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Radiocarbon dating

Radiocarbon dating is a radiometric dating method that uses the naturally occurring isotope carbon-14 (14C) to determine the age of carbonaceous materials up to about 60,000 years.[1] Raw, i.e. uncalibrated, radiocarbon ages are usually reported in radiocarbon years "Before Present" (BP), "Present" being defined as AD 1950. Such raw ages can be calibrated to give calendar dates.

The technique of radiocarbon dating was discovered by Willard Libby and his colleagues in 1949[2] during his tenure as a professor at the University of Chicago. Libby estimated that the steady state radioactivity concentration of exchangeable carbon-14 would be about 14 disintegrations per minute (dpm) per gram. In 1960, he was awarded the Nobel Prize in chemistry for this work.

One of the frequent uses of the technique is to date organic remains from archaeological sites. Plants fix atmospheric carbon during photosynthesis, so the level of C14 in living plants and animals equals the level of C14 in the atmosphere.

Additional recommended knowledge


Basic physics

Carbon has two stable, nonradioactive isotopes: carbon-12 (12C), and carbon-13 (13C). In addition, there are trace amounts of the unstable isotope carbon-14 (14C) on Earth. Carbon-14 has a half-life of 5730 years and would have long ago vanished from Earth were it not for the unremitting cosmic ray impacts on nitrogen in the Earth's atmosphere, which create more of the isotope. The neutrons resulting from the cosmic ray interactions participate in the following nuclear reaction on the atoms of nitrogen molecules (N2) in the atmospheric air:

n + \mathrm{~^{14}_{7}N}\rightarrow\mathrm{~^{14}_{6}C}+ p


The highest rate of carbon-14 production takes place at altitudes of 9 to 15 km (30,000 to 50,000 ft), and at high geomagnetic latitudes, but the carbon-14 spreads evenly throughout the atmosphere and reacts with oxygen to form carbon dioxide. Carbon dioxide also permeates the oceans, dissolving in the water. For approximate analysis it is assumed that the cosmic ray flux is constant over long periods of time; thus carbon-14 is produced at a constant rate and the proportion of radioactive to non-radioactive carbon is constant: ca. 1 part per trillion (600 billion atoms/mole). In 1958 Hessel de Vries showed that the concentration of carbon-14 in the atmosphere varies with time and locality. For the most accurate work, these variations are compensated by means of calibration curves. When these curves are used, their accuracy and shape are the factors that determine the accuracy and age obtained for a given sample.

Plants take up atmospheric carbon dioxide by photosynthesis, and are ingested by animals, so every living thing is constantly exchanging carbon-14 with its environment as long as it lives. Once it dies, however, this exchange stops, and the amount of carbon-14 gradually decreases through radioactive beta decay.

\mathrm{~^{14}_{6}C}\rightarrow\mathrm{~^{14}_{7}N}+ e^- + \bar{\nu}_e

By emitting an electron and an anti-neutrino, carbon-14 is changed into stable (non-radioactive) nitrogen-14. This decay can be used to measure how long ago once-living material died. However, aquatic plants obtain some of their carbon from dissolved carbonates which are likely to be very old, and thus deficient in the carbon-14 isotope, so the method is less reliable for such materials as well as for samples derived from animals with such plants in their food chain.

Computation of ages and dates

The radioactive decay of carbon-14 follows an exponential decay. A quantity is said to be subject to exponential decay if it decreases at a rate proportional to its value. Symbolically, this can be expressed as the following differential equation, where N is the quantity and λ is a positive number called the decay constant:

\frac{dN}{dt} = -\lambda N.

The solution to this equation is:

N = N_0e^{-\lambda t}\,,

where, for a given sample of carbonaceous matter:

N0 = number of radiocarbon atoms at t = 0, i.e. the origin of the disintegration time,
N = number of radiocarbon atoms remaining after radioactive decay during the time t,
λ = radiocarbon decay or disintegration constant.
Two related times can be defined:
  • mean- or average-life: mean or average time each radiocarbon atom spends in a given sample until it decays.
  • half-life: time lapsed for half the number of radiocarbon atoms in a given sample, to decay,

