Plant diversity, biogeography and environment in Iberia: Patterns and possible causal factors
Article first published online: 24 FEB 2009
2002 IAVS - the International Association of Vegetation Science
Journal of Vegetation Science
Volume 13, Issue 2, pages 245–258, April 2002
How to Cite
Benayas, R., José, M. and Scheiner, S. M. (2002), Plant diversity, biogeography and environment in Iberia: Patterns and possible causal factors. Journal of Vegetation Science, 13: 245–258. doi: 10.1111/j.1654-1103.2002.tb02045.x
- Issue published online: 24 FEB 2009
- Article first published online: 24 FEB 2009
- Received 23 November 2000; Revision received 27 July 2001; Accepted 21 February 2002.
- Available energy;
- Community type;
- Environmental heterogeneity;
- Global change;
- Mosaic diversity;
- Soil type;
- Species richness;
- Transition zone
Abstract. We associated patterns of plant diversity with possible causal factors by considering 93 local regions in the Iberian Peninsula and Balearic Islands with respect to biogeography, environmental favourability, and environmental heterogeneity, and their relationship with measured species diversity at four different scales: mean local species richness standardized at a grain of 100 m2, total species richness in a community type within a region (regional community richness), mean compositional similarity, and mosaic diversity.
Local regions in biogeographic transition zones to the North African and Atlantic floras had higher regional community richness and greater mosaic diversity than did non-transitional regions, whereas no differences existed in mean local species richness or mean compositional similarity. Mean local species richness was positively related to environmental favourability as measured by actual evapotranspiration, but negatively related to total precipitation and temporal heterogeneity in precipitation. Mean local species richness was greatest in annual grassland and dwarf shrubland communities, and on calcareous bedrock types. Regional community richness was similarly related to actual evapotranspiration and total precipitation, but in addition was positively related to spatial heterogeneity in topography and soil water holding capacity. Mean compositional similarity decreased with increasing spatial heterogeneity and temperature seasonality. Mosaic diversity, a measure of complexity, increased with increasing local and regional richness.
We hypothesize that these relationships can be explained by four ecological and evolutionary classes of causal factors: numbers of individuals, intermediate environments, limits to adaptation, and niche variation. These factors operate at various scales and manifest themselves in various ways. For example, at the site level, apparently processes that increase the number of individuals increase mean local species richness, but at the level of the entire region no such effects were found.