共查询到20条相似文献,搜索用时 15 毫秒
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Andreote FD Jiménez DJ Chaves D Dias AC Luvizotto DM Dini-Andreote F Fasanella CC Lopez MV Baena S Taketani RG de Melo IS 《PloS one》2012,7(6):e38600
Here we embark in a deep metagenomic survey that revealed the taxonomic and potential metabolic pathways aspects of mangrove sediment microbiology. The extraction of DNA from sediment samples and the direct application of pyrosequencing resulted in approximately 215 Mb of data from four distinct mangrove areas (BrMgv01 to 04) in Brazil. The taxonomic approaches applied revealed the dominance of Deltaproteobacteria and Gammaproteobacteria in the samples. Paired statistical analysis showed higher proportions of specific taxonomic groups in each dataset. The metabolic reconstruction indicated the possible occurrence of processes modulated by the prevailing conditions found in mangrove sediments. In terms of carbon cycling, the sequences indicated the prevalence of genes involved in the metabolism of methane, formaldehyde, and carbon dioxide. With respect to the nitrogen cycle, evidence for sequences associated with dissimilatory reduction of nitrate, nitrogen immobilization, and denitrification was detected. Sequences related to the production of adenylsulfate, sulfite, and H(2)S were relevant to the sulphur cycle. These data indicate that the microbial core involved in methane, nitrogen, and sulphur metabolism consists mainly of Burkholderiaceae, Planctomycetaceae, Rhodobacteraceae, and Desulfobacteraceae. Comparison of our data to datasets from soil and sea samples resulted in the allotment of the mangrove sediments between those samples. The results of this study add valuable data about the composition of microbial communities in mangroves and also shed light on possible transformations promoted by microbial organisms in mangrove sediments. 相似文献
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Recent molecular studies on magnetotactic bacteria have identified a number of proteins associated with bacterial magnetites (magnetosomes) and elucidated their importance in magnetite biomineralisation. However, these analyses were limited to magnetotactic bacterial strains belonging to the α‐subclass of Proteobacteria. We performed a proteomic analysis of magnetosome membrane proteins in Desulfovibrio magneticus strain RS‐1, which is phylogenetically classified as a member of the δ‐Proteobacteria. In the analysis, the identified proteins were classified based on their putative functions and compared with the proteins from the other magnetotactic bacteria, Magnetospirillum magneticum AMB‐1 and M. gryphiswaldense MSR‐1. Three magnetosome‐specific proteins, MamA (Mms24), MamK, and MamM, were identified in strains RS‐1, AMB‐1, and MSR‐1. Furthermore, genes encoding ten magnetosome membrane proteins, including novel proteins, were assigned to a putative magnetosome island that contains subsets of genes essential for magnetosome formation. The collagen‐like protein and putative iron‐binding proteins, which are considered to play key roles in magnetite crystal formation, were identified as specific proteins in strain RS‐1. Furthermore, genes encoding two homologous proteins of Magnetococcus MC‐1 were assigned to a cryptic plasmid of strain RS‐1. The newly identified magnetosome membrane proteins might contribute to the formation of the unique irregular, bullet‐shaped crystals in this microorganism. 相似文献
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Indigenous arsenic(V)‐reducing microbial communities in redox‐fluctuating near‐surface sediments of the Mekong Delta
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Arsenic (As) cycling within soils and sediments of the Mekong Delta of Cambodia is affected by drastic redox fluctuations caused by seasonal monsoons. Extensive flooding during monsoon seasons creates anoxic soil conditions that favor anaerobic microbial processes, including arsenate [As(V)] respiration—a process contributing to the mobilization of As. Repeated oxidation and reduction in near‐surface sediments, which contain 10–40 mg kg?1 As, lead to the eventual downward movement of As to the underlying aquifer. Amplification of a highly conserved functional gene encoding dissimilatory As(V) reductase, arrA, can be used as a molecular marker to detect the genetic potential for As(V) respiration in environmental samples. However, few studies have successfully amplified arrA from sediments without prior enrichment, which can drastically shift community structure. In the present study, we examine the distribution and diversity of arrA genes amplified from multiple sites within