施肥方式对干旱半干旱地区土壤氨氧化微生物数量和群落的影响

氨氧化是硝化作用的限速步骤,也是评估土壤氮循环和提高氮肥利用效率的重要指标。以内蒙古农牧业科学院旱作实验站长期定位实验为基础,通过实时荧光定量PCR和末端限制性片段长度多态性分析,研究了5种施肥方式（单施氮肥、单施有机肥、氮磷钾配施、有机无机配施和不施肥）对土壤氨氧化古菌（AOA）和氨氧化细菌（AOB）群落丰度、结构和活性的影响。结果表明：单施氮肥、氮磷钾肥配施以及有机无机肥配施均能显著提高AOB的丰度以及土壤硝化潜势。Nitrosospiria cluster 3a.1是不施肥土壤中主要的AOB种群,而施用氮肥后优势种群转变为Nitrosospiria cluster 3a.2。Nitrosospiria cluster 3b的比例在施用有机肥处理土壤中显著升高。在干旱半干旱地区,土壤pH和含水量是解释AOB群落结构变化的关键环境因子。AOA的丰度在单独施用氮肥处理中显著升高,但不同施肥方式对AOA的群落结构没有显著影响。     

甘肃白银铜矿矿坑土壤细菌和古菌的多样性及坡度分布特征

【背景】甘肃白银铜矿作为西部地区的重要矿区，探究其细菌和古菌多样性及坡度分布特征对明确矿区微生物多样性分布具有关键意义。【目的】通过分析白银铜矿矿坑不同坡度的土壤细菌群落多样性和古菌群落多样性，探究不同坡度土壤样品细菌及古菌多样性与理化性质之间的关系。【方法】以不同坡度的白银铜矿土样为材料，采用Illumina HiSeq测序技术，分析样品的细菌多样性和古菌多样性。【结果】α和β多样性分析表明，ACE、Chao1、Shannon和Simpson等多样性指数在样品间存在显著差异。白银铜矿矿坑土壤的细菌排名前十的纲是Gammaproteobacteria、Oxyphotobacteria、Alphaproteobacteria、Bacteroidia、Actinobacteria、Clostridia、Nitrospira、Bacilli、Mollicutes和Acidimicrobiia，相对丰度最高的是Gammaproteobacteria。在纲水平上，白银铜矿的古菌由Thermoplasmata、Nitrososphaeria、Methanomicrobia、Halobacteria、Methanobacteria、Group_1.1c和Bathyarchaeia组成，相对丰度最高的是Thermoplasmata。冗余分析(redundancy analysis,RDA)得出，pH和速效磷是影响土壤多样性的最重要因素。【结论】白银铜矿为强酸性铜矿，其土壤铜离子含量最高。从坡顶到坡底，pH呈现先降低再升高的趋势(2.18-4.75)，铜离子(20-150mg/kg)和总铁(2.5-50mg/kg)呈现先升高后降低的趋势，铵态氮(3.61-44.90mg/kg)、速效磷(0-56.79mg/kg)和速效钾(9.07-35.65mg/kg)含量低且呈现波动趋势，硫化物(1mg/kg)无明显变化。白银铜矿矿坑土壤细菌相对丰度最高的属为Acidithiobacillus，古菌相对丰度较高的属为uncultured_bacterium_f_Ferroplasmaceae和uncultured_bacterium_f_Nitrososphaeraceae。其中，细菌多样性受到pH驱动，古菌多样性受到速效磷的驱动。本研究有助于我们进一步了解白银铜矿土壤微生物群落的变化。     

