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432 Pages·2015·57.622 MB·English
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Discovering the Deep A Photographic Atlas of the Seafloor and Ocean Crust ThedeepoceansandglobalseaflooraretrulyEarth’slastfrontier. cabledobservatory,fundedbytheNSF.SheistheformerChair Theyremainlargelyunexplored,yetarecriticaltooursurvival of the UNOLS Deep Submergence Science Committee. Her onthisplanet.Thismagnificentvolumetransportsyoutovolca- research examines the linkages between submarine volcanoes, noes, boiling hot springs, and fault zones in mountains a mile underwater hot springs and how they support life in the beneaththeoceansurface,wherebizarrelandscapeshostexotic absenceofsunlight.Dr.Kelleyhasparticipatedinover35blue lifeformsthatrivalthemostimaginativesciencefiction. watercruisesroutinelyusingroboticvehicles,andhasbeenon over50Alvindeep-seasubmersibledives,todepthsasgreatas Illustratedthroughoutwithspectacularcolorphotographs,the 4000meters. book starts with a historical summary of seafloor exploration and the developing technologies used to study this extreme Daniel J. Fornari is a marine geologist and Senior Scientist at environment.Itthenpresentsaseriesofchaptersthatdescribe the Woods Hole Oceanographic Institution (WHOI). He was thedistinctivegeologicalcomponentsoftheEarth’soceanfloor thefirstChiefScientistofDeepSubmergenceatWHOI,apast and the myriad environments found along mid-ocean ridges Director of WHOI’sDeep Ocean Exploration Institute (DOEI), wherenewcrustiscreated.Itisherethatdiscoveriesofchemo- and was a Chair of the Ridge 2000 Program, a NSF-funded synthetic biological communities revolutionized our ideas national program studying mid-ocean ridges. Dr. Fornari is about the origins of life and the potential for life’s existence the author or co-author of over 100 research publications and elsewhereintheUniverse.Theauthorsprovideelegantexplan- hasparticipatedinover100researchcruisesandasmanydives ationsofhowthevariousgeologicalandhydrothermalfeatures indeep-seasubmersibles.Hisresearchfocusesonvolcanicand of the seafloor are formed through physical, chemical, and hydrothermal processes along the global mid-ocean ridge, biological processes, and present comparative examples from usingavarietyofsurfaceanddeep-towedsonarsystems,sub- placeswheretheseafloorisexposedonland. mersibles,ROVs,andAUVs. DiscoveringtheDeepisanindispensablereferenceforresearch- Michael R. Perfit is Professor of Geological Sciences at the ers, teachers, and students of marine science, and a visually University of Florida, where he has received several awards stunningresourcethatwillenlightenandintrigueoceanograph- forexcellenceinteaching.Hehasco-authoredmorethan100sci- ersandenthusiastsalike.Asuiteofonlineresources,including entificpublicationsonvolcanismandmagmagenesisatoceanic photographsandvideoclips,combinewiththebooktoprovide spreadingcentersandseamounts.Dr.Perfithasparticipatedin fascinating insights into the hidden world of seafloor geology 30oceanographicresearchcruisesandtakenmorethan35dives and biology using the latest deep-sea imaging and geological inAlvin.HehasservedastheChairoftheDeepSubmergence concepts. ScienceCommittee,andisalsoaFellowoftheGeologicalSoci- ety of America and the American Geophysical Union, and a JeffreyA.KarsonisProfessorofGeologyintheDepartmentof