Hindawi International Journal of Microbiology Volume 2018, Article ID 6280484, 13 pages https://doi.org/10.1155/2018/6280484 Research Article Bacterial Community of the Rice Floodwater Using Cultivation-Independent Approaches MichelePittol ,1ErinScully,2DanielMiller,3LisaDurso,3 LidiaMarianaFiuza,1andVictorHugoValiati1 1ProgramadePo´s-Gradua¸ca˜oemBiologia,UniversidadedoValedoRiodosSinos(UNISINOS),950UnisinosAvenue, Sa˜oLeopoldo,RS,Brazil 2UnitedStatesDepartmentofAgriculture(USDA),AgriculturalResearchService(ARS),CenterforGrainandAnimalHealthResearch, StoredProductInsectandEngineeringResearchUnit(SPIERU),1515CollegeAve.,Manhattan,KS,USA 3UnitedStatesDepartmentofAgriculture(USDA),AgriculturalResearchService(ARS), AgroecosystemManagementResearchUnit(AMRU),251FilleyHall,UNLEastCampus,Lincoln,NE,USA CorrespondenceshouldbeaddressedtoMichelePittol;[email protected] Received 2 August 2017; Revised 9 December 2017; Accepted 26 December 2017; Published 30 January 2018 AcademicEditor:ClemenciaChaves-Lo´pez Copyright©2018MichelePittoletal.ThisisanopenaccessarticledistributedundertheCreativeCommonsAttributionLicense, whichpermitsunrestricteduse,distribution,andreproductioninanymedium,providedtheoriginalworkisproperlycited. Inagriculturalsystems,interactionsbetweenplantsandmicroorganismsareimportanttomaintainingproductionandprofitability. Inthisstudy,bacterialcommunitiesinfloodwatersofricefieldsweremonitoredduringthevegetativeandreproductivestages of rice plant development using 16S amplicon sequencing. The study was conducted in the south of Brazil, during the crop years2011/12and2012/13.Comparativeanalysesshowedstrongdifferencesbetweenthecommunitiesoffloodwatersassociated withthetwodevelopmentalstages.Duringthevegetativestage,1551operationaltaxonomicunits(OTUs)weredetected,while lessthanhalfthatnumber(603)wereidentifiedinthereproductivestage.Thehigherbacterialrichnessobservedinfloodwater collected during the vegetative stage may have been favored by the higher concentration of nutrients, such as potassium, due torhizodepositionandfertilizerapplication.Eighteenbacterialphylawereidentifiedinbothsamples.Bothcommunitieswere dominatedbyGammaproteobacteria.Inthevegetativestage,AlphaproteobacteriaandBetaproteobacteriaweremoreabundant and,incontrast,BacilliandClostridiawerethemoredominantclassesinthereproductivestage.Themajorbacterialtaxaidentified havebeenpreviouslyidentifiedasimportantcolonizersofricefields.Therichnessandcompositionofbacterialcommunitiesover cultivationtimemaycontributetothesustainabilityofthecrop. 1.Introduction varyingphysicalandchemicalpropertiesinthisenvironment could support the growth of microorganisms possessing Rice (Oryza sativa L.) is the most important cereal crop in widerangesofmetabolicplasticity,allowingthemtoquickly theworld,feedingmorethan50%ofthehumanpopulation. adapt to changing environmental conditions [4]. Thus, the In South America, Brazil is the main producer [1], with rice ecosystem may be a prime habitat for microorganisms floodedricefieldsaccountingfor50%ofthetotalcroparea adaptedtofluctuatingnutritionallevelsandoxygenandlight undercultivationinthecountry[2].Infloodedrice,theneed availability. to maintain adequate water depth throughout most of the The phyla Acidobacteria, Actinobacteria, Bacteroidetes, cropyearcharacterizestheagriculturalsystemasaquaticin Chloroflexi,andProteobacteriahavebeenpreviouslyfound nature.Incomparisontootheraquaticenvironments,suchas in soil samples of rice-alfalfa [5] and rice-wheat cropping lakes, ponds, and swamps, the environmentalconditionsin [6]. In these agroecosystems, rice exudates and nutrients floodedricefieldsarerelativelyunstableduetophysicaland fromstraw incorporationwere shown to influencethe bac- chemical and biological characteristics that vary according terial community’s composition. Breidenbach and Conrad tocurrentagriculturalpracticesandwatersupplies[3].The [7] found a uniform bacterial composition in soil over the 2 InternationalJournalofMicrobiology rice growing season, with Proteobacteria being the most searchfortherichnessandabundanceofthelocalmicrobiota. highly abundant phylum, while Firmicutes represented the Afterwards, the 16 subsamples from each stage within a fifth most abundant phylum. Firmicutes were also present locationwerecombinedintoasinglecompositewatersample in relatively low abundance upon the introduction of a of 800mL for DNA isolation. The 12 samples representing maizerotationintoanirrigatedricefield[8].Althoughthese twolifestagesfromthreedifferentlocationswerecentrifuged microorganismsarecommoninhabitantsofagriculturesoils, at12,000×gfor15minat4∘Candthepelletswerestoredat thelowcountsofFirmicutesareintriguingconsideringthat −20∘CforsubsequentDNAextractionandanalysis. thisgroupcontainstheclassesBacilliandClostridia,which are often highly abundant in rice agricultural soils where 2.2. DNA Extraction and Pyrosequencing. Total DNA was theydecomposeplantresiduesusingcellulolyticenzymes[9]. extracted from each of the 12 pellets collected from the Furthermore, the researchers observed higher bacterial 16S floodwater samples from two life stages at three locations rRNAabundanceinthefloodingstagethanindrainagestage, using the MoBio Power Soil(cid:2) DNA Isolation Kit (MoBio, whichwasascribedtothericestrawthatremainedinthefield LaboratoriesInc.,Carlsbad,CA,USA)followingthemanu- [10]. facturer’sinstructions.TheDNAyieldwasmeasuredusinga In the studies mentioned above, the shifts in microbial