Dynamic mercury methylation and demethylation in oligotrophic marine water
Dynamic mercury methylation and demethylation in oligotrophic marine water
复制标题
寡营养海水中的动态汞甲基化和去甲基化
作者:
K. Munson;C. Lamborg;R. Boiteau;M. Saito
Abstract. Mercury bioaccumulation in open-ocean food webs depends on the net rate of
inorganic mercury conversion to monomethylmercury in the water column. We
measured significant methylation rates across large gradients in oxygen
utilization in the oligotrophic central Pacific Ocean. Overall, methylation
rates over 24 h incubation periods were comparable to those previously
published from Arctic and Mediterranean waters despite differences in
productivity between these marine environments. In contrast to previous
studies that have attributed Hg methylation to heterotrophic bacteria, we
measured higher methylation rates in filtered water compared to unfiltered
water. Furthermore, we observed enhanced demethylation of newly produced
methylated mercury in incubations of unfiltered water relative to filtered
water. The addition of station-specific bulk filtered particulate matter, a
source of inorganic mercury substrate and other possibly influential
compounds, did not stimulate sustained methylation, although transient
enhancement of methylation occurred within 8 h of addition. The addition
of dissolved inorganic cobalt also produced dramatic, if transient, increases
in mercury methylation. Our results suggest important roles for noncellular
or extracellular methylation mechanisms and demethylation in determining
methylated mercury concentrations in marine oligotrophic waters. Methylation
and demethylation occur dynamically in the open-ocean water column, even in
regions with low accumulation of methylated mercury.