Microbial community succession and bacterial diversity in soils during 77,000 years of ecosystem development

The origins of the biological complexity and the factors that regulate the development of community composition, diversity and richness in soil remain largely unknown. To gain a better understanding of how bacterial communities change during soil ecosystem development, their composition and diversity in soils that developed over c. 77 000 years of intermittent aeolian deposition were studied. 16S rRNA gene clone libraries and fatty acid methyl ester (FAME) analyses were used to assess the diversity and composition of the communities. The bacterial community composition changed with soil age, and the overall diversity, richness and evenness of the communities increased as the soil habitat matured. When analysed using a multivariate Bray-Curtis ordination technique, the distribution of ribotypes showed an orderly pattern of bacterial community development that was clearly associated with soil and ecosystem development. Similarly, changes in the composition of the FAMEs across the chronosequence were associated with biomarkers for fungi, actinomycetes and Gram-positive bacteria. The development of the soil ecosystem promoted the development of distinctive microbial communities that were reminiscent of successional processes often evoked to describe change during the development of plant communities in terrestrial ecosystems.     

大兴安岭落叶松林不同演替阶段土壤细菌群落结构与功能潜势

采用土壤细菌16S rDNA高通量测序方法研究了大兴安岭汗马自然保护区落叶松林不同演替阶段的土壤细菌群落结构和功能.结果表明: 不同演替阶段落叶松林土壤细菌优势门为变形菌门、酸杆菌门、疣微菌门、拟杆菌门、放线菌门、浮霉菌门和绿弯菌门,随着演替的进行,酸杆菌门相对丰度逐渐增加,绿弯菌门相对丰度逐渐减少,优势门相对丰度在不同演替阶段不同.细菌群落α多样性在不同演替阶段间无显著差异,但其群落结构分别在落叶松幼龄林与中龄林、幼龄林与过熟林、近熟林与成熟林之间存在显著差异.土壤氧化还原电位、土壤pH和有效磷是影响细菌群落结构的主要环境因素,其中土壤氧化还原电位对微生物群落结构影响最大.随着演替的进行,细菌参与的固氮作用、反硝化作用、氨氧化作用、木质素降解作用呈逐渐减弱的趋势,硫酸盐异化还原作用呈先降后升的趋势,碳固定作用呈先升后降的趋势,碱性磷酸酶没有明显的变化规律,影响土壤功能的主要因素有土壤有效磷和氧化还原电位等.     

Soil parent material is a key determinant of the bacterial community structure in arable soils

The bacterial community composition in soil and rhizosphere taken from arable field sites, differing in soil parent material and soil texture, was analyzed using terminal restriction fragment length polymorphism (T-RFLP) of 16S rRNA genes. Nine sandy to silty soils from North-East Germany could clearly be distinguished from each other, with a relatively low heterogeneity in the community structure within the field replicates. There was a relationship between the soil parent material, i.e. different glacial and aeolian sediments, and the clustering of the profiles from different sites. A site-specific grouping of T-RFLP profiles was also found for the rhizosphere samples of the same field sites that were planted with potatoes. The branching of the rhizosphere profiles corresponded partly with the soil parent material, whereas the effect of the plant genotype was negligible. Selected terminal restriction fragments differing in their relative abundance within the nine soils were analyzed based on the cloning of the 16S rRNA genes of one soil sample. A high phylogenetic diversity observed to include Acidobacteria, Betaproteobacteria, Bacteroidetes, Verrucomicrobia, and Gemmatimonadetes. The assignment of three out of the seven selected terminal restriction fragments to members of Acidobacteria suggested that this group seems to participate frequently in the shifting of community structures that result from soil property changes.     

