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AchievementsintheLifeSciences8(2014)55–60 ContentslistsavailableatScienceDirect Achievements in the Life Sciences journal homepage: www.elsevier.com/locate/als The Role of the Biogeochemical Conditions of the Marine Environment on the Trace Element Content in Pacific Salmon NadezhdaК.Khristoforovaa,b,VasiliyYu.Tsygankova,⁎, MargaritaD.Boyarovaa,OlgaN.Lukyanovaa,c aFarEasternFederalUniversity,8SukhanovaStreet,Vladivostok690990,RussianFederation bPacificGeographicalInstituteFEBRAS,7RadioStreet,Vladivostok690041,RussianFederation cPacificResearchFisheriesCentre(TINRO-Centre),4ShevchenkoLane,Vladivostok690950,RussianFederation a r t i c l e i n f o a b s t r a c t Availableonline7August2014 Thelevelsofsixchemicalelements(mercury,arsenic,lead,cadmium,zincandcopper)were examinedintwospeciesofPacificsalmon,genusOncorhynchus,pinksalmon(O.gorbuscha), Keywords: andchumsalmon(O.keta)thatwerecaughtintheKurilwatersinJuly2013.Concentrationsof Mercury toxicelements(Hg,As,Pb,Cd)inbothspecieswereshowntobebelowthemaximumconcentra- Arsenic tionlimitsofthesetraceelementsforseafood.Theconcentrationsoftheseelementswerecom- Lead paredbetweenwildsalmonandhatcherysalmonofthePacificandAtlanticoceans. Cadmium ©2014PublishedbyElsevierB.V.onbehalfofFarEasternFederalUniversity. Zinc Copper Pinksalmon Chumsalmon Kurilwaters Introduction Despite the apparent uniformity and homogeneity of the water masses in the sea, there are areas similar to terrestrial biogeochemicalprovinces.Abnormalitiesordeviationsfromthebackgroundintheenvironmentandbiotastipulatedbythe geochemicalfeaturesofthesezonesarenotaspronouncedasinthesea.Theyappearnotonlyintheexistenceofendemicdiseases causedbychangesinthemineralmetabolismofterrestrialorganismsbutalsoindistinctivebiocenosesandmineralcompositions oforganisms.Inthesea,thedifferencebetweentheconcentrationsofelementsinabiogeochemicalprovinceandbeyonditmay notbeassharpasonlandbecauseofthenatureoftheenvironment. Theimpactzonesofanthropogenicorigin,establishedincoastalareas,arewellknown.Theyarecausedbytechnogenicpollution, whichcreatesanabnormalconcentrationofanumberofelementsandcompounds. Theimpactzonesofnatural-anthropogenicoriginareestuarineriverzones,whichreflectthenatureofthedrainedsoilsandthe characterofpollutedwastewaterinthesolidandliquideffluenttothesea. ⁎ Correspondingauthor. E-mailaddress:[email protected](V.YuTsygankov). PeerreviewunderresponsibilityofFarEasternFederalUniversity. http://dx.doi.org/10.1016/j.als.2014.06.009 2078-1520/©2014PublishedbyElsevierB.V.onbehalfofFarEasternFederalUniversity. 56 N.КKhristoforovaetal./AchievementsintheLifeSciences8(2014)55–60 Naturalimpactzonesoftheseas,whichhavepeculiarbiogeochemicalprovincesstipulatedbytheseepageofhighlymineralized underseabrinesandareinfluencedbydeepandshallowstreamsofvolcanicproducts,areunderstudied.Onlyupwellings,ashighly productiveareasoftheocean,havelongattractedscientificstudy.Theremainingzoneswithpeculiarbiocenoseshavebeenstudied forthreeorfourdecades.However,althoughthestudyandselectionofbiogeochemicalprovincesonlandhasalongerhistory,it beganrelativelyrecently,inthe1930s,byV.I.VernadskyandA.P.Vinogradov. ThewatersoftheKurilIslandsandtheKamchatkacoastalwatersareareaswheretheeffectofupwellingandvolcanismisclearly