Seasonal changes and diversity of bacteria in Bohai Bay by RFLP analysis of PCR-amplified 16S rDNA gene fragments

Information about seasonal bacterial composition and diversity is of great value for exploitation of marine biological resources and improvement of ecological environment. Here PCR-amplified restriction fragment length polymorphism (PCR–RFLP) of 16S rRNA genes was used to evaluate seasonal bacterial diversity and community composition in Bohai Bay. A total of 24 bacterial communities were sampled from seawater and sediment of three representative sites in a whole seasonal cycle: spring (April), summer (July), autumn (October), and winter (January). Bacterial Genomic DNA was extracted and PCR-amplified to obtain 16S rDNA fragments which were cloned to construct 24 16s rDNA libraries. Clones of each library were selected randomly for PCR–RFLP analysis of rDNA fragments, and eventually 101 genotypes were identified by RFLP fingerprintings. These 101 genotypes were sequenced and their respective phylotype was identified through the Blast tool of NCBI (similarity 96–100%) and phylogenetic analyses. Among our phylotypes, 80.2% belonged to the genera α-Proteobacteria, β-proteobacteria,γ-Proteobacteria, δ-Proteobacteria, ε-proteobacteria, Flavobacteria, Cytophaga-Flavobacteria-Bacteroides, Verrucomicrobia, Firmicutes and Actinobacteria. Sequence analyses revealed that 47.5% (48) of clone sequences were similar to those of uncultured marine bacteria in the environment. In addition, bacterial diversity and composition clearly displayed seasonal variety. More genera were discovered in summer than any other seasons, and some special species appeared only in specific season.     

Survey and phylogenetic analysis of culturable microbes in the oral secretions of three bark beetle species

In a recent study, we reported a previously undescribed behavior in which a bark beetle exuded oral secretions containing bacteria that have antifungal properties, and hence defend their galleries against pervasive antagonistic Hyphomycete fungi. Actinobacteria, a group known for their antibiotic properties, were the most effective against fungi that invade the spruce beetle galleries. In the present study, we describe the isolation and identification of microorganisms from oral secretions of three bark beetles (Coleoptera: Curculionidae: Scolytinae): the spruce beetle, Dendroctonus rufipennis Kirby, the mountain pine beetle, Dendroctonus ponderosae Hopkins, and the pine engraver, Ips pini Say. Bacteria isolated from these three species span the major bacterial classes α-, β-, and γ-Proteobacteria, Firmicutes, Bacteroidetes, and Actinobacteria, except for D. ponderosae , which yielded no α-proteobacteria or Bacteroidetes isolates. Spruce beetles and pine engraver beetles had similar numbers of α-proteobacteria isolates, but pine engravers yielded twice as many Bacteroidetes isolates as spruce beetles. In contrast, mountain pine beetles yielded more isolates in the β- and γ-proteobacteria than spruce beetles and pine engravers. The highest percentage of Actinobacteria was obtained from spruce beetles, followed by pine engravers and mountain pine beetles. All of the fungal isolates obtained from the three beetle species were Ascomycetes. The greatest fungal diversity was obtained in spruce beetles, which had nine species, followed by pine engravers with five, and mountain pine beetles with one.     

Effect of single-species and mixed-species leaf leachate on bacterial communities in biofilms