TrusteeoftheConsortiumforOceanLeadership. EarthSciencesatSyracuseUniversityandaFellowoftheGeo- logical Society of America. He investigates the interplay of Timothy M. Shank is an Associate Scientist in the Biology magmatic construction and mechanical deformation of exten- DepartmentoftheWoodsHoleOceanographicInstitutionand sional and transform fault environments from ophiolites, con- Director of WHOI’s Ocean Exploration Institute. His research temporary oceanic crust, Iceland, continental rifts, and focusses on ecological and evolutionary processes that affect continental margins. Professor Karson has participated in ecosystem structure, faunal evolution, and biodiversity in the numerous field projects and seafloor research cruises world- deep sea. Dr. Shank has conducted more than 57 scientific wide. He is the author or co-author of over 150 publications expeditions, using a wide variety of submersibles, ROV and onseafloorspreadingandrelatedphenomena. AUVsystems(includingmorethan50Alvindives).Heiscur- rently the Director of the Hadal Ecosystems Studies Program, DeborahS.KelleyisaProfessorintheSchoolofOceanography pioneeringthefirstresearchuseofthefull-oceandepthhybrid attheUniversityofWashingtonandalsoAssociateDirectorof ROV(Nereus)inthedeepesttrenches. ScienceforthefirstUSunderwaterhigh-power,high-bandwidth Praise for Discovering the Deep “Though it’s fashionable to say we know little about the theEarthandthetechnologyrequiredtoinvestigateit.Not mysteries of the deep, this book shows the vast wealth of sinceBruceHeezenandCharlieHollister’sclassicbook,The understanding that pioneering researchers have already FaceoftheDeep,firstpublishedin1971,haveweseensucha gleaned,withtheirprobingsoundwaves,persistentrobots comprehensivephotographicatlasofwhatliesinthehidden and courageous submariners. This is the book I wish I’d depthsofthesea.” had on my eight deep ocean expeditions, to better under- Dr.RobertD.Ballard,PresidentoftheOcean stand the wonders I was gazing upon. A must-own for ExplorationTrust anyone in the ocean sciences, and for those simply curious “Discovering the Deep is an exquisite synthesis of the com- about what lies down there in the most remote realm on plexityofnaturalprocesses,thebeautyofoftunseenenvir- ourplanet.” onments,andthecriticalscientificdiscoveriesofourrecent JamesCameron,explorerandfilm-maker past. To read this volume is to become an enlightened “DiscoveringtheDeepwillopenyoureyestothelargestand travelerintothefascinatingrealmoftheseafloorandocean most unexplored region on Earth – the global Mid-Ocean crust. No student of the natural world should be without Ridge.MyownintroductiontotheMid-OceanRidgebegan thismagnificentatlasofourplanet’srichlystructureddeep withtheFAMOUSExpeditiontotheMid-AtlanticRidgein oceanenvironment.” 1974, and this beautifully illustrated and comprehensive Dr.KathrynD.Sullivan,UnderSecretaryofCommerce accountshowshowfarwehavecomeoverthelast40years forOceansandAtmosphereandNOAAAdministrator; inourunderstandingofthisfundamentaltectonicfeatureof formerNASAastronaut Discovering the Deep A Photographic Atlas of the Seafloor and Ocean Crust jeffrey a. karson Syracuse University deborah s. kelley University of Washington daniel j. fornari Woods Hole Oceanographic Institution michael r. perfit University of Florida timothy m. shank Woods Hole Oceanographic Institution UniversityPrintingHouse,CambridgeCB28BS,UnitedKingdom