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contaminate
function now also produces a plot, and
more details of the calculations.decontaminate
function has been renamed to
clean
and has been updated with clearer messages; it now
removes contamination to calculate the true/target age. A plot is made,
and calculation details are provided.muck
to calculate how much contamination
has to be inferred to go from an observed age to a true/target age. A
plot is made, and calculation details are provided.C14tocalBP
and C14toBCAD
.
Since these rely on the outdated ‘intercept calibration’ method, these
functions are provided for illustrative purposes only.oncurve
option. If so, then the curve and dates
can also be plotted in the F14C
or pMC
realms.r.calib
that samples random calendar ages
from a calibrated distribution.p.range
to calculate a calibrated age’s
probability of lying between a range of BC/AD or cal BP ages.as.one
to calculate the product of
multiple calibrated ages, assuming that they all stem from (exactly) the
same calendar age. Not that this is dangerous, and care should be taken
to make sure that the assumptions are met.as.bin
to calculate how many of a set of
calibrated radiocarbon dates fall into bins of a specified width. The
bin moves along the range of calibrated ages, to visualise how many
dates fit bins over time. This would be safer than using the function
as.one
.spread
shows the spread (in calendar
years) of a set of dates. Accompanies the functions pool
and as.one
.BCADto14C
to calculate the 14C age
belonging to a BC/AD age (this calls the function
calBPto14C
)as.F
to calibrate in the F14C realm (the
default remains to calibrate in the C14 realm)print.truncate.warning=FALSE
age.F14C
, F14C.age
,
age.pMC
and pMC.age
to, respectively,
C14toF14C
, F14CtoC14
, C14topMC
and pMCtoC14
. This because age
is an
ambivalent term in this contextBCADtocalBP
and calBPtoBCAD
to transfer cal BP into BC/AD ages and vice versa. Can deal with
(e.g. Gregorian/Julian) calendars which do not include 0calBP
, BCAD
, C14
,
F14C
, pMC
and D14C
.smooth.ccurve
to smooth a calibration
curve using a moving window of a specified width. This can be useful to
calibrate material that is known to have accumulated, say, over two
decadespool
which calculates the chi2 and
accompanying p-value for a set of multiple measurements on the same
sample. If the scatter between the values is low enough for the p-value
to be below a threshold, then the pooled mean and uncertainty are
returnedoncurve
to
draw the dates onto the calibration curve.shroud
, which contains replicate
radiocarbon measurements on the Shroud of Turin, from three labs.decontaminate
to estimate the percentage
of contamination needed to explain the difference between a ‘real’ and
an ‘observed’ radiocarbon age.bombalert
to the calibrate function. If
set to false, plots ages close to 0 C14 BP without warnings.shells
find.shells
and map.shells
to plot shells data in maps based on their coordinatesshells.mean
to plot deltaRs of selected
shells, and calculate a weighted mean deltaRweighted_means
to calculate weighted means
and errors for multiple radiocarbon dates (or delta R values)draw.D14C
draw.ccurve
now can plot the C14 in the ‘realms’ of C14
BP, F14C, pMC and D14C using the ‘realm’ option.older
These binaries (installable software) and packages are in development.
They may not be fully stable and should be used with caution. We make no claims about them.