Bacterial communities in two shallow eutrophic aquatic ecosystems (eastern China) were studied using culture-dependent methods, and their correlations with the other water parameters were analyzed. Although the values of the comprehensive trophic state index in Xizi Lake and Hangzhou Canal were almost identical, the abundances of cultivable bacterial communities, such as protein-hydrolyzing bacteria (PHB), fecal coliforms (FC), nitrogen-utilizing bacteria, phosphate-mineralizing bacteria, and cellulose-decomposing bacteria (CDB), differed significantly. They were much less in Xizi Lake than in Hangzhou Canal. Correlation analyses indicated that the abundances of physiological groups of bacteria were determined mainly by the biomasses of phytoplankton and zooplankton, rather than by the utilized substrates. Xizi Lake was an algae-dominated aquatic ecosystem, a situation that mainly arose from the influx of inorganic nutrients, and the Hangzhou Canal was bacteria-dominated due to the influx of organic sewage. Molecular characterization and phylogenetic analysis of isolates showed that there were 6 phylogenetic lineages out of 15 isolates screened from Xizi Lake, including γ-proteobacteria (5), β-proteobacteria (3), α-proteobacteria (2), actinobacteria (1), firmicutes (4), and bacteroidetes (1). While in Hangzhou Canal there were only 4 bacterial groups among 22 isolates, γ-proteobacteria comprised about 82%, α-proteobacteria made up 9%, firmicutes and bacteroidetes made up only 4.5%, respectively, and no β-proteobacteria were found. Enterobacteriaceae were the principal bacteria components in the two aquatic ecosystems, especially in the sewage-polluted Hangzhou Canal. It can be concluded preliminarily that the bacterial diversity in Xizi Lake is richer than that in Hangzhou Canal. Handling editor: J. Padisak     

Characterization of Viable Bacteria from Siberian Permafrost by 16S rDNA Sequencing

Abstract Viable bacteria were found in permafrost core samples from the Kolyma-Indigirka lowland of northeast Siberia. The samples were obtained at different depths; the deepest was about 3 million years old. The average temperature of the permafrost is −10°C. Twenty-nine bacterial isolates were characterized by 16S rDNA sequencing and phylogenetic analysis, cell morphology, Gram staining, endospore formation, and growth at 30°C. The majority of the bacterial isolates were rod shaped and grew well at 30°C; but two of them did not grow at or above 28°C, and had optimum growth temperatures around 20°C. Thirty percent of the isolates could form endospores. Phylogenetic analysis revealed that the isolates fell into four categories: high-GC Gram-positive bacteria, β-proteobacteria, γ-proteobacteria, and low-GC Gram-positive bacteria. Most high-GC Gram-positive bacteria and β-proteobacteria, and all γ-proteobacteria, came from samples with an estimated age of 1.8–3.0 million years (Olyor suite). Most low-GC Gram-positive bacteria came from samples with an estimated age of 5,000–8,000 years (Alas suite). Received: 11 April 1996 Accepted: 8 May 1996     

Bacterial Diversity and Distribution in the Holocene Sediments of a Northern Temperate Lake

Sediments contain an abundance of microorganisms. However, the diversity and distribution of microorganisms associated with sediments are poorly understood, particularly in lacustrine environments. We used banding patterns from denaturing gradient gel electrophoresis (DGGE) and 16S rDNA sequences to assess the structure of bacterial communities in the Holocene sediments of a meromictic lake in Minnesota. Cluster analysis of the DGGE banding patterns indicates that the early- and middle-Holocene samples group separately from the late-Holocene samples. About 79% of the recovered bacterial sequences cluster with the α-, β-, δ-, ɛ-, and γ- Proteobacteriaceae and Firmicutes. The remaining ∼21% lack cultured representatives. The taxonomic lineages of bacteria differ statistically among the early-, middle-, and late-Holocene samples, although the difference is smallest between early- and middle-Holocene samples. Early- and middle-Holocene samples are dominated by ɛ-Proteobacteriaceae, and late-Holocene samples are dominated by sequences from uncultured subphyla. We only recovered δ-Proteobacteriaceae in late-Holocene sediments and α- and γ- Proteobacteriaceae in late- and middle-Holocene sediments. Diversity estimates derived from early-, middle-, and late-Holocene clone libraries indicate that the youngest (late-Holocene) samples had significantly greater bacterial diversity than the oldest (early-Holocene) samples, and the middle-Holocene samples contained intermediate levels of diversity. The observed patterns of diversity may be caused by increased bacterial niche-partitioning in younger sediments that contain a greater abundance of labile organic matter than older sediments. D. M. Nelson and S. Ohene-Adjei contributed equally to this work     

Microbial Diversity in Sediments Collected from the Deepest Cold-Seep Area, the Japan Trench

