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Calculator · Earth and life

Carbon dating calculator

Enter how much carbon-14 is left in a sample, as percent modern carbon or a fraction, and get its conventional radiocarbon age with the uncertainty. Watch the sample slide down the decay curve and sink into older layers of a dig.

Carbon-14 left, percent modern carbon
Fraction modern, F¹⁴C
Radiocarbon age
Measurement uncertainty, ± (optional)
Radiocarbon age…
Half-lives gone…
With 5,730 y half-life…
Carbon-14 atoms left…
Datable?…
Working

Conventional radiocarbon age, t = −8033 ln F¹⁴C, with the Libby half-life of 5,568 years, in years before 1950. Calendar dates need calibration with a curve such as IntCal20, which this tool does not do. See decay in action in the radioactive decay simulation.

Living things keep topping up

Plants take in carbon-14 made in the upper air, and animals eat the plants. While alive, they match the level in the air. When they die, the topping up stops.

about 1 in 1012 carbon atoms

Half gone every 5,568 years

Radiocarbon ages use Libby's half-life by convention. After one half-life 50% is left, after two 25%, and so on.

t = −8033 ln F

About 50,000 years at most

After nine half-lives only 0.2% is left, and a trace of modern carbon would swamp it. A radiocarbon age also needs calibrating to become a calendar date.

0.59 ≈ 0.2%

How do you calculate a carbon dating age?

Take the natural log of the fraction of carbon-14 left compared with the modern standard and multiply by −8033 years. A sample with 25% of modern carbon is −8033 × ln 0.25 = 11,136 years old in radiocarbon years, two half-lives. The 8033 years comes from Libby's half-life of 5,568 years, which radiocarbon labs still use by convention.

A radiocarbon age counts back from 1950 (BP, before present) and is not yet a calendar date: it must be calibrated with a curve such as IntCal20. The method reaches back about 50,000 years. How it all works is in How does carbon dating work, and how far back can it go?, and you can watch decay happen atom by atom in the radioactive decay simulation.

Key results

  • Conventional age: t = −8033 × ln(F¹⁴C) years before 1950, where F¹⁴C is the fraction of the modern carbon-14 level left.
  • Half-lives: 50% left is 5,568 years, 25% is 11,136 years, 12.5% is 16,704 years.
  • Libby or Cambridge: with the more accurate 5,730 year half-life, 25% left would take 11,460 years, about 3% longer. Labs report the Libby figure and calibration corrects for it.
  • Limit: after about 50,000 years only 0.2% is left, so standard dating stops around there.

Six worked examples

Each button loads the example into the calculator. The samples are illustrations, not particular finds.

Half the carbon-14 left: 5,568 years

one half-life

−8033 × ln 0.5 = 8033 × 0.693 = 5,568 years, exactly Libby's half-life. With the Cambridge half-life the same decay takes 5,730 years, which is why calibrated dates for this sample would come out older than the radiocarbon age.

Left 50% Radiocarbon age 5,568 years Cambridge 5,730 years Half-lives 1

90% left: 846 years

a recent sample

Only a tenth has decayed: −8033 × ln 0.90 = 846 years BP. A measurement uncertainty of ±0.3 pMC gives ±27 years. For young samples the wiggles in the calibration curve often matter more than the measurement.

Left 90 ± 0.3% Age 846 ± 27 Half-lives 0.15 Calendar date needs calibration

Charcoal with 25% left: 11,136 years

two half-lives

Two half-lives have passed, so −8033 × ln 0.25 = 11,136 years BP. At ±0.3 pMC the uncertainty is ±8033 × 0.003 ÷ 0.25 = ±96 years: the same absolute error matters more as less carbon-14 remains.

Left 25 ± 0.3% Age 11,136 ± 96 Cambridge 11,460 years Half-lives 2

2% left: 31,425 years

old sample

After 5.64 half-lives, ±0.1 pMC becomes ±402 years. At this level a tiny amount of modern carbon from roots, handling or the lab makes a big difference, which is why old samples are cleaned so carefully.

