LECTURE 26 CH 23-24 SPECIES DIVERSITY, HISTORY, AND BIOGEOGRAPHY Multiple scales of species diversity Local Regional Latitudinal Continental Global Local-scale: Factors affecting distributions/presence of species Abiotic factors, biological interactions, dispersal limitation, human introduction, chance Equilibrium theory: number of species is a balance of Additions (e.g. immigration and speciation) Subtractions (e.g. emigration and extinctions) E.g. at continental scale: affected by balance of speciation and extinction E.g. Theory of Island Biogeography Number of species at equilibrium results from balance of immigration on regional scale and extinction on local scale Distance from mainland: affects immigration rate so no. species > near than far Island area: affects extinction rate so no. species > large than small islands Applicability to ‘terrestrial habitat’ islands too Regional-scale: Factors affecting patterns species diversity Habitat heterogeneity Suitability of physical conditions Isolation from centers of diversity Effect of regional-scale on local-scale Compare diversities in similar habitats in different regions reveals regional effects Saturation of local communities: test how local and regional diversity relate Variation in local diversity depends on regional diversity Comparisons of tree diversity among regions: effects of loss of habitat during glaciation gains due to building stepping stones for dispersal regions with more species have species in greater ecological range Latitudinal-scale Increase in diversity with decrease in latitude Hypotheses to explain (see earlier lecture) Time Hypotheses: tropics are older; more time to accumulate species But…what happened to species diversity in tropics during glacial era? Continental/global-scale How do history and biogeography influence local communites and species diversity? Diversity has not been constant over geological time Catastrophes have caused major changes in direction of evolution Historical roots affect current species distributions Continental drift Altered positions of continents; some separations; some joining Changed routes of dispersal Land bridges connected land masses Exchanges of biotas possible; affected migration and extinctions Drift separated lineages onto different continents subsequent divergence Result = organisms not distributed uniformly over earth (Phylogenetic effects: traits shared by lineage irrespective of environment e.g. marsupials limited to Australia because of evolution lineage, not env. of Aust.) Zoogeographic regions reflect long-term evolutionary isolation (e.g. 6 regions) Contrast: similar environments among regions has led to convergent evolution Climatic history determines species distributions Glaciations Caused extinctions in Europe because of dispersal barriers; no refuges Species in N.A. behaved individualistically shifts in community composition Miocene cooler/drier in NA major shifts in community and species diversity