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Risingoceantemperaturesmaypushcoralreefstotheirlimits. ClimateChangeandCoralBleaching http://www.nova.org.au/coral-bleaching Essentials ! Coralsareanimalsthatliveinamutuallybeneficialrelationshipwithatypeofmicroalgaecalled zooxanthellae ! Thezooxanthellaeprovideorganiccarbon(energy)tothecorals,andreceiveinorganicnutrients (fertilizer)fromtheircoralhosts ! Coralsaresensitivetosmallchangesinwatertemperatures—longperiodsofhighertemperatures resultinthebreakdownofthecoral-zooxanthellaerelationship,andifwarmforlongenough,will leadtocoraldeath ! Coralbleachingoccurswhenthezooxanthellaeleavethecorals—withoutthenutrientsprovided bythezooxanthellae,thecoralseventuallydieofstarvationanddisease ImagineyouareonabeautifultropicalislandontheGreatBarrierReef.Youputonyourmask,finsand snorkelandjumpintothewater.Butinsteadofthefamousbrightlycoloredcoral,youseeadrab underwaterlandscapedominatedbyblue-greenalgae(cyanobacteria)andseaweed,butnocorals. Astheworld'soceansbecomewarmer,andmoreacidic,thisscenariowilloccurmorefrequently,onthe GreatBarrierReefandcoralreefstheworldover. Coralsareanimals TheancientGreeksmistakenlybelievedcoralstobeplants. Theyareactuallysimplemulticellularanimalsthatarerelated toanemonesandjellyfish.Individualcoralanimals,called polyps,buildexternalskeletonsmadeofcalciumcarbonate (similartolimestone). Hundredsofindividualsjointogethertomakecoralcolonies. Eachpolypsitsinitsskeletoncup,andhasacentralmouth surroundedbytentacleswithstingingcellsonthem.Thetiny tentaclestrappassingplanktonandpushitintoasmallcavity thatactsasastomach. Awin-winrelationship Butittakesmorethanabunchofcoralpolypstomakeahealthycoralreef.Coralsalsoplayhostto thousandsoftinyorganismscalledzooxanthellae,individualsthatlivewithineachcoralcell. Zooxanthellaearesingle-celleddinoflagellatemicroalgaethatusephotosynthesistoproduceorganic carbon(energy)intheformofsugarsandothercompounds.Theypassmostoftheseontotheircoral hosts.Thesecompoundsmakeupover95percentofthecoral’sfoodandnutritionrequirements.In return,thezooxanthellaereceiveinorganicnitrogenandphosphorusfromthewasteproductsofthecoral polypsownmetabolicprocesses. coral_bleaching.docx 3/16/17 Thezooxanthellaearealsoresponsibleforthebrowncolorofmanycorals.Thebrightpinks,greensand bluesalsoseenincoralreefsareproducedbyfluorescentcompoundsmadebythecoralhostthatprotect thezooxanthellaefromgettingtoomuchsunlight,whichcanbeaproblematthemiddleofthedayon coralreefsinthetropics. Coralsalsomakecompounds(calledmycosporine-likeaminoacids),whichactasasunscreen,protecting themfromtoomuchultravioletradiation.Coralscanvarytheconcentrationofbothofthesecompounds tohelpthemacclimatizetolocalconditions.However,therearelimitstotheabilityofthesepigmentsto respondandprotectthezooxanthellae.Ifconditionschangetooquicklyorsubstantially,thecoral’sability toacclimatizewillbeoverwhelmed,leadingtocoraldamageordeath. Nottoohot,nottoocold...it’sgottobejustright Coralsarealsofussyaboutthetemperatureofthewaterinwhichtheylive.Somecoolwatercoralsare happywithwatertemperaturesofaround18°C,whilelotsoftropicalcoralsliveinwaterswith temperaturesbetween23and29°C.Some,likethoseintheArabianGulf,canexperiencetemperaturesup