Reconstructing Earth's Climate History

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Kristen St. John. Reconstructing Earth's Climate History
Table of Contents
List of Tables
List of Illustrations
Guide
Pages
Reconstructing Earth's Climate History. Inquiry‐Based Exercises for Lab and Class
The Authors
Foreword from First Edition
Acknowledgments
Book Introduction to the Second Edition for Students and Instructors
Motivation and Purpose
Use of Real Data
Content Topics
Transportable Skills
Practical Use of Multipart Exercises
Audience
Classroom Tested
About the Companion Website
Chapter 1 Introduction to Paleoclimate Records
SUMMARY
Part 1.1. Archives and Proxies
Part 1.2. Obtaining Cores from Terrestrial and Marine Paleoclimate Archives
Coring Terrestrial Paleoclimate Archives
Tree Rings: Dendrochronology
Cave Deposits: Speleothems
Glacial Ice
Coring Marine Paleoclimate Archives. Corals
Ocean Sediments
Part 1.3. Owens Lake – An Introductory Case Study of Paleoclimate Reconstruction
References
Chapter 2 Seafloor Sediments
SUMMARY
Part 2.1. Sediment Predictions
Part 2.2. Core Observation and Description. Introduction
Part 2.3. Sediment Composition. Introduction
DETERMINING LITHOLOGIC NAMES WITH A DECISION TREE
Part 2.4. Seafloor Sediment Synthesis
References
Chapter 3 Geologic Time and Geochronology. SUMMARY
Part 3.1. The Geologic Timescale. Introduction
Initial Observations
Part 3.2. Principles of Stratigraphy and Determining Relative Ages. Using Principles of Stratigraphy to Determine Relative Ages
Part 3.3. Radiometric Age Dating Fundamentals. Introduction to Radiometric Age Dating
Limitations on Radiometric Dating Techniques
Part 3.4. Using 40K – 40Ar Dating to Determine the Numerical Ages of Layered Volcanic Rocks. Introduction to a Case Study from Jokuldalur, Iceland
Extension: Radiometric Dating and the Development of the Geomagnetic Polarity Timescale
Part 3.5. Using Uranium Series Dating to Determine Changes in Growth Rate of Speleothems. An Introduction to Radiometric Dating of Sediments and Sedimentary Rocks
An Introduction to Uranium Series Dating of Corals and Speleothems
A Case Study of Speleothem Dating using 234U – 230Th
References
Chapter 4 Paleomagnetism and Magnetostratigraphy
SUMMARY:
Part 4.1. Earth's Magnetic Field Today and the Paleomagnetic Record of Deep‐Sea Sediments. Initial Ideas
Earth's Magnetic Field Today: A Useful Analogy
Why Do We Care About Paleomagnetism?
Natural Remanent Magnetization in Sediments and Igneous Rocks
Paleomagnetic Reversals (i.e. Reversals of Magnetic Polarity)
Paleomagnetism in Sediment Cores
Part 4.2. History of Discovery: Paleomagnetism in Ocean Crust and Marine Sediments. Magnetic Intensity Data from the East Pacific Rise
Seafloor Magnetic Anomalies
Connecting Magnetic Data from the Sea and Land
Part 4.3. Using Paleomagnetism to Test the Seafloor Spreading Hypothesis. The Seafloor Spreading Hypothesis
Application of Paleomagnetism
Part 4.4. The Geomagnetic Polarity Timescale
References
Chapter 5 Microfossils and Biostratigraphy
SUMMARY
Part 5.1. What Are Microfossils? Why Are They Important in Climate Change Science? Introduction
Trophic Levels and Productivity
Marine Microfossils of the Mesozoic and Cenozoic Eras
Part 5.2. Microfossils in Deep‐Sea Sediments. Initial Ideas
Microfossils in Smear Slides
Biostratigraphy Case Study: A First Look at Calcareous Nannofossil Data from ODP Hole 1208A
Part 5.3. Application of Microfossil First and Last Occurrences. Introduction
Biostratigraphy Overview
Biostratigraphy Case Study: Applying a Biostratigraphic Zonal Scheme to ODP Hole 1208A
Part 5.4. Using Microfossil Datums to Calculate Sedimentation Rates. Introduction to Sedimentation Rates
