新疆沙湾冷泉沉积物中免培养古菌多样性初步研究

【目的】了解新疆沙湾冷泉沉积物的古菌组成及多样性。【方法】采用免培养法,液氮研磨提取冷泉沉积物总DNA,使用古菌通用引物进行16S rRNA基因扩增,构建16S rRNA基因文库。对阳性克隆进行HhaI限制性酶切分型,选出具有不同酶切图谱的序列进行测序,将所得序列与GenBank数据库中序列比对并构建16S rRNA基因系统发育树。【结果】从冷泉沉积物古菌16S rRNA基因文库中随机挑选了121个阳性克隆,共得到22个不同的可操作分类单元,BLAST结果表明全部克隆子归属于泉古菌门(Crenarchaeote)中免培养类群。系统发育分析归类为Soil-Freshwater-subsurface group和MarinegroupI,2个亚群并且各占整个文库的50%。其中40%左右的克隆子与具有无机碳和硝酸盐同化能力的泉古菌有高的相似性。此外还发现40%的克隆子与低温泉古菌类群具有很高的相似性。【结论】新疆沙湾冷泉沉积物中古菌类群多样性较低,但存有大量高度适应此低温、贫营养环境的泉古菌类群。     

洋山深水港海域表层海水中古菌多样性特点

利用DGGE、定量PCR以及16S rRNA基因克隆文库技术对洋山深水港海域表层海水中的古菌多样性组成进行了调查和分析。通过Quantity One软件分析不同样品的DGGE图谱,发现洋山深水港3个不同海域(小洋山港口区、大洋山港口区、中间航道)的古菌群落多样性组成不存在明显的区别;利用定量PCR的方法对3个不同样品中的古菌16S rRNA基因拷贝进行计数,发现3个不同海域的古菌16S rRNA基因拷贝数的数量关系为:大洋山海域((1.69±0.19)×10~6copies/mL)中间航道((2.17±0.20)×10~6copies/mL)小洋山港口区((2.42±0.22)×10~6copies/mL),这说明洋山深水港3个不同海域的古菌群落组成是一致的,只是在数量上略有差异,为对该海域古菌的更深入调查研究提供了便利和数据基础。洋山深水港海域表层海水的古菌16S rRNA基因文库分析表明,古菌由三大门类组成:广古菌门(Euryarchaeota)、泉古菌门(Crenarchaeota)和奇古菌门(Thaumarchaeota)。广古菌门所占比例约为26.8%,泉古菌门约为33.0%,奇古菌门约为40.2%。广古菌门含有2个类群,分别是Mathanobacteriales(10.3%)和Marine GroupⅡ(16.5%);泉古菌门含有1个类群,为Unidentified Crenarchaeotic Group(33.0%);奇古菌门含有1个类群,为Marine GroupⅠ(40.2%)。结果显示,Mathanobacteriales类群和Marine GroupⅡ类群的比例失调,这可能预示着洋山深水港海域存在油污污染及外来微生物物种入侵的风险。     

新疆乌鲁木齐10号冷泉古菌群落结构多样性

[目的]探究新疆地震断裂带含硫冷泉泉水古菌群落组成及多样性.[方法]利用酶解法直接从冷泉泉水样品中提取环境总DNA,采用古菌通用引物对16S rRNA基因进行扩增,构建16S rRNA基因克隆文库,通过Alu Ⅰ和AfaⅠ两种限制性内切酶对随机挑选的115个阳性克隆子进行酶切分型,将不同酶切带型对应的克隆子送样测序,测序结果与GenBank序列进行比对并构建16S rRNA基因系统发育树.[结果]古菌克隆文库中共得到44个不同的酶切带型,BLAST序列比对和系统发育分析将它们划分于广古菌门(Euryarchaeota,94.78％)和奇古菌门(Thaumarchaeota,4.35％).奇古菌门克隆与Nitrosopumilus.sp序列相似性达到了93％;而广古菌门类群较为多样,其中,42.61％的克隆子属于RC-V cluster,20.87％与13.91％的克隆子分别属于LDS cluster和Methanomicrobiales,4.35％的克隆子与甲烷厌氧氧化相关的类群(ANME-1a-FW)具有较高的的相似.另外,13.05％的克隆子属于广古菌门中的未知类群.[结论]乌鲁木齐10号泉水体中广古菌类群多样,可能蕴藏有大量潜在的古菌新类群.     

