基于加权共变化网络分析水稻根系微生物群落间的差异

为了解水稻根系微生物群落间的差异,比较水稻根内、根表以及根际3个生态位微生物群落组成差异;探究水稻根系生态位之间、变化种群间的相互关系;以期为今后水稻根系微生物研究提供具有参考价值的依据.本研究利用WGCNA算法对水稻根系3个生态位的微生物群落数据分别构建共表达网络,找出根内、根表以及根际微生物群落间的差异网络,以网络为单位比较分析不同生态位间微生物群落的差异,并基于共变化网络分析进一步探究差异种群间的相互关系.通过WGCNA算法对水稻根系3个生态位的微生物群落进行共表达网络分析,结果发现:在水稻根内-根表-根际3个生态位间,微生物群落构成的共表达互作网络存在差异.进一步分析3个生态位间差异网络,发现根际-根表差异网络中的OTUs分布于6个门18个属中,优势菌门为变形菌门(Proteobacteria,72.97％);在根际-根内差异网络中的OTUs分布于9个门35个属,优势菌门为变形菌门(Proteobacteria,66.36％)、放线菌门(Actinobacteria,9.09％)、拟杆菌门(Bacteroidetes,10.9％);根表-根内差异网络中的OTUs分布于12个门36个属中,其中优势菌门为变形菌门(Proteobacteria,41.41％)、拟杆菌门(Bacteroidetes,10.10％)、厚壁菌门(Firmicutes,12.12％)、疣微菌门(Verrucomicrobia,10.10％).Rhodobacter、No-vosphingobium等3个核心菌属、Blvii28、Dechloromonas等6个核心菌属和Cellvibrio、Geobacter等5个核心菌属,分别在根际-根表差异种群微生物共变化网络、根际-根内差异种群微生物共变化网络和根表-根内差异种群微生物共变化网络中起重要的调控作用.     

柴达木盆地尕斯库勒盐湖区邻近水体对湖泊微生物群落的贡献

【目的】探究尕斯库勒盐湖生态系统中邻近水体对湖泊微生物的贡献。【方法】采集尕斯库勒盐湖区湖水、沉积物以及邻近的泉水、河水和盐田的水样,对其进行地球化学分析;通过16S rRNA基因的Illumina MiSeq高通量测序分析样品的微生物群落组成。【结果】尕斯库勒盐湖区水体和沉积物中的优势门是变形菌门(Proteobacteria)、拟杆菌门(Bacteroidetes)、放线菌门(Actinobacteria)和广古菌门(Euryarchaeota)。盐度和pH是影响尕斯库勒盐湖区群落组成的最主要环境因素。邻近水体对湖泊水体和沉积物的贡献分别为12.94%和7.53%。【结论】邻近水体对尕斯库勒盐湖微生物群落的贡献有限。     

青海湖主湖区与湖水淹没区的细菌群落结构差异分析

为对比青海湖与湖滨淹没区的微生物群落结构及多样性的差异, 利用16S rRNA高通量测序技术, 研究不同环境条件下水体的微生物群落组成的异同。结果表明: 青海湖主湖区及淹没区的细菌在分类门级水平上相对丰度最高的为变形菌门(Proteobacteria, 44.8%), 其次分别隶属于拟杆菌门[Bacteroidetes, (25.9%±7.8)%]、蓝细菌门[Cyanobacteria, (13.6%±5.4)%]、放线菌门[Actinobacteria, (7.54%±9)%]和柔壁菌门[Tenericutes, (3.32%±2)%]。淹没区整体微生物多样性显著高于主湖区水体。部分微生物分类属在两个湖区呈现显著的分布差异暗示这些细菌对于环境特征的适应性。节线藻在青海湖主湖的分布广泛显示其可能在高原咸水湖泊的碳氮循环过程中扮演着重要角色。研究对于深入了解栖居地如何塑造咸水水体微生物群落结构具有重要意义。     