Case Study: Determining Sedimentation Rates at ODP Hole 1208A
Part 5.5. How Reliable Are Microfossil Datums? Introduction
Comparison of Sediment Accumulation Rate Histories
Part 5.6. Organic‐Walled Microfossils: Marine Dinoflagellates and Terrestrial Pollen and Spores. Introduction to Palynomorphs
Palynomorphs Case Study: Hole M27A on the New Jersey Continental Shelf
References
Chapter 6 CO2 as a Climate Regulator During the Phanerozoic and Today
SUMMARY
Part 6.1. The Short‐Term Global Carbon Cycle. Introduction
Part 6.2. CO2 and Temperature. The Greenhouse Effect
A Special Note about Ozone
The Direct Effect of CO2 on Temperature: Understanding Radiative Forcing
Other Radiative Forcing Factors
Indirect Effects of CO2 on Temperature: Earth System Feedbacks
Temperature Sensitivity
Part 6.3. Recent Changes in CO2
Part 6.4. The Long‐Term Global Carbon Cycle, CO2, and Phanerozoic Climate History. The Long‐Term Carbon Cycle
CO2 and Long‐Term Climate History: What Proxies and Models Tell Us
Long‐Term Climate States: Greenhouse and Icehouse Worlds
Predictions of Future CO2 Levels
Our Species and the CO2 Story
Part 6.5. Carbon Isotopes as a Tool for Tracking Changes in the Carbon Cycle. Introduction
UNDERSTANDING STABLE CARBON ISOTOPES
The Atmospheric δ13C Record of the Recent Past
Trends in Global Ocean δ13C for the Past 80 Million Years
References
Chapter 7 Oxygen Isotopes as Proxies of Climate Change
SUMMARY
Part 7.1. Introduction to Oxygen Isotope Records from Ice and Ocean Sediments. Introduction
Part 7.2. The Hydrologic Cycle and Isotopic Fractionation. Introduction
Stable Isotopes of Oxygen
Hydrologic Cycle and Isotopic Fractionation
Part 7.3. δ18O in Meteoric Water and Glacial Ice. Introduction
Temperature‐Dependent Fractionation
MEASURING δ18O IN METEORIC WATER AND ICE
Revisiting the Pleistocene–Holocene δ18O Greenland Ice Sheet Record
Hydrogen: Another Isotopic Paleotemperature Proxy in Ice
Comparison of Isotopic Paleotemperature Proxies and CO2 in Ice
Part 7.4. δ18O in Marine Sediments. An Application of Important Marine Microfossils
A Biogeochemical Proxy for Ice Volume and Temperature
MEASURING δ18O FROM MARINE MICROFOSSILS
Using the Marine δ18O Record to Interpret Cenozoic Climate Change
References
Chapter 8 Climate Cycles
SUMMARY
Part 8.1. Patterns and Periodicities. Introduction
Record 1. Greenhouse Gases in the Vostok Ice Core, Antarctica
Record 2. Magnetic Susceptibility in Loess and Soil, Central China
Record 3. Freshwater Diatoms, North Atlantic Ocean
Record 4. Benthic Oxygen Isotopes, Global Ocean
Record 5. Terrestrial Pollen and Spores, Marine Microfossils, and Ice‐rafted Debris, Central Arctic Ocean
Record 6. Color Reflectance of Lacustrine Mudstone and Limestone, NE Spain
Record 7. Color Reflectance and Sediment Bulk Density, Shatsky Rise, NW Pacific Ocean
Synthesis
Case Study of Record 7 from Shatsky Rise, NW Pacific
Smear Slide Compositional Data
XRF Elemental Composition Data
Part 8.2. Orbital Metronome. Annual Cyclicity
Long‐term Changes of Earth's Geometry in Space Relative to the Sun
Orbital Control of Earth's Climate Cycles
Part 8.3. Glacial–Interglacial Periods and Modern Climate Change. Characterizing Glacial and Interglacial Periods
Situating Modern Climate Change within the Glacial–Interglacial Cycles
References
Chapter 9 The Paleocene–Eocene Thermal Maximum (PETM) Event
SUMMARY
Part 9.1. An Important Discovery. Introduction
Dynamic Science
Part 9.2. Global Consequences of the PETM. Global Data Exploration
Record A. Benthic Foram Carbon and Oxygen Stable Isotope Records from Multiple Deep‐Sea Sites
Record B1. ODP Leg 198 Sites on Shatsky Rise in the Paleo‐Subtropical Pacific
