“…Organic carbon has (Saez et al, 2009;Burnett et al, 2011;Liu et al, 2013;Gadd et al, in press), validating the use of this proxy for sediment organic matter content. Further, bromine (Br) has been found to be a reliable proxy for organic matter content in both lacustrine and oceanic sediments (Phedorin et al, 2000;Croudace et al, 2006;Ziegler et al, 2008;Hahn et al, 2014) and Br content is significantly higher in organosols (the dominant soil type in southwest Tasmania) than in other soil types (Maw and Kempton, 1982), thus, providing an additional proxy for sediment organic matter content.…”