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    IAP STATEMENT ON OCEAN ACIDIFICATION

    Headline messages

    OceansplayacriticalroleintheglobalcarboncyclebyabsorbingaboutaquarterotheCO2emittedtotheatmosphereromhumanactivities;

    TherapidincreaseinCO2emissionssincetheindustrialrevolutionhasincreasedtheacidityotheworldsoceanswithpotentiallyprooundconsequencesormarineplantsandanimalsespeciallythosethatrequirecalciumcarbonatetogrowandsurvive,andotherspeciesthatrelyontheseorood;

    Atcurrentemissionratesmodelssuggestthatallcoralreesandpolarecosystemswillbeseverelyaectedby2050orpotentiallyevenearlier;

    Marineoodsuppliesarelikelytobereducedwithsignifcantimplicationsoroodproductionandsecurityinregionsdependentonfshprotein,andhumanhealthandwellbeing;

    Oceanacidifcationisirreversibleontimescalesoatleasttensothousandsoyears;

    EvenwithstabilisationoatmosphericCO2at450ppm,oceanacidifcationwillhaveprooundimpactsonmanymarinesystems.LargeandrapidreductionsoglobalCO 2emissionsareneededgloballybyatleast50%by2050.

    1. CO2 and ocean chemistry

    Overthepast200years,theoceanshaveabsorbedapproximatelyaquarterotheCO 2producedromhumanactivities.ThisCO2wouldotherwisehaveaccumulatedintheatmosphereleadingtogreaterclimatechange.However,theabsorptionothisCO2hasaectedoceanchemistryandhascausedtheoceans(whichareonaverageslightlyalkaline)tobecomemoreacidic.TheaveragepHooceanicsuracewatershasbeenloweredby0.1unitssincethepre-industrialperiod.Thisrepresentsa30%increaseinhydrogenionactivity.Hydrogenionsattackcarbonateionswhicharethebuildingblocksneededbymanymarineorganisms,suchascoralsandshellfsh,toproducetheirskeletons,shellsandotherhardstructures.Thislossocarbonateionsproducelowersaturationlevelsorthecarbonateminerals,aragoniteandcalcite,whichareusedinmanyshellsandskeletons.Carbonateionconcentrationsarenowlowerthanatanyothertimeduringthelast800000years.

    GlobalatmosphericCO 2concentrationsarenowat387ppm.IcurrenttrendsinCO 2emissionscontinue,modelprojectionssuggestthatbymid-centuryCO 2concentrationswillbemorethandoublepre-industriallevelsandtheoceanswillbemoreacidicthantheyhavebeenortensomillionsoyears.Thecurrentrateochangeismuchmorerapidthanduringanyeventoverthelast65millionyears.Thesechangesinoceanchemistryareirreversibleormanythousandsoyears,andthe

    biologicalconsequencescouldlastmuchlonger.

    2. Environmental damage rom ocean acidifcation

    Oceanacidifcationimpactsonmarineliewilldependontherateandmagnitudeochangesinoceanchemistryandbiologicalresponses.Whiletheoceanchemistrychangesarepredictablewithhighcertainty,ourunderstandingotheimpactsisstilldeveloping.Nevertheless,thereisstrongevidenceemergingorarangeobiologicaleectsandchangesinthemarinebiogeochemicalprocessesthataectthecarboncycle.Thelong-termconsequencesothisaredifculttopredict.

    Impactsarealreadybeingobservedinthepolarandtropicalregions.Coralcalcifcationrateshavedeclinedinrecentdecades,althoughattributingcausesortheseimpactsamongmultipledrivers(acidifcation,warming,pollution,etc.)isachallenge.FundamentalecologicaloceanprocesseswillbeaectedasmanymarineorganismsdependdirectlyorindirectlyoncalciumcarbonatesaturatedwatersandareadaptedtocurrentlevelsoseawaterpHorphysiologicalandmetabolicprocessessuchascalcifcation,growthandreproduction.ThepHchangesexpectedwillexceedtheseasonalandregional

    variationscurrentlyexperiencednaturally.

