Desulfovibrio portus sp. nov., a novel sulfate-reducing bacterium in the class Deltaproteobacteria isolated from an estuarine sediment

Pseudodesulfovibrio thermohalotolerans sp. nov., a novel obligately anaerobic, halotolerant, thermotolerant, and sulfate-reducing bacterium isolated from a western offshore hydrocarbon reservoir in India

OBJECTIVE

Characterization and documentation of strain MCM B-1480T, a novel sulfate-reducing bacterium isolated from produced water of India's western offshore hydrocarbon reservoir.

METHOD

Strain MCM B-1480T was unequivocally identified using a polyphasic approach routinely followed in bacterial systematics. The morphological and biochemical characterization of strain MCM B-1480T was carried out using standard microbiological techniques.

RESULTS

MCM B-1480T was a Gram-stain-negative, motile, non-spore-forming, curved-rod-shaped bacterium. MCM B-1480T could grow at temperatures between 20 and 60 °C (optimum 37 °C), pH 6-8 (optimum 7), and required 1-6% NaCl (optimum 3%) for growth. Strain MCM B-1480T was reducing sulfate to produce hydrogen sulfide during growth. This strain used lactate and pyruvate as prominent electron donors, whereas sulfate, sulfite, thiosulfate, and nitrate served as electron acceptors. MCM B-1480T shared maximum 16S rRNA gene sequence homology of 98.65% with the members of the genus Pseudodesulfovibrio. The G + C content of the 3.87 Mb MCM B-1480T genome was 60.39%. Digital DDH (27.7%) and average nucleotide identity (ANI 84%) with the closest phylogenetic affiliate (less than 70% and 95%, respectively) reaffirmed its distinctiveness. The major cellular fatty acids components, namely iso-C15:0, anteiso-C15:0, C16:0, and anteiso-C17:0, differentiated strain MCM B-1480T from other species of Pseudodesulfovibrio. Genome annotation revealed the presence of genes encoding dissimilatory sulfate reduction and nitrate reduction in strain MCM B-1480T.

CONCLUSION

The polyphasic studies, including SSU rRNA gene sequencing, average nucleotide identity, Digital DNA-DNA hybridization, cell wall fatty acids analysis, etc., identified strain MCM B-1480T as a novel taxon and Pseudodesulfovibrio thermohalotolerans sp. nov. was proposed (= JCM 39269T = MCC 4711T).

Pseudodesulfovibrio nedwellii sp. nov., a mesophilic sulphate-reducing bacterium isolated from a xenic culture of an anaerobic heterolobosean protist

A novel sulphate-reducing bacterium, strain SYK^T, was isolated from a xenic culture of an anaerobic protist obtained from a sulphidogenic sediment of the saline Lake Hiruga in Fukui, Japan. The results of phylogenetic analysis based on 16S rRNA gene sequences indicated that SYK^T clustered with the members of the genus Pseudodesulfovibrio. The closest relative of strain SYK^T was Pseudodesulfovibrio sediminis SF6^T, with 16S rRNA gene sequence identity of 97.43 %. Digital DNA-DNA hybridisation and average nucleotide identity values between SYK^T and species of the genus Pseudodesulfovibrio fell below the respective thresholds for species delineation, indicating that SYK^T represents a novel species of the genus Pseudodesulfovibrio. Cells measured 1.7-3.7×0.2-0.5 µm in size and were Gram-stain-negative, obligately anaerobic, motile by means of a single polar flagellum and had a curved rod or sigmoid shape. Cell growth was observed under saline conditions from pH 6.0 to 9.5 (optimum pH 8.0-9.0) and at a temperature of 10-30 °C (optimum 25 °C). SYK^T used lactate, pyruvate, fumarate, formate and H₂ as electron donors. It used sulphate, sulphite, thiosulphate and sulphur as terminal electron acceptors. Pyruvate and fumarate were fermented. Major cellular fatty acids were anteiso-C_15 : 0, C_16 : 0, anteiso-C_17 : 1ω9c, summed feature 3 (C_16 : 1ω6c and/or C_16 : 1ω7c) and summed feature 8 (C_18 : 1ω7c and/or C_18 : 1ω6c). The DNA G+C content of SYK^T was 49.4 mol%. On the basis of the the genetic and phenotypic features, SYK^T was determined to represent a novel species of the genus Pseudodesulfovibrio for which the name Pseudodesulfovibrio nedwellii sp. nov. is proposed with type strain SYK^T (=DSM 114958^T=JCM 35746^T).

