Verfügbarkeit: Earth system history

Earth system history:

Gespeichert in:

Bibliographische Detailangaben
Hauptverfasser:	Stanley, Steven M. 1941- (VerfasserIn), Luczaj, John A. (VerfasserIn)
Format:	Buch
Sprache:	English
Veröffentlicht:	New York, NY W.H. Freeman and Company 2015
Ausgabe:	Fourth edition
Schlagworte:	Historical geology Physical geology Geologie Historische Geologie Geodynamik Paläogeografie Paläontologie Lehrbuch
Online-Zugang:	Inhaltsverzeichnis
Beschreibung:	Previous edition: 2009 Includes bibliographical references and index
Beschreibung:	XXVI, 587 Seiten Illustrationen, Diagramme, Karten 28 cm
ISBN:	9781429255264 9781319154028

Internformat

MARC


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245	1	0	\|a Earth system history \|c Steven M. Stanley ; John A. Luczaj
250			\|a Fourth edition
264		1	\|a New York, NY \|b W.H. Freeman and Company \|c 2015
300			\|a XXVI, 587 Seiten \|b Illustrationen, Diagramme, Karten \|c 28 cm
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500			\|a Previous edition: 2009
500			\|a Includes bibliographical references and index
650		4	\|a Historical geology
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Datensatz im Suchindex

_version_	1804152313411010560
adam_text	PREFOCE PART I L{ATERIALS, PROTESSEL, AND PRINCIPLES (IIAPTTR I EARTH AS A SYSTEM EXPLORING THE EARTH SYSTEM EARTH IS A SPECIAL PLANET THE COMPONENTS OF THE EARTH SYSTEM ARE INTERRELATED ASPECTS OF THE EARTH SYSTEM ARE FRAGILE THE PRINCIPLE OF ACTUALISM GEOLOGISTS CONDUCT RESEARCH BASED ON ACTUALISM ACTUALISM REPLACED CATASTROPHISM IN THE NINETEENTH CENTURY THE NATURE AND ORIGIN OF ROCKS IGNEOUS, SEDIMENTARY AND METAMOLPHIC ROCKS CAN FORM FROM ONE ANOTHER BODIES OF ROCK ARE CLASSIFIED INTO FORMAL UNITS STENO S THREE PRINCIPLES CONCERN SEDIMENTARY ROCKS THE ROCK CYCLE RELATES ALL KINDS OFROCKS TO ONE ANOTHER GLOBAL DATING OF THE ROCK RECORD FOSSILS AND PHYSICAL MARKERS INDICATE THE RELATIVE AGES OFROCKS RADIOMETRIC DATINGPROVIDES ACTUAL AGES OF ROCKS THE GEOLOGIC TIME SCALE DIVIDES EARTH S HISTORY INTO FORMAL UNITS INTERVALS OF THE GEOLOGIC TIME SCALE ARE DISTINCTIVE LMAGING EARTH BELOW EARTHH DENSITY INCREASES WITH DEPTH SOLID, BRITTLE PLATES OF LITHOSPHERE MOVE OVER THE SEMISOLID ASTHENOSPHERE PLATE TECTONICS PLATES SPREAD APART WHERE THEY FBRM, SLIDE PAST ONE ANOTHER, AND EVENTUALLY SINK HEAT FROM RADIOACTIVE DECAY FIRES THE ENGINE OI PLATE TECTONICS X-LX PLUMES OF MAGMA RISE INTO THE CRUST FROM DEEP WITHIN THE MANTLE 17 PLATE TECTONICS PLAYS A ROLE IN THE ROCK CYCLE 17 THE WATER CYCLE WATER MOVES BETWEEN RESERVOIRS THE WATER CYCLE AND THE ROCK CYCLE ARE INSEPARABLE DIRECTIONAL CHANGE IN EARTH S HISTORY EVOLUTION RESHAPES LIFE DRASTICALLY AND THE STRUCTURE OF MINERALS AN ELEMENT CONSISTS OF A UNIQUE KIND OF ATOM ISOTOPES OF AN ELEMENT HAVE DISTINCTIVE ATOMIC WEIGHTS CHEMICAL REACTIONS PRODUCE MINERALS CHEMICAL REACTIONS CREATE CHEMICAL BONDS CRYSTALS HAVE THREE-DIMENSIONAL MOLECULAR STRUCTURES IONS OF AN ELEMENT CAN SUBSTITUTE FOR IONS OF ANOTHER SIMILAR ELEMENT THE PROPERTIES OF MINERALS CHEMICAL BONDS DETERMINE HARDNESS THE WEIGHT AND PACHNG OF ATOMS DETERMINE DENSITY FRACTURE PATTERNS REFECT CRYSTAL STRUCTURE MINERALS AND ROCKS FORM UNDER PARTICULAR PHYSICOCHEMICAL CONDITIONS 31 31 32 32 32 32 32 18 18 19 I9 1 2 2 2 2 .) ,) IRREVERSIBLY 20 PHYSICAL AND CHEMICAL FEATURES OF EARTH HAVE ALSO CHANGED 20 LIFE AND ENVIRONMENTS HAVE CHANGED IN CONCERT 20 EPISODIC CHANGE IN EARTH S HISTORY ZL SEDIMENTATION OCCURS IN PULSES 2L DEPOSITION CAN BE CATASTROPHIC 2L UNCONFORMITIES REPRESENT LARGE BREALA