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    Oceanacidifcationisaglobalissue.However,changesinoceanchemistrywillberegionallyvariablewithsomeregionsaectedmorerapidlythanothers.ThehighCO 2watersinpolarandupwellingregionssuchastheeasternPacifcandBeringSeaorexample,willexperiencelowpHmorerapidlythanotherregions.Tropicalwaters,suchasthosearoundtheGreatBarrierReewillalsoexperiencerapiddeclinesinthecarbonateionsimportantorcoralreeconstruction.Accordingtorecentmodelprojectionsalmostalltropicalandsub-tropicalcoralreesweresurroundedbywatersavourabletocoralgrowthbeoretheindustrialrevolution.IatmosphericCO 2isstabilizedat450ppm,onlyaverysmallraction(~8%)oexistingtropicalandsubtropicalcoralreeswillbesurroundedbysuchwater,andat550ppm,coralreesmaybedissolvingglobally.Coldwatercoralsarealsovulnerableandarelikelytobeaectedbeoretheyhaveevenbeenullyexplored.By2100,ithasbeenestimatedthat70%willbeinwatersunavourableorgrowth.

    Inthepolarregions,modelprojectionsusingcurrentCO 2emissionratessuggestthatpartsotheSouthernOceanwillbeundersaturatedoraragoniteby2050.Aragoniteundersaturationisprojectedor10%oArcticwatersbyaround2020,andby2060,80%owaterswillbeundersaturatedoraragoniteandcalcite.ThismeansthewaterswillbecorrosivetoArcticcalciferssuchaspteropods,andbivalvessuchasclams,whichplayakeyroleinArcticoodwebs.

    Theoceanchemistrychangesprojectedwillexceedtherangeonaturalvariability,whichislikelytobetoorapidormanyspeciestoadaptto.Manycoastalanimalsandgroupsophytoplanktonandzooplanktonmaybedirectlyaectedwithimplicationsorfsh,marinemammalsandtheothergroupsthatdependonthemorood.IncreasedCO 2maybeparticularlystressulororganismswithhighmetabolicratessuchassquid.Theimpactsothesechangesonoceanicecosystemsandtheservicestheyprovide,orexampleinfsheries,coastalprotection,tourism,carbonsequestrationandclimateregulation,cannotyetbeestimatedaccuratelybuttheyarepotentiallylarge.

    Althoughsomespeciesmaybeneft,mostareadaptedtocurrentconditionsandtheimpactsonoceanbiologicaldiversityandecosystemunctioningwilllikelybesevere.AnalysisopasteventsinEarthsgeologichistorysuggeststhatchemicalrecoverywilltaketensothousandsoyearswhiletherecoveryoecosystemunctionandbiologicaldiversitycantake

    muchlonger.

    4. Mitigation

    Oceanacidifcationisirreversibleduringourlietimesandthoseomanygenerationstocome.Tominimisetheriskotheselarge-scaleandlong-termchangestotheoceanstheincreaseinatmosphericCO 2mustbecurbedbyreducingemissionsromhumanactivities.

    RecentscenariostudieshaveestimatedthatstabilisationoatmosphericCO 2concentrationsat550ppmwillproduceenoughacidifcationtobedisastrousorsensitiveoceanicecosystemsinmanypartsotheworld.Evenat450ppm,morethan10%otheworldsoceanswillbeimpactedincludinglargepartsotheSouthern,NorthPacifc,andArcticoceans.

    Mitigationapproachessuchasaddingchemicalstocountertheeectsoacidifcationarelikelytobeexpensive,onlypartlyeectiveandonlyataverylocalscale,andmayposeadditionalunanticipatedriskstothemarineenvironment.Therehasbeenverylittleresearchontheeasibilityandimpactsotheseapproaches.Substantialresearchisneededbeorethesetechniquescouldbeapplied.

    5. Conclusions and recommendations

    OceanacidifcationisadirectconsequenceoincreasingatmosphericCO 2concentrations.Toavoidsubstantialdamagetooceanecosystems,deepandrapidreductionsoglobalCO 2emissionsbyatleast50%by2050,andmuchmorethereaterareneeded.

