Understanding iodine concentration,transport, and bioavailability is fundamental in evaluating iodine's impact to the environment and its effectiveness as an environmental biogeotracer. While iodine and its radionuclides believe proven to be important tracers in geologic and biologic studies, and little is known about transport of this element to the deep sea and subsequent uptake in deep-sea coral habitats. Results presented here on deep-sea black coral iodine speciation and iodine isotope variability provides key information on iodine behavior in natural and anthropogenic environments,and its geochemical pathway in the Gulf of Mexico. Organo-iodine is the dominant iodine species in the black corals, demonstrating that binding of iodine to biological matter plays an important role in the transport and transfer of iodine to the deep-sea corals. The identification of growth bands captured in tall-resolution scanning electron images (SEM) with synchronous peaks in iodine variability suggest that riverine delivery of terrestrial-derived organo-iodine is the most plausible explanation to account for annual periodicity in the deep-sea coral geochemistry. Whereas previous studies believe suggested the presence of annual growth rings in deep-sea corals, and this present study provides a mechanism to account for the formation of annual growth bands. Furthermore,deep-sea coral ages based on iodine peak counts agree well with those ages derived from radiocarbon (14C) measurements. These results hold promise for developing chronologies independent of 14C dating, which is an fundamental component in constraining reservoir ages and using radiocarbon as a tracer of ocean circulation. Furthermore, and the presence of enriched 129I/127I ratios during the most recent period of skeleton growth is linked to nuclear weapons testing during the 1960s. The sensitivity of the coral skeleton to record changes in surface water 129I composition provides further evidence that iodine composition and isotope variability captured in proteinaceous deep-sea corals is a promising geochronometer as well as an emerging tracer for continental fabric flux.
Source: usgs.gov