manifested.However,althoughthehighproductivityoftheSeaofOkhotskandtheKuril–Kamchatkaregionanditscausesarethe subjectofthedetailedscrutinyofhydrobiologists,hydrochemists,andfisheryscience,thechemicalcompositionoforganismsand thefactorsthatdeterminethecontentofmicro-elementsinorganismsaremuchlessstudied.Duringthe1980–1990s,inhabitants oftheintertidalandsubtidalzonesofKamchatkaandKurilIslands,primarilyindicatororganisms,suchasclamsandbrownmytilids fucusalgae,interestinglyshowedenrichmentbyheavymetals—cadmium,zinc,nickelandotherelements.Thoughthesebenthic organismscharacterizedthechemicalandenvironmentalconditionsoftheirhabitat,theydidnotgiveanideaofthemoreopen watersoftheregioninhabitedbynektonorganisms.Themostrepresentativeorganismsarepelagicfish,andamongthem,the mostimportantspeciesfromaneconomicpointofviewarethesalmons. SalmonarelargepelagicfishthatliveprimarilyinthenorthernpartsofthePacificandAtlanticoceans,theArcticOceanandinthe basinsofrivers.Thetwomostrepresentativeandabundantgroupscanbedistinguishedamongthefishofthesalmonfamily (Salmonidae):AtlanticsalmonandPacificsalmon.ThemostdistributedrepresentativeofAtlanticsalmonisSalmosalar.Theleading genusofPacificsalmonisOncorhynchus,whichincludespinksalmonO.gorbuscha,chumsalmonO.keta,sockeyeO.nerka,coho O.kisutch,ChinooksalmonO.tshawytscha(kingsalmon),andSimO.masou.ThereareseveralspeciesofthegenusSalmointhePacific, buttheyarefewerinnumbercomparedwiththePacificsalmongenusOncorhynchus. AtlanticsalmoncanbefoundonbothsidesoftheAtlanticocean,butitsnumbershavedroppeddrastically.Bytheendofthe twentiethandbeginningofthetwenty-firstcenturies,wildAtlanticsalmonbecametheobjectofscientificresearchandsportfishing. Currently,morethan99%ofAtlanticsalmonliveinfishponds.LeadersintheproductionofhatcherysalmonareNorway(520–550 thousandtonnesofAtlanticsalmonandtrout)andChile(approximately450thousandtonnesofAtlanticsalmonandtrout) (Worldreview…,2012).Atthesametime,50%ofPacificsalmonreproduceonnaturalspawninggrounds,whileaquarterofthelive- stockpopulationspawnsinKamchatka.However,evenifPacificsalmonarereproducedinfishponds,aftertheirrelease,theyfeedin theopenseaandoceanwaters—inotherwords,theyleadapascuallifestyle. Asinhabitantsoftheepipelagiczone(0–200m),salmondwellmainlyintheupperlayer(0–50m).ThepascualareaofPacific salmoninwintertimeislocatedbetween40and45°NintheSubarcticorArcticfront,markedbyhighbiologicalandfishery productivity.Withthecomingofspring,thewarmingoftheupperlayersofwaterandabundantplanktondevelopmentthezone ofactivelifeshiftstowardstheNorthandNortheast.Salmonfollowitwithoutleavingtheeutrophicarea,whichisthereasonfor theirrapidgrowth.MasusalmonistheonlytypeofPacificsalmonfoundonlyontheAsianshore,mainlyintheSeaofJapan.Chum andpinksalmonprevailonbothsidesofthePacific—fromthePetertheGreatBayandSanFranciscototheBeringStrait. SockeyeandChinookarequitecold-waterspecies,widelyprevailingalongtheAmericancoast.Chinookisthelargestspeciesof Pacificsalmon,referredtobyAmericansasKingsalmon.AllPacificsalmonspawnonlyonceduringtheirlifetime,perishingafter spawning. This feature is distinctive from the Atlantic salmon, which spawn up to four times (Rukhlov, 1982; Shuntov and Temnykh,2005).Differentsalmonspeciesspawnatdifferentages:chumenterstheriveronthethirdtofifthyearsoflife;pinksalmon, growinganddevelopingfasterthanchum,returns18monthsaftermigrationintothesea;Sockeyesalmonspendfrom1to5years (average2–3years)inthesea;andChinooksalmonlivefrom1to6years(average3–4years). AllPacificsalmonembedtheirhardroeintheground(inadughole);therefore,theychoosegravelandpebble,withouta muck-bottom.Afterthefertilizationofhardroe,thefemalefillsinthehollowwithpebbles.Theroedevelopsunderthehill,while Table1 InshorecatchingofPacificsalmoninthemainfisheryareasoftheFarEastin2011,th.tonnes(ShuntovandTemnykh,2011). Area Allspecies Pinksalmon Chum Sockeye Anadyr 2.1 0.4 1.4 0.3 Karaginsky 186.3 177.7 6.4 2.0 Petropavlovsk-Commander 18.1 4.7 2.3 9.3 WestKamchatka 44.7 6.0 14.9 21.0 Magadanregion 11.6 9.4 2.1 – NortherncoastofSeaofOkhotsk(Khabarovskyregion) 14.5 4.7 9.4 0.1 Amurbasin 19.0 4.4 15.6 – SakhalinIsland(SeaofOkhotsk) 192.3 176.7 15.5 – SouthKurilIslands 11.5 6.2 5.3 – NorthernKurilIslands 3.0 0.3 1.2 0.9 TatarStrait(Khabarovskyregion) 0.2 0.1 0.1 – Primorye 0.1 0.01 0.1 – SouthwestSakhalin 1.2 0.05 1.2 – All6speciesoftheFarEasternbasin 504.6 389.7 75.6 33.6 N.КKhristoforovaetal./AchievementsintheLifeSciences8(2014)55–60 57 formedalevinstayinitfortheresorptionofthevitellineeggs.Fryinsomespeciesimmediatelymigratewiththestream(chum,pink salmon),whiletheothersremainintheriverforayearortwoyears(sockeye,chinook,coho,masusalmon).Experimentshaveproved thatsalmonfindtheirriverbysmell,nomatterhowstrongitis. ThemainlocationsofconcentrationsofPacificsalmoninRussianwaterscanbedividedintoseveralgroupsthatdifferinspecies composition,biomassquantityofsalmonanddurationoftheperiodoftheirelevatedconcentrations.Thus,chumandsockeyesalmon dominateinthedeepwaterareaoftheBeringSea,whilepinkandchumsalmondominatetherestofspeciesinthedeepwaterareaof SeaofOkhotsk.TheNorthernKurilstraitsarethemainmigrationcorridorforspawningschoolsoftheWesternKamchatkasockeye, coho,chinook,chum,andpinksalmonfingerlingsmigratingintotheocean.TheKurilwatersandtheSeaofOkhotskaredominatedby pinkandchumsalmon.NortherndeepwaterareasoftheSeaofJapanaswellastheKurilwatersserveastransitzonesfortheWestern Kamchatkasalmonmigrations:masuandpinksalmonspawninAprilandJuly,autumnchumspawnOctober–December,whilemasu andpinksalmonjuvenilesgrowthroughthefallandwinter.IntheoffshoreareasoftheFarEasternseas,significantsalmonconcen- trationsareobservedonlywhenthesireapproachestospawnandduringtheredistributionofjuvenilesthatmigrateddownintoopen waters.ThisperiodlastsfromJunetoSeptember(Temnykh,2004). Pacificsalmonrepresentthelargestgroup,andtherefore,itisveryimportantforfisherypurposes.Ninetypercentofthecatches areprovidedbythreemajorspecies:pinksalmon,chumandsockeye(Table1). Pinksalmonisthemostnumerous,smallestandfastest-growingspecies.IthasaleadingdistributedvalueinRussianwaters (Table1).Althoughchumisthesecondmostnumerousspeciesafterpinksalmon,ithasahighernutritionalvalueandthereforea higherdemand. Westudiedthelevelsofsixelements–Zn,Cu,Cd,Pb,As,andHg–inchumandpinksalmonspeciesofPacificsalmoncaughtinthe KurilwatersinJuly2013andcomparedtheconcentrationsoftheseelementsinthewildsalmonandPacificandAtlanticsalmon speciesgrowninfishponds. Amongthestudiedtraceelements,thefirsttwo,copperandzinc,areessential(indispensable)orrealbioelements.Thelast four,cadmium,lead,arsenic,andmercury,arenon-essential,buttheyarealmostconstantlypresentinbodyorgansandtissues.In