Genome Sequence of the Sulfate-Reducing Bacterium Pseudodesulfovibrio portus JCM 14722 T

Pseudodesulfovibrio portus JCM 14722 T is a strictly anaerobic, mesophilic sulfate-reducing bacterium isolated from estuarine sediments in Japan. Its draft genome sequence comprises 1 circular chromosome (3,403,863 bp), harboring 3,182 predicted protein- and 60 tRNA-encoding genes, as well as 2 rRNA operons.

Pseudodesulfovibrio sediminis sp. nov., a mesophilic and neutrophilic sulfate-reducing bacterium isolated from sediment of a brackish lake

A novel mesophilic and neutrophilic sulfate-reducing bacterium, strain SF6^T, was isolated from sediment of a brackish lake in Japan. Cells of strain SF6^T were motile and rod-shaped with length of 1.2-2.5 μm and width of 0.6-0.9 μm. Growth was observed at 10-37 °C with an optimum growth temperature of 28 °C. The pH range for growth was 5.8-8.2 with an optimum pH of 7.0. The most predominant fatty acid was anteiso-C_15:0. Under sulfate-reducing conditions, strain SF6^T utilized lactate, ethanol and glucose as growth substrate. Chemolithoautotrophic growth on H₂ was not observed, although H₂ was used as electron donor. Fermentative growth occurred on pyruvate. As electron acceptor, sulfate, sulfite, thiosulfate and nitrate supported heterotrophic growth of the strain. The complete genome of strain SF6^T is composed of a circular chromosome with length of 3.8 Mbp and G+C content of 54 mol%. Analyses of the 16S rRNA gene and whole genome sequence indicated that strain SF6^T belongs to the genus Pseudodesulfovibrio but distinct form all existing species in the genus. On the basis of its genomic and phenotypic properties, strain SF6^T (= DSM111931^T = NBRC 114895^T) is proposed as the type strain of a new species, with name of Pseudodesulfovibrio sediminis sp. nov.

Effects of dietary bamboo ( Phyllostachys pubescens Mazel) culm powder on blood properties and intestinal environment of rabbits

This study investigated the effects of bamboo powder as an alternative feed for rabbits. The normal hay diet of rabbits was replaced with bamboo culm powder (10% and 20%) and fed to the rabbits until they were 90 days old. The blood samples were collected when the rabbits were 46, 66, and 90 days old to assess the effects of bamboo powder on blood parameters. The organs and intestinal contents were harvested at the age of 90 days, and the functions and morphologies of different organs were evaluated. The concentration of short-chain fatty acids (SCFAs) and the composition of microbiota in the cecum were measured. Substituting bamboo powder did not affect the growth, hematology profile, intestinal morphologies, and cecum SCFA concentration in rabbits. In contrast, it significantly altered the cecum microbiota composition, particularly the abundance of Ruminococcus and Bacteroides related to fiber degradation and Tyzzerella spp., associated with large intestine inflammation. These findings suggest that the substitution of hay with bamboo powder in rabbit diets does not negatively affect the overall health of rabbits and could be considered an alternative feed for rabbits; nevertheless, the protein and lipid deficiency in the bamboo powder should be taken into account.

