

Here, we report the genome sequence of Bacillus subtilis strain 29R7-12, a piezophilic bacterium isolated from coal-bearing sediment down to ~2.4 km below the ocean floor in the northwestern Pacific. The strain is a Gram-positive spore-forming bacterium, closely related to Bacillus subtilis within the phylum Firmicutes . This is the first complete genome sequence of a Bacillus subtilis strain from the deep biosphere. The genome sequence will provide a valuable resource for comparative studies of microorganisms from the surface and subsurface environments.

Phylogenetically diverse microorganisms have been observed in marine subsurface sediments down to ~2.5 km below the seafloor (kmbsf). However, very little is known about the pressure-adapted and/or pressure-loving microorganisms, the so called piezophiles, in the deep subseafloor biosphere, despite that pressure directly affects microbial physiology, metabolism, and biogeochemical processes of carbon and other elements in situ. In this study, we studied taxonomic compositions of microbial communities in high-pressure incubated sediment, obtained during the Integrated Ocean Drilling Program (IODP) Expedition 337 off the Shimokita Peninsula, Japan. Analysis of 16S rRNA gene-tagged sequences showed that members of spore-forming bacteria within Firmicutes and Actinobacteria were predominantly detected in all enrichment cultures from ~1.5 to 2.4 km-deep sediment samples, followed by members of Proteobacteria, Acidobacteria, and Bacteroidetes according to the sequence frequency. To further study the physiology of the deep subseafloor sedimentary piezophilic bacteria, we isolated and characterized two bacterial strains, 19R1-5 and 29R7-12, from 1.9 and 2.4 km-deep sediment samples, respectively. The isolates were both low G+C content, gram-positive, endospore-forming and facultative anaerobic piezophilic bacteria, closely related to Virgibacillus pantothenticus and Bacillus subtilis within the phylum Firmicutes, respectively. The optimal pressure and temperature conditions for growth were 20 MPa and 42°C for strain 19R1-5, and 10 MPa and 43°C for strain 29R7-12. Bacterial (endo)spores were observed in both the enrichment and pure cultures examined, suggesting that these piezophilic members were derived from microbial communities buried in the ~20 million-year-old coal-bearing sediments after the long-term survival as spores and that the deep biosphere may host more abundant gram-positive spore-forming bacteria and their spores than hitherto recognized.

We developed an electrical modulation method for attachment and detachment of microorganisms. Living microorganisms suspended in non-nutritive media such as PBS(−) and artificial seawater were attracted by and selectively attached to indium tin oxide (ITO)/glass electrode regions to which a negative potential was applied. The microorganisms suspended in LB medium and glucose solution were not attracted to the ITO electrode. Dead microorganisms were not attracted to the ITO electrode. The living microorganisms were retrieved after detachment from the ITO electrode by application of a high-frequency triangular wave potential. When we applied this method to separate microorganisms from deep-sea sediment, bacteria belonging to 19 phyla and 23 classes were collected without undesirable high molecular weight contaminants such as humic acids. At the phylum and class level, respectively, 95 and 87 % of the phylotypes among electrically retrieved bacteria were common to the gene clones from the direct sediment DNA extraction. This technique is a novel useful method to prepare bacterial cells in a single population or a community for metagenomic analyses.

Organisms living in deep seas such as the Mariana Trench must be adapted to the extremely high pressure environment. For example, the 3-isopropylmalate dehydrogenase from the obligate piezophile Shewanella benthica DB21MT-2 (SbIPMDH) remains active in extreme conditions under which that from the land bacterium S. oneidensis MR-1 (SoIPMDH) becomes inactivated. In order to unravel the differences between these two IPMDHs, their structures were determined at ~1.5 Å resolution. Comparison of the structures of the two enzymes shows that SbIPMDH is in a more open form and has a larger internal cavity volume than SoIPMDH at atmospheric pressure. This loosely packed structure of SbIPMDH could help it to avoid pressure-induced distortion of the native structure and to remain active at higher pressures than SoIPMDH.

Shewanella violacea DSS12, a deep-sea bacterium, produces eicosapentaenoic acid (EPA) as a component of membrane phospholipids. Although various isolates from the deep sea, such as Photobacterium profundum SS9, Colwellia psychrerythraea 34H and various Shewanella strains, produce EPA- or docosahexaenoic acid-containing phospholipids, the physiological role of these polyunsaturated fatty acids remains unclear. In this article, we illustrate the physiological importance of EPA for high-pressure adaptation in strain DSS12 with the help of an EPA-deficient mutant (DSS12(pfaA)). DSS12(pfaA) showed significant growth retardation at 30 MPa, but not at 0.1 MPa. We also found that DSS12(pfaA) grown at 30 MPa forms filamentous cells. When an EPA-containing phospholipid (sn-1-oleoly-sn-2-eicosapentaenoyl phosphatidylethanolamine) was supplemented, the growth retardation and the morphological defect of DSS12(pfaA) were suppressed, indicating that the externally added EPA-containing phospholipid compensated for the loss of endogenous EPA. In contrast, the addition of an oleic acid-containing phospholipid (sn-1,2-dioleoyl phosphatidylethanolamine) did not affect the growth and the morphology of the cells. Immunofluorescent microscopic analysis with anti-FtsZ antibody revealed a number of Z-rings and separated nucleoids in DSS12(pfaA) grown at 30 MPa. These results demonstrate the physiological importance of EPA for the later step of Z-ring formation of S. violacea DSS12 under high-pressure conditions.

