Bj. Bratina et al., MANGANESE REDUCTION BY MICROBES FROM OXIC REGIONS OF THE LAKE VANDA (ANTARCTICA) WATER COLUMN, Applied and environmental microbiology (Print), 64(10), 1998, pp. 3791-3797
Depth profiles of metals in Lake Vanda, a permanently ice-covered, str
atified Antarctic lake, suggest the importance of particulate manganes
e oxides in the scavenging, transport, and release of metals. Since ma
nganese oxides can be solubilized by manganese-reducing bacteria, micr
obially mediated manganese reduction was investigated in Lake Vanda. M
icrobes concentrated from oxic regions of the water column, encompassi
ng a peak of soluble manganese [Mn(II)], reduced synthetic manganese o
xides (MnO2) when incubated aerobically. Pure cultures of manganese-re
ducing bacteria were readily isolated from waters collected near the o
xic Mn(II) peak Based on phylogenetic analysis of the 16S rRNA gene se
quence, most of the isolated manganese reducers belong to the genus Ca
rnobacterium. Cultures of a phylogenetically representative strain of
Carnobacterium reduced synthetic MnO2 in the presence of sodium azide,
as was seen in field assays. Unlike anaerobes that utilize manganese
oxides as terminal electron accepters in respiration, isolates of the
genus Carnobacterium reduced Mn(IV) via a diffusible compound under ox
ic conditions. The release of adsorbed trace metals accompanying the s
olubilization of manganese oxides may provide populations of Carnobact
erium with a source of nutrients in this extremely oligotrophic enviro
nment.