IN THE ROCK RECORD 22 LIFE ON EARTH HAS EXPERIEACEDPULSES OF CHARGE 22 (HAPTER SUMMARY/REVIEW QUELTIONL ZS 4 5 5 8 I I T0 10 I1 11 T2 L3 13 L4 15 15 T7 28 28 28 29 29 FLTAPTFL I ROCK-FORMING MINERALS AND ROCKS A FEW FAMILIES OF MINERALS FORM MOST ROCKS TLPES OF ROCKS IGNEOUS ROCKS FORM WHEN MOLTEN ROCK COOLS SEDIMENTARRY ROCKS FORM FROM PARTICLES THAT SETTLE THROUGH WATER OR AIR METAMOQPHIC ROCKS FORM FROM OTHER ROCKS AT HIGH TEMPERATURES AND PRESSURES [LRPTER !UMMARYLIEVIEW QUESTIONL UEIAEPTTR } THE DIVERSITY OF LIFE FOSSILS AND CHEMICAL REMAINS OF ANCIENT LIFE HARD PARTS ARE THE MOST COMMONLY PRESERVED FEATURES OF ANIMALS SOFT PARTS OF ANIMALS ARE RARELY PRESERVED PERMINERALIZATION PRODUCES PETRIFIED WOOD MOLDS AND IMPRESSIONS ARE IMPRINTS TRACE FOSSILS ARE RECORDS OF MOVEMENT THE QUAL§ OF THE FOSSIL RECORD IS HIGHLY VARIABLE BIOMARKERS ARE USEFUL CHEMICAL INDICATORS OF LIFE DEAD ORGANISMS DECAY TO FORM FOSSIL FUELS TAXONOMIC GROUPS LDENTI{YING CLADES AND THEIR RELATIONSHIPS ARCHAEA AND BACTERIA: THE TWO DOMAINS OF PROKARYOTES ARCHAEA CAN TOLERATE HOSTILE ENVIRONMENTS BACTERIA INCLUDE DECOMPOSERS, PHOTOSYNTHESIZERS, CAUSES OF DISEASE, AND POLLUTERS THE PROTISTS: A PARAPHYLETIC GROUP OF EUKARYOTES GREEN ALGAE AND LAND PLANTS SEEDLESS VASCULAR PLANTS CAME FIRST SEED PLANTS INVADED DRY LAND OPISTHOKONTS: FUNGI AND ANIMALS FUNGI ARE DECOMPOSERS ANIMALS ARE MULTICELLULAR CONSUMERS SPONGES ARE SIMPLE INVERTEBRATES CNIDARIANS INCLUDE THE CORALS LOPHOTROCHOZOANS INCLUDE MANY HNDS OF ANIMALS THAT LACK SKELETONS ECDYSOZOANS HAVE AN EXTERNAL SKELETON 35 JA JD 3B THE DEUTEROSTOMES INCLUDE INVERTEBRATES AS WELL AS VERTEBRATES (HAPTER SUMMARY/REVIEW QUESTIONS (IIAPTTR I ENVIRONMENTS AND LIFE PRINCIPLES OF ECOLOGY A SPECIES NICHE IS ITS POSITION IN THE ENVIRONMENT A COMMUNITY OF ORGANISMS AND ITS ENVIRONMENT FORM AN ECOSYNTEM 83 BIOGEOGRAPHY IS THE STUDY OFBROAD PATTERNS OFOCCURRENCE 85 THE ATMOSPHERE 85 NITROGEN, OXYGEN, AND CARBON DIOXIDE CONSTITUTE MOST OF THE ATMOSPHERE 85 TEMPERATURE VARIATIONS AND EARTH S ROTATION GOVERN CIRCULATION IN THE ATMOSPHERE 86 THE TERRESTRIAL REALM 88 VEGETATION PATTERNS PARALLEL CLIMATIC ZONES 88 CLIMATES CHANGE WITH ELEVATION 91 LAND AND WATER INFLUENCE SEASONAL TEMPERATURE CHANGE 92 FOSSIL PLANTS REFLECT ANCIENT CLIMATIC CONDITIONS 94 THE MARINE REALM 95 WINDS DRIVE CURRENTS AT THE OCEAN S SURFACE 95 MARINE LIFE VARIES WITH WATER DEPTH 96 MARINE LIFE FLOATS, SWIMS, OR OCCUPIES THE SEAFLOOR 98 WATER TEMPERATURE INFLUENCES BIOGEOGRAPHIC PATTERNS 100 SALINITY IS AN IMPORTANT LIMITING FACTOR NEAR SHORE FRESHWATER ENVIRONMENTS (HAPTER 5UMMARY/REVIEW QUESTIONS NONMARINE ENVIRONMENTS ANCIENT SOILS CAN POINT TO PAST CLIMATIC CONDITIONS FRESHWATER LAKES AND GLACIERS LEAVE CLUES TO ANCIENT CLIMATES DESERTS AND ARID BASINS ACCUMULATE SALT AND SAND IT) 77 B2 83 45 47 49 52 52 52 53 DJ 54 54 54 54 55 57 61 61 61 62 64 66 66 67 67 67 67 68 69 7L 101 101 RO2 R06 106 L07 FITMIIR T SEDI MENTARY ENVIRONMENTS 109 BRAIDED AND MEANDERING RIVERS DEPOSIT SEDIMENT IN MOIST REGIONS MARGINAL MARINE AND OPEN-SHELF ENVIRONMENTS A DELTA FORMS WHERE A RIVER MEETS THE SEA LAGOONS HE BEHIND BARRIER ISLANDS OF SAND OPEN-SHELF DEPOSITS INCLUDE TEMPESTITES FOSSILS SERVE AS INDICATORS OF MARINE ENVIRONMENTS ORGANIC REEFS ARE BODIES OFCARBONATE ROCK CARBONATE PLATFORMS FORRR IN WARM SEAS DEEP-SEA ENVIRONMENTS TURBIDITY CURRENTS FLOW DOWN SUBMARINE SLOPES PELAGIC SEDIMENTS ARE FINE-GRAINED AND ACCUMULATE SLOWLY (HAPTER SUMMARY/REVIEW QUESTIONS (I{APTTR 6 CORRELATION AND DATING OF THE ROCK RECORD THE CEOLOGIC TIME SCALE FOSSIL SUCCESSION