“…S2); in fact, EFc is among or the highest in the entire ice core record for Ag (7), As (1.5), Bi (2), Cd (30), Cr (8), Cu (20), Mo (800), Pb (5), and Sb (3). In Antarctica, a new phase of concentration enhancements for Ag (7 times), Bi (10 times), Cr (2-4 times) after the mid 1940s (38), Pb (3 times) after A.D. 1950 (7), As (5 times), Mo (2 times), and Sb (3 times) after A.D. 1970 (39) are temporally synchronous with the corresponding increments in the Quelccaya ice core record and consistent with an influence of South American anthropogenic emissions on Antarctica during the 20th century (see, for example, Pb in Fig. 4).…”