July 13, 2015

Closer look at microorganism provides insight on carbon cycling



Some of the world’s tiniest organisms may have a large impact on climate change.

(July 13, 2015)  Researchers from the U.S. Department of Energy’s Argonne National Laboratory and the University of Tennessee found that microorganisms called archaea living in marine sediments use completely novel enzymes to break down organic matter into carbon dioxide.
These single-celled archaea eat organic carbon in marine sediments. Enzymes in the archaea break down large carbon molecules into smaller units. This process releases carbon dioxide and methane into the water and eventually, into the atmosphere.

However, as the temperature of oceans and bodies of freshwater increases, this carbon cycling process accelerates. The temperature at the bottom of the ocean, for example, is approximately two to four degrees Celsius (35 to 39 degrees Fahrenheit). According to Andrzej Joachimiak, Argonne distinguished fellow and director of the Structural Biology Center, if the ocean temperature rises one or two degrees, the rate of carbon release might increase.

“About 40 percent of Earth’s organic carbon is stored in marine sediments,” Joachimiak said. “An increase in temperature and acceleration of the carbon cycling process in these sediments is a major concern.”

Joachimiak said scientists are uncertain about how fast archaea process carbon and whether the release is accelerating. Once researchers have these statistics, they may find ways to better predict the environment’s response to a changing climate.

This understanding starts at the molecular level. Using resources at the Advanced Photon Source, a DOE Office of Science User Facility, and the Advanced Protein Characterization Facility, the research team produced and crystallized bathyaminopeptidase, or BAP – one of the enzymes found in the archaea – to look into its structure and observe how it operates. They found that BAP plays an important role in breaking down proteins and, consequently, the turnover of atmospheric carbon.

The biggest challenge the researchers had was determining BAP’s function, because no previously cultured organisms shared a close ancestry. These types of organisms are considered microbial “dark matter” because their physiologies are unknown and they have never been grown in a lab.

And because it is difficult to study their physiologies, scientists cannot determine their precise impact on ecosystems and major global events. For example, BAP was found to be structurally similar to the known amino acid ester hydrolase, but had evolved to serve an entirely different function.

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