Illumina高通量测序揭示艾比湖湿地6种盐生植物根际土壤真菌群落组成及多样性

[目的] 通过研究新疆艾比湖湿地不同盐生植物根际土壤真菌的多样性和群落结构,为艾比湖湿地退化恢复工作和真菌深入研究提供理论支持。[方法] 利用高通量测序技术对真菌扩增子ITS1区进行测定,从而分析艾比湖湿地6种盐生植物根际土壤真菌群落多样性,并结合相关土壤理化因子分析环境与真菌群落多样性和丰富度的关联。[结果] 艾比湖湿地6种盐生植物根际土壤真菌群落多样性及丰富度存在差异,碱蓬根际土壤真菌多样性最高,芦苇根际土壤真菌群落丰富度最高。真菌群落组成分析表明,土壤样品中真菌菌落主要隶属于子囊菌门（Ascomycota）和担子菌门（Basidiomycota）,其中子囊菌门为主要优势菌门;链格孢霉属（Alternaria）是6种植物共有的优势菌属,但是其在不同植物之间的丰度存在差异,在戟叶鹅绒藤中的丰度最高,在准噶尔大戟中的丰度最低。pH与真菌多样性呈显著负相关,全磷（TP）与真菌群落丰富度呈显著正相关,pH、电导率（EC）和有机质（OM）对优势菌属的影响最大。[结论] 艾比湖湿地6种盐生植物根际土壤真菌群落组成及多样性具有显著差异,碱蓬和芦苇根际土壤真菌的多样性和丰度高于其他植物,子囊菌门和链格孢霉属是艾比湖湿地的主要土壤真菌门属。研究结果可为艾比湖湿地的生态修复提供理论指导。     

不同风化时间碳酸岩表面古菌群落结构与功能特征

【背景】古菌群落是碳酸岩表面微生物群落的重要成员,也是碳酸岩表面生物演替的先锋生物,能够促进碳酸岩风化和加快土壤形成,在生物地球化学循环中起重要作用。【目的】揭示在不同风化时间碳酸岩表面风化残积物中的古菌群落结构及生态功能。方法】采集19-213年风化时间段废弃碳酸岩墓碑表面风化残积物样品(n=18),基于宏基因组测序技术分析其古菌群落结构与功能特征。【结果】门水平上,优势门有广古菌门(Euryarchaeota),随后为奇古菌门(Thaumarchaeota)、未鉴定古菌门(unclassified Archaea)、深古菌门(Bathyarchaeota)和泉古菌门(Crenarchaeota);属水平上,优势属主要由甲烷八叠球菌属(Methanosarcina)、甲烷丝状菌属(Methanothrix)、Methanoperedens、氨氧化古菌属(Nitrosocosmicus)、亚硝化球菌属(Nitrososphaera)及其他未鉴定属组成;C/N、C/P、N/P是显著影响碳酸岩表面古菌群落的主要环境因子。进一步分析发现,碳酸岩表面古菌群落功能丰富,其中新陈代谢(metabo...     

攀枝花不同海拔高度烤烟农田红壤中氨氧化细菌与氨氧化古菌的群落结构分析

为探究攀枝花干热河谷区农田土壤氨氧化古菌（Ammonia oxidizing archaea,AOA）与氨氧化细菌（Ammonia oxidizing bacteria,AOB）群落对海拔高度的响应特征,深入认识该区域的氮素循环过程。以攀枝花米易县不同海拔（1600 m、1800 m和2000 m）农田红壤为研究对象,运用化学分析和末端限制性片段长度多态性（Terminal restriction fragment length polymorphism,T-RFLP）分别测定土壤理化性质、AOA和AOB群落组成及多样性,研究不同海拔农田土壤中AOA和AOB群落变异及其驱动因子。研究结果显示,不同海拔农田土壤pH均小于7,土壤有机碳（SOC）、全氮（TN）、速效钾（AK）和铵态氮（NH₄⁺-N）含量随海拔升高而降低,碱解氮（AN）、有效磷（AP）和硝态氮（NO₃^--N）含量随海拔升高先增加后降低;随海拔升高,AOA群落多样性指数增加,而AOB群落多样性指数先增加后降低;AOA以亚硝基球菌属（Nitrososphaera）为优势菌群,AOB以亚硝化螺菌属（Nitrosospira）为优势菌群;土壤有机碳（SOC）、速效钾（AK）和硝态氮（NO₃^--N）是影响该区域农田土壤AOA和AOB群落发育的主要因子。总体而言,攀枝花干热河谷区不同海拔农田土壤AOA和AOB群落结构变化明显,土壤硝态氮、速效钾和有机碳是影响AOA和AOB群落结构变异的主要因子;研究结果可为揭示干热河谷区农田红壤氮循环相关微生物的海拔分布格局提供理论依据。     

