h tt p : / / w w w . b j m i c r o b i o l . c o m . b r /
Environmental
Microbiology
Eichhornia
azurea
decomposition
and
the
bacterial
dynamic:
an
experimental
research
Zaryf
Dahroug
a,
Natália
Fernanda
Santana
a,
Thomaz
Aurélio
Pagioro
b,∗aProgramadePós-graduac¸ãoemEcologiadeAmbientesAquáticosContinentais,UniversidadeEstadualdeMaringá(UEM),Mariná, PR,Brazil
bUniversidadeTecnológicaFederaldoParaná(UTFPR),Curitiba,PR,Brazil
a
r
t
i
c
l
e
i
n
f
o
Articlehistory:
Received13December2012 Accepted19August2015 Availableonline2March2016 AssociateEditor:LaraDurãesSette
Keywords: Decompositionrate Dryweight Aquaticmacrophyte COD
a
b
s
t
r
a
c
t
Organicdecompositionisacomplexinteractionbetweenchemical,physicalandbiological processes,wherethevarietyofaquaticvascularplantsisessentialforthetrophicdynamics offreshwaterecosystems.Thegoalofthisstudywastodeterminetheaquaticmacrophyte
Eichhornia azurea(Sw.)Kunthdecompositionrate,the timerelationwith the limnologi-calparameters,andwhetherthisrelationshipisaresultofdecompositionprocesses.To thatend,wecollectedwaterandleavesofE.azureainSurfLeopoldo,PR.Theexperiment consistedoftwotreatments:25containerswith450mLofwaterand0.8gofbiomassdry weightwereusedwithorwithouttheadditionofmacrophytes.Sampleswerecollectedin triplicateattimes0,3h,6h,12h,24h,72h,120h,168hand240h.Whenthecontainerwas removed,theplantmaterialwasdriedinanoven.After48h,thematerialwasmeasured toobtainthefinaldryweight.AnalysesofpH,conductivity,dissolvedoxygen,total phos-phorusN-ammonia(NH4),solublereactivephosphorus(PO4)anddissolvedorganiccarbon
wereperformed,andthedecompositionratewascalculated.Theresultsshowedsignificant temporalvariationoflimnologicalparametersinthestudy.Additionally,dissolvedoxygen, conductivity,dissolvedorganiccarbonandtotalphosphoruswerecorrelatedwiththedry weightofthebiomass,suggestingthatE.azureadecompositionsignificantlyinterfereswith thedynamicsofthesevariables.
©2016SociedadeBrasileiradeMicrobiologia.PublishedbyElsevierEditoraLtda.Thisis anopenaccessarticleundertheCCBY-NC-NDlicense
(http://creativecommons.org/licenses/by-nc-nd/4.0/).
Introduction
Aquaticmacrophytes areimportantcomponentsof ecosys-temsthatprovidefloodpulse.Theyhavespatialandtemporal characteristicsthat maketheminterestingforthestudy of decompositioninaquaticplants.1–3Macrophytesareoftenthe
∗ Correspondingauthor.
E-mail:pagioro@utfpr.edu.br(T.A.Pagioro).
primary producers,especiallyin lenticenvironments. They haveamajorroleinnutrientcyclingandindebrisformation, beinganabundantsourceoforganicmatter.4,5Additionally,
theyareamixedstands,whichinfluencesthephysicaland chemical characteristics of water, altering the turbulence, temperature,sunlightpenetration,concentrationand distri-butionofdissolvedoxygenandnutrients.6
http://dx.doi.org/10.1016/j.bjm.2015.08.001
1517-8382/©2016SociedadeBrasileiradeMicrobiologia.PublishedbyElsevierEditoraLtda.ThisisanopenaccessarticleundertheCC BY-NC-NDlicense(http://creativecommons.org/licenses/by-nc-nd/4.0/).
Eichhorniaazurea(Sw.)Kunthisamajormacrophytein con-strained,floodedenvironments.Itisafloatingfixingspecies, perennial and rhizomatous.7,8 It is distributed in natural
and artificial reservoirsfrom south ofthe UnitedStates to ArgentinaandinalloftheregionsandecosystemsofBrazil.9
It serves as food for capybaras, pigs and other herbivores andasahabitatformanyfish,insectlarvae,snailsandtheir eggs,etc.10Aquaticmacrophytesreachhighbiomassvalues,
makingthemanimportantsourceoforganicmaterialtobe decomposed.11 Severalstudieshavehypothesizedaboutthe
relationship of this macrophyte with others species, such asephemeropteras,12fishes,13–17insects10,18,19andthe
endo-phyticfungalcommunity.20
Plant material decomposition releases much dissolved organicmatter intoaquaticenvironments. Thisproducesa quantityofdebriscapableofregulatingthenutrientflowinthe ecosystembothspatiallyandtemporally.21Thereisastrong
linkbetweenprimaryproduction,decompositionandnutrient cycling.22Thus,thecompoundsreleasedduringtheaquatic
macrophytedecompositioncanberesponsibleformostofthe energyflowinaquaticecosystems.23Onewaytomonitorthe
masslossovertimeisbycalculatingthedecompositionrate.It affectsthenutrientrelease,theaccumulationofdecomposing materialinthesedimentandthequalityofthedetritus,22and
itisusuallyexpressedbytheweightlossinacertainperiodof time.