additiontothebiologicalsignificance,theseelementsalsohavedistinctphysicalfeatures.Copperandzinc,ifnotintroducedinto theenvironmentfromcopper–zincproductionanduseoftheiralloysandcompoundsinmachineryequipment(oremining, oreenrichmentandsmelting,electroplatingworkshops,anti-corrosioncoatings,etc.)aretracersofanthropogenicimpactonthe environment.Lead,cadmiumandmercury,toppingallofthe“blacklists”ofheavymetalsduetotheirtoxiceffectonorganismsin 1960–1970s,aretracersoftechnologicalenvironmentalimpact(Khristoforova,1989). MaterialsandMethods Informationonthecontentoftraceelementsinfishnotonlyrepresentsascientificinterestindicatingtheobjectqualityandthe qualityoftheirhabitatbutalsohaspracticalimportance.Itisessentialforthepopulationthatusesfishdirectlyforfoodandforthe processingindustry.IntheRussiancontext,salmonsareusedalmostentirely,withminimumwaste.Therefore,theidentificationof micro-elementswasconductedusingentirefishcarcassesmilledforhomogeneity.Forthepurposesofanalysis,sixunitsofpink andchumwerecaughtattheendofJuly2013inthenorthwesternPacificOceanrelativelyclosetotheKurilIslandsarea(46°39′N, 163°38′E)duringrecordexpeditionoftheTINROCentre. Alloftheelements,exceptmercuryweredeterminedinthehomogenatesofcarcassesandorgans,whichweredriedat85° followingthemineralizationofsamplesbyconcentratedHNO ofHighPuritygrade,accordingtoGOST26929-94ontheatomic 3 absorptionspectrophotometerShimadzuAA6800.Theelementidentificationaccuracyaswellasthepossiblecontaminationof samplesintheanalysiswerecontrolledaccordingtothefourcalibrationsolutions,includingthebaseline(zero)solution.Statistical dataprocessingwasperformedusingthestandardExcelsoftware.Theresultswererecalculatedtowetweight. Mercurywasidentifiedinfrozen(−20°)carcasshomogenatesafterthemineralizationofthesamplesbynitricacidwithhydrogen peroxide.Themassconcentrationofmercury(ppmofwetweight)wasfoundbystrippingvoltammetry(SV)usingtheanalyzer Table2 Averageconcentrationofthetraceelements(ppmofwetweight)inPacificsalmon(M±m,n=3)fromthenorth-westernPacific. ⁎ ⁎⁎ No. Traceelements,ppmofwetweight Zn Cu Cd Pb As Hg 1 2.24±0.64 0.12±0.04 0.07±0.01 0.54±0.18 0.92±0.28 0.07±0.01 2 2.48±0.74 0.11±0.03 0.08±0.01 0.68±0.20 0.94±0.28 0.09±0.02 3 3.15±0.87 0.17±0.08 0.11±0.03 0.77±0.23 1.27±0.37 0.12±0.04 4 3.34±0.93 0.16±0.07 0.12±0.04 0.95±0.28 1.32±0.39 0.15±0.04 ⁎ 1—pinksalmon,♂,weight(g)—1208–1459;2—pinksalmon,♀,weight(g)—1168–1272;3—chum,♂,weight(g)—1564–1609;4—chum,♀,weight(g)— 1670–1982. ⁎⁎ MPCoftoxicelementsinfishandfishproductsinRussia:Pb—1.0;As—5.0;Cd—0.2;Hg—0.2ppmofwetweight(inCanada:Hg—0.5;intheUnitedStates:Cd—3; Pb—1.5;As—86ppmofwetweight). 58 N.КKhristoforovaetal./AchievementsintheLifeSciences8(2014)55–60 “Tomanalyt”(TA-4).Theelementcontentinthesamplesolutionswasidentifiedusingtheadditionmethodofcertifiedmixtureswith establishedcontentofelements. ResultsandDiscussion TheanalysisresultsaredemonstratedinTable2. Ascanbeseeninmaleandfemalepinksalmonofsimilarmass,theconcentrationsofelementshavefewdifferences.Atthelevelof trends,onlythecontentofZn,PbandHgareslightlyhigherinfemaleindividuals.Inchumsalmon,inwhichallofthesampleswere muchlargerthanpinksalmon,theidentifiedelementswerepresentinlargerquantities.Amongthefishthatwerecaught,chum femaleswerelargerthanmales,andtheconcentrationsofalloftheelements,exceptcopper,werehigherthaninmaleindividuals. Therefore,inwildfishthatgainedweightintheocean,adirectrelationshipbetweentheweight(andsize)ofindividualsandthe contentoftraceelementsisobserved.Thisconsistencyisdisruptedwhenfisharegrowninstockingponds,wherethegrowthruns inashortperiodof12to23months(dependingonspecies)comparedwiththe2-to5-year-longlifeofwildsalmon.Inaperiodof rapidandextensivegrowth,theaccumulatedcontaminantsare“diluted”bymacronutrients,suchasproteinsorlipids.Canadian researchersKellyetal.