REVEALED THE RELATIVE AGES OF ROCKS GEOLOGIC SYSTEMS WERE FOUNDED IN THE NINETEENTH CENTURY STRATIGRAPHIC UNITS THE ROCK RECORD LS DIVIDED INTO TIME-ROCK UNITS AND GEOLOGIC TIME INTO TIME UNITS BIOSTRATIGRAPHIC UNITS ARE BASED ON FOSSIL OCCURRENCES MAGNETIC STRATIGRAPHY IDENTIFI ES POLARITY TIME-ROCK UNITS ROCK UNITS ARE DEFINED BY LITHOLOGY, NOT AGE EARTH S ABSOLUTE AGE EARLY GEOLOGISTS UNDERESTIMATED EARTH S ANTIQUITY RADIOACTIVE DECAY PROVIDES ABSOLUTE AGES OF ROCKS FOSSILS OFTEN PROVIDE MORE ACCURATE CORRELATION THAN RADIOMETRIC DATING CHANGES IN STABLE ISOTOPES PERMIT GLOBAL CORRELATION EVENT STRATIGRAPHY MARKER BEDS ALLOR,V CORRELATION OVER WIDE AREAS BACK-AND-FORTH SHIFTING OF FACIES BOUNDARIES CREATES A TIME LINE FOR CORRELATION UNCONFORMITIES CAN BE DETECTED BY SEISMIC STRATIGRAPHY SEQUENCES RECORD CHANGES IN SEA LEVEL CHANGES IN EARTH S ROTATION AND THE SHAPE OF ITS ORBIT CREATE GEOLOGIC CLOCKS (HAPTER SUMMARY/REVIEW QUESTIONS (IIFIPTTR I EVOLUTION AND THE FOSSIL RECORD ADAPTATIONS CHARLES DARWIN S CONTRIBUTION THE VOYAGE OF THE BEAGLE PROVIDED GEOGRAPHIC EVIDENCE FOR EVOLUTION DARWIN S ANATOMICAL EVIDENCE FOR E.VOHRTION WAS BROADLY BASED NATURAL SELECTION IS THE PRIMARY MECHANISM OF EVOLUTION CENES, DNA, AND CHROMOSOMES 161 762 162 PARTICULATE INHERITANCE IS FUNDAMENTAL TO GENETICS 162 MUTATIONS PROVIDE RAW MATERIAL FOR NATURAL SELECTION 163 GENETIC RECOMBINATION ALSO PROVIDES RAW MATERIAL FOR NATURAL SELECTION 163 HORIZONTAL GENE TRANSFER IS A NOVEL MECHANISM OFGENETIC CHANGE 764 REGULATORY CENES AND PATTERNS OF DEVELOPMENT 164 POPULATIONS, SPECIES, AND SPECIATION 764 RATES OF ORIGINATION 165 EVOLUTIONARY RADIATIONS RESULT FROM NEW ECOLOGICAL OPPORTUNITIES AND ADAPTIVE BREALTHROUGHS 166 RAPID SPECIATION CAN OCCUR BY WAY OF SMALL, ISOLATED POPULATIONS 168 A NEW HIGHER TAXON CAN ARISE THROUGH A SINGLE SPECIATION EVENT L7L THE MOLECULAR CLOCK AND TIMES OF ORIGINATION 171 EVOLUTIONARY CONVERGENCE L72 EXTINCTION 173 RATES OF EXTINCTION VARY GREATLY 173 A MASS EXTINCTION IS OCCURRING TODAY 174 EVOLUTIONARY TIENDS 175 ANIMALS TEND TO EVOLVE TOWARD LARGER BODYSIZE L75 EVOLUTIONARY TRENDS CAN BE SIMPLE OR COMPLEX EVOLUTION IS IRREVERSIBLE (HAPTER SUMMARY/REVIEW QUESTIONS T77 180 180 112 114 LT4 TT7 118 118 118 L2L L24 L24 150 151 153 R55 R58 159 159 T25 126 R2S 132 R32 133 T34 T34 134 136 136 74{) 1.40 147 L44 146 146 T47 148 T48 F *T LLLHE THEORY OF PLATE TECTONICS FHE HISTORY OF CONTINENTAL DRIFT THEORY ,, SOME EARLY OBSERVATIONS WERE MISINTELPRETED ,DL&ED WEGENER WAS A TWENTIETH-CENTURY N,, PIONEER ALEXANDER DU TOIT FOCUSED ON THE GONDWANA SELLUENCE ILRI C,ONTINENTAL DRIFT WAS WIDELY REJECTED CHEMICAL RESERVOIRS 226 FLUXES ARE RATES OF MOVEMENT BETWEEN SMALL LANDMASSES MAY BE SUTURED TO CONTINENTS TECTONICS OF CONTINENTAL LNTERIORS (HAPTER SUMMARY/REVIEW QUESTIONS GLACIERS LOCK UP OXYGEN 16 OXYGEN ISOTOPE RATIOS VARY WITH SALINITY WATER VAPOR ACTS AS A GREENHOUSE GAS USE OF CARBON LSOTOPES TO STUDY CLOBAL CHEMICALCYCLES ATMOSPHERIC CARBON RESERVOIR PHANEROZOIC TRENDS IN ATMOSPHERIC CARBON DIOXIDE 183 186 186 187 188 T90 278 2L9 222 226 226 OON 227 228 228 228 229 231 2,T.5 234 235 235 PALEOMAGNETISMSHOWEDPUZZLINGPATTERNS 191 TH RISE OF PLATE TECTONICS T92 SEAFLOOR SPREADING EXPLAINED MANY PHENOMENA 192 PALEOMAGNETISM PROVIDED A DEFINITIVE TEST L94 F,AUHING AND VOLCANISM ALONG PLATE BOUNDARIES 195 OCEANIC CRUST FORMS ALONG MID-OCEAN RIDGES 196 TRANSFORM FAULTS OFFSET MID-OCEAN RIDGES 196 LITHOSPHERE IS SUBDUCTED ALONG DEEP-SEA TRENCHES PLATE MOVEMENTS PLATES MOVE FOR FOUR REASONS FREE SLABS SINK DEEP INTO THE MANTLE