| BLACKSBURG,
Va.-- An ancient organism from the pit of a collapsed volcano may hold
the key to tomorrow's hydrogen economy. Scientists from across the world
have formed a team to unlock the process refined by a billions-year old
archaea. The U.S. Department of Energy Joint Genome Institute will expedite
the research by sequencing the hydrogen-producing organism for comparative
genomics.
When members of the Russian Academy
of Sciences isolated a rare archaeal microorganism that breaks down cellulose
and produces hydrogen, Biswarup Mukhopadhyay, an assistant professor with
the Virginia Bioinformatics Institute at Virginia Tech, saw an opportunity
to open a door for development of a cellulose-based high-temperature hydrogen
production process. “Hydrogen can be easily converted to electrical and
mechanical energy without any production of carbon dioxide,” said Mukhopadhyay,
whose lab specializes in very high temperature or hyperthermophilic archaea
and in energy production.
Elizaveta Bonch-Osmolovskaya and
her colleagues at the Winogradsky Institute of Microbiology of the Russian
Academy of Sciences discovered the rare archaeon that can chew up cellulose
and exhale hydrogen. They found Desulfurococcus fermentans in the Uzon
Caldera on the Kamchatka Peninsula, an isolated spit of land in eastern
Siberia that is full of volcanoes and their remnants. D. fermentans degrades
cellulose from the higher plants that fall in the caldera. Meanwhile, this
renegade archaeon’s four closest relatives do not degrade cellulose or
make hydrogen, Bonch-Osmolovskaya wrote in the February 2005 edition of
the International Journal of Systematic and Evolutionary Microbiology.
Like most such organisms, these relatives reduce sulfur to hydrogen sulfide
(think rotten eggs).
The East Thermal Field of the Uzon
Caldera, Kamchatka, is home to hydrogen producing archaeon. Image courtesy
of Elizaveta Bonch-Osmolovskaya of the Russian Academy of Sciences
“Since hydrogen blocks the growth
for most fermenting archaea, they rarely produce hydrogen,” said Mukhopadhyay.
“But D. fermentans is not bothered by hydrogen. We want to discover why.
One way will be to compare the genomes of D. fermentans and its relatives
that do not have the special abilities.”
This novel hyperthermophilic archaea
grows best at 80 to 82 degrees Celsius (176-180 Farenheit), close to the
boiling point of water. “The ability to operate at high temperatures has
advantages – it is faster and the hydrogen producing bioreactor will not
be contaminated by common microbes,” said Mukhopadhyay.
At the Thermophiles 2007 conference
in Bergen, Norway, Mukhopadhyay discussed collaboration with Bonch-Osmolovskaya,
Haruyuki Atomi of Kyoto University, and Todd Lowe of the University of
California, Santa Cruz. He had similar conversations with Venkat Gopalan
of the Ohio State University and Nikos Kyrpides and Iain Anderson of the
U.S. Department of Energy Joint Genome Institute (JGI).
Mukhopadhyay’s laboratory began conducting
physiological studies with D. fermentans, which provided some information
on the growth and hydrogen production kinetics with cellulose and starch
as substrates. With these preparations and with support from the team,
Mukhopadhyay submitted a proposal to sequence the genomes of D. fermentans
and two of it cousins to the Joint Genome Institute’s Community Sequencing
Program, which sequences the genomes of organisms relevant to department
of energy missions at no charge. Organisms to be sequenced are selected
from proposals based on scientific merit and the degree of interest by
the scientific community. The researchers then have six months to use the
information before it is submitted to a gene bank for use by the world’s
scientific community. In mid-June, the Joint Genome Institute approved
the proposal titled “A Comparative Genomics Investigation on Hydrogen Production
from Cellulosic Materials and Starch by a Hyperthermophilic Archaeon.”
(See the department of energy announcement.)
The Joint Genome Institute had already
targeted another sulfur-reducing cousin of D. fermentans to fill in a gap
in the Genomic Encyclopedia of Bacteria and Archaea (GEBA). “Therefore,
we will have genome information of D. fermentans that degrade cellulose
and make hydrogen and similar information for three cousins that do not
have these properties. We will perform genomic subtraction exercises to
figure out which genes and regulatory circuits make D. fermentans so capable.
These data will guide more intensive and focused investigations on the
cellulose degradation and hydrogen production,” Mukhopadhyay said. “This
is just the beginning of an exploration of hitherto unknown processes with
potential to advance energy production and having a team will make it more
innovative, productive and fun.”
The East Thermal Field of the Uzon
Caldera, Kamchatka, is home to hydrogen producing archaeon. Image courtesy
of Elizaveta Bonch-Osmolovskaya of the Russian Academy of Sciences.
Contact Susan Trulove at strulove@vt.edu
or (540) 231-5646. |