Distribution of marine viruses and their potential hosts in Prydz Bay and adjacent Southern Ocean,Antarctic

Viruses play a key role in all marine ecosystems, and yet little is known of their distribution in Antarctic waters, especially in bathypelagic waters (>1000 m). In this study, the abundance and distribution of viruses and their potential hosts from the surface to the bottom of Prydz Bay, Antarctic, was investigated using flow cytometry. Viruses and autotrophs were abundant in nearshore and continental shelf waters, while heterotrophic bacteria and picoeukaryotes were abundant in offshore waters. Virus and bacteria abundances generally decreased with increasing depth but increased slightly just above the seafloor. Within the water column, maximum virus numbers coincided with the maximum values of chlorophyll a (when greater than 0.1 μg l^?1), in the surface and subsurface (25 m). In the open ocean, however, virus abundance usually correlated with bacterial abundance at greater depths (50, 300 and 500 m) where the surface chlorophyll a concentration was lower than 0.1 μg l^?1. Viral abundance was correlated with the host cell abundance, and this was different in different pelagic zones (bacteria and autotrophs (i.e., chlorophyll a concentration) in the epipelagic waters, picoeukaryotes and bacteria in mesopelagic waters and bacteria in bathypelagic waters). Principle component analysis and Pearson correlation analysis indicated that there was a close relationship between virus abundance and chlorophyll a, bacteria and nutrients (NO₂ + NO₃, phosphate and silicate), and picoeukaryote abundance was mainly correlated with water depth and salinity.     

Diversity and abundance of the arsenite oxidase gene aioA in geothermal areas of Tengchong, Yunnan, China

A total of 12 samples were collected from the Tengchong geothermal areas of Yunnan, China, with the goal to assess the arsenite (AsIII) oxidation potential of the extant microbial communities as inferred by the abundance and diversity of the AsIII oxidase large subunit gene aioA relative to geochemical context. Arsenic concentrations were higher (on average 251.68 μg/L) in neutral or alkaline springs than in acidic springs (on average 30.88 μg/L). aioA abundance ranged from 1.63 × 10¹ to 7.08 × 10³ per ng of DNA and positively correlated with sulfide and the ratios of arsenate (AsV):total dissolved arsenic (As_Tot). Based on qPCR estimates of bacterial and archaeal 16S rRNA gene abundance, aioA-harboring organisms comprised as much as ~15 % of the total community. Phylogenetically, the major aioA sequences (270 total) in the acidic hot springs (pH 3.3–4.4) were affiliated with Aquificales and Rhizobiales, while those in neutral or alkaline springs (pH 6.6–9.1) were inferred to be primarily bacteria related to Thermales and Burkholderiales. Interestingly, aioA abundance at one site greatly exceeded bacterial 16S rRNA gene abundance, suggesting these aioA genes were archaeal even though phylogenetically these aioA sequences were most similar to the Aquificales. In summary, this study described novel aioA sequences in geothermal features geographically far removed from those in the heavily studied Yellowstone geothermal complex.     

Halomonas cibimaris sp. nov., isolated from jeotgal, a traditional Korean fermented seafood

Two moderately halophilic, facultatively aerobic, motile bacteria with flagella, designated strains 10-C-3^T and 30-C-3, were isolated from jeotgal, a traditional Korean fermented seafood. Cells of the strains were observed to be ovoid-rods showing catalase- and oxidase-positive reactions and production of creamy-pink pigments. Growth of strain 10-C-3^T was observed at 15–35 °C (optimum, 25–30 °C), at pH 5.5–9.0 (optimum, pH 7.0–7.5), and in the presence of 3–15 % (w/v) salts (optimum: 5–10 %). The two strains were found to contain C_18:1 ω7c, C_16:0, summed feature 3 (as defined by the MIDI system, comprising C_16:1 ω7c and/or C_16:1 ω6c), and C_12:0 3-OH as the major cellular fatty acids. The G+C contents of the genomic DNA of strains 10-C-3^T and 30-C-3 were determined to be 63.2 and 63.1 mol%, respectively and the respiratory quinone detected was ubiquinone 9 (Q-9) only. Phylogenetic analyses based on 16S rRNA gene sequences indicated that strains 10-C-3^Tand 30-C-3 formed a distinct phyletic lineage within the genus Halomonas and are most closely related to Halomonas fontilapidosi 5CR^T with 95.2 % of 16S rRNA sequence similarity. Strains 10-C-3^Tand 30-C-3 shared 99.2 % of 16S rRNA gene sequence similarity and their DNA–DNA relatedness value was 96.6 ± 0.9 %. On the basis of phenotypic, chemotaxonomic and molecular features, strains 10-C-3^Tand 30-C-3 represent a novel species of the genus Halomonas, for which the name Halomonas cibimaris sp. nov. is proposed. The type strain is 10-C-3^T (= KACC 14932^T = JCM 16914^T).     