We have isolated thirteen different bacterial strains as poly e-caprolactone (PCL)-degrading bacteria from the Kurile and Japan Trenches at a depth of 5,000-7,000 m (deeper ocean bottoms). The isolates belong to the Shewanella, Moritella, Psychrobacter and Pseudomonas genera. This is the first record of PCL degrading bacteria isolated from deep-sea environments at depth of over 5,000 m. Six strains of the isolates, numbered CT01 in genus Shewanella, CT12, JT01 and JT04 in genus Moritella, JT05 in genus Psychrobacter, and JT08 in genus Pseudomonas were selected for investigation of their cell shapes, degrading abilities for several aliphatic polyesters, and growth profiles. The cell shapes of the strains, except JT05, were rod-shaped, non-spore-forming and motile by means of a single or multi polar flagella. The cell shapes of JT05 were coccal with no visible flagella. From the results of degradation tests on six different alihphatic polyesters, all strains could degrade only PCL. Strains CT01, CT12, JT01 and JT04 are psychrophilic and pressure tolerant bacteria and three strains except JT04 showed typical piezophilic growth profiles. Therefore, it is possible that these strains might play a role in degrading aliphatic polyesters under deep-sea conditions, ie., low-temperatures and high hydrostatic pressures.

To examine whether dihydrofolate reductase (DHFR) from deep-sea bacteria has undergone molecular evolution to adapt to high-pressure environments, we cloned eight DHFRs from Shewanella species living in deep-sea and ambient atmospheric-pressure environments, and subsequently purified six proteins to compare their structures, stabilities, and functions. The DHFRs showed 74–90% identity in primary structure to DHFR from S. violacea, but only 55% identity to DHFR from Escherichia coli (ecDHFR). Far-ultraviolet circular dichroism and fluorescence spectra suggested that the secondary and tertiary structures of these DHFRs were similar. In addition, no significant differences were found in structural stability as monitored by urea-induced unfolding and the kinetic parameters, K m and k cat; although the DHFRs from Shewanella species were less stable and more active (2- to 4-fold increases in k cat/K m) than ecDHFR. Interestingly, the pressure effects on enzyme activity revealed that DHFRs from ambient-atmospheric species are not necessarily incompatible with high pressure, and DHFRs from deep-sea species are not necessarily tolerant of high pressure. These results suggest that the DHFR molecule itself has not evolved to adapt to high-pressure environments, but rather, those Shewanella species with enzymes capable of retaining functional activity under high pressure migrated into the deep-sea.

A procedure for the isolation of aliphatic polyester-degrading bacteria from deep-sea environments was developed using three step high-pressure cultivation. First, the sediments collected from the deep-sea floor, the Kurile and Japan Trenches at a depth of 5000-7000 m, were cultivated with poly e-caprolactone (PCL) films under low-temperature (4°C) and high-pressure (50MPa) conditions. Secondly, high-pressure continuous cultivation using the deep-sea baro-piezophile and thermophile isolation and cultivation (DEEPBATH) system was performed three times to accumulate piezophilic bacteria. Finally, piezophilic PCL degrading bacteria were isolated using the pressure bag method involving media with PCL granules. Using this procedure, we succeeded in isolating several piezophilic aliphatic polyester-degrading bacteria from the sediment samples of deep-trenches.

To understand sulfur oxidation in thioauto-trophic deep-sea clam symbionts, we analyzed the recently reported genomes of two chemoautotrophic symbionts of Calyptogena okutanii (Candidatus Vesicomyosocius okutanii strain HA: Vok) and C. magnifica (Candidatus Ruthia magnifica strain Cm: Rma), and examined the sulfur oxidation gene expressions in the Vok by RT-PCR. Both symbionts have genes for sulfide-quinone oxidoreductase (sqr), dissimilatory sulfite reductase (dsr), reversible dissimilatory sulfite reductase (rdsr), sulfur-oxidizing multienzyme system (sox)(soxXYZA and soxB but lacking soxCD), adenosine phosphosulfate reductase (apr), and ATP sulfurylase (sat). While these genomes share 29 orthologous genes for sulfur oxidation implying that both symbionts possess the same sulfur oxidation pathway, Rma has a rhodanese-related sulfurtransferase putative gene (Rmag0316) that has no corresponding ortholog in Vok, and Vok has one unique dsrR (COSY0782). We propose that Calyptogena symbionts oxidize sulfide and thiosulfate, and that sulfur oxidation proceeds as follows. Sulfide is oxidized to sulfite by rdsr. Sulfite is oxidized to sulfate by apr and sat. Thiosulfate is oxidized to zero-valence sulfur by sox, which is then reduced to sulfide by dsr. In addition, thiosulfate may also be oxidized into sulfate by another component of sox. The result of the RT-PCR showed that genes (dsrA, dsrB, dsrC, aprA, aprB, sat, soxB, and sqr) encoding key enzymes catalyzing sulfur oxidation were all equally expressed in the Vok under three different environmental conditions (aerobic, semioxic, and aerobic under high pressure at 9 MPa), indicating that all sulfur oxidation pathways function simultaneously to support intracellular symbiotic life.

Shewanella violacea DSS12 is facultative piezophile isolated from the deep-sea. The expression of cydDC genes (required for d-type cytochrome maturation) of the organism is regulated by hydrostatic pressure. In this study, we analyzed the nucleotide sequence upstream of cydDC in detail and found that there are putative binding sites for the NarL protein which is part of a two-component regulatory system also containing the sensor protein NarX. Furthermore, we identified the narQP genes (homologues of narXL) from S. violacea DSS12 and demonstrated the heterologous expression of narP in Escherichia coli. These results will be helpful in examining pressure regulation of gene expression in S. violacea at the molecular level.

The effect of pressure on viability and the synthesis of bacterial cellulose (BC) by Gluconacetobacter xylinus ATCC53582 were investigated. G. xylinus was statically cultivated in a pressurized vessel under 0.1, 30, 60, and 100 MPa at 25 degrees C for 6 days. G. xylinus cells remained viable and retained cellulose producing ability under all the conditions tested, though the production of cellulose decreased with increasing the pressure. The BCs produced at each pressure condition were analyzed by field emission scanning electron microscopy (FE-SEM) and Fourier Transform Infrared (FT-IR). FE-SEM revealed that the widths of BC fibers produced under high pressure decreased as compared with those produced under the atmospheric pressure. By FT-IR, all the BCs were found to be of Cellulose type I, as the same as typical native cellulose. Our findings evidently showed that G. xylinus possessed a piezotolerant (barotolerant) feature adapting to 100 MPa without losing its BC producing ability. This was the first attempt in synthesizing BC with G. xylinus under elevated pressure of 100 MPa, which corresponded to the deep sea at 10,000 m.