石油污染对土壤微生物群落多样性的影响

土壤中的微生物主要有细菌、放线菌、真菌三大类群,微生物在石油污染的土壤中发挥着维持生态平衡和生物降解的功能。文中以四川省遂宁市射洪县某废弃油井周围不同程度石油污染土壤为供试土壤,首先对各组供试土壤的基本理化性质进行测定分析;然后采用平板菌落计数法测定了供试土壤中三大类微生物数量的变化,结果表明:相比未被污染的对照土壤,石油污染的土壤中细菌、放线菌、真菌数量均减少,并且土壤中可培养微生物的数量与土壤含水量呈正相关;再采用454焦磷酸测序技术对土壤中的细菌群落多样性及变化进行16S rRNA基因分析。在所有供试的4个土壤样品中,共鉴定出不少于23 982个有效读取序列和6 123种微生物,相比于未被污染的对照土壤,石油污染土壤中细菌的种类更加丰富,主要优势门类为酸杆菌门、放线菌门、拟杆菌门、绿弯菌门、浮霉菌门和变形菌门。但不同土壤样品中优势菌群的群落结构有所差异,石油污染的土壤中,酸杆菌门、放线菌门和变形菌门的数量最多,未被石油污染的土壤中,放线菌门、拟杆菌门和变形菌门的数量最多。     

Dynamics of bacterial community succession in a salt marsh chronosequence: evidences for temporal niche partitioning

The mechanisms underlying community assembly and promoting temporal succession are often overlooked in microbial ecology. Here, we studied an undisturbed salt marsh chronosequence, spanning over a century of ecosystem development, to understand bacterial succession in soil. We used 16S rRNA gene-based quantitative PCR to determine bacterial abundance and multitag 454 pyrosequencing for community composition and diversity analyses. Despite 10-fold lower 16S rRNA gene abundances, the initial stages of soil development held higher phylogenetic diversities than the soil at late succession. Temporal variations in phylogenetic β-diversity were greater at initial stages of soil development, possibly as a result of the great dynamism imposed by the daily influence of the tide, promoting high immigration rates. Allogenic succession of bacterial communities was mostly driven by shifts in the soil physical structure, as well as variations in pH and salinity, which collectively explained 84.5% of the variation concerning community assemblage. The community assembly data for each successional stage were integrated into a network co-occurrence analysis, revealing higher complexity at initial stages, coinciding with great dynamism in turnover and environmental variability. Contrary to a spatial niche-based perspective of bacterial community assembly, we suggest temporal niche partitioning as the dominant mechanism of assembly (promoting more phylotype co-occurrence) in the initial stages of succession, where continuous environmental change results in the existence of multiple niches over short periods of time.     

Diversity of bacterial community in freshwater of Woopo wetland

Diversity of bacterial community in water layer of Woopo wetland was investigated. Cultivable bacterial strains were isolated by the standard dilution plating technique and culture-independent 16S rRNA gene clones were obtained directly from DNA extracts of a water sample. Amplified rDNA restriction analysis (ARDRA) was applied onto both of the isolates and 16S rRNA gene clones. Rarefaction curves, coverage rate and diversity indices of ARDRA patterns were calculated. Representative isolates and clones of all the single isolate/clone phylotype were partially sequenced and analyzed phylogenetically. Sixty-four and 125 phylotypes were obtained from 203 bacterial isolates and 235 culture-independent 16S rRNA gene clones, respectively. Bacterial isolates were composed of 4 phyla, of which Firmicutes (49.8%) and Actinobacteria (32.0%) were predominant. Isolates were affiliated with 58 species. Culture-independent 16S rRNA gene clones were composed of 8 phyla, of which Proteobacteria (62.2%), Actinobacteria (15.5%), and Bacteroidetes (13.7%) were predominant. Diversity of 16S rRNA gene clones originated from cultivation-independent DNA extracts was higher than that of isolated bacteria.     

Organic matter and nitrogen accumulation and nitrogen fixation during early ecosystem development in Hawaii

