Geochemical Niches of Iron-Oxidizing Acidophiles in Acidic Coal Mine Drainage
ABSTRACTA legacy of coal mining in the Appalachians has provided a unique opportunity to study the ecological niches of iron-oxidizing microorganisms. Mine-impacted, anoxic groundwater with high dissolved-metal concentrations emerges at springs and seeps associated with iron oxide mounds and deposits. These deposits are colonized by iron-oxidizing microorganisms that in some cases efficiently remove most of the dissolved iron at low pH, making subsequent treatment of the polluted stream water less expensive. We used full-cycle rRNA methods to describe the composition of sediment communities at two geochemically similar acidic discharges, Upper and Lower Red Eyes in Somerset County, PA, USA. The dominant microorganisms at both discharges were acidophilicGallionella-like organisms, “Ferrovum” spp., andAcidithiobacillusspp.ArchaeaandLeptospirillumspp. accounted for less than 2% of cells. The distribution of microorganisms at the two sites could be best explained by a combination of iron(II) concentration and pH. Populations of theGallionella-like organisms were restricted to locations with pH >3 and iron(II) concentration of >4 mM, whileAcidithiobacillusspp. were restricted to pH <3 and iron(II) concentration of <4 mM.Ferrovumspp. were present at low levels in most samples but dominated sediment communities at pH <3 and iron(II) concentration of >4 mM. Our findings offer a predictive framework that could prove useful for describing the distribution of microorganisms in acid mine drainage, based on readily accessible geochemical parameters.