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1.
Microbial succession during leaf breakdown was investigated in a small forested stream in west-central Georgia, USA, using multiple culture-independent techniques. Red maple (Acer rubrum) and water oak (Quercus nigra) leaf litter were incubated in situ for 128 days, and litter breakdown was quantified by ash-free dry mass (AFDM) method and microbial assemblage composition using phospholipid fatty acid analysis (PLFA), ribosomal intergenic spacer analysis (RISA), denaturing gradient gel electrophoresis (DGGE), and bar-coded next-generation sequencing of 16S rRNA gene amplicons. Leaf breakdown was faster for red maple than water oak. PLFA revealed a significant time effect on microbial lipid profiles for both leaf species. Microbial assemblages on maple contained a higher relative abundance of bacterial lipids than oak, and oak microbial assemblages contained higher relative abundance of fungal lipids than maple. RISA showed that incubation time was more important in structuring bacterial assemblages than leaf physicochemistry. DGGE profiles revealed high variability in bacterial assemblages over time, and sequencing of DGGE-resolved amplicons indicated several taxa present on degrading litter. Next-generation sequencing revealed temporal shifts in dominant taxa within the phylum Proteobacteria, whereas γ-Proteobacteria dominated pre-immersion and α- and β-Proteobacteria dominated after 1 month of instream incubation; the latter groups contain taxa that are predicted to be capable of using organic material to fuel further breakdown. Our results suggest that incubation time is more important than leaf species physicochemistry in influencing leaf litter microbial assemblage composition, and indicate the need for investigation into seasonal and temporal dynamics of leaf litter microbial assemblage succession.  相似文献   

2.
Patterns and Processes of Microbial Community Assembly   总被引:1,自引:0,他引:1  

SUMMARY

Recent research has expanded our understanding of microbial community assembly. However, the field of community ecology is inaccessible to many microbial ecologists because of inconsistent and often confusing terminology as well as unnecessarily polarizing debates. Thus, we review recent literature on microbial community assembly, using the framework of Vellend (Q. Rev. Biol. 85:183–206, 2010) in an effort to synthesize and unify these contributions. We begin by discussing patterns in microbial biogeography and then describe four basic processes (diversification, dispersal, selection, and drift) that contribute to community assembly. We also discuss different combinations of these processes and where and when they may be most important for shaping microbial communities. The spatial and temporal scales of microbial community assembly are also discussed in relation to assembly processes. Throughout this review paper, we highlight differences between microbes and macroorganisms and generate hypotheses describing how these differences may be important for community assembly. We end by discussing the implications of microbial assembly processes for ecosystem function and biodiversity.  相似文献   

3.
Here, we describe the metagenome and functional composition of a microbial community in a historically metal-contaminated tropical freshwater stream sediment. The sediment was collected from the Mina Stream located in the Iron Quadrangle (Brazil), one of the world’s largest mining regions. Environmental DNA was extracted and was sequenced using SOLiD technology, and a total of 7.9 Gbp was produced. A taxonomic profile that was obtained by comparison to the Greengenes database revealed a complex microbial community with a dominance of Proteobacteria and Parvarcheota. Contigs were recruited by bacterial and archaeal genomes, especially Candidatus Nitrospira defluvii and Nitrosopumilus maritimus, and their presence implicated them in the process of N cycling in the Mina Stream sediment (MSS). Functional reconstruction revealed a large, diverse set of genes for ammonium assimilation and ammonification. These processes have been implicated in the maintenance of the N cycle and the health of the sediment. SEED subsystems functional annotation unveiled a high degree of diversity of metal resistance genes, suggesting that the prokaryotic community is adapted to metal contamination. Furthermore, a high metabolic diversity was detected in the MSS, suggesting that the historical arsenic contamination is no longer affecting the prokaryotic community. These results expand the current knowledge of the microbial taxonomic and functional composition of tropical metal-contaminated freshwater sediments.  相似文献   

4.
Studies were conducted to examine interrelationships between the heterotrophic and phototrophic populations within an epilithic community in the outlet stream of a high alpine lake. Levels of nitrates, phosphates, and total organic compounds in the lake were consistently near the lower limits of detectability. Microscopic examination of the community by phase-contrast light microscopy and scanning electron microscopy revealed diatoms, filamentous algae, and bacteria embedded within a dense gelatinous matrix. Chlorophyll a and primary productivity measurements had peak values in early August, with subsequent declines. Bacterial heterotrophic activity, as measured by Vmax, turnover rate, and relative activity, increased significantly as the phototrophic community declined. This trend in heterotrophic activity was not accompanied by an increase in total bacterial numbers as determined by epi-illuminated fluorescence microscopy. These results suggest that the phototrophic community responded to changes in, or interactions among, various chemical and physical factors throughout the study period. The catabolic activity of the sessile bacteria appeared to be positively influenced by changes in the mat environment resulting from the decline of the phototrophic populations.  相似文献   