Themetabolicactivityofheterotrophicbacteriahas impor-tantimplications forthe functionofaquaticecosystems.24
Bacteria and fungi are essential for organic matter decomposition.25 They useavarietyoforganiccompounds
underdifferentenvironmentalconditions,extractingenergy from these compounds by fermentation and aerobic and anaerobic respiration.26 They convert large amounts of
matterinto inorganicnutrients.Thefactors that affectthe compositionofthebacterialcommunityanditsactivityhave beenthebasisformanystudiesinrecentyears.1,2,27–29 With
no evaluation of the mechanisms that regulate microbial foodwebsandgiventheareacoveredbyaquaticecosystems, thefunctioningofaquaticecosystemshasbeenonlypartly described.30
Thisstudyinvestigatedtheexistenceoftemporal fluctu-ations oflimnological parameters during E. azurea decom-position that simulates the flood pulse because in this period, there is an organic matter input from aquatic macrophytes.
Materials
and
methods
Collectionandassemblyoftheexperiment
SamplesofwaterandE.azurealeavesweregatheredinthe RessacoLeopoldo(22◦4524S,53◦167W),locatedinPuerto Rico,intheFloodPlainoftheAltoParanáRiver.
The species E. azurea was chosen because it is more common in areas subjected to flooding and because it has high biomass levels.11 In addition, many
decomposi-tion studieshave beenperformed withthis macrophyte in floodplains.30,31
Inthelaboratory,thewatercollectedwaskeptunder aera-tionuntiltheexperimentalassembly.Themacrophyteswere driedin anovenfor sevendaysinorder toobtain the dry weight.
Fortheexperimentalassembly,51bottlesofpolyethylene wereused(500mL).Anaerationsystemwasusedineach indi-vidual container.Theexperiment occurred in aninsulated environment inorder tomaintain astabletemperature. In theexperiment,450mLofwaterand0.8gofmacrophytedry weightwereaddedtothebottles.
Themasswasbasedonthevaluesofmacrophytebiomass obtained in the environments of the Upper Paraná River Floodplain30andsimulatedthedecompositioneventsduring
thefloodpulse.
TheincreaseinE.azureabiomasscansimulatethenutrient inputeffectcharacteristicofthefloodpulseprocess.Inthis process,alargebiomassconcentrationdecomposes,leading toanincreaseinnutrientcyclingandaffectingthemicrobial loop.32
Acontrolwasalsoperformed,inwhichthesamevolume ofwaterwasaddedwithouttheadditionofthemacrophyte dryweight.Samplesweretakenat0(experimentinitiation), 3h,6h,12h,24h, 72h,120h,168hand240h.These samp-ling times represent the leachingperiod oforganic matter decomposition.Ateachtimepoint,threecontainersfromeach treatment were randomlyremoved,and theplantmaterial containedwithinwassenttotheovenfordrying.After48h, thematerialwasweighedtoobtainthefinaldryweight. Fur-thermore,5mLofwaterwasseparatedforthebacteriological analysis. The remainingvolume was used inphysical and chemicalanalyses.
Bacterialdensityandbiomass
Thedensityandbacterialbiomasswereestimatedbyfiltering 0.1mL of water from the experiment. Black polycarbo-nate filters (Nucleopore®) with pore openings of 0.2m,
stainedwith1mLofthefluorochromeDAPI (4,6-diamidino-2-phenylindole),wereusedfor5mininthedark.Thefilterswere mountedonslidesand storedinthefreezer. Bacteriawere quantifiedusinganepifluorescencemicroscope(1000×).The biovolumewasdeterminedusingtheequationproposedby Fry(1990):v=(p/4)·w2(l×w/3),wherev=cellvolume,l=length,
w=width.Fortheconversionofbiovolumetobiomass,itwas consideredthat1m3=3.5×10−13gC.13
Abioticanalysis
Thedissolvedoxygen(mgL−1)levelsandthewater tempera-tureweredetermineddirectlyinthebottlesusingaportable digitaloxymeter(YSI-550A).Theelectricalconductivity and pH values were determined using portable digital poten-tiometers.Analiquot of50mLwasusedfortotaldissolved organic carbon(DOC)determination,whichwascarriedout by catalyticoxidation ata high temperature (720◦C) using theShimadzuTOCanalyzerV-CSN.Theremainingwaterwas filteredthroughafiberglassfilter(Whatman®GF/C)to
deter-minethesolublephosphorus(P-PO43−),ammonia(NH4+),and
0 3 6 12 24 48 72 96 120 144 168 192 216 240 Time (h) 0.54 0.56 0.58 0.60 0.62 0.64 0.66 0.68 0.70 0.72 0.74 0.76 0.78 0.80 0.82 Dry weight (g)
Fig.1–DryweightlossofE.azureaduringdecompositionprocess.
Decompositionrate
Formacrophytedecompositionratedetermination,the neg-ativeexponentialmodel“Wt=W0e−kt”wasused,whereWtis
theremnantweightfractionofthevegetationattime“t”,W0
istheinitialweightandkisthedecompositionrate(day−1). Thismodelassumesthataconstantfractionoftheremaining masskdecaysineachtimeunit.37
Statisticalanalysis
TheANCOVAcovariancetestwasconductedtodeterminethe existenceofsignificantdifferencesbetweentreatments.The timeparameterwasusedasacovariate.
ThedatawerecorrelatedusingthePearson’slinear corre-lationcoefficient(r)toidentifywhichlimnologicalvariables wereassociatedwithbacterialdensityandbiomass.