新疆顿巴斯他乌盐湖沉积物免培养古菌多样性

【目的】了解新疆顿巴斯他乌盐湖沉积物免培养古菌组成及多样性。【方法】利用免培养法直接从顿巴斯他乌盐湖沉积物样品中提取环境总DNA,采用古菌通用引物对16S rRNA基因进行扩增,构建基因克隆文库。对随机挑选的59个阳性克隆进行HaeⅢ限制性酶切分型并测序、BLAST比对及构建16S rRNA基因系统发育树。【结果】文库覆盖率为89%,Shannon-Wiener指数为2.69,共得到21个不同的可操作分类单元,分属于广古菌门(Euryarchaeota,92%)和泉古菌门(Crenarchaeota,8%),其中多数为盐杆菌科(Halobacteriaceae,88%)的盐杆菌属(Halobacterium,24%)、盐盒菌属(Haloarcula,18%)、盐碱红菌属(Natronorubrum,14%)、盐红菌属(Halorubrum,8%)等,与海盐环境(thalassohaline)获得的16S rRNA基因序列相似性最高(﹥95%);整个文库中约11%的克隆与可培养古菌多个属的相似性小于97%。【结论】顿巴斯他乌盐湖古菌多样性略低于同类高盐环境,组成较为一致,只是各类群所占百分比稍有不同,且可能存在一些潜在新物种或新类群。     

中国和美国原始土壤中非高温泉古菌的发现和鉴定

近年来在非极端环境中已经发现有古菌(Archaea)的存在, 但在中国原始土壤中还未见报道。本研究的目的是调查古菌是否存在于两个分别取自中国新疆和广西的土壤及两个美国亚利桑那州南部地区的土壤中。我们分别构建了这四个原始土壤的古菌16S rDNA文库并对28个克隆的16S rDNA进行了鉴定。所有这些16S rDNA的序列都归类于古菌的泉古菌门(Crenarchaeota)。进化树分析表明, 这些泉古菌的16S rDNA属于非高温陆地环境中的泉古菌种群, 明显区别于海洋和淡水地带的泉古菌种群。这个泉古菌种群又有两个分支, 这两个分支在16S rDNA序列上和G C含量上有明显的区别。本研究在两个中国和两个美国原始土壤中鉴定了非高温泉古菌的存在, 由此证明泉古菌的存在范围不只局限于高温等极端环境。另外, 美国原始土壤中的泉古菌只属于一个进化分支, 这说明非高温泉古菌种群的类型和土壤的地理位置及土壤特性有关。     

西藏米拉山土壤古茵16S rRNA及amoA基因多样性分析

[目的]本研究旨在了解西藏米拉山高寒草甸土壤中古菌及氨氧化古菌群落结构组成情况.[方法]采用未培养技术直接从土壤中提取微生物总DNA,分别利用通用引物构建古菌16S rRNA基因和氨氧化古菌amoA基因克隆文库.利用DOTUR软件将古菌和氨氧化古菌序列按照相似性97%的标准分成若干个可操作分类单元(OTUs).[结果]通过构建系统发育树,表明古菌16s rRNA基因克隆文库包括泉古菌门和未分类的古菌两大类,并且所有泉古菌均属于热变形菌纲.氨氧化古菌amoA基因克隆文库中序列均为泉古菌.古菌16s rRNA基因和古菌amoA基因克隆文库分别包括64个OTUs和75个OTUs.[结论]西藏米拉山高寒草甸土壤中古菌多样性比较丰富,表明古菌在高寒草甸土壤的氮循环中可能具有重要的作用.     

