Isolation and molecular characterization of theSinorhizobium meliloti bet locus encoding glycine betaine biosynthesis

To cope with osmotic stress,Sinorhizobium meliloti accumulates organic compatible solutes such as glutamate, trehalose, N-acetylglutaminylglutamine amide, and the most potent osmoprotectant glycine betaine. In order to study the regulation of the glycine betaine biosynthetic pathway, a genetic and molecular analysis was performed. We have selected a Tn5 mutant ofS. meliloti which was deficient in choline dehydrogenase activity. The mutation was complemented using a genomic bank ofS. meliloti. Subcloning and DNA sequencing of a 8-6 kb region from the complemented plasmid showed four open reading frames with an original structural organization of thebet locus compared to that described inE. coli. (i) ThebetB and thebetA genes which encode a glycine betaine aldehyde dehydrogenase, and a choline dehydrogenase, respectively, are separated from thebetI gene (regulatory protein) by an additional gene namedbetC. The BetC protein shares about 30% identity with various sulphatases and is involved in the conversion of choline-O-sulphate into choline. Choline-O-sulphate is used as an osmoprotectant, or as a carbon or sulphur source and this utilization is dependent on a functionalbet locus. (ii) No sequence homologous tobetT (encoding a high-affinity choline transport system inE. coli) was found in the vicinity of thebet locus. (iii) ThebetB and thebetA genes, as well as thebetI and thebetC genes are, respectively, separated by 211 and 167 bp sequences containing inverted repeats. Southern blot analysis indicated that thebet locus is located on the chromosome, and not on the megaplasmids.     

Mechanism of choline O-sulphate utilization in fungi

1. The position of the enzyme blocks in a number of parathiotrophic mutants of Aspergillus nidulans A 69 and mutants A and C of a biotinless mutant of Aspergillus nidulans were examined by nutritional and heterokaryosis experiments and by assay in vitro of enzyme systems and specific enzymes. 2. The mutants were in five groups: A and C blocked at sulphate transport; gamma at ATP sulphurylase; iota at adenosine 5′-sulphatophosphate kinase; eta at the adenosine 3′-phosphate 5′-sulphatophosphate reductase system; alpha, beta and zeta between sulphite and thiosulphate. 3. The ability of the various mutants to synthesize choline O-sulphate in vivo and in vitro and to utilize choline O-sulphate as a source of sulphur indicated that the utilization of endogenously formed choline O-sulphate involved the splitting off of inorganic sulphate, which was then reduced. 4. Choline O-sulphate acted as a source of choline for cholineless strains of Neurospora crassa, suggesting that choline O-sulphate breakdown occurred by simple hydrolysis involving a choline sulphatase. 5. After de-repression of mycelia by growing for a period on a sulphur-free medium the presence of choline sulphatase in physiologically significant amounts was demonstrated in all the A. nidulans strains tested. 6. Choline O-sulphate is transported across the mycelial wall by a mechanism different to that responsible for inorganic sulphate transport.     

Sulphur uptake by ryegrass and its relationship to inorganic and organic sulphur levels and sulphatase activity in soil

Summary Yield of perennial ryegrass and uptake of S at 10, 18 and 25°C were studied in a pot trial using 12 soils with different levels of adsorbed sulphate, total organic S, ester-S, C-bonded S and sulphatase activity.Adsorbed sulphate gave the best correlations with yield and S-uptake at each temperature. At the end of the trial appreciable levels of adsorbed sulphate remained in all the soils. For a given soil, the amount remaining was the same irrespective of the growth temperature employed. This adsorbed sulphate was considered to be unavailable for plant growth.Sulphur uptake was greater in all cases (except at 10°C for one soil) than the decrease in adsorbed sulphate during the trial. This additional sulphur was presumed to have come from organic sources and was significantly correlated (0.1%) with organic S, ester-S, C-bonded S and sulphatase activity at each temperature. These correlations were, however, markedly influenced by one organic S rich soil. When this was omitted the significance of the organic S, ester-S and sulphatase activity correlations fell to 5% and the C-bonded S correlations became non-significant. In this latter instance the absence of significant relationships with C-bonded S was taken to indicate that in this trial the fraction was of less importance in S mineralisation than ester-S.Although sulphatase activity is implicated in the mineralisation process by its significant correlations with the uptake of organic S, other factors are discussed which suggest that the correlations may not be conclusive.     