Coralslurrinella hongkonensis gen. nov., sp. nov., a novel bacterium in the family Psychromonadaceae, isolated from the coral Platygyra carnosus

A novel bacterial strain, JLT2006^T, was isolated from the scleractinian coral Platygyra carnosus, located in Hong Kong, China. Cells of this strain were Gram-negative, rod-shaped or oval-shaped and motile by the means of polar flagella. They formed faint-yellow, round colonies on marine agar medium. Phylogenetic analyses based on the 16S rRNA gene sequence indicated that the strain JLT2006^T belonged to the class Gammaproteobacteria and was most closely related to Alteromonas-like bacteria of the genera Psychromonas, Pseudoalteromonas, Moritella, Shewanella and Ferrimonas, with less than 93 % sequence similarity. The predominant fatty acids were identified as C18:1ω7c/C18:1ω6c (23.0 %), C16:1ω7c/C16:1ω6c (18.2 %) and C16:0 (16.4 %). The quinone was menaquinone-7 (100 %). The polar lipids were determined to be phosphatidylglycerol, phosphatidylethanolamine, phospholipid, glycolipid and lipid. The genomic DNA G+C content was 40.3 mol%. Based on the 16S rRNA gene sequence as well as the physiological and biochemical features that separate the strain JLT2006^T from other recognized bacteria, a novel species of a new genus with the name Coralslurrinella hongkonensis gen. nov., sp. nov. is proposed. The type strain is JLT2006^T (=JCM 18796^T = CGMCC 1.10992^T).     

Alteromonas australica sp. nov., isolated from the Tasman Sea

A non-pigmented, motile, Gram-negative bacterium designated H 17^T was isolated from a seawater sample collected in Port Phillip Bay (the Tasman Sea, Pacific Ocean). The new organism displayed optimal growth between 4 and 37 °C, was found to be neutrophilic and slightly halophilic, tolerating salt water environments up to 10 % NaCl. Strain H 17^T was found to be able to degrade starch and Tween 80 but unable to degrade gelatin or agar. Phosphatidylglycerol (27.7 %) and phosphatidylethanolamine (72.3 %) were found to be the only associated phospholipids. The major fatty acids identified are typical for the genus Alteromonas and include C_16:0, C_16:1ω7, C_17:1ω8 and C_18:1ω7. The G+C content of the DNA was found to be 43.4 mol%. A phylogenetic study, based on the 16S rRNA gene sequence analysis and Multilocus Phylogenetic Analysis, clearly indicated that strain H 17^T belongs to the genus Alteromonas. The DNA?DNA relatedness between strain H 17^T and the validly named Alteromonas species was between 30.7 and 46.4 mol%. Based on these results, a new species, Alteromonas australica, is proposed. The type strain is H 17^T (= KMM 6016^T = CIP 109921^T).     

Microbiological and biogeochemical processes in a pockmark of the Gdansk depression,Baltic Sea

Comprehensive microbiological and biogeochemical investigation of a pockmark within one of the sites of gas-saturated sediments in the Gdansk depression, Baltic Sea was carried out during the 87th voyage of the Professor Shtokman research vessel. Methane content in the near-bottom water and in the underlying sediments indicates stable methane flow from the sediment into the water. In the 10-m water layer above the pockmark, apart from methane anomalies, elevated numbers of microorganisms and enhanced rates of dark CO₂ fixation (up to 1.15 µmol C/(l day)) and methane oxidation (up to 2.14 nmol CH₄/(l day)) were revealed. Lightened isotopic composition of suspended organic matter also indicates high activity of the near-bottom microbial community. Compared to the background stations, methane content in pockmark sediments increased sharply from the surface to 40–60 ml/dm³ in the 20–30 cm horizon. High rates of bacterial sulfate reduction (SR) were detected throughout the core (0–40 cm); the maximum of 74 µmol S/(dm³ day) was located in subsurface horizons (15–20 cm). The highest rates of anaerobic methane oxidation (AMO), up to 80 µmol/dm³ day), were detected in the same horizon. Good coincidence of the AMO and SR profiles with stoichiometry close to 1: 1 is evidence in favor of a close relation between these processes performed by a consortium of methanotrophic archaea and sulfate-reducing bacteria. Methane isotopic composition in subsurface sediments of the pockmark (from ?53.0 to ?56.5‰) does not rule out the presence of methane other than the biogenic methane from the deep horizons of the sedimentary cover.     