Aregressionanalysiswasperformedtoevaluatethemain variablesofthebacterialcommunityandtheirpowerto pre-dictthe dependentvariable.Theregression wasperformed including all significant factors in the Pearson correlation (independentvariables)andexcludingnon-significantfactors (p>0.05), looking for the simplest model by which to pro-ducethemostrepresentativeparameters(backwardstepwise method).Theassumptionsoftheseanalyseswereverifiedby residuesanalysis.
Allstatisticalanalyseswereperformedusingthestatistical package“Statistica”version5.5.38Thesignificancelevelwas
setatp<0.05.
Results
E.azureadecompositionrate
The reduction inthe dry weight was the mostprominent duringthefirst6h(12.75%).Afterthis time,thedryweight graduallydiminished,withtheexceptionofT5days,whenan increasewasobtainedrelativetotheearlierandlatertimes. AtT8,whichrepresentstendaysofdecomposition,therewas adecreaseof22.38%indryweight(Fig.1).Thedecomposition exponentialrate(k)ofthemacrophyteE.azureawas0.0025d−1. According to the results, it can be presumed that the decomposition rate is inversely proportional to time, thus showingthatthe decompositionisgreatestinthefirst few hoursandslowsinthefollowinghours.
Abioticanalyzes
Theabioticparameters(Table1)differedbetweenthe treat-mentandcontrolgroups.
Theparametersanalyzedwere pH, conductivity(Cond.), dissolvedoxygen(DO),watertemperature(TH2O),ammonia
(NH4),solublephosphorus(P-PO43−),TPandDOC.
Table1–Limnologicaldataforcontrolandtreatmentduringexperimentsamplingtime(T=treatment;C=control;DOin mgL−1;conductivityinScm−1;NH4,P-PO43−,TPandDOCingL−1).
pH Cond. DO TH2O NH4 P-PO4 TP DOC
T C T C T C T C T C T C. T C T C T0–0h 7.2 7.24 72.5 72.5 6.74 6.93 22.4 22.4 48 48 13.5 13.5 24.77 24.7 3.86 3.86 T1–3h 6.88 7.28 214 70.73 4.9 6.69 25.1 25.7 32.9 49.58 351.7 9.64 440.4 33.6 8.76 4 T2–6h 6.9 7.18 216.6 67.83 4.45 6.32 27.1 27.8 53.8 34.29 575.9 10.6 657.7 49.4 11.3 4.33 T3–12h 6.54 7.17 215.6 72.4 2.98 3.86 28.9 29.4 26.9 28.31 471.5 12.5 596.8 36.2 18.7 5.76 T4–24h 6.23 7.28 222.5 69.13 0.59 4.51 28.6 28.8 30.0 16.88 47.34 9.64 710.1 44.7 23.4 5.2 T5–72h 6.57 7.15 233.6 72.8 1.48 4.31 24.93 25.5 78.8 16.36 344.5 4.72 661.4 45.6 14.0 5.46 T6–120h 6.64 7.29 218 74.2 1.71 4.12 27.86 27.6 55.3 19.26 235.6 5.2 623.9 59.6 33.9 5.16 T7–168h 6.76 7.24 249.5 77.96 2.61 4.18 26.6 26.4 42.4 8.97 415.4 3.78 695.2 75.8 25.9 5 T8–240h 7 7.36 308 76.6 2.42 4.25 27.6 27.3 55.3 21.89 453.2 6.4 845. 63.3 36.5 4.76
Table2–ANCOVAresultsfordifferencebetweencontrolandtreatment.
pH Cond. OD NH4 PO4 Ptotal COD
ANCOVA results
F=51.50,p<0.05 F=244.9,p<0.05 F=37.9,p<0.05 F=16.3,p<0.05 F=118.6,p<0.05 F=144.1,p<0.05 F=75.2,p<0.05
Table3–ANCOVAresultsfordifferencebetweentemporaldata.
pH Cond. OD NH4 PO4 Ptotal COD
ANCOVA results
F=0.657,p<0.05 F=62.42,p<0.05 F=52.71,p<0.05 F=3.04,p<0.05 F=3.43,p<0.05 F=7.71,p<0.05 F=24.10,p<0.05
Inalloftheabioticparametersstudied,therewere signif-icantdifferencesbetweenthecontrolandtreatmentgroups
(Table2).All parametersalsosignificantlyvariedwithtime
(Table3).
Effectofdecompositioninthelimnologicalparameters
ThedryweightofE.azureahadasignificantnegative corre-lationwithDOC(r=−0.73,p<0.0001),conductivity(r=−0.73,
p<0.0001) and P-PO43− (r=−0.70, p<0.0001) and a positive
correlation with DO (r=0.80, p<0.0001).This suggests that thedynamicsofthesefactorsarecloselyassociatedwiththe decompositionprocess.
Bacterialdensityandbiomass
The total bacterial density ranged from 4.76×107 to
9.31×107cellsmL−1 in the controlgroup. In the treatment
group,thehighestdensityreached2.95×108cellsmL−1atthe
endoftheexperiment(Fig.2).
Thedensityvariationinthecontrolgrouphadadynamic verysimilartothesigmoidcurve.Inthetreatmentgroupthere wasacontinuousincreaseindensity,exceptforadecrease thatoccurredwithin72h.Atthissampling time,therewas alsoadecreaseinDOC(14.0g/L).
TheANCOVAcovariancetestshowedasignificant differ-ence indensity betweenthe controland treatmentgroups (F=20.33p<0.05). 0 3 6 12 24 48 72 96 120 144 168 192 216 240 Time (h) –1E8 0 1E8 2E8 3E8 4E8 5E8 6E8
Bacterial density (cel/mL)
Control Treatment
Fig.2–Meanvaluesandstandarddeviationofdensityin controlandtreatment.