NanoDrop(cid:2)ND-1000spectrophotometer(NanoDropTech- community structure were governed by environmental fac- nologies, Inc. Wilmington, DE, USA) and the DNA quality tors found in rice fields. These factors can be related to the was verified on a 1.5% agarose gel stained with ethidium input of nutrients from water sources, rice residues, and −1 bromide(0.1mgmL ). fertilizers,weatherconditions,andcroprotation,highlight- Purified DNA from the six replicates collected during ing the complex network of elements that govern bacterial the vegetative stage and the six replicates collected during structure in this agricultural system. Although microbial the reproductive stage were pooled together to create a ecologystudiesinsoil,rhizosphere,andendophyticenviron- single DNA pool for the vegetative samples and a single ments have been previously conducted in rice systems [11– DNA pool for the reproductive samples. These two DNA 14], the dynamics of bacterial communities in floodwaters pools(oneDNApoolfromvegetativesamplesandoneDNA from rice fields have not been extensively studied despite pool from reproductive samples) were used as templates the important roles of the floodwaters and microbial com- forampliconpyrosequencinganalysis,whichwasperformed munities in rice plant nutrition [15]. Because microbes can by MR DNA Laboratory (Shallow Water, TX, USA), with contribute strongly to rice nutrition and production, there the goal of investigating the bacterial community structure ismuchinterestinsurveyingthemicrobialcommunitiesin and composition. The V1–V3 variable regions of the 16S this flooded agroecosystem and determining how agricul- rRNA gene were amplified using primers ill27Fmod (5 - tural practices influence the composition and structure of AGRGTTTGATCMTGGCTCAG-3 ) and ill519Rmod (5 - these communities [16]. The purpose of the present study GTNTTACNGCGGCKGCTG-3 ) [19]. The PCR reactions was to investigate the bacterial community structure and werepreparedwith1𝜇LofDNA(5ng𝜇L−1)usingHotStar- composition in floodwaters associated with vegetative and TaqPlusMasterMix(Qiagen,Valencia,CA,USA).DNAwas reproductivestagesofriceinordertoverifyifthereisamicro- ∘ initiallydenaturedat94 Cfor3minfollowedby28cyclesof bialcommunityrelatedtoaparticularstageofthericesystem. ∘ ∘ ∘ 94 C for 30s; 53 C for 40s and 72 C for 1min; and a final ∘ extensionat72 Cfor5min.PCRproductsofapproximately 2.MaterialsandMethods 300bpwerepurifiedusingAgencourtAmpurebeads(Agen- court Bioscience Corporation, MA, USA). The amplicons 2.1. Study Area and Sampling Protocols. Three isolated were sequenced using 454 GS FLX Titanium chemistry floodedricefieldswereselectedforthisstudy.Thericefields (Roche)followingthemanufacturer’sguidelines.Theraw454 werebetween164and310hainareaandarelocatedinthecity readsgeneratedduringthecurrentstudyhavebeendeposited ∘ ∘ ofViama˜o(30 04 51 S,51 01 22 W),outercoastalplain,Rio inNCBI’sSequenceReadArchive(SRA)undertheaccession GrandedoSul(RS),Brazil,Figure1. SRP077313andareassociatedwithBioProjectPRJNA326968. Twelve water samples were collected from the three locationsaboveintheagriculturalyears2011/12and2012/13, 2.3. Protocols and Equipment Used for the Physicochemical sixinthevegetativeandsixinthereproductivestages.One Measurements of Water. Water parameters such as temper- sample from each location and developmental stage was ature,turbidity,andpHwere measuredfromall12 samples collected during the 2011/12 growing season and another usingtheIntelligentMeterequipment(INSTRUTHERMPH- sample was collected during the 2012/13 growing season. 1300).Inaddition,nutrientlevels,includingtotalphosphorus The collections were organized as follows: the vegetative (P)andpotassium(K),weremeasuredfromeachofthesix (tillering) (October/November) stage was defined by active water samples collected from the two developmental stages tilleringandcoleoptileandradicle(2-3mm)formationtothe using standard methods [18]. The available P and K were beginning of panicle differentiation, while the reproductive determined using Mehlich-1 solution by molecular colori- stagewasdefinedfromtheformationuntilcompletematura- metricandflameemissionmethods,respectively[20,21]. tionofthepanicle(DecembertoMarch)[17].Eachofthe12 individualwatersamplescollectedrepresentedacombination 2.4. Data Analysis. The 454 amplicon data from bacterial of16subsamplesof50mLcollectedfromthetopsurfaceof communitiessampledfromfloodwatersfromthereproduc- thefloodwaterto10cmindepth[18],therebymaximizingthe tive(𝑛=1)andvegetative(𝑛=1)stageswereanalyzedusing InternationalJournalofMicrobiology 3 7 7 7 7 7 7 7 7 0 15 30 45 0 15 30 45 8 6 4 2 1 9 7 5 5 5 5 5 5 4 4 4 ∘50 ∘50 ∘50 ∘50 ∘50 ∘50 ∘50 ∘50 80∘007 60∘007 40∘007 0∘00 0∘00 29∘53153 23∘2703 23∘2703 29∘5503 46∘5403 46∘5403 29∘56453 80∘00760∘007 40∘007 (a) 29∘58303 56∘5007 53∘1007 49∘3007 30∘0153 27∘3003 27∘3003 30∘203 31∘1003 31∘1003 30∘3453 0 2.500 5.(0m00) 10.000 56∘5007 53∘1007 49∘3007 (b) 7 7 7 7 7 7 7 7 0 5 0 5 0 5 0 5 58 61 43 24 51 91 73 54 ∘50 ∘05 ∘05 ∘05 ∘50 ∘04 ∘04 ∘04 5 5 5 5 5 5 (c) Figure1:(a)LocationofRioGrandedoSulstate,SouthernofBrazil.