http://news.sciencemag.org/sciencenow/2011/03/long-neglected-experiment-
gives-.html?ref=hp

A classic experiment that has sat on the shelf for more than a
half-century is yielding new clues about how life may have arisen on
Earth, according to a team of scientists that has gone back and analyzed
the data with modern techniques.

In 1952, Stanley Miller of the University of Chicago in Illinois and his
colleagues conducted one of the most famous experiments in all of
science. They repeatedly sent electric sparks through flasks filled with
the gases thought to resemble Earth's early atmosphere, including water
vapor, hydrogen, methane, and ammonia. After 1 week of near-continuous
zapping, the simulated lightning had converted a substantial portion of
the gases into organic compounds, including several of the amino acids
needed to produce proteins, indicating that this might be how life began
on our planet.

In the next few years, Miller and his colleagues repeated the experiment
with the same lab equipment and procedures but with different sets of
gases. For some reason, the results of the experiments were shelved but
not analyzed, surfacing again only after Miller died and colleagues
began poring through his archives. In 2008, researchers reported the
results of one of those experiments, in which the half-century-old
residues yielded 22 amino acids, 10 of which hadn't been detected in the
original 1952 experiment. 

Now, researchers have analyzed the results of another of Miller's
studies, one conducted in 1958. In that research, the team sent sparks
through a mixture of methane, ammonia, carbon dioxide, and hydrogen
sulfide. These gasses may have been similar to the noxious blend spewing
from early volcanoes, and thus they may have been more representative of
the environment in and around volcanic plumes than the gasses used in
the 1952 experiment. The resulting dried sludge has been stored in glass
vials inside cardboard boxes and kept at room temperature for more than
50 years.

Organic chemist Henderson "Jim" Cleaves of the Carnegie Institution for
Science in Washington, D.C., and his colleagues have now analyzed that
sludge using modern techniques and instruments that are more than 1
billion times more sensitive than the methods used by Miller in the
1950s. 

Their results, reported online today in the Proceedings of the National
Academy of Sciences, suggest that the 1958 experiment produced 23 amino
acids, including six that contained sulfur. The residue samples included
nearly equal proportions of left-handed and right-handed versions of
several amino acids, a sign that the organic chemicals had been
generated during the experiment and not by microorganisms that had
somehow made their way into the sealed glass vials. Living cells use and
produce only left-handed versions of amino acids, Cleaves says.

Not only did the newly analyzed experiment yield more amino acids than
did the one conducted in 1952, two of the sulfur-containing amino acids
produced in Miller's 1958 experiment-cysteine and methionine, which
weren't found in the results of the 1952 experiment-play particularly
important roles in biological processes, says Nicholas Hud, a biochemist
at the Georgia Institute of Technology in Atlanta, who was not
affiliated with the team. Moreover, he notes, "it's difficult to believe
that life as we know it wasn't incorporating sulfur-containing compounds
early on."

In addition to the sulfur-containing amino acids, the 53-year-old
residues contained threonine, leucine, and isoleucine, amino acids
important for certain biological processes that weren't detected in any
other electric-discharge experiments that Miller conducted.

The presence of hydrogen sulfide in the 1958 experiment seems to have
played a key role in producing the wealth of prebiotic chemicals
Cleaves's group found, says Hud. And although researchers still argue
about the precise composition of Earth's early atmosphere, most agree
that volcanic eruptions would have contributed hydrogen sulfide, he
adds.

The origin of life is a hotly debated topic, and the source of the
prebiotic chemicals in Earth's so-called primordial soup is one of its
enduring mysteries. Some researchers have argued that life could have
begun around deep-sea hydrothermal vents, where a warm, chemically
active, and mineral-rich broth spews from the ocean floor. But the new
analyses-like many of Miller's previously reported results-hint that
many of those substances could have formed in the lightning-riddled,
steam-filled plumes of volcanoes. 

However, the new analyses also suggest that the chemicals could have
fallen to Earth in meteorites, Cleaves says, because the relative
amounts of amino acids produced by Miller's 1958 experiment and those
found in certain carbon-rich meteorites are intriguingly similar.
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