Tropical Soil Bacterial Communities in Malaysia: pH Dominates in the Equatorial Tropics Too

The dominant factors controlling soil bacterial community variation within the tropics are poorly known. We sampled soils across a range of land use types--primary (unlogged) and logged forests and crop and pasture lands in Malaysia. PCR-amplified soil DNA for the bacterial 16S rRNA gene targeting the V1-V3 region was pyrosequenced using the 454 Roche machine. We found that land use in itself has a weak but significant effect on the bacterial community composition. However, bacterial community composition and diversity was strongly correlated with soil properties, especially soil pH, total carbon, and C/N ratio. Soil pH was the best predictor of bacterial community composition and diversity across the various land use types, with the highest diversity close to neutral pH values. In addition, variation in phylogenetic structure of dominant lineages (Alphaproteobacteria, Beta/Gammaproteobacteria, Acidobacteria, and Actinobacteria) is also significantly correlated with soil pH. Together, these results confirm the importance of soil pH in structuring soil bacterial communities in Southeast Asia. Our results also suggest that unlike the general diversity pattern found for larger organisms, primary tropical forest is no richer in operational taxonomic units of soil bacteria than logged forest, and agricultural land (crop and pasture) is actually richer than primary forest, partly due to selection of more fertile soils that have higher pH for agriculture and the effects of soil liming raising pH.     

云南松林次生演替阶段土壤细菌群落的变化

土壤细菌多样性是维持森林生态系统功能的关键因子,森林演替是影响其动态变化的重要因素。研究云南松林不同演替阶段土壤细菌群落结构及其多样性的变化规律,有助于深入理解森林生态系统恢复过程的驱动机制。本研究以云南省永仁县皆伐后形成的针叶林、针阔混交林和常绿阔叶林为对象,基于Illumina Hiseq高通量测序技术,分析森林演替过程中土壤细菌群落组成、结构、多样性及其影响因子的变化。结果表明: 土壤细菌的种群分类单元、Ace指数、Chao1指数和Shannon指数均随着演替进行呈减少趋势,演替早期阶段土壤的细菌总数、菌群丰富度及复杂程度最高。不同演替阶段细菌群落结构存在显著差异,其中,针阔混交林的差异最大,变形菌门和酸杆菌门为各演替序列共有的优势类群,放线菌门、绿弯菌门和Patescibacteria是演替早期的优势类群,且随着演替进行呈现减少趋势;变形菌门和WPS-2相对多度随演替进行呈增加趋势。土壤pH和乔木层物种丰富度是驱动次生演替过程中土壤细菌群落组成变化的关键因子。随着演替的进行,土壤细菌多样性减少,群落组成差异加大。     

文峪河上游河岸带不同植被类型土壤nirS反硝化菌群结构及功能

以文峪河上游河岸带不同演替阶段的8种植被类型五花草甸(WH)、沙棘林(HR)、柳树林(SS)、山杨林(PC)、山杨白桦林(PQ)、山杨白桦落叶松林(PQL)、落叶松云杉林(LP)和云杉林(PM)土壤为研究对象,采用高通量测序技术测定nirS反硝化细菌群落组成及相对丰度,乙炔抑制法测定反硝化酶活性(DEA)。对其土壤理化性质及反硝化细菌群落组成及相对丰度进行方差分析,采用冗余分析(RDA)和Spearman相关性分析不同植被类型及土层反硝化细菌群落结构及功能及土壤理化因子的关联性。结果表明:1)不同植被类型及土层土壤理化因子存在显著差异,柳树林(SS)0—15 cm土层硝态氮(NO~+_3-N)含量显著高于其他植被类型各土层;2)土壤反硝化菌群多样性指数在五花草甸(WH)、山杨白桦林(PQ)和云杉林(PM)中较其他植被类型高;3)沙棘林(HR)及柳树林(SS)反硝化酶活性(DEA)显著高于其他植被类型;4)不同植被类型反硝化优势菌群分布存在显著差异及特异性,如浮霉菌门(Planctomycetes)仅在落叶松云杉混交林(LP)和云杉林(PM)植被类型15—30 cm土层中分布;5)土壤pH、土壤有机碳(SOC)、土壤铵态氮(NH~+_4-N)和硝态氮(NO~+_3-N)等是影响土壤反硝化细菌群落结构及组成的重要因子,其中土壤铵态氮和硝态氮含量变化是导致土壤反硝化菌群多样性和反硝化酶活性差异的关键因子。本研究揭示了文峪河上游河岸带不同植被类型土壤反硝化细菌群落结构及功能的变化和分布特征,为进一步研究该区域河岸带氮素循环及水体污染防治提供重要参考依据。     