北部湾红树林沉积物中微生物群落结构的时空变化分析

微生物群落结构对海洋红树林湿地生态系统中的物质循环非常关键。本研究从中国亚热带北部湾典型海洋红树林湿地生态系统中采集沉积物样品,利用宏基因组学技术手段,完成了沉积物样品16S rDNA基因的扩增子的高通量测序,分析了不同时空条件下红树林沉积物的微生物群落结构分布和变化规律。研究结果表明,不管在干季还是湿季,在门分类水平上变形菌门(Proteobacteria)是最丰富的类别。此外,变形菌门(Proteobacteria)与绿弯菌门(Chloroflexi)、拟杆菌门(Bacteroidetes)、酸杆菌门(Acidobacteria)、硝化螺旋菌门(Nitrospirae)和放线菌门(Actinobacteria)一共占据总丰度的80%左右。干季时期的微生物α多样性显著高于湿季,主坐标分析(principal co-ordinates analysis, PCoA)显示干、湿两季的微生物群落结构具有明显差异。干季时期的细菌的相对丰度显著高于湿季,而古菌则相反。不同时空期(干季和湿季)的变形菌门(Proteobacteria)的相对丰度没有显著差异。冗余分析(redundancy analysis, RDA)和相关性分析表明温度和盐度对微生物群落结构具有显著影响。本研究对揭示亚热带海洋红树林湿地生态系统沉积物中的微生物多样性及其群落结构演替规律具有重要的实践意义。     

污水处理活性污泥微生物群落多样性研究

为研究污水处理活性污泥微生物多样性,提取了活性污泥宏基因组DNA,并采用细菌通用引物27F和1492R扩增了上海污泥厂活性污泥细菌16S rDNA片段,构建了细菌16S rDNA克隆文库,并对该文库中的微生物群落进行了分析。共获得200条高质量序列并建立系统发育树,结果显示活性污泥主要的细菌类群为变形菌门(Proteobacteria)(91.9%)、厚壁菌门(Firmicures)(4.6%)、拟杆菌门(Bacteroidetes)(2%)、绿弯菌门(Chloroflexi)(0.5%)、硝化螺菌门(Nitrospirae)(1%)。其中,明显的优势菌群为Alcaligenes feacalis(55%)、Pseudomonas aeruginosa(12.8%)和Stenotrophomonas(12.8%),优势菌的产酶能力在活性污泥中显示生态修复功能菌的作用。     

基于高通量测序的鱼菜共生池塘与普通池塘微生物群落结构比较

鱼菜共生(Aquaponics)作为一种可持续、循环型、零排放的新型的复合耕作体系, 因具有良好的生态环境效应和食品安全保障, 成为解决农业生态危机的有效途径。研究采用Illumina高通量测序平台对西北地区典型池塘鱼菜共生养殖模式下, 养殖水环境与根系细菌微生物16S rRNA基因(V3—V5区)进行高通量测序。比较群落结构和微生物多样性表明, 细菌总有效序列为56444条, 细菌物种平均注释OTU数目为945条。在鱼菜共生模式下的优势门类为变形菌门(Proteobacteria)、拟杆菌门(Bacteroidetes)、厚壁菌门(Firmicutes)、蓝菌门(Cyanobacteria)。根系微生物群落中占优势地位的分别为拟杆菌门(Bacteroidetes)和变形菌门(Proteobacteria)。OTU聚类分析结果显示6个样品共有OTU数目为165, 其中新疆水生野生动物救护中心鱼菜共生池塘水样(JH.KX)特有OTU数量最高(137), 其空心菜根系水样(JH.R)最低(30), 而乌鲁木齐市米东区长山子镇水源地养殖基地空心菜根系水样(MD.R)和新疆水生野生动物救护中心对照池塘水样(JH.C)数量相同(85)。通过对各OTU进行注释, 发现了根瘤菌、鱼类致病菌、耐寒细菌、降解有机物细菌、降低重金属及毒素危害的细菌。研究为鱼菜共生生态养殖模式下微生物群落结构及其生态调控机理提供了参考依据。     