Transmission of Atherosclerosis Susceptibility with Gut Microbial Transplantation

Recent studies indicate both clinical and mechanistic links between atherosclerotic heart disease and intestinal microbial metabolism of certain dietary nutrients producing trimethylamine N-oxide (TMAO). Here we test the hypothesis that gut microbial transplantation can transmit choline diet-induced TMAO production and atherosclerosis susceptibility. First, a strong association was noted between atherosclerotic plaque and plasma TMAO levels in a mouse diversity panel (n = 22 strains, r = 0.38; p = 0.0001). An atherosclerosis-prone and high TMAO-producing strain, C57BL/6J, and an atherosclerosis-resistant and low TMAO-producing strain, NZW/LacJ, were selected as donors for cecal microbial transplantation into apolipoprotein e null mice in which resident intestinal microbes were first suppressed with antibiotics. Trimethylamine (TMA) and TMAO levels were initially higher in recipients on choline diet that received cecal microbes from C57BL/6J inbred mice; however, durability of choline diet-dependent differences in TMA/TMAO levels was not maintained to the end of the study. Mice receiving C57BL/6J cecal microbes demonstrated choline diet-dependent enhancement in atherosclerotic plaque burden as compared with recipients of NZW/LacJ microbes. Microbial DNA analyses in feces and cecum revealed transplantation of donor microbial community features into recipients with differences in taxa proportions between donor strains that were transmissible to recipients and that tended to show coincident proportions with TMAO levels. Proportions of specific taxa were also identified that correlated with plasma TMAO levels in donors and recipients and with atherosclerotic lesion area in recipients. Atherosclerosis susceptibility may be transmitted via transplantation of gut microbiota. Gut microbes may thus represent a novel therapeutic target for modulating atherosclerosis susceptibility.     

Regulation of choline sulphatase synthesis and activity in Aspergillus nidulans

1. Choline O-sulphate is taken up from the growth medium to the same extent by sulphur-deficient and sulphur-sufficient mycelia of Aspergillus nidulans, but hydrolysis of the transported sulphate ester in vivo only occurs in the sulphur-deficient mycelia. 2. Choline sulphatase activity could not be detected in vitro in sulphur-sufficient mycelia of wild-type and sulphur mutants of A. nidulans, but after sulphur starvation all strains showed appreciable activity of this enzyme. 3. Optimum activity of choline sulphatase in an ultrasonically treated preparation of sulphur-deficient mycelia was at pH7.5. The optimum substrate concentration was in excess of 25mm and K(m) was 0.035m. The enzyme was completely inhibited by 10mm-SO(3) (2-), PO(4) (3-), CN(-) and cysteine. 4. Growth of sulphur-deficient mycelia on various sulphur sources resulted in a decrease of choline sulphatase activity in vitro. The decrease appeared to be due to a repression of choline sulphatase synthesis rather than to inhibition of activity. De-repression by growth on a sulphur-deficient medium was prevented by cycloheximide. Unlike the choline sulphatase of bacteria the fungal enzyme did not need to be substrate-induced. 5. By using sulphur mutants the identity of the co-repressor was limited to S(2)O(3) (2-), cysteine-S-sulphonate, cysteine or compounds derived directly from them. Circumstantial evidence suggests that the co-repressor is cysteine. 6. Inhibition of choline sulphatase activity in vivo was demonstrated with cysteine as the sulphur source for growth.     

Impaired degradation of keratan sulphate by Morquio A fibroblasts.

Upon incubation of keratan [35S]sulphate with normal fibroblasts both [35S]sulphate and N-acetylglucosamine 6-[35S]sulphate are liberated. From the products obtained after digestion with various mutant fibroblasts and with purified N-acetylgalactosamine 6-sulphate sulphatase we suggest that (i) [35S]sulphate is released almost exclusively from galactose 6-sulphate residues; (ii) N-acetylgalactosamine 6-sulphate sulphatase exhibits galactose 6-sulphate sulphatase activity; (iii) both sulphatase activities are deficient in Morquio disease type A.     