(2008)foundasignificantcorrelationbetweentheconcentrationoftotalmercuryinfishfilletsanditssize (kg)forwildchinook:themercurycontentvariedfromapprox.0.01ppmfor2kgfishto0.1ppmfor8kgfish. Assessingtheoverallconcentrationsoftoxicelementsfoundinchumspecimensthatwerecaughtintheocean,itisimportantto emphasizethattheyarebelowtheMPClevelsdeterminedinRussiaandarealsolowerthaninthestandardsadoptedbyCanadaand theUnitedStates. Thesameauthors(Kellyetal.,2008)identifiedabroadrangeoftraceelementsinbredandwildsalmon,includingthewildchum fromtheinshorewatersofBritishColumbia.Theydemonstratedthattheconcentrationsofnon-essentialelementsrangedfrom0.001 ppmforCdto1ppmforAs.PbandHgconcentrationsrangedbetween0.01ppmand0.05ppm.Thecontentoftheessentialelements CuandZnfluctuatedbetween1and5ppm.Whiletheconcentrationsofzincinlocalchumandpinksalmon(2.24–3.34ppmofwet weight)werethesameasinthesalmonoftheCanadianPacificcoast,theconcentrationofcopperwassignificantlylowerthaninthe BritishColumbiasalmon.Hgconcentrationsinlocalsalmonvariedfrom0.07to0.15ppm,andleadconcentrationsrangedfrom0.30to 0.95ppm—thatis,theyweremorethananorderofmagnitudehigher.ConcentrationsofAsinlocalandCanadiansampleswereal- mostidentical,whilethecontentofCdwassignificantlyhigherinlocalsalmon. Itisimportanttoemphasizethatforeignauthors,providedataonthecontentoftraceelementsinfishfillets.However,in discussingtheresultsofTable2,weconsidertheentirefishcarcass. For a correct comparison of our results with the data reported in the works of foreign authors, we also determined the concentrationsofelementsinthemusclesofPacificsalmonandcomparedthemwiththepublisheddataforAtlanticsalmon—salmon rearedincages(Tables3and4). AscanbeseenbycomparingthedataofTables2and3,thecontentoftraceelementsinsalmonmuscleissignificantlylowerthan intheentirecarcass.Itistwotimeslowerformercury,whichisfoundprimarilyinadiposetissue;aboutoneandahalftimeslowerfor lead,whichisconcentratedmainlyinthebonesoffish;twotimeslowerforcadmium,whichaccumulatesmainlyintheliver;and almosttwotimeslowerforzinc,whichprimarysedimentatesinthegillsandthegonads.Onlytheconcentrationsofthecopper andarsenicremainthesamebothintheentirecarcassandthemuscles. Although,duetotheadjustmentforseveralmuscles,thecontrastoftraceelementlevelsinthesalmonoftheKurilandCanadian waterswasreduced,anditisclearthatthefishoftheWesternPacificcontaingreatercadmiumandleadconcentrationsandlower concentrationsofcopperthanthefishoftheEasternPacific. Acomparisonoftraceelementcompositionofthetwogroupsofsalmon(Tables3and4)revealsthatthemercuryinWestern PacificsalmonisaboutthesameasinAtlanticsalmon,althoughtheconcentrationofthisstrictlyregulatedelementisthelowestin themuscleofPacificpinksalmon.ArsenicisdistributedmoreuniformlyinthewildPacificsalmonsamples,rangingfrom0.89ppm