新疆两典型微咸水湖水体免培养古菌多样性

微咸水湖是湖泊演化过程中的一个重要中间状态,以新疆两典型微咸水湖-赛里木湖和柴窝堡湖水为研究对象,采用微孔滤膜收集菌体,SDS-酚-氯仿抽提法直接提取湖水总DNA,利用古菌16S rRNA基因通用引物进行PCR扩增,分别构建两湖古菌16S rRNA基因克隆文库。用限制性内切酶Hae Ⅲ对随机挑选的阳性克隆子进行酶切分型,分别得到7个和8个可操作分类单元(Operational Taxonomic Units, OTUs),两文库覆盖率均大于98%。BLAST比对和系统发育分析表明赛里木湖全部克隆子归属于泉古菌门(Crenarchaeota),97%的克隆子与不同环境免培养氨氧化泉古菌有较高的序列相似性(>97%)。柴窝堡湖水古菌归为3个门:Thaumarchaeota (81.2%)、广古菌门(Euryarchaeota)(13%)和泉古菌门(Crenarchaeota) (5.8%),81.2%的克隆子与具有氮代谢功能的氨氧化古菌纯培养物具有较高的序列相似性(97%-98%),13%的克隆子与已分离到的产甲烷古菌序列同源性大于97%。研究发现新疆微咸水湖可能存有大量新划分的古菌Thaumarchaeota门类群、可培养氨氧化及产甲烷古菌类群,两典型微咸水湖泊中古菌类群多样性较低且群落组成差异大。     

腾冲两热泉泉古菌多样性及系统发育的初步分析

通过构建16S rRNA基因片段的克隆文库对腾冲热海两温泉中泉古菌的多样性和系统发育关系进行了初步的研究.一共得到18个泉古茵克隆序列,可分为12个OTUs,两温泉的克隆序列与已知GenBank上关系最近序列的平均相似性较低,无名泉为92.56%,热爆区为93%.从基于16S rRNA基因片段序列构建的系统发育树来看,74℃的无名泉样点中既有属于超高温环境类群的泉古菌,同时又有属于和常温环境较接近的泉古菌;45℃的热爆区样点的泉古茵,相对来说则更接近于常温类群.本次研究表明,腾冲热泉与世界其它同类热泉之间的泉古茵类群存在着一定的差异;而且两实验样点代表了超高温和高温环境泉古菌逐渐向常温过度的两个重要环境.     

西藏米拉山土壤古菌16S rRNA及amoA基因多样性?分析

摘要：【目的】硝化作用在全球土壤氮循环中具有重要的作用,虽然细菌一度被认为单独负责催化这个过程的限速步骤,但是最近一些研究结果表明泉古菌具有氨氧化的能力。本文通过构建古菌16S rRNA 基因克隆文库和氨氧化古菌amoA基因文库,分析西藏米拉山高寒草甸土壤中古菌及氨氧化古菌群落结构组成情况,为揭示青藏高原高寒草甸土壤古菌的多样性提供理论基础。【方法】采用未培养技术直接从土壤中提取微生物总DNA,分别利用通用引物构建古菌16S rRNA 基因和氨氧化古菌amoA基因克隆文库。【结果】通过构建系统发育树,表明古菌16S rRNA 基因克隆文库包括泉古菌门和未分类的古菌两大类,并且所有泉古菌均属于热变形菌纲。氨氧化古菌amoA基因克隆文库中序列均为泉古菌。通过DOTUR软件分析,古菌16S rRNA基因和古菌amoA基因克隆文库分别包括64个OTUs和 75个OTUs。【结论】西藏米拉山高寒草甸土壤中古菌多样性比较丰富,表明古菌在高寒草甸土壤的氮循环中可能具有重要的作用。所获得的一些序列与已知环境中土壤、淡水及海洋沉积物中获得的一些序列具有很高的相似性,其古菌及氨氧化古菌来自不同环境的可能性比较大,可能与青藏高原的地质历史变迁过程有关。米拉山古菌及氨氧化古菌与陆地设施土壤中相似性最高,说明与西藏米拉山高寒草甸土壤的退化有关。     

