The stable HCNOS isotope compositions can be reported as (a) the isotope ratio of two stable isotopes (R); (b) the isotope delta value (δ); and (c) the atom fraction of the isotopes (x). Recalculations between these different expressions are needed frequently and require the use of the absolute isotope ratio for the zero points of the stable isotope delta scales (R std). The inconsistent use of R std values may lead to a discrepancy in recalculated results. Methods: We summarised the recalculation procedures between different expressions of the stable isotope compositions and introduced a user-friendly EasyIsoCalculator that allows the recalculation between the main expressions of isotope compositions. We mathematically and empirically evaluated the possible inconsistencies in reporting of the stable isotope data due to the use of different R std and different normalisation methods. Results: The recalculation between δ-values and other expressions of the stable isotope compositions always involves the use of R std. The choice of R std will have a significant influence on the recalculated values. The use of different R std values has a significant influence also on the normalisation of raw values but only when the normalisation is conducted versus the working standard gas value, causing discrepancy, e.g. for δ(13 C/ 12 C) up to 0.3 ‰. Conclusions: Differences in the selection of R std value may lead to significant differences among different laboratories. The uncertainty in the calculations originates primarily from the uncertainty in the R std determination; however, it is lower than the discrepancy arising from the inconsistent use of R std. Consistent use of the same R std values is required to eliminate the unnecessary discrepancy if different data sets are recalculated from delta value to other expressions. 1 | INTRODUCTION Stable HCNOS isotope compositions are reported in different ways, based on common consensus and the requirements of a scientific discipline. The most frequently reported forms are (a) the ratio of two isotopes expressed as a fraction (hereafter referred to as the absolute isotope ratio); (b) the isotope delta value (δ) expressed in native form, in permille (‰), or sometimes permeg; and (c) the atom fraction of the isotopes expressed as a fraction, a percentage (%) or in parts per million (ppm). 1 Reporting of the absolute isotope ratio is consistent with the International System of Units (SI) but is not very widely used for light stable isotopes because it is impractical for reporting very small differences at natural abundance levels. Moreover, the absolute ratio is very rarely directly determined for those elements [e.g. using inductively coupled plasma mass spectrometry (ICP-MS); sometimes, it is indirectly calculated using isotope ratio mass spectrometry (IRMS) analyses]. Typically, the stable isotope composition is determined relative to a working reference material using IRMS and then is reported as a relative ratiothe isotope delta value. The isotope delta notation requires a common...