The influence of humic substances on the geochemistry of iodine in nearshore and hemipelagic marine sediments

Abstract

Iodine is characteristically enriched at the surface of hemipelagic and nearshore sediments deposited under oxygenated conditions. In such sediments, bulk I/C org ratios usually decrease with depth to values which are characteristic of anoxic sediments, reflecting a preferential release of I during early diagenesis. There is some debate as to whether sedimentary I is associated with the iron oxyhydroxide phase or with the organic fraction, and whether the decrease in I/C org with depth is due to the dissolution of the iron oxyhydroxides or the decomposition of labile organic matter. It is shown that in a surficial hemipelagic sediment sample and in a nearshore sediment core I is mainly associated with the organic fraction and, moreover, that humic substances are involved in the surficial iodine enrichment. Laboratory experiments on the uptake and release of I by and from sedimentary humic substances also suggest a mechanism whereby humic materials reduce iodate at the sediment/water interface to an electrophilic I species which further reacts with the organic matter to produce iodinated organic molecules. During burial, this excess I could be displaced from the organic matrix by nucleophiles such as sulphide ions or thiosulphate, thus providing a possible explanation for the decrease in I/C org ratio with depth observed in many nearshore and hemipelagic sediments.