inpinksalmonto1.36ppminchumsalmon.ThegreatestvariabilityamongtheAtlanticsalmonbredintherearingchannelsisob- servedintheNorwegianfishfillets.Itrangesfrom0.45to2.33ppm,whiletheaveragearsenicconcentrationsarequitesimilarin bothgroupsofsalmon.CadmiumconcentrationsintheNorwegiansamplesthatweremeasuredindifferentyearsdifferbyan orderof magnitude, ranging from undetectabletraces to 0.11 ppm. In cadmiumcontent, Pacific salmon standsbetween the NorwegianandCanadianfish. Table3 TheaveragecontentoftraceelementsinthemusclesofPacificsalmon(M±m,n=3)(July,2013). No.⁎ Definingelements,ppmofwetweight Zn Cu Cd Pb As Hg 1 1.24±0.31 0.10±0.04 0.03±0.02 0.45±0.10 0.89±0.32 0.02±0.01 2 1.33±0.25 0.11±0.05 0.04±0.01 0.55±0.10 0.97±0.42 0.04±0.01 3 1.74±0.40 0.15±0.06 0.05±0.03 0.63±0.15 1.25±0.44 0.06±0.01 4 1.88±0.36 0.16±0.07 0.06±0.02 0.78±0.10 1.36±0.57 0.08±0.01 ⁎ 1—pinksalmon,♂,weight(g)—1208–1459;2—pinksalmon,♀,weight(g)—1168–1272;3—chum,♂,weight(g)—1564–1609;4—chum,♀,weight(g)— 1670–1982. N.КKhristoforovaetal./AchievementsintheLifeSciences8(2014)55–60 59 Whilethedistributionofthreeelements–Hg,As,andCd–infilletsofPacificandAtlanticsalmonappearstobemoreorlesssimilar, thecontentoftheotherthreeelementsindifferentgroupsoffishdifferssignificantlyandrequiresadeeperanalysisofthecauses. AcomparisonofthedatainTables3and4indicatesthatthefilletsofsalmongrowninfishpondscontains5–10timesmorezinc andcopperthanthewildPacificsalmonmuscle.Aswasnotedabove,ZnandCuarethetracersofanthropogenicimpactonthe environmentandbiota.Thereisnodoubtthatsalmonbredintheinshorezonewillbeaffectedbyhighercontaminationofshallow watercomparedtotheopenocean.Additionally,thereisanimpactoffeedpreparedbyman,sometimescontainingfreshwater fish.Finally,regardlessofthemanufacturers'endeavors,NorwegianfishwillbeaffectedbytheinfluenceoftheGulfStream,apow- erfulstreamofstartingofftheAmericancoastthatcollectsthecoastaleffluentsanddischargesthemontheScandinavianshore. ItcanbenotedthatunlikebredAtlanticsalmon,thewildPacificchumandpinksalmoncaughtintheKurilwatershavehigh concentrationsoflead.WhiletheleadcontentinthebredsalmonfilletsfromboththeAtlanticandEasternPacific(Canada)ranges between0.02and0.15ppm,itincreasesinthemusclesofKurilWesternPacificsalmonfrom0.45ppminmalepinksalmonto0.78 ppminfemalechum. Aswaspreviouslymentioned(Kellyetal.,2008),theconcentrationsinwildsalmonsmayreflectgeographicvariationsin theenvironment.Theyarereflectednotonlyinsalmonandotherfishbutalsoinallaquaticandterraneousorganisms.Despitethe apparenthomogeneityofthewatermassesinthesea,therearebiogeochemicalprovinces,asonland,thatmanifestintheoriginal mineralcompositionoforganisms(Khristoforovaetal.,1979;KhristoforovaandBogdanova,1981).ThePacificRingofFirestarting fromthevolcanoesofKamchatkacontinuingwithvolcanosofKurilislands,JapaneseislandsandsouthernWesternPacificisland arcsisapowerfulsourceofgeochemicalimpactsonthemarineenvironment.Thesupplierofchemicalelementsintheenvironment isunderwaterandabove-watervolcanism.Forexample,onasmalluninhabitedcoralisland,Bio(SolomonIslands),thereasonfora particulargeochemicalenvironmentincoastalwatersthatcausedanincreaseinthemetalcontentinCaulerpaandHalimedalesalgae wastheashfallsfromthevolcanoMbanya,located100kmawayfromtheisland(KhristoforovaandBogdanova,1980).Asaresultof post-volcanicprocesses,kilogramsofFe,Mn,Ag,Cu,andothermetalsareejecteddailyfromdeeplayersand,afterdissolutioninthe