Spatial Scaling Effects on Soil Bacterial Communities in Malaysian Tropical Forests

Spatial scaling to some extent determines biodiversity patterns in larger organisms, but its role in microbial diversity patterns is much less understood. Some studies have shown that bacterial community similarity decreases with distance, whereas others do not support this. Here, we studied soil bacterial communities of tropical rainforest in Malaysia at two spatial scales: a local scale with samples spaced every 5 m over a 150-m transect, and a regional scale with samples 1 to 1,800 km apart. PCR-amplified soil DNA for the bacterial 16S rRNA gene targeting the V1–V3 region was pyrosequenced using Roche/454 GS FLX Titanium platform. A ranked partial Mantel test showed a weak correlation between spatial distance and whole bacterial community dissimilarity, but only at the local scale. In contrast, environmental distance was highly correlated with community dissimilarity at both spatial scales, stressing the greater role of environmental variables rather than spatial distance in determining bacterial community variation at different spatial scales. Soil pH was the only environmental parameter that significantly explained the variance in bacterial community at the local scale, whereas total nitrogen and elevation were additional important factors at the regional scale. We obtained similar results at both scales when only the most abundant OTUs were analyzed. A variance partitioning analysis showed that environmental variables contributed more to bacterial community variation than spatial distance at both scales. In total, our results support a strong influence of the environment in determining bacterial community composition in the rainforests of Malaysia. However, it is possible that the remaining spatial distance effect is due to some of the myriad of other environmental factors which were not considered here, rather than dispersal limitation.     

Abiotic drivers and plant traits explain landscape‐scale patterns in soil microbial communities

The controls on aboveground community composition and diversity have been extensively studied, but our understanding of the drivers of belowground microbial communities is relatively lacking, despite their importance for ecosystem functioning. In this study, we fitted statistical models to explain landscape‐scale variation in soil microbial community composition using data from 180 sites covering a broad range of grassland types, soil and climatic conditions in England. We found that variation in soil microbial communities was explained by abiotic factors like climate, pH and soil properties. Biotic factors, namely community‐weighted means (CWM) of plant functional traits, also explained variation in soil microbial communities. In particular, more bacterial‐dominated microbial communities were associated with exploitative plant traits versus fungal‐dominated communities with resource‐conservative traits, showing that plant functional traits and soil microbial communities are closely related at the landscape scale.     

