posted on 2018-12-28, 00:00authored byN. Haghipour, B. Ausin, M. O. Usman, N. Ishikawa, L. Wacker, C. Welte, K. Ueda, T. I. Eglinton
We
examine instrumental and methodological capabilities for microscale
(10–50 μg of C) radiocarbon analysis of individual compounds
in the context of paleoclimate and paleoceanography applications,
for which relatively high-precision measurements are required. An
extensive suite of data for 14C-free and modern reference
materials processed using different methods and acquired using an
elemental-analyzer–accelerator-mass-spectrometry (EA-AMS) instrumental
setup at ETH Zurich was compiled to assess the reproducibility of
specific isolation procedures. In order to determine the precision,
accuracy, and reproducibility of measurements on processed compounds,
we explore the results of both reference materials and three classes
of compounds (fatty acids, alkenones, and amino acids) extracted from
sediment samples. We utilize a MATLAB code developed to systematically
evaluate constant-contamination-model parameters, which in turn can
be applied to measurements of unknown process samples. This approach
is computationally reliable and can be used for any blank assessment
of small-size radiocarbon samples. Our results show that a conservative
lower estimate of the sample sizes required to produce relatively
high-precision 14C data (i.e., with acceptable errors of
<5% on final 14C ages) and high reproducibility in old
samples (i.e., F14C ≈ 0.1) using current isolation
methods are 50 and 30 μg of C for alkenones and fatty acids,
respectively. Moreover, when the F14C is >0.5, a precision
of 2% can be achieved for alkenone and fatty acid samples containing
≥15 and 10 μg of C, respectively.