几种农田土壤中古菌、泉古菌和细菌的数量分布特征

真核生物、细菌和古菌三者共同构成了生命的三域系统.古菌作为第3种生命形式,不仅能在高温、强酸和高盐等极端环境下生存,而且在海洋、湖泊和土壤等生境中也广泛分布,预示其在整个生态系统中有着不可估量的作用.本文以2个农田剖面土壤和2个长期施肥试验站祁阳(QY)和封丘(FQ)的土壤为对象,以实时定量PCR方法为主要研究手段,对土壤中古菌(包括泉古菌)和细菌的16S rRNA基因拷贝数丰度变化进行了研究.结果表明:土壤泉古菌16S rRNA基因拷贝数要低于古菌l～2个数量级,两者与细菌相比,16S rRNA基因拷贝数大小顺序为土壤泉古菌＜古茵＜细菌,而古菌和泉古菌16S rRNA基因拷贝数与细菌的比值均随土壤深度加深而增大.不同施肥处理对土壤古菌和泉古茵的数量有显著影响.QY试验站土壤古菌和细菌的数量与土壤pH值显著相关(分别为r=0.850,P＜0.01和r=0.676,P＜0.05).FQ古菌、泉古菌和细菌与土壤pH值相关性不显著,与土壤有机质含量相关性均达显著水平(分别为r=0.783,P＜0.05;r=0.827,P＜0.05;r=0.767,P＜0.05).了解古菌包括泉古菌在农田土壤中的分布,可为评价其在生态系统和物质循环中的作用提供重要的理论依据.     

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.     

Mesophilic Crenarchaeota: proposal for a third archaeal phylum, the Thaumarchaeota

The archaeal domain is currently divided into two major phyla, the Euryarchaeota and Crenarchaeota. During the past few years, diverse groups of uncultivated mesophilic archaea have been discovered and affiliated with the Crenarchaeota. It was recently recognized that these archaea have a major role in geochemical cycles. Based on the first genome sequence of a crenarchaeote, Cenarchaeum symbiosum, we show that these mesophilic archaea are different from hyperthermophilic Crenarchaeota and branch deeper than was previously assumed. Our results indicate that C. symbiosum and its relatives are not Crenarchaeota, but should be considered as a third archaeal phylum, which we propose to name Thaumarchaeota (from the Greek 'thaumas', meaning wonder).     

A thaumarchaeal provirus testifies for an ancient association of tailed viruses with archaea

Archaeal viruses, or archaeoviruses, display a wide range of virion morphotypes. Whereas the majority of those morphotypes are unique to archaeal viruses, some are more widely distributed across different cellular domains. Tailed double-stranded DNA archaeoviruses are remarkably similar to viruses of the same morphology (order Caudovirales) that infect many bacterial hosts. They have, so far, only been found in one phylum of the archaea, the Euryarchaeota, which has led to controversial hypotheses about their origin. In the present paper, we describe the identification and analysis of a putative provirus present in the genome of a mesophilic thaumarchaeon. We show that the provirus is related to tailed bacterial and euryarchaeal viruses and encodes a full complement of proteins that are required to build a tailed virion. The recently discovered wide distribution of tailed viruses in Euryarchaeota and the identification of a related provirus in Thaumarchaeota, an archaeal phylum which might have branched off before the separation of Crenarchaeota and Euryarchaeota, suggest that an association of these viruses with Archaea might be more ancient than previously anticipated.     