5.
Ammonia oxidation is performed by both ammonia-oxidizing bacteria (AOB) and ammonia-oxidizing archaea (AOA). To explore the effect of ammonia concentration on the population dynamic changes of ammonia-oxidizing microorganisms, we examined changes in the abundance and community composition of AOA and AOB in different layers. Most of the archaeal amoA sequences were Nitrosotalea-related and the proportion that Nitrosotalea cluster occupied decreased in the surface layer and increased in the deep layer during the cultivation process. Nitrosopumilus-related sequences were only detected in the deep layer in the first stage and disappeared later. Both phylogenetic and quantitative analysis showed that there were increased Nitrosomonas-related sequences appeared in the surface layer where the ammonia concentration was the highest. Both AOA and AOB OTU numbers in different layers decreased under selective pressure and then recovered. The potential nitrification rates were 25.06 μg·N·L(-1)·g(-1) dry soil·h(-1) in the mid layer which was higher than the other two layers. In general, obvious population dynamic changes were found for both AOA and AOB under the selective pressure of exogenous ammonia and the changes were different in three layers of the soil column.  相似文献   

6.
Microbially induced concrete corrosion (MICC) in sewer systems has been a serious problem for a long time. A better understanding of the succession of microbial community members responsible for the production of sulfuric acid is essential for the efficient control of MICC. In this study, the succession of sulfur-oxidizing bacteria (SOB) in the bacterial community on corroding concrete in a sewer system in situ was investigated over 1 year by culture-independent 16S rRNA gene-based molecular techniques. Results revealed that at least six phylotypes of SOB species were involved in the MICC process, and the predominant SOB species shifted in the following order: Thiothrix sp., Thiobacillus plumbophilus, Thiomonas intermedia, Halothiobacillus neapolitanus, Acidiphilium acidophilum, and Acidithiobacillus thiooxidans. A. thiooxidans, a hyperacidophilic SOB, was the most dominant (accounting for 70% of EUB338-mixed probe-hybridized cells) in the heavily corroded concrete after 1 year. This succession of SOB species could be dependent on the pH of the concrete surface as well as on trophic properties (e.g., autotrophic or mixotrophic) and on the ability of the SOB to utilize different sulfur compounds (e.g., H2S, S0, and S2O32−). In addition, diverse heterotrophic bacterial species (e.g., halo-tolerant, neutrophilic, and acidophilic bacteria) were associated with these SOB. The microbial succession of these microorganisms was involved in the colonization of the concrete and the production of sulfuric acid. Furthermore, the vertical distribution of microbial community members revealed that A. thiooxidans was the most dominant throughout the heavily corroded concrete (gypsum) layer and that A. thiooxidans was most abundant at the highest surface (1.5-mm) layer and decreased logarithmically with depth because of oxygen and H2S transport limitations. This suggested that the production of sulfuric acid by A. thiooxidans occurred mainly on the concrete surface and the sulfuric acid produced penetrated through the corroded concrete layer and reacted with the sound concrete below.  相似文献   

7.
复合微生物菌剂在剩余污泥堆肥中的作用研究   总被引:1,自引:0,他引:1  
应用复合微生物菌剂对剩余污泥进行堆肥试验,较系统地研究了复合微生物菌剂在剩余污泥堆肥系统中的作用。结果表明:接种复合微生物菌剂进行剩余污泥堆肥,与对照组相比,不但能够提高堆肥温度,而且高温持续时间长,堆肥反应速率加快,腐熟时间缩短,当接种量为7%(体积比)时,腐熟时间比对照组提前了12 d。  相似文献   

