Plant species and functional group effects on abiotic and microbial soil properties and plant–soil feedback responses in two grasslands
Article first published online: 11 JUL 2006
Journal of Ecology
Volume 94, Issue 5, pages 893–904, September 2006
How to Cite
BEZEMER, T. M., LAWSON, C. S., HEDLUND, K., EDWARDS, A. R., BROOK, A. J., IGUAL, J. M., MORTIMER, S. R. and VAN DER PUTTEN, W. H. (2006), Plant species and functional group effects on abiotic and microbial soil properties and plant–soil feedback responses in two grasslands. Journal of Ecology, 94: 893–904. doi: 10.1111/j.1365-2745.2006.01158.x
- Issue published online: 11 JUL 2006
- Article first published online: 11 JUL 2006
- Received 20 March 2006 revision accepted 24 May 2006 Handling Editor: Rien Aerts
- chalk grassland;
- ecosystem functioning;
- mechanisms of plant–soil feedback;
- soil biodiversity;
- soil chemistry;
- variance partitioning
- 1Plant species differ in their capacity to influence soil organic matter, soil nutrient availability and the composition of soil microbial communities. Their influences on soil properties result in net positive or negative feedback effects, which influence plant performance and plant community composition.
- 2For two grassland systems, one on a sandy soil in the Netherlands and one on a chalk soil in the United Kingdom, we investigated how individual plant species grown in monocultures changed abiotic and biotic soil conditions. Then, we determined feedback effects of these soils to plants of the same or different species. Feedback effects were analysed at the level of plant species and plant taxonomic groups (grasses vs. forbs).
- 3In the sandy soils, plant species differed in their effects on soil chemical properties, in particular potassium levels, but PLFA (phospholipid fatty acid) signatures of the soil microbial community did not differ between plant species. The effects of soil chemical properties were even greater when grasses and forbs were compared, especially because potassium levels were lower in grass monocultures.
- 4In the chalk soil, there were no effects of plant species on soil chemical properties, but PLFA profiles differed significantly between soils from different monocultures. PLFA profiles differed between species, rather than between grasses and forbs.
- 5In the feedback experiment, all plant species in sandy soils grew less vigorously in soils conditioned by grasses than in soils conditioned by forbs. These effects correlated significantly with soil chemical properties. None of the seven plant species showed significant differences between performance in soil conditioned by the same vs. other plant species.
- 6In the chalk soil, Sanguisorba minor and in particular Briza media performed best in soil collected from conspecifics, while Bromus erectus performed best in soil from heterospecifics. There was no distinctive pattern between soils collected from forb and grass monocultures, and plant performance could not be related to soil chemical properties or PLFA signatures.
- 7Our study shows that mechanisms of plant–soil feedback can depend on plant species, plant taxonomic (or functional) groups and site-specific differences in abiotic and biotic soil properties. Understanding how plant species can influence their rhizosphere, and how other plant species respond to these changes, will greatly enhance our understanding of the functioning and stability of ecosystems.