the Cambodian Mekong Delta as a function of near‐surface depth (10, 50, 100, 200, and 400 cm), where sediments undergo seasonal redox fluctuations. We report successful amplification of 302 arrA gene sequences (72 OTUs) from near‐surface Cambodian soils (without prior enrichment or stimulation with carbon amendments), where a large majority (>70%) formed a well‐supported clade that is phylogenetically distinct from previously reported sequences from Cambodia and other South and Southeast Asian sediments, with highest sequence similarity to known Geobacter species capable of As(V) respiration, further supporting the potentially important role of Geobacter sp. in arsenic mobilization in these regions. 相似文献
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R. Peixoto G. M. Chaer F. L. Carmo F. V. Araújo J. E. Paes A. Volpon G. A. Santiago A. S. Rosado 《Antonie van Leeuwenhoek》2011,99(2):341-354
The majority of oil from oceanic oil spills converges on coastal ecosystems such as mangrove forests. A major challenge to
mangrove bioremediation is defining the mangrove’s pollution levels and measuring its recuperation from pollution. Bioindicators
can provide a welcome tool for defining such recovery. To determine if the microbial profiles reflected variation in the pollutants,
samples from different locations within a single mangrove with a history of exposure to oil were chemically characterised,
and the microbial populations were evaluated by a comprehensive range of conventional and molecular methods. Multivariate
ordination of denaturing gradient gel electrophoresis (DGGE) microbial community fingerprints revealed a pronounced separation
between the sediment and rhizosphere samples for all analysed bacterial communities (Bacteria, Betaproteobacteria, Alphaproteobacteria, Actinobacteria and Pseudomonas). A Mantel test revealed significant relationships between the sediment chemical fertility and oil-derived pollutants, most
of the bacterial community fingerprints from sediment samples, and the counts by different cultivation strategies. The level
of total petroleum hydrocarbons was significantly associated with the Bacteria and Betaproteobacteria fingerprints, whereas anthracene and the total level of polycyclic aromatic hydrocarbons were associated with the Actinobacteria. These results show that microbial communities from the studied mangrove reflect the spatial variation of the chemicals in
the sediment, demonstrating the specific influences of oil-derived pollutants. 相似文献
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Marcial Gomes NC Borges LR Paranhos R Pinto FN Mendonça-Hagler LC Smalla K 《FEMS microbiology ecology》2008,66(1):96-109
Municipal sewage, urban runoff and accidental oil spills are common sources of pollutants in urban mangrove forests and may have drastic effects on the microbial communities inhabiting the sediment. However, studies on microbial communities in the sediment of urban mangroves are largely lacking. In this study, we explored the diversity of bacterial communities in the sediment of three urban mangroves located in Guanabara Bay (Rio de Janeiro, Brazil). Analysis of sediment samples by means of denaturing gradient gel electrophoresis (DGGE) of 16S rRNA gene fragments suggested that the overall bacterial diversity was not significantly affected by the different levels of hydrocarbon pollution at each sampling site. However, DGGE and sequence analyses provided evidences that each mangrove sediment displayed a specific structure bacterial community. Although primer sets for Pseudomonas, alphaproteobacterial and actinobacterial groups also amplified ribotypes belonging to taxa not intended to be enriched, sequence analyses of dominant DGGE bands revealed ribotypes related to Alteromonadales, Burkholderiales, Pseudomonadales, Rhodobacterales and Rhodocyclales. Members of these groups were often shown to be involved in aerobic or anaerobic degradation of hydrocarbon pollutants. Many of these sequences were only detected in the sampling sites with high levels of anthropogenic inputs of hydrocarbons. Many dominant DGGE ribotypes showed low levels of sequence identity to known sequences, indicating a large untapped bacterial diversity in mangrove ecosystems. 相似文献
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G. Christian Jagersma Roel J. W. Meulepas Ineke Heikamp‐de Jong Jarno Gieteling Adam Klimiuk Stefan Schouten Jaap S. Sinninghe Damsté Piet N. L. Lens Alfons J. M. Stams 《Environmental microbiology》2009,11(12):3223-3232