8.
Microorganisms will be an integral part of biologically based waste processing systems used for water purification or nutrient recycling on long-term space missions planned by the National Aeronautics and Space Administration. In this study, the function and stability of microbial inocula of different diversities were evaluated after inoculation into plant-based waste processing systems. The microbial inocula were from a constructed community of plant rhizosphere-associated bacteria and a complexity gradient of communities derived from industrial wastewater treatment plant-activated sludge. Community stability and community function were defined as the ability of the community to resist invasion by a competitor (Pseudomonas fluorescens 5RL) and the ability to degrade surfactant, respectively. Carbon source utilization was evaluated by measuring surfactant degradation and through Biolog and BD oxygen biosensor community level physiological profiling. Community profiles were obtained from a 16S–23S rDNA intergenic spacer region array. A wastewater treatment plant-derived community with the greatest species richness was the least susceptible to invasion and was able to degrade surfactant to a greater extent than the other complexity gradient communities. All communities resisted invasion by a competitor to a greater extent than the plant rhizosphere isolate constructed community. However, the constructed community degraded surfactant to a greater extent than any of the other communities and utilized the same number of carbon sources as many of the other communities. These results demonstrate that community function (carbon source utilization) and community stability (resistance to invasion) are a function of the structural composition of the community irrespective of species richness or functional richness.  相似文献   

9.
Understanding the impacts of leaks from geologic carbon sequestration, also known as carbon capture and storage, is key to developing effective strategies for carbon dioxide (CO2) emissions management and mitigation of potential negative effects. Here, we provide the first report on the potential effects of leaks from carbon capture and storage sites on microbial functional groups in surface and near-surface soils. Using a simulated subsurface CO2 storage leak scenario, we demonstrate how CO2 flow upward through the soil column altered both the abundance (DNA) and activity (mRNA) of microbial functional groups mediating carbon and nitrogen transformations. These microbial responses were found to be seasonally dependent and correlated to shifts in atmospheric conditions. While both DNA and mRNA levels were affected by elevated CO2, they did not react equally, suggesting two separate mechanisms for soil microbial community response to high CO2 levels. The results did not always agree with previous studies on elevated atmospheric (rather than subsurface) CO2 using FACE (Free-Air CO2 Enrichment) systems, suggesting that microbial community response to CO2 seepage from the subsurface might differ from its response to atmospheric CO2 increases.  相似文献   

