The IRMS is used exclusively for δ13C and δ15N on organic matter. We analyse a range of sample types - collagen, cellulose, plant material, hair and animal tissues
We continually measure three different IAEA standards to estimate the machine
uncertainty of the IRMS.
We also track the reproducibility of our bone pretreatment by measuring replicates
of, among other things an 8300 year old whale bone. Since we had poor reproduciblity
of the δ13C on this bone, Dr Svetlana Svyatko has carried out
a series of tests (2013)on bones of various animals and ages to test the effect of
pretreatment on this variability.
Sufficient material for 10 measurements was homogenised prior to pretreatment.
As the table below shows, the variability on the sample population of 10 replicates
is in most cases lower than the machine variability, measured with over 1500 replicates
of R041. We conclude that the large variability on the long term replicates of UBA-No 8968 (shown in blue below) is due to bone inhomogeneity,
which is not seen in the mammoth bone UBA-No 15593 (shown in brown below). However we conservatively report the machine variability from R041 as the uncertainty on our δ13C and δ15N measurements.
sigδ13C=0.22 |
sigδ15N=0.15 |
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