The Japan Trench land slope at a depth of 6,400 m is the deepest cold-seep environment with Calyptogena communities. Sediment samples from inside and beside the Calyptogena communities were collected, and the microbial diversity in the sediment samples was studied by molecular phylogenetic techniques. From DNA extracted directly from the sediment samples, 16S rDNAs were amplified by the polymerase chain reaction method. The sequences of the amplified 16S rDNAs selected by restriction fragment length polymorphism analysis were determined and compared with sequences in DNA databases. The results showed that 33 different bacterial 16S rDNA sequences from the two samples analyzed fell into similar phylogenetic categories, the α-, γ-, δ-, and ɛ-subdivisions of Proteobacteria, Cytophaga, and gram-positive bacteria; some of the 16S rDNA sequences were common to both samples. δ- and ɛ-Proteobacteria-related sequences were abundant in both sediments. These sequences are mostly related to sulfate-reducing or sulfur-reducing bacteria and epibionts, respectively. Eight different archaeal 16S rDNA sequences were cloned from the sediments. The majority of the archaeal 16S rDNA sequences clustered in Crenarchaeota and showed high similarities to marine group I archaeal rDNA. A Methanococcoides burtonii–related sequence obtained from the sediment clustered in the Euryarchaeota indicating that M. burtonii–related strains in the area of Calyptogena communities may contribute to production of methane in this environment. From these results, we propose a possible model of sulfur circulation within the microbial community and that of Calyptogena clams in the cold-seep environment. Received June 15, 1998; accepted November 10, 1998.     

Comparative molecular biological analysis of the microbial community of the Holocene and Pleistocene deposits of Posol’skaya Shoal,Lake Baikal

The bacterial diversity was studied in sediment layers of Posol’skaya Shoal station (Southern Baikal) belonging to different periods. A set of primers specific to individual bacterial groups was used to analyze the 16S rRNA gene fragments. The bacterial diversity in the Holocene deposits was found to be higher than in the Pleistocene ones. In the upper sediments, a positive PCR reaction with bacterial primers and with specific cyanobacterial and archaebacterial primers was detected. The following phylogenetic groups were revealed in the microbial community of the surface horizon: green nonsulfur bacteria, δ-proteobacteria, β-proteobacteria (Nitrospirae), α-proteobacteria, acidobacteria, crenarchaeota, euryarchaeota, and groups of uncultured bacteria. From the DNA of the Pleistocene deposits, the PCR product was obtained only with bacterial primers. The representatives of the genus Pseudomonas were most closely related to the sequences obtained (95–97% homology).     

Bacterial,archaeal and eukaryotic diversity in Arctic sediment as revealed by 16S rRNA and 18S rRNA gene clone libraries analysis

We studied the microbial diversity in the sediment from the Kongsfjorden, Svalbard, Arctic, in the summer of 2005 based on the analysis of 16S rRNA and 18S rRNA gene clone libraries. The sequences of the cloned 16S rRNA and 18S rRNA gene inserts were used to determine the species identity or closest relatives by comparison with sequences of known species. Compared to the other samples acquired in Arctic and Antarctic, which are different from that of ours, the microbial diversity in our sediment is much higher. The bacterial sequences were grouped into 11 major lineages of the domain Bacteria: Proteobacteria (include α-, β-, γ-, δ-, and ε-Proteobacteria); Bacteroidetes; Fusobacteria; Firmicutes; Chloroflexi; Chlamydiae; Acidobacteria; Actinobacteria; Planctomycetes; Verrucomicrobiae and Lentisphaerae. Crenarchaeota were dominant in the archaeal clones containing inserts. In addition, six groups from eukaryotes including Cercozoa, Fungi, Telonema, Stramenopiles, Alveolata, and Metazoa were identified. Remarkably, the novel group Lentisphaerae was reported in Arctic sediment at the first time. Our study suggested that Arctic sediment as a unique habitat may contain substantial microbial diversity and novel species will be discovered.     