10.
Cryptosporidium parvum oocysts accumulate on biofilm surfaces. The percentage of oocysts attached to biofilms remained nearly constant while oocysts were supplied to the system but decreased to a new steady-state level once oocysts were removed from the feed. More oocysts attached to summer biofilm cultures than winter biofilm cultures.Cryptosporidium causes a potentially life-threatening gastrointestinal disease. Because conventional water treatment may not effectively target Cryptosporidium, source water monitoring and protection are important to avoid infection outbreaks.Biofilms can accumulate pathogens at densities that are much higher than water column densities, with the potential for pathogen release long after entrapment (5, 13, 15, 19). Biofilms have been identified as a drinking water contamination source (7), causing infections for which the source cannot be identified (4, 6).Several previous studies examined pathogen transport in biofilms using Cryptosporidium parvum oocysts (2, 6, 15, 16) or beads as pathogen surrogates (3, 5, 11, 12). The former studies did not use natural microbial assemblages (2, 16) or quantify oocyst attachment or sloughing (6, 15). The current study provides novel information about C. parvum oocyst attachment to environmental biofilms, including a mass balance analysis to identify the daily number of oocysts that (i) remained in the flowing water or were sloughed from the biofilm and (ii) were attached to the biofilm. We imaged biofilms using scanning confocal laser microscopy, as used in other studies (9, 17, 20, 21), to identify spatial patterns of oocyst attachment.Biofilms were scraped from rocks found in Monocacy Creek (Bethlehem, PA) into 1 liter of creek water in January 2007 (winter biofilm culture) and July 2008 (summer biofilm culture). The biofilm suspension was vacuum filtered through a 6-μm cellulose filter. The filtrate was centrifuged (1,754 × g for 15 min), and the resulting biofilm pellet was resuspended in 1 ml of raw creek water. The cell concentration was quantified by DAPI (4′,6-diamidino-2-phenylindole) staining (14). Cells were split into aliquots (5 × 106 cells each) and stored at −80°C in cryovials containing 30% glycerol.Single-channel flow chambers (length by width by height, 24 mm by 8 mm by 4 mm) with glass coverslips (Stovall Life Science, Inc., Greensboro, NC) were inoculated with 5 × 106 biofilm cells for 24 h before the flow was started. Filter-sterilized creek water was used as the flow medium. A 12-channel peristaltic pump (Ismatec, Glattbrugg, Switzerland) maintained a constant flow of 0.2 mm/s (1).For biofilm imaging, the following two setups were used: (i) 1 × 104 C. parvum oocysts (Iowa isolate; Waterborne, Inc., New Orleans, LA) (all oocysts were used within 3 weeks of shedding) in the influent each day for 3 days and (ii) 3 × 104 C. parvum oocysts added to the influent for the last 24 h of a 3-day flow experiment. Biofilms were imaged with a Zeiss LSM 510 META laser scanning microscope, using an argon laser (458-nm, 477-nm, 488-nm, and 514-nm excitation wavelengths) and a HeNe1 laser (543-nm excitation wavelength). Biofilms were fixed with methanol, blocked using a 1:10 dilution of fetal bovine serum, and stained with 20 μM SYTO 9 (Invitrogen, Molecular Probes, Eugene, OR) (16). C. parvum oocysts in the biofilm were stained with a Cy3-conjugated monoclonal antibody solution specific for Cryptosporidium (Waterborne, Inc.) (16).For the mass balance analysis, C. parvum oocysts (1 × 104 per day for 3 days) were added to 500 ml constantly stirred influent water to keep oocysts in suspension. Influent water was replaced each day. Experiments to quantify sloughing included 2 or 5 additional days with oocyst-free feed water, for a total of 5 or 8 days. Biofilms used for the 3- and 5-day experiments were grown with the winter biofilm culture; biofilms used for the 8-day experiments were grown with the summer biofilm culture.After each 24-hour period, the remaining influent and effluent waters were processed by membrane filtration (MF) and immunomagnetic separation (IMS) to recover the oocysts. On the last day of each experiment, biofilms were scraped from the flow chambers, resuspended in sterile creek water, and also processed by MF and IMS. MF was performed according to the method of Oda et al. (10), using the 3-μm filter only. IMS was performed on the filtrate using the Aureon IMS kit (ImmTech, Inc., New Windsor, MD), and oocysts were dissociated from the magnetic beads with 0.05 M HCl. IMS products were counted by hemocytometry and corrected for MF and IMS processing losses. An average IMS recovery of 65% ± 4.2% standard error (SE) (determined by four trials using 1 × 104 oocysts in deionized water) was used. MF recoveries were consistent within each day but varied between days. Therefore, an MF recovery control was performed each day using 1 × 104 oocysts in 1 liter deionized water to obtain a daily MF correction factor.The mass balance analysis demonstrated that these methods were effective for tracking oocysts throughout the flow system for the experiment''s duration, accounting for all the oocysts within 8% (Table (Table1).1). In a control flow chamber with no biofilm growth (i.e., a clean glass surface), oocyst loss within the system was 1% or less, indicating that very few oocysts attached to any abiotic surface within the flow system. Laboratory biofilms composed of natural microbial assemblages were successfully created, although grazing impacts that would affect biofilm dynamics in the environment were eliminated. The thicknesses of laboratory biofilms (average thickness, 39.6 μm; SD, 4.7 μm; n = 16) were not statistically different (P of 0.17 by independent t test) than those of natural biofilms in Monocacy Creek (average thickness, 35.8 μm; SD, 10.2 μm; n = 36).

TABLE 1.