环境选择和扩散限制驱动温带森林土壤细菌群落的构建

环境选择和扩散限制是生态系统中生物群落构建的两个基本过程,而两者相对作用的大小因研究尺度、群落属性和类型等有所不同.目前对温带亚高山森林土壤微生物群落构建的驱动因子和机制尚缺乏了解.本文利用PCR-DGGE技术研究庞泉沟自然保护区内5种典型森林包括华北落叶松林、青杄林、白杄林、油松林以及桦树林的6个森林土壤细菌群落(Lp MC1、Lp MC2、Pw MC、Pm MC、Pt MC、BMC)的结构特征及其影响因素,分析细菌群落结构与环境因子的相关性,以及土壤因子、植被和空间因素对细菌群落结构的影响.结果表明:研究区各样地土壤细菌群落的结构和生物多样性具有显著差异,低海拔落叶松和油松土壤细菌群落多样性较高(20条带),白杄林土壤细菌群落(13条带)多样性最低,高海拔落叶松土壤细菌群落多样性最高;土壤环境因子,如pH、土壤含水量、总碳、总氮、土壤有机质、速效磷以及土壤酶活性与土壤细菌群落多样性和结构显著相关;样地土壤细菌群落的beta多样性与群落的空间距离呈显著相关,表明扩散限制对群落结构具有一定的影响;方差分解分析结果显示,6个样地细菌群落结构的驱动因素大小依次为土壤因子(0.27)、空间因素(0.19)和植被(0.15);将区域土壤微生物作为"源群落",微宇宙试验结果显示,土壤因子是细菌群落结构形成的主要驱动力(0.35),同时源群落丰富的物种多样性对微宇宙土壤细菌群落结构具有显著影响.总之,在局域尺度下,环境选择对温带森林土壤细菌群落结构动态和多样性发挥主导作用,地理距离对群落结构具有显著影响,即确定性过程和随机过程共同决定局域森林土壤细菌群落结构,前者占主导地位.对于土壤细菌群落而言,扩散群落的组成和结构受到源群落的多样性特征和环境因子的双重影响.     

Soil bacterial diversity in the Arctic is not fundamentally different from that found in other biomes

The severe environmental stresses of the Arctic may have promoted unique soil bacterial communities compared with those found in lower latitude environments. Here, we present a comprehensive analysis of the biogeography of soil bacterial communities in the Arctic using a high resolution bar‐coded pyrosequencing technique. We also compared arctic soils with soils from a wide range of more temperate biomes to characterize variability in soil bacterial communities across the globe. We show that arctic soil bacterial community composition and diversity are structured according to local variation in soil pH rather than geographical proximity to neighboring sites, suggesting that local environmental heterogeneity is far more important than dispersal limitation in determining community‐level differences. Furthermore, bacterial community composition had similar levels of variability, richness and phylogenetic diversity within arctic soils as across soils from a wide range of lower latitudes, strongly suggesting a common diversity structure within soil bacterial communities around the globe. These results contrast with the well‐established latitudinal gradients in animal and plant diversity, suggesting that the controls on bacterial community distributions are fundamentally different from those observed for macro‐organisms and that our biome definitions are not useful for predicting variability in soil bacterial communities across the globe.     

Relationship Between Soil Properties and Patterns of Bacterial β-diversity Across Reclaimed and Natural Boreal Forest Soils

Productivity gradients in the boreal forest are largely determined by regional-scale changes in soil conditions, and bacterial communities are likely to respond to these changes. Few studies, however, have examined how variation in specific edaphic properties influences the composition of soil bacterial communities along environmental gradients. We quantified bacterial compositional diversity patterns in ten boreal forest sites of contrasting fertility. Bulk soil (organic and mineral horizons) was sampled from sites representing two extremes of a natural moisture-nutrient gradient and two distinct disturbance types, one barren and the other vegetation-rich. We constructed 16S rRNA gene clone libraries to characterize the bacterial communities under phylogenetic- and species-based frameworks. Using a nucleotide analog to label DNA-synthesizing bacteria, we also assessed the composition of active taxa in disturbed sites. Most sites were dominated by sequences related to the α-Proteobacteria, followed by acidobacterial and betaproteobacterial sequences. Non-parametric multivariate regression indicated that pH, which was lowest in the natural sites, explained 34% and 16% of the variability in community structure as determined by phylogenetic-based (UniFrac distances) and species-based (Jaccard similarities) metrics, respectively. Soil pH was also a significant predictor of richness (Chao1) and diversity (Shannon) measures. Within the natural edaphic gradient, soil moisture accounted for 32% of the variance in phylogenetic (but not species) community structure. In the boreal system we studied, bacterial β-diversity patterns appear to be largely related to “master” variables (e.g., pH, moisture) rather than to observable attributes (e.g., plant cover) leading to regional-scale fertility gradients.     