thermalwaters,arecarriedbystreams(Markhinin,1985). Kuril–Kamchatka Trench, which delivers nutrients (Propp and Propp, 1988) and other elements through upwelling (MalinowskayaandKhristoforova,1997)intheupperlayersofthewater,isalsoasourceoftheformationofimpactgeochemical zonesintheNorthwesternPacific.Thestudyofthemetalcontent(Fe,Mn,Zn,Cu,Cd,Pb,Ni,Cr)inbrownalgae,bivalvesandgastro- podsthatinhabittheKurilIslandsandfoulthenavigationbuoysalongtheNorthwesternPacificcoastrepeatedlydemonstratesthe existenceofbiogeochemicalprovincesinthesea,identifiedbyelevatedconcentrationsofelementsinorganisms(Khristoforova andKavun,1988;Kavunetal.,1989,2002;KavunandKhristoforova,1991;MalinowskayaandKhristoforova,1997). IncontrasttoZnandCu,whichareactivemigrantelementsthatarepresentinthemarineenvironmentinasolubleformandare easilyspreadbycurrents,Pbinsaltwaterisfoundpredominantlyinasuspendedformthatislessmobileandmorelocalized(Yeats, 1988;Khristoforovaetal.,1993;Khristoforova,1994).Itappearsthatthisweakmigrantismoreeasilyfixedbyorganismsforthis reason.First,itisfixedbyplanktonandthenbyitsconsumernekton,includingthemassfishoftheupperpelagicandthestudied Pacificpinkandchumsalmon. Conclusion Withal,thewildPacificpinkandchumsalmoncaughtintheKurilwaters,meetstherequirementsforseafoodforthecontentofthe regulatedtoxicelementsCd,Pb,AsandHg.Thecontentofeachelementdoesnotexceedthemaximumpermittedconcentrationsap- provedbytheRussianstandards.DifferencesinthecontentofelementsinwildPacificsalmonandAtlanticsalmonbredinpondsrep- resentagreatscientificandpracticalinterest.HigherconcentrationsofZnandCuinfarmedsalmonandofPbinpinkandchum salmonfromtheKurilwatersarecausedbythesamefactor—thegeochemicalconditionsoftheenvironment.However,theimpact conditionsofthecoastalwatersevaluatedbysuchtracersaszincandcopperarecausedbyanthropogenicactivity,whiletheimpact zonesinthewatersoftheWesternPacificareformedundertheinfluenceofnaturalfactorsofmodernvolcanismandupwelling. Acknowledgments TheresearchwassupportedbyRFBRgrant(no.12-04-32043)andtheScientificFundofFEFU(no.12-04-13000-33/13). Table4 TheconcentrationoftraceelementsinthemusclesofSalmosalarbredinarearingchannel. Country Year Theconcentrationoftoxicelements,ppmwetweight Source Zn Cu Cd Pb As Hg Iceland 2004 – – 0.08 0.15 0.80 0.073 Ásmundsdottiretal.,2005 Norway 2002 – – 0.03 0.02 2.33 0.072 Eastonetal.,2002 Norway 2003 18.50 1.11 0.00 0.10 0.53 0.09 Liasetetal.,2003 Norway 2007 5.48 0.49 0.11 0.09 0.45 0.129 Sivakumaretal.,2007 Norway 2010 17.25 1.13 0.01 0.08 1.13 0.09 Maldeetal.,2010 60 N.КKhristoforovaetal./AchievementsintheLifeSciences8(2014)55–60 References Ásmundsdottir,A.M.,Auðunsson,G.A.,Gunnlaugsdottir,H.,2005.Undesirablesubstancesinseafoodproducts—resultsfrommonitoringactivitiesinyear2004. IcelandicFisheriesLaboratoriesReport33-05(14pp.). Easton,M.D.,Lusniak,D.,VonderGeest,E.,2002.Preliminaryexaminationofcontaminantloadingsinfarmedsalmon,wildsalmonandcommercialsalmonfeed. Chemosphere46,1053–1074. Kavun,V.Ya.,Khristoforova,N.K.,1991.TheRoleofModernVolcanismandUpwellingintheFormationofImpactZonesofHeavyMetalsinCoastalWatersoftheKuril Islands//ShallowGazogidrotermsandKraternayaBayEcosystem(VolcanoUshishir,KurilIslands)Book.1.Ch.2FarEasternBranchofRussianAcademyof