Carbon-14 Dating Calculator
Calculate radiocarbon age and remaining C-14 activity for archaeological dating.
How Radiocarbon Dating Works
Cosmic rays continuously produce carbon-14 in the upper atmosphere, where it mixes as CO2 and enters the food chain. While an organism lives it exchanges carbon with the environment and maintains the atmospheric 14C ratio. At death that exchange stops, and the clock starts.
| Half-lives elapsed | Fraction remaining | Age (years) |
|---|---|---|
| 1 | 50% | 5,730 |
| 2 | 25% | 11,460 |
| 3 | 12.5% | 17,190 |
| 5 | 3.1% | 28,650 |
| 8 | 0.39% | 45,840 |
| 10 | 0.098% | 57,300 |
The practical limit is around 50,000 years, roughly nine half-lives. Beyond that, so little 14C remains that contamination by even a trace of modern carbon overwhelms the signal. A sample 50,000 years old retains about 0.2% of its original activity.
Why It Only Works on Once-Living Material
The method requires that the sample started with the atmospheric ratio. That is true only for organisms that took up carbon from the biosphere — wood, bone, textile, charcoal, shell. Rocks never contained atmospheric carbon, which is why 14C cannot date them; potassium-argon and uranium-lead serve there instead, with half-lives in the billions of years.
Calibration and Its Corrections
| Effect | Cause | Correction |
|---|---|---|
| Atmospheric variation | Cosmic ray flux and carbon cycle changes | Calibration curves from tree rings and corals |
| Suess effect | Fossil fuel CO2 since 1850 dilutes 14C | Post-1950 samples need special handling |
| Bomb pulse | Nuclear testing doubled atmospheric 14C in the 1960s | Enables very precise dating of recent material |
| Reservoir effect | Marine carbon is older than atmospheric | Several hundred year offset for marine samples |
| Libby half-life | Original 5,568-year value still used in reporting | Conventional dates use it, then calibrate |
Raw radiocarbon years are not calendar years. Dates are reported as “BP” — before present, meaning before 1950 — and then converted using calibration curves such as IntCal, which are built from tree ring sequences extending back more than 12,000 years.
Worked Examples
Common Mistakes
Only material that exchanged carbon with the atmosphere while alive can be dated. Rocks require potassium-argon or uranium-lead methods with far longer half-lives.
Atmospheric 14C has varied over time, so raw dates must be calibrated against tree ring records. The correction can exceed several hundred years.
After nine half-lives, remaining activity is so low that trace modern contamination dominates. Older samples need different isotope systems.
Ocean carbon is several hundred years older than atmospheric carbon. Marine shells and fish bone need a reservoir correction before calibration.
Frequently Asked Questions
Formula Explorer connections
Interpretation: This relationship connects isotopic composition, decay, radiation, mass defect or nuclear energy to a measurable quantity. Assumption: Use the correct nuclide, decay constant, branching behavior and time units. Radiation estimates also depend on geometry, shielding and detector response.