Specific Microbial Attachment to Root Knot Nematodes in Suppressive Soil

Understanding the interactions of plant-parasitic nematodes with antagonistic soil microbes could provide opportunities for novel crop protection strategies. Three arable soils were investigated for their suppressiveness against the root knot nematode Meloidogyne hapla. For all three soils, M. hapla developed significantly fewer galls, egg masses, and eggs on tomato plants in unsterilized than in sterilized infested soil. Egg numbers were reduced by up to 93%. This suggested suppression by soil microbial communities. The soils significantly differed in the composition of microbial communities and in the suppressiveness to M. hapla. To identify microorganisms interacting with M. hapla in soil, second-stage juveniles (J2) baited in the test soil were cultivation independently analyzed for attached microbes. PCR-denaturing gradient gel electrophoresis of fungal ITS or 16S rRNA genes of bacteria and bacterial groups from nematode and soil samples was performed, and DNA sequences from J2-associated bands were determined. The fingerprints showed many species that were abundant on J2 but not in the surrounding soil, especially in fungal profiles. Fungi associated with J2 from all three soils were related to the genera Davidiella and Rhizophydium, while the genera Eurotium, Ganoderma, and Cylindrocarpon were specific for the most suppressive soil. Among the 20 highly abundant operational taxonomic units of bacteria specific for J2 in suppressive soil, six were closely related to infectious species such as Shigella spp., whereas the most abundant were Malikia spinosa and Rothia amarae, as determined by 16S rRNA amplicon pyrosequencing. In conclusion, a diverse microflora specifically adhered to J2 of M. hapla in soil and presumably affected female fecundity.     

4种绿化树种盆栽土壤微生物对柴油污染响应及对PAHs的修复

采用室内盆栽实验,利用柴油按不同比例混合土壤0 g/kg(CK),2 g/kg(L1),10 g/kg(L2)和50 g/kg(L3)制备了含不同浓度PAHs的污染土样,选择1年生樟树(Cinnamomum camphora)、广玉兰(Magnolia grandiflora)、栾树(Koelreuteria bipinnata)、马褂木(Liriodendron chinense)幼苗为供试植物,进行了土壤微生物对柴油的响应及对PAHs的修复研究。结果表明:(1)4个树种土壤微生物区系组成以细菌占优势,放线菌次之,真菌最少。(2)在各测定时间树种间土壤微生物总数对污染处理响应差异较大。栾树各污染处理组土壤微生物总数均高于对照组;樟树各污染处理土壤微生物在实验前期低于对照;广玉兰为污染处理组在4月份显著低于对照,而在其他月份多高于对照;马褂木在4月份均低于对照,其他月份为L1处理低于对照,L2、L3处理高于对照(1月L2除外)。(3)4个树种对照土壤中微生物总数随时间的变化都是从10月逐渐增加至翌年4月,然后不断减少至10月;污染处理土壤微生物总数呈现峰值提前或滞后现象,主要出现在1月或7月。真菌是控制PAHs降解的重要因素。(4)经过1a实验,各树种L1、L2处理土壤中的PAHs浓度已与对照土壤相当;L3处理各树种土壤中PAHs含量为马褂木>栾树>广玉兰>樟树。     

Analysis of the Microbial Community Structure by Monitoring an Hg Methylation Gene (hgcA) in Paddy Soils along an Hg Gradient

Knowledge of the diversity of mercury (Hg)-methylating microbes in the environment is limited due to a lack of available molecular biomarkers. Here, we developed novel degenerate PCR primers for a key Hg-methylating gene (hgcA) and amplified successfully the targeted genes from 48 paddy soil samples along an Hg concentration gradient in the Wanshan Hg mining area of China. A significant positive correlation was observed between hgcA gene abundance and methylmercury (MeHg) concentrations, suggesting that microbes containing the genes contribute to Hg methylation in the sampled soils. Canonical correspondence analysis (CCA) showed that the hgcA gene diversity in microbial community structures from paddy soils was high and was influenced by the contents of total Hg, SO₄²⁻, NH₄⁺, and organic matter. Phylogenetic analysis showed that hgcA microbes in the sampled soils likely were related to Deltaproteobacteria, Firmicutes, Chloroflexi, Euryarchaeota, and two unclassified groups. This is a novel report of hgcA diversity in paddy habitats, and results here suggest a link between Hg-methylating microbes and MeHg contamination in situ, which would be useful for monitoring and mediating MeHg synthesis in soils.     