3-Isopropylmalate dehydrogenase (IPMDH) from the extreme piezophile Shewanella benthica (SbIPMDH) is more pressure-tolerant than that from the atmospheric pressure-adapted Shewanella oneidensis (SoIPMDH). To understand the molecular mechanisms of this pressure tolerance, we analyzed mutated enzymes. The results indicate that only a single mutation at position 266, corresponding to Ala (SbIPMDH) and Ser (SoIPMDH), essentially affects activity under higher-pressure conditions. Structural analyses of SoIPMDH suggests that penetration of three water molecules into the cleft around Ser266 under high-pressure conditions could reduce the activity of the wild-type enzyme; however, no water molecule is observed in the Ala266 mutant.

Microbial communities in Calyptogena sediment and microbial mats of Sagami Bay, Japan, were characterized using 16S rRNA gene sequencing and lipid biomarker analysis. Characterization of 16S rRNA gene isolated from these samples suggested a predominance of bacterial phylotypes related to Gammaproteobacteria (57–64%) and Deltaproteobacteria (27–29%). The Epsilonproteobacteria commonly found in cold seeps and hydrothermal vents were only detected in the microbial mat sample. Significantly different archaeal phylotypes were found in Calyptogena sediment and microbial mats; the former contained only Crenarchaeota clones (100% of the total archaeal clones) and the latter exclusively Euryarchaeota clones, including the anaerobic oxidation of methane archaeal groups ANME-2a and ANME-2c. Many of these lineages are as yet uncultured and undescribed groups of bacteria and archaea. Phospholipid fatty acid analysis suggested the presence of sulphate-reducing and sulphur-oxidizing bacteria. Results of intact glyceryl dialkyl glyceryl tetraether lipid analysis indicated the presence of nonthermophilic marine planktonic archaea. These results suggest that the microbial community in the Sagami Bay seep site is distinct from previously characterized cold-seep environments.

Microbial communities inhabiting deep-sea cold seep sediments at the northeastern Japan Sea were characterized by molecular phylogenetic and chemical analyses. White patchy microbial mats were observed along the fault offshore the Hokkaido Island and sediment samples were collected from two stations at the southern foot of the Shiribeshi seamount (M1 site at a depth of 2,961 m on the active fault) and off the Motta Cape site (M2 site at a depth of 3,064 m off the active fault). The phylogenetic and terminal-restriction fragment polymorphism analyses of PCR-amplified 16S rRNA genes revealed that microbial community structures were different between two sampling stations. The members of ANME-2 archaea and diverse bacterial components including sulfate reducers within Deltaproteobacteria were detected from M1 site, indicating the occurrence of biologically mediated anaerobic oxidation of methane, while microbial community at M2 site was predominantly composed of members of Marine Crenarchaeota group I, sulfate reducers of Deltaproteobacteria, and sulfur oxidizers of Epsilonproteobacteria. Chemical analyses of seawater above microbial mats suggested that concentrations of sulfate and methane at M1 site were largely decreased relative to those at M2 site and carbon isotopic composition of methane at M1 site shifted heavier ((13)C-enriched), the results of which are consistent with molecular analyses. These results suggest that the mat microbial communities in deep-sea cold seep sediments at the northeastern Japan Sea are significantly responsible for sulfur and carbon circulations and the geological activity associated with plate movements serves unique microbial habitats in deep-sea environments.

We have investigated the molecular phylogeny of cold-seep sediments obtained from the Nankai Trough, at depths of about 600, 2,000, and 3,300 m, and compared the microbial diversity profiles of those sediments samples. The gamma-Proteobacteria that might function as sulfide oxidizers and the symbiotically related delta-Proteobacteria which might function as sulfate reducers were identified amongst the bacteria from all depths of the sediments. However, anoxic methane oxidizing archaea (ANME) and methanogens were only found in the 600 m deep sediments. These results indicated that the cold-seep microbial sulfur circulation system could be functioning in the shallow seep sediment at a depth of 600 m and the microbial activities at these sites might be more dynamic than at other deeper cold-seep sites.

Some rod-shaped bacteria, including Escherichia coli, exhibit cell filamentation without septum formation under high-hydrostatic-pressure conditions, indicating that the cell-division process is affected by hydrostatic pressure. The effects of elevated pressure on FtsZ-ring formation in E. coli cells were examined using indirect immunofluorescence microscopy. Elevated pressure of 40 MPa completely inhibited colony formation of E. coli cells under the cultivation conditions used, and the cells exhibited obviously filamentous shapes. In the elongated cells, normal cell-division processes appeared to be inhibited, because no FtsZ rings were observed by indirect immunofluorescent staining. In addition, it was observed that hydrostatic pressure dissociated the E. coli FtsZ polymers in vitro. These results suggest that high hydrostatic pressure directly affects cell survival and morphology through the dissociation of the cytoskeletal frameworks.

We have cloned the rpoZ gene, encoding RNA polymerase omega protein, by PCR approach from the deep-sea piezophilic and psychrophilic bacterium, Shewanella violacea strain DSS12. The cloned gene, 285bp in length, was found to encode a protein consisting of 94 amino acid residues with a molecular mass of 10,327 Da. Significant homology was evident comparing the RpoZ protein of S. violacea with that of Shewanella oneidensis (69% identity), Vibrio cholerae (65% identity), Escherichia coli K-12 (64% identity) and Haemophilus influenzae (61% identity). From the Northern blot analysis, S. violacea rpoZ gene was expressed constitutively under pressure conditions of 0.1, 30 and 50MPa. We constructed expression plasmid to overproduce the RpoZ protein and transformed into E. coli JM109 as a host of overproduction. Upon induction, the recombinant protein encoded by plasmid pQrpoZ was overexpressed and purified using Ni2+ affinity column.

