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Drawing the optimal depth-age curve on the basis of calibrated radiocarbon dates

Walanus A.

Geochronometria

2008

Vol. 31

1-5

The radiocarbon determination of age has the form of a complicated probability density function. In some cases however it is possible to exploit it in a precise way, in drawing the depth-age curve when a stratigraphic sequence of 14C ages is available. It is also possible to use this function in drawing the depth-age curve by hand. The necessary additional constraint on the depth-age curve adopted here is the simplicity of its shape, namely the low curvature.