Degradation of Crude Oil and PAHs in Iron–Manganese Concretions and Sediment from the Northern Baltic Sea

The ability of different sea bottom types to recover from oil contamination under oxic and anoxic conditions is poorly known in the brackish Baltic Sea. We carried out microcosm experiments to examine the capacity of iron–manganese concretions and sediment to remove petroleum compounds at 10°C. The biological degradation potential of polycyclic aromatic hydrocarbons (PAHs) was indicated by the 1000-fold increase in the copy numbers of PAH-degradation genes resulting in 2.2 × 10⁶ gene copies g^?1 DW. In the experiments 35?81% of the crude oil and 96% of PAHs disappeared through abiotic and biotic pathways, and there was little difference between the concretions and sediment. Bacterial community analysis revealed that the bacterial sequences obtained from the oil-treated concretions were affiliated to groups typical for concretions and metal-rich environments, whereas oil-treated sediment sequences were similar to those originating from sediments and oil-contaminated environments. The high frequency of concretion clones affiliated with specific taxonomic groups of α-, β-, γ-, and δ-proteobacteria may indicate the existence of new clades of bacteria within the Rhizobiales and Rhodospirillales of the α-proteobacteria, Burkholderiales—incertae sedis of the β-proteobacteria, Chromatiales of the γ-proteobacteria and the Syntrophobacteriales of the δ-proteobacteria. Our study suggests that concretions and bottom sediment maintain rich, distinct bacterial communities under oil exposure that have the potential to remove petroleum compounds in oxic and anoxic conditions.     

Characterization of Bacterial Communities Associated with Organic Aggregates in a Large, Shallow, Eutrophic Freshwater Lake (Lake Taihu, China)

Although organic-aggregate-associated bacteria play a pivotal role in microbial food webs and in the cycling of major elements, their community composition and diversity have not been extensively studied, especially in shallow freshwater systems. This study is among the first to explore intra-lake horizontal heterogeneity of organic-aggregate-associated bacterial community composition (OABC) in the large, shallow, and eutrophic Lake Taihu. During November 2006, samples were collected at four locations representing different trophic states and food web structures. Regional variability of OABC and diversity were studied by amplified ribosomal DNA restriction analysis and comparative analysis of four large 16S ribosomal RNA clone libraries. Our results demonstrate that OABC were numerically dominated by members of the β-proteobacteria (19.2–38.6%), Bacteroidetes (3.6–20.0%), and α-proteobacteria (11.5–19.2%) groups. The dominance of the Bacteroidetes group was related to algae-based aggregates. Horizontal heterogeneity of OABC exists within habitats, suggesting that the trophic state of the water and the physicochemical properties of organic aggregates (OA) play a key role. Diverse bacterial communities found on OA were substantially different from free-living ones. Comparative statistical analyses of the habitats of OA-associated bacteria highlight the potential ecological importance of the exchange between OABC and the surrounding planktonic community. Lastly, we found at least 45% of sequences closely related to ones previously found in soils, sludge, sediments, and other habitats. This demonstrates that microorganisms from terrestrial and sediment habitats are an important component of OA. Electronic supplementary material  The online version of this article (doi:) contains supplementary material, which is available to authorized users.     

Methanogen and bacterial diversity and distribution in deep gas hydrate sediments from the Cascadia Margin as revealed by 16S rRNA molecular analysis

The microbial community of a deep (to 234 m below the sea floor) sediment gas hydrate deposit (Cascadia Margin Ocean Drilling Program Site 889/890, Leg 146) was analysed for the first time by molecular genetic techniques. Both bacterial and methanogen diversity were determined by phylogenetic analysis of ribosomal DNA sequences. High molecular mass DNA, indicative of active bacteria, was present in all of the samples. Ribosomal RNA genes were amplified from extracted DNA extracted from sediment using bacteria, and methanogen specific PCR primers, the latter designed in this study. Phylogenetic analysis of approximately 400 bacterial clones demonstrated that 96% were members of the Proteobacteria. These clones were affiliated with the alpha, beta and gamma subdivisions, with Caulobacter (Zymomonas group), Ralstonia and Pseudomonas phylotypes predominating. The methanogen clones were of low diversity and clustered in three sub-groups. Two of these sub-groups (contained 96% of the 400 clones) were closely related to Methanosarcina mazeii, while the third sub-group clustered in the Methanobacteriales. This analysis of a deep sediment gas hydrate environment shows a bacteria and methanogen community of limited diversity and confirms that the gas hydrate zone is biogeochemically active. These results are consistent with the presence of bacterial populations capable of methanogenesis throughout the core, and suggest that the methane hydrate at this site is at least partially biogenic in origin.     