It can be shown that:

t_{avg} \, = \frac{1}{\lambda} = radiocarbon mean- or average-life = 8033 years (Libby value)
t_\frac{1}{2} \, = t_{avg} \cdot \ln 2 = radiocarbon half-life = 5568 years (Libby value)

Notice that dates are customarily given in years BP which implies t(BP) = -t because the time arrow for dates runs in reverse direction from the time arrow for the corresponding ages. From these considerations and the above equation, it results:

For a raw radiocarbon date:

t(BP) = \frac{1}{\lambda} {\ln \frac{N}{N_0}}

and for a raw radiocarbon age:

t(BP) = -\frac{1}{\lambda} {\ln \frac{N}{N_0}}

After replacing values, the raw radiocarbon age becomes any of the following equivalent formulae:

using logs base e and the average life:

t(BP) = -t_{avg}\cdot \ln{\frac{N}{N_0}}


using logs base 2 and the half-life:

t(BP) = -t_\frac{1}{2}\cdot \log_2 \frac{N}{N_0}

Measurements and scales

Measurements are traditionally made by counting the radioactive decay of individual carbon atoms by gas proportional counting or by liquid scintillation counting, but these are relatively insensitive and subject to relatively large statistical uncertainties for small samples (below about 1g carbon). If there is little carbon-14 to begin with, a half-life that long means that very few of the atoms will decay while their detection is attempted (4 atoms/s) /mol just after death, hence e.g. 1 (atom/s)/mol after 10,000 years).

Sensitivity has since been greatly increased by the use of accelerator-based mass-spectrometric (AMS) techniques, where all the 14C atoms can be counted directly, rather than only those decaying during the counting interval allotted for each analysis. The AMS technique allows one to date samples containing only a few milligrams of carbon, although the maximum age reported is still around 60,000 years[3].

Raw radiocarbon ages (i.e., those not calibrated) are usually reported in years "before present" (BP). This is the number of radiocarbon years before 1950, based on a nominal (and assumed constant - see "calibration" below) level of carbon-14 in the atmosphere equal to the 1950 level. They are also based on a slightly-off historic value for the half-life maintained for consistency with older publications (see "Radiocarbon half-life" below). See the section on computation for the basis of the calculations. Corrections for isotopic fractionation have not been included.

Radiocarbon labs generally report an uncertainty, e.g., 3000±30BP indicates a standard deviation of 30 radiocarbon years. Traditionally this includes only the statistical counting uncertainty and some labs supply an "error multiplier" that can be multiplied by the uncertainty to account for other sources of error in the measuring process. Additional error is likely to arise from the nature and collection of the sample itself, e.g., a tree may accumulate carbon over a significant period of time. Such old wood, turned into an artifact some time after the death of the tree, will reflect the date of the carbon in the wood.

The current maximum radiocarbon age limit lies in the range between 58,000 and 62,000 years (approximately 10 half-lives)(cf refs [1, 3]). This limit is encountered when the radioactivity of the residual 14C in a sample is too low to be distinguished from the background radiation.


The need for calibration

  A raw BP date cannot be used directly as a calendar date, because the level of atmospheric 14C has not been strictly constant during the span of time that can be radiocarbon dated. The level is affected by variations in the cosmic ray intensity which is affected by variations in the earth's magnetosphere caused by solar storms. In addition there are substantial reservoirs of carbon in organic matter, the ocean, ocean sediments (see methane hydrate), and sedimentary rocks. Changing climate can sometimes disrupt the carbon flow between these reservoirs and the atmosphere. The level has also been affected by human activities—it was almost doubled for a short period due to atomic bomb tests in the 1950s and 1960s and has been reduced by the release of large amounts of CO2 from ancient organic sources where 14C is not present—the fossil fuels used in industry and transportation, known as the Suess effect.

The atmospheric 14C concentration may differ substantially from the concentration in local water reservoirs. Eroded from CaCO3 or organic deposits, old carbon may be easily assimilated and provide diluted 14C carbon into trophic chains.

Calibration methods

The raw radiocarbon dates, in BP years, are therefore calibrated to give calendar dates. Standard calibration curves are available, based on comparison of radiocarbon dates of samples that can be independently dated by other methods such as examination of tree growth rings (dendrochronology), ice cores, deep ocean sediment cores, lake sediment varves, coral samples, and speleothems (cave deposits).

