Readership: earth science students at a variety of levels studying paleoclimatology, oceanography, Quaternary science, or earth–system science.
Book Introduction for Students and Instructors
Chapter 1. Introduction to Paleoclimate Records.
Part 1.1. Archives and Proxies
Part 1.2. Owens Lake An Introductory Case Study of Paleoclimate Reconstruction
Part 1.3. Coring Glacial Ice and Seafloor Sediments
Chapter 2. Seafloor Sediments.
Part 2.1. Sediment Predictions
Part 2.2. Core Observations and Descriptions
Part 2.3. Sediment Composition
Part 2.4. Geographic Distribution and Interpretation
Chapter 3. Microfossils and Biostratigraphy.
Part 3.1. What are Microfossils? Why are they Important in Climate Change Science?
Part 3.2. Microfossils in Deep–sea Sediments
Part 3.3. Application of Microfossil First and Last Occurrences
Part 3.4. Using Microfossil Datums to Calculate Rates
Part 3.5. How Reliable are Microfossil Datums?
Chapter 4. Paleomagnetism and Magnetostratigraphy.
Part 4.1. Earth′s Magnetic Field Today and the Paleomagnetic Record of Deep–Sea Sediments
Part 4.2. Paleomagnetism in Ocean Crust
Part 4.3. Using Paleomagnetism to Test the Seafloor Spreading Hypothesis
Part 4.4. The Geomagnetic Polarity Time Scale
Chapter 5. CO2 as a Climate Regulator during the Phanerozoic and Today.
Part 5.1. The Short Term Global Carbon Cycle
Part 5.2. CO2 and Temperature
Part 5.3. Recent Changes in CO2
Part 5.4. The Long–term Global Carbon Cycle, CO2, and Phanerozoic Climate History
Chapter 6. The Benthic Foraminiferal Oxygen Isotope Record of Cenozoic Climate Change.
Part 6.1. Introduction
Part 6.2. Stable Isotope Geochemistry
Part 6.3. A Biogeochemical Proxy
Part 6.4. Patterns, Trends and Implications for Cenozoic Climate
Chapter 7. Scientific Drilling in the Arctic Ocean: A Lesson on the Nature of Science.
Part 7.1. Climate Models and Regional Climate Change
Part 7.2. Arctic Drilling Challenges and Solutions
Part 7.3. The Need for Scientific Drilling
Part 7.4. Results of the Arctic Drilling Expedition
Chapter 8. Climate Cycles.
Part 8.1. Patterns and Periodicities
Part 8.2. Orbital Metronome
Part 8.3. A Break in the Pattern
Chapter 9. The Paleocene Eocene Thermal Maximum (PETM) Event.
Part 9.1. The Cenozoic 13C Record and an Important Discovery
Part 9.2. Global Consequences of the PETM
Part 9.3. Bad Gas: Is Methane to Blame?
Part 9.4. How fast? How long?
Part 9.5. Global Warming Today and Lessons from the PETM
Chapter 10. Glaciation of Antarctica: The Oi1 Event.
Part 10.1. Initial Evidence
Part 10.2. Evidence for Global Change
Part 10.3. Mountain Building, Weathering, CO2 and Climate
Part 10.4. Legacy of the Oi1 Event: The Development of the Psychrosphere
Chapter 11. Antarctica and Neogene Global Climate Change.
Part 11.1. What do we Think we Know about the History of Antarctic Climate?
Part 11.2. What is Antarctica s Geographic & Geologic Context?
Part 11.3. Selecting Drillsites to Best Answer our Questions
Chapter 12. Interpreting Antarctic Sediment Cores: A Record of Dynamic Neogene Climate.
Part 12.1. What Sediment Facies are Common on the Antarctic Margin?
Part 12.2. ANDRILL 1–B The BIG Picture
Part 12.3. Pliocene Sedimentary Patterns in the ANDRILL 1–B Core
13. Pliocene Warmth: Are We Seeing Our Future?
Part 13.1. The last 5 million years
Part 13.2. Sea Level Past, Present, and Future
Chapter 14. Northern Hemisphere Glaciation.
Part 14.1. Concepts & Predictions
Part 14.2. What is the Evidence?
Part 14.3. What Caused It?
"In developing Reconstructing Earth′s Climate History, St John et al. say that they were driven by the philosophy that "addressing how we know is as important as addressing what we know about past climate". They have, without question, lived up to the billing. The book is composed of exercises based on authentic data, with well–constructed, full–color graphs, photos, tables, and diagrams. In fact, the graphic elements are the central features of this book, and the text, which is mostly organized by series of questions, tasks, and boxes, is supplementary – an entirely refreshing and inviting format that is designed to enhance inquiry–based learning by working directly with real paleoclimate data and their underlying geological concepts...St John et al. have provided a tremendous educational gift to the paleoclimate community. If you are in the field and want a textbook that will be sure to stimulate student interest in this important topic, look no further." (Eos, April 2013)
"This publication has added value for and warmly recommend to support not only courses in palaeoclimatology, but also courses in a wider array of interdisciplinary environmental sciences. (Int. J. Environment and Pollution, 1 May 2013)