Carbon-14 Dating Calculator

Compute the age of an organic sample from the fraction of carbon-14 remaining, or vice versa.

Science t½ 5730 yr Age 0–57k Two modes
Rate this calculator · 4.0 (2)

Carbon-14 Dating

t = −(t½/ln 2)·ln(N/N₀) · half-life 5730 yr · limit ~57,000 yr

Instructions — Carbon-14 Dating Calculator

1

Choose the mode

Mode 1: enter the fraction of C-14 remaining (N/N₀) and get the age. Mode 2: enter the age and get the expected fraction remaining. Default half-life is 5730 years (Cambridge half-life).

2

Enter the fraction

The fraction N/N₀ ranges from 1 (fresh sample) to ~0 (very old). 0.5 means one half-life has elapsed = 5730 years old. Modern measurement noise sets a practical floor around 0.001 (about 57,000 years).

3

Read the age

The output shows the radiocarbon age in years and the number of half-lives elapsed. Real archaeology adds a calibration step (IntCal, SHCal) to convert radiocarbon years to calendar years.

Formulas

Exponential decay
$$ N(t) = N_0 \cdot e^{-\lambda t} $$
N(t) is the number of C-14 atoms remaining at time t. N₀ is the initial count (equal to the atmospheric value when the organism stopped exchanging carbon). λ is the decay constant.
Decay constant for C-14
$$ \lambda = \frac{\ln 2}{t_{1/2}} = \frac{0.693}{5730} \approx 1.21 \times 10^{-4}\,\text{yr}^{-1} $$
Each year, about 0.012% of the remaining C-14 in a sample decays. After 5730 years exactly half is gone.
Age from fraction remaining
$$ t = -\frac{1}{\lambda} \ln\!\left( \frac{N}{N_0} \right) = -\frac{t_{1/2}}{\ln 2} \ln\!\left( \frac{N}{N_0} \right) $$
Solve the decay equation for time. A sample with 25% C-14 remaining is two half-lives old (~11,460 yr). 12.5% is three half-lives (~17,190 yr).
Using half-lives directly
$$ N(t) = N_0 \cdot \left( \frac{1}{2} \right)^{t / t_{1/2}} $$
An equivalent form that uses base-2 instead of base-e. Useful for quick mental math: each half-life halves the remaining fraction.

Reference

Half-life table for radiocarbon
Half-livesYears elapsed% C-14 remaining
00100.00 %
15,73050.00 %
211,46025.00 %
317,19012.50 %
422,9206.25 %
528,6503.125 %
634,3801.5625 %
845,8400.391 %
1057,3000.098 %

What radiocarbon can and cannot date

  • Works for — wood, charcoal, bone collagen, textiles, peat, papyrus, leather, shell carbonate (recent corals)
  • Effective range — about 500 to 50,000 years; AMS can push to ~57,000
  • Too young — < 200 years; modern atmospheric C-14 spike from 1950s atomic tests confounds the signal
  • Too old — > 57,000 years; switch to K-Ar (250k+ years) or U-Pb (10⁶+ years)
  • Not applicable — pure minerals, metals, ceramics (no organic carbon)
  • Calibration — radiocarbon years differ from calendar years; IntCal20 and SHCal20 are the international standards

Article — Carbon-14 Dating Calculator

Carbon-14 Dating Calculator: Age from Radiocarbon Fraction Remaining

Carbon-14 dating uses the formula t = −(t½ / ln 2) · ln(N/N₀), where t½ is the C-14 half-life of 5730 years and N/N₀ is the ratio of radiocarbon remaining compared to a living sample. A bone with half the modern C-14 level is one half-life old (5730 years). A quarter level is two half-lives (11,460 years). Modern accelerator mass spectrometry (AMS) pushes the practical limit to about 57,000 years — 10 half-lives — where only 0.1% of the original C-14 remains. Willard Libby developed the method between 1946 and 1949 and won the 1960 Nobel Prize in Chemistry for it; modern radiocarbon labs date Egyptian mummies, charcoal from cave paintings, and forensic remains with precision of ±30 to 50 years for samples younger than 5,000 years old.

This calculator runs in two directions. Enter the fraction of C-14 remaining (between 0 and 1) and get the age. Or enter the age and get the expected fraction. Default half-life is the Cambridge value of 5730 years; the calculator lets you change it for special applications (Libby's original value was 5568 years).

