Iron and nitrogen cycling, bacterioplankton community composition and mineral transformations involving phosphorus stabilisation in the ferruginous hypolimnion of a post-mining lake
Keyword(s):
C And N
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In the ferruginous and sulfate-rich bottom waters of the oligotrophic Lake Medard, P is bound to mineral clusters dominated by FeOOH polymorphs. Below the hypolimnion, Fe, C and N cycling seems largely controlled by Proteobacteria.