In the control group (Fig. 3A), the rod density started at 2.95×107cellsmL−1, reaching its highest value in 12h
(5.16×107cellsmL−1)andthendecreasinguntilreachingits
lowestdensity at240h(2.4×107cellsmL−1).Thecocci
den-sity was the highest at 120h (2.78×107cellsmL−1), and
then,itdecreasedat168h(2.7×107and1.61×107cellsmL−1,
respectively). Thevibriosdensity increasedwiththe samp-ling times, starting with 6.5×106cellsmL−1 and reaching
4.03×107cellsmL−1atthefinaltimepoint.Thespirillumwere
onlyobservedatthelastsamplingtimepoint,withalow den-sityof6×105cellsmL−1.
Inthetreatmentgroup(Fig.3B),thebacillusdensity,except fortime T7(8×107cellsmL−1), increasedwithtime,
reach-ingitshighestvalueatT8(1.26×108cellsmL−1).Thehighest
coccidensitywasobtainedat120h(4.66×107cellsmL−1),and
itslowestdensitywasat240h(6.83×106cellsmL−1).The
vib-rioshaditshighestdensityat240h(4.36×107cellsmL−1).The
spirillumwereonlyobservedatthelastfoursamplingtime points, with adensity ranging from 1.66×105cellsmL−1 at
120hto2.16×106cellsmL−1at240h.
Thebiomassvalueswerehigherinthetreatmentthanin thecontrolgroup(Fig.3A).Inthecontrolgroup,thebiomass attimeT0ofthe experimentwas0.11mgCL−1,reachingits maximumvalueof0.22mgCL−1at24and168h.Inthe treat-ment group, the biomass values were crescent, except at 72 and 168h (0.8 and 1.81mgCL−1, respectively), reaching 2.78mgCL−1bytheendoftheexperiment.
TheANOVAcovariancetestshowedasignificantdifference betweenthebiomassobtainedinthecontrolandtreatment groups(F=59.61,p<0.05).
Abioticandbioticparameters
The parametersDO, NH4+, P-PO43−, PT and DOC were
sig-nificantlyassociatedwiththebacterialdensityandbiomass duringtheexperimentalcontrolgroup.Inthetreatmentgroup, theparametersconductivity,PTandDOCweresignificantly associated with biomass and density, while DO was only associated withbiomass(Table 4). Both inthe control and inthetreatmentgroups,thestrongestassociationsbetween biomassanddensitywerewithDOC.
Multiple linear regression analyses were calculated to developapredictionmodelforbacterialdensityinthe con-trolgroup.TheanalysissuggestedthatDOandDOCcompose themodel(N=27,F(5,21)=152.23,p<0.0001),withanR2=0.97.
0.00E+00 1.00E+07 2.00E+07 3.00E+07 4.00E+07 5.00E+07 6.00E+07 7.00E+07 8.00E+07 9.00E+07 1.00E+08 1.10E+08 1.20E+08 1.30E+08 1.40E+08 T0 T1 T2 T3 T4 T5 T6 T7 T8 Density (cells mL –1 ) Sampling time Control 0.00E+00 1.00E+07 2.00E+07 3.00E+07 4.00E+07 5.00E+07 6.00E+07 7.00E+07 8.00E+07 9.00E+07 1.00E+08 1.10E+08 1.20E+08 1.30E+08 1.40E+08 T0 T1 T2 T3 T4 T5 T6 T7 T8 Density (cells mL –1) Sampling time Treatment
A
B
Bacillus Coccus Vibrio Spirilum
Fig.3–Densityvalueofeachbacterialmorphotypeobservedincontrol(A)andtreatment(B).
The model predictions are represented by the equation below:
Bacterialdensityincontrol=31829+6047DO+195937DOC ThebacterialdensityinthetreatmentgrouponlyhadDOC asasignificantparameterintheregressionanalysis(N=27,
F(1,25)=26.734,p<0.00002),withR2=0.93.Themodel
predic-tionsarerepresentedbytheequationbelow:
Bacterialbiomassincontrol=6545×104+5876433DOC Thebacterialbiomassinthecontrolgrouphad onlyDO andDOCassignificantparametersinthemultipleregression analysis(N=27,F(2,24)=138.94,p<0.000001),withR2=0.9204.
Themodelpredictionsarerepresentedbytheequationbelow:
Bacterialdensityintreatment=0.01348+0.002303DO +0.045362DOC
Thebacterial biomassin the treatmentgroup was only significant with COD in the analysis of multiple linear regression(N=27,F(1,25)=440.56,p<0.000001)withR2=0.9463.