    We,theacademiesoscienceworkingthroughtheInterAcademyPanelonInternationalIssues(IAP),callonworldleadersto:

    AcknowledgethatoceanacidifcationisadirectandrealconsequenceoincreasingatmosphericCO 2concentrations,isalreadyhavinganeectatcurrentconcentrations,andislikelytocausegraveharmtoimportantmarineecosystemsasCO2concentrationsreach450ppmandabove;

    RecognisethatreducingthebuildupoCO2intheatmosphereistheonlypracticablesolutiontomitigatingocean

    acidifcation;WithinthecontextotheUNFCCCnegotiationsintherunuptoCopenhagen2009,recognisethedirectthreatsposedbyincreasingatmosphericCO 2emissionstotheoceansandthereoresociety,andtakeactiontomitigatethisthreat;

    ImplementactiontoreduceglobalCO2emissionsbyatleast50%o1990levelsby2050andcontinuetoreducethemthereater;

    Reinvigorateactiontoreducestressors,suchasoverfshingandpollution,onmarineecosystemstoincreaseresiliencetooceanacidifcation.

    Theollowingacademieshaveendorsedthisstatement.

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    TWAS,theacademyosciencesorthedevelopingworld

    AlbanianAcademyoSciences

    NationalAcademyoExact,PhysicalandNaturalSciences,Argentina

    AustralianAcademyoScience

    BangladeshAcademyoSciences

    TheRoyalAcademiesorScienceandtheArtsoBelgium

    BrazilianAcademyoSciences

    BulgarianAcademyoSciences

    CameroonAcademyoSciences

    RSC:TheAcademiesoArts,HumanitiesandSciencesoCanada

    AcademiaChilenadeCiencias

    ChineseAcademyoSciences

    ColombianAcademyoExact,PhysicalandNaturalSciences

    CroatianAcademyoArtsandSciences

    CubanAcademyoSciences

    AcademyoSciencesotheCzechRepublic

    RoyalDanishAcademyoSciencesandLetters

    AcademiadeCienciasdelaRepblicaDominicana

    AcademyoScientifcResearchandTechnology,Egypt

    TheDelegationotheFinnishAcademiesoScienceandLetters

    AcadmiedesSciences,France

    GeorgianAcademyoSciences

    UnionderDeutschenAkademienderWissenschaten

    DeutscheAkademiederNaturorscherLeopoldina

    TheAcademyoAthens

    AcademiadeCienciasMedicas,FisicasyNaturalesdeGuatemala

    IndianNationalScienceAcademy

    IndonesianAcademyoSciences

    AcademyoSciencesotheIslamicRepublicoIran

    RoyalIrishAcademy

    IsraelAcademyoSciencesandHumanities

    AccademiaNazionaledeiLincei

    ScienceCounciloJapan

    RoyalScientifcSocietyoJordan

    IslamicWorldAcademyoSciences

    AricanAcademyoSciences

    KenyaNationalAcademyoSciences

    TheKoreanAcademyoScienceandTechnology

    KosovoAcademyoSciencesandArts

    NationalAcademyoSciencesotheKyrgyzRepublic

    AkademiSainsMalaysia

    MauritiusAcademyoScienceandTechnology

    AcademiaMexicanadeCiencias

    MontenegrinAcademyoSciencesandArts

    TheRoyalNetherlandsAcademyoArtsandSciences

    AcademyotheRoyalSocietyoNewZealand

    NigerianAcademyoSciences

    NorwegianAcademyoSciencesandLetters

    PakistanAcademyoSciences

    PalestineAcademyorScienceandTechnology

    AcademiaNacionaldeCienciasdelPeru

    AcademiadasCienciasdeLisboa

    AcadmiedesSciencesetTechniquesduSngal

    SerbianAcademyoSciencesandArts

    SlovakAcademyoSciences

    SlovenianAcademyoSciencesandArts

    AcademyoScienceoSouthArica

    RoyalAcademyoExact,PhysicalandNaturalSciencesoSpain

    NationalAcademyoSciences,SriLanka

    SudaneseNationalAcademyoScience

    RoyalSwedishAcademyoSciences

    AcademiaSinica,Taiwan,China

    TanzaniaAcademyoSciences

    TheCaribbeanAcademyoSciencesTurkishAcademyoSciences

    TheUgandaNationalAcademyoSciences

    TheRoyalSociety,UK

    USNationalAcademyoSciences

    AcademiadeCienciasFsicas,MatemticasyNaturalesdeVenezuela

    ZimbabweAcademyoSciences