Main > MICROORGANISM > Archaebacteria > Feroplasma acidarmanus > Iron-Oxidizing. Acid-Tolerant

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OBSERVATION'S The archaeon, which is able to grow at pH 0, is the dominant microorganism in the subsurface environment the team investigated, accounting for < 85% of the resident microbial community. The organism lacks a cell wall, a feature that may be related to its ability to tolerate extremely acidic conditions.
The researchers believe it contributes to acid mine drainage by regenerating Fe(III), the primary oxidant at low pH in the process by which pyrite (FeS2) is converted to SO4H2 & water
- FeS2 + 14Fe(III) + 8H2O = 15Fe(II) + 2SO4(II) + 16H(I)
PREPARATION A primitive microorganism that oxidizes Fe & thrives at pH 0.5 has been isolated from the slimes & sediments that line a subsurface tunnel of an unused Cu mine in northern California
UPDATE 03.00
AUTHOR Edwards Katrina J.; Geomicrobiologist at Woods Hole Oceanographic Institute
LITERATURE REF. Science, 287, p. 1796 (2000)

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