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EarthWillSurviveGlobalWarming,ButWillWe?
Thenotionthathumanactivity,ortheactivityofanyorganism,canaffectEarthonaplanetaryscaleisstillahardoneformanypeopletoswallow.Anditisthiskindofdisbeliefthatfuelsmuchofthepublicskepticismsurroundingglobalwarming.
ApollconductedlastsummerbythePewResearchCenterfoundthatonly41percentofAmericansbelievetheburningoffossilfuelscausesglobalwarming.ButinameetingthisweekinParis,officialsfrom113nationshaveagreedthatahighlyanticipatedinternationalreportwillstatethatglobalwarmingwas"
verylikely"
causedbyhumanactivity.Theideathatbiologycanaltertheplanetinbroadanddramaticwaysiswidelyacceptedamongscientists,andtheypointtoseveralprecedentsthroughoutthehistoryoflife.
Themightymicrobes
Human-causedglobalwarming--alsocalled"
anthropogenic"
globalwarming--isthelatestexampleoflifealteringEarth,butitisnotthemostdramatic.
ThattitleprobablygoestotheoxygenationofEarth'
searlyatmospherebyancientmicrobesastheybegantoharnessthepowerofsunlightthroughphotosynthesis(光合作用).
Humans"
arehavingastrongeffectonglobalgeochemicalcycles,butitdoesnotcompareatalltotheadventofoxygenicphotosynthesis,"
saidKatrinaEdwards,ageo-microbiologistattheUniversityofSouthernCalifornia(USC)."
Thatwasacatastrophicenvironmentalchangethatoccurredbefore2.2billionyearsagowhichwreakeditsfullwrathontheEarthsystem."
Edwardsstudiesanotherwaylifeimpactstheplanetinlargelyunseenways.Shefocusesonhowmicrobeslivingonthedarkoceanfloortransformmineralsthroughakindofunderwaterpower.
"
Thesemicrobesarecompletelyoffradarintermsofglobalbiogeochemicalcycles,"
EdwardstoldLive-Science."
Wedon'
tconsiderthemaspartoftheEarthsystemrightnowinourcalculationaboutwhat'
sgoingon,andwedon'
tconsiderthemintermsofhowtheEarthsystemwillmoveforwardintothefuture."
Thesereactionsarestronglyinfluencedbylifeandhavebeenoccurringforbillionsofyears,foraslongastheoceanshavebeenoxygenatedandtherehavebeenmicrobesinhabitingtheseafloor,Edwardssaid.
CreatingEarth
Onland,microbes,andinparticularaformofbacteriacalledcyanobacteria(固氮蓝藻),helpkeepsoilinplaceandsuppressdust.
We'
dcertainlyhavemoreduststormsanditwouldnotbeanywhereasniceonEarthiftheyweren'
taround,"
saidJayneBelnap,aresearcherwiththeUnitedStatesGeologicalSurvey.
Scientistsbelievethetinylife-formsperformedthesamerolesonearlyEarth."
Oneofthebigproblemsforgeologistsisthat,OK,youhavethisbigballofrock,thesoilisweatheringoutandyouhavetheseferociouswinds.Whatintheworldisholdingthesoilinplaceasitweathersoutoftherocks?
"
Belnapsaidinatelephoneinterview."
Cyanobacteriaarealsocreditedwiththatfunction."
Themicrobesanchoredsoiltotheground;
thiscreatedhabitatsforlandplantstoevolveandeventuallyforustoevolve."
TheyliterallycreatedEarthinasense,"
Belnapsaid.
Cyanobacteriaarejustlike'
it'
"
shecontinued."
I'
vebeentellingeverybodytomakeasmallaltarandoffersacrificeseverynight.Weowethemeverything."
Asnowballplanet
Themightymicrobesalsotriggeredsuddenclimaticshiftssimilartowhathumansaredoingnow.Recentstudiessuggestthattheproliferationofcyanobacteria2.3billionyearsagoledtoasuddeniceageandthecreationofa"
SnowballEarth."
Astheycarryoutphotosynthesis,cyanobacteriabreakapartwaterandreleaseoxygenasawasteproduct.Oxygenisoneofthemostreactiveelementsaround,anditsreleaseintotheatmosphereinlargeamountsdestroyedmethane(沼气),agreenhousegasthatabsorbedthesun'
senergyandhelpedkeepourplanetwarm.
SomescientiststhinkthedisappearanceofthismethaneblanketplungedtheplanetintoacoldspellsoseverethatEarth'
sequatorwascoveredbyamile-thicklayerofice.
Earthmightstillbefrozentodayifnotfortheappearanceofnewlifeforms.Asorganismsevolved,manydevelopedtheabilitytobreatheoxygen.Intheprocess,theyexhaledanothergreenhousegas,Carbondioxide,whicheventuallyice-outtheworld.Thatwasthefirstbiologicallytriggerediceage,butothersfollowed,saidRichardKopp,aCaltechresearcherwhohelpedpiecetogethertheSnowballEarthscenario.
