“…Ever since the postulation of reaction (1) as the main C fractionation route in strongly shielded regions (Watson et al 1976), a notable contrast has emerged between the above general predictions (by chemistry models) of the strong 13 C depletion in C-containing molecules (Langer et al 1984) and the general absence of this observable effect in surveys conducted, for example, in abundant species such as CS (Liszt & Ziurys 2012), CN (Milam et al 2005), C 2 (Hamano et al 2019), CCS (Sakai et al 2007), HNC (Liszt & Ziurys 2012), C 3 (Giesen, T. F. et al 2020), and HC 3 N (Takano et al 1998) that are not formed directly from CO and whose 12 C/ 13 C ratios thus inferred are in agreement with (or even lower than) the gas elemental values. Such a conflict therefore opened up new avenues for the possibility of an overall 13 C enrichment in species other than CO, and led to the proposition of alternative isotope-exchange reactions (e.g., 13 C (+) +CN (Langer 1992;Roueff, E. et al 2015), 13 CO+HCO + (Smith & Adams 1980; Mladenović, M. & Roueff, E. 2017), 13 C+C 2 (Roueff, E. et al 2015), and 13 C+C 3 (Giesen, T. F. et al 2020;Colzi, L. et al 2020;Loison et al 2020)) and novel formation pathways (Takano et al 1998;Sakai et al 2007;Furuya et al 2011) deemed to contribute to the 13 C fractionation chemistry.…”