Mass balance analysis of biofilms grown for 3, 5, and 8 days, with 3-day oocyst dosinga
Biofilm growthNo. of oocysts ± % SE
% of oocysts ± % SE
Avg biofilm thickness ± SE (μm)
InfluentEffluentBiofilmbIn biofilm at end of oocyst dosing (day 3)In biofilm at end of experimentcAccounted for in system
Day 3 (n = 3)1.5 × 104 ± 1.88.6 × 103 ± 9.36.4 × 103 ± 7.143 ± 5.643 ± 5.6100 ± 1.931 ± 6.1
Day 5 (n = 2)1.9 × 104 ± 2.41.8 × 104 ± 3.53.2 × 103 ± 5.340 ± 4.54.8 ± 2.1108 ± 1.037 ± 3.8
Day 8 (n = 2)2.0 × 104 ± 3.11.5 × 104 ± 2.97.6 × 103 ± 1.864 ± 5.028 ± 0.2107 ± 0.942 ± 3.6
Open in a separate windowaData from two or three replicate experiments are presented.bData determined from direct hemacytometer counts of scraped biofilm at the end of the experiment.cCalculated from influent and effluent data [(influent − effluent)/influent].Oocyst attachment location within the biofilm is important for transport dynamics. Oocyst attachment at the biofilm surface may be followed by (i) no transport into the biofilm depth, (ii) burial by biofilm overgrowth, or (iii) transport into the biofilm depth through water channels. In these experiments, oocysts attached to the biofilm surface and were not observed to move to depths or be buried by biofilm overgrowth (Fig. (Fig.1).1). In the 28 biofilms examined, no difference in oocyst attachment location was seen whether oocysts were present in the flow for the entire study duration (n = 14) or whether oocysts were added to the flow on the last study day (n = 14).Open in a separate windowFIG. 1.Top-down projection (A) and cross-sectional view (B) of a summer biofilm culture, with C. parvum oocysts attached at the biofilm surface. Biofilm cells are stained green with SYTO 9; oocysts are stained red with Cy3. The white line in panel A indicates the location of the cross section shown in panel B. Direction of water flow is from right to left. The biofilm is approximately 24-μm thick; oocysts are located 16 μm above the biofilm base.Previous studies (11, 12) also reported that particle attachment and detachment occurred at the biofilm surface. The inner biofilm was denser, with less pore space, while the biofilm surface had more water channels, providing more surface area for particle attachment. The mean pore size in a variety of biofilms was reported as 1.7 to 2.7 μm at the water surface and 0.3 to 0.4 μm at the substrate surface (11), which would restrict larger particle movement, including oocysts (4 to 7 μm).Oocysts became attached to biofilms and rapidly reached a steady state (Fig. (Fig.2),2), as seen in other studies (5, 6). The percentage of oocysts attached to the biofilm remained nearly constant while oocysts were supplied to the system. Once the oocyst supply was removed, the percentage of oocysts in the biofilm decreased to a new steady state. For winter biofilm cultures, the cumulative percentage of oocysts attached to the biofilm at day 3 (i.e., the end of the dosing period; average, 40.0%; SD, 25%; n = 2) was statistically higher (P of 0.003 by independent t test) than the cumulative percentage of oocysts attached to the biofilm at day 5 (average, 4.8%; SD, 1.4%; n = 2). For the summer biofilm cultures, the cumulative percentage of oocysts attached to the biofilm at day 3 (average, 63.7%; SD, 4.5%; n = 2) was also statistically higher (P of 0.01) than the cumulative percentage of oocysts attached to the biofilm at day 5 (average, 33.5%; SD, 1.1%; n = 2). The oocysts that remained in the biofilm at day 5 likely attached to more-stable or sheltered portions of the biofilm that did not slough.Open in a separate windowFIG. 2.Cumulative percentage of oocysts (±SE; n = 2) associated with the biofilm. The cumulative number of oocysts in the biofilm each day was calculated by adding the daily differences between the number of oocysts in the effluent and influent. This number was converted to a percentage by dividing by the cumulative number of influent oocysts. The biofilm accumulation on the last day was determined from the oocysts collected and counted directly from the biofilm, which agreed with the number calculated using the above-described method. Time zero indicates when the flow began; biofilm growth began 24 h earlier by seeding with microbial concentrate at zero flow. The solid black line on the x axis indicates the period of oocyst addition to the inflow. Error bars are smaller than symbols where not visible.The cumulative percentage of oocysts attached to summer biofilm cultures was statistically higher (P of 0.02 and 0.002 at days 3 and 5, respectively, by independent t test) than the cumulative percentage of oocysts attached to the winter biofilm cultures (Fig. (Fig.2).2). In addition, the thickness of summer biofilm cultures (average thickness, 42.1 μm; SD, 4.2 μm; n = 8) was statistically higher (P of 0.03 by independent t test) than that of winter biofilm cultures (average, 37.0 μm; SD, 3.9 μm; n = 8). However, it is unlikely that biofilm thickness explains the increased oocyst attachment to summer biofilm cultures, because all oocysts were observed to attach at the biofilm surface and no oocysts were ever observed within biofilm depths. These observations are in agreement with those of other studies (3, 8, 16) and suggest that other biofilm characteristics (e.g., surface roughness or pore size) may (i) be more important than biofilm thickness for oocyst attachment and (ii) vary with seasonal differences in water chemistry or microbial community caused by water quality differences, such as temperature, pH, or dissolved organic carbon (16).Biofilms are significant reservoirs for oocysts compared to abiotic surfaces (5, 12, 15, 16). Oocysts that remain in the biofilm have important public health implications because they may persist in the biofilm and eventually be released, resulting in potential human exposure.These results confirm that C. parvum oocysts quickly attach to natural microbial biofilms and can be released into the flowing water over time. Oocyst attachment and release dynamics are important for assessing and potentially reducing the risk of human exposure and infection. Although this study used natural stream biofilms, these transport dynamics have important implications for the drinking water industry. Biofilms in the raw water source, represented here by stream biofilms, are linked to drinking water intakes, where any disturbance event can affect water quality. For this reason, a better understanding of the environmental transport of oocysts is important for tracking oocyst contamination, which ultimately affects the drinking water industry. Further investigation is necessary to understand the differences between the summer and winter biofilm cultures as well as the pathogen reservoir that forms in the biofilm.  相似文献   