Record B2. Stable Isotope Data from ODP Leg 198 Site 1209 on Shatsky Rise
DEEP‐SEA CARBONATE AND THE CALCITE (OR CARBONATE) COMPENSATION DEPTH (THE “CCD”)
Record B3. Planktic and Benthic Foram Changes at ODP Leg 198 Sites 1209 and 1210, Shatsky Rise
Record C. ODP Leg 199 Sites 1220 and 1221 in the Paleo‐Tropical Central Pacific
Record D. ODP Leg 113 Site 690 in the Southern High Latitudes Near Antarctica
Record E. ODP Leg 208 Sites on Walvis Ridge in the Southeast Atlantic
Record F. Environmental Changes on the Paleo‐Continental Shelf of Eastern North America
Record G. The Arctic Ocean, Lomonosov Ridge, IODP Expedition 302
Record H. The North Atlantic Igneous Province and the Opening of the Northern North Atlantic
Record I. Floral Changes in Wyoming
Record J. Clay Mineral Changes in North Dakota
Synthesis and Discussion
Part 9.3. Two Hypotheses for the Cause of the PETM
Part 9.4. Rates of Onset and Duration of Event. How Quickly Did the PETM Carbon Isotope Excursion Occur?
High Resolution Exploration of the Onset and Duration of the PETM
Part 9.5. Global Warming Today and Lessons from the PETM. Introduction
Comparing Rates of Global Warming and Carbon Accumulation for the PETM and Today
Thinking About the PETM Recovery and Our Future
References
NOTES
Chapter 10 Glaciation of Antarctica: The Oi1 Event
SUMMARY
Part 10.1. Initial Evidence. Introduction
Initial Observations from ODP Site 748
Part 10.2. Evidence for Global Change. Introduction
Record A1. High‐resolution Record of the Oi1 Event at ODP Site 1218 (ODP Leg 199) in the Tropical Pacific
DEEP‐SEA CARBONATE AND THE CALCITE (OR CARBONATE) COMPENSATION DEPTH (THE “CCD”)
Record A2. The Eocene–Oligocene Transition and the Oi1 Event in the Deep Sea Tropical Pacific (ODP Leg 199)
Record B. The Eocene–Oligocene Transition and the Oi1 Event in the Deep Sea Southeast Atlantic along the Walvis Ridge (ODP Leg 208)
Record C. The Eocene–Oligocene transition on the South Tasman Rise (ODP Leg 189)
Record D1. The Eocene–Oligocene Transition at Site 699, Southern South Atlantic (ODP Leg 114)
Record D2. High‐resolution Records of the Eocene–Oligocene Transition in the Southern Ocean: Southern Kerguelen Plateau Sites 748 (ODP Leg 120) and 744 (ODP Leg 119), and Maud Rise Site 689 (ODP Leg 113)
Record E. New Jersey Coastal Plain and Continental Margin Sea Level Reconstruction
Record F. Tanzania Coastal Plain Biotic Turnover
Synthesis and Discussion
Part 10.3. Mountain Building, Weathering, CO2 and Climate
Putting it All Together
Alternate Hypotheses for the Glaciation of Antarctica
Part 10.4. Legacy of the Oi1 Event: The Development of the Psychrosphere
Water Masses and Water Column Stratification
The Psychrosphere, Deep Water Masses, and Thermohaline Circulation
References
Chapter 11 Antarctic Climate Variability in the Neogene
SUMMARY
Part 11.1. What Do We Think We Know About the History of Antarctic Climate? Introduction
Part 11.2. What is Antarctica's Geographic and Geologic Context? Weather
Antarctic Ice
Bedrock Geology of the McMurdo Sound Region
The Cenozoic Sedimentary Sequence in the Ross Sea Region
Challenges Associated with Obtaining a Drillcore
Part 11.3. Selecting Drillsites to Best Answer our Questions. Introduction
Selecting Two Drillsites
Part 11.4. What Sediment Facies are Common on the Antarctic Margin? Introduction
Ice‐proximal and Ice‐distal Lithologies
LITHOLOGY: DIATOMITE
LITHOLOGY: SEDIMENT CONTAINING ICEBERG‐RAFTED DEBRIS
LITHOLOGY: DIAMICT
LITHOLOGY: WELL‐SORTED SANDS AND/OR GRAVELS
SEDIMENTARY FACIES
SEQUENCE MOTIFS
Part 11.5. The BIG Picture of ANDRILL 1‐B. About ANDRILL
LITHOSTRATIGRAPHIC UNITS (LSUs)
References
Chapter 12 Pliocene Warmth as an Analog for Our Future
