Radiocarbon dating

Radiocarbon dating uses the decay of a radioactive isotope of carbon (C-34) to measure time and date objects containing carbon-bearing material. With a half-life of 5,700 +/- 30 years, detection of C-34 is a useful tool for determining the age of a specimen formed over the past 55,000 years. In this Primer, we outline key advances in C-34 measurement and instrument capacity, as well as optimal sample selection and preparation. We discuss data processing, carbon reservoir age correction, calibration and statistical analyses. We then outline examples of radiocarbon dating across a range of applications, from anthropology and palaeoclirnatology to forensics and medical science. Reproducibility and minimum reporting standards are discussed along with potential issues related to accuracy and sensitivity. Finally, we look forwards to the adoption of radiocarbon dating in various fields of research thanks to continued instrument improvement.

Automated summary

Radiocarbon dating utilizes the decay of a radioactive isotope of carbon to measure time and date objects, proving particularly useful for specimens formed over the past 55,000 years. Advancements in measurement techniques, instrument capacity, sample selection, and data processing have expanded the application of radiocarbon dating across various fields.