(b)Viama˜ocity,outercoastalplainofRioGrandedoSulstate;(c)study areawiththethreesamplingsitesinthefloodedricefields. the mothur pipeline (version 1.32.1) [22]. In brief, flow- taxonomy for each OTU was determined using the clas- grams were demultiplexed using the trim.flows command sify.otucommand.Rarefactioncurveswerecalculatedusing and denoised using the shhh.flows command, which is therarefaction.singlecommandatageneticdistanceof0.03, themothurimplementationofPyroNoise[23]. In addition, while the summary.single command was used to compute adapters,barcodes,primers,shortreads,andreadscontain- various community metrics including the Shannon-Wiener ingmorethaneighthomopolymerbaseswereremovedfrom (H )andSimpsonindices,theChao1richnessestimator[26], the dataset with trim.seqs command. Cleaned sequences which estimates species richness based on the number of were aligned to the Silva reference database [24] using the rareOTUsdetectedineachcommunity,andtheAbundance Needlemanalignerwiththealign.seqscommand.Chimeric Coverage-basedEstimator(ACE),whichestimatesthenum- sequenceswereflaggedandremovedfromthedatasetusing berofundetectedOTUsbasedontheabundanceanddistri- theuchimealgorithmwiththereference=self-flag[25].Then, butionofrareOTUs.Priortocomputingrarefactioncurves the remaining high quality sequences were taxonomically andcommunitydiversity/richnessmetrics,thesamenumber classified using the Wang method of the classify.seqs com- ofreads(7,348)weresubsampledwithoutreplacementfrom mand and the Silva reference taxonomy files. An 80% con- eachofthelibrariesfornormalizationandtopreventdiffer- fidence score was required for all taxonomic assignments. encesinlibraryyieldsfromdrivingdifferencesbetweenthe Ampliconsclassifiedasmitochondrial,chloroplast,Archaeal, twocommunities.ThemothurcommandLibshuffwasused eukaryotic, or unknown in origin were removed from the to determine whether the bacterial communities from the dataset. vegetative and reproductive stages have the same structure Theremainingbacterialsequenceswerecategorizedinto withiterssetto1000. operationaltaxonomicunits(OTUs)at3%sequencedissimi- Heatmapsandcluster dendrogramsbasedonEuclidean larity using the average neighbor algorithm. The consensus dissimilarity metrics were built according to the relative 4 InternationalJournalofMicrobiology −3 −2 −1 0 1 2 3 physicalandchemicalvariationsoffloodwaterofricefields in vegetative and reproductive stage of two consecutive 0.6 3 agricultural years. The physical and chemical patterns of floodwater retrieved from the vegetative and reproductive 0.4 Temperature 2 ricestagesareshowninFigure2. Thefirsttwoprincipalcomponentsexplainedacombined 0.2 K 1 total of 68% of the total variance. Most water samples % 5 collected from the vegetative stage were separated from the 1. axis 2 0.0 P 0 rdeipffreorednuccetsivebesttwageeensamlocpaletisonalsonogr tahgeriPcuCl1tuarxails.yeNaorsmwaejorer 2 PC −0.2 −1 noted. In general, vegetative stage samples tended to have higherlevelsofpH,K,andPcomparedtothereproductive −0.4 pH −2 samples.Incontrast,thereproductivesamplestendedtobe Turbidity more turbid and had higher temperatures compared to the vegetativesamples.Inaddition,somevariabilitywasapparent −0.6 −3 withinthewatersamplescollectedfromeachdevelopmental stage,whichislikelyreflectiveofthedynamicnatureofthe −0.6 −0.4 −0.2 0.0 0.2 0.4 0.6 physicalandchemicalvariablesinricefloodwaters(Figure2). PC 1 axis 46.5% Temperature and K differed significantly between the two Vegetative ricedevelopmentstages.Specifically,thetemperaturewason Reproductive averagethreedegreeswarmerinfloodwatersassociatedwith thereproductivestage.Kwasalmostfourtimeshigherinthe Figure2:PCAbiplotofphysicalandchemicalparameterssampled vegetativecomparedtothereproductivestage(Table1). fromricefloodwatersfromvegetativeandreproductivestages. 3.2.CompositionoftheBacterialCommunityinFloodwaters abundancesofthemostcommongenerainthetwocommu- over Two Stages of Rice Growth. The pyrosequencing-based nitiesusingthe“vegan,”“heatmap.2,”and“cluster”packages analysis generated 25,981 amplicons from the vegetative [27] in the R statistical computing environment (version stage samples and 18,849 amplicons from the reproductive 3.1.0).Toselectthemostabundantgenera,readscountsfor stage samples. After quality filtering and dereplication of allOTUsassignedtothesamegenusfrombothsampleswere identicalsequences,8,483readswereretainedfromthewater summed together, normalized by relative abundance, and samples collected during vegetative stage and 7,348 reads rankedinascendingorder.Therelativeabundancesofthese wereretainedfromsamplescollectedduringthereproductive genera in floodwaters associated with each developmental stage. For normalization purposes, 7,348 reads were ran- stagewerelog2 transformed,𝑧-scalestandardized,andused domlysubsampledwithoutreplacementfromthevegetative forclusteringandheatmapanalysis.Venndiagramsdepicting librarypriortoOTUanalysisandtaxonomicclassification. OTUsfoundinfloodwatersfrombothdevelopmentalstages The structures of the bacterial community differed sig- and and OTUs unique to each developmental stage were nificantlybetweenthevegetativeandreproductivestagesof constructedusingthevenncommandinmothur. flooded rice (𝑝 = 0,0001) using Libshuff. In the vegetative The physical and chemical characteristics of the flood- stage, 1,551OTUs were identified, while less than half the water from the rice fields sampled during two agricultural number of OTUs (603) were detected in water samples yearswereanalyzedbyprincipalcomponentsanalysis(PCA) collected from the reproductive stage (Table 2). Further, ∘ using the following variables: temperature ( C), turbidity only 88 (4.08%) of the OTUs detected in this analysis were (NTU), pH, total phosphorus (P) (mgL−1), and potassium commontobothcropstages,possiblyreflectingthedynamic (K)(mgL−1).Priortoanalysis,allvariableswerelog10trans- structure