EM复合菌对新疆色素辣椒生长及根际细菌群落的影响

【背景】Effective microorganisms （EM）复合菌在我国农业种植上的应用越来越广泛,但对色素辣椒的促生作用与根际细菌群落结构的影响未见报道。【目的】评估EM复合菌对新疆色素辣椒的促生长作用,并分析其对色素辣椒根际细菌群落组成的影响。【方法】通过随水灌溉方式将EM复合菌接种到色素辣椒根部,在收获期测定辣椒生长指标、土壤养分和酶活活性,明确EM复合菌对辣椒生长和土壤质量的影响;利用16S rRNA基因高通量测序技术测定EM复合菌对辣椒根系细菌群落组成和结构的影响。【结果】与对照组相比,EM复合菌的施用使辣椒株高、鲜重、单个果重和单株结果数分别提高23.89%、85.41%、42.31%和46.04%;土壤中碱解氮和速效磷含量分别提高5.83%和13.39%,土壤中脲酶、蔗糖酶和过氧化物酶的活性分别提高11.47%、9.42%和21.43%;施用EM复合菌显著改变辣椒根际微生物群落的α多样性和β多样性,提高有益菌群变形菌门（Proteobacteria）、酸杆菌门（Acidobacteria）、芽单胞菌门（Gemmatimonadetes）、放线菌门（Actinobacteria）和厚壁菌门（Firmicutes）的相对丰度,其中变形菌门黄单胞菌科（Xanthomonadaceae）的相对丰度增加119.32%;在属的水平上,施用EM复合菌显著增加了藤黄色杆菌属（Luteitalea）、藤黄单胞菌属（Luteimonas）、鞘脂单胞菌属（Sphingobacterium）和盐单胞菌属（Halomonas）的相对丰度,尤其是藤黄单胞菌属的丰度提高244.17%,同时显著降低黄杆菌属（Flavobacterium）的相对丰度。此外,与土壤理化指标呈正相关的微生物菌群相对丰度也显著升高。【结论】EM复合菌能够通过提高土壤营养成分与酶活活性,调控根系微生物群落结构,富集大量在盐碱地生存能力较强的有益菌群,进而起到促进色素辣椒生长的功效。     

基于Illumina MiSeq测序技术对冰川棘豆(Oxytropis glacialis)不同组织内生菌多样性的研究

植物内生菌（Endophyte）在宿主植物组织中的分布规律是内生菌对外界适应的重要机制。基于Illumina MiSeq测序技术,对适应青藏高原极端环境的主要疯草植物-冰川棘豆叶和根组织中的内生菌16S rRNA、ITS rDNA进行高通量测序和生物信息学分析,通过明晰内生菌在冰川棘豆组织中的菌群结构、功能以及环境之间的关系,探讨了组织间内生菌的分布特征对冰川棘豆适应极端环境的可能影响。分析结果表明,冰川棘豆组织间共有菌属丰度占菌属总丰度90%以上,不同组织间形成了保守性内生细菌和特异性内生真菌共存的群落结构特点,植物组织结构和环境的影响可能为推动内生菌选择合适的组织生态位定植提供动力,其中土壤含水量显著影响内生细菌（R²=0.241,P=0.024）和内生真菌（R²=0.223,P=0.031）的组间Beta多样性,土壤pH值显著影响内生真菌（R²=0.571,P < 0.001）Alpha多样性丰富度指数,而环境因素对组织间存在显著差异的内生菌功能和营养型解释并不显著。综合认为,保守性与差异性的内生菌菌群结构和功能为植物不同组织适应极端环境提供帮助,这有利于冰川棘豆的生存与扩散。     