PLATE MOVEMENTS ARE MEASURABLE FTAPTER 5UMMARYLIEVIEW QUESTIONS (IIAPITR 9 CONTINENTAL TECTONICS AND MOUNTAIN CHAINS THE RIFTING OF CONTINENTS HOT SPOTS GIVE RISE TO THREE-ARMED RIFTS RIFT VALLEYS FORM WHEN CONTINENTAL BREAKUP BEGINS RIFTING CREATES PASSIVE MARGINS BENDING AND FLOWING OF ROCKS MOUNTAIN BUILDING CONTINENTAL COLLISION PRODUCES OROGENIES OROGENIES CAN OCCUR WITHOUT CONTINENTAL COLLISION MOUNTAIN BELTS HAVE A CHARACTERISTIC STRUCTURE COMPRESSIVE FORCES CAUSE DEFORMATION THE WEIGHT OF A MOUNTAIN BELT CREATES A FORELAND BASIN THE ANDES EXEMPLLFY MOUNTAIN BUILDING WITHOUT CONTINENTAL COLLISION THE PYRENEES EXEMPLIF, MOUNTAIN BUILDING BY CONTINENTAL COLLISION RESELVOLRS FEEDBACKS AFFECT FLUXES CARBON DIOXIDE, OXYGEN, AND BIOLOGICAL PROCESSES PLANTS EMPLOY A PHOTOSLNTHESIS-RESPIRATION CYCLE PHOTOSPTHESIS PRODUCES TISSUE GROWTH RESPIRATION RELEASES ENERG/ DECOMPOSERS EMPLOY RESPIRATION BURIAL OF PLANT DEBRIS ALTERS ATMOSPHERIC CHEMISTRY MARINE PHOTOSPTHESIS-RESPIRATION CYCLES RESEMBLE THOSE ON LAND OXYGEN LSOTOPES, CLIMATE, AND THE WATER CYCLE 231 OXYGEN ISOTOPE RATIOS IN SKELETONS REFLECT TEMPERATURES 232 T97 198 198 199 199 201 203 206 206 207 209 209 2R2 272 2L2 213 213 2T4 2T5 2T7 CARBON ISOTOPE RATIOS RECORD THE CYCLING OF ORGANIC CARBON 235 ISOTOPE RATIOS IN LIMESTONES AND DEEP-SEA SEDIMENTS RECORD CHANGES IN RATES OF CARBONBURIAL 236 CARBON AND SULFUR BURIAL ENLARGES THE ATMOSPHERET OXYGEN RESERYOIR 236 CARBON DIOXIDE IS REMOVED FROM THE ATMOSPHERE BY WEATHERING AND ENDS UP IN LIMESTONE 237 CHANGES IN RATES OF WEATHERING AFFECT THE ATMOSPHERIC CARBON RESERVOIR 238 CHANGES IN GLOBAL TEMPERATURE ALSO AFFECT THE 240 FIT[PTRN R0 MAJOR GEOCHEMICAL CYCLES 24L POSITIVE FEEDBACKS INFLUENCE THE CARBON CYCLE NEGATIVE FEEDBACKS HOLD CARBON DIOXLDE LEVELS IN CHECK CARBON AND OXYGEN LSOTOPE EXCURSIONS CHANGES IN RESPIRATION RATES OF BACTERIA INFLUENCE CARBON ISOTOPE RATIOS CHANGES IN THE VOLUME OF METHANE HYDRATES INFLUENCE CARBON ISOTOPE RATIOS CHANGES IN PHYTOPLANKTON PRODUCTIVITY INFLUENCE CARBON ISOTOPE RATIOS EPISODES OF MASSIVE CARBON BURIAL CAN OVERRIDE OTHER FACTORS THAT INFLUENCE CARBON ISOTOPE RATIOS OCEAN CHEMISTRY AND SKELETAL MINERALOGY VARIATIONS IN MAGNESIUM AND CALCIUM OVER TIME INFLUENCE THE PRODUCTION OF MARINE CARBONATES VARIATIONS IN POTASSIUM AND SULFATE OVER TIME INFLUENCE THE MINERALOGY OF EVAPORITES ORGANISMS REMOVE SILICA FROM THE OCEAN (HAPTER SUMMARY/FLEVIEW QUESTIONS PART IL THE STORY OF [ARTH (IIAPTTR II THE HADEAN AND ARCHEAN EONS OF PRECAMBRIAN TIME THE AGES OF THE PLANETS AND THE UNIVERSE THE ORIGIN OF THE SOLAR SYSTEM THE SUN FORMED FROM A NEBULA THE PLANETS FORMED FROM THE SOLAR NEBULA THE HADEAN EON EARLY MELTING PRODUCED A LAYERED EARTH THE MOON FORMED FROM A COLLISION THE OCEAN S WATER CAME FROM VOLCANOES AND COMETS, AND ITS SALTS CAME FROM ROCKS EARTH S EARLY ATMOSPHERE MOSTLY CAME FROM WITHIN EARLY EARTH ERPERIENCED MANY METEORITE IMPACTS EARLY EARTH WAS HOT, NND ITS PLATES WERE SMALL THE ORIGIN OF CONTINENTAL CRUST FELSIC CRUST FORMED BY MELTING OF OCEANIC LITHOSPHERE CONTINENTAL CRUST APPEARED EARLY IN EARTH S HISTORY 242 242 243 244 244 243 THE ARCHEAN EON ARCHEAN CONTINENTS REMAINED SMALL BECAUSE OF EARTH S HOT INTERIOR THE TOTAL AMOUNT OF CONTINENTAL CRUST INCREASED RAPIDLY GREENSTONE BELTS EARTH SYSTEM SHIFT 11-1 LARGE CRATONS A14:EAR NECR THE END OF ARCLWAN TINV EVIDENCE OF ARCHEAN LIFE CHEMICAL EVIDENCE BEARING ON THE ORIGIN OF LIFE AMINO ACIDS FORMED EASILY PERHAPS THERE WAS AN RNA WORLD LIFE MAY HAVE ORIGINATED ALONG MID-OCEAN RIDGES ATMOSPHERIC OXYGEN (HAPTER 5UMMARY/REVIEW