of the bacterial communities associated with this formed in order to facilitate comparisons among variables environment(Figure3). expressedindifferentunits.Thecorrelationmatrixwiththe The sequences were distributed among 18 different bac- varimaxrotationwassetandonlyautovaluesgreaterthan1 terial phyla. The most species-rich phyla in both the repro- wereutilizedascriteriaforextractionoftheprincipalcom- ductive and vegetative stages were Proteobacteria, which ponents. The analysis was performed in the R statistical contained 53.34% of the OTUs detected in both sam- computing environment (version 3.1.0) using the princomp ples, Bacteroidetes (16.80% of the OTUs), Actinobacteria andbiplotfunctions.Thedifferencesamongphysicochemical (7.84%),andFirmicutes(5.52%).Intotal,83.50%ofthetotal parametersbetweenthericestagesweretestedusingStudent’s OTUs detected in these two communities was associated 𝑡-testinSYSTAT12(SystatSoftware,Inc.,CA,USA).𝑝values with these four phyla. Several phyla with lower richness of<0.05wereconsideredstatisticallysignificant. estimates were also detected in these samples, defined as phyla containing less than 1% of the total OTUs detected 3.Results in this analysis. Based on this criterion, a total of twelve rare phyla were detected including Chloroflexi, Deferrib- 3.1.PhysicalandChemicalCharacteristicsofRiceFieldWater. acteres, Deinococcus-Thermus, Fusobacterium, Gemmati- Principal components analysis was used to monitor the monadetes, OP10, Planctomycetes, SR1, Spirochaetes, TM7, InternationalJournalofMicrobiology 5 Table1:Meanvaluesandcorrespondingstandarddeviations,forthephysicochemicalparametersmeasuredinthewatersamplesinrelation tothericestages. Ricestages Temperature∗(∘C) pH Turbidity(NTU) TotalP(mg/L) TotalK(mg/L)∗ 30.20 6.50 4.30 0.65 14.70 24.06 6.21 34.16 0.44 31.75 22.73 7.43 68.83 0.84 12.34 Vegetative 29.40 6.70 39.86 0.01 11.77 23.60 6.50 37.56 0.02 4.29 27.20 7.43 42.20 1.30 11.59 Mean±SD 26.20±3.18 6.80±0.51 37.82±20.60 0.54±0.49 14.41±9.19 28.70 6.17 108.00 0.05 4.50 31.30 6.70 41.80 0.05 4.20 27.30 6.20 253.20 0.01 1.89 Reproductive 29.20 6.43 93.10 NA 6.10 29.60 6.50 27.55 0.17 5.04 30.80 6.50 391.00 0.14 1.62 Mean±SD 29.48±1.44 6.42±0.20 152.44±141.70 0.08±0.06 3.89±1.77 NA:notavailable;SD:standarddeviation;∗meansdifferedsignificantly(𝑝<0.05). Table2:Richnessestimators(Chao1andAce)anddiversityindicesofShannon-Wiener(H)andSimpsonfrombacterialcommunities sampledfromfloodwatersduringreproductiveandvegetativestagesofriceusing16Samplicons.A3%nucleotidedissimilaritywasusedfor OTUdiscrimination. Numberofsequences 3%divergence Cropstage Rawsequences Analysedsequences Normalization OTUs Chao1 Ace Shannon-Wiener(H) Simpson Vegetative 25,981 8,483 7,348 1,551 2,282 2,266 5.77 0.03 Reproductive 18,849 7,348 7,348 603 822 842 4.28 0.05 the class level distributions of OTUs unique to floodwaters sampled from either the vegetative or reproductive stages Vegetative Reproductive were drastically different. For example, the community of OTUs unique to the floodwaters of vegetative stage plants 1463 88 515 wasdominatedbyGammaproteobacteria(34.5%),Alphapro- teobacteria (18.4%), and Betaproteobacteria (10.8%) (Fig- ure 4(c)). Of significance, 24.6% of the amplicon reads derivedfromOTUsexclusivelyassociatedwiththevegetative stage could not be conclusively assigned to the class level (Figure 4(c)). In contrast, the community of OTUs unique Figure 3: Venn diagram of 16S OTUs shared and unique to floodwater samples collected from vegetative and reproductive tofloodwatersofreproductivestageplantswasdominatedby stages of rice plants. Sequences were classified into OTUs at 97% Gammaproteobacteria(43.9%oftheampliconreads),Bacilli similarityusingtheaverageneighboralgorithminmothur. (25.4%), Clostridia (21.8%), and Betaproteobacteria (17.7%) (Figure4(d)). Of the 169 genera identified in the two developmental Tenericutes, and Verrucomicrobia, which were detected in ricestages,22(13%)occurredinbothstages(Figure5).Bei- both stages of crop development. The phyla Acidobacteria jerinckia, Curvibacter, Pelomonas, and Rhodoferax occurred (1.94% of the OTUs) and Cyanobacteria (1.25%) were also in high counts in both phenological stages. In general, the present,butatlowfrequencies(≤2%oftheOTUs). abundancesofBeijerinckia,Pelomonas,andRhodoferaxwere In total, 27 different bacterial classes were identified in similar in flood waters from both communities; however, both developmental stages. In general, the class level abun- therelativeabundanceofCurvibacter wasslightlyhigherin dancesofthe88OTUssharedbetweenthefloodwatersfrom vegetative stage. The abundances of the genera Aeromonas, thevegetativeandreproductivestageswereverysimilarand Bradyrhizobium,Emticicia,Massilia,Methylibium,andSpiro- werebothdominatedbyBetaproteobacteria,Actinobacteria, soma were lower and did not differ significantly between andAlphaproteobacteria(Figures4(a)and4(b)).Incontrast, vegetativeandreproductivestages(Figure5). 