Published July 13, 1990 | Version v1
Journal article

A thiosulfate shunt in the sulfur cycle of marine sediments

  • 1. Univ. of Aarhus (Denmark)

Description

The oxidation of sulfide, generated by bacterial sulfate reduction, is a key process in the biogeochemistry of marine sediments, yet the pathways and oxidants are poorly known. By the use of 35S-tracer studies of the S cycle in marine and freshwater sediments, a novel shunt function of thiosulfate (S2O32-) was identified. The S2O32- constituted 68 to 78% of the immediate HS--oxidation products and was concurrently reduced back to HS-, oxidized to SO42-, and disproportionated to HS- + SO42-. The small thiosulfate pool is thus involved in a dynamic HS--S2O32- cycle in anoxic sediments. The disproportionation of thiosulfate may help account for the large difference in isotopic composition of sulfate and sulfides in sediments and sedimentary rocks

Additional details

Publishing Information

Journal Title
Science (Washington, D.C.)
Journal Volume
249
Journal Issue
4965
Series
Science (Washington, D.C.).
Journal Page Range
152-154
ISSN
0036-8075
CODEN
SCIEA