Pseudodesulfovibrio alkaliphilus, sp. nov., an alkaliphilic sulfate-reducing bacterium isolated from a terrestrial mud volcano

The diversity of anaerobic microorganisms in terrestrial mud volcanoes is largely unexplored. Here we report the isolation of a novel sulfate-reducing alkaliphilic bacterium (strain F-1^T) from a terrestrial mud volcano located at the Taman peninsula, Russia. Cells of strain F-1^T were Gram-negative motile vibrios with a single polar flagellum; 2.0-4.0 µm in length and 0.5 µm in diameter. The temperature range for growth was 6-37 °C, with an optimum at 24 °C. The pH range for growth was 7.0-10.5, with an optimum at pH 9.5. Strain F-1^T utilized lactate, pyruvate, and molecular hydrogen as electron donors and sulfate, sulfite, thiosulfate, elemental sulfur, fumarate or arsenate as electron acceptors. In the presence of sulfate, the end products of lactate oxidation were acetate, H₂S and CO_2. Lactate and pyruvate could also be fermented. The major product of lactate fermentation was acetate. The main cellular fatty acids were anteiso-C_15:0, C_16:0, C_18:0, and iso-C_17:1ω8. Phylogenetic analysis revealed that strain F-1^T was most closely related to Pseudodesulfovibrio aespoeensis (98.05% similarity). The total size of the genome of the novel isolate was 3.23 Mb and the genomic DNA G + C content was 61.93 mol%. The genome contained all genes essential for dissimilatory sulfate reduction. We propose to assign strain F-1^T to the genus Pseudodesulfovibrio, as a new species, Pseudodesulfovibrio alkaliphilus sp. nov. The type strain is F-1^T (= KCTC 15918^T = VKM B-3405^T).

Pseudodesulfovibrio mercurii sp. nov., a mercury-methylating bacterium isolated from sediment

The sulfate-reducing, mercury-methylating strain ND132^T was isolated from the brackish anaerobic bottom sediments of Chesapeake Bay, USA. Capable of high levels of mercury (Hg) methylation, ND132^T has been widely used as a model strain to study the process and to determine the genetic basis of Hg methylation. Originally called Desulfovibrio desulfuricans ND132^T on the basis of an early partial 16S rRNA sequence, the strain has never been formally described. Phylogenetic and physiological traits place this strain within the genus Pseudodesulfovibrio, in the recently reclassified phylum Desulfobacterota (formerly Deltaproteobacteria). ND132^T is most closely related to Pseudodesulfovibrio hydrargyri BerOc1^T and Pseudodesulfovibrio indicus J2^T. Analysis of average nucleotide identity (ANI) of whole-genome sequences showed roughly 88 % ANI between P. hydrargyri BerOc1^T and ND132^T, and 84 % similarity between ND132^T and P. indicus J2^T. These cut-off scores <95 %, along with a multi-gene phylogenetic analysis of members of the family Desulfovibrionacea, and differences in physiology indicate that all three strains represent separate species. The Gram-stain-negative cells are vibrio-shaped, motile and not sporulated. ND132^T is a salt-tolerant mesophile with optimal growth in the laboratory at 32 °C, 2 % salinity, and pH 7.8. The DNA G+C content of the genomic DNA is 65.2 %. It is an incomplete oxidizer of short chain fatty acids, using lactate, pyruvate and fumarate with sulfate or sulfite as the terminal electron acceptors. ND132^T can respire fumarate using pyruvate as an electron donor. The major fatty acids are iso-C_15 : 0, anteiso-C_15 : 0, iso-C_17 : 0, iso-C_17 : 1ω9c and anteiso-C_17 : 0. We propose the classification of strain ND132^T (DSM 110689, ATCC TSD-224) as the type strain Pseudodesulfovibrio mercurii sp. nov.

Pseudodesulfovibrio hydrargyri sp. nov., a mercury-methylating bacterium isolated from a brackish sediment

The strain BerOc1^T was isolated from brackish sediments contaminated with hydrocarbons and heavy metals. This strain has been used as a model strain of sulfate-reducer to study the biomethylation of mercury. The cells are vibrio-shaped, motile and not sporulated. Phylogeny and physiological traits placed this strain within the genus Pseudodesulfovibrio. Optimal growth was obtained at 30 °C, 1.5 % NaCl and pH 6.0-7.4. The estimated G+C content of the genomic DNA was 62.6 mol%. BerOc1^T used lactate, pyruvate, fumarate, ethanol and hydrogen. Terminal electron acceptors used were sulfate, sulfite, thiosulfate and DMSO. Only pyruvate could be used without a terminal electron acceptor. The major fatty acids were C18 : 0, anteiso-C15 : 0, C16 : 0 and C18 : 1ω7. The name Pseudodesulfovibrio hydrargyri sp. nov. is proposed for the type strain BerOc1^T (DSM 10384^T=JCM 31820^T).