Paenibacillus brassicae sp. nov., isolated from cabbage rhizosphere in Beijing, China

A novel Gram-positive, rod-shaped, motile, spore-forming, nitrogen-fixing bacterium, designated strain 112^T, was isolated from cabbage rhizosphere in Beijing, China. The strain was found to grow at 10–40 °C and pH 4–11, with an optimum of 30 °C and pH 7.0, respectively. Phylogenetic analysis based on a fragment of the full-length 16S rRNA gene sequence revealed that strain 112^T is a member of the genus Paenibacillus. High levels of 16S rRNA gene similarities were found between strain 112^T, Paenibacillus sabinae DSM 17841^T (97.82 %) and Paenibacillus forsythiae DSM 17842^T (97.22 %). However, the DNA–DNA hybridization values between strain 112^T and the type strains of these two species were 10.36 and 6.28 %, respectively. The predominant menaquinone was found to be menaquinone 7 (MK-7). The major fatty acids were determined to be anteiso-C_15:0 and C_16:0. The major polar lipids were found to be diphosphatidylglycerol, phosphatidylethanolamine, phosphatidylglycerol and unknown aminophospholipids. The cell wall peptidoglycan was found to contain meso-diaminopimelic acid. The DNA G+C content was determined to be 55.4 mol%. On the basis of its phenotypic characteristics, 16S rRNA gene sequence analysis and the value of DNA–DNA hybridization, strain 112^T is considered to represent a novel species of the genus Paenibacillus, for which the name Paenibacillus brassicae sp. nov. is proposed. The type strain is 112^T (= ACCC 01125^T = DSM 24983^T).     

Diversity and Bioprospective Potential (Cold-Active Enzymes) of Cultivable Marine Bacteria from the Subarctic Glacial Fjord, Kongsfjorden

The diversity and abundance of culturable bacteria in Kongsfjorden water (15 stations) and sediments (12 stations) were studied. Viable numbers ranged between 10⁵–10⁶ CFU l^?1 in water and 10²–10⁴ CFU g^?1 in the sediments. A total of 291 and 43 bacterial isolates were retrieved from the water (KJF) and sediments (FS), respectively. Based on 16S rRNA gene sequence similarities, the KJF and FS isolates were grouped into 49 and 23 phylotypes, respectively. The KJF and FS phylotypes represented three phyla namely, Actinobacteria, Bacteroidetes, and Proteobacteria. At the genus level, Flavobacterium and Shewanella and at the species level, Pseudoaltermonas arctica and Colwellia psychrerythraea were dominant in the water and sediments, respectively. Most phylotypes were psychrotolerant with upper growth temperature limit of 25–37 °C and tolerated 0.3–2.5 M NaCl and pH values of 5.0–11.0. Majority of the phylotypes produced one or more of the extracellular hydrolytic enzymes amylase, lipase, caseinase, urease, gelatinase, and DNase at 4 and 18 °C, while none were chitinolytic. Few of the FS phylotypes exhibited extracellular activity only at 4 or 18 °C. Nine FS and 21 KJF isolates were pigmented. The predominant cellular fatty acids were unsaturated, branched, and modified fatty acids, which are unique to cold-adapted bacteria.     