What is carbon-14 dating

Carbon-14 dating, also called radiocarbon dating, is a way to estimate the age of organic materials by measuring how much carbon-14 remains in a sample. Living organisms continuously exchange carbon with the atmosphere through photosynthesis and the food chain, so their tissues hold the atmospheric ratio of C-14 to C-12. When the organism dies, exchange stops and the C-14 begins to decay at a known rate. Measuring the remaining C-14 and comparing it to the modern atmospheric ratio gives the elapsed time since death.

The method works because C-14 is unstable and decays to N-14 by emitting a beta particle (an electron and antineutrino). C-12 and C-13 are stable, so the ratio C-14/C-12 decreases with time at a predictable rate.

Did you know

Atmospheric nuclear tests between 1945 and 1963 nearly doubled the C-14 content of the atmosphere — the so-called "bomb spike." Modern wines, oils, and forensic tissues can be dated within a few years by where they fall on the bomb curve as atmospheric C-14 declines back toward natural levels. The bomb spike is now Earth's most precise short-term radiometric clock.

Carbon dating formula and half-life

The carbon dating formula is t = −(t½ / ln 2) · ln(N/N₀), derived from the exponential decay law N = N₀·e^(−λt). λ = ln 2 / t½ is the decay constant, equal to 1.21 × 10⁻⁴ per year for C-14. The half-life is 5730 years (the Cambridge value), measured precisely in the 1960s. Libby used 5568 years originally; the difference is small but matters for very old samples and is automatically handled by calibration curves.

An equivalent form uses base-2: N(t) = N₀ · (1/2)^(t/t½). This makes it easy to count half-lives mentally: 50% remaining is one half-life (5730 yr), 25% is two (11,460 yr), 12.5% is three (17,190 yr), and so on.

Half-life shortcuts
1 half-life 5730 yr / 50%
2 half-lives 11,460 yr / 25%
5 half-lives 28,650 yr / 3.1%
10 half-lives 57,300 yr / 0.1%
λ for C-14 1.21×10⁻⁴ /yr

How carbon-14 is produced in the atmosphere

Carbon-14 is produced when cosmic rays strike nitrogen in the upper atmosphere. A neutron knocks out a proton from N-14, creating C-14: n + ¹⁴N → ¹⁴C + p. The resulting C-14 atom quickly bonds with oxygen to form ¹⁴CO₂, which mixes through the atmosphere. About one C-14 atom exists for every 10¹² C-12 atoms — vanishingly small but measurable.

The production rate has varied through history with solar activity (which modulates cosmic-ray flux) and the Earth's magnetic field strength. Calibration curves correct for these long-term variations.

Carbon dating age range and limits

The carbon dating age range runs from about 500 years to 50,000 years for routine measurements, with AMS pushing to ~57,000. Below 500 years the signal is too close to modern atmospheric C-14 to be precise; recent atmospheric variability (Suess effect from fossil fuels, bomb-test spike) adds noise that calibration handles only partially. Above 50,000 years, only 0.2% of the original C-14 remains, and instrument background becomes a serious source of error.

Wood
5000 yr
87% gone
Bone
12,000 yr
~23% remaining
Charcoal
35,000 yr
~1.5% remaining

Calibrating radiocarbon years to calendar years

Calibrating radiocarbon years to calendar years uses the IntCal20 (Northern Hemisphere) and SHCal20 (Southern Hemisphere) calibration curves. These are built from tree rings (back ~13,000 years), corals, foraminifera, and speleothems with independently known ages. Radiocarbon dates published as "cal BP" (calibrated years before 1950) account for these variations and are the standard for archaeological publication.

The raw radiocarbon age and the calibrated age can differ by hundreds of years, especially for samples between 1700 and 1900 CE (the Suess effect from fossil fuels) and across the late Pleistocene "Hallstatt plateau" (~2500 BP).

Materials that can be carbon-dated

Materials that can be carbon-dated include anything that contains organic carbon: wood, charcoal, bone collagen, antler, tooth dentin, textiles, papyrus, leather, hair, peat, lake-bottom sediments, and shell carbonate from molluscs and corals. The carbon should be from a single biogenic source — laminated or composite materials can give average ages weighted by carbon content.