Plant Community Composition as a Predictor of Regional Soil Carbon Storage in Alaskan Boreal Black Spruce Ecosystems

The boreal forest is the largest terrestrial biome in North America and holds a large portion of the world’s reactive soil carbon. Therefore, understanding soil carbon accumulation on a landscape or regional scale across the boreal forest is useful for predicting future soil carbon storage. Here, we examined the relationship between floristic composition and ecosystem parameters, such as soil carbon pools, the carbon-to-nitrogen (C/N) ratio of live black spruce needles, and normalized basal area increment (NBAI) of trees in black spruce communities, the most widespread forest type in the boreal forest of Alaska. Variability in ecosystem properties among black spruce stands was as large as that which had previously been documented among all forest types in the central interior of Alaska; we found an eightfold range in NBAI and fivefold range in mineral soil carbon and nitrogen pools. Acidic black spruce communities had significantly more carbon in the organic soil horizon than did nonacidic black spruce communities, but did not differ in any other measured ecosystem parameter. We explained 48% of the variation in total soil carbon with a combination of plant community indices and abiotic and biotic factors. Plant community composition was at least as effective as any single environmental factor or stand characteristic in predicting soil C pools in Alaskan black spruce ecosystems. We conclude that among the community properties analyzed, the presence of key groups of species, overall species composition, and diversity of certain functional types, especially Sphagnum moss species, are important predictors of soil carbon sequestration in the black spruce forest type.     

东北丘陵区林地转型耕地对土壤编码碱性磷酸酶基因的细菌群落的影响

【目的】通过研究林地转型耕地对土壤编码碱性磷酸酶基因的细菌群落丰度、多样性和结构的影响,为丘陵区耕地长期施肥下农田土壤微生物多样性丧失的影响机制以及未来的退耕还林过程中土壤微生物多样性的提升和土地可持续利用研究提供一些基础数据和技术支撑。【方法】采用实时荧光定量PCR (real-time quantitative PCR,qPCR)和高通量测序技术解析土壤编码碱性磷酸酶基因的细菌群落的丰度、多样性和结构变化,并耦合土壤化学性质分析,明确土壤编码碱性磷酸酶基因的细菌群落丰度和多样性与土壤化学性质的关系以及关键的驱动因子。【结果】林地垦殖为农田后,长期施肥导致土壤酸化,pH从5.58降至4.72,而土壤速效磷则从2.49 mg/kg增至49.3 mg/kg。相应地,耕地土壤编码碱性磷酸酶基因的细菌群落的丰度和Shannon指数均显著低于林地。基于编码碱性磷酸酶的phoD基因(alkaline phosphatase-encoding gene)序列的物种分类表明,丘陵区土壤编码碱性磷酸酶基因的细菌群落的优势门为变形菌门(Proteobacteria)、蓝藻门(Cyanobacteria)、浮霉菌门(Planctomycetes)、放线菌门(Actinobacteria)、厚壁菌门(Firmicutes)和疣微菌门(Verrucomicrobia),其中林地土壤的蓝藻门的相对丰度显著高于耕地。耕地土壤的慢生根瘤菌属(Bradyrhizobium)和芽孢杆菌属(Bacillus)的相对丰度显著高于林地,而中慢生根瘤菌属(Mesorhizobium)、假单胞菌属(Pseudomonas)、Chlorogloea属、Gemmata属、Phormidesmis属和Pseudolabrys属的相对丰度显著低于林地。土壤编码碱性磷酸酶基因的细菌群落结构因林地转型耕地而发生显著改变。phoD基因丰度和Shannon指数与pH显著正相关,而与总磷、速效磷、硝态氮和铵态氮均显著负相关,其中土壤速效磷是这些影响因素中影响最强烈的,长期施用无机磷肥导致含碱性磷酸酶的土壤细菌群落对有机磷分解的能力退化。【结论】林地转型耕地加之长期施肥改变了土壤pH和速效磷,并在其他理化因子的协同驱动下,导致土壤编码碱性磷酸酶基因的细菌群落丰度、多样性和结构的显著变化。     

Assessment of soil bacterial communities on Alexander Island (in the maritime and continental Antarctic transitional zone)

