Measured Δ47 values are a function of absolute 13C/12C, 17O/16O and 18O/16O ratios.
Using different isotopic parameters produces systematic Δ47 offsets (up to 0.04‰).
These offsets are not canceled out by current standardization procedures.
Inaccurate parameters may partly explain current inter-laboratory discrepancies.
Isotopic parameters of Brand et al. (2010) appear to yield accurate Δ47 values.