Left 2 ± 0.1% Age 31,425 ± 402 Half-lives 5.64 1% modern contamination reads as 28,222 years

0.15% left: past the 50,000 year limit

the limit

The arithmetic gives 52,233 years, but with ±0.05 pMC the uncertainty is ±2,678 years, and the carbon-14 left is no more than contamination could add. Labs report such samples as older than a limit instead of giving an age.

Left 0.15% Formula says 52,233 years Uncertainty ±2,678 years Report as older than ~50,000

More than 100%: post-bomb carbon

modern sample

Nuclear weapons tests in the 1950s and early 1960s roughly doubled the carbon-14 in the air. Anything that grew since then can carry more than the 1950 standard, so it cannot be given a radiocarbon age. Instead it is matched against records of bomb carbon in the air, a method used in forensics and biology.

Left 120% Radiocarbon age none Air peak about double Dated by post-bomb curves

Carbon-14 left and conventional radiocarbon age

Carbon-14 leftHalf-livesRadiocarbon age (Libby)With 5,730 y half-life
90%0.152846 BP871 years
75%0.4152,311 BP2,378 years
50%15,568 BP5,730 years
25%211,136 BP11,460 years
10%3.3218,497 BP19,035 years
5%4.3224,065 BP24,765 years
1%6.6436,993 BP38,069 years
0.5%7.6442,561 BP43,799 years
0.2%8.9749,922 BP51,374 years

Conventional radiocarbon ages, t = −8033 ln F, in years before 1950. These are not calendar ages: calibrate them with IntCal20 or its Southern Hemisphere and marine counterparts.

How the calculator works

Percent modern carbon (pMC) is 100 × F¹⁴C, the sample's carbon-14 level as a fraction of the modern standard, after the lab's corrections. The tool works with F¹⁴C.

The conventional radiocarbon age is t = −8033 × ln(F¹⁴C) years BP, where 8033 is the mean life from Libby's half-life of 5,568 years and BP counts back from 1950. That convention was kept in 1962 so older results stay comparable, even though the half-life is now known to be about 5,730 years.

An uncertainty in F becomes an uncertainty in age of 8033 × σF ÷ F years. The tool also shows how long the same decay would take with the 5,730 year half-life.

Above 100% modern the sample is post-bomb and has no radiocarbon age. Below about 0.2% (around 50,000 years) the result is beyond the practical limit.

What the model leaves out

  • Calibration: turning a radiocarbon age into calendar years needs a calibration curve such as IntCal20, which covers 0 to 55,000 calendar years before 1950. This tool does not calibrate.
  • Reservoir effects: sea creatures and some lake samples take up older carbon, so they look older; marine samples need the marine calibration curve and a local correction.
  • Isotope corrections: labs correct for the way plants take up carbon isotopes unequally (δ¹³C). Enter the lab's corrected pMC or F¹⁴C.

Common misconceptions

"Carbon dating can date dinosaurs." No. Dinosaurs died out tens of millions of years ago; after about 50,000 years there is too little carbon-14 left. Rocks are dated with other isotopes.

"A radiocarbon age is a calendar date." It needs calibrating. The amount of carbon-14 in the air has changed over time.

"Labs use the wrong half-life." They use Libby's by agreement, and calibration curves are built with the same convention, so calibrated dates come out right.

Frequently asked questions

How do you calculate a radiocarbon age?

Multiply the natural log of the fraction of modern carbon left by −8033 years. 25% left gives −8033 × ln 0.25 = 11,136 years before 1950.

What is the half-life of carbon-14?

About 5,730 years (the Cambridge value). Radiocarbon ages are still calculated with Libby's earlier value of 5,568 years by convention, and calibration curves correct for the difference.

How far back can carbon dating go?

About 50,000 years with standard methods, when only about 0.2% of the original carbon-14 is left. Special preparation can sometimes reach 60,000 years or more.

What does BP mean in radiocarbon dating?

Before present, where the present is fixed at 1950. A radiocarbon age of 1,000 BP means 1,000 radiocarbon years before 1950.

Why do radiocarbon dates need calibration?

The carbon-14 level in the air has varied, so a radiocarbon age does not map exactly onto calendar years. Calibration curves such as IntCal20, built from tree rings and other dated records, convert one into the other.

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