Measurement of the arylsulphatase of Patella vulgata with 4-methylumbelliferone sulphate

1. The preparation, purification, chemical and spectral properties of potassium 4-methylumbelliferone sulphate are described. 2. The use of 4-methylumbelliferone sulphate as a substrate for the arylsulphatase of Patella vulgata is presented with specific reference to the fluorimetric assay procedure used with this substrate. 3. 4-Methylumbelliferone sulphate is compared with the previously used synthetic sulphatase substrates nitrocatechol sulphate and p-nitrophenyl sulphate with respect to K_m, V_max. and sensitivity in the assay of arylsulphatase. 4. 4-Methylumbelliferone sulphate was strongly inhibited by phosphate. Sulphate, a less potent inhibitor, appeared to be of the competitive type with some anomalous characteristics.     

The regulation of aryl sulphatase in Aspergillus nidulans

The aryl sulphatase of Aspergillus nidulans is derepressed in a medium that contains low amounts of inorganic sulphate or sulphur-containing amino acids. Isotopic labelling experiments show that the enzyme molecules are made de novo. However, once derepressed, the formation of the enzyme becomes progressively insensitive to cycloheximide. It is suggested that active sulphatase is made in two steps, one sensitive to cycloheximide and the other insensitive. Both of these steps appear to be regulated by sulphur metabolites.     

水热增加下黑土细菌群落共生网络特征

黑土是有机质含量高且肥沃的土壤类型之一,气候变化会显著改变黑土中微生物群落的结构,同时影响群落间的潜在相互作用关系。[目的] 揭示水热增加对黑土中的细菌群落结构及潜在互作关系的影响。[方法] 基于土壤移置试验,采用16S rRNA高通量测序解析农田黑土（原位黑土、水热增加1和水热增加2）中的细菌群落结构对水热增加的响应;使用CoNet构建微生物群落共生网络,识别共生网络中的枢纽微生物;利用结构方程模型、相关性分析探究水热条件变化下土壤性质、微生物交互作用、多样性之间的直接、间接关系。[结果] 黑土中的微生物以疣微菌、变形杆菌、酸性杆菌和放线菌为主。水热增加下土壤微生物共生网络的拓扑性质发生显著变化,网络中表征微生物潜在竞争关系的负连线随着水热增加而显著增加。气候因素通过改变微生物潜在相互作用影响了群落水平分类多样性。物种竞争增强可能直接导致了土壤有机碳含量的降低。[结论] 水热增加会显著改变黑土中微生物之间的潜在交互作用,枢纽微生物的响应更加敏感。     

宁夏燃煤电厂周边土壤、植物和微生物生态化学计量特征及其影响因素

大气酸沉降增加对陆地生态系统的影响已得到了广泛证实,但有关酸沉降累积下工业排放源周边植被-土壤系统元素平衡特征及其影响机制的研究较少。燃煤电厂是主要的工业酸排放源之一。因此,以宁东能源化工基地3个燃煤电厂为观测点,研究了电厂周边土壤-植物叶片-微生物生态化学计量特征,分析了叶片和微生物生物量生态化学计量特征与降水降尘S、N沉降量及土壤性质的关系。结果表明：土壤和微生物生物量C ： N ： P生态化学计量特征变异系数较大,叶片各指标的变异系数较小。与受人类活动影响较少的其他同类型区相比,研究区具有较高的土壤有机C水平和N、P供给,且P相对于N丰富。植物可能主要受N限制,而微生物主要受P限制;土壤及微生物元素间均存在极显著的线性关系（P<0.001）。叶片全C与全N、全P均无显著的关系（P>0.05）。叶片全N、全P和N ： P具有高的内稳性。微生物生物量N ： P内稳性较强,但生物量N和P内稳性较弱,对土壤环境的变化反应敏感;SO₄^2-沉降有助于促进叶片对P的摄取和微生物对C、N、P的固持。少量NO₃^-沉降有利于叶片N摄取,但持续增加的NO₃^-沉降可能会使土壤P受限性增强,进而抑制叶片P摄取和微生物生物量积累。土壤酶活性、Ca²⁺和含水量亦显著影响着植物和微生物元素生态化学计量关系（P<0.05）。因此,今后还需结合多个电厂的土壤性质和植被状况,从较长时间尺度上深入揭示酸沉降增加对工业排放源周边植被-土壤系统元素平衡特征的影响机制。     

Comparative genomics reveals the acquisition of mobile genetic elements by the plant growth-promoting Pantoea eucrina OB49 in polluted environments

Heavy metal-tolerant plant growth-promoting bacteria (PGPB) have gained popularity in bioremediation in recent years. A genome-assisted study of a heavy metal-tolerant PGPB Pantoea eucrina OB49 isolated from the rhizosphere of wheat grown on a heavy metal-contaminated site is presented. Comparative pan-genome analysis indicated that OB49 acquired heavy metal resistance genes through horizontal gene transfer. On contigs S10 and S12, OB49 has two arsRBCH operons that give arsenic resistance. On the S12 contig, an arsRBCH operon was discovered in conjunction with the merRTPCADE operon, which provides mercury resistance. P. eucrina OB49 may be involved in an ecological alternative for heavy metal remediation and growth promotion of wheat grown in metal-polluted soils. Our results suggested the detection of mobile genetic elements that harbour the ars operon and the fluoride resistance genes adjacent to the mer operon.     

