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MADISON -- A newfound microbe that eats iron and lives in
acid-drenched conditions has been identified as a chief suspect in
the environmental damage caused by metal ore mining.
Writing in the Friday, March 10, edition of the journal Science, a
team of scientists from the University of Wisconsin-Madison report
the discovery in an old mine of an archaeon that thrives when metal
sulfide ores are exposed to air and water, conditions that mimic hot
battery acid. The microbe, the scientists say, is present in such
abundance that it is believed to be a key mediator of the process of
acid mine drainage, the primary environmental problem associated with
the extraction of metal ores from the earth.
The microbe shows an ability to transform the sulfide found in metal
ores to sulfuric acid, the chemical pollutant that contaminates
mining sites and drains into nearby rivers, streams and groundwater.
"We think this new archaeon might be one of the more important
players in catalyzing these reactions," says Katrina J. Edwards, the
lead author of the Science article.
Microbial archaea, a branch of life with ancient roots, have
different basic characteristics than other microscopic organisms such
as bacteria.
Edwards is a geomicrobiologist at the Woods Holes Oceanographic
Institute, Woods Hole, Mass. The work, funded largely by the National
Science Foundation, was conducted as part of her doctoral thesis at
UW-Madison in the lab of Jillian Banfield, a professor of geology and
geophysics and a co-author of the study.
The discovery of the new microbe is important because it helps
explain how the natural cycle of the conversion of sulfide to
sulfuric acid is greatly accelerated around mines. Moreover, the
physiological character of the archaeon is of great interest because
it has no cell wall, defying the idea that microorganisms tough it
out in nasty environments with the help of durable external walls to
shield themselves from extreme conditions.
It is possible, according to Edwards, that the microbe found in such
abundance at the Iron Mountain Mine near Redding, Calif., is
ubiquitous in nature, living off ore bodies exposed naturally to air
and water and geochemically impacting iron and sulfur cycles.
But under the conditions created by the mining of metal ores, where
many tons or ores and tailings are exposed, the organism thrives and
revs up the production of sulfuric acid.
"It speeds up environmental damage," says Banfield, an authority on
the relationship between microbes and minerals. "The organism's
metabolism greatly accelerates the acid mine drainage process" by
converting the solid sulfide mineral to sulfuric acid, a corrosive
liquid that leaches from mining sites into the surrounding
environment. The process has caused billions of dollars in damage to
the environment worldwide.
"This is a process that takes place all over the Earth's crust, but
mining exacerbates the problem by exposing metal to air and water,"
she says.
Banfield's group has been working at the Iron Mountain Mine for
nearly five years, and has gained significant insight into an
environment that is extremely hostile to any form of life, an
environment that is acidic, hot and full of toxic metals.
"The mine has a fairly simple ecology and this seems to be the major
player," says Banfield. "It oxidizes irons and forms slimes and grows
on pyrite sediments."
The new archaeon, dubbed Ferroplasma acidarmanus, is one of about a
dozen microbes found in the mine, Banfield says. Her group determined
the newfound microbe was among the most active and numerous in the
mine by sampling during the summer when the sediment solutions in the
mine are concentrated.
The biology of Ferroplasma acidarmanus is sure to be of interest in
part because of the peculiar fact that it has no cell wall. "It turns
out to be a bit of an irony that the most abundant organisms in the
mine might be considered to be rather fragile since they lack cell
walls," says Edwards. "It's cytoplasm is surrounded only by a single,
peripheral membrane."
How the microbe endures the heat, acid and high metal concentrations
of its own environment is unknown. But the fact that it does, says
Banfield, is certain to be of interest to people studying the origins
of life on Earth and the possibility that microbial life may exist
beyond the confines of Earth.
It could be, says Banfield, that the organism's seemingly fragile
cytoplasmic membrane confers an advantage that is yet unknown to
science.
Research on the new microbe and its remarkable abilities will
continue at UW-Madison in collaboration with Brian Fox, a UW-Madison
professor of biochemistry, and Charles Kaspar, a UW-Madison
environmental toxicologist and professor of food microbiology and
toxicology.
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WRITER: Terry Devitt (608) 262-8282; trdevitt@facstaff.wisc.edu
CONTACT: Katrina Edwards (508) 289-3620, kedwards@whoi.edu; Jillian Banfield (608) 265-9528, jill@geology.wisc.edu.
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