新疆乌尔禾地区盐渍土壤耐盐细菌多样性与群落结构研究

研究新疆北部乌尔禾地区盐渍土壤中微生物群落结构及多样性,以期发现新的高盐环境耐盐性微生物资源菌株。采用传统分离培养法获得可培养耐盐菌株并对菌株形态学、16S rRNA基因测序、耐盐特性进行研究,同时结合高通量测序技术分析新疆乌尔禾地区盐渍土壤耐盐细菌的多样性与群落结构。共分离得到耐盐细菌11株,分属6个属,均为中度耐盐菌,以芽胞杆菌属(Bacillus)为优势菌。对盐渍土壤微生物16S rRNA(V3～V4)基因测序,共获得细菌序列290 952条,分属24个门410个属,变形菌门(Proteobacteria, 60.31%)、厚壁菌门(Firmicutes, 21.52%)、拟杆菌门(Bacteroidetes, 6.9%)和放线菌门(Actinobacteria, 6%)相对丰度较高。优势属为克吕沃尔菌属(Kluyvera,21%)、Hafnia-Obesumbacterium(19.6%)和假单胞菌属(Pseudomonas,7.5%)。结果表明,新疆乌尔禾地区盐渍土壤耐盐细菌优势菌群以芽胞杆菌属(Bacillus)居多,细菌群落结构较复杂,潜在可利用微生物资源较为丰富,对高盐极端环境耐盐微生物新资源有进一步研究的意义。     

中国林蛙蝌蚪肠道及皮肤微生物多样性分析

肠道及皮肤微生物群落对宿主的健康有着至关重要的影响。本研究使用16S rRNA基因测序技术研究中国林蛙(Rana chensinensis)Gosner38期蝌蚪肠道和皮肤共生微生物群落组成之间的差异。在门水平上,林蛙蝌蚪肠道中的优势门为变形菌门(Proteobacteria)、厚壁菌门(Firmicutes)和拟杆菌门(Bacteroidetes),皮肤中的优势门为拟杆菌门、变形菌门和疣微菌门(Verrucomicrobia)。此外,显著性检验结果显示,肠道中厚壁菌门和放线菌门(Actinobacteria)的丰度显著偏高,皮肤中拟杆菌门的丰度显著偏高。肠道微生物群落多样性高于皮肤,而肠道和皮肤的物种丰富度之间无显著差异。在对KEGG通路的丰度进行比较时,结果显示肠道"环境信息处理"功能的丰度显著高于皮肤,而皮肤中"遗传信息处理"及"新陈代谢"功能显著偏高。本研究提示林蛙蝌蚪肠道及皮肤微生物群落组成之间存在显著差异。     

台风利奇马对海水贝塘浮游生物群落的影响

为了揭示台风前后海水池塘贝类养殖过程中浮游生物群落结构的变化,对养殖水体环境基因组DNA中16S和18S rRNA基因进行了高通量测序和生物信息学分析。结果显示,原核生物OTU数(28728)明显高于真核生物(8498),其中原核生物优势类群主要为变形菌门(Proteobacteria)、蓝藻门(Cyanobacteria)、拟杆菌门(Bacteroidetes)、放线菌门(Actinobacteria)和绿菌门(Chlorobi)等;真核生物优势类群为纤毛虫、鞭毛虫、原绵虫、杯鞭虫、隐藻、棕鞭藻和硅藻等,其中硅藻丰度占比在台风后显著性增加(P<0.05)。台风过后真核生物多样性均未发生显著改变,原核生物Shannon指数和Simpson指数出现显著性差异(P<0.05),表现为先降低后升高,而OTU数和Chao I指数则未发生显著改变。PCoA分析显示,台风后原核和真核生物群落结构均产生时间异质性,但仅原核生物群落结构产生显著差异。ANOSIM显示,真核和原核微生物群落在台风前后均存在显著性差异(P<0.05),其中原核微生物每个时间点之间均有显著差异(P<0...     

