Warming global temperatures may not affect carbon stored deep in northern peatlands
Deep stores of carbon in northern peatlands may remain stable despite rising temperatures, according to a team of researchers from several U.S.-based institutions.
And that is good news for now, the researchers said.
Florida State University research scientist Rachel Wilson and University of Oregon graduate student Anya Hopple are the first authors on a new study published in Nature Communications. The study details experiments suggesting that carbon stored in peat — a highly organic material found in marsh or damp regions — may not succumb to the Earth’s warming as easily as scientists thought.
That means if these northern peatlands — found in the upper half of the northern hemisphere — remain flooded, a substantial amount of carbon will not be released into the atmosphere.
“We do see some breakdown of peat on the surface, but not below 2 feet deep, where the bulk of the carbon is stored,” Wilson said.
The study is part of a long-term look at how carbon stored in peat will respond to climate and environmental change. The team of researchers, led by Paul Hanson of the Department of Energy’s Oak Ridge National Laboratory, includes scientists from FSU, University of Oregon, Georgia Institute of Technology, the U.S. Department of Agriculture-Forest Service, Chapman University, and Lawrence Livermore, Pacific Northwest and Oak Ridge national laboratories.
Researchers ran four different temperature simulations — increasing the temperature of the peat to a 2-foot depth by 2.25 degrees Celsius, 4.5 degrees Celsius, 6.25 degrees Celsius and 9 degrees Celsius — to see how it would respond to increased heat.
They found that the surface peat did emit more methane gas when warmed, but the deep peat did not break down and did not start emitting additional methane or carbon dioxide.
“If the release of greenhouse gases is not enhanced by temperature of the deep peat, that’s great news because that means that if all other things remain as they are, the deep peat carbon remains in the soil,” said Joel Kostka, professor of microbiology at Georgia Institute of Technology.
The Earth’s soils contain 1,550 billion tons of organic carbon, and 500 billion tons of this carbon is stored in northern peatlands around the world. This quantity is roughly the same amount as carbon in the atmosphere. Scientists have been anxious to learn how these northern peatlands will respond to warming because a tremendous amount of carbon could be released into the atmosphere.
Researchers worked at the DOE-funded ORNL experiment (operated on the USDA Forest Service's Marcell Experimental Forest) known as SPRUCE in northern Minnesota to examine both surface peat and peat up to 6 feet deep.
Large environmental chambers were constructed by the Oak Ridge team to enclose portions of the peatlands. Within these chambers, scientists simulated climate change effects such as higher temperatures and elevated carbon dioxide levels. They also took some of the deep peat back to their labs to heat in additional studies.
While scientists said they were surprised by the results, they also cautioned that this came only after one year of warming.
“There are the necessary caveats that this was only for one year, and the experiment is planned to run for a decade, and other ecosystem feedbacks may become important in greenhouse gas emissions,” said Scott Bridgham, director of the Institute of Ecology and Evolution at University of Oregon and Hopple’s adviser.
In the future, scientists also plan to look at how these peatlands respond to heightened carbon dioxide levels combined with the temperature increases.
“In the future, we’ll be warmer, but we’ll also have more carbon dioxide in the atmosphere, so we need to understand how these deep stores of peat, which have all this carbon, respond to these conditions,” said Jeff Chanton, professor of oceanography at Florida State University.
“These initial SPRUCE results demonstrate the importance of direct experiments for expanding our understanding of peatland carbon cycling processes,” ORNL’s Paul Hanson, SPRUCE project coordinator, said. “They suggest a need to improve how models project future carbon cycle changes and greenhouse gas emissions.”
SPRUCE is supported by DOE’s Office of Science, Office of Biological and Environmental Research, Climate and Environmental Science Division and the Terrestrial Ecosystem Science Program.
UT-Battelle manages ORNL for the DOE’s Office of Science. The Office of Science is the single largest supporter of basic research in the physical sciences in the United States and is working to address some of the most pressing challenges of our time. For more information, please visit http://science.energy.gov/.
Contributed by Sara Shoemaker, Communications