6 InternationalJournalofMicrobiology Vegetative Reproductive Gammaproteobacteria Flavobacteria 0.1% Holophagae Gammaproteobacteria Holophagae Deltaproteobacteria 1.2% 0.09% Sphingobacteria Flavobacteria 0.1% 0.2% 0.7% 1.1% 3.5% Sphingobacteria Deltaproteobacteria 3.7% Cyanobacteria 0.2% Actinobacteria 0.02% Cyanobacteria 17.8% 0.07% Actinobacteria Alpha- 18.8% proteobacteria 7.0% Alpha- proteobacteria 12.1% Betaproteobacteria 65.5% Betaproteobacteria 63.7% (a) (b) Reproductive Alphaproteobacteria Sphingobacteria Vegetative 2.8% 2.7% Actinobacteria Deltapr3o.t3e%obacteria Bac3te.2r%oidiaO8.t9h%er Unc3la.5s%sified 1.7% O2.t8h%er Gammap4r3o.9te%obacteria Sphingobacteria Flavobacteria 4.6% Unclassified 3.8% 24.6% Erysipelotrichia Flavobacteria 5.0% 8.0% Actinobacteria 8.3% Betaproteobacteria Betaproteobacteria 17.7% 10.8% Alphaproteobacteria 18.4% Clostridia Gammaproteobacteria 21.8% Bacilli 34.5% 25.4% (c) (d) Figure 4: Relative abundances of class level assignments for the 88 shared OTUs in the vegetative stage (a) and reproductive stage (b) andrelativeabundancesoftheclasslevelassignmentsofthe1463OTUsuniquetothevegetativestage(c)andthe515OTUsuniquetothe reproductivestage(d).OTUsweretaxonomicallyclassifiedbytheWangmethodinmothurusingan80%confidencethresholdforclasslevel assignments. Figure5showsacomparativeanalysisofthetwenty-two isprobablydueinparttothelowerrichnessassociatedwith mostabundantbacterialgeneradetectedinthereproductive the reproductive stage, the higher number of rare OTUs andvegetativestagesoffloodedrice. foundinthevegetativestage,andtheoverabundanceofthree Polynucleobacter (29.5%),Curvibacter (23%),andRhod- genera, Alcaligenes, Curvibacter, and Flavobacterium in the oferax (10.3%) represented the most abundant genera in reproductivestage.TheChao1richnessestimatorpredicted the vegetative stage, while Curvibacter (18.3%), Alcaligenes atotalof2,282OTUsinthevegetativebacterialcommunity (11.8%),andFlavobacterium(11.3%)weremoreabundantin (32%moreOTUsthanwhatweredetected),while822OTUs thereproductivestage(Figure6). werepredictedinthereproductivebacterialcommunity(27% TheShannon-Wiener(H)indexwasapproximately25% more OTUs than what were detected). Considering these higher in the water sample collected from the vegetative results, it is clear that a larger number of rare species were stage compared to the reproductive stage, suggesting that associated with water collected from the vegetative stage the vegetative community is richer. In addition, the Simp- comparedtothereproductivestage(Table2). son index, which represents the probability that two reads Reflecting the higher richness and higher numbers of selected at random belong to the same OTU, was higher in rare OTUs, the rarefaction curve of the vegetative stage thesamplecollectedfromthereproductivestage.Thisfinding did not reach complete saturation considering the number InternationalJournalofMicrobiology 7 −2 −1 0 1 2 Column Z-score Vegetative Reproductive Flavobacterium Arcicella Aquitalea Alcaligenes Polynucleobacter Leptothrix Geobacter Novosphingobium Sediminibacterium Brevundimonas Spirosoma Pelomonas Curvibacter Bradyrhizobium Roseomonas Aeromonas Rhodoferax Emticicia Methylibium Massilia Geothrix Beijerinckia Figure5:Heatmapandcorrelationanalysisofthe22bacterialgenerafoundinboththevegetativeandreproductivestagesoffloodedrice. Therelativeabundancesofthesegenerainfloodwatersassociatedwitheachdevelopmentalstagewerelog2transformed,scaledby𝑧-score, andusedforclusteringandheatmapanalysis.Colorintensityiscorrelatedwiththerelativeabundanceofeachgenusinfloodwatersassociated withthetwodevelopmentalstages,withblueindicatinghigherrelativeabundanceandyellowindicatinglowerrelativeabundance. Vegetative Reproductive Sedimin0i.8b%acteriumGe0o.3th%rAixr0c.i8c%ella Spi0ro.8s%oma Em0t.8ic%iciaBrBaedijy5e2r.r4h.i4%ni%zcokbiaium GeothrixE m0.7ti%cicAiar c1i.c0e%lla 11.1% Sedimin0i.2b%acteriuSmpirosomBar 0a.d5y%1rh.9i%zobBieuimjerinckia 7.5% Flavobacterium Brevundimonas 3.0% Aeromonas 0.5% Brevundimonas 1.7% 3.3% Aeromonas Novosphingobium 1.1% Novosp0h.2in%gobium 0.5% Roseomonas 0.3% Roseomonas 1.2% Ge2o.b2a%cter Alc0a.l5ig%enes Flavobacterium 11.3% Alcaligenes 11.8% Rhodoferax Aquitalea Geobacter 1.0% 10.6% 0.3% Curvibacter Rhodoferax 10.3% Aquitalea 7.0% 23.0% Polynucleobacter Leptothrix Polynucleobacter Curvibacter 18.3% 29.5% Massilia 4.6% 4.6% 0.3% Pelomonas 7.2% Pelomonas Methylibium Massilia 0.5% Leptothrix 1.2% 9.2% 0.3% Methylibium 0.5% (a) (b) Figure6:RelativeabundancesofgenuslevelassignmentsfortheOTUssharedbetweenvegetativestage(a)andreproductivestage(b). 8 InternationalJournalofMicrobiology 1600 stagesoffloodedrice,withthediversityandrichnessvalues 1400 associatedwiththevegetativestageexceedingthoseobserved Us1200 in the reproductive stage. Previous research on rice crops OT1000 reportedthattherichnessanddiversityofbacterialcommu- of 800 nities can change throughout the rice cultivation period in ber 600 aquaticenvironments[31–33]andinthesoilandrhizosphere m u 400 environments [34–36]. Although previous studies did not N 200 elucidate the environmental factors responsible for these 0 changesincommunitystructure,floodwatercharacteristics, 1 0 0 0 0 0 0 0 0 0 0 0 0 0 0 such as pH, temperature, changes in nutrient profiles, and 0 0 0 0 0 0 0 0 0 0 0 0 0 0 5 10 15 20 25 30 35 40 45 50 55 60 65 70 seasonalvariationsinfertilizerapplication,havebeenrelated Number of amplicons toshiftsinmicrobialcommunitystructureandcomposition Vegetative over crop development [32]. Additional factors related to Reproductive plantgrowthcanalsocauseshiftsinmicrobialcommunities. Forexample,Okabeandcoworkers[31]determinedthatplant Figure7:Rarefactioncurvesgeneratedfrom16Sampliconssampled growthvarieswiththeincidenceofsunlight,which,inturn, from floodwaters from vegetative and reproductive rice stages. canimpactthewatertemperatureandalgalgrowth.Higher Rarefaction curves were generated using the rarefaction.single commandinmothurwithfreq=100anditers=10000. photosynthesis