The effect of pressure and temperature on the growth of the mesophilic lactic acid bacteria Lactococcus lactis and Lactobacillus sanfranciscensis was studied. Both strains were piezosensitive. Lb. sanfranciscensis failed to grow at 50 MPa and the growth rate of Lc. lactis at 50 MPa was less than 30% of that at atmospheric pressure. An increase of growth temperature did not improve the piezotolerance of either organism. During growth under high-pressure conditions, the cell morphology was changed, and the cells were elongated as cell division was inhibited. At atmospheric pressure, temperatures above the optimal temperature for growth caused a similar effect on cell morphology and cell division in both bacteria as that observed under high-pressure conditions. The segregation and condensation of chromosomal DNA were observed by DAPI staining and occurred normally at high-pressure conditions independent of changes in cell morphology. Immunofluorescence microscopy of Lc. lactis cells demonstrated an inhibitory effect of high pressure on the formation of the FtsZ ring and this inhibition of the FtsZ ring formation is suggested to contribute to the altered cell morphology and growth inhibition induced by high pressure.

Two strains of obligately piezophilic bacteria were isolated from sediment collected from the deepest cold-seep environment with chemosynthesis-based animal communities within the Japan Trench, at a depth of 7434 m. The isolated strains, JT7301 and JT7304 T , were closely affiliated with members of the genus Psychromonas on the basis of 16S rDNA sequence analysis. Hybridization values for DNA-DNA relatedness between these strains and the Psychromonas antarctica reference strain were significantly lower than that accepted as the phylogenetic definition of a species. The optimal temperature and pressure for growth of the isolates were 10 °C and 50 MPa and they produced both eicosapentaenoic acid (C20:5ω3) and docosahexaenoic acid (C22:6) in the membrane layer. Based on the taxonomic differences observed, the isolated strains appear to represent a novel obligately piezophilic Psychromonas species. The name Psychromonas kaikoae sp. nov. (type strain JT7304 T = JCM 11054 T = ATCC BAA-363 T ) is proposed. This is the first proposed obligately piezophilic species of the genus Psychromonas.

The dcw cluster of genes involved in cell division and cell wall synthesis from the piezophilic deep-sea bacterium Shewanella violacea was isolated and characterized. It comprises 15 open reading frames, of which the organization is mraZ-mraW-ftsL-ftsI-murE-murF-mraY-murD-ftsW-murG-murC-ftsQ-ftsA-ftsZ-envA, in that order. To analyze transcription upstream from the ftsZ gene, Northern blot and primer extension analyses were performed. The results showed that gene expression is not pressure dependent. Western blot analysis showed that the FtsZ protein is equally expressed under several pressure conditions in the range of atmospheric (0.1 MPa) to high (50 MPa) pressures. Using immunofluorescence microscopy, the FtsZ ring was observed in the center of cells at pressure conditions of 0.1 to 50 MPa. These results imply that the FtsZ protein function is not affected by elevated pressure in this piezophilic bacterium.

A depth profile of naturally occurring bacterial community structures associated with the deep-sea cold seep push-core sediment in the Japan Trench at a depth of 5343 m were evaluated using molecular phylogenetic analyses of RNA reverse transcription-PCR (RT-PCR) amplified 16S crDNA fragments. A total of 137 clones of bacterial crDNA (complimentary rDNA) phylotypes (phylogenetic types) obtained at three different depths (2-4, 8-10 and 14-16 cm) were identified in partial crDNA sequencings. crDNA phylotypes from the cold seep sediment were dominantly composed of delta- and epsilon-Proteobacteria (36% and 42% respectively). Phylotype analysis of crDNA clone libraries and terminal restriction fragment length polymorphism (T-RFLP) analysis revealed that the majority of bacterial components shifted from delta- Proteobacteria to epsilon-Proteobacteria with increasing depth. Among the delta-proteobacterial crDNA clones, the sequences related to the genus Desulfosarcina were dominant. Almost all sequences of crDNA belonging to epsilon-Proteobacteria were affiliated with the same cluster (epsilon-CSG: epsilon-proteobacterial cold seep group), and were closely related with rDNA sequences from deep-sea hydrothermal vent environments.

When non-extremophiles encounter extreme environmental conditions, which are natural for the extremophiles, stress reactions, e.g., expression of heat shock proteins (HSPs), are thought to be induced for survival. To understand how the extremophiles live in such extreme environments, we studied the effects of high hydrostatic pressure on cellular contents of HSPs and their mRNAs during growth in a piezophilic bacterium, Shewanella violacea. HSPs increased at high hydrostatic pressures even when optimal for growth. The mRNAs and proteins of these HSPs significantly increased at higher hydrostatic pressure in S. violacea. In the non-piezophilic Escherichia coli, however, their mRNAs decreased, while their proteins did not change. Several transcriptional start sites (TSSs) for HSP genes were determined by the primer extension method and some of them showed hydrostatic pressure-dependent increase of the mRNAs. A major refolding target of one of the HSPs, chaperonin, at high hydrostatic pressure was shown to be RplB, a subunit of the 50S ribosome. These results suggested that in S. violacea, HSPs play essential roles, e.g., maintaining protein complex machinery including ribosomes, in the growth and viability at high hydrostatic pressure, and that, in their expression, the transcription is under the control of σ(32).

