library(learnr) knitr::opts_chunk$set(echo = FALSE)
Bchron is easiest to use. OxCal is very popular with archaeologists as it has models they can use.
Calibrate and plot the dates 2450 +/- 30 BP and 2600 +/- 30 BP measured on terrestrial leaves.
First, load the Bchron
package.
Function BchronCalibrate
will calibrate individual dates.
The most important arguments are ages
, ageSds
, and calCurves
, which take the radiocarbon age, error, and the name of the calibration curve to use.
Either a single value or a vector can be used for each argument, but all three must be the same length.
The standard calibration curves are 'intcal20', 'shcal20' and 'marine20'.
library(Bchron) cal <- BchronCalibrate( ages = , ageSds = , calCurves = ) summary(cal) plot(cal)
cal <- BchronCalibrate( ages = c(2450, 2600), ageSds = c(30, 30), calCurves = rep("intcal20", 2)) summary(cal) plot(cal)
1 Why are the calibrated dates' probability density functions so irregular?
2 Why do the two dates give such different shaped calibrated dates?
3 Calibrate the dates as if they are on marine fossils and compare the results.
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