First description of giant Archaea (Thaumarchaeota) associated with putative bacterial ectosymbionts in a sulfidic marine habitat

Archaea may be involved in global energy cycles, and are known for their ability to interact with eukaryotic species (sponges, corals and ascidians) or as archaeal-bacterial consortia. The recently proposed phylum Thaumarchaeota may represent the deepest branching lineage in the archaeal phylogeny emerging before the divergence between Euryarchaeota and Crenarchaeota. Here we report the first characterization of two marine thaumarchaeal species from shallow waters that consist of multiple giant cells. One species is coated with sulfur-oxidizing γ-Proteobacteria. These new uncultured thaumarchaeal species are able to live in the sulfide-rich environments of a tropical mangrove swamp, either on living tissues such as roots or on various kinds of materials such as stones, sunken woods, etc. These archaea and archaea/bacteria associations have been studied using light microscopy, transmission electron microscopy and scanning electron microscopy. Species identification of archaeons and the putative bacterial symbiont have been assessed by 16S small subunit ribosomal RNA analysis. The sulfur-oxidizing ability of the bacteria has been assessed by genetic investigation on alpha-subunit of the adenosine-5'-phosphosulfate reductase/oxidase's (AprA). Species identifications have been confirmed by fluorescence in situ hybridization using specific probes designed in this study. In this article, we describe two new giant archaeal species that form the biggest archaeal filaments ever observed. One of these species is covered by a specific biofilm of sulfur-oxidizing γ-Proteobacteria. This study highlights an unexpected morphological and genetic diversity of the phylum Thaumarchaeota.     

Nanoarchaea: representatives of a novel archaeal phylum or a fast-evolving euryarchaeal lineage related to Thermococcales?

Background  

Cultivable archaeal species are assigned to two phyla - the Crenarchaeota and the Euryarchaeota - by a number of important genetic differences, and this ancient split is strongly supported by phylogenetic analysis. The recently described hyperthermophile Nanoarchaeum equitans, harboring the smallest cellular genome ever sequenced (480 kb), has been suggested as the representative of a new phylum - the Nanoarchaeota - that would have diverged before the Crenarchaeota/Euryarchaeota split. Confirming the phylogenetic position of N. equitans is thus crucial for deciphering the history of the archaeal domain.     

Insights into the evolution of Archaea and eukaryotic protein modifier systems revealed by the genome of a novel archaeal group

The domain Archaea has historically been divided into two phyla, the Crenarchaeota and Euryarchaeota. Although regarded as members of the Crenarchaeota based on small subunit rRNA phylogeny, environmental genomics and efforts for cultivation have recently revealed two novel phyla/divisions in the Archaea; the 'Thaumarchaeota' and 'Korarchaeota'. Here, we show the genome sequence of Candidatus 'Caldiarchaeum subterraneum' that represents an uncultivated crenarchaeotic group. A composite genome was reconstructed from a metagenomic library previously prepared from a microbial mat at a geothermal water stream of a sub-surface gold mine. The genome was found to be clearly distinct from those of the known phyla/divisions, Crenarchaeota (hyperthermophiles), Euryarchaeota, Thaumarchaeota and Korarchaeota. The unique traits suggest that this crenarchaeotic group can be considered as a novel archaeal phylum/division. Moreover, C. subterraneum harbors an ubiquitin-like protein modifier system consisting of Ub, E1, E2 and small Zn RING finger family protein with structural motifs specific to eukaryotic system proteins, a system clearly distinct from the prokaryote-type system recently identified in Haloferax and Mycobacterium. The presence of such a eukaryote-type system is unprecedented in prokaryotes, and indicates that a prototype of the eukaryotic protein modifier system is present in the Archaea.     

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.     

Split decision: a thaumarchaeon encoding both FtsZ and Cdv cell division proteins chooses Cdv for cytokinesis

Cytoskeletal proteins play a pivotal role in cytokinesis in prokaryotes and eukaryotes. Most bacteria and a major branch of the archaea called the Euryarchaeota harbour a tubulin homologue, FtsZ, which assembles into a dynamic polymeric ring structure required for cytokinesis. However, Crenarchaeota, another branch of the archaea, lack FtsZ and instead use Cdv proteins, which are homologues of the ESCRT-III-like system involved in vesicular sorting and cytokinesis in eukaryotes, for cell division. Recently, a group of Crenarchaeota that grow in non-extreme environments was found to be sufficiently divergent to warrant its own branch of the archaea called the Thaumarchaeota. Notably, Thaumarchaeota have both Cdv and FtsZ homologues, which begs the question of which system is used for cell division. In this issue of Molecular Microbiology,Pelve et al. (2011) Pelve and colleagues tackle this question. They found that cells of the thaumarchaeon Nitrosopumilus maritimus likely divide using the Cdv system and not FtsZ, based on localization of Cdv proteins but not FtsZ to division sites. The authors also provide evidence that the cell cycle during growth of N. maritimus differs significantly from those of other archaea.     