This chapter focuses on the isolation, taxonomy, and diversity of piezophilic microorganisms and their habitats. Based upon several studies the authors have indicated that cultivated psychrophilic and piezophilic deep-sea bacteria could be affiliated with one of five genera within the Gammaproteobacteria subgroup: Shewanella, Photobacterium, Colwellia, Moritella, and Psychromonas, which was formally classified as ‘’an unidentified genus’’. The chapter describes taxonomic features of the piezophilic genera. For handling piezophiles for further study, JAMSTEC developed a deep-sea baropiezophile and thermophile isolation and cultivation system, referred to as the DEEPBATH system. The DEEPBATH system consists of four separate devices: (1) a pressure-retaining sampling device, (2) a dilution device under pressure conditions, (3) an isolation device, and (4) a cultivation device. From the analyses of 16S rRNA gene sequences after cultivation at 65 MPa, two groups of the bacterial genera Shewanella and Moritella were identified. The authors have analyzed the microbial community structures by the terminal restriction fragment length polymorphism for the bacterial 16S rRNA gene and determined that the community is drastically changed at different pressure conditions of cultivation using the DEEPBATH system. Piezophiles are characterized by high levels of unsaturated fatty acids in their cell membrane layers, but long-chain polyunsaturated fatty acid (PUFA) like EPA and DHA are not necessarily required for high-pressure growth. The diversity of piezophilic bacteria is closely linked with the global deep-sea ocean circulation, but some of the closed oceans, like the Japan Sea, also contain piezophilic bacteria taxonomically similar to deep-sea microbes in the open oceans.

Shewanella species live widely in deep-sea and shallow-water areas, and thus grow piezophilically and piezosensitively. Piezophilic and psychrophilic Shewanella benthica cytochrome c 5 (SB cytc 5) was the most stable against guanidine hydrochloride (GdnHCl) and thermal denaturation, followed by less piezophilic but still psychrophilic Shewanella violacea cytochrome c 5 (SV cytc 5). These two were followed, as to stability level, by piezosensitive and mesophilic Shewanella amazonensis cytochrome c 5 (SA cytc 5), and piezosensitive and psychrophilic Shewanella livingstonensis cytochrome c 5 (SL cytc 5). The midpoint GdnHCl concentrations of SB cytc 5, SV cytc 5, SL cytc 5, and SA cytc 5 correlated with the optimal growth pressures of the species, the correlation coefficient value being 0.93. A similar trend was observed for thermal denaturation. Therefore, the stability of each cytochrome c 5 is related directly to its host's optimal growth pressure. Phylogenetic analysis indicated that Lys-37, Ala-41, and Leu-50 conserved in piezosensitive SL cytc 5 and SA cytc 5 are ancestors of the corresponding residues in piezophilic SB cytc 5 and SV cytc 5, Gln, Thr, and Lys, respectively, which might have been introduced during evolution on adaption to environmental pressure. The monomeric Shewanella cytochromes c 5 are suitable tools for examining protein stability with regard to the optimal growth pressures of the source species.

9 páginas.-- 3 figuras.-- referencias.-- El autor González Grau, Juan Miguel pertenece actualmente al Instituto de Recursos Naturales y Agrobiología de Sevilla, A new anaerobic, thermophilic, CO-utilizing marine bacterium, strain JMT, was isolated from a submarine hot vent in Okinawa Trough. Cells of strain JMT were non-motile thin straight rods, sometimes branching, with a cell wall of the Gram-positive type, surrounded with an S-layer. Chains of three to five cells were often observed. The isolate grew chemolithotrophically on CO, producing equimolar quantities of H2 and CO2 (according to the equation CO+H2O-->CO2+H2) and organotrophically on peptone, yeast extract, starch, cellobiose, glucose, galactose, fructose and pyruvate, producing H2, acetate and CO2. Growth was observed from 50 to 80 degrees C with an optimum at 70 degrees C. The optimum pH was 6.8-7.1. The optimum concentration of sea salts in the medium was 20.5-25.5 g l(-1). The generation time under optimal conditions was 7.1 h. The DNA G+C content was 33 mol %. Growth of isolate JMT was not inhibited by penicillin, but ampicillin, streptomycin, kanamycin and neomycin completely inhibited growth. The results of 16S rDNA sequence analysis revealed that strain JMT belongs to the Thermoanaerobacter phylogenetic group within the Bacillus-Clostridium subphylum of Gram-positive bacteria but represents a separate branch of this group. On the basis of morphological and physiological features and phylogenetic data, this isolate should be assigned to a new genus, for which the name Carboxydobrachium is proposed. The type species is Carboxydobrachium pacificum; the type strain is JMT (= DSM 12653T)., The authors are grateful to G. A. Zavarzin and A. V. Lebedinsky, Institute of Microbiology, Russian Academy of Sciences, for helpful discussions. This work was supported by the Russian Foundation for Basic Research, grants nos 96-04-49463 and 99-04-48360, the ‘Biodiversity’ program of the Russian Ministry of Science and Technology, a NATO CLG grant to T. S. and F. T. R. and by NSF LEXEN Program support to F. T. R. and J. M. G.

A glutamine synthetase gene ( glnA ) was isolated from a deep-sea piezophilic bacterium, Shewanella violacea strain DSS12. A 7.5-kb Sac I fragment containing the complete glnA gene was cloned and sequenced. The glnA gene was found to encode a protein consisting of 469 amino acid residues, showing 75.0% identity to the glutamine synthetase of Escherichia coli . Primer extension analyses revealed two transcription initiation sites in glnA and expression from each site was positively regulated by pressure. Putative promoters recognized by σ 70 and σ 54 were identified in the region upstream of glnA . An electrophoretic mobility shift assay demonstrated that S. violacea σ 54 specifically binds to the promoter region of glnA , suggesting that σ 54 may play an important role in pressure-regulated transcription in this piezophilic bacterium.