QUESTIONL 262 262 262 263 264 266 268 269 269 275 278 280 280 28T 283 283 287 287 288 244 244 244 247 247 247 269 272 272 249 254 :ZD5 256 256 257 258 258 259 259 259 260 260 26T 26T 0TLPFIN N THE PROTEROZOIC EON OF PRECAMBRIAN TIME A MODERN STYLE OF OROGENY GLOBAL EVENTS OF THE PALEOPROTEROZOIC AND MESOPROTEROZOIC GLACIATION WAS WIDESPREAD EARLY IN PROTEROZOIC TIME CYANOBACTERIA FLOURISHED IN THE OCEANS, AND EUKARYOTES JOINED THEM THE BEGINNINGS OF ANIMAL LIFE ANIMALS BURST ON THE SCENE A BUILDUP OF ATMOSPHERIC OXYGEN FAVORED EUKARYOTES TWICE DURING PROTEROZOIC TIME WIDESPREAD GLACIATION EXTENDED TO LOW LATITUDES EARTH SYSTEM SHIFT 12-1 THE GREAT UEXIDATIOU 7)UETFT EARTH SYSTEM SHIFT 12-2 WOS THERE A SNOWBNLL. EAFTH L 2SUE THE DIVERSIFICATION OF ANIMALS MAY HAVE CHANGED THE EVOLUTION OFPHYTOPLANKTON 292 THE EXPANSION AND CONTRACTION OF CONTINENTS 292 THE ASSEMBLY OF NORTH AMERICA 293 CONTINENTAL ACCRETION EXPANDED LAURENTIA DURING PROTEROZOIC TIME 293 AN EXTRATERRESTRIAL IMPACT PRODUCED HUGE ORE DEPOSITS 294 -{ RIFT FORMED IN CENTRAL AND EASTERN NORTH.{MERICA 296 THE GRENVILLE OROGENY BUILT MOUNTAINS IN EASTERN NORTH AMERICA THE ASSEMBLY AND BREAKUP OF NEOPROTEROZOIC SUPERCONTINENTS THE SUPERCONTINENT NUNA CONTAIN OED ALL OF EARTH S LARGE LANDMASSES THE SUPERCONTINENT RODINIA WAS SMALLER THAN NUNA THE SUPERCONTINENT PANNOTIA, ALTHOUGH IT SOON LOST LAURENTIA, BECAME PART OF GONDWANALAND (HAPTER 5UMMARY/REVIEW QUELTIONL UETLPTIN L3 THE EARLY PALEOZOIC WORLD 3OL THE CAMBRIAN EXPLOSION OF LIFE 304 THE BASE OF THE CAMBRIAN IS DEFINED BY BURROWS OF COMPLEX FORM 304 MANY EARLY CAMBRIAN GROUPS EVOLVED SKELETONS 304 EARLY CAMBRIAN ANIMALS HAD FEW MODES OF LIFE SO7 EARTH SYSTEM SHIFT 13-1 SKELETANS EAOLUE IN MUR TY ANI,RNUL GROU1TS AS PREDOLARS DI,AERSIFU 308 LATER CAMBRIAN DIVERSIFICATION PRODUCED (HAPTER SUMMARY/REVIEW QUETTIONL 327 (IIAPTTR II THE MIDDLE PALEOZOIC WORLD RENEWED DIVERSIFICATION OF LIFE LIFE RECOVERED AND EXPANDED IN AQUATIC HABITATS 332 PLANTS INVADED THE LAND 338 ANIMALS MOVED ASHORE 341 EARTH SYSTEM SHIFT 14-1 PLC.RRTS ALTERLANDSTT4TES ANRL OYTEN THE WAY FORYERTEBRATAS TO CONQUER THE LNND. 342 THE PALEOGEOGRAPHY OF THE MIDDLE PALEOZOIC WORLD 345 GLACIATION AND A MASS EXTINCTION 346 REGIONAL EVENTS OF MIDDLE PALEOZOIC TIME 347 EASTERN NORTH AMERICA AGAIN BECAME A PASSIVE MARGIN 347 EARTH SYSTEM SHIFT T4-2 T HE EXPANSION OF PLANTS OUER LA NCL (LOUSES GLOBAL CLIMTTTIC CHUNGE, CKTC IATION, AND BLASS EXTINC:TION 348 EURAMERICA FORMED DURING THE SECOND APPALACHIAN OROGENY 350 REEF BUILDING AND OROGENY OCCURRED IN WESTERN NORTH AMERICA 353 (HAPTER SUMMARY/REVIEW QUELTIONS S54 (IIAPTTR I THE LATE PALEOZOIC WORLD 357 LATE PALEOZOIC LIFE 360 NEW FORMS OF LIFE EMERGED IN PALEOZOIC SEAS 361 ARAGONITIC REEF BUILDERS FLOURISHED IN ARAGONITE SEAS 362 TREES GREW IN SWAMPS 362 UPLANDFLORAS EXPANDED 365 ANIMALS DIVERSIFIED ON LAND AND INVADED FRESHWATER HABITATS 366 EARTH SYSTEM SHIFT 15 - 1 WEAKENECL. C REENHANSE WANNI,NGPREVR,L,TS IN, A GREAT LCE AGE 368 PALEOGEOGRAPHY OF THE LATE PALEOZOIC WORLD 37L WARM, MOIST CONDITIONS WERE WIDESPREAD IN EARLY CARBONIFEROUS TIME 373 IN MID-CARBONIFEROUS TIME, CONTINENTS COLLIDED AND A GREAT ICE AGE BEGAN 373 DRY HABITATS EXPANDED IN PERMIAN TIME 374 297 297 297 298 299 299 329 332 VERTEBRATE ANIMALS ORDOVICIAN LIFE AMONG EARLY PALEOZOIC ANIMALS WERE FLOATERS AND SWIMMERS A GREAT RADIATION OFLIFE OCCURRED LATER IN THE ORDOVICIAN ANIMALS CAUSED STROMATOLITES TO DECLINE EXTINCTION SET BACK MARINE DIVERSIFFCATION INVERTEBRATES INVADED FRESH WATER AND PLANTS INVADEDLAND 316 PALEOGEOGRAPHY OF THE