单室微生物电解池除镍途径分析及微生物群落动态特征北大核心CSCD

【目的】为探究UASB颗粒污泥启动的单室微生物电解池(Single-chamber microbial electrolysis cell,SMEC)对Ni(II)的去除途径和SMEC中微生物群落的动态特征。【方法】以乙酸钠为底物,采用单因子控制方法分析SMEC对Ni(II)的去除途径和应用Illumina高通量测序技术解析SMEC启动过程中微生物群落的组成和结构动态学特征。【结果】结果表明,SMEC对重金属的去除主要通过吸附和微生物作用。经培养驯化功能菌群发生变化。成熟单室微生物燃料电池(Single-chamber microbial fuel cell,SMFC)阳极生物膜菌群主要是Proteobacteria(变形菌门,91.42%)中的Geobacter sp.(地杆菌属,76.25%);阴极生物膜菌群主要是Bacteroidetes(拟杆菌门,47.99%)中的Niabella sp.(布鲁氏菌属,33.01%)和Proteobacteria(45.74%)中的Ochrobactrum sp.(苍白杆菌属,10.80%)。成熟SMFC改装成的SMEC在12.5 mg-Ni(II)/L下,阳极生物膜菌群由单一优势菌Geobacter sp.转变为Geobacter sp.(41.56%)和Proteobacteria中的Azospirillum sp.(固氮螺菌属,5.97%);阴极生物膜菌群由Niabella sp.和Ochrobactrum sp.转变为Firmicutes(厚壁菌门,25.21%)中的Acetoanaerobium sp.(19.28%)、Proteobacteria(51.42%)中的Dokdonella sp.(16.48%)和Azospirillum sp.(9.49%)。【结论】本研究表明,污泥微生物经SMFC和SMEC驯化过程及Ni(II)的淘汰和选择,在电极上形成了稳定、高效产电与除镍菌群,优势菌群为Proteobacteria。     

Increases in soil respiration following labile carbon additions linked to rapid shifts in soil microbial community composition

Organic matter decomposition and soil CO₂ efflux are both mediated by soil microorganisms, but the potential effects of temporal variations in microbial community composition are not considered in most analytical models of these two important processes. However, inconsistent relationships between rates of heterotrophic soil respiration and abiotic factors, including temperature and moisture, suggest that microbial community composition may be an important regulator of soil organic matter (SOM) decomposition and CO₂ efflux. We performed a short-term (12-h) laboratory incubation experiment using tropical rain forest soil amended with either water (as a control) or dissolved organic matter (DOM) leached from native plant litter, and analyzed the effects of the treatments on soil respiration and microbial community composition. The latter was determined by constructing clone libraries of small-subunit ribosomal RNA genes (SSU rRNA) extracted from the soil at the end of the incubation experiment. In contrast to the subtle effects of adding water alone, additions of DOM caused a rapid and large increase in soil CO₂ flux. DOM-stimulated CO₂ fluxes also coincided with profound shifts in the abundance of certain members of the soil microbial community. Our results suggest that natural DOM inputs may drive high rates of soil respiration by stimulating an opportunistic subset of the soil bacterial community, particularly members of the Gammaproteobacteria and Firmicutes groups. Our experiment indicates that variations in microbial community composition may influence SOM decomposition and soil respiration rates, and emphasizes the need for in situ studies of how natural variations in microbial community composition regulate soil biogeochemical processes.     

典型冷暖季沉水植物凋落物分解特性及沉积物微生物群落变化

为研究湿地沉水植物腐败分解对水体的污染状况,选择典型沉水植物金鱼藻（暖季植物）和菹草（冷季植物）进行了为期60 d的凋落物分解实验。结果表明金鱼藻和菹草凋落物分解规律相似,0—15 d快速分解,15—60 d缓慢分解,60 d凋落物失重率分别达到60.43%和66.72%。菹草的有机物释放量明显高于金鱼藻,N和P释放量相反,分解释放的N主要是NH4+-N和有机氮。三维荧光光谱（Excitation-Emission Matrix Spectroscopy, EEMs）结合平行因子分析法解析出一种类色氨酸物质C2和3种类腐殖质物质C1、C3、C4,易降解的类色氨酸有机物先增加后减少,难降解的类富里酸和类腐殖酸有机物逐渐增加。EEMs和四种组分的最大荧光强度百分比表明,溶解性有机物（Dissolved organic matter, DOM）在0—15 d以易降解有机物为主,15—60 d以难降解有机物为主。两种植物凋落物分解释放的DOM含量及特性不同,整体上呈低腐殖化特征,可能是水中难降解DOM的一个重要来源。植物凋落物的分解促进了沉积物中微生物的丰富度,降低了微生物的多样性;参与分解的主要微生物包括4 d时的Pseudomonas属（26%—35%）、15 d和30 d时的Malikia属（>8%）和Bacillus属（2.6%—9%）,分解难降解有机物的微生物逐渐增加,如Flavobacterium属;沉积物中微生物群落结构的变化受营养物质可利用性变化的影响。分析发现植物凋落物分解对水质的影响具有阶段性,0—15 d,N和P释放量增加暂时导致了水质恶化;15—60 d,N和P释放量降低,难降解有机物含量逐渐增加,可能会加剧水体甚至是沉积物的腐殖化程度。因此,在植物衰亡期应及时打捞或者做好植物平衡收割管理,避免因植物大量腐败导致水质恶化。     