We used a chronosequence comprised of 10 y, 52 y and 142 yold `a'a lava flows on Mauna Loa, Hawaii, to determine theaccumulation of organic matter and nitrogen and rates of nitrogenfixation through time. The mass of organic matter (live and deadbiomass and soil organic matter) on the 1984, 1942 and 1852 lavaflows was 0.6, 2.2 and 7.6 kg m^{– 2}, respectively, while total N was 4.8, 10.9 and 85.7 g m^{– 2}.We estimated the total rates of nitrogen fixation for thethree different aged ecosystems using an acetylene reduction assaycalibrated with ¹⁵N incubations. While mean rates of total N fixation remained largely constant across the three sites – between2.0 and 3.1 kg ha^{– 1} y^{– 1} – the most important sources of N fixation changed. On the 10 y flow, the most important fixer was the pioneering cyanolichen, Stereocaulon vulcani. After 52 years ofecosystem development, the most important N fixer was a cyanoalga,while after 142 years, the predominant N fixers were heterotrophicbacteria associated with leaf litter, twigs and detritus. The totalamount of N accumulated after 52 years of ecosystem development wasequivalent to cumulative inputs through biological N fixation. After 142 years, however, cumulative inputs from N fixation couldonly account for between 27–59% of the total nitrogen accrued.We used fertilizer additions of all essential nutrients otherthan N to test whether the availability of lithophilic nutrientsregulated rates of N fixation in early ecosystem development. Ratesof nitrogen fixation by the lichen, S. vulcani, approximately doubled when fertilized on the 1984 and 1942 flows. Rates of N-fixation by heterotrophic nitrogen fixing bacteria on leaf litter ofMetrosideros polymorpha also increased significantly when fertilized with lithophilic nutrients. These findings suggest that weathering rates of lava in part regulate rates of nitrogen fixation in these young ecosystems.     

不同土壤深度对宁夏石嘴山盐碱地细菌菌群多样性的影响

宁夏自治区是我国受到土壤次生盐渍化危害的重点区域,然而对该地区盐碱化形成机制及影响因素的研究资料较少。在宁夏石嘴山地区采集土壤样本,采用基于16S rRNA的PCR-DGGE技术对不同深度土壤的细菌群落多样性和优势种群进行分析,以期从土壤生态角度探索该地盐渍化成因及改良措施。带谱相似性和UPGMA聚类结果表明,表层(D20 cm)土壤和底层(D80 cm)土壤样本中细菌菌群相似程度较高;而中间层(20 cmD80 cm)土壤样本中细菌菌群相似程度很低。多样性指数分析显示,随着地层深度的增加,菌落的丰富度和多样性均趋于下降;而均匀程度变化幅度不大。对其中5个优势条带进行测序比对的结果表明,该地区土壤可识别优势细菌菌群为变形细菌门Proteobacteria和拟杆菌门Bacteroidetes,但大部分条带未可识别。结果表明该地区盐碱土壤中的细菌菌群多样性程度较高,且优势菌群不尽相同;土壤深度与细菌菌落多样性在一定程度上存在线性关系。为深入研究次生盐渍化土壤的形成机制以及影响因素提供理论参考。     

Bacterial community succession in a high‐altitude subarctic glacier foreland is a three‐stage process

Alpine glaciers are retreating rapidly, exposing foreland minerals, which develop into soils. Bacterial communities in glacier forelands exhibit high rates of turnover and undergo dramatic shifts in composition within the first 50 years after deglaciation, followed by relative stabilization and convergence. This period of microbial development occurs simultaneously with plant colonization in most systems; thus, it remains unclear whether the changes in the bacterial communities occur primarily as the result of edaphic, climatic or biotic factors. We examined bacterial community structure along two replicate chronosequences within the glacial foreland of Duke River Glacier, Yukon, Canada. This foreland is estimated to include >200 years of bare soils before an appreciable grassline, likely due to the high latitude and altitude of the glacier. This enabled us to examine bacterial community development prior to plant colonization over a longer period than previous studies. We observed three successional groups in the chronosequence: (i) an ‘early’ group in soils of less than approximately 50 years since deglaciation; (ii) an ‘intermediate’ group within bare soils, after the early period but before the grassline, containing communities with a relatively high degree of variability in composition; and (iii) a ‘grassline’ group in soils collected after plant colonization with higher diversity but lower age‐group variability in community composition. These findings suggest rapid replacement and addition of species better adapted to glacier foreland conditions followed by slower community shifts over the next 150 years and, finally, indications of a possible response to plant colonization.     