Reprint of: Contribution of enrichments and resampling for sulfate reducing bacteria diversity assessment by high-throughput cultivation

The development of new high-throughput cultivation methods aims to increase the isolation efficiency as compared to standard techniques that often require enrichment procedures to compensate the low microbial recovery. In the current study, estuarine sulfate-reducing bacteria were isolated using an anaerobic isolation procedure in 384-well microplates. Ninety-nine strains were recovered from initial sediments. Isolates were identified according to their partial 16S rRNA sequences and clustered into 13 phylotypes. Besides, the increase in species richness obtained through enrichments or resampling was investigated. Forty-four enrichment procedures were conducted and shifts in sulfate-reducing bacterial communities were investigated through dsrAB gene fingerprinting. Despite efforts in conducting numerous enrichment conditions only few of them were statistically different from initial sample. The cultural diversity obtained from 3 of the most divergent enrichments, as well as from resampled sediments equally contributed to raise the sulfate-reducing diversity up to 22 phylotypes. Enrichments (selection of metabolism) or resampling (transient populations and micro-heterogeneity) may still be helpful to assess new microbial phylotypes. Nevertheless, all the newly cultivated strains were all representatives of minor Operational Taxonomic Units and could eventually be recovered by maintaining high-throughput isolation effort from the initial sediments.

Pseudodesulfovibrio indicus gen. nov., sp. nov., a piezophilic sulfate-reducing bacterium from the Indian Ocean and reclassification of four species of the genus Desulfovibrio

A novel sulfate-reducing bacterium, strain J2T, was isolated from a serpentinized peridotite sample from the Indian Ocean. Phylogenetic analysis based on 16S rRNA gene sequences showed that strain J2T clustered with the genus Desulfovibrio within the family Desulfovibrionaceae, but it showed low similarity (87.95 %) to the type species Desulfovibrio desulfuricans DSM 642T. It was most closely related to Desulfovibrio portus MSL79T (96.96 %), followed by Desulfovibrio aespoeensis Aspo-2T (96.11 %), Desulfovibrio piezophilus C1TLV30T (96.04 %) and Desulfovibrio profundus DSM 11384T (95.17 %). Other available sequences shared less than 93.33 % 16S rRNA gene sequence similarity. Cells were Gram-staining-negative, anaerobic, motile vibrios (2-6×0.4-0.6 µm). Growth was observed at salinities ranging from 0.2 to 6 % (optimum 2.5 %), from pH 5 to 8 (optimum pH 6.5-7) and at temperatures between 9 and 40 °C (optimum 30-35 °C). J2T was piezophilic, growing optimally at 10 MPa (range 0-30 MPa). J2T used lactate, malate, pyruvate, formate and hydrogen as energy sources. Sulfate, thiosulfate, sulfite, fumarate and nitrate were used as terminal electron acceptors. Lactate and pyruvate were fermented. The main fatty acids were iso-C15 : 0, anteiso-C15 : 0, summed feature 9 (iso-C17 : 1ω9c and/or C16 : 0 10-methyl) and iso-C17 : 0. The DNA G+C content of strain J2T was 63.5 mol%. The combined genotypic and phenotypic data show that strain J2T represents a novel species of a novel genus in the family Desulfovibrionaceae, for which the name Pseudodesulfovibrio indicus gen. nov., sp. nov. is proposed, with the type strain J2T (=MCCC 1A01867T = DSM 101483T). We also propose the reclassification of D. piezophilus as Pseudodesulfovibrio piezophilus comb. nov., D. profundus as Pseudodesulfovibrio profundus comb. nov., D. portus as Pseudodesulfovibrio portus comb. nov. and D. aespoeensis as Pseudodesulfovibrio aespoeensis comb. nov.

