Changes in plant species and functional composition with time since fire in two mediterranean climate plant communities
Article first published online: 29 MAY 2012
© 2012 International Association for Vegetation Science
Journal of Vegetation Science
Volume 23, Issue 6, pages 1071–1081, December 2012
How to Cite
Gosper, C. R., Yates, C. J., Prober, S. M. (2012), Changes in plant species and functional composition with time since fire in two mediterranean climate plant communities. Journal of Vegetation Science, 23: 1071–1081. doi: 10.1111/j.1654-1103.2012.01434.x
- Issue published online: 7 NOV 2012
- Article first published online: 29 MAY 2012
- Manuscript Accepted: 18 APR 2012
- Manuscript Received: 27 OCT 2011
- Department of Environment and Conservation's
- Saving Our Species Initiative
- CSIRO Ecosystem Sciences
- Fire-return interval;
- Obligate seeder;
- Plant functional type;
- Seed bank;
- South-western Australia
Do floristic composition and plant functional type (PFT) richness and dominance change with time since fire, in the directions predicted through consideration of their fire response traits?
Two vegetation communities in the globally significant biodiversity hotspot of south-western Australia: mallee, dominated by resprouters, and mallee-heath, dominated by non-resprouters.
Species richness and cover were sampled in replicated plots across a time since fire gradient ranging from 2 to >55 yr post-fire, using a space-for-time approach. Species were allocated to PFTs according to traits relevant to the processes of vegetation change underpinning the initial floristic composition model of vegetation assembly: their capacity to resprout, the location and persistence of the seed bank, competitive stratum and longevity. Ordination and ANOVA were used to test for differences in floristic and PFT composition between young (<10 yr post-fire), mature (18–35 yr) and old (>40 yr) vegetation in each community.
Plant functional type and floristic analyses were similar, showing substantial changes in the composition of mallee-heath vegetation with time since fire, but not in mallee. The direction of change in PFT composition in mallee-heath was consistent with predictions, with increasing cover of non-resprouting, serotinous PFTs, an intermediate peak in cover of PFTs with persistent soil-stored seed banks, and decreasing cover of post-fire ephemerals and non-resprouting, non-serotinous dwarf shrubs, herbs and graminoids with increasing time since fire. Success in predicting changes in PFT dominance in mallee was lower.
The similarity of floristic and PFT analyses suggest that these approaches are interchangeable for characterizing vegetation change with increasing time since fire. PFTs were more effective for predicting fire response trajectories in the vegetation community dominated by non-resprouting, serotinous shrubs (mallee-heath) than that dominated by resprouting, serotinous trees (mallee). The underlying vegetation assembly model and PFTs used appear suitable for broader application in fire-prone communities with competitive dominance by non-resprouting, serotinous shrubs, but less so in communities dominated by other PFTs.