Phylogenetic analysis of the succession of bacterial communities in the Great South Bay (Long Island)

Bacterial community composition and succession were examined over the course of the summer season in the Great South Bay, Long Island, NY, USA, using a 16S rDNA clone library approach. There was a progression of changes in dominant species in the libraries during the summer of 1997. The July library had several groups dominant, the SAR407 relatives of the alpha-Proteobacteria (24%) and the SAR86 (18%), sulfur-oxidizing symbiont relatives (8%) of the gamma-Proteobacteria, and unidentified Cytophaga-Flexibacter representatives (22%). In August, the Cytophaga-Flexibacter (Gelidibacter sp. and unidentified Cytophaga-Flexibacter representative) and Cyanobacteria (Synechococcus sp.) increased to 28% and 14%, respectively. High GC Gram-positives appeared at 18%, and beta-Proteobacteria (Ralstonia sp.) at 10%. By September these groups had either declined or were absent, while the SAR86 cluster, Pseudoalteromonas and Alteromonas of the gamma-Proteobacteria were dominant in the community (61%). The dominance of open ocean bacteria along with the presence of Aureococcus anophagefferens (Pelagophyceae) in July suggests possible open ocean coupling to bloom events. Many clones in this study were related to previously described clones from a wide distribution of marine environments, substantiating the cosmopolitan nature of pelagic bacteria. Only one isolated bacterium was closely related to 16S rDNA found in the August library.     

胜利油田单12高温油藏非培养和富集培养样品的细菌组成特性

[目的]通过比较分析油藏样品的微生物群落结构特点,认识油藏微生物的生态功能.[方法]利用3种油藏微生物研究中常用的富集培养方法,对胜利油田单12区块S12-4油井产出水样品进行了选择性富集培养,运用构建16S rRNA基因文库的方法分析了富集样品和非培养样品的细菌多样性.[结果]通过16S rRNA基因序列比对发现,非培养样品、异养菌富集样品、烃降解菌富集样品和硫酸盐还原菌富集样品中的优势菌分别为Pseudomonas属,Thermotoga属,Thermaerobacter属和Thermotoga属的成员.多样性分析结果表明,非培养样品的微生物多样性最丰富,同时非培养样品和富集样品的微生物群落结构存在很大的差异,富集样品中的微生物包括优势菌在油藏原位环境中含量很低.[结论]细菌组成差异的比较结果,对油藏微生物的生态功能研究和微生物驱油潜力评估具有重要意义.     

Current reclamation practices after oil and gas development do not speed up succession or plant community recovery in big sagebrush ecosystems in Wyoming

Reclamation is an application of treatment(s) following disturbance to promote succession and accelerate the return of target conditions. Previous studies have framed reclamation in the context of succession by studying its effectiveness in reestablishing late‐successional plant communities. Reestablishment of plant communities is especially important and challenging in drylands such as shrub steppe ecosystems where succession proceeds slowly. These ecosystems face threats from climate change, invasive species, altered fire regimes, and land‐use change, as well as fossil‐fuel extraction and associated disturbance. As such, the need for effective reclamation after this type of energy development is great. However, past research regarding this type of reclamation has focused on mining rather than oil and gas development. To better understand the effect of reclamation on rates of succession in dryland shrub steppe ecosystems, we sampled oil and gas wellpads and adjacent undisturbed big sagebrush plant communities in Wyoming, U.S.A., and quantified the extent of recovery for forbs, grasses, and shrubs on reclaimed and unreclaimed wellpads relative to undisturbed plant communities. Reclamation increased the recovery rate for early‐successional types, including combined forbs and grasses and perennial grasses, but did not affect recovery rate of late‐successional types, particularly big sagebrush and perennial forbs. Rather, subsequent analyses showed that recovery of late‐successional types was affected by soil texture and time since wellpad abandonment. This is consistent with studies in other ecosystems where reclamation has been implemented, suggesting that reclamation may not help reestablish late‐successional plant communities more quickly than they would reestablish naturally.     