Plant and Bird Presence Strongly Influences the Microbial Communities in Soils of Admiralty Bay,Maritime Antarctica

Understanding the environmental factors that shape microbial communities is crucial, especially in extreme environments, like Antarctica. Two main forces were reported to influence Antarctic soil microbes: birds and plants. Both birds and plants are currently undergoing relatively large changes in their distribution and abundance due to global warming. However, we need to clearly understand the relationship between plants, birds and soil microorganisms. We therefore collected rhizosphere and bulk soils from six different sampling sites subjected to different levels of bird influence and colonized by Colobanthus quitensis and Deschampsia antarctica in Admiralty Bay, King George Island, Maritime Antarctic. Microarray and qPCR assays targeting 16S rRNA genes of specific taxa were used to assess microbial community structure, composition and abundance and analyzed with a range of soil physico-chemical parameters. The results indicated significant rhizosphere effects in four out of the six sites, including areas with different levels of bird influence. Acidobacteria were significantly more abundant in soils with little bird influence (low nitrogen) and in bulk soil. In contrast, Actinobacteria were significantly more abundant in the rhizosphere of both plant species. At two of the sampling sites under strong bird influence (penguin colonies), Firmicutes were significantly more abundant in D. antarctica rhizosphere but not in C. quitensis rhizosphere. The Firmicutes were also positively and significantly correlated to the nitrogen concentrations in the soil. We conclude that the microbial communities in Antarctic soils are driven both by bird and plants, and that the effect is taxa-specific.     

Differential Nutrient Limitation of Soil Microbial Biomass and Metabolic Quotients (qCO2): Is There a Biological Stoichiometry of Soil Microbes?

Background

Variation in microbial metabolism poses one of the greatest current uncertainties in models of global carbon cycling, and is particularly poorly understood in soils. Biological Stoichiometry theory describes biochemical mechanisms linking metabolic rates with variation in the elemental composition of cells and organisms, and has been widely observed in animals, plants, and plankton. However, this theory has not been widely tested in microbes, which are considered to have fixed ratios of major elements in soils.

Methodology/Principal Findings

To determine whether Biological Stoichiometry underlies patterns of soil microbial metabolism, we compiled published data on microbial biomass carbon (C), nitrogen (N), and phosphorus (P) pools in soils spanning the global range of climate, vegetation, and land use types. We compared element ratios in microbial biomass pools to the metabolic quotient qCO₂ (respiration per unit biomass), where soil C mineralization was simultaneously measured in controlled incubations. Although microbial C, N, and P stoichiometry appeared to follow somewhat constrained allometric relationships at the global scale, we found significant variation in the C∶N∶P ratios of soil microbes across land use and habitat types, and size-dependent scaling of microbial C∶N and C∶P (but not N∶P) ratios. Microbial stoichiometry and metabolic quotients were also weakly correlated as suggested by Biological Stoichiometry theory. Importantly, we found that while soil microbial biomass appeared constrained by soil N availability, microbial metabolic rates (qCO₂) were most strongly associated with inorganic P availability.

Conclusions/Significance

Our findings appear consistent with the model of cellular metabolism described by Biological Stoichiometry theory, where biomass is limited by N needed to build proteins, but rates of protein synthesis are limited by the high P demands of ribosomes. Incorporation of these physiological processes may improve models of carbon cycling and understanding of the effects of nutrient availability on soil C turnover across terrestrial and wetland habitats.     