rates associated with algal proliferation and alsoplantgrowth[34]canultimatelyleadtoincreasedlevels of photosynthates in the water, altering the water pH and of sequences sampled, indicating that additional OTUs will potentiallyalteringthebacterialcommunity. likelybedetectedwithadditionalsequencing.Ontheother Atotalof2,066OTUsat3%dissimilaritywereidentified hand,rarefactioncurveofthereproductivestageshowedsta- infloodwaterscollectedfromthereproductiveandvegetative bilization,indicatingthatthesequencingeffortwassufficient developmental stages of rice. In flooded rice systems, the tocapturethemajorityoftheOTUsassociatedwiththiscom- short spacing between the plants, the low depth of the munity(Figure7). floodwaters (10cm deep), and soil management regimes can increase the levels of suspended soil particles in the 4.Discussion floodwaters [37], which is in contrast to other more static aquatic ecosystems. Due to the high turbidity and the Infloodedrice,thewatersourceusedforcultivationisakey presence of soil in the floodwaters, it is expected that component in the management of the crop. Nutrient levels bacterialgroupsassociatedwithsoil,suchasProteobacteria, in these water sources can have significant effects on plant Bacteroidetes,Actinobacteria,andFirmicutes,willbepresent nutrition[28]whilevaryingphysicalandchemicalproperties in the floodwaters of rice fields, contributing to the total inthesewatersourcescanalsoinfluencethestructure,diver- bacterialdiversity[38].Supportingthishypothesis,themajor sity, and taxonomic composition of microbial communities phyla identified in the floodwaters associated with both inthefloodwaters,whichinturncanalsoprofoundlyimpact developmental stages were Proteobacteria, Bacteroidetes, plant nutrition. In the rice field plots used for this study, Actinobacteria, and Firmicutes, while Acidobacteria and the primary water source contains a high proportion of Cyanobacteria were less frequent. The same phyla were wastewaterinputfrombothurbanandagriculturalareas[29]. highlyabundantinotherricehabitats[7],andspecificallyin Therefore,avarietyofchemicalelementsenterthefloodplain water samples collected from flooded rice crops [3, 32, 39]. and the temporal fluctuations in the abundance and types Furthermore, Proteobacteria (alpha- and beta-subdivision), of chemical elements entering the fields can have strong Bacteroidetes,andActinobacteriawerealsocitedasthemajor influences on the microbial community in rice floodwaters groups of bacteria found in freshwater environments [39]. [30]. Inunstableenvironments,suchasricefields,Proteobacteria In the current study, the water samples retrieved from may contribute to the growth, development, and physiol- vegetativeandreproductivestagesshowedvariationsinphys- ogy of rice plants due to the presence of plant growth- ical and chemical parameters. The abiotic parameters most promoting bacteria, which are often able to induce callus stronglyassociatedwiththevegetativestagewerepH,P,andK in rice and produce phytohormones [40]. According to andinthereproductivestage,theparametersweretempera- Mhuantongetal.[16],thepresenceofthesebacterialgroups tureandturbidity(Table1).Oftheseparameters,temperature in a variety of freshwater ecosystems is related to their (higher in floodwaters from the reproductive stage) and K metabolicplasticitytodecomposeanassortmentoforganic (higher in floodwaters from the vegetative stage) differed matter. significantlybetweenthetworicedevelopmentstages.These Despitethepresenceofseveralcommonphylainflood- results reflect differences in microenvironments between waters sampled from both developmental stages, only 88 the rice plant-phenological stages that may have affected (4.08%)oftheOTUswerecommonbetweenvegetativeand microbial growth and persistence. Supporting the possible reproductive stages, suggesting that the dynamics of the impactoftheseenvironmentalconditionsonbacterialcom- bacterialcommunitiesinfloodwaterschangethroughoutthe munities,significantdifferencesincommunitycomposition growingseason.Thesechangescouldreflecttemporalvaria- were observed between the vegetative and reproductive tionsincarbonavailability.Forexample,inapreviousstudy, InternationalJournalofMicrobiology 9 Aulakh and coworkers [41] documented higher exudation Beijerinckia, Curvibacter, Pelomonas, and Rhodoferax rates over the course of rice plant development, in which were the four most abundant genera in both stages of the sugars in the exudates were eventually replaced by organic crop. These bacterial groups are often associated with high acidsinlaterdevelopmentalstages.Bothsugarsandorganic availabilitiesofsugar(e.g.,glucose)[52].Inagriculturaland acidsareessentialforbacterialnutritionandcontributetothe freshwaterenvironments,Beijerinckiaarereportedasgrowth process of microbial colonization [42]. Furthermore, when promoters in plants [53], while the genomes of Curvibacter soluble carbon is released into the rhizosphere, microbes spp.oftencodeforlargenumbersofsugartransporters[54], in the soil quickly mineralize the available carbon [43]. enhancing its ability to explore nutrients from the environ- Thereby,theamountofrootexudatesinthesoilcouldaffect ment. Other genera, such as Pelomonas sp. and Rhodoferax the relative amounts of carbon and nitrogen available for sp.,werefoundinapproximatelythesameproportioninboth microbial growth [44], promoting transitions in the size of rice stages. Previous rDNA 16S amplicon analysis showed