11.
The structure and dynamics of small eukaryotes (cells with a diameter less than 5 μm) were studied over two consecutive years in an oligomesotrophic lake (Lake Pavin in France). Water samples were collected at 5 and 30 m below the surface; when the lake was stratified, these depths corresponded to the epilimnion and hypolimnion. Changes in small-eukaryote structure were analyzed using terminal restriction fragment length polymorphism (T-RFLP) and cloning and sequencing of the 18S rRNA genes. Terminal restriction fragments from clones were used to reveal the dominant taxa in T-RFLP profiles of the environmental samples. Spumella-like cells (Chrysophyceae) did not dominate the small eukaryote community identified by molecular techniques in lacustrine ecosystems. Small eukaryotes appeared to be dominated by heterotrophic cells, particularly Cercozoa, which represented nearly half of the identified phylotypes, followed by the Fungi-LKM11 group (25%), choanoflagellates (10.3%) and Chrysophyceae (8.9%). Bicosoecida, Cryptophyta, and ciliates represented less than 9% of the community studied. No seasonal reproducibility in temporal evolution of the small-eukaryote community was observed from 1 year to the next. The T-RFLP patterns were related to bottom-up (resources) and top-down (grazing) variables using canonical correspondence analysis. The results showed a strong top-down regulation of small eukaryotes by zooplankton, more exactly, by cladocerans at 5 m and copepods at 30 m. Among bottom-up factors, temperature had a significant effect at both depths. The concentrations of nitrogenous nutrients and total phosphorus also had an effect on small-eukaryote dynamics at 5 m, whereas bacterial abundance and dissolved oxygen played a more important structuring role in the deeper zone.  相似文献   

12.
Human-associated bacteria dominate the built environment (BE). Following decontamination of floors, toilet seats, and soap dispensers in four public restrooms, in situ bacterial communities were characterized hourly, daily, and weekly to determine their successional ecology. The viability of cultivable bacteria, following the removal of dispersal agents (humans), was also assessed hourly. A late-successional community developed within 5 to 8 h on restroom floors and showed remarkable stability over weeks to months. Despite late-successional dominance by skin- and outdoor-associated bacteria, the most ubiquitous organisms were predominantly gut-associated taxa, which persisted following exclusion of humans. Staphylococcus represented the majority of the cultivable community, even after several hours of human exclusion. Methicillin-resistant Staphylococcus aureus (MRSA)-associated virulence genes were found on floors but were not present in assembled Staphylococcus pan-genomes. Viral abundances, which were predominantly enterophages, human papilloma virus, and herpesviruses, were significantly correlated with bacterial abundances and showed an unexpectedly low virus-to-bacterium ratio in surface-associated samples, suggesting that bacterial hosts are mostly dormant on BE surfaces.  相似文献   

13.
Lake Lanier is an important freshwater lake for the southeast United States, as it represents the main source of drinking water for the Atlanta metropolitan area and is popular for recreational activities. Temperate freshwater lakes such as Lake Lanier are underrepresented among the growing number of environmental metagenomic data sets, and little is known about how functional gene content in freshwater communities relates to that of other ecosystems. To better characterize the gene content and variability of this freshwater planktonic microbial community, we sequenced several samples obtained around a strong summer storm event and during the fall water mixing using a random whole-genome shotgun (WGS) approach. Comparative metagenomics revealed that the gene content was relatively stable over time and more related to that of another freshwater lake and the surface ocean than to soil. However, the phylogenetic diversity of Lake Lanier communities was distinct from that of soil and marine communities. We identified several important genomic adaptations that account for these findings, such as the use of potassium (as opposed to sodium) osmoregulators by freshwater organisms and differences in the community average genome size. We show that the lake community is predominantly composed of sequence-discrete populations and describe a simple method to assess community complexity based on population richness and evenness and to determine the sequencing effort required to cover diversity in a sample. This study provides the first comprehensive analysis of the genetic diversity and metabolic potential of a temperate planktonic freshwater community and advances approaches for comparative metagenomics.  相似文献   