Assessment of Factors Influencing Direct Enumeration of Viruses within Estuarine Sediments

Accurate enumeration of viruses within environmental samples is critical for investigations of the ecological role of viruses and viral infection within microbial communities. This report evaluates differences in viral and bacterial direct counts between estuarine sediment samples which were either immediately processed onboard ship or frozen at −20°C and later processed. Viral and bacterial abundances were recorded at three stations spanning the length of the Chesapeake Bay in April and June 2003 within three sediment fractions: pore water (PW), whole sediment (WS), and sediment after pore water removal (AP). No significant difference in viral abundance was apparent between extracts from fresh or frozen sediments. In contrast, bacterial abundance was significantly lower in the samples subjected to freezing. Both bacterial and viral abundance showed significant differences between sediment fractions (PW, WS, or AP) regardless of the fresh or frozen status. Although pore water viral abundance has been used in the past as a measurement of viral abundance in sediments, this fraction accounted for only ca. 5% of the total sediment viral abundance across all samples. The effect of refrigerated storage of sediment viral extracts was also examined and showed that, within the first 2 h, viral abundance decreased ca. 30% in formalin-fixed extracts and 66% in unfixed extracts. Finally, the reliability of direct viral enumeration via epifluorescence microscopy was tested by using DNase treatment of WS extractions. These tests indicated that a large fraction (>86%) of the small SYBR gold fluorescing particles are likely viruses.     

Phylogenetic profiling of bacterial community from two intimately located sites in Balramgari,North-East coast of India

Microbial communities in coastal subsurface sediments play an important role in biogeochemical cycles. In this study microbial communities in tidal subsurface sediments of Balramgari in the state of Orissa, India were investigated using a culture independent approach. Two 16S rDNA cloned libraries were prepared from the closely located (100 m along the coast) subsurface sediment samples. Library I sediment samples had higher organic carbon content but lower sand percentage in comparison to Library II. A total of 310 clone sequences were used for DOTUR analysis which revealed 51 unique phylotypes or operational taxonomic units (OTUs) for both libraries. The OTUs were affiliated with 13 major lineages of domain bacteria including Proteobacteria (α, β, δ and λ), Acidobacteria, Actinobacteria, Cyanobacteria, Chloroflexi, Firmicutes, Verrucomicrobia, Bacteroidetes, Gemmatimonadetes and TM7. We encountered few pathogenic bacteria such as Aeromonas hydrophila and Ochrobactrum intermedium, in sediment from Library I. ∫-LIBSHUFF comparison depicts that the two libraries were significantly different communities. Most of the OTUs from both libraries possessed ≥85% to <97% similarity to RDP database sequences depicting the putative presence of new species, genera and phylum. This work revealed the complex and unique bacterial diversity from coastal habitat of Balramgari and shows that, in coastal habitat a variability of physical and chemical parameter has a prominent impact on the microbial community structure.     

Distribution Characteristics of Anammox Bacteria in Ancient Canal (Guyun River) Riparian Sediment of Zhenjiang,China

Riparian sediment is an important active interface zone for nitrogen-biogeochemical cycles. However, the distribution characteristics of anammox bacteria are not adequately described in the riparian sediment of urban rivers. Therefore, the distribution characteristics of anammox bacteria of Guyun river riparian sediment, which is the representative urban river, were investigated in this study. Research results showed that anammox bacterial abundance showed a significant spatial variation at the study area. Abundance values ranged from 2.00?×?10⁵ to 1.92?×?10⁷ copies·g^?1?dry sediment. And the average value was 6.64×10⁶ copies·g^?1 dry sediment in six collected samples. Abundance of anammox bacteria was significantly related to TN, NH₄⁺-N, and pH. Slight spatial variations of richness and diversity in Guyun river riparian sediment were obtained and physicochemical parameters of sediment samples did not significantly influence the biodiversity index of anammox bacteria. Phylogenetic analysis indicated that all amplified sequences fell within the known anammox bacterial group, i.e., Brocadia, Anammoxoglobus/Jettenia, and Kuenenia, with proportions of 33.91%, 24.35%, and 41.74%, respectively. The relative abundance of anammox bacteria showed distinctive spatial heterogeneity in six different sample sites. This finding indicated a distinct spatial variation of anammox bacterial in Guyun river riparian sediment.     