Analysis of the bacterial community developing in the course of Sphagnum moss decomposition

Slow degradation of organic matter in acidic Sphagnum peat bogs suggests a limited activity of organotrophic microorganisms. Monitoring of the Sphagnum debris decomposition in a laboratory simulation experiment showed that this process was accompanied by a shift in the water color to brownish due to accumulation of humic substances and by the development of a specific bacterial community with a density of 2.4 x 10(7) cells ml(-1). About half of these organisms are metabolically active and detectable with rRNA-specific oligonucleotide probes. Molecular identification of the components of this microbial community showed the numerical dominance of bacteria affiliated with the phyla Alphaproteobacteria, Actinobacteria, and Phanctomycetes. The population sizes of Firmicutes and Bacteroidetes, which are believed to be the main agents of bacterially-mediated decomposition in eutrophic wetlands, were low. The numbers of planctomycetes increased at the final stage of Sphagnum decomposition. The representative isolates of Alphaproteobacteria were able to utilize galacturonic acid, the only low-molecular-weight organic compound detected in the water samples; the representatives of Planctomycetes were able to decompose some heteropolysaccharides, which points to the possible functional role of these groups of microorganisms in the community under study. Thus, the composition of the bacterial community responsible for Sphagnum decomposition in acidic and low-mineral oligotrophic conditions seems to be fundamentally different from that of the bacterial community which decomposes plant debris in eutrophic ecosystems at neutral pH.     

The Effects of Soil Bacterial Community Structure on Decomposition in a Tropical Rain Forest

Soil microorganisms are key drivers of terrestrial biogeochemical cycles, yet it is still unclear how variations in soil microbial community composition influence many ecosystem processes. We investigated how shifts in bacterial community composition and diversity resulting from differences in carbon (C) availability affect organic matter decomposition by conducting an in situ litter manipulation experiment in a tropical rain forest in Costa Rica. We used bar-coded pyrosequencing to characterize soil bacterial community composition in litter manipulation plots and performed a series of laboratory incubations to test the potential functional significance of community shifts on organic matter decomposition. Despite clear effects of the litter manipulation on soil bacterial community composition, the treatments had mixed effects on microbial community function. Distinct communities varied in their ability to decompose a wide range of C compounds, and functional differences were related to both the relative abundance of the two most abundant bacterial sub-phyla (Acidobacteria and Alphaproteobacteria) and to variations in bacterial alpha-diversity. However, distinct communities did not differ in their ability to decompose native dissolved organic matter (DOM) substrates that varied in quality and quantity. Our results show that although resource-driven shifts in soil bacterial community composition have the potential to influence decomposition of specific C substrates, those differences may not translate to differences in DOM decomposition rates in situ. Taken together, our results suggest that soil bacterial communities may be either functionally dissimilar or equivalent during decomposition depending on the nature of the organic matter being decomposed.     

Uncoupling of Bacterial and Terrigenous Dissolved Organic Matter Dynamics in Decomposition Experiments