Tip

Bone collagen is usually the best substrate for archaeological dating because collagen is chemically stable and the cleaning procedures effectively remove contaminants. Tooth dentin works similarly. Shell carbonate and freshwater fish bone need correction for the marine or freshwater reservoir effect, which can offset apparent age by hundreds of years.

Carbon dating precision and AMS

Carbon dating precision depends on the technique. Classic beta counting (Libby's method) needs grams of material and counts decay events over hours or days. Modern accelerator mass spectrometry (AMS) counts atoms directly using a particle accelerator, needs only milligrams, and finishes in minutes. AMS gives precision of ±30 to 50 years for Holocene samples and ±100 to 200 years for samples near the limit. Sample preparation, contamination control, and laboratory standards drive the final uncertainty more than the count statistics.

Common carbon dating mistakes and myths

The most persistent myth is that carbon dating "always" gives ages of millions of years. It cannot — the method tops out at ~57,000 years. Anything older needs K-Ar (potassium-argon, good for volcanic rocks), U-Pb (uranium-lead, geological time), or other isotope systems. A second common error is assuming the calibration is one-to-one with calendar years; in reality, radiocarbon years and calendar years differ systematically, especially across the bomb spike, the Suess effect, and the Hallstatt plateau.

Contamination is the killer

Modern carbon contamination of an old sample makes it look much younger than it is. Just 1% modern carbon in a 50,000-year-old sample halves the apparent age. Sample handlers wear gloves, work in clean labs, and use multiple extraction and purification steps. For very old samples, results below 0.5 percent modern carbon are reported as "infinite age" rather than risk over-stating precision.

FAQ

Living organisms exchange carbon with the atmosphere, so their tissue holds the atmospheric ratio of C-14 to C-12. When they die, exchange stops and C-14 decays at a known rate. Measuring how much C-14 is left and comparing it to the original ratio gives the age: t = −(t½/ln 2)·ln(N/N₀).
5730 years (the Cambridge half-life, used today). Willard Libby originally used 5568 years — the difference is small but matters for old samples. Calibration curves automatically convert between the two conventions.
Reliable from about 500 to 50,000 years. AMS (accelerator mass spectrometry) pushes the upper limit to ~57,000 years. Below ~500 years, atmospheric variability and the post-1950 bomb-curve spike make precise dating hard.
Anything containing organic carbon: wood, charcoal, bone (collagen fraction), textiles, peat, papyrus, leather, antler, ivory, hair, and shell carbonate from corals or molluscs. Pure minerals, metals, and ceramics cannot be dated unless they hold an organic inclusion.
Two main reasons. First, the atmospheric C-14 level has varied with solar activity and the Earth's magnetic field. Calibration curves (IntCal20, SHCal20) correct for this. Second, contamination — newer or older carbon mixing in — biases the result. Bone collagen and charcoal are usually the most reliable substrates.
Burning fossil fuels since the Industrial Revolution has released CO₂ with effectively zero C-14 (the carbon is millions of years old). This dilutes atmospheric C-14 and would make modern wood look 100+ years older than it is. Calibration curves correct for it.
Atmospheric nuclear tests from 1945 to 1963 nearly doubled atmospheric C-14. The signal peaked around 1964 and has been declining since, with a roughly 16-year exchange half-life with the oceans. The bomb curve is now used to date very recent materials, including forensic samples and modern wines.
Modern AMS measurements have a precision of ±30–50 years for samples younger than 5000 years. Precision degrades for older samples because less C-14 remains. Calibration adds its own uncertainty — typical reported ages give a 2-sigma calendar-year range (e.g. 3450–3520 cal BP).
After 10 half-lives, only 0.1% of the original C-14 remains. The atomic count becomes comparable to instrument background, so the age estimate becomes very imprecise. For older samples use potassium-argon (volcanic rocks, ~100k–10M years), uranium-series, or uranium-lead dating.
Willard Libby developed the method between 1946 and 1949 at the University of Chicago, then verified it against samples of known age (Egyptian tomb wood, tree rings). He won the 1960 Nobel Prize in Chemistry for it. The original technique counted beta decays directly. Modern radiocarbon labs use AMS — accelerator mass spectrometry — which counts atoms directly and needs much smaller samples.