Dating age range graph

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It is calculated on the assumption that the atmospheric radiocarbon concentration has always been the same as it was in 1950 and that the half-life of radiocarbon is 5568 years.

For this purpose `present' refers to 1950 so you do not have to know the year in which the measurement was made.

Once calibrated a radiocarbon date should be expressed in terms of cal BC, cal AD or cal BP.

The cal prefix indicates that the dates are the result of radiocarbon calibration using tree ring data.

To give an example if a sample is found to have a radiocarbon concentration exactly half of that for material which was modern in 1950 the radiocarbon measurement would be reported as 5568 BP.

For two important reasons, this does not mean that the sample comes from 3619 BC: Many types of tree reliably lay down one tree ring every year.

These are the basis for the calibrations performed by the programs like CALIB and Ox Cal. Calibration of radiocarbon determinations is in principle very simple.

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By using these widths, it is possible to compare the tree rings in a dead tree to those in a tree that is still growing in the same region.

This requires a computer since the calculations are more complicated.

It gives the time range, from which you can be 95% sure the sample came.

For older periods we are able to use other records of with idependent age control to tell us about how radiocarbon changed in the past.

The information from measurements on tree rings and other samples of known age (including speleothems, marine corals and samples from sedimentary records with independent dating) are all compiled into calibration curves by the Int Cal group.

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