Different pathways of choline metabolism in two choline-independent strains of Streptococcus pneumoniae and their impact on virulence

The two recently characterized Streptococcus pneumoniae strains—R6Chi and R6Cho⁻—that have lost the unique auxotrophic requirement of this bacterial species for choline differ in their mechanisms of choline independence. In strain R6Chi the mechanism is caused by a point mutation in tacF, a gene that is part of the pneumococcal lic2 operon, which is essential for growth and survival of the bacteria. Cultures of lic2 mutants of the encapsulated strain D39Chi growing in choline-containing medium formed long chains, did not autolyze, had no choline in their cell wall, and were completely avirulent in the mouse intraperitoneal model. In contrast, while the Cho⁻ strain carried a complete pneumococcal lic2 operon and had no mutations in the tacF gene, deletion of the entire lic2 operon had no effect on the growth or phenotype of strain Cho⁻. These observations suggest that the biochemical functions normally dependent on determinants of the pneumococcal lic2 operon may also be carried out in strain Cho⁻ by a second set of genetic elements imported from Streptococcus oralis, the choline-independent streptococcal strain that served as the DNA donor in the heterologous transformation event that produced strain R6Cho⁻. The identification in R6Cho⁻ of a large (20-kb) S. oralis DNA insert carrying both tacF and licD genes confirms this prediction and suggests that these heterologous elements may represent a “backup” system capable of catalyzing P-choline incorporation and export of teichoic acid chains under conditions in which the native lic2 operon is not functional.     

Microbial Community Structure of Relict Niter-Beds Previously Used for Saltpeter Production

From the 16th to the 18th centuries in Japan, saltpeter was produced using a biological niter-bed process and was formed under the floor of gassho-style houses in the historic villages of Shirakawa-go and Gokayama, which are classified as United Nations Educational, Scientific and Cultural Organization (UNESCO) World Heritage Sites. The relict niter-beds are now conserved in the underfloor space of gassho-style houses, where they are isolated from destabilizing environmental factors and retain the ability to produce nitrate. However, little is known about the nitrifying microbes in such relict niter-bed ecosystems. In this study, the microbial community structures within nine relict niter-bed soils were investigated using 454 pyrotag analysis targeting the 16S rRNA gene and the bacterial and archaeal ammonia monooxygenase gene (amoA). The 16S rRNA gene pyrotag analysis showed that members of the phyla Proteobacteria, Actinobacteria, Bacteroidetes, Chloroflexi, Firmicutes, Gemmatimonadetes, and Planctomycetes were major microbial constituents, and principal coordinate analysis showed that the NO₃ ⁻, Cl⁻, K⁺, and Na⁺ contents were potential determinants of the structures of entire microbial communities in relict niter-bed soils. The bacterial and archaeal amoA libraries indicated that members of the Nitrosospira-type ammonia-oxidizing bacteria (AOB) and “Ca. Nitrososphaera”-type ammonia-oxidizing archaea (AOA), respectively, predominated in relict niter-bed soils. In addition, soil pH and organic carbon content were important factors for the ecological niche of AOB and AOA in relict niter-bed soil ecosystems.     

Pyrosequencing Characterization of the Microbiota from Atlantic Intertidal Marine Sponges Reveals High Microbial Diversity and the Lack of Co-Occurrence Patterns

Sponges are ancient metazoans that host diverse and complex microbial communities. Sponge-associated microbial diversity has been studied from wide oceans across the globe, particularly in subtidal regions, but the microbial communities from intertidal sponges have remained mostly unexplored. Here we used pyrosequencing to characterize the microbial communities in 12 different co-occurring intertidal marine sponge species sampled from the Atlantic coast, revealing a total of 686 operational taxonomic units (OTUs) at 97% sequence similarity. Taxonomic assignment of 16S ribosomal RNA tag sequences estimated altogether 26 microbial groups, represented by bacterial (75.5%) and archaeal (22%) domains. Proteobacteria (43.4%) and Crenarchaeota (20.6%) were the most dominant microbial groups detected in all the 12 marine sponge species and ambient seawater. The Crenarchaeota microbes detected in three Atlantic Ocean sponges had a close similarity with Crenarchaeota from geographically separated subtidal Red Sea sponges. Our study showed that most of the microbial communities observed in sponges (73%) were also found in the surrounding ambient seawater suggesting possible environmental acquisition and/or horizontal transfer of microbes. Beyond the microbial diversity and community structure assessments (NMDS, ADONIS, ANOSIM), we explored the interactions between the microbial communities coexisting in sponges using the checkerboard score (C-score). Analyses of the microbial association pattern (co-occurrence) among intertidal sympatric sponges revealed the random association of microbes, favoring the hypothesis that the sponge-inhabiting microbes are recruited from the habitat mostly by chance or influenced by environmental factors to benefit the hosts.