不同季节艾比湖湿地盐角草根际nirS-型与nirK-型反硝化细菌群落组成分析

旨在了解艾比湖湿地盐生植物盐角草根际与非根际中不同类型反硝化细菌的分布及其随季节变化情况,为温带干旱地区荒漠盐化生态系统的代表-艾比湖湿地在生态植被恢复过程中,由微生物推动的土壤氮素循环过程提供数据支撑。采集了艾比湖湿地夏、秋、春三个季节的盐角草根际和非根际土壤样本,通过高通量测序技术,比较分析了nirS-型和nirK-型两种类型的反硝化细菌的多样性和群落结构特点;利用RDA (redundancy analysis)探究了土壤理化因素对反硝化细菌多样性及群落结构的影响。艾比湖湿地盐角草根际与非根际中,nirS-型和nirK-型反硝化细菌多样性最高的为秋季根际土壤样本;各土壤样本中的反硝化细菌多样性均呈现根际>非根际。盐角草各土壤样本中的nirS-型反硝化细菌在门分类水平上隶属于变形菌门(Proteobacteria),厚壁菌门(Firmicutes)和放线菌门(Actinobacteria),而nirK-型反硝化细菌在门水平上分类仅包括了Proteobacteria和Firmicutes。Proteobacteria在各土壤样本中的占比均较高;其中Gamma-Proteobacteria的盐单胞菌属(Halomonas)和假单胞菌属(Pseudomonas)是各土壤样本所共有的nirS-型反硝化菌的优势菌属,但它们在每个土壤样本中的相对丰度各有差异。Alpha-Proteobacteria的根瘤菌属(Rhizobium)是盐角草各土壤样本中较为广泛存在的nirK-型反硝化细菌。艾比湖湿地盐角草各土壤样本中的反硝化细菌群落结构存在着一定的差异。RDA结果显示含水量、有机质、全氮和铵态氮等对各土壤样本中的nirS-型反硝化细菌的多样性影响较大,含水量、有机质、全氮、碱解氮等是nirK-型反硝化细菌多样性的主要影响因素。土壤电导率、全磷、全钾、全氮和碱解氮协同影响nirS-型反硝化细菌的群落结构,有机质、速效钾、速效磷、pH和硝态氮是nirK-型反硝化细菌群落结构组成的主要影响因素。艾比湖湿地反硝化细菌呈现季节性变化,nirS-型和nirK-型反硝化细菌以不同的主要菌属,共同推进湿地反硝化作用。而对于湿地生态系统的保护,则需要进行长期而广泛的土壤状态评估和土壤反硝化微生物菌群的动态监测。     

长期集约种植对雷竹林土壤氨氧化古菌群落的影响

应用荧光定量PCR以及PCR-DGGE技术研究了雷竹林长期集约种植过程中土壤氨氧化古菌种群数量及群落结构的演变趋势,并利用典范对应分析(CCA)方法研究影响土壤氨氧化古菌群落的主要环境因子。研究结果表明,水稻田改种雷竹后,土壤氨氧化古菌种群数量显著增加,在4 a时达到最高,但在集约种植后快速下降,9 a雷竹林土壤氨氧化古菌数量最低,随后逐渐稳定。雷竹林土壤氨氧化古菌种群主要为不可培养泉古菌,聚类分析结果表明集约种植前后氨氧化古菌群落结构存在明显差异,长期集约经营雷竹林土壤以适应较低pH值的物种为主要优势种群。CCA分析表明,集约种植时间较长的11 a和15 a林地群落结构较为类似,与7 a和9 a样地明显区分。土壤NO-3-N与氨氧化古菌群落变化的相关性最强,说明氨氧化古菌在雷竹林土壤硝化过程中发挥着重要作用。土壤pH值及速效养分对土氨氧化古菌群落也具有较大影响,它们与NO-3-N合计解释了59.7%的样本总变异,表明土壤酸化以及过量养分的积累对氨氧化古菌群落具有重要影响。     

亚热带不同林分土壤氨氧化菌群落特征

为揭示亚热带不同森林类型对土壤氨氧化菌群落特征的影响,采用荧光定量PCR以及PCR-DGGE技术研究了阔叶林、杉木林、马尾松林和毛竹林土壤氨氧化古菌和细菌丰度及古菌群落结构特征.结果表明:不同林分土壤中氨氧化古菌数量(1.62×106~1.88×107个·g-1干土)高于相应土壤中的氨氧化细菌(2.41×105~4.36×105个·g-1干土);毛竹林土壤氨氧化古菌数量显著高于杉木林,而后者又显著高于阔叶林和马尾松林,但氨氧化细菌数量在不同林分之间没有显著差异.DGGE图谱分析表明,不同林分土壤中氨氧化古菌的物种有所差异,且毛竹林和杉木林土壤古菌群落结构迥异.氨氧化古菌在亚热带主要林分土壤中表现出明显优势,且除植被类型外,土壤速效钾、pH和有机质是引起土壤氨氧化古菌群落结构及多样性变异的主要因素.     