Succession of bacterial community composition over two consecutive years in two aquatic systems: a natural lake and a lake-reservoir

The succession in bacterial community composition was studied over two years in the epilimnion and hypolimnion of two freshwater systems: a natural lake (Pavin Lake) and a lake-reservoir (Sep Reservoir). The bacterial community composition was determined by cloning-sequencing of 16S rRNA and by terminal restriction fragment length polymorphism. Despite large hydrogeological differences, in the Sep Reservoir and Pavin Lake the dominant bacteria were from the same taxonomic divisions, particularly Actinobacteria and Betaproteobacteria. In both ecosystems, these major bacterial divisions showed temporal fluctuations that were much less marked than those occurring at a finer phylogenetic scale. Nutrient availability and mortality factors, the nature of which differed from one lake to another, covaried with the temporal variations in the bacterial community composition at all sampling depths, whereas factors related to seasonal forces (temperature and outflow for Sep Reservoir) seemed to account only for the variation of the hypolimnion bacterial community composition. No seasonal reproducibility in temporal evolution of bacterial community from one year to the next was observed.     

转几丁质酶和葡聚糖酶双价基因棉花对土壤细菌种群多样性的影响

以转几丁质酶和葡聚糖酶双价基因棉花为研究对象,非转基因受体棉花为对照,通过比较可培养细菌数量和基于16S rRNA克隆文库细菌种群分析,评价外源双价基因的导入在苗期、蕾期、花铃期和吐絮期对棉花根际细菌群落多样性的影响。结果表明,可培养细菌的数量不受外源双价基因的影响,随着棉花生育期的交替而变化,以代谢旺盛的花铃期最多。构建的转基因和非转基因不同生育期根际土壤细菌16S rRNA文库容量为2400个克隆,涵盖了细菌的283个属。其中,Acidobacterium是最大优势类群,共包括624个克隆,其次为未知细菌种群和Flavisolibacter。比较转基因和非转基因棉花根际土壤细菌的种群结构,结果显示,同一生育期内前者种群的多样性显著低于后者,二者的共有类群随着生长发育的进行而增多。研究结果说明几丁质酶基因和葡聚糖酶基因对棉花根际细菌种群多样性有着不同程度的削减作用,但是随着种植时间的延长,该差异呈现逐渐缩小的趋势。     

Bacterial Community Structure in a Semi-Arid Haloalkaline Soil Using Culture Independent Method

Bacterial community structures in two physicochemically different soils from the coastal region of Gujarat, India were investigated using PCR, 16S rRNA gene clone libraries and sequencing methods. The aim of the study was to determine the diversity of bacterial communities inhabiting haloalkaline soil from a semi-arid coastal region. The phylogenetic diversity of bacteria in a haloalkaline soil (EC 20 dS/m; pH 9.5) was compared with a normal soil (EC 0.93 dS/m; pH 7.2). Clones representing phyla Proteobacteria, Bacteroidetes, Chloroflexi, Firmicutes, Actinobacteria, Acidobacteria and Planctomycetes were found in both soils. Cyanobacteria, Verrucomicrobia, OP10 and Bacteria incertae sedis were detected in normal soil whereas Nitrospira was found only in haloalkaline soil. The dominant phylum in the haloalkaline soil was Bacteroidetes followed by Proteobacteria whereas normal soil was dominated by Proteobacteria and Actinobacteria. About 82% of the sequences from the haloalkaline library were related to those previously retrieved from various saline, alkaline and oil-natural gas field ecosystems whereas 50% of the sequences from normal soil resembled sequences of bacteria retrieved from agriculture-related habitats viz. agriculture fields, rhizosphere and grasslands. One third of the total sequences from both soil samples showed low BLAST identities (<95%) suggesting that these soils may harbor unique, novel taxa. Further, the correlation analysis revealed negative correlations of Shannon diversity indices and species evenness with salinity (EC) and pH but positive correlations with total carbon and total nitrogen contents of the soil samples. The haloalkaline soil exhibited less bacterial diversity and communities were significantly different from those of normal soil. In this study, the haloalkaline soil from a semi-arid region supports oligotrophic microbes.

Supplemental materials are available for this article. Go to the publisher's online edition of Geomicrobiology Journal to view the supplemental file.     