CAMBRIAN WORLD 316 EPISODIC MASS EXTINCTIONS OF CAMBRIAN TRILOBITES 317 ORDOVICIAN PALEOGEOGRAPHY, CLIMATIC CHANGE, AND MASS EXTINCTION 319 CLIMATIC COOLING BROUGHT ABOUT AN ICE AGE 319 EARTH SYSTEM SHIFT 13-2 CLIURUTIC COOLINGRESULTS IN GLACIATION ANTL MUSS EXTIRTCTION 320 CLIMATIC COOLING ALSO BROUGHT ABOUT A MAJOR 311 312 ,JIJ JIOE 315 S15 322 322 MASS EXTINCTION REGIONAL EVENTS OF EARLY PALEOZOIC TIME THE TACONIC OROGENY RAISED MOUNTAINS IN EASTERN LAURENTIA 322 A PASSIVE MARGIN PERSISTED IN WESTEM LAURENTIA 326 MASS EXTINCTIONS ENDED THE PALEOZOIC ERA EARTH SYSTEM SHIFT 15-2 THE MOST DESTRUCTIUE OF ASS H,IA SS ERTINDTINTLS ENDS THE PALEOTIC ERA REGIONAL EVENTS OF LATE PALEOZOIC TIME THE ALLEGHENIAN OROGENY FORMED THE APPALACHIAN MOUNTAINS OROGENIES ALSO OCCURRED IN THE SOUTHWESTERN UNITED STATES COAL DEPOSITS FORMED WITHIN CYCLOTHEMS REEFS FORMED IN THE DELAWARE BASIN OF WESTERN TEXAS 384 THE SONOMA OROGENY EXPANDED THE NORTH AMERICAN CONTINENT 386 (HAPTER SUMMARY/LEVIRW QUESTIONL 387 BENTHIC LIFE WAS ALSO MODERNIZED FLOWERING PLANTS EXPANDED ON LAND DINOSAURS DWARFED EARLY MAMMALS 375 376 379 381 382 426 428 429 LIFE IN THE OCEANS: A NEW BIOTA THREE MASS EXTINCTIONS SLOWED THE EARLY TRIASSIC RECOVERY PELAGIC LIFE INCLUDED NEW GROUPS OF PHYTOPLANKON AND NUMEROUS SWIMMING PREDATORS LIFE ON LAND GYMNOSPERMS DOMINATED THE MESOZOIC FLORA THE AGE OF DINOSAURS BEGAN EARTH SYSTEM SHIFT 16-1 THE RISA OFTHE UEWSAURS: WHY WERE T LRCQ SO SUCCESSFUL? EARTH SYSTEM SHIFT 16-2 YOLCNNISM AND IV{ASS EXTINCTION A MASS EXTINCTION ENDED THE TRIASSIC PERIOD THE PALEOGEOGRAPHY OF THE EARLY MESOZOIC ERA THE SIZE OF PANGAEA AFFECTED CLIMATES AND DISTRIBUTIONS OF ORGANISMS PANGAEA BEGAN TO FRAGMENT TROPICAL AND NONTROPICAL ZONES WERE EVIDENT TECTONIC EVENTS IN NORTH AMERICA FAULT BLOCK BASINS FORMED IN THE EAST NORTH AMERICA GREW WESTWARD (HAPTER SUMMARY/REVIEW QUESTIONL QTLPLTN TI THE CRETACEOUS WORLD CRETACEOUS LIFE PELAGIC LIFE WAS MODERNIZED PALEOGEOGRAPHY OF THE CRETACEOUS WORLD 4SS CONTINENTS FR.AGMENTED AND NARROW OCEANS EXPANDED SSS SEA LEVEL ROSE, THE DEEP OCEAN STAGNATED, AND CLIMATES WARMED 43G THE TERMINAL CRETACEOUS EXTINCTION 457 THE TERMINAL CRETACEOUS IMPACT SERVES AS A WARNING 438 FOSSILS DISGUISED THE TIMING OF THE EXTINCTION 438 OPPORTUNISTIC SPECIES FOURISHED IN THE AFTERMATH OF THE EXTINCTION 438 NORTH AMERICA IN THE CRETACEOUS WORLD 439 CORDILLERAN MOUNTAIN BUILDING CONTINUED 439 EARTH SYSTEM SHIFT 17-1 DEATHFRAMOTTTERSPAC.E 44O A SEAWAY CONNECTED THE GULF OF MEXICO AND THE ARCTIC OCEAN AN ANCIENT RIVER EXCAVATED THE CHASM THAT BECAME THE GRAND CANYON THE MODERN CONTINENTAL SHELF FORMED IN EASTERN NORTH AMERICA THE CHALK SEAS OF EUROPE (HAPTER SUMMARY/REVIEW QUESTIONS 379 392 393 394 398 398 399 401 408 4TT 4TT 412 412 413 4L4 414 415 4TG LIFE OF THE PALEOGENE MARINE LIFE RECOVERED FLOWERING PLANTS ROSE TO DOMINANCE MAMMALS RADIATED DRAMATICALLV IN THE PALEOCENE AND EOCENE R EARLY PALEOGENE BIRDS WERE LARGE MODERN GROUPS OF HOOFED ANIMALS, CARNIVORES, AND PRIMATES EXPANDED IN THE OLIGOCENE FROGS AND INSECTS WERE MODERNIZED IN PALEOGENE TIME 460 PALEOGENE CLIMATES 460 THE EOCENE BEGAN WITH A PULSE OF WARMING 460 WARMTH EXTENDED TO HIGH LATITUDES 462 COOLING AND HIGH-LATITUDE GLACIATION BEGAN IN THE MIDDLE EOCENE 464 CLIMATIC CHANGE, GLACIAL EXPANSION, AND A MASS EXTINCTION MARKED THE EOCENE-OLIGOCENE TRANSITION REGIONAL EVENTS OF PALEOGENE TIME 445 446 447 448 452 452 454 454 457 458 464 465 42T 421 424 (IIAPTTR I6 THE EARLY MESOZOIC ERA (IIAPTTR I8 THE PALEOGENE WORLD POSITIONS OFLAND AND SEA CHANGED NEAR THE POLES