“…To the best of our knowledge, researchers have only studied ice or snow cores as a natural archive for airborne PFASs or PBDEs in the Arctic (Hermanson et al, 2010;Meyer et al, 2012;Young et al, 2007). Other types of natural archives or sampling techniques that record temporal trends of PBDEs include long-term passive sampling (Schuster et al, 2010), vegetation and soil samples (Hassanin et al, 2005;Schuster et al, 2011), and lake sediment cores Kohler et al, 2008). Peat bogs, human serum, sediment cores and associated biota record PFASs back to the 1950s (Ahrens et al, 2009;Dreyer et al, 2012;Sturm and Ahrens, 2010).…”