CambridgeUniversityPressispartoftheUniversityofCambridge. ItfurtherstheUniversity’smissionbydisseminatingknowledgeinthepursuitof education,learningandresearchatthehighestinternationallevelsofexcellence. www.cambridge.org Informationonthistitle:www.cambridge.org/9780521857185 ©CambridgeUniversityPress2015 Thispublicationisincopyright.Subjecttostatutoryexception andtotheprovisionsofrelevantcollectivelicensingagreements, noreproductionofanypartmaytakeplacewithoutthewritten permissionofCambridgeUniversityPress. Firstpublished2015 PrintedintheSpainbyGrafosSA,Artesobrepapel AcatalogrecordforthispublicationisavailablefromtheBritishLibrary LibraryofCongressCataloginginPublicationdata Karson,JeffreyA. Discoveringthedeepaphotographicatlasoftheseafloorandoceancrust/JeffreyA.Karson, SyracuseUniversity,NewYork,DeborahS.Kelley,UniversityofWashington,DanielJ. Fornari,WoodsHoleOceanographicInstitution,Massachusetts,MichaelR.Perfit,University ofFlorida,TimothyM.Shank,WoodsHoleOceanographicInstitution,Massachusetts. pages cm 1. Oceanbottom–Pictorialworks. 2. Earth(Planet)–Crust–Pictorialworks. I. Title. GC87.K372015 551.460800222–dc23 2014028680 ISBN978-0-521-85718-5Hardback Additionalresourcesforthispublicationatwww.cambridge.org/discoveringthedeep CambridgeUniversityPresshasnoresponsibilityforthepersistenceoraccuracyof URLsforexternalorthird-partyinternetwebsitesreferredtointhispublication, anddoesnotguaranteethatanycontentonsuchwebsitesis,orwillremain, accurateorappropriate. Contents ForewordbyPaulJ.Fox pageviii 2.4 Unveilingtheoceaniclithosphere 38 Preface:NewviewsofEarthfrombelowtheoceans ix 2.5 Geophysicalframeworkofseafloor Acknowledgments xv spreading 39 2.6 Compositionoftheoceaniccrust 41 1 Entering the abyss: oceanographic technology 1 2.7 Directaccesstotheoceaniccrust 43 2.8 Unravelinggeologyontheseafloor 45 1.1 Firstencounters 1 2.9 Deepcrustaldrilling 46 1.2 Acousticimaging 4 1.2.1 Echosounding 4 2.10 Oceaniccrustandmantleonland 49 1.2.2 Satelliteoceanography 5 2.11 Linkingophiolitestooceaniclithosphere 50 1.2.3 Multibeamsonar 6 2.12 Cross-pollinationofdataandconcepts 51 1.2.4 Sidescansonar 7 1.3 Twentieth-centurydevelopmentsin 3 Diversity in seafloor spreading 56 deep-seaopticalimagingtechnology 10 3.1 Seafloorspreading:afirst-orderglobal 1.4 Submergencevehicles 16 process 56 1.4.1 Human-occupiedvehicles 16 3.2 Magmabudget:keytovariabilityalong 1.4.2 Tetheredroboticvehicles 18 theMORsystem 58 1.4.3 Autonomousunderwatervehicles 18 3.3 Diversemorphologiesofspreadingcenters 59 1.4.4 Hybridremotelyoperatedvehicles 22 3.3.1 Fast-spreadingMORs 59 1.5 Seismicmonitoringandimaging 22 3.3.2 Slow-spreadingMORs 60 1.5.1 Revealingthedetailsofcrustaland 3.3.3 Intermediate-spreadingMORs 60 uppermantlestructureatMORsusing 3.3.4 MORsegmentation 60 multichannelseismictechniques 22 3.4 Componentsofspreadingsystems 63 1.5.2 Ocean-bottomseismometers 24 3.4.1 Neovolcaniczone 63 1.5.3 Recordingseismicityalongtheglobal 3.4.2 MORfaults 67 MORaxisusingautonomous 3.4.3 Oceaniccorecomplexes 69 hydrophonesandtheSOFAR 3.4.4 Transformfaults 71 channel 25 3.4.5 Propagatingrifts 73 1.6 Oceandrilling:probingintotheseafloor 28 3.4.6 Microplates 75 1.7. Real-timeaccesstotheoceanrealm: 3.5 Internalstructureoftheoceaniccrust 75 oceanobservatories 29 3.5.1 Uppercrust 76 1.8 Telepresence:seagoingparticipationand 3.5.2 LowercrustandMohotransitionzone 