Abstract
This chapter discusses the role of 14 C dating in sea-level research and includes a brief historical overview, an outline of the basic principles of 14 C dating, and a discussion of the differences between the radiometric approach and accelerator mass spectrometry (AMS). Sources of error in 14 C dating, specifically those relevant to sea-level studies, receive considerable attention. This includes uncertainties associated with isotopic fractionation and reservoir effects. The latter are of particular concern, especially in estuarine environments. Finally, 14 C calibration and various widely used programs to convert 14 C ages into calendar ages are discussed.
Original language | American English |
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Title of host publication | Handbook of Sea‐Level Research |
DOIs | |
State | Published - Jan 1 2015 |
Externally published | Yes |
Keywords
- accelerator mass spectrometry
- 14C variations
- calibration curves
- calibration software
- error assessment
- half-life
- isotopic fractionation
- radiometric dating
- reservoir effect
- wiggle matching
Disciplines
- Life Sciences