Bacterial Endosymbioses of Gutless Tube-Dwelling Worms in Nonhydrothermal Vent Habitats

Gutless tube-dwelling worms of pogonophorans (also known as frenulates) and vestimentiferans depend on primary production of endosymbiotic bacteria. The endosymbionts include thiotrophs that oxidize sulfur for autotrophic production and methanotrophs that oxidize and assimilate methane. Although most of the pogonophoran and vestimentiferan tube worms possess single thiotrophic 16S rRNA genes (16S rDNA) related to γ-proteobacteria, some pogonohorans are known to bear single methanotroph species or even dual symbionts of thiotrophs and methanotrophs. The vestimentiferan Lamellibrachia sp. L1 shows symbiotic 16S rDNA sequences of α-, β-, γ-, and ε-proteobacteria, varying among specimens, with RuBisCO form II gene (cbbM) sequences related to β-proteobacteria. An unidentified pogonophoran from the world’s deepest cold seep, 7326-m deep in the Japan Trench, hosts a symbiotic thiotroph based on 16S rDNA with the RuBisCO form I gene (cbbL). In contrast, a shallow-water pogonophoran (Oligobrachia mashikoi) in coastal Japan Sea has a methanotrophic 16S rDNA and thiotrophic cbbL, which may suggest the feature of type X methanotrophs. These observations demonstrate that pogonophoran and vestimentiferan worms have higher plasticity in bacterial symbioses than previously suspected.     

Bacterial diversity in surface sediments from the Pacific Arctic Ocean

In order to assess bacterial diversity within four surface sediment samples (0–5 cm) collected from the Pacific Arctic Ocean, 16S ribosomal DNA clone library analysis was performed. Near full length 16S rDNA sequences were obtained for 463 clones from four libraries and 13 distinct major lineages of Bacteria were identified (α, β, γ, δ and ε-Proteobacteria, Acidobacteria, Bacteroidetes, Chloroflexi, Actinobacteria, Firmicutes, Planctomycetes, Spirochetes, and Verrucomicrobia). α, γ, and δ-Proteobacteria, Acidobacteria, Bacteroidetes, Actinobacteria were common phylogenetic groups from all the sediments. The γ-Proteobacteria were the dominant bacterial lineage, representing near or over 50% of the clones. Over 35% of γ-Proteobacteria clones of four clone library were closely related to cultured bacterial isolates with similarity values ranging from 94 to 100%. The community composition was different among sampling sites, which potentially was related to geochemical differences.     

Assessment of factors influencing direct enumeration of viruses within estuarine sediments

Accurate enumeration of viruses within environmental samples is critical for investigations of the ecological role of viruses and viral infection within microbial communities. This report evaluates differences in viral and bacterial direct counts between estuarine sediment samples which were either immediately processed onboard ship or frozen at -20 degrees C and later processed. Viral and bacterial abundances were recorded at three stations spanning the length of the Chesapeake Bay in April and June 2003 within three sediment fractions: pore water (PW), whole sediment (WS), and sediment after pore water removal (AP). No significant difference in viral abundance was apparent between extracts from fresh or frozen sediments. In contrast, bacterial abundance was significantly lower in the samples subjected to freezing. Both bacterial and viral abundance showed significant differences between sediment fractions (PW, WS, or AP) regardless of the fresh or frozen status. Although pore water viral abundance has been used in the past as a measurement of viral abundance in sediments, this fraction accounted for only ca. 5% of the total sediment viral abundance across all samples. The effect of refrigerated storage of sediment viral extracts was also examined and showed that, within the first 2 h, viral abundance decreased ca. 30% in formalin-fixed extracts and 66% in unfixed extracts. Finally, the reliability of direct viral enumeration via epifluorescence microscopy was tested by using DNase treatment of WS extractions. These tests indicated that a large fraction (>86%) of the small SYBR gold fluorescing particles are likely viruses.     