Despite an increasing number of Antarctic soil diversity assessments, understanding of the bacterial community composition in the arid soil environments of the maritime/continental Antarctic transitional zone remains lacking. Most documented microbiological studies had focused on either the wetter environments of the Antarctic Peninsula/Scotia arc or the exceptionally arid deserts of the Dry Valleys of continental Antarctica. In this study, soil bacterial diversity from three relatively arid sites on Alexander Island and the physicochemical parameters that might influence it were assessed. In general, the study sites exhibited levels of pH, hydration and metal content different from previous reports of maritime or continental Antarctic soil habitats. Although the soil from Alexander Island exhibited similar phylum-level bacterial taxonomic composition to those of other cold and arid environments, each study site was found to harbour significantly different bacterial assemblages. The latter finding was supported by three complementary molecular methods selected to address different elements of diversity. Our analyses of the measured parameters suggest that the differences in bacterial communities were best explained by soil pH and copper content. Using these data, we suggest that soil pH might play an important role in structuring bacterial assemblage patterns across polar soils.     

Bacterial community of very wet and acidic subalpine forest and fire-induced grassland soils

The subalpine forest and grassland ecosystems at Tatajia in Yushan National Park, Taiwan, at an elevation of 2,700 m, mean annual precipitation of 4,100 mm, mean annual temperature of 9.5°C, and soil pH near 3.5, represent land types whose bacterial communities have not been previously characterized. To this end, small subunit (SSU) rRNA libraries were prepared from environmental DNA, and 319 clones were sequenced and characterized. Despite differences in vegetation, Acidobacteria, Proteobacteria and Firmicutes were the most abundant phyla in soil communities from the forest and grassland. Although not significantly different, on the basis of Chao1, Shannon and other indices and rarefaction analyses, the diversity of the bacterial community of grassland appeared higher than that of the forest. The composition of the most abundant operational taxonomic units (OTUs) also differed between the grassland and forest communities. Because the grassland was formed by fire 30 years ago from forest, these results indicated a different bacterial community could form within that time. Moreover, most of the OTUs abundant in Tatajia soils had been previously detected in other studies, but in lower numbers. Therefore, the bacterial communities in Tatajia differed in relative abundance but not in types of bacteria present. However, one acidobacterial OTU abundant in Tatajia had previously been found to be abundant in soils from around the world. Thus, this OTU may represent a particularly abundant and cosmopolitan bacterial phylotype.     

武夷山常绿阔叶林土壤微生物多样性的季节动态

为了解武夷山自然保护区常绿阔叶林土壤微生物群落特征和季节变化,采用Illumina Miseq高通量测序技术分析了土壤微生物多样性的季节响应。结果表明,武夷山常绿阔叶林土壤为典型的南方酸性土壤,有效钾、土壤温度四季内存在显著差异,其他理化指标均无显著差异。土壤中的微生物多样性比较丰富,已鉴定出23门206属细菌和2门17属的古菌。夏季反映细菌总数的Chao指数最高,但反映细菌多样性的Shannon指数比春季低0.21,夏季古菌的Chao指数和Shannon指数分别比冬季高21.7%和0.27%。4个季节共有的细菌和古菌分别占总数的83.1%和70.0%,说明武夷山常绿阔叶林土壤不同季节的核心微生物组成具有很好的稳定性。在门和属水平的聚类树分析表明,春季和冬季的细菌和古菌群落组成最为接近,而夏季与其他3个季节的差异最大。冗余分析和热图分析结果表明,土壤p H是决定和影响细菌和古菌多样性的主要环境因子,有效钾、有效碳和总氮对微生物群落组成均有很大的影响。因此,随季节变化武夷山常绿阔叶林土壤微生物多样性呈现出规律性变化。     

Interaction effects of pH and land cover on soil microbial diversity are climate-dependent

