New research shows how marine organisms help oceans sequester carbon
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ARGONNE, Ill. (June 6, 2008)—As the international search for ways to
remove carbon dioxide and other greenhouse gases from the environment intensifies,
a team of scientists has identified a process by which marine organisms influence
the amount of atmospheric carbon the sea absorbs.
Oceanic diatoms—unicellular glassy algae—harvest a key energy-storing
molecule containing phosphorus from the dissolved compounds in ocean water.
Instead of processing the phosphorus and releasing it back into the environment,
the algae collect and store it in a compound known as a polyphosphate, said
physicist Ian McNulty of the U.S. Department of Energy's Argonne National
Laboratory. McNulty collaborated with researchers from the Skidaway
Institute of Oceanography, Georgia, and the Georgia
Institute of Technology and the University
of South Carolina.
The algae then convert these polyphosphate compounds into microscopic pellets
that they store for energy. When these diatoms die, however, the polyphosphate
pellets contained in their skeletons sink to sediments at the bottom of the
ocean. With time, the polyphosphates are transformed into a mineral phosphate
called apatite, thus completing the sequestration of phosphorus from seawater.
"If we can understand how phosphorus uptake, metabolism and sequestration
take place within marine organisms, we could uncover information
that might give us clues as to how carbon uptake and sequestration take place
in the ocean and affect the global carbon balance," McNulty said. "This
research is of huge interest to climatologists and bears directly on and the
potential to combat global warming."
Phosphorus is one of the principal ingredients of fertilizer as well as many
other compounds present in significant quantities in agricultural runoff that
winds up in large bodies of water, said oceanographer Jay Brandes of Skidaway,
who collaborated with McNulty on the research.
"Oceans are the repositories of everything that washes off of the lands,
and phosphorus is an important nutrient for all kinds of life, especially plant
life." Brandes said. "The interesting thing about this particular
process is that because these diatoms need it to survive, the levels of phosphorus
will control the size of the algae population. As the diatoms use up the available
phosphorus and turn it into polyphosphates, they will die off in large numbers,
altering the phosphorus balance."
In most regions of the ocean, nutrient levels in the water dictate the rate
of both phosphorus and carbon sequestration. The removal of carbon from the
environment is controlled by the removal of phosphorus and nitrogen, according
to Brandes.
During the course of their research, McNulty and his colleagues were surprised
to discover that the diatoms created polyphosphates even in waters that contained
relatively low concentrations of dissolved phosphorus. The polyphosphates created
by the diatoms also proved more durable than anticipated, Brandes said, allowing
the researchers to glimpse their entire lifecycle from solutes to apatite.
Much of the research, led by oceanographer Ellery Ingall of Georgia
Tech, was performed at Argonne's Advanced Photon Source. The results were
published in the May 2 issue of the journal Science.
McNulty's work on this research project was funded by the U.S. Department
of Energy's Office of Science, Office of Basic
Energy Sciences. Brandes' and
Ingall's work was funded by the National
Science Foundation.
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of Science.
By Jared Sagoff.
For more information, please contact Steve McGregor (630/252-5580 or media@anl.gov) at Argonne.
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