Week 9 lecture 1 Biogeography and Island Species Richness - General Biology
Terms in this set (20)
Biogeography is the study of ecological structure and processes at large geographic scales, focusing on species composition and diversity across different locations.
Species richness generally increases with increasing area sampled, often demonstrated by island studies.
Islands can include mountain ranges, plateaus, isolated lakes, and habitat fragments created by humans, all acting as isolated habitats.
Because species richness and area data are often non-linear, log transformations help linearize the relationship for analysis.
Islands tend to have a steeper slope in species richness vs. area, indicating higher species richness per area compared to mainland.
Developed by MacArthur and Wilson, it explains island species richness as a balance between immigration rates and extinction rates.
Islands closer to the mainland have higher immigration rates because species can disperse more easily.
Larger islands have lower extinction rates due to greater resource availability and niche partitioning.
Immigration rates decrease as the number of species present increases, due to fewer new species available to colonize.
An island that is near and large is predicted to have the highest species richness due to high immigration and low extinction rates.
It was a test of the equilibrium theory where bird species recolonized Krakatau island after a volcanic eruption, matching predicted species richness.
They showed that near islands regained insect species faster than far islands after fumigation, supporting the theory that proximity affects immigration rates.
Primary producers and smaller organisms tend to have lower extinction rates, while higher trophic level species and those with mutualistic partners have higher extinction rates.
Good dispersers like birds and wind-dispersed plants have higher immigration rates, while amphibians and freshwater fish have lower immigration rates.
Oceanic islands form as continental islands (land breaking from continents) or volcanic islands (new land from volcanic activity).
Continental islands start with species already present, while volcanic islands rely solely on immigration to gain species.
Islands can form from sediment accumulation (e.g., coral or mangrove barriers), landslides, or erosion creating isolated lakes or mountain tops.
Regional processes, geographic history, and temporal changes affect species richness beyond just distance and island size.
Species turnover is the rate at which species are replaced on an island, reflecting ongoing immigration and extinction dynamics.
Habitat fragmentation creates isolated patches that function as 'islands', affecting species richness through altered immigration and extinction rates.