Factors regulating the diversity and composition of soil microbial communities include soil properties, land cover and climate. How these factors interact at large scale remains poorly investigated. Here, we used an extensive dataset including 715 locations from 24 European countries to investigate the interactive effects of climatic region, land cover and pH on soil bacteria and fungi. We found that differences in microbial diversity and community composition between land cover types depended on the climatic region. In Atlantic, Boreal and Continental regions, microbial richness was higher in croplands and grasslands than woodlands while richness in Mediterranean areas did not vary significantly among land cover types. These differences were further related to soil pH, as a driver of bacterial and fungal richness in most climatic regions, but the interaction of pH with land cover depended on the region. Microbial community composition differed the most between croplands and woodlands in all regions, mainly due to differences in pH. In the Mediterranean region, bacterial communities in woodlands and grasslands were the most similar, whereas in other regions, grassland and cropland-associated bacteria showed more similarity. Overall, we showed that key factors interact in shaping soil microbial communities in a climate-dependent way at large scale.     

大兴安岭森林火烧后不同演替阶段土壤细菌多样性动态

【目的】研究我国最大的林区之一——大兴安岭森林火烧后不同演替阶段土壤细菌多样性动态,为天然林保护工程对于生物多样性的影响增添新的认识。【方法】以空间替代时间的方法分析大兴安岭森林演替对于土壤细菌多样性动态的影响。大兴安岭森林火烧后典型的自然演替序列为火烧迹地(LG-BA)、灌丛(SHR)、白桦林(BP)、白桦落叶松混交林(BP-LG)、落叶松林(LG-OM)。在演替序列的每个典型样地上采集0-10 cm土样,采用Illumina Mi Seq高通量测序技术测定土壤细菌群落组成及其多样性。【结果】细菌操作分类单位(OTU)数量从少到多的顺序为火烧迹地落叶松白桦混交林灌丛落叶松林白桦林。随着森林演替,多样性指数Simpson先增高后降低;Shannon指数先增加后减少再增加;OTU的丰度变化比较平缓,表明物种变化较小。在各演替阶段中,土壤细菌种类主要有变形菌门(Proteobacteria)、酸杆菌门(Acidobacteria)、放线菌门(Actinobacteria)和浮霉菌门(Planctomycetes),4个门的种类含量随演替顺序都呈现先增加后减少的趋势。主成分分析表明不同演替阶段土壤细菌群落存在一定的差异性。冗余分析表明有机质(SOM)、全氮(TN)、全磷(TP)和p H对于土壤细菌群落变化有影响。【结论】随着森林演替,大兴安岭地区土壤细菌种类和生物多样性会发生变化,其变化与土壤化学成分和p H有关。     

How Does Conversion of Natural Tropical Rainforest Ecosystems Affect Soil Bacterial and Fungal Communities in the Nile River Watershed of Uganda?

Uganda''s forests are globally important for their conservation values but are under pressure from increasing human population and consumption. In this study, we examine how conversion of natural forest affects soil bacterial and fungal communities. Comparisons in paired natural forest and human-converted sites among four locations indicated that natural forest soils consistently had higher pH, organic carbon, nitrogen, and calcium, although variation among sites was large. Despite these differences, no effect on the diversity of dominant taxa for either bacterial or fungal communities was detected, using polymerase chain reaction-denaturing gradient gel electrophoresis (PCR-DGGE). Composition of fungal communities did generally appear different in converted sites, but surprisingly, we did not observe a consistent pattern among sites. The spatial distribution of some taxa and community composition was associated with soil pH, organic carbon, phosphorus and sodium, suggesting that changes in soil communities were nuanced and require more robust metagenomic methods to understand the various components of the community. Given the close geographic proximity of the paired sampling sites, the similarity between natural and converted sites might be due to continued dispersal between treatments. Fungal communities showed greater environmental differentiation than bacterial communities, particularly according to soil pH. We detected biotic homogenization in converted ecosystems and substantial contribution of β-diversity to total diversity, indicating considerable geographic structure in soil biota in these forest communities. Overall, our results suggest that soil microbial communities are relatively resilient to forest conversion and despite a substantial and consistent change in the soil environment, the effects of conversion differed widely among sites. The substantial difference in soil chemistry, with generally lower nutrient quantity in converted sites, does bring into question, how long this resilience will last.     

