Common structure in the heterogeneity of plant-matter decay
- PMID: 22535699
- PMCID: PMC3405759
- DOI: 10.1098/rsif.2012.0122
Common structure in the heterogeneity of plant-matter decay
Abstract
Carbon removed from the atmosphere by photosynthesis is released back by respiration. Although some organic carbon is degraded quickly, older carbon persists; consequently carbon stocks are much larger than predicted by initial decomposition rates. This disparity can be traced to a wide range of first-order decay-rate constants, but the rate distributions and the mechanisms that determine them are unknown. Here, we pose and solve an inverse problem to find the rate distributions corresponding to the decomposition of plant matter throughout North America. We find that rate distributions are lognormal, with a mean and variance that depend on climatic conditions and substrate. Changes in temperature and precipitation scale all rates similarly, whereas the initial substrate composition sets the time scale of faster rates. These findings probably result from the interplay of stochastic processes and biochemical kinetics, suggesting that the intrinsic variability of decomposers, substrate and environment results in a predictable distribution of rates. Within this framework, turnover times increase exponentially with the kinetic heterogeneity of rates, thereby providing a theoretical expression for the persistence of recalcitrant organic carbon in the natural environment.
Figures
References
-
- Falkowski P., et al. 2000. The global carbon cycle: a test of our knowledge of earth as a system. Science 290, 291–296 10.1126/science.290.5490.291 (doi:10.1126/science.290.5490.291) - DOI - PubMed
-
- Gholz H. L., Wedin D. A., Smitherman S. M., Harmon M. E., Parton W. J. 2000. Long-term dynamics of pine and hardwood litter in contrasting environments: toward a global model of decomposition. Glob. Change Biol. 6, 751–765 10.1046/j.1365-2486.2000.00349.x (doi:10.1046/j.1365-2486.2000.00349.x) - DOI
-
- Tenney F. G., Waksman S. A. 1929. Composition of natural organic materials and their decomposition in the soil. IV. The nature and rapidity of decomposition of the various organic complexes in different plant materials, under aerobic conditions. Soil Sci. 28, 55–84 10.1097/00010694-192907000-00005 (doi:10.1097/00010694-192907000-00005) - DOI
-
- Berg B., McClaugherty C. 2007. Plant litter: decomposition, humus formation, carbon sequestration, 2nd edn. Berin, Germany: Springer
-
- Oades J. 1988. The retention of organic matter in soils. Biogeochemistry 5, 35–70 10.1007/BF02180317 (doi:10.1007/BF02180317) - DOI
Publication types
MeSH terms
Substances
LinkOut - more resources
Full Text Sources