Plant traits and wood fates across the globe: rotted, burned, or consumed?
Article first published online: 13 MAR 2009
© 2009 Blackwell Publishing Ltd
Global Change Biology
Volume 15, Issue 10, pages 2431–2449, October 2009
How to Cite
CORNWELL, W. K., CORNELISSEN, J. H. C., ALLISON, S. D., BAUHUS, J., EGGLETON, P., PRESTON, C. M., SCARFF, F., WEEDON, J. T., WIRTH, C. and ZANNE, A. E. (2009), Plant traits and wood fates across the globe: rotted, burned, or consumed?. Global Change Biology, 15: 2431–2449. doi: 10.1111/j.1365-2486.2009.01916.x
- Issue published online: 4 SEP 2009
- Article first published online: 13 MAR 2009
- Received 26 September 2008; revised version received 2 February 2009 and accepted 5 February 2009
- C cycle;
- microbial decay;
Wood represents the defining feature of forest systems, and often the carbon in woody debris has a long residence time. Globally, coarse dead wood contains 36–72 Pg C, and understanding what controls the fate of this C is important for predicting C cycle responses to global change. The fate of a piece of wood may include one or more of the following: microbial decomposition, combustion, consumption by insects, and physical degradation. The probability of each fate is a function of both the abiotic environment and the wood traits of the species. The wood produced by different species varies substantially in chemical, micro- and macro-morphological traits; many of these characteristics of living species have ‘afterlife’ effects on the fate and turnover rate of dead wood. The colonization of dead wood by microbes and their activity depends on a large suite of wood chemical and anatomical traits, as well as whole-plant traits such as stem-diameter distributions. Fire consumption is driven by a slightly narrower range of traits with little dependence on wood anatomy. Wood turnover due to insects mainly depends on wood density and secondary chemistry. Physical degradation is a relatively minor loss pathway for most systems, which depends on wood chemistry and environmental conditions. We conclude that information about the traits of woody plants could be extremely useful for modeling and predicting rates of wood turnover across ecosystems. We demonstrate how this trait-based approach is currently limited by oversimplified treatment of dead wood pools in several leading global C models and by a lack of quantitative empirical data linking woody plant traits with the probability and rate of each turnover pathway. Explicitly including plant traits and woody debris pools in global vegetation climate models would improve predictions of wood turnover and its feedback to climate.