Book Review: Oxygen: A Four Billion Year History
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Katherine Byerly
Reviewed Publication:
Book Review: Oxygen: A Four Billion Year History. ( 2015 ) By Canfield Donald E.. Princeton University Press. ISBN: 9781400849888, 216 pp. Paperback $17.95.
A glance at the table of contents of Oxygen: A Four Billion Year History, by Donald Canfield (University of Southern Denmark) suggests that his book will be an up-to-date summary of almost the entire subject matter of oxygen levels through time. This is a heroic undertaking even for an Earth history and geochemistry specialist, and the book does not disappoint. A goal of the book is to bridge the gap between experts in their field and a more general readership interested in learning about Earth’s O2 history. The effort is as important as it is difficult, and the author achieves this with both personality and humanity.
Canfield begins with an interdisciplinary summary of present-day Earth processes and of the reasons the Earth is the premier planet for life. This chapter serves as both an introduction and review of topics such as the importance of water, sun-created thermal balance, and the carbon cycle. This chapter provides the most relatable and important background information that a non-specialist, who is interested in the evolution of the atmosphere, should know about our planet for these processes are the very ingredients of life itself.
Canfield is conservative where discussing oxygen content in the first billion years, describing it as “whiffs of oxygen” before the Great Oxidation Event (GOE). He cites that any free oxygen would quickly react with iron, until the point was reached that free oxygen began to overcome the iron “oxygen sinks,” launching into the single most important shift in Earth history—the GOE. It is at this point that Canfield addresses one of the “gaps” in research, starting with our inability to explain the approximately 900 million year gap from the debut of photosynthetic organisms to actual worldwide oxygenation.
Canfield uses the gap preceding worldwide oxygenation to initiate discussion of different hypotheses. In the case of the GOE oxygen gap, Canfield ultimately champions the idea that ocean floor iron kept ocean anoxia high during this time, but also touches on other hypotheses to show that our evidence is limited with new discoveries to be made.
The approach taken to explain conclusions and models in his sources illustrates a general strength of the book: Canfield explains the derivation of the conclusions and then follows them up with a discussion of their implications. His discussion of setting up the models, may lack some technical detail, but this is to help readers with less rigorous scientific backgrounds grasp the material. Science needs more researchers capable of breaking down complex scientific discoveries in an accessible, complete, and engrossing narrative. Canfield brings out his own personality and sheer enjoyment in the information being presented, all while providing true insight into fundamentals of our natural world.

© 2017 by Walter de Gruyter Berlin/Boston
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Artikel in diesem Heft
- Review: Minerals in the Human Body
- Mineral precipitation and dissolution in the kidney
- Special Collection: Nanominerals and Mineral Nanoparticles
- Luogufengite: A new nano-mineral of Fe2O3 polymorph with giant coercive field
- Special Collection: Apatite: A Common Mineral, Uncommonly Versatile
- Column anion arrangements in chemically zoned ternary chlorapatite and fluorapatite from Kurokura, Japan
- Special Collection: Apatite: A Common Mineral, Uncommonly Versatile
- Magmatic graphite inclusions in Mn-Fe-rich fluorapatite of perphosphorus granites (the Belvís pluton, Variscan Iberian Belt)
- Special Collection: Apatite: A Common Mineral, Uncommonly Versatile
- Barometric constraints based on apatite inclusions in garnet
- Special collection: Olivine
- A comparison of olivine-melt thermometers based on DMg and DNi: The effects of melt composition, temperature, and pressure with applications to MORBs and hydrous arc basalts
- Special collection: Dynamics of magmatic processes
- Water transfer during magma mixing events: Insights into crystal mush rejuvenation and melt extraction processes
- Special collection: Rates and depths of magma ascent on earth
- A new clinopyroxene-liquid barometer, and implications for magma storage pressures under Icelandic rift zones
- The S content of silicate melts at sulfide saturation: New experiments and a model incorporating the effects of sulfide composition
- Bond valence and bond energy
- Fluvial transport of impact evidence from cratonic interior to passive margin: Vredefort-derived shocked zircon on the Atlantic coast of South Africa
- Iron partitioning in natural lower-mantle minerals: Toward a chemically heterogeneous lower mantle
- Identifying biogenic silica: Mudrock micro-fabric explored through charge contrast imaging
- Compressibility and high-pressure structural behavior of Mg2Fe2O5
- Thermo-elastic behavior of grossular garnet at high pressures and temperatures
- Experimental constraints on the stability of baddeleyite and zircon in carbonate- and silicate-carbonate melts
- Polarized FTIR spectroscopic examination on hydroxylation in the minerals of the wolframite group, (Fe,Mn,Mg)[W,(Nb,Ta)][O,(OH)]4
- Tourmaline-rich features in the Heemskirk and Pieman Heads granites from western Tasmania, Australia: Characteristics, origins, and implications for tin mineralization
- Ca L2,3-edge near edge X-ray absorption fine structure of tricalcium aluminate, gypsum, and calcium (sulfo)aluminate hydrates
- Fluorwavellite, Al3(PO4)2(OH)2F·5H2O, the fluorine analog of wavellite
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