Lihuaxuella thermophila gen. nov., sp. nov., isolated from a geothermal soil sample in Tengchong, Yunnan, south-west China

A novel filamentous bacterium, designated YIM 77831^T, was isolated from a geothermal soil sample collected at Rehai National Park, Tengchong, Yunnan province, south-west China. Growth occurred from 28 to 65 °C (optimum 50 °C), pH 6.0–8.0 (optimum pH 7.0). The strain formed branched substrate mycelia, endospores were produced on the substrate mycelium and aerial mycelium was not produced on any of the growth media tested. Phylogenetic analyses based on 16S rRNA gene sequences indicated that strain YIM 77831^T was affiliated with the family Thermoactinomycetaceae. The stain YIM 77831^T contained meso-diaminopimelic acid in the cell wall. Whole-cell hydrolysates contained glucose, galactose, mannose, ribose and rhamnose. The polar lipids were phosphatidylmethylethanolamine, diphosphatidylglycerol, phosphatidylethanolamine, phosphatidylglycerol, an unidentified aminophospholipid and four unknown phospholipids. The only menaquinone was MK-7. Major fatty acids were iso-C_15:0, anteiso-C_15:0 and anteiso-C_17:0. The G+C content was 55.6 mol%. On the basis of the morphological and chemotaxonomic characteristics as well as genotypic data, strain YIM 77831^T represents a novel genus and species, Lihuaxuella thermophila gen. nov., sp. nov., in the family Thermoactinomycetaceae. The type strain is YIM 77831^T (CCTCC AA 2011024^T = JCM 18059^T).     

Thermus tengchongensis sp. nov., isolated from a geothermally heated soil sample in Tengchong, Yunnan, south-west China

A Gram-stain negative aerobic bacterium, designated YIM 77924^T, was isolated from a geothermally heated soil sample collected at Rehai National Park, Tengchong, Yunnan province, south-west China. Growth was found to occur from 55 to 75 °C (optimum 65 °C), pH 6.0–8.0 (optimum pH 7.0) and 0–1 % NaCl (w/v). Cells were observed to be rod-shaped and the colonies convex, circular, smooth, yellow and non-transparent. Phylogenetic analysis based on the 16S rRNA gene sequence indicated that strain YIM 77924^T belongs to the genus Thermus. The 16S rRNA gene sequence similarity values between strain YIM 77924^T and other species of the genus Thermus were all below 97 %. The polar lipids of strain YIM 77924^T were determined to be aminophospholipid, phospholipid and glycolipid. The predominant respiratory quinone was determined to be MK-8 and the G+C content was 66.64 mol%. The major fatty acids identified were iso-C_16:0, iso-C_15:0, iso-C_17:0 and C_16:0. On the basis of the morphological and chemotaxonomic characteristics as well as genotypic data, strain YIM 77924^T is proposed to represent a novel species, Thermus tengchongensis sp. nov., in the genus Thermus. The type strain is YIM 77924^T (=KCTC 32025^T = CCTCC AB2012063^T).     

Lysobacter thermophilus sp. nov., isolated from a geothermal soil sample in Tengchong, south-west China

A Gram-negative and aerobic bacterium, designated YIM 77875^T, was isolated from a geothermal soil sample collected at Rehai National Park, Tengchong, Yunnan Province, south-west China. Bacterial growth occurred from 37 to 65 °C (optimum 50 °C), pH 6.0–8.0 (optimum pH 7.0) and 0–1 % NaCl (w/v). Cells were rod-shaped and colonies were convex, circular, smooth, yellow and non-transparent. Phylogenetic analysis based on the 16S rRNA gene sequence indicated that strain YIM 77875^T belongs to the genus Lysobacter. The 16S rRNA gene sequence similarity values between strain YIM 77875^T and other species of the genus Lysobacter were all below 94.7 %. The polar lipids of strain YIM 77875^T were diphosphatidylglycerol, phosphatidylglycerol, phosphatidylethanolamine and five unknown phospholipids. The predominant respiratory quinone was Q-8 and the G+C content was 68.8 mol%. Major fatty acids were iso-C_16:0, iso-C_15:0 and iso-C_11:0. On the basis of the morphological and chemotaxonomic characteristics, as well as genotypic data, strain YIM 77875^T represents a novel species, Lysobacter thermophilus sp. nov., in the genus Lysobacter. The type strain is YIM 77875^T (CCTCC AB 2012064^T = KCTC 32020^T).     

