Litter Decomposition in Grasslands
Bontti, E.E., Decant, J.P., Munson, S.M., Gathany, M.A., Prezeszlowska, A., Haddix, M.L., Owens, S., Burke, I.C., Parton, W.J. and Harmon, M.E. 2009. Litter decomposition in grasslands of Central North America (US Great Plains). Global Change Biology 15: 1356-1363.
"Contrary to expectations," as the ten researchers report, "temperature did not explain variation in root and leaf decomposition," while precipitation only partially explained variation in root decomposition. Percent lignin, on the other hand, was found to be "the best predictor of leaf and root decomposition" and "also explained most variation in root decomposition in models which combined litter quality and climatic variables." These latter consequences were said by them to be due to the fact that "litter that is high in percent lignin contains a large amount of decay-resistant carbon material and a relatively small proportion of easily decomposable compounds," so that it decomposes at relatively slower rates.
Based on the results of their specific study, Bontti et al. conclude that "carbon flux from root decomposition in grasslands would increase, as a result of increasing temperature, only if precipitation is not limiting [italics added]," and that "where precipitation is limiting, increased temperature would decrease root decomposition, thus likely increasing carbon storage in grasslands."
These observations suggest that global warming likely does not possess "the potential to elicit a positive feedback between increased temperature, decomposition, and carbon dioxide emissions, further increasing global temperatures." Indeed, the research team explicitly states that the results of their study "do not support the hypothesis of increased decomposition as a result of increased global temperature."