Dear Christopher,
As you may recall from another thread, I compared U-Th dates and 14C dates on a number of mid-Holocene samples from a site to estimate ∆R, for each sample and also for the whole population.
With the introduction of Marine20, I've now recalculated everything.
A comparison of results is below:
Sample ∆R (yr) ± 1sigma ∆R (yr) ± 1sigma
for Marine13 for Marine20
Sample 1 -15 ± 27 -164 ± 44
Sample 2 173 ± 31 -18 ± 54
Sample 3 -39 ± 28 -212 ± 51
Sample 4 7 ± 35 -191 ± 56
Sample 5 -20 ± 28 -206 ± 51
Sample 6 23 ± 26 -118 ± 45
Sample 7 20 ± 27 -142 ± 44
Sample 8 -10 ± 26 -160 ± 44
Sample 9 31 ± 31 -107 ± 47
Sample 10 22 ± 27 -125 ± 46
Sample 11 -6 ± 31 -149 ± 48
Sample 12 4 ± 27 -153 ± 48
Overall Site 15 ± 9 -145 ± 14
The average difference is ~160 years, close to what's stated at
But I notice the uncertainties in ∆R are systematically larger with Marine20.
I'll think a bit about the mathematical reasons why that might be, but before I go far down that road, can I double check that these larger uncertainties are real and expected, based on the new calibration curve?
Separately, I realize the Overall Site ∆R seems to be a single value of ∆R that fits ~95% of the individual sample ∆Rs. If I instead wanted to estimate a larger uncertainty for the Overall Site ∆R that encompasses ~95% of all the variability (and uncertainty) at that site, is there a way to do that in OxCal?
Thanks, and best regards,
Aron