Anewleaf
Whentreesfirstappearedabout380millionyearsago,theyalsodisturbedEarth'
satmosphericbalance.
Unlikeanimals,plantsbreatheincarbondioxideandexpeloxygen.Treestransformsomeofthatatmosphericcarbonintolignin(木质素)--themajorconstituentofwoodandoneofthemostabundantproteinsontheplanet.Ligninisresistanttodecay,sowhenatreedies,muchofitscarbonbecomesburiedinsteadofreleasedbackintotheatmosphereascarbondioxide.LesscarbondioxideintheatmospherethinstheblanketofgasesthatkeepsEarthwarm,andthatcoolingeffectcantriggerglobalcooling,possiblyevenaniceage.
Therewassomeglaciationthatstartedaroundthatperiodthatwasdrivenatleastinpartbytheevolutionoflandplants,"
Koppsaidinatelephoneinterview.
Treesalsoaffectedtheglobalcarboncycleinanotherindirectway.Astheytunnelthroughtheground,treerootsbreakdownsilicaterocksintosedimentandsoil.Silicaterockcontainslargeamountsofcalciumandmagnesium(镁).Whentheseelementsareexposedtoair,theyreactwithatmosphericcarbondioxidetoformcalciumcarbonate(碳酸盐)andmagnesiumcarbonate,compoundsthatarewidespreadonEarth.
Thehumandifference
ThoughitmightseemasifhumansaremerefleasalongforarideonthebackofanimmenseanimalcalledEarth,ourintelligence,technologyandsheernumbersmeanourspeciespacksapunchthatcanshaketheworldinwildways.
Whilewearenotthefirstspeciestodrasticallyalterourplanet,ourinfluenceisuniqueinanumberofways,scientistssay.
Foronething,humanshavedevelopedlarge-scaleindustry,saidSpencerWeart,asciencehistorianattheAmericanInstituteofPhysics."
Wearecapableofmobilizingthingsbeyondourownbiology,"
Weartsaid."
Iemitacertainamountofcarbondioxide,butmyautomobileemitsfarmore."
AnotheristherateatwhichhumansarewarmingEarth.
Humansarethemostcommonlargeanimaltoeverwalktheplanet,"
saidKirkJohnson,achiefcuratorattheDenverMuseumofNature&
Science:
Population,plusbrainpowerandtechnology,isapotentcombinationandtheresultisthathumansareeffectingchangeatveryhighrates."
Belnapagrees."
Idon'
tthinkwe'
vefundamentallychangedanyprocess.We'
vejustcrankedupthespeed,"
shesaid."
Wehaven'
tintroducedanythingnew.We'
vejustchangedhowfastorslowithappens,andmostlyfast."
Butnomatterhowhighhumanscausethetemperaturetoriseandhowmuchdamagewedototheplanet,Earthandlifewillsurvive,scientistssay.Itjustmightnolongerbeintheformwepreferortheformthatallowsustothrive.
WhatweneedtobethinkingofashumanscausingchangestotheEarthsystemiswhattheconsequenceswillbetoushumanbeings,"
saidEdwards,theUSCgeo-microbiologist."
TheEarthcouldcareless.WewillberecordedasaminorchaosintheEarthsystem.TheEarthwillgoon.Thequestionis:
Willwe?
1.Accordingtotheworldwidereport,whatisthemainreasonforglobalwarming?
A)Americanpeople.B)People'
sactivity.
C)Industryactivity.D)Developedcountries.
2.Thephotosynthesisbyancientmicrobesisanexampleof______.
A)thechangeofEarthB)thelonghistoryofEarth
C)thelife'
sinfluencesonEarthD)thepowerofsunlight
3.AccordingtoEdwards,themicrobesarenow______.
A)recognizedbymostpeopleB)neglectedbymostpeople
C)diedoutfromtheEarthD)outofactionoftheEarthsystem
4.Whatisthemainfunctionofcyanobacteria?
A)Tomakemoreduststorms.B)Tokeepthesoilflying.
C)Tokeepthesoiltotheground.D)Tocreatemorerocks.
5.TokeeptheEarthoutofwarm,wecandestroytheMethanewith______.
A)greenhousegasB)sunlight
C)waterD)oxygen
6.Theearthisunfrozentodaywiththeappearanceof______.
A)themethaneblanketB)amile-thicklayerofice
C)newlifeformsD)thecarbondioxide
7.Differentfromanimals,thetreesinfluencetheearth'
satmosphereby______.
A)expellingcarbondioxidefromtheirleaves
B)expellingoxygenfromtheirleaves
C)directlyreducetheblanketofgases
D)turningsomecarbondioxideintolignin
8.Treescanindirectlyhelptheexpositionofcalciumandmagnesiumwiththeirroots______.
9.Eventhoughnotthefirsttoinfluencetheearth,thehumanisstillalteringtheplanetin______.
10.Undertheinfluenceofhightemperatureandmuchdamagecausedbythehuman,Earthandlifewill______.
PartⅢListeningComprehension(35minutes)
SectionA
Inthissection,youwillhearSshortconversationsand2longconversations.Attheendofeachconversation,