3-isopropylmalate dehydrogenase (IPMDH)-encoding leuB genes were obtained from the obligate piezophile Shewanella benthica DB21MT-2 and non-piezophile Shewanella oneidensis MR-1. The genes were expressed in Escherichia coli and the proteins were purified using His-tag. The estimated kinetic parameters of these enzymes indicated that IPMDH of S. benthica DB21MT-2 is more tolerant of high pressure than that of S. oneidensis MR-1. Thus such an adaptation is one of the mechanisms bacteria utilize for survival at high pressures.

Two genes for alternative sigma factors, sigma(E2) and sigma(E3), classified in the extracytoplasmic function sigma family for RNA polymerases, were identified in the deep-sea piezophilic bacterium Shewanella violacea DSS12. Amino acid alignments revealed that the domains for transcriptional functions were comparatively conserved compared with Escherichia coli sigma(E) in both proteins. Core-binding analysis suggested that both proteins function as sigma factors.

Potential regulatory elements were identified upstream of the pressure-regulated operon in the deep-sea barophilic bacterium Shewanella violacea strain DSS12 and binding of cellular proteins to this region was studied under different pressure conditions. Sequence analysis revealed the existence of a region, designated region A, showing similarity to the consensus sequence for σ54 binding, when the region upstream of the operon was compared with several consensus sequences for σ factors. A palindromic sequence AGTTAAAGATTAAACT, designated region B, was found further upstream beyond region A. In a region designated region C, just upstream of region B, a unique octamer motif AAGGTAAG, tandemly repeated 13 times, was found. By means of an electrophoretic mobility shift assay it was demonstrated that a σ54-like factor recognized region A while other unknown factors recognized the sequences in regions B and C. Different shift patterns of protein-DNA complexes were observed when extracts of cells cultured at 0.1 MPa and 50 MPa were incubated with 32P-labeled DNA probes corresponding to region B or C. These results indicate that barophilic strain DSS12 expresses different DNA-binding factors capable of recognizing these elements upstream of the pressure-regulated operon under different pressure conditions.

A sample of deep-sea sediment was obtained from the Japan Trench at a depth of 6292 m using a pressure-retaining sediment sampler. Microorganisms in the sediment sample were cultivated in marine broth 2216 at ambient pressure (65 MPa) without decompression, and at atmospheric pressure (0.1 MPa) as a control experiment. 16S ribosomal RNA genes (rDNA) were amplified by PCR from DNA extracted from the original sediment sample and the mixed cultures, and the nucleotide sequences were determined. The results of phylogenetic analysis based on 16S rDNA sequences indicated that microbial diversity in the original sediment samples showed a wide distribution of types in the domain Bacteria. Furthermore, in the mixed cultures incubated at 65 MPa without decompression, bacterial strains belonging to the Shewanella barophiles branch and the genus Moritella existed together at the beginning of cultivation, and Moritella strains became dominant towards the end of the cultivation period. Finally, in the mixed cultures incubated at atmospheric pressure, strains belonging to the genus Pseudomonas were dominant at all times. Analysis of fatty acids extracted from the cultures supported the phylogenetic results.

Several baro (piezo) -philic microorganisms have been isolated from a deep-sea high hydrostatic pressure environment in our laboratory. The results of taxonomic studies showed that all of the barophile isolates belonged to Proteobacteria gamma-subgroup, and four novel species were identified. The moderately barophilic bacterium, Shewanella violacea strain DSS 12 was one of them, and this strain was able to grow from atmospheric pressure (0. 1 MPa) to 70 MPa conditions in the same way. Molecular mechanisms of pressure-regulation on gene expression in S. violacea were analyzed, and we identified particular DNA binding proteins that might be essentially important for pressure regulation. Atmospheric pressure adapted Escherichia coli that belonged to the same gamma-subgroup of the isolated barophilic species was also studied and we could observe the positive and negative effects on pressure regulation. Finally, we observed that hyper-thermophilic archaea could grow well under higher pressure conditions at higher temperatures. These results indicated that pressure could affect microorganisms' survival in several ways in such an environment.

Deep-sea soft sediments from trench systems and depths in the northwestern Pacific Ocean ranging from less than 300 to 10,897 m in depth have been analyzed for three target genera of actinomycetes: Micromonospora, Rhodococcus, and Streptomyces. Only culturable strains, recovered at atmospheric pressure on selective isolation media, have been examined to date. Maximum recoveries of culturable bacteria were greater that 10(7)/ml wet g sediment, but actinomycetes comprised a small proportion of this population (usually less than 1%). The target actinomycetes were isolated at all depths except from the Mariana Trench sediments. Actinomycete colonies were defined initially on the basis of colony morphologies, and preliminary identification then was made by chemotaxonomic tests. Pyrolysis mass spectrometry (PyMS) of deep-sea mycolic acid-containing actinomycetes gave excellent correspondence with numerical (phenetic) taxonomic analyses and subsequently was adopted as a rapid procedure for assessing taxonomic diversity. PyMS analysis enabled several clusters of deep-sea rhodococci to be distinguished that are quite distinct from all type strains. 16S rRNA gene sequence analysis has revealed that several of these marine rhodococci have sequences that are very similar to certain terrestrial species of Rhodococcus and to Dietzia. There is evidence for the intrusion of terrestrial runoff into these deep trench systems, and the inconsistency of the phenotypic and molecular taxonomies may reflect recent speciatiion events in actinomycetes under the high-pressure conditions of the deep sea. The results of DNA-DNA pairing experiments point to the novelty of Rhodococcus strains recovered from hadal depths in the Izu Bonin Trench. Biotransformation studies of deep-sea bacteria have focused on nitrile compounds. Nitrile-metabolizing bacteria, closely related to rhodococci, have been isolated that grow well at low temperature, high salt concentrations, and high pressures, suggesting that they are of marine origin or have adapted to the deep-sea environment.

