QUB | Archaeology and Palaeoecology | The 14Chrono Centre
Age-depth models may be based on either radiocarbon age determinations (the default) or calibrated ages. Use with radiocarbon ages directly is simpler, and their input is described under Format of associated input files.
Use with calibrated ages is more complex, because of the nature of these ages. There is no one-to-one conversion of radiocarbon ages onto a calibrated calendar year timescale. The calibration curve is irregular, and the result of mapping a radiocarbon age, with its symmetrical normal probability distribution, onto the irregular calibration curve is an irregular probability distribution, which cannot be treated statistically in the same way as radiocarbon ages. psimpoll appraoches the problem through the output generated by the BCal calibration system. Other calibration programs are available (see Radiocarbon Web-info), but BCal offers two advantages:
The use of calibrated ages is determined here, in menu L, but some of the details are controlled in menu N, and discussed there.
When menu L is selected, the following submenu appears:
L Conversion of depths to ages a Convert depths to ages (off) [off] b Specify an age for the top sample [0+/-50] c Specify an age for the basal sample [] d Select an age model [1] e Select number of terms for polynomial age model [0] f Change laboratory error multiplier (1.00) [1.00] g Include timescale with depth axis (off) [off] h Convert all ages to AD-BC scale (off) [off] i Use calibrated ages from BCal (off) [off] j Mode or weighted average with calibrated dates [MODE] 9 Leave this menuLb-Lf, Lh and Li are relevant only if La is `age', Lg is `on', or the second letter of the code in input Item 4 of input is `b' (conversion of concentration data to accumulation rate data). Lj is relevant only if Li is `on'. If sample values are not converted to ages, any output file for age-depth data (menu Eb) is not used.
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