The biodegradability of terrigenous dissolved organic matter (tDOM) exported to the sea has a major impact on the global carbon cycle, but our understanding of tDOM bioavailability is fragmentary. In this study, the effects of preparative tDOM isolation on microbial decomposition were investigated in incubation experiments consisting of mesocosms containing mesohaline water from the Baltic Sea. Dissolved organic carbon (DOC) consumption, molecular DOM composition, bacterial activities, and shifts in bacterial community structure were compared between mesocosms supplemented with riverine tDOM, either as filtered, particle-free river water or as a concentrate obtained by lyophilization/tangential ultrafiltration, and those containing only Baltic Sea water or river water. As shown using ultra-high-resolution mass spectrometry (15 Tesla Fourier-transform ion cyclotron resonance mass spectrometry, FT-ICR-MS) covering approximately 4600 different DOM compounds, the three DOM preparation protocols resulted in distinct patterns of molecular DOM composition. However, despite DOC losses of 4–16% and considerable bacterial production, there was no significant change in DOM composition during the 28-day experiment. Moreover, tDOM addition affected neither DOC degradation nor bacterial dynamics significantly, regardless of the tDOM preparation. This result suggested that the introduced tDOM was largely not bioavailable, at least on the temporal scale of our experiment, and that the observed bacterial activity and DOC decomposition mainly reflected the degradation of unknown, labile, colloidal and low-molecular weight DOM, both of which escape the analytical window of FT-ICR-MS. In contrast to the different tDOM preparations, the initial bacterial inoculum and batch culture conditions determined bacterial community succession and superseded the effects of tDOM addition. The uncoupling of tDOM and bacterial dynamics suggests that mesohaline bacterial communities cannot efficiently utilize tDOM and that in subarctic estuaries other factors are responsible for the removal of imported tDOM.     

The role of dissolved organic matter bioavailability in promoting phytoplankton blooms in Florida Bay

The clear, shallow, oligotrophic waters of Florida Bay are characterized by low phytoplankton biomass, yet periodic cyanobacteria and diatom blooms do occur. We hypothesized that allochthonous dissolved organic matter (DOM) was providing a subsidy to the system in the form of bound nutrients. Water from four bay sites was incubated under natural light and dark conditions with enrichments of either DOM ( > 1 kD, 2×DOM) or inorganic nutrients (N+P). Samples were analyzed for bacterial numbers, bacterial production, phytoplankton biomass, phytoplankton community structure, and production, nutrients, and alkaline phosphatase (AP) activity. The influence of 2×DOM enrichment on phytoplankton biomass developed slowly during the incubations and was relatively small compared to nutrient additions. Inorganic nutrient additions resulted in an ephemeral bloom characterized initially as cyanobacterial and brown algae but which changed to dinoflagellate and/or brown algae by day six. The DIN:TP ratio decreased 10-fold in the N+P treatments as the system progressed towards N limitation. This ratio did not change significantly for 2×DOM treatments. In addition, these experiments indicated that both autotrophic and heterotrophic microbial populations in Florida Bay may fluctuate in their limitation by organic and inorganic nutrient availability. Both N+P and 2×DOM enrichments revealed significant and positive response in bioavailability of dissolved organic carbon (BDOC). Potential BDOC ranged from 1.1 to 35.5%, with the most labile forms occurring in Whipray Basin. BDOC at all sites was stimulated by the 2×DOM addition. Except for Duck Key, BDOC at all sites was also stimulated by the addition of N+P. BDOC was lower in the dry season than in the wet season (5.56% vs. 16.86%). This may be explained by the distinct chemical characteristics of the DOM produced at different times of year. Thus, both the heterotrophic and autotrophic microbial communities in Florida Bay are modulated by bioavailability of DOM. This has ramifications for the fate of DOM from the Everglades inputs, implicating DOM bioavailability as a contributing factor in regulating the onset, persistence, and composition of phytoplankton blooms.     