The model predictions are represented by the equation below:
Bacterialbiomassintreatment=0.021822+0.079539DOC
Discussion
E.azureadecomposition
Dissolved and particulate organic detritus decomposition influencestheenergyandmaterialflowsinlakeecosystems.23
Thegradualbiomasslosswasmostintenseinthe early timepointsandslowedovertime.Thebiomasslossdynamics areassociatedwithwater-solublecompoundrelease,which is most intensein the early hours.39 The weight loss and
changesinthechemicalcompositionoftheE.azureadebrisare affectedbythesechemicalcharacteristicsatthebeginningof thedecompositionprocessandbywhere,geographically,the processoccurs.30
The k value for this study was 0.023d−1. The average decomposition coefficient of E. azurea leaves proposed by PetersenandCumminswas0.0033d−1.40Thiscoefficientwas
classifiedas“slow”bythesameauthors.Inthedecomposition studyofE.azureaperformedbyPadialandThomaz,30thekfor
sevendayswas0.010d−1.Thesevaluesshowthatthereis vari-ationinthedecompositionrate,evenwithinthesamespecies. Thisvariationisinfluencedbythechemicalandphysical con-ditionsoftheenvironments,themicrobialdiversity,andthe chemicalcompositionofthedebris.22,30Studiesinareas
sub-jecttofloodinghaveshownthatthedecompositionrateisalso affectedbythetypeofenvironment(loticorlentic)andwater quality.30
Table4–ResultsofPearson’scorrelationtestbetweenbacterialdensityandbiomasswithlimnologicalparametersin controlandtreatment.
Density Biomass
Control Treatment Control Treatment
pH p=0.77;r=0.586 p=0.9633;r=0.009 p=0.8512;r=0.037 p=0.076;r=−0.1316 Cond. p=0.09;r=0.3294 p=0.0212;r=−0.441 p=0.067;r=−0.356 p=0.048;r=0.3832 DO p<0.0001;r=0.88 p=0.067;r=−0.3565 p<0.0001;r=−0.91 p=0.0019;r=−0.568 NH4+ p=0.0005;r=−0.624 p=0.8214;r=−0.64 p=0.0003;r=−0.64 p=0.3242;r=0.1972 PPO43− p=0.034;r=−0.407 p=0.2706;r=0.216 p=0009;r=−0.492 p=0.5357;r=0.1246 TP p=0.044;r=0.3894 p=0.014;r=0.4654 p=0.014;r=0.463 p=0.0112;r=0.4803 DOC p<0.0001;r=0.957 p<0.0001;r=0.8231 p<0.0001;r=0.9024 p<0.0001;r=0.9728
Thedecomposition process still influences the physical andchemicalcharacteristics ofwater.30Thismostlyoccurs
intropicalregions,wheretheriversystemfloodplainsshow markedtemporal variationinphysical,chemicaland biotic factors. Such variations are, mainly, related to changes in hydrometriclevels,whichhavebeenattributedtothe‘flood pulses’theory.41Thedryweightlossinthisstudywas
corre-latedwithDOCandPT.AccordingtoSridharandBarlocher,42
high nutrient concentrations are correlated with increased submerged biomass decay rates. One of the factors that influences the degradation of this material is its nutrient concentration.43Thereisapositiverelationshipbetweenthe
decompositionrateofplantsandthephosphorus concentra-tionoftheirtissues.Total phosphorusisthebest indicator ofthenutrientcontentinanyecosystem.Thismayexplain thesignificantcorrelationbetweenphosphorusandthedry weightofE.azurea.44
Bacterialdensityandbiomass
Themicroorganisms found in anaquatic environment are determined by the physical and chemical conditions that prevailinthatenvironment.45Theyqualitativelyand
quanti-tativelyvaryforlongperiodsoronashorttimescale.46Thus,
temporalvariationsaffectthepopulationecologyandmodify thestructureandfunctionofthemicrobialcommunities.29
Generally, the bacteria density ranges between 105 and
108cellsmL−1andcanincreasewiththeenvironmenttrophic
status.47 Inthis study,the bacterialdensitywas 107 inthe
controlgroup,reaching108 inthetreatmentgroup.Teixeira
et al.,48 working in similar environments, found
bacteri-oplankton densitiesvarying between 1.3±0.7×109cellsL−1
and22.0±4.7×109cellsL−1.Theincreaseofdensitywiththe
E.azureabiomasscansimulatetheeffectofthetypical nutri-tional contribution of the flood pulse process when large amountsofbiomassdecompose,causinganincreasein nutri-entcycling.Inourexperiment,weobservedanincreaseinthe densityandbacterialbiomassduringthedecomposition pro-cess.StudiesperformedintheParanaRiverdeterminedthe bacterialabundanceandproductionratesinthe lowwater period,butthedifferenceswerenotsignificantinthestudies intheParanaRiver, whilethebacterialabundancewas sig-nificantly higherduringtheflood.32 Previousstudies found
greaterbacterialabundancesandproductionratesinthelow waterperiod,butthedifferenceswerenotsignificant.20,49
Gene expression can provide valuable information regarding both structural and functional bacterial popu-lationsinaquaticecosystems.50,51Ingeneral,smallbacteria
(cocci) inhabit waters with low nutrient concentrations. Larger bacteria (bacillus, vibrios and spirillum) are more commoninenrichedenvironmentswithorganicmatter.52,53
Thus,thebacterialpopulationcompositionmaybemodified accordingtothetrophiclevel.54
Thecoccus density wasincreasedduring thetreatment until T6, decreasing thereafter. Concomitantly, the density ofthevibriosandspirilosincreasedafterT6.Becausethese bacteria have a spherical cell shape, environments with a greateravailabilityofresourcesfacilitatethemetabolic activ-ity ofthese organisms with regard to both the amount of nutrientsavailableintheenvironmentandtheabilitytodrive
nutrientsintothecells.55However,factorssuchas
competi-tionmaylimitresources,thuscontrollingorganismdensity.
