“…This condition differs from that of our subtropical oligotrophic lake, where primary production was low, , most likely decreasing the degree of Zn fractionation as a result of biological uptake. Previous studies have also demonstrated that lighter Zn isotopes are preferentially integrated into atmospheric emissions during high-temperature processes. , For example, anthropogenic Zn from urban and industrial atmospheric emissions, primarily released by smelting and mining, ,, vehicular traffic, ,, and coal combustion, exhibits lighter isotope compositions ranging from −0.41 to −0.22‰, −0.24 to −0.07‰, and −0.61 to −0.56‰, respectively (Table S4). Herein, the linear correlation between the δ 66 Zn IRMM values and 1/Zn could be attributed to binary mixing between a natural source with a higher δ 66 Zn IRMM value and an anthropogenic source with a lower δ 66 Zn IRMM value (Figure b).…”