“…Mean (±1σ) Δ 199 Hg in feed coal, zinc ores, limestone, Hg ores, and biomass in China are À0.03 ± 0.16‰, 0.02 ± 0.06‰, À0.01 ± 0.07‰, 0.01 ± 0.02‰, and À0.19 ± 0.10‰, respectively, significantly higher than those (À0.16 ± 0.18‰, À0.04 ± 0.06‰, À0.03 ± 0.08‰, À0.04 ± 0.07‰, and À0.28 ± 0.09‰, respectively) in the rest of the world (paired t test, p < 0.05, T = 3.7, n = 5). Assuming that isotopic signatures of GEM emissions from major anthropogenic sources resemble the MIF signatures of source materials Sun et al, 2014Sun et al, , 2016Tang et al, 2017), Δ 199 Hg of atmospheric GEM in mainland China, influenced by the regional anthropogenic sources, should be higher than the GEM Δ 199 Hg in other regions worldwide, as shown in Figure 2. Coal combustion in CFPPs and nonferrous metal smelting are the two important sources of atmospheric GEM in China and other regions worldwide (Pirrone et al, 2010;Zhang et al, 2015).…”