to34°Cormore. Althoughmostcoralscancopewithhighertemperaturesforshortperiodsoftime,theydon’tlikeitif temperaturesstayhighforlongperiods—acoralthatlivesin27°Cwatermaycopewiththewaterbeing 29°Cforadayortwo,butwouldn’tliketobein31°Cforaweek. Coralbleaching Bleachingoccurswhentheclose symbioticrelationshipbetweenthezooxanthellae andtheircoralhostsbreaksdown.Thiscanbe causedbyanumberofenvironmentalstresses,most commonlyhigherwatertemperatures,particularly whencombinedwithstill,warmoceanconditions. Thephotosynthesisprocessinthezooxanthellaeis disrupted,andtheyproduceanexcessofproducts thatbecometoxictothemselves.Thisinturn damagesthemetabolismofthecoralpolyp,which expelsthebrownzooxanthellae,leavingthecoral skeletonastark,‘bleached’white. Thebleachedcoralcanrecover,butonlyifwatertemperaturecoolsagainandthezooxanthellaehave timetobeabletorepopulatethecellsofthecoralhost.Iftemperaturesremainabovethebleaching threshold,zooxanthellaewillbelostforsubstantialperiodsoftime.Withoutthemealticketprovidedby theirzooxanthellae,coralswilleventuallydiefromstarvationanddisease. Causes Heatstresswillgenerallyresultinthemassbleachingoflargeareasofcoral.Smallerregionsofcoralreefs canalsoaffectedbymorelocalizedimpacts,suchas: ! exposuretotoomuchlightandultraviolet(UV)radiation ! decreaseinsalinityfromstormwaterandheavyrainsfloodingthereef ! exposuretocoraldiseases ! sedimentssuchassandordirtcoveringthecoralforextendedperiods ! exposuretochemicalcompoundssuchascyanide,herbicidesandpesticides coral_bleaching.docx 3/16/17 Temperaturesareontheup Overthepast100years,thetemperatureofseawaterinalmostalltropicalareashasbeenrisingrapidly. ComprehensiveseasurfacetemperatureshavebeenmeasuredintheAustralianregionsincetheearly 1980s.These,andhistoricalrecordsshowthatthepasttwodecadeshavebeenthewarmestsincethese recordsbeganin1870. Theserecordsarecomplementedbyrecordsfromtheskeletonsoflong-livedcoralssuchasPorites.The corals’calciumcarbonateskeletonismadefromcalcium,carbonandoxygen.Therearetwomainisotopes ofoxygenfoundwithinthecalciumcarbonate,andtheratioofthesetwoisotopesdependspartlyonthe temperatureofthewaterinwhichthecoralgrew.So,asthecoralgrows,layingdownnewlayersof calciumcarbonate,itcreatesarecordoftemperature.Bystudyinghowtheoxygenisotoperatiovaries throughacoreofthecoralskeleton,scientistshavebeenabletoreconstructseatemperaturesgoingback hundredsofyears.Theserecordsshowthatinthecontextofthepastfewhundredyears,recent temperatureshavebeenunusuallywarm. Oceantemperaturesarepredictedtocontinuetoriseifwekeepaddingcarbondioxideandother greenhousegasestotheatmosphere.The2013IntergovernmentalPanelonClimateChange(IPCC)report predictsanincreaseinthesurfacetemperatureoftropicaloceansof3–4°Cby2100ifnochangeismade tothecurrentpatternsofgreenhousegasemissions.Australianandinternationalresearchhasshown thatanincreaseinaverageglobaltemperaturesofjust1°Cabovethepreindustrialperiodwillcausecoral reefstolosealltheircoralsbymid-century. Cancoralssurvivebleaching? Althoughthecoralanimalsthatmakeupmoderncoralreefshaveoccupiedreefsystemsforatleast240 millionyears,thecurrentreefstructuresontheGreatBarrierReefformedaftersealevelsstabilized around8,000–10,000yearsago.Coralreefsgenerallyoccurinareaswhereaveragewatertemperatureis