Vertical profiles of dissolved and particulate
210Po and
210Pb were measured across the redox transition zone at Station F1 in Framvaren Fjord, Norway. In this fjord, a sharp decrease in pH above the O
2/H
2S interface facilitates the aerobic dissolution of MnO
2. In contrast, Fe(II) concentrations begin to increase only at the O
2/H
2S interface depth. Activity profiles reveal that dissolved
210Po and
210Pb are sequestered efficiently by particulates in surface waters. As polonium-210 and lead-210 activities descend down into the aerobic manganese reduction (AMR) zone, they are remobilized during the reductive dissolution of the carrier phase oxyhydroxides. Both
210Po and
210Pb are highly enriched at the O
2/H
2S interface where an active community of microbes, such as anoxygenic phototrophs (e.g.,
Chromatium,
Chlorobium sp.), thrives. The coincident peaks in
210Po,
210Pb and microbial biomass suggest a strong biological influence on the behavior of these radionuclides. There is a strong covariance between the vertical distribution of Mn and Pb, indicating that their redox cycling is closely coupled and is likely microbially mediated.
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