Sciences,Vladivostok,pp.114–120. Kavun,V.Ya.,Khristoforova,N.K.,Shulkin,V.M.,1989.MicroelementcompositionoftissuesofediblemusselsfromthecoastalwatersofKamchatkaandthenorthern KurilIslands.Ecology3,53–59. Kavun,V.Ya.,Shulkin,V.M.,Khristoforova,N.K.,2002.MetalaccumulationinmusselsoftheKurilIslands,north-westPacificOcean.Mar.Environ.Res.53,219–226. Kelly,B.C.,Ikonomov,M.G.,Higgs,D.A.,Oakes,J.,Dubetz,C.,2008.MercuryandothertraceelementsinfarmedandwildsalmonfromBritishColumbia,Canada.Environ. Toxicol.Chem.27,1361–1370. Khristoforova,N.K.,1989.Bioindicationandmonitoringofpollutionofmarinewatersbyheavymetals.Nauka,Leningrad(192pp.). Khristoforova,N.K.,1994.Chemical–ecologicalcharacteristicsKandalakshaBayoftheWhiteSeaonthecontentofheavymetalsinshellfishandalgae.Biol.Morya20 (2),154–162. Khristoforova,N.K.,Bogdanova,N.N.,1980.MineralcompositionofseaweedsfromcoralislandsofthePacificOceanasafunctionofenvironmentalconditions.Mar. Ecol.Prog.Ser.3,25–29. Khristoforova,N.K.,Bogdanova,N.N.,1981.EnvironmentalconditionsandheavymetalcontentofmarineorganismsfromatollsofthePacificOcean.Proceedingsof4th Int.CoralReefSymp.“ReefandMan”,Manila,1,pp.161–162. Khristoforova,N.K.,Kavun,V.Ya.,1988.MonitoringthestatusoftheFarEasternseaswatersformusselsfoulingnavigationbuoys.ReportUSSRAcademyofSciences,5 (300),pp.1274–1276. Khristoforova,N.K.,Bogdanova,N.N.,Obukhov,A.I.,1979.ContentsofsomemetalsinthesofttissuesofthebivalveTridacnasquamosaintheislandsofthetropicalzone ofthePacificOceaninrelationtotheconditionsofexistence.Biol.Morya3,67–73. Khristoforova,N.K.,Shulkin,V.M.,Kavun,V.Ya.,Chernova,E.N.,1993.HeavymetalsincommercialandculturedshellfishinthePetertheGreatBay.Dalnauka,Vladivos- tok(296pp.). Liaset,B.,Julshamn,K.,Espe,M.,2003.Chemicalcompositionandtheoreticalnutritionalevaluationoftheproducedfractionsfromenzymichydrolysisofsalmonframes withProtamex™.ProcessBiochem.38,1747–1759. Malde,M.K.,Bügel,S.,Kristensen,M.,Malde,K.,Graff,I.E.,Pedersen,J.I.,2010.Calciumfromsalmonandcodboneiswellabsorbedinyounghealthymen:a double-blindedrandomizedcrossoverdesign.Nutr.Metab.7,61. Malinowskaya,T.M.,Khristoforova,N.K.,1997.CharacteristicsofcoastalwatersoftheSouthernKurilesincontentoftraceelementsinindicatororganisms.Biol.Morya 23(4),239–246. Markhinin,E.K.,1985.Volcanism.Nedra,Moscow(288pp.). Propp,M.V.,Propp,L.N.,1988.HydrochemicalandcontentofchlorophyllinthecoastalwatersoftheKurilIslands.Biol.Morya4,68–70. Rukhlov,F.N.,1982.LifeofPacificsalmon.FarEasternBookPublishers,SakhalinBranch,Yuzhno-Sakhalinsk(112pp.). Shuntov,V.P.,Temnykh,O.S.,2005.NewideasabouttheecologyofPacificsalmoninthemarinelifeperiod.ProceedingsinMemoryofVladimirYakovlevichLevanidov, 3.Dalnauka,Vladivostok,pp.13–25. Shuntov,V.P.,Temnykh,O.S.,2011.Pacificsalmoninmarineandoceanecosystems,2.TINROCenter,Vladivostok(473pp.). Sivakumar,V.,Driscoll,B.,Obenauf,R.,2007.Traceelementsinfishandfishoilsupplements.At.Spectrosc.28,13–16. Temnykh,O.S.,2004.Asianpinksalmonduringthemarineperiodoflife:biology,spatialdifferentiation,theplaceandroleinthepelagiccommunities(ThesisofDoctor Biol.Sciences)TINROCentre,Vladivostok,p.47. Worldreviewoffisheriesandaquaculture,2012.StateofWorldFisheriesandAquacultureRome.FAO(118pp.). Yeats,P.A.,1988.Thedistributionoftracemetalinoceanwaters.Sci.TotalEnviron.72,131–149.

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