Elevational patterns in archaeal diversity on mt. Fuji

Little is known of how archaeal diversity and community ecology behaves along elevational gradients. We chose to study Mount Fuji of Japan as a geologically and topographically uniform mountain system, with a wide range of elevational zones. PCR-amplified soil DNA for the archaeal 16 S rRNA gene was pyrosequenced and taxonomically classified against EzTaxon-e archaeal database. At a bootstrap cut-off of 80%, most of the archaeal sequences were classified into phylum Thaumarchaeota (96%) and Euryarchaeota (3.9%), with no sequences classified into other phyla. Archaeal OTU richness and diversity on Fuji showed a pronounced 'peak' in the mid-elevations, around 1500 masl, within the boreal forest zone, compared to the temperate forest zone below and the alpine fell-field and desert zones above. Diversity decreased towards higher elevations followed by a subtle increase at the summit, mainly due to an increase in the relative abundance of the group I.1b of Thaumarchaeota. Archaeal diversity showed a strong positive correlation with soil NH(4) (+), K and NO(3) (-) (.) Archaeal diversity does not parallel plant diversity, although it does roughly parallel bacterial diversity. Ecological hypotheses to explain the mid diversity bulge on Fuji include intermediate disturbance effects, and the result of mid elevations combining a mosaic of upper and lower slope environments. Our findings show clearly that archaeal soil communities are highly responsive to soil environmental gradients, in terms of both their diversity and community composition. Distinct communities of archaea specific to each elevational zone suggest that many archaea may be quite finely niche-adapted within the range of soil environments. A further interesting finding is the presence of a mesophilic component of archaea at high altitudes on a mountain that is not volcanically active. This emphasizes the importance of microclimate - in this case solar heating of the black volcanic ash surface - for the ecology of soil archaea.     

Molecular signatures for the Crenarchaeota and the Thaumarchaeota

Crenarchaeotes found in mesophilic marine environments were recently placed into a new phylum of Archaea called the Thaumarchaeota. However, very few molecular characteristics of this new phylum are currently known which can be used to distinguish them from the Crenarchaeota. In addition, their relationships to deep-branching archaeal lineages are unclear. We report here detailed analyses of protein sequences from Crenarchaeota and Thaumarchaeota that have identified many conserved signature indels (CSIs) and signature proteins (SPs) (i.e., proteins for which all significant blast hits are from these groups) that are specific for these archaeal groups. Of the identified signatures 6 CSIs and 13 SPs are specific for the Crenarchaeota phylum; 6 CSIs and >250 SPs are uniquely found in various Thaumarchaeota (viz. Cenarchaeum symbiosum, Nitrosopumilus maritimus and a number of uncultured marine crenarchaeotes) and 3 CSIs and ~10 SPs are found in both Thaumarchaeota and Crenarchaeota species. Some of the molecular signatures are also present in Korarchaeum cryptofilum, which forms the independent phylum Korarchaeota. Although some of these molecular signatures suggest a distant shared ancestry between Thaumarchaeota and Crenarchaeota, our identification of large numbers of Thaumarchaeota-specific proteins and their deep branching between the Crenarchaeota and Euryarchaeota phyla in phylogenetic trees shows that they are distinct from both Crenarchaeota and Euryarchaeota in both genetic and phylogenetic terms. These observations support the placement of marine mesophilic archaea into the separate phylum Thaumarchaeota. Additionally, many CSIs and SPs have been found that are specific for different orders within Crenarchaeota (viz. Sulfolobales—3 CSIs and 169 SPs, Thermoproteales—5 CSIs and 25 SPs, Desulfurococcales—4 SPs, and Sulfolobales and Desulfurococcales—2 CSIs and 18 SPs). The signatures described here provide novel means for distinguishing the Crenarchaeota and the Thaumarchaeota and for the classification of related and novel species in different environments. Functional studies on these signature proteins could lead to discovery of novel biochemical properties that are unique to these groups of archaea.     