Biogeochemistry of organic carbon, CO2, CH4, and trace elements in thermokarst water bodies in discontinuous permafrost zones of Western Siberia

Active processes of permafrost thaw in Western Siberia increase the number of soil subsidencies, thermokarst lakes and thaw ponds. In continuous permafrost zones, this process promotes soil carbon mobilisation to water reservoirs, as well as organic matter (OM) biodegradation, which produces a permanent flux of carbon dioxide (CO₂) to the atmosphere. At the same time, the biogeochemical evolution of aquatic ecosystems situated in the transition zone between continuous permafrost and permafrost-free terrain remains poorly known. In order to better understand the biogeochemical processes that occur in thaw ponds and lakes located in discontinuous permafrost zones, we studied ~30 small (1–100,000 m²) shallow (<1 m depth) lakes and ponds formed as a result of permafrost subsidence and thaw of the palsa bog located in the transition zone between the tundra and forest-tundra (central part of Western Siberia). There is a significant increase in dissolved CO₂ and methane (CH₄) concentration with decreasing water body surface area, with the largest supersaturation with respect to atmospheric CO₂ and CH₄ in small (<100 m²) permafrost depressions filled with thaw water. Dissolved organic carbon (DOC), conductivity, and metal concentrations also progressively increase from large lakes to thaw ponds and depressions. As such, small water bodies with surface areas of 1–100 m² that are not accounted for in the existing lake and pond databases may significantly contribute to CO₂ and CH₄ fluxes to the atmosphere, as well as to the stocks of dissolved trace elements and organic carbon. In situ lake water incubation experiments yielded negligible primary productivity but significant oxygen consumption linked to the mineralisation rate of dissolved OM by heterotrophic bacterioplankton, which produce a net CO₂ flux to the atmosphere of 5 ± 2.5 mol C m² year^?1. The most significant result of this study, which has long-term consequences on our prediction of aquatic ecosystem development in the course of permafrost degradation is CO₂, CH₄, and DOC concentrations increase with decreasing lake age and size. As a consequence, upon future permafrost thaw, the increase in the number of small water bodies, accompanied by the drainage of large thermokarst lakes to the hydrological network, will likely favour (i) the increase of DOC and colloidal metal stocks in surface aquatic systems, and (ii) the enhancement of CO₂ and CH₄ fluxes from the water surface to the atmosphere. According to a conservative estimation that considers that the total area occupied by water bodies in Western Siberia will not change, this increase in stocks and fluxes could be as high as a factor of ten.     

Pontibacter soli sp. nov., isolated from the soil of a Populus rhizosphere in Xinjiang, China

A Gram-stain negative, rod-shaped, non-motile and pink-pigmented bacterial strain, designated strain HYL7-26^T, was isolated from a soil in the Desert Park of Huyang forest located in Xinjiang, China. Phylogenetic analysis based on 16S rRNA gene sequences indicated that strain HYL7-26^T belongs to the genus Pontibacter in the family Cytophagaceae. The 16S rRNA gene sequence similarity between strain HYL7-26^T and type strains of Pontibacter species ranged from 93.2 to 96.0 %. Strain HYL7-26^T was found to contain iso-C_15:0 (15.9 %), iso-C_17:0 3-OH (9.5 %) and summed feature 4 (comprising anteiso-C_17:1 B and/or iso-C_17:1 I, 21.0 %, as defined by the MIDI system) as the major cellular fatty acids. The major respiratory quinone was identified as MK-7 and the DNA G+C content was determined to be 43.8 mol%. sym-Homospermidine was the major polyamine observed in the cells. On the basis of phenotypic, chemotaxonomic and phylogenetic data, strain HYL7-26^T is considered to represent a novel species of the genus Pontibacter, for which the name Pontibacter soli sp. nov. is proposed. The type strain is HYL7-26^T (=CCTCC AB 206240^T = NRRL B-59490^T).     

Flavobacterium qiangtangensis sp. nov., Isolated from Qiangtang Basin in Qinghai-Tibetan Plateau,China

A flexirubin-type yellow-pigmented, non-gliding, non-flagellated, gram-negative bacterium strain, designated F3^T, was isolated from a drilling core sample of the Qiangtang basin, Qinghai-Tibetan plateau, China. Phylogenetic analysis based on 16S rRNA gene sequences showed that the strain F3^T belongs to the genus Flavobacterium, with the highest 16S rRNA gene sequence similarity to the Flavobacterium noncentrifugens CGMCC 1.10076^T (94.92 %). Strain F3^T grew optimally at temperature about 20 °C, at pH about 7.0–8.0, at NaCl concentration 0 % (w/v). The DNA G+C content of the isolate was 35.5 mol%. The major polar lipid was phosphatidylethanolamine, predominant cellular fatty acids of the strain was iso-C_15:0 (22.02 %), while the major menaquinone was menaquinone 6. Due to the phenotypic and genetic distinctiveness and several other characteristic studied in this article, we consider F3^T as a novel species of the genus Flavobacterium, and propose to name it Flavobacterium qiangtangensis sp. nov. The type strain is F3^T (=CGMCC 1.12706^T = JCM 19739^T).     