14.
The effects of antibiotics on aerobic composting are investigated by dosing of tetracycline (TC) in fresh human feces with sawdust as biomass carrier. Variability in process parameters such as temperature, pH, water-soluble carbon, germination index (GI) and dehydrogenase activity (DHA) are evaluated at TC dosages of 0, 100, 250 and 500 mg/kg in a 21-day composting. Moreover, microbial community succession is examined by high-throughput 16S rRNA gene sequencing. Findings indicate significant impacts to the process parameters with the increase of TC concentration such as inhibition of temperature increases during aerobic composting, lowering of pH, increasing of water-soluble carbon residue, a decrease of GI, and hindering of DHA. Furthermore, elevated TC concentrations significantly alter the microbial community succession and reduce the community diversity and abundance. Therefore, interference in microbial community structures and a hindrance to biological activity are believed to be the main adverse effects of TC on the composting process and maturity of the composting products.  相似文献   

15.
A semi-continuous four-channel colon simulator was used to study the effects of lactose for the first time on the growth and fermentation dynamics of colonic microbiota. In six separate simulations, lactose supplementation increased the total SCFA concentration by 3–5 fold as compared with the baseline in the respective vessels. The total bacterial density was inversely correlated with lactic acid production (P=0.003), while production of butyrate (P=0.007) and propionate (P=0.02) correlated with higher numbers of bacteria. A major shift in the microbial community structure in the lactose supplemented vessels was demonstrated by bacterial genomic %G+C-profiling of the total population, where lactose supplementation induced a clearly dominant peak in the bifidobacteria prominent area, %G+C 60–65. The transient shift to increased numbers of bifidobacteria (23–27%) of all bacteria in the first two vessels was also confirmed by the bifidobacteria-specific QPCR-method. In conclusion, lactose produced dramatic changes in microbiota composition and activity as compared with the baseline fermentation.  相似文献   

16.
Bioaugmentation of bioreactors focuses on the removal of xenobiotics, with little attention typically paid to the recovery of disrupted reactor functions such as ammonium-nitrogen removal. Chloroanilines are widely used in industry as a precursor to a variety of products and are occasionally released into wastewater streams. This work evaluated the effects on activated-sludge reactor functions of a 3-chloroaniline (3-CA) pulse and bioaugmentation by inoculation with the 3-CA-degrading strain Comamonas testosteroni I2 gfp. Changes in functions such as nitrification, carbon removal, and sludge compaction were studied in relation to the sludge community structure, in particular the nitrifying populations. Denaturing gradient gel electrophoresis (DGGE), real-time PCR, and fluorescent in situ hybridization (FISH) were used to characterize and enumerate the ammonia-oxidizing microbial community immediately after a 3-CA shock load. Two days after the 3-CA shock, ammonium accumulated, and the nitrification activity did not recover over a 12-day period in the nonbioaugmented reactors. In contrast, nitrification in the bioaugmented reactor started to recover on day 4. The DGGE patterns and the FISH and real-time PCR data showed that the ammonia-oxidizing microbial community of the bioaugmented reactor recovered in structure, activity, and abundance, while the number of ribosomes of the ammonia oxidizers in the nonbioaugmented reactor decreased drastically and the community composition changed and did not recover. The settleability of the activated sludge was negatively influenced by the 3-CA addition, with the sludge volume index increasing by a factor of 2.3. Two days after the 3-CA shock in the nonbioaugmented reactor, chemical oxygen demand (COD) removal efficiency decreased by 36% but recovered fully by day 4. In contrast, in the bioaugmented reactor, no decrease of the COD removal efficiency was observed. This study demonstrates that bioaugmentation of wastewater reactors to accelerate the degradation of toxic chlorinated organics such as 3-CA protected the nitrifying bacterial community, thereby allowing faster recovery from toxic shocks.  相似文献   

17.
The Nyack floodplain is located on the Middle Fork of the Flathead River, an unregulated, pristine, fifth-order stream in Montana, USA, bordering Glacier National Park. The hyporheic zone is a nutritionally heterogeneous floodplain component harboring a diverse array of microbial assemblages essential in fluvial biogeochemical cycling, riverine ecosystem productivity, and trophic interactions. Despite these functions, microbial community structure in pristine hyporheic systems is not well characterized. The current study was designed to assess whether physical habitat heterogeneity within the hyporheic zone of the Nyack floodplain was sufficient to drive bacterial β diversity between three different hyporheic flow path locations. Habitat heterogeneity was assessed by measuring soluble reactive phosphorous, nitrate, dissolved organic carbon, dissolved oxygen, and soluble total nitrogen levels seasonally at surface water infiltration, advection, and exfiltration zones. Significant spatial differences were detected in dissolved oxygen and nitrate levels, and seasonal differences were detected in dissolved oxygen, nitrate, and dissolved organic carbon levels. Denaturing gradient gel electrophoresis (DGGE) and cell counts indicated that bacterial diversity increased with abundance, and DGGE fingerprints covaried with nitrate levels where water infiltrated the hyporheic zone. The ribosomal gene phylogeny revealed that hyporheic habitat heterogeneity was sufficient to drive β diversity between bacterial assemblages. Phylogenetic (P) tests detected sequence disparity between the flow path locations. Small distinct lineages of Firmicutes, Actinomycetes, Planctomycetes, and Acidobacteria defined the infiltration zone and α- and β-proteobacterial lineages delineated the exfiltration and advection zone communities. These data suggest that spatial habitat heterogeneity drives hyporheic microbial community development and that attempts to understand functional differences between bacteria inhabiting nutritionally heterogeneous hyporheic environments might begin by focusing on the biology of these taxa.  相似文献   