北极表层海水中氯代十六烷降解菌的多样性

[目的]为了研究北极地区表层海水中氯代十六烷(C16H33Cl)降解菌的多样性,并获得新的卤代烃降解菌资源.[方法]以C16H33Cl为唯一碳源和能源在4℃和250℃下对表层海水样品进行富集,通过平板分离鉴定可培养菌株,并验证其降解能力;同时利用变性梯度凝胶电泳(DGGE)分析降解菌群结构.[结果]从12个北极表层海水样品中富集分离得到112株可培养菌株.经过降解实验验证,发现19株菌株能够降解氯代十六烷,其中食烷菌(Alcanivorax)、红球菌(Rhodococcus)表现出很好的乳化和降解现象,海杆菌(Marinobacter)也有较好的降解效果.DGGE分析显示,富集驯化的降解菌群中主要优势菌为Alcanivorax,Parvibaculum和Thioclava属的菌株.[结论]北极海水中卤代烃降解菌主要是α-proteobacteria,γ-proteobacteria,Actinobacteria和Bacteroidetes.文章首次报道了北极海水卤代烷烃降解菌多样性,研究结果对于认识北极环境中的降解菌资源与生物多样性有参考价值.     

Vertical distribution and diversity of bacteria and archaea in sulfide and methane-rich cold seep sediments located at the base of the Florida Escarpment

The bacterial and archaeal communities of the sediments at the base of the Florida Escarpment (Gulf of Mexico, USA) were investigated using molecular phylogenetic analysis. The total microbial community DNA of each of three vertical zones (top, middle and bottom) of a sediment core was extracted and the 16S rRNA genes were amplified by PCR, cloned and sequenced. Shannon–Weaver Diversity measures of bacteria were high in all three zones. For the archaea, diversity was generally low, but increased with depth. The archaeal clonal libraries were dominated by representatives of four groups of organisms involved in the anaerobic oxidation of methane (ANME groups). Phylogenetic analysis of bacteria suggests the dominance of -proteobacteria in the top zone, the -, - and -proteobacteria in the middle zone and the -proteobacteria in the bottom zone of the core. Members of the Cytophaga–Flexibacter–Bacteroidetes group, the Chloroflexi/green non-sulfur bacteria, the Gram+ (Firmicutes), the Planctomyces, candidate division WS3 and Fusobacterium were also detected. Our data suggest that the community structure and diversity of microorganisms can shift greatly within small vertical distances, possibly in response to changes in the physical and chemical conditions.     

Bacterial community along a historic lake sediment core of Ardley Island, west Antarctica

The bacterial community in a historic lake sediment core of Ardley Island, Antarctica, spanning approximately 1,600 years, was investigated by molecular approaches targeting the 16S rRNA gene fragments. The cell number in each 1 cm layer of the sediment core was deduced through semi-quantification of the 16S rRNA gene copies by quantitative competitive PCR (QC-PCR). It was found that the total bacterial numbers remained relatively stable along the entire 59 cm sediment core. Denaturing Gradient Gel Electrophoresis (DGGE) analysis and sequencing of PCR-amplified 16S rRNA gene fragments were performed to analyze the bacterial diversity over the entire column. Principle coordinates analysis suggested that the bacterial communities along the sediment core could be separated into three groups. There were obvious bacterial community shift among groups of 1–20 cm, 21–46 cm and 46–59 cm. Diversity indices indicated that the bacterial community in the 21–46 cm depth showed the highest species diversity and uniformity. The main bacterial groups in the sediments fell into 4 major lineages of the gram-negative bacteria: the α, γ and δ subdivision of Proteobacteria, the Cytophaga-Flavobacteria-Bacteroides, and some unknown sequences. The gram-positive bacteria Gemmatimonadetes, Firmicutes and Actinobacteria were also detected. The results demonstrated the presence of highly diverse bacterial community population in the Antarctic lake sediment core. And the possible influence of climate and penguin population change on the bacterial community shift along the sediment core was discussed.Shengkang Li and Xiang Xiao contributed equally to this paper