“…As overestimation of the extraction efficiency of 234 Th could occur to the cartridge method [ Cai et al , 2006a] and the extent of this overestimation may vary with depth, temperature and dissolved organic carbon (DOC) concentrations [ Santschi et al , 2006]; hence those using deep‐water MnO 2 cartridge samples as standards should be cautious. Hung et al [2008] cited studies in the equatorial Pacific as verification that deep water 234 Th: 238 U equilibration was achieved [ Bacon et al , 1996], but ignored the fact that a 234 Th deficiency throughout the whole water column was observed in some of the studies with the cartridge method [e.g., Baskaran et al , 1996; Guo et al , 2002; Hung et al , 2004; Lepore and Moran , 2007; Lepore et al , 2007; Moran et al , 2005; Santschi et al , 1999; Shimmield et al , 1995].…”