Geoscientists use radiocarbon, or carbon-14, to establish a chronology of Earth’s processes. Because of the 5,730 ± 40 year half-life of this isotope, carbon-14 dating is used in disciplines like geology, archaeology, geochemistry, oceanography, forensic sciences, and more. Levels of carbon-14 in the atmosphere have varied greatly. This variation has natural causes, such as solar magnetic activity and ocean circulation, but since the industrial period, they can also be anthropogenic, such as the burning of fossil fuels or nuclear bombs and tests.
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Annual Review of Earth and Planetary Sciences, Volume 42, 2014
The Annual Review of Earth and Planetary Sciences, in publication since 1973, covers significant developments in all areas of earth and planetary sciences, from climate, environment, and geological hazards to the formation of planets and the evolution of life.
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| Weight | 2 kg |
|---|---|
| Dimensions | 24 × 19 × 4 cm |
| Book Author | Katherine H. Freeman, Raymond Jeanloz |
| Format | Hardback |
| Importers | Saras Books |
| ISBN | 9780824320423 |
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