健康与感染青枯病烟株根际土壤与茎秆细菌群落结构与多样性

【目的】了解健康烟株与感染青枯病烟株在根际土壤、茎杆发病部位、茎杆病健交界部位以及未发病茎杆的细菌群落结构与多样性。【方法】分别对土壤与茎杆样品中细菌的16S rRNA基因V3-V4区进行扩增,采用Illumina MiSeq测序技术对扩增片段进行高通量测序,然后对健康烟株与感染青枯病烟株不同部位细菌群落结构与多样性进行分析。【结果】感染青枯病烟株发病茎杆及根际土壤的细菌群落多样性高于健康烟株茎杆及其根际土壤样品,病健交界茎杆样品细菌群落多样性低于健康烟株。变形菌门(Proteobacteria)在所有样品中均为优势菌门;所有烟株根际土壤的优势菌门为拟杆菌门(Bacteroidetes)、酸杆菌门(Acidobacteria)、放线菌门(Actinobacteria)和绿弯菌门(Chloroflexi);健康烟株茎杆部位的优势菌门为蓝细菌门(Cyanobacteria);感染青枯病烟株发病茎杆和病健交界茎杆部位的优势菌门为蓝细菌门(Cyanobacteria)和厚壁菌门(Firmicutes)。所有根际土壤样品的优势菌属为劳尔氏菌属(Ralstonia)、假单胞菌属(Pseudomonas)、鞘脂单胞菌属(Sphingomonas)、黄杆菌属(Flavobacterium)和代尔夫特菌属(Delftia),而感染青枯病烟株根际土壤的劳尔氏菌属(Ralstonia)和假单胞菌属(Pseudomonas)相对丰度显著高于健康烟株根际土壤,鞘脂单胞菌属相对丰度显著低于健康烟株根际土壤。烟株茎杆的优势菌属为劳尔氏菌属和假单胞菌属等。感染青枯病烟株病健交界茎杆中劳尔氏菌属、肠杆菌属(Enterobacter)和泛菌属(Pantoea)相对丰度显著低于健康烟株样品。【结论】健康与感染青枯病烟株茎杆样品细菌群落的丰富度和多样性明显低于相应的根际土壤样品。较健康烟株而言,感染青枯病烟株根际土壤和茎杆样品细菌群落丰富度和多样性均表现出不同程度地增加,且根际土壤细菌群落结构变化较茎杆样品明显,而病健交界茎杆样品细菌群落丰富度和多样性降低。烟草青枯病为典型土传病害,其病原茄科劳尔氏菌尽管能在烟株维管束中蔓延扩增,但主要还是分布于土壤中;它的存在似乎对土壤细菌群落的影响大于茎杆样品的。该研究结果提示对于青枯病的防治不能局限于烟株本身,田间土壤也应加大防治力度。     

Phylogenetic congruence and ecological coherence in terrestrial Thaumarchaeota

Thaumarchaeota form a ubiquitously distributed archaeal phylum, comprising both the ammonia-oxidising archaea (AOA) and other archaeal groups in which ammonia oxidation has not been demonstrated (including Group 1.1c and Group 1.3). The ecology of AOA in terrestrial environments has been extensively studied using either a functional gene, encoding ammonia monooxygenase subunit A (amoA) or 16S ribosomal RNA (rRNA) genes, which show phylogenetic coherence with respect to soil pH. To test phylogenetic congruence between these two markers and to determine ecological coherence in all Thaumarchaeota, we performed high-throughput sequencing of 16S rRNA and amoA genes in 46 UK soils presenting 29 available contextual soil characteristics. Adaptation to pH and organic matter content reflected strong ecological coherence at various levels of taxonomic resolution for Thaumarchaeota (AOA and non-AOA), whereas nitrogen, total mineralisable nitrogen and zinc concentration were also important factors associated with AOA thaumarchaeotal community distribution. Other significant associations with environmental factors were also detected for amoA and 16S rRNA genes, reflecting different diversity characteristics between these two markers. Nonetheless, there was significant statistical congruence between the markers at fine phylogenetic resolution, supporting the hypothesis of low horizontal gene transfer between Thaumarchaeota. Group 1.1c Thaumarchaeota were also widely distributed, with two clusters predominating, particularly in environments with higher moisture content and organic matter, whereas a similar ecological pattern was observed for Group 1.3 Thaumarchaeota. The ecological and phylogenetic congruence identified is fundamental to understand better the life strategies, evolutionary history and ecosystem function of the Thaumarchaeota.     