only1–2°Cbelowthetemperatureatwhichthecoralsbecomestressedandundergobleaching,soan averagetemperatureincreaseof3–4°Cbytheendofthiscentury,aspredictedbythe2013IPCCreport, doesnotbodewell. Somescientistshavesuggestedthatcoralsmaybeabletoadapttowarmertemperaturesbychangingthe typeofsymbioticzooxanthellaetheyhost.However,thereislittlescientificevidenceofcoralsbeingable toswaptheirsymbioticzooxanthellaefornew,warmervarieties.Thereissomeevidencethatsometypes ofcoralcancopebetterwithwarmertemperaturesthanothertypes.However,thesedifferencesbetween coraltypeswillonlygivemorethermallytolerantcoralsaleewayof1–2°C.Consequently,these differenceswillonlyhelpintheshorttermandwillcertainlynotofferalongtermsolutioninthefaceof continuedincreasingtemperatures. Aswatertemperaturescontinuetoincrease,goingbeyondthewindow oftemperaturesthatcoralsliketolivein,theywillfinditharderto survive.Thestressesofincreasedtemperatureswillbecompounded bythoseofincreasedextremeweathereventslikecyclonesand storms,andalsooceanacidification.Coralsinwarmerandmoreacidic seaswillfindithardertorecoverafternaturaldisturbances,leadingto aneverdiminishingamountofcoralontheworld’scoralreefs. coral_bleaching.docx 3/16/17 Coralreefsneedourprotection Preventingstressfromthingsliketoomuchsediment,pollutionanddestructivefishingwillhelpour reefs.Ultimately,though,itisthesustainedhighertemperaturesthatclimatechangeisprojectedtobring thatposethegreatestthreattothewell-beingofcoralreefs.Curbingofgreenhousegasemissionswill makethebiggestdifferenceinensuringtheirlong-termsurvival. Whyarecoralreefsimportant? Coralreefsareimportantformanydifferentreasons.Thelargecalciumcarbonate(limestone-like)reef structuresthatcoralscreatehelpunderpintheconstructionofislandswhileatthesametimeprotecting shorelinesfromthedamagingimpactsofwavesandstorms.Reefsalsoprovidecomplexthreedimensionalhabitatsthatareextremelyrichinbiodiversity.It’sthoughtthatasmanyasonemillion speciesoffishandothermarineorganismsliveinandaroundcoralreefs.Reefssustainlivelihoodssuch asfisheriesandtourism,whichsupportanestimated500millionpeoplewholivealongtheworld’s tropicalcoastlines.TheGreatBarrierReefisespeciallyimportanttotheAustralianeconomyand generatesmorethanfivebilliondollarseveryyear. Inaddition,long-livingcoralsthatgrowoverhundredsofyearsareveryusefultoscientists,aschangesin thethicknessandisotopicchemistryofthegrowthbandsintheircalciumcarbonateskeletonscan provideinformationaboutpastclimatesandgrowthandvitalityofcoralsovertime. coral_bleaching.docx 3/16/17 ClimateChangeandCoralBleaching http://www.nova.org.au/coral-bleaching Name: Per: Date: 1. Discussthetermcoral. Explainhowcoralcoloniesareformed. 2. Definemutualismanddescribewhytherelationshipbetweencoralsandalgaerepresentsa mutualism. Explaintheroleandimportanceofalgaetothesurvivalofcoral. 3. Whatiscoralbleaching? Whathappensduringableachingeventandwhyisthisaconcerntoscientists? coral_bleaching.docx 3/16/17 4. Listfivecausesofcoralbleaching. a. b. c. d. e. 5. Explainwhyoceantemperaturesareunusuallywarm? Describehowclimatechangecouldaffectthecoral-algaemutualism. 6. Cancoralssurvivebleaching? 7. Givefourreasonswhycoralreefsareimportant. a. b. c. d. coral_bleaching.docx 3/16/17