The Authors |
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viii | |
Foreword from First Edition |
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x | |
Acknowledgments |
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xi | |
Book Introduction to the Second Edition for Students and Instructors |
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xvii | |
About the Companion Website |
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xii | |
Chapter 1 Introduction to Paleoclimate Records |
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1 | (30) |
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Part 1.1 Archives and Proxies |
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3 | (10) |
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Part 1.2 Obtaining Cores from Terrestrial and Marine Paleoclimate Archives |
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13 | (14) |
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Part 1.3 Owens Lake - An Introductory Case Study of Paleoclimate Reconstruction |
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27 | (4) |
Chapter 2 Seafloor Sediments |
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31 | (26) |
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Part 2.1 Sediment Predictions |
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33 | (1) |
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Part 2.2 Core Observation and Description |
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34 | (7) |
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Part 2.3 Sediment Composition |
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41 | (11) |
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Part 2.4 Seafloor Sediment Synthesis |
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52 | (5) |
Chapter 3 Geologic Time and Geochronology |
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57 | (32) |
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Part 3.1 The Geologic Timescale |
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59 | (3) |
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Part 3.2 Principles of Stratigraphy and Determining Relative Ages |
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62 | (2) |
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Part 3.3 Radiometric Age Dating Fundamentals |
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64 | (5) |
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Part 3.4 Using 40K - 40Ar Dating to Determine the Numerical Ages of Layered Volcanic Rocks |
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69 | (7) |
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Part 3.5 Using Uranium Series Dating to Determine Changes in Growth Rate of Speleothems |
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76 | (13) |
Chapter 4 Paleomagnetism and Magnetostratigraphy |
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89 | (30) |
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Part 4.1 Earth's Magnetic Field Today and the Paleomagnetic Record of Deep-Sea Sediments |
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91 | (9) |
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Part 4.2 History of Discovery: Paleomagnetism in Ocean Crust and Marine Sediments |
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100 | (8) |
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Part 4.3 Using to Test the Seafloor Spreading Hypothesis |
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108 | (6) |
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Part 4.4 The Geomagnetic Polarity Timescale |
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114 | (5) |
Chapter 5 Microfossils and Biostratigraphy |
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119 | (46) |
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Part 5.1 What Are Microfossils? Why Are They Important in Climate Change Science? |
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121 | (9) |
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Part 5.2 Microfossils in Deep-Sea Sediments |
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130 | (7) |
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Part 5.3 Application of Microfossil First and Last Occurrences |
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137 | (7) |
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Part 5.4 Using Microfossil Datums to Calculate Sedimentation Rates |
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144 | (5) |
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Part 5.5 How Reliable Are Microfossil Datums? |
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149 | (7) |
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Part 5.6 Organic-Walled Microfossils: Marine Dinoflagellates and Terrestrial Pollen and Spores |
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156 | (9) |
Chapter 6 CO2 as a Climate Regulator During the Phanerozoic and Today |
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165 | (35) |
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Part 6.1 The Short-Term Global Carbon Cycle |
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167 | (2) |
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Part 6.2 CO2 and Temperature |
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169 | (10) |
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Part 6.3 Recent Changes in CO2 |
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179 | (4) |
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Part 6.4 The Long-Term Global Carbon Cycle, CO2, and Phanerozoic Climate History |
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183 | (8) |
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Part 6.5 Carbon Isotopes as a Tool for Tracking Changes in the Carbon Cycle |
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191 | (9) |
Chapter 7 Oxygen Isotopes as Proxies of Climate Change |
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200 | (26) |
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Part 7.1 Introduction to Oxygen Isotope Records from Ice and Ocean Sediments |
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202 | (3) |
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Part 7.2 The Hydrologic Cycle and Isotopic Fractionation |
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205 | (4) |
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Part 7.3 δ18O in Meteoric Water and Glacial Ice |
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209 | (9) |
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Part 7.4 δ18O in Marine Sediments |
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218 | (8) |
Chapter 8 Climate Cycles |
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226 | (29) |
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Part 8.1 Patterns and Periodicities |
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228 | (17) |
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Part 8.2 Orbital Metronome |
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245 | (5) |
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Part 8.3 Glacial-Interglacial Peribds and Modern Climate Change |
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250 | (5) |
Chapter 9 The Paleocene-Eocene Thermal Maximum (PETM) Event |
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255 | (59) |
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Part 9.1 An Important Discovery |
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257 | (3) |
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Part 9.2 Global Consequences of the PETM |
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260 | (36) |
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Part 9.3 Two Hypotheses for the Cause of the PETM |
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296 | (3) |
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Part 9.4 Rates of Onset and Duration of Event |
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299 | (7) |
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Part 9.5 Global Warming Today and Lessons from the PETM |
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306 | (8) |
Chapter 10 Glaciation of Antarctica: The Oil Event |
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314 | (41) |
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Part 10.1 Initial Evidence |
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316 | (5) |
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Part 10.2 Evidence for Global Change |
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321 | (21) |
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Part 10.3 Mountain Building, Weathering, CO2 and Climate |
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342 | (7) |
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Part 10.4 Legacy of the Oi1 Event: The Development of the Psychrosphere |
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349 | (6) |
Chapter 11 Antarctic Climate Variability in the Neogene |
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355 | (43) |
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Part 11.1 What Do We Think We Know About the History of Antarctic Climate? |
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358 | (4) |
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Part 11.2 What is Antarctica's Geographic and Geologic Context? |
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362 | (13) |
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Part 11.3 Selecting Drillsites to Best Answer our Questions |
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375 | (4) |
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Part 11.4 What Sediment Facies are Common on the Antarctic Margin? |
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379 | (11) |
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Part 11.5 The BIG Picture of ANDRILL 1-B |
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390 | (8) |
Chapter 12 Pliocene Warmth as an Analog for Our Future |
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398 | (32) |
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Part 12.1 The Last 5 Million Years |
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400 | (7) |
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Part 12.2 Pliocene Latitudinal Temperature Gradient |
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407 | (7) |
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Part 12.3 Estimates of Pliocene CO2 |
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414 | (2) |
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Part 12.4 Sea Level Past, Present, and Future |
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416 | (14) |
Chapter 13 Climate, Climate Change, and Life |
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430 | (57) |
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432 | (1) |
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Part 13.2 The Long View: "Precambrian" and Phanerozoic Life and Climate |
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433 | (8) |
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Part 13.3 Examples of Cenozoic Terrestrial Evolution and Climate Connections |
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441 | (17) |
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Part 13.4 Examples of Cenozoic Marine Biotic Evolution and Climate Connections |
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458 | (11) |
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Part 13.5 Humanity, Climate, and Life |
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469 | (12) |
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Part 13.6 Humanity and Future Climate: At a Tipping Point |
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481 | (6) |
Chapter 14 Climate Change and Civilization |
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487 | (49) |
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Part 14.1 Climate Change Here and Now |
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489 | (8) |
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Part 14.2 Evidence of Climatic Stress on Ancient Maya Civilization |
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497 | (16) |
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Part 14.3 The Precipitation Record of the North American Southwest: The Physical Record and Human Response |
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513 | (23) |
Index |
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536 | |