Isotopic fractionation can serve as a powerful tracer of chemical evolution during star and planet formation. To accurately interpret observations, it is crucial to identify the dominant pathways of nitrogen and carbon fractionation at different evolutionary stages. We aim to study nitrogen and carbon fractionation in a sample of young cores at the onset of star formation. We mapped H 13 CN and HC^15N around one starless and three pre-stellar cores. We computed the N(H13CN)/N(HC15N)columndensityratioacrossthecoresandcomparedthedistributionwithN(H2)mapsfrom/SPIRE.Inaddition,wecalculated14N/(H^13CN)/N(HC^15N) column density ratio across the cores and compared the distribution with N(H_2) maps from /SPIRE. In addition, we calculated ^14N/^ Herschel 15 N maps using the double isotope method for comparison with earlier studies. We compared these results with astrochemical modeling of carbon and nitrogen fractionation for a 1D pre-stellar core model. The computed N(H13CN)/N(HC15N)ratioexhibitsclearspatialvariationacrossthemaps.ThisvariationcorrelateswithN(H(HC^15N) ratio exhibits clear spatial variation across the maps. This variation correlates with N(H_2) in three out of four cores. Our analysis reveals a correlation between the H 13 CN/HC^15N ratios and the N(H2)maps.Accordingtotheastrochemicalmodel,thecorrelationismainlyduetovariationsinthe12C/13Cratio.Consequently,theresultscautionagainstapplyingthedoubleisotopemethodtoderive14N/15Nratioswithoutindependentlyassessingpossiblespatialvariationsin12C/(H_2) maps. According to the astrochemical model, the correlation is mainly due to variations in the ^12C/^13C ratio. Consequently, the results caution against applying the double-isotope method to derive ^14N/^15N ratios without independently assessing possible spatial variations in ^12C/^ 13 C. Furthermore, the leading cause of the isotopic variation in the model is not isotope-selective photodissociation, but rather more efficient fractionation through exchange reactions at lower temperatures in the denser regions of the cores.