Two Invasive Plants Alter Soil Microbial Community Composition in Serpentine Grasslands

Plant invasions pose a serious threat to native ecosystem structure and function. However, little is known about the potential role that rhizosphere soil microbial communities play in facilitating or resisting the spread of invasive species into native plant communities. The objective of this study was to compare the microbial communities of invasive and native plant rhizospheres in serpentine soils. We compared rhizosphere microbial communities, of two invasive species, Centaurea solstitialis (yellow starthistle) and Aegilops triuncialis (barb goatgrass), with those of five native species that may be competitively affected by these invasive species in the field (Lotus wrangelianus, Hemizonia congesta, Holocarpha virgata, Plantago erecta, and Lasthenia californica). Phospholipid fatty acid analysis (PLFA) was used to compare the rhizosphere microbial communities of invasive and native plants. Correspondence analyses (CA) of PLFA data indicated that despite yearly variation, both starthistle and goatgrass appear to change microbial communities in areas they invade, and that invaded and native microbial communities significantly differ. Additionally, rhizosphere microbial communities in newly invaded areas are more similar to the original native soil communities than are microbial communities in areas that have been invaded for several years. Compared to native plant rhizospheres, starthistle and goatgrass rhizospheres have higher levels of PLFA biomarkers for sulfate reducing bacteria, and goatgrass rhizospheres have higher fatty acid diversity and higher levels of biomarkers for sulfur-oxidizing bacteria, and arbuscular mycorrhizal fungi. Changes in soil microbial community composition induced by plant invasion may affect native plant fitness and/or ecosystem function.     

Different Effects of Transgenic Maize and Nontransgenic Maize on Nitrogen-Transforming Archaea and Bacteria in Tropical Soils

The composition of the rhizosphere microbiome is a result of interactions between plant roots, soil, and environmental conditions. The impact of genetic variation in plant species on the composition of the root-associated microbiota remains poorly understood. This study assessed the abundances and structures of nitrogen-transforming (ammonia-oxidizing) archaea and bacteria as well as nitrogen-fixing bacteria driven by genetic modification of their maize host plants. The data show that significant changes in the abundances (revealed by quantitative PCR) of ammonia-oxidizing bacterial and archaeal communities occurred as a result of the maize host being genetically modified. In contrast, the structures of the total communities (determined by PCR-denaturing gradient gel electrophoresis) were mainly driven by factors such as soil type and season and not by plant genotype. Thus, the abundances of ammonia-oxidizing bacterial and archaeal communities but not structures of those communities were revealed to be responsive to changes in maize genotype, allowing the suggestion that community abundances should be explored as candidate bioindicators for monitoring the possible impacts of cultivation of genetically modified plants.     

黄河三角洲不同类型盐生植物土壤真菌群落结构特征

盐生植物种类及其所具有的不同耐盐调节方式影响着根际微生物群落的结构与组成。为明确不同类型盐生植物根际与非根际土壤中真菌群落结构与组成的差异及其与土壤环境间的相互关系,该研究采集了黄河三角洲地区芦苇、盐地碱蓬、獐毛3种不同类型盐生植物0~20 cm土层的根际和非根际土壤,通过高通量测序对其真菌群落多样性和结构进行了分析,以探究真菌群落特征与土壤理化因子间的关系。结果表明：(1)3种不同类型盐生植物根际土壤真菌群落丰富度显著大于各自非根际土,且獐毛根际土壤真菌群落丰富度显著大于芦苇和盐地碱蓬的根际土。(2)距离热图分析表明,芦苇和盐地碱蓬非根际土壤真菌群落间的相似性最大。(3)土壤真菌多样性和丰富度与土壤总碳、总氮、有效磷、pH呈正相关关系,与土壤盐分含量呈负相关关系。(4)3种不同类型盐生植物的根际与非根际土壤中,球囊菌门(Glomeromycota)均为绝对优势门,盾巨孢囊霉属(Scutellospora)为优势属。(5)RDA分析表明,土壤盐分含量是影响土壤真菌群落结构的重要因子,球囊菌门丰度与土壤总氮、总碳、有效磷、有机碳、pH呈正相关关系,与盐分呈负相关关系。(6)植物土壤真菌群落特征随盐生植物类型的变化以及样本土壤距宿主植物根系远近存在差异。     