77 researchthroughtheInternet 32 3.5.3 Uppermantle 83 3.6 Seafloorspreading:fastandslow 84 2 Earth beneath the sea 35 2.1 AnewunderstandingofEarthandocean 4 Hydrothermal vents 87 history 35 4.1 Oasesofthedeep 87 2.2 Seafloorspreading:aconsequenceofplate 4.1.1 Fluidoverturnintheoceaniccrust 90 tectonics 36 4.1.2 Themetamorphosisofseawaterto 2.3 Continentaldrift,“geopoetry,”andseafloor hydrothermalfluidsinunderwater spreading 37 volcanoes 93 ● vi CONTENTS 4.1.3 Formationofblacksmokerchimneys 95 4.10.3 Sulfidechimneys 167 S T 4.1.4 Boilingfluidsinandattheseafloor 97 4.10.4 Extinctdeposits 168 N TE 4.1.5 Gasesfromthedeep 99 4.10.5 Dikingevents,seismicity,and N O 4.1.6 Impactofvolcaniceruptions 99 hydrothermalflow 170 C 4.1.7 Oceaniccrust,tectonics,andvent 4.10.6 The1999–2000dikingevent 171 diversity 103 4.10.7 The2005dikingevent 172 4.1.8 Lifeintheextreme:microbesof 4.10.8 Firstreal-timemonitoringof thedeep 105 geophysical,chemical,andbiological 4.1.9 Chemosynthesisandthemetabolic processes 174 menu 107 4.11 AxialSeamount:robustvolcanismonthe 4.1.10 Lifeintheextreme:ventfauna 108 JuandeFucaRidge 177 4.2 Arcticridges:fireandice 111 4.11.1 AxialSeamounteruptions 180 4.2.1 GrimseyField,northofIceland 112 4.11.2 Shallowhydrothermalventsites 182 4.2.2 Trollveggen(TrollWall)Field,Mohns 4.11.3 Boilingfluids 183 Ridge 112 4.11.4 Eruptionsandbiologicalcolonization 185 4.2.3 SoriaMoriaField,MohnsRidge 112 4.11.5 Wiringanactivesubmarinevolcano 186 4.2.4 Lokeslottet(Loki’sCastle)Field 113 4.12 GuaymasBasin:ventingatsedimented 4.2.5 Arcticventfauna 113 ridges 187 4.3 MenezGwen:ashallowventsystemon 4.12.1 GuaymasTroughandventing 189 theMAR 117 4.12.2 Microbiallifeinsedimentedsystems 190 4.4 Luckystrike:hot-spotinfluencedvent 4.12.3 Faunainhydrocarbon-rich systems 121 environments 191 4.4.1 Hydrothermalventing 122 4.13 EastPacificRise:thefastestspreading 4.4.2 Animalcommunities 125 centeronEarth 193 4.5 Rainbow:hybridgabbroic-and 4.13.1 Evolutionoffast-spreading ultramafic-hostedvents 127 hydrothermalsystems 197 4.13.2 RelationshipsbetweenEPR 4.5.1 Carbondioxide-,hydrogen-, hydrothermalventsandbiological andmethane-enrichedfluids 127 communities 199 4.5.2 Animalcommunities 129 4.14 GalápagosSpreadingCenter:firstvent 4.6 Lostcity:anewkindofventfield 131 4.6.1 LostCitygeology 131 discoveryonaspreadingcenter 204 4.14.1 Ventactivity 204 4.6.2 Anancientfield 133 4.14.2 Discoveryofhigh-temperaturevents 205 4.6.3 Alkalinefluidsrichinhydrocarbons 134 4.14.3 RosebudandCalyfieldVentFields 207 4.6.4 Lifeinhigh-pHsystems 141 4.14.4 UkaPachaandPegasusVentFields 209 4.6.5 ArarebiosphereatLostCity 142 4.6.6 Macrofaunalcommunities 142 4.14.5 TempusFugitVentField 210 4.15 CentralIndianRidge:anewbiogeographic 4.7 TAG:thelargestfieldknown 145 province 211 4.7.1 TheTAGmound 146 4.15.1 KaireiVentField 211 4.7.2 Long-livedventing 146 4.15.2 EdmondVentFeld 213 4.7.3 Aggregatingshrimp 149 4.15.3 KaireiversusEdmondfauna 215 4.8 Logatchev:ultramafic-influencedventsites 150 4.8.1 Hydrothermalventing 153 5 Submarine volcanism: fire beneath 4.8.2 LifeinhighCO ,CH ,andH systems 154 2 4 2 the sea 217 4.9 SouthAtlantic:extremeventtemperatures 156 5.1 Volcanoesonlandandunderthesea 217 4.9.1 SMARventfauna 159 5.2 Submarinelavas 218 4.10 Endeavour:oneofthemost remarkableplaces 162 5.3 Historicalperspectives 220 4.10.1 Endeavourgeology 164 5.4 Directobservationsofthelavaunits 