Anaerobic oxidation of methane (AOM) is an important methane sink in the ocean but the microbes responsible for AOM are as yet resilient to cultivation. Here we describe the microbial analysis of an enrichment obtained in a novel submerged‐membrane bioreactor system and capable of high‐rate AOM (286 μmol gdry weight?1 day?1) coupled to sulfate reduction. By constructing a clone library with subsequent sequencing and fluorescent in situ hybridization, we showed that the responsible methanotrophs belong to the ANME‐2a subgroup of anaerobic methanotrophic archaea, and that sulfate reduction is most likely performed by sulfate‐reducing bacteria commonly found in association with other ANME‐related archaea in marine sediments. Another relevant portion of the bacterial sequences can be clustered within the order of Flavobacteriales but their role remains to be elucidated. Fluorescent in situ hybridization analyses showed that the ANME‐2a cells occur as single cells without close contact to the bacterial syntrophic partner. Incubation with 13C‐labelled methane showed substantial incorporation of 13C label in the bacterial C16 fatty acids (bacterial; 20%, 44% and 49%) and in archaeal lipids, archaeol and hydroxyl‐archaeol (21% and 20% respectively). The obtained data confirm that both archaea and bacteria are responsible for the anaerobic methane oxidation in a bioreactor enrichment inoculated with Eckernförde bay sediment. 相似文献
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Methanogenic bacteria in mangrove sediments 总被引:3,自引:0,他引:3
The occurrence of methanogenic bacteria in the Kodiakkarai (10° 18 N; 79° 52 E) mangrove sediments, whereAvicennia spp are predominant, was studied. Trimethylamine under N2:CO2 (80:20% v/v) was used as the substrate. Most Probable Number (MPN) of methanogenic bacteria was determined for a period of one year from July 1987 to June 1988 with monthly sampling. The methanogenic bacterial populations were found to be at the maximum of 1.1 × 105 MPN gm–1 of wet sediment during August 1987 and from February to June 1988. The bacterial numbers were found to decrease during October to December 1987 with a minimal value of 3.6 × 102 MPN gm–1 during December 1987. Environmental factors were correlated with the methanogenic bacterial population. 相似文献
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H. YOSHIOKA A. MARUYAMA T. NAKAMURA Y. HIGASHI H. FUSE S. SAKATA D. H. BARTLETT 《Geobiology》2010,8(3):223-233
We investigated methane production and oxidation and the depth distribution and phylogenetic affiliation of a functional gene for methanogenesis, methyl coenzyme M reductase subunit A (mcrA), at two sites of the Integrated Ocean Drilling Program Expedition 311. These sites, U1327 and U1329, are respectively inside and outside the area of gas hydrate distribution on the Cascadia Margin. Radiotracer experiments using 14C‐labelled substrates indicated high potential methane production rates in hydrate‐bearing sediments [128–223 m below seafloor (mbsf)] at U1327 and in sediments between 70 and 140 mbsf at U1329. Tracer‐free experiments indicated high cumulative methane production in sediments within and below the gas hydrate layer at U1327 and in sediments below 70 mbsf at U1329. Stable tracer experiments using 13C‐labelled methane showed high potential methane oxidation rates in near‐surface sediments and in sediments deeper than 100 mbsf at both sites. Results of polymerase chain reaction amplification of mcrA in DNA were mostly consistent with methane production: relatively strong mcrA amplification was detected in the gas hydrate‐bearing sediments at U1327, whereas at U1329, it was mainly detected in sediments from around the bottom‐simulating reflector (126 mbsf). Phylogenetic analysis of mcrA separated it into four phylotype clusters: two clusters of methanogens, Methanosarcinales and Methanobacteriales, and two clusters of anaerobic methanotrophic archaea, ANME‐I and ANME‐II groups, supporting the activity measurement results. These results reveal that in situ methanogenesis in deep sediments probably contributes to gas hydrate formation and are inconsistent with the geochemical model that microbial methane currently being generated in shallow sediments migrates downward and contributes to the hydrate formation. At Site U1327, gas hydrates occurred in turbidite sediments, which were absent at Site U1329, suggesting that a geological setting suitable for a gas hydrate reservoir is more important for the accumulation of gas hydrate than microbiological properties. 相似文献
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Ruo He Matthew J. Wooller John W. Pohlman James M. Tiedje Mary Beth Leigh 《Environmental microbiology》2015,17(9):3233-3250