Abioticfactorsandbacterialbiomassdensity
Bacterioplankton growth is dependent on the availability of inorganicnutrients. Thechange inthe concentrationof nutrients can have direct and indirect effects on bacterial growth.56,57Theelectricalconductivitywassignificantly
cor-related withthe density and bacterialbiomassonlyin the treatmentgroup.AccordingtoEsteves,44conductivityvalues
arerelatedtothetrophicstateofthewater.Thus,increased nutrientconcentrationsfromthedecompositionand subse-quentreleaseofionsaffectedtheconductivity.
In this experiment, there was a negative correlation betweenbiomassandDOinthecontrolandtreatmentgroups. Thisindicatesthemicroorganisms’actioninorganicmatter decompositionandtheformationofanoxiczones.
TheP-PO43− was positivelycorrelated with thebiomass
andbacterialdensityonlyinthecontrolgroup.Inother stud-ies,this correlationhasalsobeenfound.58 Thisresultmay
representabottom-upcontrolofthebacterialcommunity20,59
because phosphorus is an essential nutrient for bacterial growthandisoftenlimitedintheenvironment.60Thisconcept
ismostevidentbythefactthatthiscorrelationoccurredonly inthecontrolgroup,wheretheP-PO43−decreasedwithtime,
suggestingitsassimilationbythebacterialcommunity. There-fore,inthetreatmentgroup,wherenutrientsweresupplied fromE.azureadecomposition,theP-PO43−wasnotalimiting
factorofbacterialgrowth.
Usingmultiplelinearregressionanalysis,weverifiedthat the DO and DOC are the major variables that explained bacterial dynamics. The DOC strongly affects the bacterial dynamics,astheheterotrophicplanktonicbacteriaare asso-ciatedwiththecarbonmetabolisminapelagicenvironment.1
Agreatpartofthedissolvedorganicmattercanbeconsumed bytheseorganisms.47,61AstheDOCisgenerallyregardedasa
growthlimitingfactorofbacterioplankton,62,63astrong
asso-ciationbetweenbacterioplanktonandDOClikelyoccurs. Despiteitsecologicalimportance,knowledgeregardingthe diversityofaquaticenvironmentsandthefactorsthat con-trolthefreshwaterbacterioplanktoncompositionisfarfrom complete.49
Conflicts
of
interest
Theauthorhasnoconflictsofinteresttodeclare.
Acknowledgements
We thank Maria do Carmo Roberto (Maringá State Uni-versity) for field assistance and nutrients analysis, CAPES (Coordenac¸ãodeAperfeic¸oamentodePessoaldeNível Supe-rior)scholarshipsandCNPq(BrazilianCouncilofResearch). This study was alsosupportedby the “Long-Term Ecologi-cal Research”(LTER)programofCNPq(BrazilianCouncilof Research).
r
e
f
e
r
e
n
c
e
s
1.GurungTB,UrabeJ,NozakiK,YoshimizuC,NakanishiM.
BacterioplanktonproductioninawatercolumnofLake
Biwa.LakesReserv:ResManag.2002;7:317–323.
2.KirschnerAKT,VelimirovB.Aseasonalstudyofbacterial
communitysuccessioninabackwatersystem,indicatedby
variationinmorphotypenumbers,biomassandsecondary
production.MicrobEcol.1997;34:27–38.
3.SparksDL.EnvironmentalSoilChemistry.SanDiego:Academic
Press;1995.
4.BiniLM,ThomazSM,SouzaDC.Speciesrichnessand
b-diversityofaquaticmacrophytesinUpperParanáRiver
floodplain.ArchHydrobiolStuttg.2001;151(3):511–525.
5.PetrucioMM,EstevesFA.Uptakeofnitrogenand
phosphorousinthewaterbyEichhorniacrassipesandSalvinia
auriculata.RevBrasBiol.2000;60(2):229–236.
6.PompeoMLM,HenryR,Moschini-CarlosV.Chemical
compositionoftropicalmacrophyteEchinochloapolystachya
(HBK)HitchcockinJurumirimReservoir(SaoPaulo,Brazil).
Hydrobiologia.1999;411:1–11.
7.Scremin-DiasE,PottVJ,SouzaPR,HoraRC.NosJardins
SubmersosdaBodoquena:GuiaparaIdentificac¸ãodasPlantas AquáticasdeBonitoeRegiãoBonito/MS.CampoGrande;1999.
8.ThomazSM,BiniLM.EcologiaeManejodeMacrófitas
Aquáticas.5thed.Maringá:EDUEM;2003.
9.AmaralMCE.PontederiaceaeinListadeEspéciesdaFlorado Brasil.JardimBotânicodoRiodeJaneiro;2014.Available from:http://reflora.jbrj.gov.br/jabot/floradobrasil/FB13741
[accessed14.07.14].
10.PottVJ,PottA.PlantasaquáticasdoPantanal.Corumbá:
Embrapa;2001.
11.BiniLM,Influênciadopulsodeinundac¸ãonosvaloresde
fitomassadetrêsespéciesdemacrófitasaquáticasna
planíciedeinundac¸ãodoaltorio,Paraná.ArqBiolTecnol.
1996;39(3):715–721.
12.Dos-SantosI,WittmannD.Legitimatepollinationofthe
tristylousflowersofEichhorniaazurea(Pontederiaceae)by
Ancyloscelisgigasbees(Anthophoridae,Apoidea).PlantSyst
Evol.2000;223:127–137.
13.BjornsenPK.Automaticdeterminationofbacterioplankton
biomassbyimageanalysis.ApplEnvironMicrobiol.
1986;51:1199–1204.
