10th July 2012
Rising carbon dioxide levels in the atmosphere affect carbon cycling and speed carbon loss from forest soils, research shows.
The new evidence supports an emerging view that although forests remove a substantial amount of carbon dioxide from the atmosphere, much of the carbon is being stored in living woody biomass rather than as dead organic matter in soils.
After nearly two decades of research on forest ecosystem responses to global change, some of the uncertainty has been lifted about how forests are storing carbon in the wake of rising carbon dioxide levels, says lead author Richard P. Phillips, assistant professor of biology at Indiana University.
Straight from the Source
Carbon stored in soils, as opposed to in the wood of trees, is desirable from a management perspective because soils are more stable over time, so carbon can be locked away for hundreds to thousands of years and not contribute to atmospheric carbon dioxide increases.
The research, published July 9 in the online early addition of Ecology Letters, was conducted at the Duke Forest Free Air Carbon Dioxide Enrichment site in North Carolina. At this site, mature loblolly pine trees were exposed to increased levels of carbon dioxide for 14 years, making it one of the longest-running carbon dioxide enrichment experiments in the world.
Researchers were able to calculate the age of the carbon cycling through the soil by growing roots and fungi into mesh bags that contained uniquely labeled soils. The soils were then analyzed for their organic composition.
The authors also report that nitrogen cycled faster in this forest as the demand for nutrients by trees and microbes became greater under elevated CO2.
“The growth of trees is limited by the availability of nitrogen at this site, so it makes sense that trees are using the ‘extra’ carbon taken up under elevated CO2 to prime microbes to release nitrogen bound up in organic matter,” Phillips says. “What is surprising is that the trees seem to be getting much of their nitrogen by decomposing root and fungal detritus that is less than a year old.”
The two-fold effects of microbial priming, where microbes are stimulated to decompose old soil organic matter via an increase in new carbon and other energy sources, and the faster turnover of recently fixed root and fungal carbon, are enough to explain the rapid carbon and nitrogen cycling that is occurring at the Duke Forest FACE site.
“We call it the RAMP hypothesis—Rhizo-Accelerated Mineralization and Priming—and it states that root-induced changes in the rates of microbial processing of carbon and nitrogen are key mediators of long-term ecosystem responses to global change,” Phillips adds.
“Most ecosystem models have limited representations of roots, and none of them include processes such as priming. Our results demonstrate that interactions between roots and soil microbes play an underappreciated role in determining how much carbon is stored and how fast nitrogen is cycled. So including these processes in models should lead to improved projections of long-term carbon storage in forests in response to global environmental change’” he says.
Researchers from Duke University, the University of New Hampshire, Boston University, and the University of Gottingen in Germany contributed to the study that received funding from the U.S. Department of Agriculture and the U.S. Department of Energy.