结合宏基因组末端随机测序和16S rDNA技术分析温室黄瓜根围土壤细菌多样性

土壤细菌在温室土壤环境中具有十分重要的生态功能,与温室作物以及微生物内部存在互作关系。研究土壤细菌的群落结构组成,有助于了解土地利用变化与生态环境效应之间的关系。结合16S rRNA基因克隆文库和宏基因组末端测序对温室黄瓜根围土壤细菌的多样性进行了分析。在16S文库中,根据97%的序列相似性水平划分OTU,共有35个OTU,其中优势菌群是γ-Proteobacteria,其次为Firmicutes,Bacillus为优势细菌。在纲分类水平上,16S文库和宏基因组末端测序结果均包含γ-Proteobacteria、α-Proteobacteria、δ-Proteobacteria、β-Proteobacteria、Actinomycetales和Firmicutes,各纲比例有差别;在优势种群属水平上,末端测序的结果包含的属多于16S文库(4035);在优势细菌种类上,两者反映的结果一致,均为Bacillus。但是,宏基因组末端测序包含了大多数的弱势种群,更能反映细菌多样性的真实水平。与露地土壤细菌16S文库相比较,土壤细菌多样性降低,这可能与温室多年连作,种植蔬菜种类单一直接相关。     

Distinct and diverse anaerobic bacterial communities in boreal lakes dominated by candidate division OD1

Lakes have a central role in the carbon cycle of the boreal landscape. These systems typically stratify in summer and their hypolimnetic microbial communities influence burial of biogenic organic matter in sediments. The composition of bacterial communities in these suboxic habitats was studied by pyrosequencing of 16S rRNA amplicons from five lakes with variable dissolved organic carbon (DOC) concentrations. Bacterioplankton communities in the hypolimnetic waters were clearly different from the surface layer with candidate division OD1, Chlorobi and Bacteroidetes as dominant community members. Several operational taxonomic units (OTUs) affiliated with candidate division OD1 were abundant and consistently present in the suboxic hypolimnion in these boreal lakes. The overall representation of this group was positively correlated with DOC and methane concentrations. Network analysis of time-series data revealed contrasting temporal patterns but suggested similar ecological roles among the abundant OTUs affiliated with candidate division OD1. Together, stable isotope data and taxonomic classification point to methane oxidation and autotrophic denitrification as important processes in the suboxic zone of boreal lakes. Our data revealed that while hypolimnetic bacterial communities are less dynamic, they appear to be more diverse than communities from the oxic surface layer. An appreciable proportion of the hypolimnetic bacteria belong to poorly described phyla.     

Identifying the core microbial community in the gut of fungus‐growing termites

Gut microbes play a crucial role in decomposing lignocellulose to fuel termite societies, with protists in the lower termites and prokaryotes in the higher termites providing these services. However, a single basal subfamily of the higher termites, the Macrotermitinae, also domesticated a plant biomass‐degrading fungus (Termitomyces), and how this symbiont acquisition has affected the fungus‐growing termite gut microbiota has remained unclear. The objective of our study was to compare the intestinal bacterial communities of five genera (nine species) of fungus‐growing termites to establish whether or not an ancestral core microbiota has been maintained and characterizes extant lineages. Using 454‐pyrosequencing of the 16S rRNA gene, we show that gut communities have representatives of 26 bacterial phyla and are dominated by Firmicutes, Bacteroidetes, Spirochaetes, Proteobacteria and Synergistetes. A set of 42 genus‐level taxa was present in all termite species and accounted for 56–68% of the species‐specific reads. Gut communities of termites from the same genus were more similar than distantly related species, suggesting that phylogenetic ancestry matters, possibly in connection with specific termite genus‐level ecological niches. Finally, we show that gut communities of fungus‐growing termites are similar to cockroaches, both at the bacterial phylum level and in a comparison of the core Macrotermitinae taxa abundances with representative cockroach, lower termite and higher nonfungus‐growing termites. These results suggest that the obligate association with Termitomyces has forced the bacterial gut communities of the fungus‐growing termites towards a relatively uniform composition with higher similarity to their omnivorous relatives than to more closely related termites.