雅鲁藏布江下游沿岸湿地建群种植物根际土壤细菌群落结构和多样性特征

了解雅鲁藏布江大峡谷沿岸不同植被根际土壤细菌群落结构和多样性特征对于揭示该区植被与土壤的相互作用具有重要科学意义。采用Illumina Miseq高通量测序技术,研究了雅鲁藏布江沿岸自然分布和生长的艾草Artemisia argyi H. Lév.&Vaniot、白刺花Sophora davidii(Franch)、八宝Hylotelephium erythrostictum(Miq.)H. Ohba、黄刺玫Rosa xanthina Lindl4种典型植被根际土壤细菌群落结构和多样性,并结合植物根际土壤养分含量进行相关性分析。雅鲁藏布江沿岸4种植物根际土壤中共有28门、84纲、156目、262科、599属土壤细菌,其中变形菌门、酸杆菌门、放线菌门是雅鲁藏布江岸边植物根际土壤的优势菌群,相对丰度较高,其次为拟杆菌门、芽单胞菌门、疣微菌门。在门水平上,4种植物根际土壤细菌的群落结构组成表现为黄刺玫和艾草相似,而八宝和另外三种植物相差较大。土壤细菌OTUs(操作分类单元)数和Chaol均以艾草为最高,其值分别是6695和8000.02,以白刺花为最低,其值分别是4563和5113....     

一个新的古菌类群———奇古菌门(Thaumarchaeota)

基于16S rRNA基因的系统发育关系,古菌域(Archaea)被分为两个主要类群:广古菌门(Euryarchaeota)和泉古菌门(Crenarchaeota)。近20年来,微生物分子生态学技术的快速发展和应用显示,在中温环境中广泛存在着大量的未培养古菌,而且它们可能在自然界重要元素(N、C)的生物地球化学循环中发挥着重要作用。最初,这些未培养古菌因在16S rRNA基因系统发育上与泉古菌关系较密切而被称作中温泉古菌(non-thermophilic Crenarchaeota)。而近年来,对更多新发现的中温古菌核糖体RNA基因序列和其它分子标记物进行的分析均不支持中温泉古菌由嗜热泉古菌进化而来的假设,而揭示其可能代表古菌域中一个独立的系统发育分支。基因组学、生理生态特征等分析也显示中温泉古菌与泉古菌具有明显不同的特征。因而专家建议将这些古菌(中温泉古菌)划分为一个新的门,成为古菌域的第三个主要类群—Thaumarchaeota(意译为奇古菌门)。这一新古菌门提出后得到其他研究证据的支持和认可。本文对目前已知的奇古菌门的分类地位演化、基因组学、多样性和生理代谢特征等作一简要综述。     

Response of archaeal communities in the rhizosphere of maize and soybean to elevated atmospheric CO2 concentrations

Background

Archaea are important to the carbon and nitrogen cycles, but it remains uncertain how rising atmospheric carbon dioxide concentrations ([CO₂]) will influence the structure and function of soil archaeal communities.

Methodology/Principal Findings

We measured abundances of archaeal and bacterial 16S rRNA and amoA genes, phylogenies of archaeal 16S rRNA and amoA genes, concentrations of KCl-extractable soil ammonium and nitrite, and potential ammonia oxidation rates in rhizosphere soil samples from maize and soybean exposed to ambient (∼385 ppm) and elevated (550 ppm) [CO₂] in a replicated and field-based study. There was no influence of elevated [CO₂] on copy numbers of archaeal or bacterial 16S rRNA or amoA genes, archaeal community composition, KCl-extractable soil ammonium or nitrite, or potential ammonia oxidation rates for samples from maize, a model C₄ plant. Phylogenetic evidence indicated decreased relative abundance of crenarchaeal sequences in the rhizosphere of soybean, a model leguminous-C₃ plant, at elevated [CO₂], whereas quantitative PCR data indicated no changes in the absolute abundance of archaea. There were no changes in potential ammonia oxidation rates at elevated [CO₂] for soybean. Ammonia oxidation rates were lower in the rhizosphere of maize than soybean, likely because of lower soil pH and/or abundance of archaea. KCl-extractable ammonium and nitrite concentrations were lower at elevated than ambient [CO₂] for soybean.

Conclusion

Plant-driven shifts in soil biogeochemical processes in response to elevated [CO₂] affected archaeal community composition, but not copy numbers of archaeal genes, in the rhizosphere of soybean. The lack of a treatment effect for maize is consistent with the fact that the photosynthesis and productivity of maize are not stimulated by elevated [CO₂] in the absence of drought.