Contribution of enrichments and resampling for sulfate reducing bacteria diversity assessment by high-throughput cultivation

The development of new high-throughput cultivation methods aims to increase the isolation efficiency as compared to standard techniques that often require enrichment procedures to compensate the low microbial recovery. In the current study, estuarine sulfate-reducing bacteria were isolated using an anaerobic isolation procedure in 384-well microplates. Ninety-nine strains were recovered from initial sediments. Isolates were identified according to their partial 16S rRNA sequences and clustered into 13 phylotypes. Besides, the increase in species richness obtained through enrichments or resampling was investigated. Forty-four enrichment procedures were conducted and shifts in sulfate-reducing bacterial communities were investigated through dsrAB gene fingerprinting. Despite efforts in conducting numerous enrichment conditions only few of them were statistically different from initial sample. The cultural diversity obtained from 3 of the most divergent enrichments, as well as from resampled sediments equally contributed to raise the sulfate-reducing diversity up to 22 phylotypes. Enrichments (selection of metabolism) or resampling (transient populations and micro-heterogeneity) may still be helpful to assess new microbial phylotypes. Nevertheless, all the newly cultivated strains were all representatives of minor Operational Taxonomic Units and could eventually be recovered by maintaining high-throughput isolation effort from the initial sediments.

Autotrophy as a predominant mode of carbon fixation in anaerobic methane-oxidizing microbial communities

The methane-rich, hydrothermally heated sediments of the Guaymas Basin are inhabited by thermophilic microorganisms, including anaerobic methane-oxidizing archaea (mainly ANME-1) and sulfate-reducing bacteria (e.g., HotSeep-1 cluster). We studied the microbial carbon flow in ANME-1/ HotSeep-1 enrichments in stable-isotope-probing experiments with and without methane. The relative incorporation of (13)C from either dissolved inorganic carbon or methane into lipids revealed that methane-oxidizing archaea assimilated primarily inorganic carbon. This assimilation is strongly accelerated in the presence of methane. Experiments with simultaneous amendments of both (13)C-labeled dissolved inorganic carbon and deuterated water provided further insights into production rates of individual lipids derived from members of the methane-oxidizing community as well as their carbon sources used for lipid biosynthesis. In the presence of methane, all prominent lipids carried a dual isotopic signal indicative of their origin from primarily autotrophic microbes. In the absence of methane, archaeal lipid production ceased and bacterial lipid production dropped by 90%; the lipids produced by the residual fraction of the metabolically active bacterial community predominantly carried a heterotrophic signal. Collectively our results strongly suggest that the studied ANME-1 archaea oxidize methane but assimilate inorganic carbon and should thus be classified as methane-oxidizing chemoorganoautotrophs.

List of new names and new combinations previously effectively, but not validly, published

The purpose of this announcement is to effect the valid publication of the following effectively published new names and new combinations under the procedure described in the Bacteriological Code (1990 Revision). Authors and other individuals wishing to have new names and/or combinations included in future lists should send three copies of the pertinent reprint or photocopies thereof, or an electronic copy of the published paper, to the IJSEM Editorial Office for confirmation that all of the other requirements for valid publication have been met. It is also a requirement of IJSEM and the ICSP that authors of new species, new subspecies and new combinations provide evidence that types are deposited in two recognized culture collections in two different countries. It should be noted that the date of valid publication of these new names and combinations is the date of publication of this list, not the date of the original publication of the names and combinations. The authors of the new names and combinations are as given below, and these authors’ names will be included in the author index of the present issue. Inclusion of a name on these lists validates the publication of the name and thereby makes it available in bacteriological nomenclature. The inclusion of a name on this list is not to be construed as taxonomic acceptance of the taxon to which the name is applied. Indeed, some of these names may, in time, be shown to be synonyms, or the organisms may be transferred to another genus, thus necessitating the creation of a new combination.