14.FranceschiniMC,CapelloS,LhanoMG,AdisJ,WysieckiML.
MorfometriadelosestádiosninfalesdeCornopsaquaticum
BRUNER(1906)(Acrididae:Leptysminae)enArgentina.
Amazoniana.2005;18:373–386.
15.LopesTM,CunhaED,SilvaJCB,BehrendRDL,GomesLC.
Densemacrophytesinfluencethehorizontaldistributionof
fishinfloodplainlakes.EnvironBiolFish.2015;98:1741–1755.
16.PadialJM,Castroviejo-FisherS,KohlerJ,VilaC,ChaparroJC,
DelaRivaI.Decipheringtheproductsofevolutionatthe
specieslevel:theneedforanintegrativetaxonomy.ZoolScr.
2009;38(4):431–447.
17.SilvaFR,PradoVHM,Rossa-FeresDC.Amphibia,Anura,
Hylidae,Dendropsophusmelanargyreus:distributionextension,
newstaterecordandgeographicdistributionmap.CheckList.
2010;6(3):402–404.
18.FulanJA,HenryR.TheOdonata(Insecta)assemblageon
Eichhorniaazurea(Sw.)Kunth(Pontederiaceae)standsin
CamargoLake,alaterallakeontheParanapanemaRiver
(StateofSãoPaulo,Brazil),afteranextremeinundation
episode.ActaLimnolBrasiliensia.2006;18(4):423–431.
19.Urso-GuimarãesMV,Peláez-RodríguezMP,Trivinho-Strixino
S.NewspeciesofLopesia(Diptera,Cecidomyiidae)
associatedwithEichhorniaazurea(Pontederiaceae)from
Brazil.IheringiaSérieZool.2014;104(4):478–483.
20.FarjallaVF,FariaBM,EstevesFA,BozelliRL.Bacterialdensity
andbiomass,andrelationswithabioticfactorsin14coastal
lagoonsofRiodeJaneirostate.OecolBrasil.2001;9:65–76.
21.KimJG,RejmankovaE.Decompositionofmacrophytesand
dynamicsofenzymeactivitiesinsubalpinemarshesinLake
Tahoebasin,USA.PlantSoil.2004;266:303–313.
22.BianchiniIJr,Cunha-SantinoMB,PeretAM.Oxygendemand
duringmineralizationofaquaticmacrophytesfroman
oxbowlake.BrazJBiol.2008;68(1):61–67.
23.WetzelRG.Death,detritusandenergyflowinaquatic
ecosystems.FreshwBiol.1995;33:83–89.
24.LennonJT,PfaffLE.Thesourceandsupplyofterrestrial
carbonaffectsaquaticmicrobialmetabolism.AquatMicrob
Ecol.2005;39:107–119.
25.RavenPH,EvertRF,CurtisH.BiologyofPlants.2nded.New
York:WorthPublisher;1976.
26.MadiganMT,MartinkoJM,ParkerJ.BrockBiologyof
Microorganisms.NewJersey:Prentice-Hall;2000.
27.EilerA,BertilssonS.Compositionoffreshwaterbacterial
communitiesassociatedwithcyanobacterialbloomsinfour
Swedishlakes.EnvironMicrobiol.2004;6:1228–1243.
28.LindstromES,BergstromAK.Communitycompositionof
bacterioplanktonandcelltransportinlakesintwodifferent
drainageareas.AquatSci.2005;67:210–219.
29.LiuJ,LeffLG.Temporalchangesinthebacterioplanktonofa
northeastOhio(USA)river.Hydrobiologia.2002;489:151–159.
30.PagioroTA,ThomazSM.Influenceofthedecompositionof
Eichhorniaazureaonselectedabioticlimnologicalvariablesof
differentenvironmentsofthefloodplainoftheHighParaná
River.ActaLimnolBrasiliensia.1999;11(2):157–171.
31.AzevedoJCR,NozakiJ.Análisedefluorescênciade
substânciashúmicasextraídasdaágua,soloesedimentoda
LagoadosPatos-MS.QuímNova.2008;31(9):1324–1329.
32.CarvalhoP,ThomazSM,BiniLM.Effectsofwaterlevel,
abioticandbioticfactorsonbacterioplanktonabundancein
lagoonsofatropicalfloodplain(ParanaRiver,Brazil).
Hydrobiologia.2003;510:67–74.
33.BergaminH,ReisBF,ZagattoEAG.Anewdevicefor
improvingsensitivityandstabilizationinflowinjection
analysis.AnalChimActa.1978;97:427–431.
34.GinéMF,BergaminFH,ZagattoEAG,ReisBF.Simultaneous
determinationofnitrateandnitritebyflowinjection
analysis.AnalChimActa.1980;114:191–197.
35.GoltermanHL,ClymoRS,OhmstadMAM.MethodsforPhysical
andChemicalAnalysisofFreshWater.Oxford:Blackwell
Scientific;1978.
36.MackerethFYH,HeronJ,TallingJJ.WaterAnalysis:Some
RevisedMethodsforLimnologists.Ambleside:Freshwater
BiologicalAssociation;1978.
37.VillarCA,CaboL,VaithiyanathanP,BonettoC.Litter
decompositionofemergentmacrophytesinafloodplain
marshoftheLowerParanáRiver.AquatBot.2001;70:105–116.
38.StatsoftInC.Statistica(DataAnalysisSoftwareSystem).Version 5.5;2005.Availablefrom:www.statsoft.com.
