The air we breathe is twenty-one percent oxygen, an amount higher than on any other known world. While we may take our air for granted, Earth was not always an oxygenated planet. How did it become this way? Oxygen is the most current account of the history of atmospheric oxygen on Earth. Donald Canfield--one of the world's leading authorities on geochemistry, earth history, and the early oceans--covers this vast history, emphasizing its relationship to the evolution of life and the evolving chemistry of the Earth. With an accessible and colorful first-person narrative, he draws from a variety of fields, including geology, paleontology, geochemistry, biochemistry, animal physiology, and microbiology, to explain why our oxygenated Earth became the ideal place for life.
Describing which processes, both biological and geological, act to control oxygen levels in the atmosphere, Canfield traces the records of oxygen concentrations through time. Readers learn about the great oxidation event, the tipping point 2.3 billion years ago when the oxygen content of the Earth increased dramatically, and Canfield examines how oxygenation created a favorable environment for the evolution of large animals. He guides readers through the various lines of scientific evidence, considers some of the wrong turns and dead ends along the way, and highlights the scientists and researchers who have made key discoveries in the field.
Showing how Earth's atmosphere developed over time, Oxygen takes readers on a remarkable journey through the history of the oxygenation of our planet.
Donald E. Canfield is professor of ecology at the University of Southern Denmark and director of the Nordic Center for Earth Evolution (NordCEE). He is a member of the National Academy of Science, coauthor of Aquatic Geomicrobiology and coeditor of Fundamentals of Geobiology.
"His excellent descriptions of the scientific process show how competing hypotheses, and the scientists who present them, vie for supremacy. Canfield also offers a philosophical perspective: scientific understanding provides true insight into the structure of the natural world."--Publishers Weekly
"Engaging and authoritative."--Nature
"Concise and easily read, Oxygen provides an ideal starting block for those interested in learning about Earth's O2 history and, more broadly, the function and history of biogeochemical cycles. . . . The endnotes provide valuable entries for readers who wish to explore particular points in greater depth and, in other cases, enable brief digressions for interesting personal notes without disrupting the logical thread of a given concept. And the detailed bibliography captures a vast swath of the relevant primary literature. I highly recommend Canfield's book for anyone with even a remote interest in Earth history, as O2 singularly encompasses much of what makes our planet special."--Woodward W. Fischer, Science
"Oxygen takes readers on a remarkable journey through the history of the oxygenation of our planet."--Devorah Bennu, GrrlScientist at The Guardian
"This is the sort of science writing we would all do well to read more of. . . . Engage[s] with the ambiguity of a world where evidence is imperfect, knowledge evolves, and mistakes can be made in interpreting the data."--Ian Scheffler, Los Angeles Review of Books
"Oxygen: A Four Billion Year History will be an entertaining and informative read, however, for anyone with a serious interest in the long-term history of the Earth: students contemplating working in the area and specialists in related disciplines as well as engaged general readers."--Danny Yee, Danny Reviews
Table of Contents:
Chapter 1. What Is It about Planet Earth? 1
Chapter 2. Life before Oxygen 13
Chapter 3. Evolution of Oxygenic Photosynthesis 26
Chapter 4. Cyanobacteria: The Great Liberators 41
Chapter 5. What Controls Atmospheric Oxygen Concentrations? 56
Chapter 6. The Early History of Atmospheric Oxygen: Biological Evidence 72
Chapter 7. The Early History of Atmospheric Oxygen: Geological Evidence 85
Chapter 8. The Great Oxidation 98
Chapter 9. Earth's Middle Ages: What Came after the GOE 110
Chapter 10. Neoproterozoic Oxygen and the Rise of Animals 123
Chapter 11. Phanerozoic Oxygen 138
Chapter 12. Epilogue 153