populations and structure of microbial communities in the that Rhodoferax spp. are common in diverse freshwater rhizosphere[45].Nevertheless,thecompositionandquantity systems [55]. Some species of the genera Rhodoferax are ofexudatesaredynamicintimeandspace,andthereforeit nitrate-reducers [56], while Pelomonas spp. often code for becomesdifficulttoresolvetheroleofasinglecomponentin machinery required for nitrogen fixation (nifH gene) [57]. thestructureofmicrobialcommunity[46]. Thus, the OTUs assigned to these genera in the current The richest bacterial classes found in the vegetative studymaycontributetonitrogenfluxinfloodedricefields. stage were Gammaproteobacteria (276OTUs), Alphapro- In contrast, the abundance of the genus Polynucleobacter teobacteria(237OTUs),andBetaproteobacteria(211OTUs), differedsignificantlyinfloodwatersfromthetwolifestages. while richness was the highest in Gammaproteobacteria Itsabundancewassignificantlyhigherinthevegetativestage (24OTUs), followed by Bacilli (46OTUs) and Clostridia (29.5%) compared to reproductive stage (4.6%). This result (18OTUs) during the reproductive stage. In flooded plains, could suggest that the OTUs derived from this genus are theadherenceofBetaproteobacteriarepresentativestoparti- notwelladaptedtoenvironmentalconditionsassociatedwith clescanplayanimportantroleintheirtransportfromtheter- floodwaterscollectedfromreproductivestageplants.Polynu- restrialenvironmenttofloodwater[47],whilethericephyl- cleobacter members often dominate planktonic freshwater losphere is greatly colonized by Alphaproteobacteria class communities [58], where pH, conductivity, and dissolved [48].Thus,Beta-andAlphaproteobacteriarepresentrelevant organiccarbonconcentrationplayanimportantroleincolo- bacteria groups in the soil whose abundances are strongly nization[59].Also,flagellategrazingandtheconsumptionof linkedtocarbonsupply[49].Infloodedricesystems,these lowmolecularweightsubstratesarerelatedtothesurvivalof bacterial groups decompose organic matter derived from Polynucleobacterinfreshwaterenvironments[60,61]. rice straw and other fermentable crop residues along with Rises in temperature can increase the abundance of fertilizerwhereorganicmolecules(humicsubstances)canact prokaryotes of the natural communities by enhancing their asanelectrondonorduringmicrobialrespiration[47]. growthrates[62].TheabundanceofthephylumFirmicutes Gammaproteobacteriawerepresentinhighrichnessand (5.52%) found in the reproductive stage is consistent with abundanceinfloodwatersassociatedwithbothricedevelop- the abundance of this phylum commonly found in the rice mentalstages.Overall,membersfromthephylumProteobac- fields [63]. However, the presence of these spore-forming teriaareoftenthemostabundantfreshwaterprokaryotes,but populations in the reproductive stage may be related to the Gammaproteobacteriaareusuallypresentinlowortransient characteristicsoftheorganicmatteravailableassociatedwith abundances [38], although they were previously found in this developmental stage [63] which may vary from straw high amounts in the rice phyllosphere [40]. This finding residues and root residues [64]. Species belonging to the suggests that specific environmental factors associated with class Clostridia are able to express enzymes that degrade the rice agroecosystem, such as the source of water used the cellulose and sugar transport systems to quickly uptake to irrigate the fields and the turbidity of the floodwaters, sugars released from plant cell walls [65]. In rice field soil, provided conditions for the survival and persistence of these organisms were responsible for the decomposition of ∘ members of this phylum with the entrance of nutrients. strawresidueat15and30 C[64].Fromthisbasis,conditions ThisclasshoststhegeneraEscherichia,Salmonella,Yersinia, found in reproductive stage such as the high temperature Vibrio, and Pseudomonas characterized by their metabolic andcarbonavailabletobedegradedmayhavepromotedthe plasticity that can be adapted to varying levels of temper- proliferation of OTUs belonging to Gammaproteobacteria ature, oxygen supply, and nutritional requirements. Hence, andFirmicutes. membersoftheclassGammaproteobacteriaoftendominate Rhizodepositionoccurscontinuouslyduringthelifetime microbial assemblages after nutrient enrichment [50]. In ofplantsintheformofwatersolubleexudates,secretions,and addition, the members of this group contain pathways for plantdeadcells.Thisprocesscontributesasaprimarysource degradationofcarbohydrates,aminoacids,andxenobiotics ofenergyandnutrientsformicrobesinthefloodwaters[66]. thatmayprovidecompetitiveadvantagesundercertaineco- In future studies, the release of carbon compounds from logicalcondition[51].Furthermore,theinteractionbetween rice roots should be considered in the investigation of the Gammaproteobacteria members and rice plants may be factors responsible for shaping the structure of the bacte- beneficial to both parties, with the leaf exudates providing rial communities in floodwaters of rice systems [34]. With nutrientsthatsupportmicrobialgrowthandmicroorganisms respect to environmental and nutritional conditions during assistingbetterriceyield[40]. the vegetative stage, approximately 20% of the absorbed 10 InternationalJournalofMicrobiology photosynthetic carbon is released through rhizodeposition regarding the composition and quantification of root exu- [67]. Moreover, during the reproductive stage, the plants dates and the impacts of rice exudates