We investigated for the first time the respiratory chain system of a deep-sea barophilic bacterium, Shewanella sp. strain DB-172F. A membrane-bound ccb-type quinol oxidase, from cells grown at 60 MPa pressure, was purified to an electrophoretically homogeneous state. The purified enzyme complex consisted of four kinds of subunits with molecular masses of 98, 66, 18.5, and 15kDa, and it contained 0.96 mol of protoheme and 1.95mol of covalently bound heme c per mol of enzyme. Only protoheme in the enzyme reacted with CO and CN-, and the catalytic activity of the enzyme was 50% inhibited by 4 microM CN-. The isoelectric point of the native enzyme complex was determined to be 5.0. This enzyme was specifically induced only under conditions of elevated hydrostatic pressure, and high levels were expressed in cells grown at 60 MPa. The membranes isolated from cells grown at atmospheric pressure (0.1 MPa) exhibited high levels of both cytochrome c oxidase and N,N,N',N'-tetramethyl-p-phenylenediamine (TMPDH2)-oxidase activity. These results suggest the presence of two kinds of respiratory chains regulated in response to pressure in the deep-sea bacterium DB-172F.

From a deep-sea barophilic bacterium, Shewanella sp. strain DB-172F, a membrane-bound cytochrome c-551 and a cytoplasmic cytochrome c-552 were purified. The cytochrome c-551 contained 44.2 nmol of heme c mg protein−1 and cytochrome c-552 contained 31.3 nmol of heme c mg protein−1. The CO difference spectrum of cytochrome c-551 showed a peak at 413.7 nm and troughs at 423.2, 522 and 552 nm which indicated that this cytochrome combined with CO. Cytochrome c-551 was found to consist of two subunits with molecular masses of 29.1 kDa and 14.7 kDa, respectively, and each subunit contained one heme c molecule. Cytochrome c-552 also consisted of two subunits with molecular masses of 16.9 kDa and 14.7 kDa, respectively, and only one of these subunits contained heme c. Cytochrome c-551 was constitutively synthesized when the cells were grown at pressures of either 0.1 MPa or 60 MPa, whereas cytochrome c-552 was synthesized only at 0.1 MPa. These results together with the results of analysis of membrane-associated catalytic activities suggest that the respiratory system of DB-172F is regulated by pressure and may be intimately related to the baroadaptability mechanism of this deep-sea bacterium.

DNA regions corresponding to portions of two different pressure-regulated operons previously identified in two deep-sea barophilic bacteria were separately PCR amplified from a variety of deep-sea microorganisms and sequenced. With the two sets of primers employed, amplification was particularly successful from the more barophilic bacteria examined. 16S rRNA sequence analysis revealed that these bacteria are all phylogenetically related and belong in a sub-branch of the genus Shewanella containing only the deep-sea Shewanella barophilic bacteria. We define this sub-branch as the ‘Shewanella barophile branch’ containing at least two different species. Our results suggest that the DNA sequences of the pressureregulated operons can be regarded as marker sequences to identify the Shewanella barophilic strains. z 1998 Federation of European Microbiological Societies. Published by Elsevier Science B.V.

The denitrifying bacterium strain MT-1 was isolated from the mud of the Mariana Trench. The optimal temperature and pressure for growth of this bacterium were found to be 30 degrees C and 0.1 MPa, respectively. However, it showed greater tolerance to low temperature (4 degrees C) and high hydrostatic pressure (50 MPa) as compared with denitrifiers obtained from land. From the results, it can be said that this organism is adapted to the environment of the deep sea. Strain MT-1 was shown to belong to the genus Pseudomonas by analysis of its 16S rDNA. The cytochrome contents of the bacterium were similar to those of Ps. stutzeri in spectrophotometric studies.

Recently, so many genome analysis programs of the microorganisms have been investigating in the world, and some of them (5 strains) have finished and opened the sequencing data on computer net-work. From these results, we realyzed that the genome size of microorganisms and the quantity of regulatory functional genes and pseudo genes were corresponding. For example, 134 regulatory genes were identified in Synechocystis sp. PCC 6803 (3.6 Mb), however only 7 regulatory genes in Methanococcus Jannaschii (1.7 Mb). We believe that such difference of the genome size is corresponded to the quantity of the environmental stresses. Thus, this is very important to study the smaller genome organisms like hyperthermophilic archaea to realize the minimum genome for organisms. In my country, the genome project of new hyperthermophilic archaeon, Pyrococcus horikoshii, is in progress. P. horikoshii showed obligately barophilic growth profile at maximum high temperature (103°C), thus we may expect that the barophily of the deep-sea hyperthermophiles will be more understandable to consider about the origin of life and its evolution from the its genomic results.

The facultative piezophile Shewanella violacea DSS12 is known to have respiratory components that alter under the influence of hydrostatic pressure during growth, suggesting that its respiratory system is adapted to high pressure. We analyzed the expression of the genes encoding terminal oxidases and some respiratory components of DSS12 under various growth conditions. The expression of some of the genes during growth was regulated by both the O2 concentration and hydrostatic pressure. Additionally, the activities of cytochrome c oxidase and quinol oxidase of the membrane fraction of DSS12 grown under various conditions were measured under high pressure. The piezotolerance of cytochrome c oxidase activity was dependent on the O2 concentration during growth, while that of quinol oxidase was influenced by pressure during growth. The activity of quinol oxidase was more piezotolerant than that of cytochrome c oxidase under all growth conditions. Even in the membranes of the non-piezophile Shewanella amazonensis, quinol oxidase was more piezotolerant than cytochrome c oxidase, although both were highly piezosensitive as compared to the activities in DSS12. By phylogenetic analysis, piezophile-specific cytochrome c oxidase, which is also found in the genome of DSS12, was identified in piezophilic Shewanella and related genera. Our observations suggest that DSS12 constitutively expresses piezotolerant respiratory terminal oxidases, and that lower O2 concentrations and higher hydrostatic pressures induce higher piezotolerance in both types of terminal oxidases. Quinol oxidase might be the dominant terminal oxidase in high-pressure environments, while cytochrome c oxidase might also contribute. These features should contribute to adaptation of DSS12 in deep-sea environments.