The calibration curves can vary significantly from a straight line, so comparison of uncalibrated radiocarbon dates (e.g., plotting them on a graph or subtracting dates to give elapsed time) is likely to give misleading results. There are also significant plateaus in the curves, such as the one from 11,000 to 10,000 radiocarbon years BP, which is believed to be associated with changing ocean circulation during the Younger Dryas period. The accuracy of radiocarbon dating is lower for samples originating from such plateau periods.

The 2004 version of the calibration curve extends back quite accurately to 26,000 years BP. Any errors in the calibration curve do not contribute more than ±16 years to the measurement error during the historic and late prehistoric periods (0 - 6,000 yrs BP) and no more than ±163 years over the entire 26,000 years of the curve, although its shape can reduce the accuracy as mentioned above.[5]

Radiocarbon half-life

Libby vs Cambridge values

Carbon dating was developed by a team led by Willard Libby. Originally a carbon-14 half-life of 5568±30 years was used, which is now known as the Libby half-life. Later a more accurate figure of 5730±40 years was determined, which is known as the Cambridge half-life. However, laboratories continue to use the Libby figure to avoid inconsistencies when comparing raw dates and when using calibration curves to obtain calendrical dates.

Carbon exchange reservoir

Libby's original exchange reservoir hypothesis has recently been criticized by Anatoly Fomenko because of its central assumptions that: (a) the exchange reservoir is constant all over the world; (b) the variations in 14C level are global, such that a small number of samples from a specific year are sufficient for calibration of the dating scale[6]. However, since Libby's early work was published (1950 to 1958), temporal, latitudinal and continental variations in the carbon exchange reservoir have been observed by Hessel de Vries (1958; as reviewed by Lerman et al., 1959, 1960). Subsequently, calibration curves have been developed that allow the correction of raw radiocarbon dates. The reservoir effects that necessitate this correction include:

  • Erosion and immersion of carbonate rocks (which are older than 60,000 years and so do not contain 14C) causes an increase in 12C and 13C in the exchange reservoir, which depends on local weather conditions and can vary the ratio of carbon that living organisms incorporate. This is believed negligible since most erosion will flow into the sea[7].
  • Volcanic eruptions eject large amount of carbonate into the air, causing an increase in 12C and 13C in the exchange reservoir and can vary the exchange ratio locally. This explains the often irregular dating achieved in volcanic areas[8].
  • 14C is known to behave chemically in a way different from 12C and 13C (due to different atomic mass), such that it is possible one isotope will be involved in decomposition reactions out of ratio with other isotopes, but the chemical behavior effects are extremely minor[9].
  • The earth is not affected evenly by cosmic radiation, the magnitude of the radiation depends on land altitude and earth's magnetic field strength at any given location, causing minor variation in the local 14C production. This is accounted for by having calibration curves for different locations of the globe. However this could not always be performed, as tree rings for calibration were only recoverable from certain locations in 1958[10].

These effects were first confirmed when samples of wood from around the world, which all had the same age (based on tree ring analysis), showed deviations from the dendrochronological age. Calibration techniques based on tree-ring samples have contributed to increase the accuracy since 1962, when they were accurate to 700 years at worst[11].

Speleothem studies extend 14C calibration

Relatively recent (2001) evidence has allowed scientists to refine the knowledge of one of the underlying assumptions. A peak in the amount of carbon-14 was discovered by scientists studying speleothems in caves in the Bahamas. Stalagmites are calcium carbonate deposits left behind when seepage water, containing dissolved carbon dioxide, evaporates. Carbon-14 levels were found to be twice as high as modern levels[12]. These discoveries improved the calibration for the radiocarbon technique and extended its usefulness to 45,000 years into the past[13].