18.
Soil microbial communities mediate critical ecosystem carbon and nutrient cycles. How microbial communities will respond to changes in vegetation and climate, however, are not well understood. We reciprocally transplanted soil cores from under oak canopies and adjacent open grasslands in a California oak–grassland ecosystem to determine how microbial communities respond to changes in the soil environment and the potential consequences for the cycling of carbon. Every 3 months for up to 2 years, we monitored microbial community composition using phospholipid fatty acid analysis (PLFA), microbial biomass, respiration rates, microbial enzyme activities, and the activity of microbial groups by quantifying 13C uptake from a universal substrate (pyruvate) into PLFA biomarkers. Soil in the open grassland experienced higher maximum temperatures and lower soil water content than soil under the oak canopies. Soil microbial communities in soil under oak canopies were more sensitive to environmental change than those in adjacent soil from the open grassland. Oak canopy soil communities changed rapidly when cores were transplanted into the open grassland soil environment, but grassland soil communities did not change when transplanted into the oak canopy environment. Similarly, microbial biomass, enzyme activities, and microbial respiration decreased when microbial communities were transplanted from the oak canopy soils to the grassland environment, but not when the grassland communities were transplanted to the oak canopy environment. These data support the hypothesis that microbial community composition and function is altered when microbes are exposed to new extremes in environmental conditions; that is, environmental conditions outside of their “life history” envelopes.  相似文献   

19.
To explore how microbial community composition and function varies within a coral reef ecosystem, we performed metagenomic sequencing of seawater from four niches across Heron Island Reef, within the Great Barrier Reef. Metagenomes were sequenced from seawater samples associated with (1) the surface of the coral species Acropora palifera, (2) the surface of the coral species Acropora aspera, (3) the sandy substrate within the reef lagoon and (4) open water, outside of the reef crest. Microbial composition and metabolic function differed substantially between the four niches. The taxonomic profile showed a clear shift from an oligotroph-dominated community (e.g. SAR11, Prochlorococcus, Synechococcus) in the open water and sandy substrate niches, to a community characterised by an increased frequency of copiotrophic bacteria (e.g. Vibrio, Pseudoalteromonas, Alteromonas) in the coral seawater niches. The metabolic potential of the four microbial assemblages also displayed significant differences, with the open water and sandy substrate niches dominated by genes associated with core house-keeping processes such as amino acid, carbohydrate and protein metabolism as well as DNA and RNA synthesis and metabolism. In contrast, the coral surface seawater metagenomes had an enhanced frequency of genes associated with dynamic processes including motility and chemotaxis, regulation and cell signalling. These findings demonstrate that the composition and function of microbial communities are highly variable between niches within coral reef ecosystems and that coral reefs host heterogeneous microbial communities that are likely shaped by habitat structure, presence of animal hosts and local biogeochemical conditions.  相似文献   

20.
The influence of the stem on delivery of Ca Sr to the plant top was studied by noting the extent to which the stem interfered with through passage of these elements. Tagged Ca Sr solutions were forced through bean stem sections, and solute which completed passage to the exudate was considered indicative of the nutrition normally available to the plant top. Tests were conducted over two widely different xylem stream flow rates, and with or without the addition of dinitrophenol to the source solution. Approximately identical amounts of cation were introduced into the stem for all test situations. In all cases, the stem retained the bulk of introduced cation and allowed only a fraction (ca 25 percent) to complete passage to the exudate. Within this pattern, less stem retention and greater through passage occurred at the high (versus the low) stream flow rate, and also where dinitrophenol was present in the source solution. In all cases, the stem preferentially retained Sr over Ca so that the exudate was relatively dilute in Sr. Such discrimination was less at the high (versus the low) stream flow rate. It was enhanced by the presence of dinitrophenol.  相似文献   

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