The deep archaeal roots of eukaryotes

The set of conserved eukaryotic protein-coding genes includes distinct subsets one of which appears to be most closely related to and, by inference, derived from archaea, whereas another one appears to be of bacterial, possibly, endosymbiotic origin. The "archaeal" genes of eukaryotes, primarily, encode components of information-processing systems, whereas the "bacterial" genes are predominantly operational. The precise nature of the archaeo-eukaryotic relationship remains uncertain, and it has been variously argued that eukaryotic informational genes evolved from the homologous genes of Euryarchaeota or Crenarchaeota (the major branches of extant archaea) or that the origin of eukaryotes lies outside the known diversity of archaea. We describe a comprehensive set of 355 eukaryotic genes of apparent archaeal origin identified through ortholog detection and phylogenetic analysis. Phylogenetic hypothesis testing using constrained trees, combined with a systematic search for shared derived characters in the form of homologous inserts in conserved proteins, indicate that, for the majority of these genes, the preferred tree topology is one with the eukaryotic branch placed outside the extant diversity of archaea although small subsets of genes show crenarchaeal and euryarchaeal affinities. Thus, the archaeal genes in eukaryotes appear to descend from a distinct, ancient, and otherwise uncharacterized archaeal lineage that acquired some euryarchaeal and crenarchaeal genes via early horizontal gene transfer.     

荒漠孑遗植物四合木对土壤古菌群落的影响

土壤是植物定居的场所,也是植物-微生物互作的重要界面。古菌是土壤微生物重要组份,在碳、氮、硫、铁等元素的生物地球化学循环和植物的生长发育、适应生境中发挥重要作用。植物定居对土壤古菌群落的影响研究鲜有开展,孑遗植物在研究植物-微生物-环境互作中具有独特的优势。采用扩增子高通量测序技术,研究以荒漠孑遗植物四合木为建群种或优势种的四合木-红砂-珍珠-针茅群落、四合木-针茅群落和四合木群落等三种荒漠植物群落类型中,四合木根区土壤和光板地土体土壤古菌群落特征,揭示四合木定居对土壤古菌物种数量、多样性、群落组成及功能的影响。结果表明,荒漠孑遗植物四合木定居不仅增加了根区土壤古菌的物种数量,提高了根区土壤古菌群落多样性,而且改变了土壤古菌群落组成,减少了奇古菌门Nitrososphaeraceae科未分类的属氨氧化古菌（unclassified_f_Nitrososphaeraceae）和暂定Nitrososphaera属氨氧化古菌（Candidatus Nitrososphaera）相对丰度,增加了Nitrososphaeraceae科暂定Nitrocosmicus属氨氧化古菌（Candidatus Nitrocosmicus）和广古菌门海洋古菌类群Ⅱ中未分类的属（norank_o_Marine_Group_II）相对丰度,广古菌门热原体纲未分类的属（unclassified_c__Thermoplasmata）相对丰度变化显著。植物群落演替对四合木根区土壤和光板地土体土壤古菌群落均无显著影响。Nitrososphaeraceae科氨氧化古菌是三种不同荒漠植物群落类型中土壤古菌的核心微生物组。四合木定居也显著改变土壤古菌群落的功能,减弱了高丰度功能,增强了低丰度功能,对有氧呼吸、核苷酸合成、氨基酸合成等途径影响显著。荒漠孑遗植物四合木定居改变了土壤古菌群落物种数量、多样性、组成、功能等特征。