4.10.2 Ventfields 165 fromtectonicwindowsandcrustaldrilling 220 ● CONTENTS vii 5.5 Seafloorvolcanoesalongthemid-oceanridge 225 7.3 Deformationandmetamorphisminthe C 5.6 Submarinelavamorphologies 228 middletoloweroceaniccrust 295 O N 7.3.1 Oceaniccrustalmetamorphism 297 T 5.7 Eruptionsontheseafloor 235 E 7.3.2 Hydrothermalmetamorphism 298 N T 5.8 Mid-oceanridgelavageochemistry S 7.3.3 Deformationandmetamorphismin andmagmaticprocesses 238 oceaniccorecomplexes 299 5.9 CompositionalvariabilityofMORB 241 7.4 Petrology,geochemistry,andmagmatic 5.10 CrystalsinMORB 245 processesinoceanicgabbros 300 5.11 GeneratingMORBmagma 247 7.4.1 Petrology 301 7.4.2 Gabbrogeochemistry:decipheringthe 5.12 Historicsubmarineeruptions 247 chemicalfingerprintsofmagmatic 6 Dike intrusion and sheeted dike processes 301 complexes 255 7.5 Gabbroicrocksinophiolites 304 7.5.1 Sheeteddike–gabbrocontactin 6.1 Seafloorspreading:onemeteratatime 255 ophiolites 305 6.2 Dikesbeneaththeseafloor 258 7.5.2 Internalstructureofgabbroicand 6.2.1 Dikesandsheeteddikesincrust relatedrocksinophiolites 306 formedatfasttointermediaterates 260 7.5.3 GeologicalexpressionsoftheMoho 310 6.2.2 Dikesandsheeteddikesin 7.6 Buildingthemiddletoloweroceaniccrust 313 slow-spreadingcrust 266 6.2.3 DikesandsillsatsedimentedMORs 267 8 Peridotites: windows into mantle 6.3 Petrologyandgeochemistryofsheeteddike processes 317 complexes 267 8.1 BelowtheMoho:theoceanicmantle 317 6.4 Metamorphisminsheeteddikes 271 8.2 Mantlerocks 318 6.5 Dikesandsheeteddikecomplexesonland 272 8.3 Peridotiteexposuresontheseafloor 319 6.5.1 Generalformandinternalstructure 8.3.1 Peridotitesfromsuperfast-to ofdikes 273 intermediate-ratespreadingcenters 323 6.5.2 Internalstructureofdikeswarms 8.3.2 Peridotitesfromslow-to andsheeteddikecomplexes 275 ultraslow-spreadingMORs 324 6.5.3 Contacts:linkingthelavaandgabbroic units 278 8.4 Serpentinizationontheseafloor 328 6.6 Dikeintrusionalongspreadingcenters 282 8.5 Peridotitesinophiolites 331 6.6.1 Dikeintrusioneventsinspreading 8.6 Peridotitepetrologyandgeochemistry 332 environments 282 8.6.1 Peridotitemineralogyandphasechemistry 335 6.7 Accretionoftheupperoceaniccrustfrom 8.6.2 Peridotitegeochemistry 336 sheeteddikes 283 8.7 Evolutionoftheoceanicmantlelithosphere 338 8.8 Meltgenerationandtransport 338 7 Gabbroic rocks: clues to magmatic processes 286 9 Future research 342 7.1 Thefoundationoftheoceaniccrust 286 Abbreviations 346 7.2 Plutonicrockexposuresontheseafloor 289 Figurecredits 347 7.2.1 GabbrosfromfasttointermediaterateMORs 290 References 355 7.2.2 Gabbrosfromslow-spreadingMORs 294 Index 401 Foreword AnalienapproachingEarthforthefirsttimewouldobserve Earthlive.SpanningenvironmentsfromtheArctic,Atlantic, a watery planet but would have no clue as to what lies Pacific,andIndianOceans,theauthorsprovidecaptivating beneath the blue-gray liquid surface. This book unveils images of these seafloor oases, which host novel microbes andilluminates,inwaysneverbeforepossible,thathidden that use toxic gases rising from Earth’s interior as their world and the astounding processes that occur at the energysource. seafloorandwithintheoceaniccrust.Drawingfromunpar- Theauthorshavesucceededinpresentingaholisticview alleledimageryanddatafromtwenty-firstcenturytechnol- of the oceanic crust from top to bottom. They present the ogy, which includes human-occupied and robotic vehicles, current