深圳大鹏湾海域锥状斯氏藻赤潮期间细菌群落结构变化研究

目的:近年来,赤潮在我国的发生呈增加的趋势,并造成了极大的经济损失。过去研究赤潮发生的机理主要集中在理化因素的影响,而越来越多的证据表明仅凭借营养盐等环境因素并不能解释大部分赤潮现象,藻际微生物可能发挥着重要作用。本文跟踪观测了2010年7月深圳大鹏湾海域爆发的锥状斯氏藻赤潮生消过程中细菌群落丰度种类的变化,从微生物与赤潮藻相互作用的角度探讨了赤潮的生消过程,讨论了不同时期不同关键菌群的特殊作用,为解释赤潮爆发和消亡提供了新的视角,为赤潮的监控和防治新方法的建立奠定了理论基础。方法:本文按时间顺序共采集该赤潮9次样本,利用末端限制性酶切片段长度多态性分析(T-RFLP)等分子生物学方法,通过主成分分析、克隆文库的构建,研究了微生物群落的变化过程,并探讨了特定种属的微生物在赤潮发生、发展和消亡过程中的作用。结果:从浮游细菌丰度来看,随着锥状斯氏藻细胞数量的波动,浮游细菌总数也随之呈现相应的变化。从浮游细菌的种类来看,它们主要属于变形杆菌门(Proteobacteria)、拟杆菌门(Bacteroidetes)和厚壁菌门(Firmicutes)。从浮游细菌的动态变化过程来看,赤潮生消过程中,浮游细菌群落呈现出一定的演替现象,特别是在赤潮后期,群落主成分变化尤为显著。从关键菌群的作用来看,属于γ变形杆菌门的Alteromonas sp.一直占有较高的丰度,赤潮中后期受到菌群相互作用导致比例下降,而赤潮后期其他关键菌群的丰度的增高可能是导致赤潮消亡的重要原因。结论:本文利用T-RFLP这一DNA指纹技术分析微生物群落结构和多样性特征,通过研究赤潮生消过程中藻际浮游细菌群落的动态变化,发现随着赤潮的发展,浮游细菌群落发生着相应的变化。结果说明赤潮藻体丰度数量的改变影响着浮游细菌群落的组成。相对地,细菌群落的适应调整迅速造成赤潮藻体局部生长环境的改变,从而影响赤潮的发展过程。     

Plant Communities, Soil Microorganisms, and Soil Carbon Cycling: Does Altering the World Belowground Matter to Ecosystem Functioning?

Soil microorganisms mediate many critical ecosystem processes. Little is known, however, about the factors that determine soil microbial community composition, and whether microbial community composition influences process rates. Here, we investigated whether aboveground plant diversity affects soil microbial community composition, and whether differences in microbial communities in turn affect ecosystem process rates. Using an experimental system at La Selva Biological Station, Costa Rica, we found that plant diversity (plots contained 1, 3, 5, or > 25 plant species) had a significant effect on microbial community composition (as determined by phospholipid fatty acid analysis). The different microbial communities had significantly different respiration responses to 24 labile carbon compounds. We then tested whether these differences in microbial composition and catabolic capabilities were indicative of the ability of distinct microbial communities to decompose different types of litter in a fully factorial laboratory litter transplant experiment. Both microbial biomass and microbial community composition appeared to play a role in litter decomposition rates. Our work suggests, however, that the more important mechanism through which changes in plant diversity affect soil microbial communities and their carbon cycling activities may be through alterations in their abundance rather than their community composition.     

Vertebrate Decomposition Is Accelerated by Soil Microbes

Carrion decomposition is an ecologically important natural phenomenon influenced by a complex set of factors, including temperature, moisture, and the activity of microorganisms, invertebrates, and scavengers. The role of soil microbes as decomposers in this process is essential but not well understood and represents a knowledge gap in carrion ecology. To better define the role and sources of microbes in carrion decomposition, lab-reared mice were decomposed on either (i) soil with an intact microbial community or (ii) soil that was sterilized. We characterized the microbial community (16S rRNA gene for bacteria and archaea, and the 18S rRNA gene for fungi and microbial eukaryotes) for three body sites along with the underlying soil (i.e., gravesoils) at time intervals coinciding with visible changes in carrion morphology. Our results indicate that mice placed on soil with intact microbial communities reach advanced stages of decomposition 2 to 3 times faster than those placed on sterile soil. Microbial communities associated with skin and gravesoils of carrion in stages of active and advanced decay were significantly different between soil types (sterile versus untreated), suggesting that substrates on which carrion decompose may partially determine the microbial decomposer community. However, the source of the decomposer community (soil- versus carcass-associated microbes) was not clear in our data set, suggesting that greater sequencing depth needs to be employed to identify the origin of the decomposer communities in carrion decomposition. Overall, our data show that soil microbial communities have a significant impact on the rate at which carrion decomposes and have important implications for understanding carrion ecology.