Contrasting elevational diversity patterns for soil bacteria between two ecosystems divided by the treeline

Above- and below-ground organisms are closely linked, but how elevational distribution pattern of soil microbes shifting across the treeline still remains unknown. Sampling of 140 plots with transect, we herein investigated soil bacterial distribution pattern from a temperate forest up to a subalpine meadow along an elevational gradient using Illumina sequencing. Our results revealed distinct elevational patterns of bacterial diversity above and below the treeline in responding to changes in soil conditions: a hollow elevational pattern in the forest (correlated with soil temperature, pH, and C:N ratio) and a significantly decreasing pattern in the meadow (correlated with soil pH, and available phosphorus). The bacterial community structure was also distinct between the forest and meadow, relating to soil pH in the forest and soil temperature in the meadow. Soil bacteria did not follow the distribution pattern of herb diversity, but bacterial community structure could be predicted by herb community composition. These results suggest that plant communities have an important influence on soil characteristics, and thus change the elevational distribution of soil bacteria. Our findings are useful for future assessments of climate change impacts on microbial community.     

川西亚高山三种天然次生林土壤微生物多样性变化特征

开展川西亚高山相似土壤母质背景下天然次生林土壤微生物群落结构及其多样性探究,可加深次生林更新过程中土壤微生物群落结构变化的认知。选取川西米亚罗林区20世纪60年代采伐后经自然更新恢复形成的3种天然次生林（槭-桦阔叶林,ABB;桦-槭-冷杉针阔混交林,BAA;岷江冷杉林,AFF）,分析林下表层（0-20 cm）土壤微生物群落结构变化及其影响因素,结果显示：（1）3种林型土壤细菌Chao1和Shannon指数均极显著高于真菌,但仅真菌群落的Shannon指数差异显著,表现为BAA > ABB > AFF;（2）细菌群落优势门主要为变形杆菌门、酸杆菌门、疣微菌门、拟杆菌门、绿弯菌门,相对丰度占比超过82%;真菌群落则为子囊菌门和担子菌门,占比超过85%,AFF担子菌门相对丰度最高而子囊菌门最低。（3） RDA分析显示,土壤pH和乔木物种多样性（Shannon指数）是影响微生物群落结构变化的主导因子;土壤养分元素对细菌群落影响不显著,真菌群落主要受TN、TP含量显著影响。总体上,林型间乔木层物种多样性、土壤酸碱度及其氮磷含量是导致微生物群落结构变化的关键因素。     

毛竹入侵马尾松林的土壤菌群多样性变化

为揭示毛竹入侵邻域林分过程中对土壤细菌群落多样性变化的影响,以马尾松林为研究对象,采集纯毛竹林、竹针混交林和常绿针叶(马尾松)混交林3类样地的混合土样,基于高通量测序技术分析土壤细菌群落多样性和结构变化.结果表明: 研究期间共得到细菌类群39门88纲134目160科511属;在门的分类水平上,与竹针混交林、常绿针叶混交林相比,纯毛竹林酸杆菌门所占比例显著较低,而放线菌门、拟杆菌门、TM7和衣原体门所占比例较高;在属的分类水平上,相对于纯毛竹林,竹针混交林和常绿针叶混交林均有多属表现出所占比例显著上升或下降,单独出现在竹针混交林或常绿针叶混交林且所占比例在0.005%～0.1%的非优势属有130属;α多样性指数均表现为常绿针叶混交林>竹针混交林>纯竹林,且纯竹林与两者均有显著差异,而常绿针叶混交林和竹针混交林之间差异不显著.PCoA分析表明,毛竹入侵对土壤细菌的种群多样性和群落结构产生了影响;所占比例小于0.1%的非优势菌群门分类水平的百分比特征与土壤环境梯度(水溶性有机氮和硝态氮)之间有显著相关性,两者对毛竹入侵马尾松林后土壤细菌群落的非优势种群影响巨大,具有重要的参考价值.