SUMMARY
Learning Objectives
Part 12.1. The Last 5 Million Years. 12.1 Initial Observations: Pliocene vs. Modern Geography
The Deep‐Sea Benthic Foraminiferal Oxygen Isotope Record
Comparison of Climate Cyclicity in Deep‐Sea Oxygen Isotopes and Antarctic Marine Sediments
Continental Record of the Late Pliocene and Pliocene–Pleistocene Transition: Lake E, NE Siberia
Part 12.2. Pliocene Latitudinal Temperature Gradient. The Pliocene Research, Interpretation and Synoptic Mapping (PRISM) Project
Part 12.3. Estimates of Pliocene CO2. Atmospheric Carbon Dioxide and Global Climate
Part 12.4. Sea Level Past, Present, and Future. Pliocene Sea Level Compared with Pleistocene Interglacials
What if Global Warming Causes Ice Sheet Collapse this Century?
Relative Sea Level Rise Has Begun
Future Sea Level Rise
References
Chapter 13 Climate, Climate Change, and Life
SUMMARY
Learning Objectives
Part 13.1. Initial Ideas
Part 13.2. The Long View: “Precambrian” and Phanerozoic Life and Climate. Overview of Early Life on Earth
Exploring Evolutionary Relationships Between Animals and the Base of the Food Chain
Exploration 1: Evolutionary Relationships between Animals and Land Plants in the Late Paleozoic
Exploration 2: Marine Phytoplankton and Animal Evolution in the Mesozoic and Cenozoic Eras
Part 13.3. Examples of Cenozoic Terrestrial Evolution and Climate Connections
Mammal Evolution in the Aftermath of the K/Pg Mass Extinction and PETM
Early Primates and the PETM
Large Terrestrial Mammals and Global Climate During the Cenozoic
Coevolution of Horses and Grasses
Global Climate and the Spread of Grasslands
Part 13.4. Examples of Cenozoic Marine Biotic Evolution and Climate Connections. Biosiliceous Sediments and the Climate Connection
Climate Connections
Evolution of Marine Ecosystems During the Cenozoic: Diatoms to Whales
Abstract
Summary Points (Modified Slightly from Uhen 2010)
Synthesis
Part 13.5. Humanity, Climate, and Life
Hominin Evolution and Climate Change
Human Population and Alteration of the Earth
The Anthropocene: A New Geologic Time Unit?
Part 13.6. Humanity and Future Climate: At a Tipping Point
References
Chapter 14 Climate Change and Civilization
SUMMARY
Learning Objectives
Part 14.1. Climate Change Here and Now. Recent Changes Globally to Locally
Vulnerability and Readiness
Part 14.2. Evidence of Climatic Stress on Ancient Maya Civilization. Introduction
Regional Tropical Climate
The Cariaco Basin Geologic Setting and Sediment Record
The Cariaco Basin Paleoclimate Record – Extreme Events
The Lake Chichancanab Paleoclimate Record – A Local Perspective
The Lake Punta Laguna Paleoclimate Record – Another Local Perspective
Synthesis
Part 14.3. The Precipitation Record of the North American Southwest: The Physical Record and Human Response. Introduction
Examining Current Drought Conditions in the Four Corners Region
Reconstructing the Local History of Precipitation Using Proxy Data from Tree Rings
Reconstructing Drought Conditions in the Four Corners Region from Tree Rings
Expanding to a Regional‐Scale View of Drought
Water Availability and the Anasazi
From Proxies to the Instrumental Record
From the Past and Present into the Future
References
Index
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Second edition
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In using this inquiry‐based book we hope you gain new knowledge, new skills, and greater confidence in making sense of the causes and consequences of climate change. Enjoy the challenge and the reward of working with scientific data and results!
Kristen St. John, Mark Leckie, Kate Pound, Megan Jones, and Larry Krissek
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