MOUNTAIN BUILDING CONTINUED IN WESTERN NORTH AMERICA EARTH SYSTEM SHIFT 18-1 GLOBULCOOLINGAND DRYINGSSEGINS A RIFT DEVELOPED IN THE AMERICAN SOUTHWEST SHALLOW SUBDUCTION PRODUCED VOLCANISM IN THE YELLOWSTONE REGION DEPOSITION CONTINUED ALONG THE GULF COAST A METEORITE CREATED THE SITE OF THE CHESAPEAKE BAY (HAPTER §UMMARY/REVIEW QUELTIONS (IIIPTTR 19 THE LATE CENOZOIC WORLD BEFORE THE HOLOCENE LIFE OF THE NEOGENE PERIOD IN THE OCEAN, WHALES RADIATED AND FORAMINIFERA RECOVERED ON LAND, SPECIES ADAPTED TO SEASONALLY DRY HABITATS FLOURISHED THE MODERN LCE AGE OF THE NORTHERN HEMISPHERE EARLY PLIOCENE CLIMATES WERE RELATIVELY WARRN CONTINENTAL GLACIERS FORMED IN THE NORTHERN HEMISPHERE THE CHRONOLOG,U OF GLACIATION CAN BE READ IN ISOTOPE RATIOS CLIMATIC CHANGES ALTERED FLORAS GLACIERS EXPANDED AND CONTRACTED MANY TIMES EARTH SYSTEM SHIFT 19- 1 SLTOCKINGLY RAPID CLINWTIC SHIFTS OCRU,R DURI,NGTHE LCE AGE VEGETATION PATTERNS CHANGED DURING GLACIAL MAXIMA CHANGES IN OCEANIC CIRCULATION MAY HAVE TRIGGERED THE ICE AGE CHANGES IN EARTHT ROTATIONAL MOVEMENT HAVE AFFECTED GLACIAL CYCLES CHANGES IN THE GREENHOUSE EFFECT RESULTED FROM CLIMATIC OSCILLATIONS REGIONAL EVENTS OF NEOGENE TIME MOUNTAINS ROSE UP THROUGHOUT THE AMERICAN WEST THE APPALACHIANS BOBBED UP AND SHED SEDIMENT EASTWARD THE CARIBBEAN SEA WAS BORN NORTH AND SOUTH AMERICA EXCHANGED MAMMALS THE HIMALAYA ROSE TO BECOME EARTH S HIGHEST MOUNTAIN RANGE THE TETHYS SEAWAY CAME TO AN END HUMAN EVOLUTION EARLY APES RADIATED IN AFRICA AND ASIA THE EARLIEST HOMINID LIVED ABOUT 6 MILLION YEARS AGO THE AUSTRALOPITHECINES RESEMBLED BOTH APES AND HUMANS THE HUMAN GENUS MADE A SUDDEN APPEARANCE HOMA ERECTUS RESEMBLED US EARTH SYSTEM SHIFT 19-2 THE LHTNTOTT, CENUS ARISES UT A TIRNE OF SUD.D,EN CLINMTIC CHANGE THE FLORES PEOPLE WERE CURIOUS DWARFS HORUTHEIDEHERGENSI,S WAS MORE SIMILAR TO US THAT HOMO ERECTUS THE NEANDERTHALS EMERGED IN EURASIA HOMO SAPIENS EVOLVED IN AFRICA AND SPREAD NORTH (HAPTRR SUMMARY/REVIEW QUELTIONS 465 506 508 509 509 509 509 511 513 514 516 516 577 518 519 465 466 47L 471 472 473 475 477 480 480 481 485 485 485 487 488 489 490 492 493 494 494 495 495 503 504 505 (IIIPTTR ILL THE RETREAT OF GLACIERS AND THE HOLOCENE THE RETREAT OF GLACIERS 525 ABRUPT GLOBAL EVENTS OF THE LATEST PLEISTOCENE 52L AND EARLY HOLOCENE THE YOUNGER DRYAS EARTH SYSTEM SHIFT 2O- L LIUIDSNCE THAT A CCSMET STRU.CK EAFTLZ, CRUSINGTHE YOUNGER DTTLAS EUENL,TLTE EFUENCTI TN OF LARGE MANTRW S, AND TLW DISTT.,PPEARANCE AJ THE CLOAI.S CULTURE THE FIRST AMERICANS A SUDDEN EXTINCTION OF LARGE MAMMALS CLIMATIC FLUCTUATIONS OF THE LAST 10,000 YEARS THE HYPSITHERMAL INTERVAL WAS A BRIEF PERIOD OF GLOBAL WARMTH HUMANS INVENTED AGRICULTURE GLACIERS, TREE LINES, AND TREE RINGS RECORD CLIMATIC CHANGE TEMPERATURES HAVE FLUCTUATED SINCE THE HLPSITHERMAL INTERVAL SEVERE DROUGHTS HAVE OCCURRED DURING HOLOCENE TIME 536 SEA LEVEL CHANGES 538 SEA LEVEL ROSE RAPIDLY IN THE EARLY HOLOCENE 538 526 526 528 531 5S2 533 534 534 DJD 536 COASTLINES HAVE SHIFTED DURING THE PAST 7000 YEARS THE TWENTIETH AND TWENTY-FIRST CENTURIES: THE LMP;RCT O{ L- NUMANS ANTHROPOGENIC GASES IN THE ATRNOSPHERE ARE CAUSING GREENHOUSE WARMING FUTURE CLIMATIC CHANGE WILL HAVE SERIOUS CONSEQUENCES INCREASED CARBON DIOXIDE CONCENTRATIONS IN THE OCEANS ARE INHIBITING CALCIFICATION BY RNARINE ORGANISMS SEA LEVEL IS RISING POSITIVE FEEDBACKS MAY SPEED CLIMATIC CHANGE (HAPTER SUMMARY/REVIEW QUELTIONS GLOSSARY LNDEX 543 O+D 546 549 553 569 538 540 540 541 543 APP ENDIX : STRATIGRAPHIC ST AGES
any_adam_object	1
author	Stanley, Steven M. 1941- Luczaj, John A.
