Schwehr, Kathleen ASantschi, Peter HElmore, DavidLimnology and Oceanography: Methods2010-02-152010-02-152005http://hdl.handle.net/1969.3/18518pgs. 326-337Variations in super(129)I/ super(127)I ratios were used to trace terrestrial organic carbon (tDOC) across an estuary because (1) iodine is biophilic, up to 75% of total iodine in fresh and coastal marine waters partitions into organic iodine; (2) super(129)I/ super(127)I ratios in tDOC are greatly elevated over those from marine systems because atmospheric emissions of super(129)I from European nuclear fuel reprocessing facilities were mixed more quickly in the surface ocean, up to 500 m in a decade, than the terrestrial system, which mixed approximately 10 cm in 10 to 50 y; and (3) the oceanic contribution of super(127)I (50 to 65 ppb) to the ratio has a greater dilution effect than super(127)I from freshwater (0.5 to 40 ppb). Analytical techniques were developed for super(129)I/ super(127)I ratio determination in dissolved organic iodine (DOI) and the other iodine species, using dehydrohalogenation, anion chromatography, high- performance liquid chromatography, and accelerator mass spectrometry, to be applied to samples from Galveston Bay, Texas. Results indicate that super(129)I/ super(127)I ratios in DOI from terrestrial sources are elevated in the upper estuary up to salinity of about 20, similar to a behavior previously described for this estuary for stable isotopic signals for dissolved organic matter. super(129)I/ super(127)I ratios in the other iodine species, e.g., iodide and iodate, did not show this feature, indicating fast isotopic and chemical equilibration between the two isotopes among the different inorganic species in the estuary. These results thus provide proof of concept that super(129)I/ super(127)I- DOI can serve as a tracer for tDOC in the coastal zone.anionscoastal zonedissolved solidsdissolved organic matterestuariesiodidesiodineisotopesliquid chromatographymass spectrometrymethodologysalinitysurface watertracersArticle