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E-grāmata: Reconstructing Earth's Climate History: Inquiry-Based Exercises for Lab and Class

(St Cloud State University), (University of Massachusetts), (Ohio State University), (James Madison University), (North Hennepin Community College)
  • Formāts: PDF+DRM
  • Izdošanas datums: 25-Jun-2021
  • Izdevniecība: Wiley-Blackwell
  • Valoda: eng
  • ISBN-13: 9781119544104
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  • Formāts: PDF+DRM
  • Izdošanas datums: 25-Jun-2021
  • Izdevniecība: Wiley-Blackwell
  • Valoda: eng
  • ISBN-13: 9781119544104
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"Think about how we know about past events in human history (e.g., the expansion of the Roman Empire, or the American Revolution). What types of records document those events? Now think about Earth's history, specifically the past environmental or climatic conditions at times before recorded human history. What records might there be of such conditions? Make a list of your ideas. n assemblage of five major types of natural archives of Earth's environmental and climatic history. What common feature(s) do each of these paleoclimate archives share? an assemblage of 5 major types of natural records, or archives, of Earth's environmental and climatic history. Just like a diary or other historical document, the layers in these natural archives contain indirectevidence (i.e., proxies) about past conditions and events, recorded in a sequential order. The evidence is specific to a certain time period and may be general or very detailed, depending on the rate that information was recorded. The faster the rate at which the recorder grew (trees and corals), accumulated (snow and ice), or was deposited (sedimentary sequences), the more detailed the record is, and the higher its resolution. For example, a record in which an annual signal can observed has a very high resolution. In contrast, if the finest observable details are on the order of a million years, then that record would have a low resolution"--

Reconstructing Earth&;s Climate History

There has never been a more critical time for students to understand the record of Earth&;s climate history, as well as the relevance of that history to understanding Earth&;s present and likely future climate. There also has never been a more critical time for students, as well as the public-at-large, to understand how we know, as much as what we know, in science. This book addresses these needs by placing you, the student, at the center of learning. In this book, you will actively use inquiry-based explorations of authentic scientific data to develop skills that are essential in all disciplines: making observations, developing and testing hypotheses, reaching conclusions based on the available data, recognizing and acknowledging uncertainty in scientific data and scientific conclusions, and communicating your results to others.

The context for understanding global climate change today lies in the records of Earth&;s past, as preserved in archives such as sediments and sedimentary rocks on land and on the seafloor, as well as glacial ice, corals, speleothems, and tree rings. These archives have been studied for decades by geoscientists and paleoclimatologists. Much like detectives, these researchers work to reconstruct what happened in the past, as well as when and how it happened, based on the often-incomplete and indirect records of those events preserved in these archives. This book uses guided-inquiry to build your knowledge of foundational concepts needed to interpret such archives. Foundational concepts include: interpreting the environmental meaning of sediment composition, determining ages of geologic materials and events (supported by a new section on radiometric dating), and understanding the role of CO2 in Earth&;s climate system, among others. Next, this book provides the opportunity for you to apply your foundational knowledge to a collection of paleoclimate case studies. The case studies consider: long-term climate trends, climate cycles, major and/or abrupt episodes of global climate change, and polar paleoclimates. New sections on sea level change in the past and future, climate change and life, and climate change and civilization expand the book&;s examination of the causes and effects of Earth&;s climate history.

In using this book, we hope you gain new knowledge, new skills, and greater confidence in making sense of the causes and consequences of climate change. Our goal is that science becomes more accessible to you. Enjoy the challenge and the reward of working with scientific data and results!

Reconstructing Earth&;s Climate History, Second Edition, is an essential purchase for geoscience students at a variety of levels studying paleoclimatology, paleoceanography, oceanography, historical geology, global change, Quaternary science and Earth-system science.