Aerobic methane (CH4) oxidation mitigates CH4 release and is a significant pathway for carbon and energy flow into aquatic food webs. Arctic lakes are responsible for an increasing proportion of global CH4 emissions, but CH4 assimilation into the aquatic food web in arctic lakes is poorly understood. Using stable isotope probing (SIP) based on phospholipid fatty acids (PLFA‐SIP) and DNA (DNA‐SIP), we tracked carbon flow quantitatively from CH4 into sediment microorganisms from an arctic lake with an active CH4 seepage. When 0.025 mmol CH4 g?1 wet sediment was oxidized, approximately 15.8–32.8% of the CH4‐derived carbon had been incorporated into microorganisms. This CH4‐derived carbon equated to up to 5.7% of total primary production estimates for Alaskan arctic lakes. Type I methanotrophs, including Methylomonas, Methylobacter and unclassified Methylococcaceae, were most active at CH4 oxidation in this arctic lake. With increasing distance from the active CH4 seepage, a greater diversity of bacteria incorporated CH4‐derived carbon. Actinomycetes were the most quantitatively important microorganisms involved in secondary feeding on CH4‐derived carbon. These results showed that CH4 flows through methanotrophs into the broader microbial community and that type I methanotrophs, methylotrophs and actinomycetes are important organisms involved in using CH4‐derived carbon in arctic freshwater ecosystems. 相似文献
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The long‐term adaptation of bacterial communities in metal‐contaminated sediments: a metaproteogenomic study
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The aim of the study was to understand the effect of a long‐term metal exposure (110 years) on sediment microbial communities. Two freshwater sites, Férin and MetalEurop, differing by one order of magnitude in metal levels (MetalEurop: 3218 mg Zn kg?1; 913 mg Pb kg?1) were compared by shotgun metaproteogenomics. A total of 69–118 Mpb of DNA and 943–1241 proteins were obtained. Phymm BL analysis of the DNA sequences indicated that the phylogenetic profile was similar in both stations and that β‐Proteobacteria were dominant. However, subtle but significant changes were observed for some bacteria: e.g. Pseudomonas (+0.4%), Leptothrix (–0.4%), Thiobacillus (+0.36%) and Acidovorax (+0.48%). Using the stamp software, the two communities were found to be functionally very similar. However, significant genetic differences (10?6 < P < 10?3) were observed for three SEED categories: synthesis of exopolymeric substances, virulence and defence mechanisms (including czcA metal efflux genes), and elements involved in horizontal gene transfer. The CzcA protein was found by metaproteomics in MetalEurop, but the levels were too low to allow comparisons. It is concluded that bacterial communities in freshwater sediments may adapt to high metal levels without broad changes in the structure of the population. 相似文献
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古菌在红树林沉积物中的多样性及其碳代谢机制 总被引:1,自引:0,他引:1
红树林湿地生态系统具有维持生物多样性、净化环境及维持海岸带生态平衡等多种功能。古菌普遍存在于红树林沉积物中,在元素的生物地球化学循环中发挥着重要作用。古菌具有丰富的碳代谢多样性,能固定CO_2,参与甲烷循环,产乙酸,降解蛋白质、多聚碳水化合物等有机质,但目前对于红树林沉积物中古菌碳代谢的研究才刚刚起步。高通量测序技术的快速发展促进了大量新的古菌门类的发现,这些新的古菌门类具备多样的碳代谢潜力。本文简要概述古菌的主要类群与分布,综述国内外有关古菌碳代谢多样性的最新研究进展,并阐明这些古菌在红树林生态系统中的生态分布和功能特征,为进一步探究古菌代谢机制提供知识基础。 相似文献
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Structure of ground‐dwelling ant communities in burned and unburned areas in Brazilian subtropical grasslands
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Fire is frequently used in the management of pastures in southern Brazil, but its effects on ground‐dwelling ant communities in Brazilian subtropical grasslands is still poorly understood. Here, we compared ant species richness and composition between periodically burned and unburned areas in native grasslands of the Atlantic Forest biome. In total, we found 35 epigeic ant species in burned and unburned areas. There was slightly higher species richness in burned than in unburned areas, independent of the sampling period (season). There was a significant difference in richness over the sampling period (season effect). Species composition varied significantly between the areas, in which nine species (26%) occurred only in burned areas, eight (23%) occurred only in unburned areas, and 18 (51%) occurred in both. Four species showed a significant preference for burned sites (Camponotus crassus, Linepithema humile and two undetermined species of Pheidole and Solenopsis). Although this study did not separate fire effects on ground‐dwelling ant communities (due to sampling design), it provides new information regarding subtropical native grasslands that can be used as a baseline for future studies. 相似文献