Gracilibacillus xinjiangensis sp. nov., a new member of the genus Gracilibacillus isolated from Xinjiang region, China

A Gram-positive, endospore-forming, rod-shaped bacterium, designated isolate J2^T was isolated from a soil sample from Xinjiang Uyghur Autonomous Region, China. The isolate was observed to grow at 16–46 °C and pH 6.5–8.0. Chemotaxonomic analysis showed menaquinone-7 (MK-7) to be the major isoprenoid quinone; diphosphatidylglycerol, phosphatidylglycerol, one aminophospholipid, two phosphoglycolipids and one glycolipid as the major cellular polar lipids; and anteiso-C_15:0, iso-C_15:0, anteiso-C_17:0 and C_16:0 as the major fatty acids. Comparative analyses of the 16S rRNA gene sequence showed that strain J2^T is most closely related to Gracilibacillus ureilyticus (with 98.8 % similarity), Gracilibacillus dipsosauri (97.2 %), Gracilibacillus quinghaiensis (97.1 %) and Gracilibacillus thailandensis (97.0 %). The DNA–DNA reassociation values between strain J2^T and G. ureilyticus MF38^T, G. dipsosauri DD1^T, G. quinghaiensis YIM-C229^T and G. thailandensis TP2-8^T were 29.8 ± 3.7, 23.0 ± 3.5, 15.8 ± 4.9 and 15.9 ± 5.0 %, respectively. The genomic DNA G+C content of strain J2^T was determined to be 36.5 mol%. Based on these data, strain J2^T is considered as a novel species of the genus Gracilibacillus, for which the name Gracilibacillus xinjiangensis sp. nov. is proposed. The type species is J2^T (= CGMCC 1.12449^T = JCM 18859^T).     

Two novel species Enterococcus lemanii sp. nov. and Enterococcus eurekensis sp. nov., isolated from a swine-manure storage pit

A polyphasic taxonomic study using morphological, biochemical, chemotaxonomic and molecular genetic methods was performed on six strains of unknown Gram-positive, nonspore-forming, facultative anaerobic coccus-shaped bacteria isolated from a swine-manure storage pit. On the basis of the 16S rRNA, RNA polymerase α-subunit (rpoA) and 60 kDa chaperonin (cpn60) gene sequence analyses, it was shown that all the isolates were enterococci but formed two separate lines of descent. Pairwise 16S rRNA gene sequence comparisons demonstrated that the two novel organisms were most closely related to each other (97.9 %) and to Enterococcus aquimarinus (97.8 %). Both organisms contained major amounts of C_16:0, C_16:1 ω7c, C_16:1 ω7c, and C_18:1 ω7c/12t/9t as the major cellular fatty acids. Based on biochemical, chemotaxonomic and phylogenetic evidence, the names Enterococcus lemanii sp. nov. (type strain PC32^T = CCUG 61260^T = NRRL B-59661^T) and Enterococcus eurekensis sp. nov. (type strain PC4B^T = CCUG 61259^T = NRRL B-59662^T) are proposed for these hitherto undescribed species.     

Paludibacter jiangxiensis sp. nov., a strictly anaerobic,propionate-producing bacterium isolated from rice paddy field