  • Ancient footprints of Acahualinca
  • Haraldskær Woman
  • Kennewick Man
  • Skeleton Lake
  • Shroud of Turin
  • Thera eruption
  • Vinland map
  • Chauvet Cave

See also

  • Age of the Earth
  • Cosmogenic isotopes
  • Environmental isotopes
  • Discussion of half-life and average-life or mean-lifetime


  1. ^ Plastino, W., Kaihola, L., Bartolomei, P., Bella, F. (2001) Cosmic background reduction in the radiocarbon measurement by scintillation spectrometry at the underground laboratory of Gran Sasso, Radiocarbon, 43, 157–161
  2. ^ Arnold, J. R. and Libby, W. F. (1949) Age Determinations by Radiocarbon Content: Checks with Samples of Known Age, Science 110, 678–680.
  3. ^ "NOSAMS Radiocarbon Data and Calculations", Woods Hole Oceanographic Institution
  4. ^ Stuiver, M., Reimer, P. J. and Braziunas, T. F. (1998) High-Precision Radiocarbon Age Calibration for Terrestrial and Marine Samples. Radiocarbon 40, 1127-1151.
  5. ^ Paula J. Reimer et al., "INTCAL04 Terrestrial Radiocarbon Age Calibration, 0–26 Cal Kyr BP", Radiocarbon 46 (2004): 1029-1058; data online at .
  6. ^ Libby, W.F. Radiocarbon dating, 2nd Edition, Chicago, University of Chicago Press, 1955.
  7. ^ Kolchin, B. A., and Y. A. Shez. Absolute Archaeological Datings and their Problems, Moscow, Nauka, 1972.
  8. ^ Kolchin, B. A., and Y. A. Shez. Absolute Archaeological Datings and their Problems, Moscow, Nauka, 1972.
  9. ^ Aitken, M. J. Physics and Archaeology, New York, Interscience Publishers, 1961.
  10. ^ Crowe, C Carbon-14 activity during the past 5000 years, Nature, Volume 182, 1958.
  11. ^ Libby, W.F. Radiocarbon; an Atomic Clock, Annual Science and Humanity journal, 1962.
  12. ^ Pennicott, K., Carbon clock could show the wrong time, PhysicsWeb, 10 May 2001
  13. ^ Jensen, M. N., Peering deep into the past, The University of Arizona, Department of Physics (2001)


  • Bowman, S. (1990) Interpreting the Past: Radiocarbon Dating, University of California Press, ISBN 0-520-07037-2.
  • Currie, L. (2004) The Remarkable Metrological History of Radiocarbon Dating II, J. Res. Natl. Inst. Stand. Technol., 109, 185–217.
  • de Vries, H. (1958) Kon. Ned. Acad. Wetensch. Proc. Ser. B Phys. Sci. 61, 94; and in Researches in Geochemistry, P. H. Abelson (Ed.) (1959) Wiley, New York, p. 180.
  • Friedrich, M., Remmele, S., Kromer, B., Hofmann, J., Spurk, M., Kaiser, K. F., Orcel, C. and Küppers, M. (2004) The 12,460-Year Hohenheim Oak and Pine Tree-Ring Chronology from Central Europe—a Unique Annual Record for Radiocarbon Calibration and Paleoenvironment Reconstructions, Radiocarbon 46, 1111–1122.
  • Gove, H. E. (1999) From Hiroshima to the Iceman. The Development and Applications of Accelerator Mass Spectrometry. Bristol: Institute of Physics Publishing.
  • Kovar, A. J. (1966) Problems in Radiocarbon Dating at Teotihuacan, American Antiquity 31, 427–430.
  • Lerman, J. C., Mook, W. G., Vogel, J. C., and de Waard, H. (1969) Carbon-14 in Patagonian Tree Rings. Science, 165:1123-1125; Lerman, J. C., Mook, W. G., and Vogel, J. C. (1970) Proc. 12th Nobel Symp.
  • Lorenz, R. D., Jull, A. J. T., Lunine, J. I. and Swindle, T. (2002) Radiocarbon on Titan, Meteoritics and Planetary Science 37, 867–874.
  • Mook, W. G. and van der Plicht, J. (1999) Reporting 14C activities and concentrations, Radiocarbon 41, 227–239.
  • Weart, S. (2004) The Discovery of Global Warming - Uses of Radiocarbon Dating.
  • Willis, E.H. (1996) Radiocarbon dating in Cambridge: some personal recollections. A Worm's Eye View of the Early Days.
This article is licensed under the GNU Free Documentation License. It uses material from the Wikipedia article "Radiocarbon_dating". A list of authors is available in Wikipedia.
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