Hydrogen peroxide is ubiquitous in the surface mixed layer of the ocea
n and is an important chemical intermediate of aerobic systems. Due to
its reactive nature and numerous chemical redox processes, H2O2 decom
position has been suggested to occur mainly through abiotic pathways i
nvolving various seawater constituents. Its decomposition rates in nat
ural seawater show considerable spatial variability and generally obey
first order kinetics with half-lives ranging from less than 10 hours
in coastal waters to greater than 120 hours in surface waters of the o
pen ocean. This study demonstrates that hydrogen peroxide decompositio
n in natural seawater appears primarily to be biologically mediated by
microorganisms less than 1 mu m diameter. Cultured microorganisms add
ed to seawater, especially the prokaryotes Vibrio pelagius and Synecho
coccus sp. were very efficient mediators of H2O2 decomposition.