on microbial com- releaseloweramountsofcarboncompoundsintheirexudates munities in rice fields are essential to decipher the linkage becausetheydevotethemajorityoftheirenergytoseedpro- between the microbial community dynamics and rice plant duction [68, 69]. Breidenbach and Conrad [7] investigated overcultivationtime. the bacterial community of the soil from rice fields using 16SrDNAampliconanalysisandalsoprofiledtheexpression Disclosure levelofvarioustaxathroughoutthevegetative,reproductive, and maturation stages. According to quantitative PCR, the The U.S. Department of Agriculture, Agricultural Research authorsdetected elevatedbacterialabundancesinsoilfrom Service,isanequalopportunity/affirmativeactionemployer the reproductive stage, but there were no major differences andallagencyservicesareavailablewithoutdiscrimination. between the bacterial community compositions during the Mention of commercial products and organizations in this twogrowthstages.Changesinbacterialabundancebetween manuscriptissolelytoprovidespecificinformation.Itdoes soil collected from the vegetative and reproductive stages notconstituteendorsementbyUSDA-ARSoverotherprod- werestronglyattributedtodecreasedlevelsofrootexudates uctsandorganizationsnotmentioned. by plants nearing maturity. In general, the abundance of ConflictsofInterest bacteriainthesoilwasdynamicthroughoutthedevelopment of rice plants; however, no microbial taxa appeared to be The authors declare that there are no conflicts of interest exclusivelyassociatedwithaparticularstageofdevelopment. regardingthepublicationofthispaper. Heterotrophic microorganisms, which represent a large portionofthericefieldmicrobiome[70,71],aredependent Acknowledgments oncarbonsubstratesfortheirenergysupply.Thevegetative stage (tillering) is the most vigorous growth period of the The authors would like to thank CAPES (Coordenac¸a˜o rice plant [72]. As plant biomass and growth increase, de Aperfeic¸oamento de Pessoal de N´ıvel Superior) for the intensifications of organic carbon secretions can also occur Sandwich Ph.D. Program [Grant no. 260213-0] and USDA [73]. Thus, considering that the higher carbon levels could (United States Department of Agriculture) for the financial support the persistence of a larger diversity of microbes, support. the higher levels of exudates could contributeto the higher richnessobservedinthisstudyinfloodwaterscollectedfrom References vegetativestage.Moreover,theuseofureainfertilizers,which is applied mainly during the vegetative stage, can affect the [1] IRRI-InternationalRiceResearchInstitute,“RiceinAmerica + concentrationsofavailablenutrients,especiallyNH4 ,which Latine,past,present,andpromisingfuture,”RiceToday,vol.14, isthemainformofavailableNinthesoil[74].Thesefactors, pp.1–23,2015. aloneorincombination,mayhavehelpedtoshapethebac- [2] GRiSP-GlobalRiceSciencePartnership,“Ricealmanac,”Los terialcommunities,increasingitsdiversityinthevegetative Ban˜os,Philippines:InternationalRiceResearchInstitute,2012. stageofcrop.Inthatsense,thereleaseofrootexudatescan [3] T.Shibagaki-Shimizu,N.Nakayama,Y.Nakajima,K.Matsuya, influencethedynamicsofbacterialcommunitiesduringcrop M. Kimura, and S. Asakawa, “Phylogenetic study on a bac- developmentandshouldbeinvestigatedasacontributorto terial community in the floodwater of a Japanese paddy field bacterialcommunitydynamicsinricefloodwaters. estimatedbysequencing16SrDNAfragmentsafterdenaturing gradientgelelectrophoresis,”BiologyandFertilityofSoils,vol. 42,no.4,pp.362–365,2006. 5.Conclusion [4] A. E. Bernhard, D. Colbert, J. McManus, and K. G. Field, Thisstudyrevealedthatthecommunitiesassociatedwithrice “Microbial community dynamics based on 16S rRNA gene profilesinaPacificNorthwestestuaryanditstributaries,”FEMS floodwaters were variable and differed between floodwaters MicrobiologyEcology,vol.52,no.1,pp.115–128,2005. from the vegetative and reproductive stages of rice. The [5] A.R.Lopes,C.M.Manaia,andO.C.Nunes,“Bacterialcom- higherbacterialrichnessobservedinfloodwatersassociated munity variations in an alfalfa-rice rotation system revealed withvegetativeplantsmayhavebeen favoredby thehigher by 16S rRNA gene 454-pyrosequencing,” FEMS Microbiology concentration of nutrients (for example, phosphorus and Ecology,vol.87,no.3,pp.650–663,2014. potassium) due to changes in rhizodeposition and crop [6] J.Zhao,T.Ni,W.Xunetal.,“Influenceofstrawincorporation management. OTUs from the phylum Proteobacteria were withandwithoutstrawdecomposeronsoilbacterialcommu- present in floodwaters collected from both developmental nitystructureandfunctioninarice-wheatcroppingsystem,” stages, indicating the persistence of this phylum in flooded Applied Microbiology and Biotechnology, vol. 101, no. 11, pp. rice ecosystems. Moreover, the predominance of the class 4761–4773,2017. Gammaproteobacteria and the occurrence of the phylum [7] B.BreidenbachandR.Conrad,“Seasonaldynamicsofbacterial Firmicutes in the reproductive stage demonstrated that the andarchaealmethanogeniccommunitiesinfloodedricefields environment was favorable to microbes that can persist andeffectofdrainage,”FrontiersinMicrobiology,vol.5,article longer in paddy fields where they are able to utilize the 752,2014. degradablefractionoforganicmaterialsandsurviveinwater- [8] B.Breidenbach,M.B.Blaser,M.Klose,andR.Conrad,“Crop logged and dry conditions. However, further investigations rotationoffloodedricewithuplandmaizeimpactstheresident
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