author_GND	(DE-588)120486539 (DE-588)1053177046
author_facet	Stanley, Steven M. 1941- Luczaj, John A.
author_role	aut aut
author_sort	Stanley, Steven M. 1941-
author_variant	s m s sm sms j a l ja jal
building	Verbundindex
bvnumber	BV041935976
classification_rvk	RB 10123 TK 1000
ctrlnum	(OCoLC)884513486 (DE-599)BVBBV041935976
discipline	Geologie / Paläontologie Geographie
edition	Fourth edition
format	Book
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spelling	Stanley, Steven M. 1941- Verfasser (DE-588)120486539 aut Earth system history Steven M. Stanley ; John A. Luczaj Fourth edition New York, NY W.H. Freeman and Company 2015 XXVI, 587 Seiten Illustrationen, Diagramme, Karten 28 cm txt rdacontent n rdamedia nc rdacarrier Previous edition: 2009 Includes bibliographical references and index Historical geology Physical geology Geologie (DE-588)4020227-6 gnd rswk-swf Historische Geologie (DE-588)4025104-4 gnd rswk-swf Geodynamik (DE-588)4020212-4 gnd rswk-swf Paläogeografie (DE-588)4132305-1 gnd rswk-swf Paläontologie (DE-588)4044375-9 gnd rswk-swf (DE-588)4123623-3 Lehrbuch gnd-content Historische Geologie (DE-588)4025104-4 s Geodynamik (DE-588)4020212-4 s 1\p DE-604 Paläogeografie (DE-588)4132305-1 s 2\p DE-604 Paläontologie (DE-588)4044375-9 s 3\p DE-604 Geologie (DE-588)4020227-6 s 4\p DE-604 Luczaj, John A. Verfasser (DE-588)1053177046 aut SWB Datenaustausch application/pdf http://bvbr.bib-bvb.de:8991/F?func=service&doc_library=BVB01&local_base=BVB01&doc_number=027379143&sequence=000001&line_number=0001&func_code=DB_RECORDS&service_type=MEDIA Inhaltsverzeichnis 1\p cgwrk 20201028 DE-101 https://d-nb.info/provenance/plan#cgwrk 2\p cgwrk 20201028 DE-101 https://d-nb.info/provenance/plan#cgwrk 3\p cgwrk 20201028 DE-101 https://d-nb.info/provenance/plan#cgwrk 4\p cgwrk 20201028 DE-101 https://d-nb.info/provenance/plan#cgwrk
spellingShingle	Stanley, Steven M. 1941- Luczaj, John A. Earth system history Historical geology Physical geology Geologie (DE-588)4020227-6 gnd Historische Geologie (DE-588)4025104-4 gnd Geodynamik (DE-588)4020212-4 gnd Paläogeografie (DE-588)4132305-1 gnd Paläontologie (DE-588)4044375-9 gnd
subject_GND	(DE-588)4020227-6 (DE-588)4025104-4 (DE-588)4020212-4 (DE-588)4132305-1 (DE-588)4044375-9 (DE-588)4123623-3
title	Earth system history
title_auth	Earth system history
title_exact_search	Earth system history
title_full	Earth system history Steven M. Stanley ; John A. Luczaj
title_fullStr	Earth system history Steven M. Stanley ; John A. Luczaj
title_full_unstemmed	Earth system history Steven M. Stanley ; John A. Luczaj
title_short	Earth system history
title_sort	earth system history
topic	Historical geology Physical geology Geologie (DE-588)4020227-6 gnd Historische Geologie (DE-588)4025104-4 gnd Geodynamik (DE-588)4020212-4 gnd Paläogeografie (DE-588)4132305-1 gnd Paläontologie (DE-588)4044375-9 gnd
topic_facet	Historical geology Physical geology Geologie Historische Geologie Geodynamik Paläogeografie Paläontologie Lehrbuch
url	http://bvbr.bib-bvb.de:8991/F?func=service&doc_library=BVB01&local_base=BVB01&doc_number=027379143&sequence=000001&line_number=0001&func_code=DB_RECORDS&service_type=MEDIA
work_keys_str_mv	AT stanleystevenm earthsystemhistory AT luczajjohna earthsystemhistory

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