state of knowledge on the complex and beautiful sophisticatedsensorsandanalyticaltechniques,theauthors formsofvolcanicflowsthatpavethemid-oceanridgecrest havesucceededin“pullingtheplug”ontheglobaloceanso tothemassivebasallayersofintrusive,plutonic,andultra- that the awe-inspiring terrane of the ocean floor and pro- maficrocksthatuntilrecentlyhavebeendifficulttosample cessesthatformitarerevealed. andplaceintheirpropergeologicalcontext.Thevariations Itwas44yearsagothatBruceHeezenandCharlesHoll- instyleandstructuralcomplexityoftheseprimaryunitsare ister publishedtheir seminalbook,TheFaceofTheDeep,an nowknowntobecriticaltotheconstructionofallmid-ocean engaging and informative text that used analog seafloor ridges, from ultra-slow to fast, and the hydrothermal photographstohighlightandinterpretthemyriadprocesses systemsandlifethattheysupport.Thisworkendswithan operatingintheglobalabyss.DiscoveringtheDeepsetsanew important look towards the future and new technologies benchmark for a comprehensive treatise about visualizing that will be required to address upcoming opportunities the seafloor, how ocean crust forms, and the amazing life andchallengesinunderstandingthevastoceansthatmake forms that thrive in one of the most extreme environments Earthhabitable. on Earth – submarine hot springs. It presents up to date, The five authors of this atlas are all recognized as indi- integrated multidisciplinary concepts about the mid-ocean viduals who have made significant contributions to our ridge and its role in plate tectonics and developing the understanding of the mid-ocean ridge system. They have architectureoftheoceaniccrust.Theauthorsalsosynthesize succeeded in synthesizing the many different, but comple- published data from mid-ocean ridge analogs on land – mentary data sets – weaving together a text that elegantly ophiolites – to better understand how oceanic crust is gen- takes the reader on a journey from hydrothermal vents erated and the far-reaching implications of these processes down through the oceanic crust. They tell a story that is forinterpretingEarthandoceanhistory. entertaining, illuminating, and scholarly. For a layperson AsastudentofHeezen,acontemporaryofHollister,and interested in learning more about fundamental planetary someonewhohasspentmostofhiscareerstudyingthemid- process, a student of marine geology just embarking on a ocean ridge using ships and the submersible Alvin, I was career, or a seasoned investigator of oceanic crustal pro- drawn into all aspects of this compelling and masterful cesses,thisatlasoftheseafloorandoceaniccrustissureto synthesis, especially the high-resolution images of mid- expand horizons and enrich understanding of how our ocean ridge volcanic and hydrothermal terranes and biota. planetworksforallreaders. The more than 500 stunning images of the seafloor, many neverbeforepublished,weretakenusingthelatestindeep- paulj.fox seadigitalcameraandlightingtechnology.Theremarkable ProfessorEmeritus images provide glimpses of underwater eruptions where DepartmentofGeology&Geophysics molten rock turns to glass almost instantly, and black- TexasA&MUniversity smoker vents where the most exotic life forms known on McLeod,Montana

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Most books are stored in the elastic cloud where traffic is expensive. For this reason, we have a limit on daily download.