A mesophilic, obligately anaerobic, propionate-producing fermentative bacterium, designated strain NM7^T, was isolated from rural rice paddy field. Cells of strain NM7^T are Gram-negative, non-motile, non-spore-forming, short rods, and negative for catalase. The strain grew optimally at 37 °C (the range for growth 15–40 °C) and pH 7.0 (pH 5.0–7.5). The strain could grow fermentatively on various sugars, including arabinose, xylose, fructose, galactose, glucose, mannose, cellobiose, lactose, maltose, sucrose, pectin and starch. The main end products of glucose fermentation were acetate and propionate. Yeast extract was not required but stimulated the growth. Nitrate, sulfate, thiosulfate, elemental sulfur, sulfite, and Fe(III) nitrilotriacetate were not used as terminal electron acceptors. The G+C content of genomic DNA was 42.8 mol%. The major cellular fatty acids were C_15:0, anteiso-C_15:0, C_16:0, and C_17:0. The most abundant polar lipid of strain NM7^T was phosphatidylethanolamine. 16S rRNA gene sequence analysis revealed that it belongs to the family Porphyromonadaceae of the phylum Bacteroidetes. The closest recognized species was Paludibacter propionicigenes (91.4 % similarity in 16S rRNA gene sequence). A novel species, Paludibacter jiangxiensis sp. nov., is proposed to accommodate strain NM7^T (=JCM 17480^T = CGMCC 1.5150^T = KCTC 5844^T).     

Halomonas zhaodongensis sp. nov., a slightly halophilic bacterium isolated from saline–alkaline soils in Zhaodong, China

A slightly halophilic bacterium (strain NEAU-ST10-25^T) was isolated from saline–alkaline soils in Zhaodong City, Heilongjiang Province, China. The strain is a Gram-negative, aerobic motile rod. It accumulates poly-β-hydroxyalkanoate and produces exopolysaccharide. It produces beige-yellow colonies. Growth occurs at NaCl concentrations (w/v) of 0–15 % (optimum 3 %), at temperatures of 4–60 °C (optimum 35 °C) and at pH 6–12 (optimum pH 9). Its G+C content is 53.8 mol%. Phylogenetic analyses based on the separate 16S rRNA gene and concatenation of the 16S rRNA, gyrB and rpoD genes indicate that it belongs to the genus Halomonas in the class Gammaproteobacteria. The most phylogenetically related species is Halomonas alkaliphila DSM 16354^T, with which strain NEAU-ST10-25^T showed 16S rRNA, gyrB and rpoD gene sequence similarities of 99.2, 82.3 and 88.2 %, respectively. The results of DNA–DNA hybridization assays showed 60.47 ± 0.69 % DNA relatedness between strain NEAU-ST10-25^T and H. alkaliphila DSM 16354^T, 42.43 ± 0.37 % between strain NEAU-ST10-25^T and Halomonas venusta DSM 4743^T and 30.62 ± 0.43 % between strain NEAU-ST10-25^T and Halomonas hydrothermalis DSM 15725^T. The major fatty acids are C_18:1 ω7c (62.3 %), C_16:0 (17.6 %), C_16:1 ω7c/C_16:1 ω6c (7.7 %), C_14:0 (2.9 %), C_12:0 3-OH (2.8 %), C_10:0 (2.1 %) and C_18:1 ω9c (1.6 %) and the predominant respiratory quinone is ubiquinone 9 (Q-9). The proposed name is Halomonas zhaodongensis, NEAU-ST10-25^T (=CGMCC 1.12286^T = DSM 25869^T) being the type strain.     

Bacillus borbori sp. Nov., Isolated From an Electrochemically Active Biofilm

A Gram-positive, facultative anaerobic, motile, endospore-forming rod strain, designated DX-4^T, was isolated from an electrochemically active biofilm. Growth occurred at 30–65 °C (optimum 55 °C), at pH 6.0–8.5 (optimum pH 7.0–7.5) and with <6 % (w/v) NaCl. Cells were catalase- and oxidase-positive. The main respiratory quinone was MK-7, the predominant polar lipids were diphosphatidylglycerol, phosphatidylethanolamine, phosphatidylglycerol, phosphatidylinositol mannoside, and unidentified aminophospholipid, the DNA G+C content was 38.6 mol% and the major fatty acids (>5 %) were iso-C_15:0 (38.9 %), iso-C_17:0 (30.5 %), iso-C_16:0 (5.6 %), and anteiso-C_17:0 (5.2 %). The phylogenetic analysis based on 16S rRNA gene sequence comparisons revealed that strain DX-4^T is a member of the genus Bacillus. The results of phenotypic, chemotaxonomic, and genotypic analyses clearly indicated that strain DX-4^T represents a novel species, for which the name Bacillus borbori sp. nov. is proposed. The type strain is DX-4^T (= CCTCC AB2012196^T = KCTC 33103^T).