39.MoorheadG,DouglasP,MorriceN,ScarabeLM,AitkenA,
MackintoshC.Phosphorylatednitratereductasefrom
spinachleavesisinhibitedby14-3-3proteinsandactivated
byfusicoccin.CurrBiol.1996;6:1104–1113.
40.PetersenRC,CumminsKW.Leafprocessinginawoodland
stream.FreshwBiol.1974;1974:343–368.
41.JunkWJ,BayleyPB,SparksRE.Thefloodpulseconceptin
river–floodplainsystems.CanJFishAquat.1989;106:
110–127.
42.SridharKR,BärlocherF.Initialcolonization,nutrientsupply,
andfungalactivityonleavesdecayinginstreams.Appl
EnvironMicrobiol.2000;66:1112–1119.
43.EnríquezSCMD,Sand-JensenK.Patternsisdecomposition
ratesamongphotosyntheticorganism:theimportanceof
44.EstevesFA.FundamentosdaLimnologia.RiodeJaneiro:
Interciência/FINEP,RiodeJaneiro;1988.
45.TortoraGJ,FunkeBR,CaseCL.Microbiology:AnIntroduction.
NewYork:Hardcover;2008.
46.Regali-SeleghimMH,GodinhoMJL.Peritrichepibiont
protozoansinthezooplanktonofasubtropicalshallow
aquaticecosystem(MonjolinhoReservoir,SaoCarlos,Brazil).
JPlanktonRes.2004;26(5):501–508.
47.BouvyM,Barros-FrancaLM,CarmouzeJP.Compartimento
microbianonomeiopelágicodeseteac¸udesdoestadode
Pernambuco.ActaLimnolBras.1998;10(1):93–101.
48.TeixeiraMC,SantanaNF,AzevedoJCR,PagioroTA.
Bacterioplanktonfeaturesanditsrelationswithdoc
characteristicsandotherlimnologicalvariablesinParaná
riverfloodplainenvironments(PR/MS-Brazil).BrazJMicrobiol.
2011;42(3):897–908.
49.WuQL,ZwartG,WuMJP,MartinW.Submersedmacrophytes
playakeyroleinstructuringbacterioplanktoncommunity
compositioninthelarge,shallow,subtropicalTaihuLake,
China.EnvironMicrobiol.2007;9(11):2765–2774.
50.LaFerlaR,LoGiudiceA,MaimoneG.MorphologyandLPS
contentfortheestimationofmarinebacterioplankton
biomassintheIonianSea.SciMarin.2004;68(1):
23–31.
51.SteinbergCEW.EcologyofHumicSubstancesinFreshwaters–
FromWhole-LakeGeochemistrytoEcologicalNicheDetermination.
Berlin:Springer;2003.
52.FuhrmanJA,AzamF.Bacterioplanktonsecondary
productionestimatesforcoastalwatersofBritishColumbia,
AntarcticaandCalifornia.ApplEnvironMicrobiol.1980;39:
1085–1095.
53.UnanueM,AzúaI,ArrietaJM,Labirua-IturburuA,EgeaL,
IriberriJ.Bacterialcolonizationandectoenzymaticactivityin
phytoplankton-derivedmodelparticles:cleavageofpeptides
anduptakeofaminoacids.MicrobEcol.1998;35:136–146.
54.DucklowHW,CarlsonCA.Oceanicbacterialproduction.In:
MarshallKC,ed.AdvancesinMicrobialEcology.NewYork:
PlenumPress;1992.
55.YoungKD.Theselectivevalueofbacterialshape.Microbiol
MolBiolRev.2006;70(3):660–703.
56.PinhassiJ,BowmanJP,NedashkovskayaOI,LekunberriI,
Gómez-ConsarnauL,Pedrós-AlióC.Leeuwenhoekiella
blandensissp.nov.,agenome-sequencedmarinememberof
thefamilyFlavobacteriaceae.IntJSystEvolMicrobiol.
2006;56:1489–1493.
57.ScolfieldV,JacquesSMS,GuiamarãesJRD,FarjallaVF.
Potentialchangesinbacterialmetaboliseassociatedwith
increasedwatertemperatureandnutrientinputsintropical
humiclagoons.FrontMicrobiol.2015;6:310.
58.AnesioAM,HollasC,GraneliW,Laybourn-ParryJ.Influence
ofhumicsubstancesonbacterialandviraldynamicsin
freshwaters.ApplEnvironMicrobiol.2003;70:4848–4854.
59.TzarasA,PickFR.Therelationsbetweenbacterialand
heterotrophicflagellateabundanceinoligotrophicto
mesotrophictemperatelakes.MarMicrobFoodWebs.
1994;8:347–355.
60.BrookesPC,PowlsonDS,JenkinsonDS.Measurementof
microbialbiomassphosphorusinsoil.SoilBiolBiochem.
1982;14(4):319–329.
61.PaverSF,NelsonCE,KentAD.Temporalsuccessionof
putativeglycolate-utilizingbacterioplanktontrackschanges
indissolvedorganicmatterinahigh-elevationlake.FEMS
MicrobiolEcol.2013;83:541–551.
62.KirchmanDL.Theuptakeofinorganicnutrientsby
heterotrophicbacteria.MicrobEcol.1994;28:255–271.
63.SinistroR,SanchezML,UnreinF,SchiaffinoMR,IzaguirreI,
AllendeL.Responsesofphytoplanktonandrelatedmicrobial
communitiestochangesinthelimnologicalconditionsof
shallowlakes:ashort-termcross-transplantexperiment.