The Authors viii
Foreword from First Edition x
Acknowledgments xi
Book Introduction to the Second Edition for Students and Instructors xvii
About the Companion Website xii
Chapter 1 Introduction to Paleoclimate Records 1(30)
Part 1.1 Archives and Proxies
3(10)
Part 1.2 Obtaining Cores from Terrestrial and Marine Paleoclimate Archives
13(14)
Part 1.3 Owens Lake - An Introductory Case Study of Paleoclimate Reconstruction
27(4)
Chapter 2 Seafloor Sediments 31(26)
Part 2.1 Sediment Predictions
33(1)
Part 2.2 Core Observation and Description
34(7)
Part 2.3 Sediment Composition
41(11)
Part 2.4 Seafloor Sediment Synthesis
52(5)
Chapter 3 Geologic Time and Geochronology 57(32)
Part 3.1 The Geologic Timescale
59(3)
Part 3.2 Principles of Stratigraphy and Determining Relative Ages
62(2)
Part 3.3 Radiometric Age Dating Fundamentals
64(5)
Part 3.4 Using 40K - 40Ar Dating to Determine the Numerical Ages of Layered Volcanic Rocks
69(7)
Part 3.5 Using Uranium Series Dating to Determine Changes in Growth Rate of Speleothems
76(13)
Chapter 4 Paleomagnetism and Magnetostratigraphy 89(30)
Part 4.1 Earth's Magnetic Field Today and the Paleomagnetic Record of Deep-Sea Sediments
91(9)
Part 4.2 History of Discovery: Paleomagnetism in Ocean Crust and Marine Sediments
100(8)
Part 4.3 Using to Test the Seafloor Spreading Hypothesis
108(6)
Part 4.4 The Geomagnetic Polarity Timescale
114(5)
Chapter 5 Microfossils and Biostratigraphy 119(46)
Part 5.1 What Are Microfossils? Why Are They Important in Climate Change Science?
121(9)
Part 5.2 Microfossils in Deep-Sea Sediments
130(7)
Part 5.3 Application of Microfossil First and Last Occurrences
137(7)
Part 5.4 Using Microfossil Datums to Calculate Sedimentation Rates
144(5)
Part 5.5 How Reliable Are Microfossil Datums?
149(7)
Part 5.6 Organic-Walled Microfossils: Marine Dinoflagellates and Terrestrial Pollen and Spores
156(9)
Chapter 6 CO2 as a Climate Regulator During the Phanerozoic and Today 165(35)
Part 6.1 The Short-Term Global Carbon Cycle
167(2)
Part 6.2 CO2 and Temperature
169(10)
Part 6.3 Recent Changes in CO2
179(4)
Part 6.4 The Long-Term Global Carbon Cycle, CO2, and Phanerozoic Climate History
183(8)
Part 6.5 Carbon Isotopes as a Tool for Tracking Changes in the Carbon Cycle
191(9)
Chapter 7 Oxygen Isotopes as Proxies of Climate Change 200(26)
Part 7.1 Introduction to Oxygen Isotope Records from Ice and Ocean Sediments
202(3)
Part 7.2 The Hydrologic Cycle and Isotopic Fractionation
205(4)
Part 7.3 δ18O in Meteoric Water and Glacial Ice
209(9)
Part 7.4 δ18O in Marine Sediments
218(8)
Chapter 8 Climate Cycles 226(29)
Part 8.1 Patterns and Periodicities
228(17)
Part 8.2 Orbital Metronome
245(5)
Part 8.3 Glacial-Interglacial Peribds and Modern Climate Change
250(5)
Chapter 9 The Paleocene-Eocene Thermal Maximum (PETM) Event 255(59)
Part 9.1 An Important Discovery
257(3)
Part 9.2 Global Consequences of the PETM
260(36)
Part 9.3 Two Hypotheses for the Cause of the PETM
296(3)
Part 9.4 Rates of Onset and Duration of Event
299(7)
Part 9.5 Global Warming Today and Lessons from the PETM
306(8)
Chapter 10 Glaciation of Antarctica: The Oil Event 314(41)
Part 10.1 Initial Evidence
316(5)
Part 10.2 Evidence for Global Change
321(21)
Part 10.3 Mountain Building, Weathering, CO2 and Climate
342(7)
Part 10.4 Legacy of the Oi1 Event: The Development of the Psychrosphere
349(6)
Chapter 11 Antarctic Climate Variability in the Neogene 355(43)
Part 11.1 What Do We Think We Know About the History of Antarctic Climate?
358(4)
Part 11.2 What is Antarctica's Geographic and Geologic Context?
362(13)
Part 11.3 Selecting Drillsites to Best Answer our Questions
375(4)
Part 11.4 What Sediment Facies are Common on the Antarctic Margin?
379(11)
Part 11.5 The BIG Picture of ANDRILL 1-B
390(8)
Chapter 12 Pliocene Warmth as an Analog for Our Future 398(32)
Part 12.1 The Last 5 Million Years
400(7)
Part 12.2 Pliocene Latitudinal Temperature Gradient
407(7)
Part 12.3 Estimates of Pliocene CO2
414(2)
Part 12.4 Sea Level Past, Present, and Future
416(14)
Chapter 13 Climate, Climate Change, and Life 430(57)
Part 13.1 Initial Ideas
432(1)
Part 13.2 The Long View: "Precambrian" and Phanerozoic Life and Climate
433(8)
Part 13.3 Examples of Cenozoic Terrestrial Evolution and Climate Connections
441(17)
Part 13.4 Examples of Cenozoic Marine Biotic Evolution and Climate Connections
458(11)
Part 13.5 Humanity, Climate, and Life
469(12)
Part 13.6 Humanity and Future Climate: At a Tipping Point
481(6)
Chapter 14 Climate Change and Civilization 487(49)
Part 14.1 Climate Change Here and Now
489(8)
Part 14.2 Evidence of Climatic Stress on Ancient Maya Civilization
497(16)
Part 14.3 The Precipitation Record of the North American Southwest: The Physical Record and Human Response
513(23)
Index 536
About the Authors

Dr Kristen St. John is a Professor of Geology at James Madison University.

Dr R. Mark Leckie is a Professor of Geology at the University of Massachusetts-Amherst.

Dr Kate Pound is a Professor of Geology and a member of the Science Education Group at St. Cloud State University.

Dr Megan Jones is a Professor of Geology at North Hennepin Community College.



Dr Lawrence Krissek is a Professor Emeritus in the School of Earth Sciences, Ohio State University.