“…TGM samples collected at inland background sites (e.g., forested mountains) far from the urban/industrial centers and tectonically active regions (e.g., volcanos and faults) are commonly characterized by positive δ 202 Hg (−0.16 to 1.19‰, site-specific mean values) and slightly negative Δ 199 Hg (−0.28 to −0.05‰) and Δ 200 Hg (−0.11 to −0.02‰) values (Figure ). ,− In contrast, TGM samples collected at urban/industrial sites and areas affected by direct anthropogenic Hg emissions typically have negative δ 202 Hg (−0.96‰ to −0.08‰, site-specific mean values) and near-zero Δ 199 Hg (−0.15‰ to 0.06‰) and Δ 200 Hg (−0.03‰ to 0.02‰) values. ,,,,, The PBM samples were mostly measured at urban/industrial sites that had high Hg levels, ,− which were generally characterized by very negative δ 202 Hg (−2.60‰ to −0.53‰, site-specific mean values) and variable Δ 199 Hg (−0.31‰ to 0.47‰) and slightly positive Δ 200 Hg (0.01–0.11‰) values (Figure ). By comparison, PBM samples collected at background sites (e.g., forested mountains and coastal/offshore sites) with low Hg levels commonly had distinctly positive Δ 199 Hg (0.15–0.66‰) values. ,,,,, …”