Species Area Relationship: Species richness increases with area and decreases with isolation.
Dynamic Immigration-Extinction Balance: Species richness can be modeled as a balance between immigration and extinction.
Latitudinal Patterns: Species richness generally increases from middle and high latitudes toward the equator.
Influence of Historical Processes: Long-term historical and regional influences affect species richness and biodiversity.
Definition: Geographic ecology seeks to map the patterns of plant and animal life.
Focus Areas: Primarily concentrates on island biogeography, latitudinal patterns in species richness, and the influence of historical processes on biodiversity.
Early Contributions: Arrhenius quantitated the relationship between area and species number; a foundation for geographic ecology.
Preston's Findings: Noted that the fewest bird species exist on the smallest islands, while the largest islands host the most species.
Nilsson et al.: Identified island area as a key predictor of species richness among various taxa in Sweden.
Montane Islands: Following warming at the end of the Pleistocene, forests and habitats became fragmented into isolated mountain peaks, impacting both plant and animal distribution.
Lake Islands: Lakes function as islands with species diversity correlating with lake area studied by Tonn and Magnuson, as well as global studies by Barbour and Brown.
MacArthur and Wilson's Findings: Isolation leads to reduced bird diversity on Pacific Islands, with observed increases in diversity with larger island sizes.
Concept Overview: Introduced by MacArthur and Wilson; species diversity reflects a balance between immigration and extinction rates.
Immigration Rates: Highest on new islands; declines as species accumulate.
Extinction Rates: Increase with more species as competition intensifies and species populations diminish.
Prediction of Species Number: Point of intersection of immigration and extinction rates predicts the expected number of species on an island, influenced by both island size and distance from source populations.
Dynamic Composition: Species composition changes over time, known as species turnover; Diamond's studies on California Channel Islands illustrated this.
Simberloff and Wilson: Investigated recolonization patterns on defaunated islands, affirming the dynamic nature of species composition.
General Trend: Species richness increases as one moves from higher latitudes to the equator.
Hypotheses: Six categories of mechanisms explaining this pattern:
Time Since Perturbation: Tropics have older ecosystems with less disturbance, allowing for higher speciation rates.
Productivity: High energy in the tropics supports larger populations and reduces extinction risks.
Environmental Heterogeneity: Increased habitat complexity in the tropics supports diverse species.
Favorable Climatic Conditions: Less temperature variation and physically extreme environments in the tropics support greater biodiversity.
Niche Breadths and Interactions: Tropical species may be more limited by biological factors than physical.
Speciation and Extinction Rates: The tropics experience higher rates of speciation and lower extinction rates compared to higher latitudes.
Regional Area Influence: Larger land areas in the tropics allow for more habitat diversity, which supports greater species richness.
Exceptional Patterns: Variance in species richness that cannot simply be explained by area, illustrated by the Cape region of South Africa having more species than larger areas like California.
Historic Factors: Influences such as continental drift and climate changes have historically shaped biodiversity in regions.
Comparative Biogeographic Studies: The unique historical processes in different temperate regions lead to varying levels of biodiversity despite similar areas.
A comprehensive overview focuses on island biogeography, latitudinal species richness patterns, and historical influences affecting biodiversity, including practical applications in geographic information systems (GIS).