Hydrostatic pressure analysis is an ideal approach for studying protein dynamics and hydration. The development of full ocean depth submersibles and high pressure biological techniques allows us to investigate enzymes from deep-sea organisms at the molecular level. The aim of this review was to overview the thermodynamic and functional characteristics of deep-sea enzymes as revealed by pressure axis analysis after giving a brief introduction to the thermodynamic principles underlying the effects of pressure on the structural stability and function of enzymes.

The formation of plaques by lambda phage in Escherichia coli was prevented by elevated hydrostatic pressure; phage plaques were not detected at 30 MPa. Furthermore, using promoter fragments derived from the malB operon, we showed that gene expression initiated from both promoters (malK-lamB and malEFG) was repressed by elevated hydrostatic pressure. Our findings suggest that high pressure affects gene expression directed by the malB regulatory interval, and this may cause a decrease in the quantities of lambda receptor protein, LamB.

Several barophilic and barotolerant bacteria were isolated from deep-sea mud samples of Suruga Bay (2485 m depth), the Ryukyu Trench (5110 m depth), and the Japan Trench (land-side 6356 m, and sea-side 6269 m depth, respectivelys. The barophilic bacteria, strains DB5501, DB6101, DB6705 and DB6906, were albe to grow better under high hydrostatic pressures than under atmospheric pressure (0.1 megapascals; MPa). The optimal growth pressures for the barophilic bacteria were approximately 50 MPa at 10°C. The barotolerant strains DSK1 and DSS12 were determined to be psychrophilic, and had optimal growth temperatures of 10°C and 8°C, respectively. The degree of barophily and barotolerance was shown to be very dependent on temperature. For example, at 4°C the barophilic strains were indistinguishable from barotolerant bacteria, whereas at 15°C the barotolerant strains behaved more like the barophilic strains. Based on sequence analysis of 16S ribosomal DNA, all of the strains included in this study belong to the gamma subgroup of the Proteobacteria. Phylogenetic relations between the isolated strains and the known gamma subgroup bacteria suggested that the isolated strains belong to a new sub-branch of this group.

The facultative piezophile Shewanella violacea DSS12 is known to alter its respiratory components under the influence of hydrostatic pressure during growth, suggesting that it has a respiratory system that functions in adaptation to high pressure. We investigated the pressure- and temperature-dependencies of the respiratory terminal oxidase activity of the membrane of S. violacea relative to non-piezophilic Shewanella species. We observed that the activity in the membrane of S. violacea was more resistant to high pressure than those of non-piezophilic Shewanella even though DSS12 was cultured under atmospheric pressure. On the other hand, the temperature dependency of this activity was almost the same for all of the tested strain regardless of optimal growth temperature. Both high pressure and low temperature are expected to lower protein flexibility, causing a decrease in enzyme activity, but the results of this study suggest that the mechanism maintaining enzyme activity under high hydrostatic pressure is different from that at low temperature. Additionally, the responses of the activity to the pressure- and temperature-changes were independent of membrane lipid composition. Therefore, the piezotolerance of the respiratory terminal oxidases of S. violacea is perhaps dependent on the properties of the protein itself and not on the lipid composition of the membrane. Our observations suggest that S. violacea constitutively express piezotolerant respiratory terminal oxidases that serve adaptation to the deep-sea environment.

Microorganisms are globally dispersed and are able to proliferate in any habitat that supports their lifestyles, which, however, has not yet been explored in any specific microbial taxon. The social myxobacteria are considered typical soil bacteria because they have been identified in various terrestrial samples, a few in coastal areas, but none in other oceanic environments. To explore the prevalence of marine myxobacteria and to investigate their phylogenetic relationships with their terrestrial counterparts, we established myxobacteria-enriched libraries of 16S rRNA gene sequences from four deep-sea sediments collected at depths from 853 to 4675 m and a hydrothermal vent at a depth of 204 m. In all, 68 different myxobacteria-related sequences were identified from randomly sequenced clones of the libraries of different samples. These myxobacterial sequences were diverse but phylogenetically similar at different locations and depths. However, they were separated from terrestrial myxobacteria at high levels of classification. This discovery indicates that the marine myxobacteria are phylogeographically separated from their terrestrial relatives, likely because of geographic separation and environment selection.

The deep-sea denitrifier Pseudomonas sp. strain MT-1 has two distinct gene clusters encoding dissimilatory nitrate reductases, periplasmic nitrate reductase (Nap) and membrane-bound nitrate reductase (Nar). In order to investigate the physiological roles of these enzymes, we determined the nitrate reductase activity of the soluble and membrane fractions from MT-1 and the type strain of Pseudomonas stutzeri (closely related with MT-1) grown under various conditions. In MT-1, the activities of both fractions were highest when the cells were grown anaerobically in the presence of nitrate under atmospheric pressure. However, the activity of the soluble fraction decreased when the cells were grown under high pressure, whereas that of membrane fraction remained constant. Further, the activity of the soluble fraction decreased when the enzyme reaction was performed at low temperature, although that of membrane fraction was not similarly affected. Additionally, the results of RT-PCR showed that expression of the nar genes was strongly induced under high pressure. In contrast, P. stutzeri(T) showed no such response following a shift in growth pressure. These results suggest that MT-1 possesses a special mechanism for adaptation to the low-temperature and high-pressure environments of the deep sea, and that Nar is the main dissimilatory nitrate reductase in MT-1 in such environments.

The extracellular glucosyltransferases (GTFs) of Streptococcus mutans are not secreted into the periplasmic space of Escherichia coli when the corresponding gtf genes are isolated in the latter organism. The utilization of both deletion analysis and gtfB: phoA fusions indicate that the signal sequences of the GTFs are functional in E. coli. However, these results further suggest that amino acid sequences present in the carboxyl terminus of the GTFs inhibit secretion through the cytoplasmic membrane in E. coli.