Island biogeography theory explains species diversity on islands through immigration and extinction rates. It considers island size, distance from mainland, and habitat diversity to predict species richness and turnover.
The theory, developed by MacArthur and Wilson in the 1960s, revolutionized ecology. It applies to both actual islands and habitat fragments, influencing conservation strategies and our understanding of biodiversity patterns in isolated ecosystems.
Origins of the theory
Theory of Island Biogeography emerged as a fundamental concept in ecology and biogeography, providing insights into species distribution patterns on islands
Developed in the 1960s, this theory revolutionized understanding of ecological processes and biodiversity dynamics in isolated ecosystems
Applies to both literal islands and habitat islands, influencing conservation strategies and ecosystem management worldwide
MacArthur and Wilson's contribution
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Robert MacArthur and E.O. Wilson jointly formulated the theory in 1963, publishing their seminal work "The Theory of Island Biogeography" in 1967
Proposed a mathematical model explaining species richness on islands as a dynamic equilibrium between immigration and extinction rates
Introduced the concept of species turnover, challenging the prevailing notion of static island ecosystems
Emphasized the importance of island size and distance from mainland in determining species diversity
Historical context
Built upon earlier biogeographical observations, including those of Charles Darwin and Alfred Russel Wallace
Addressed limitations of existing equilibrium theories in ecology, which failed to explain species diversity patterns on islands
Emerged during a period of rapid advancement in ecological research and quantitative modeling techniques
Influenced by developments in population genetics and evolutionary biology, incorporating principles of species adaptation and colonization
Key principles
Theory of Island Biogeography explains biodiversity patterns on islands through a balance of colonization and extinction processes
Emphasizes the dynamic nature of island ecosystems, with species composition constantly changing over time
Provides a framework for predicting species richness based on island characteristics and geographical context
Species equilibrium
Postulates that islands reach a dynamic equilibrium in species number over time
Equilibrium occurs when immigration rate of new species equals extinction rate of existing species
Species composition may change while total number remains relatively stable
Equilibrium point varies depending on island size, distance from mainland, and other ecological factors
Immigration vs extinction rates
Immigration rate decreases as more species colonize an island due to fewer available niches
Extinction rate increases with more species present due to increased competition and limited resources
Curves of immigration and extinction rates intersect at the equilibrium point
Factors affecting these rates include island area, isolation, habitat diversity, and species characteristics
Island size effect
Larger islands support more species due to greater habitat diversity and resource availability
Increased area reduces extinction risk by providing larger populations and more refugia
Supports MacArthur and Wilson's species-area relationship, expressed as S = cA^z (where S is species number, A is area, c is a constant, and z is the slope)
Larger islands also have higher immigration rates due to larger "target" area for dispersing organisms
Distance from mainland
Islands closer to mainland or source populations have higher immigration rates
Distant islands experience lower colonization rates due to dispersal limitations
Isolation affects species composition, favoring good dispersers on remote islands
Distance influences the time lag for species to reach equilibrium after disturbances
Mathematical model
Theory of Island Biogeography employs a mathematical framework to quantify and predict species richness on islands
Model incorporates key variables such as island size, distance from mainland, and rates of immigration and extinction
Provides a basis for empirical testing and refinement of the theory across various island systems
Equation components
Species richness (S) at equilibrium expressed as a function of immigration (I) and extinction (E) rates
Immigration rate (I) decreases with increasing species richness and distance from mainland
Extinction rate (E) increases with species richness and decreases with island area
General form of the equation: dS/dt = I(t) - E(t), where dS/dt represents the rate of change in species number
Equilibrium reached when dS/dt = 0, or I(t) = E(t)
Graphical representation
Model typically depicted using a graph with species number on the x-axis and rates on the y-axis
Immigration curve slopes downward from left to right, representing decreasing colonization as species accumulate
Extinction curve slopes upward from left to right, showing increasing extinctions with more species present
Intersection of immigration and extinction curves indicates the equilibrium point
Multiple curves can be plotted to compare islands of different sizes or distances from mainland
Factors influencing colonization
Colonization processes play a crucial role in shaping island biodiversity and species composition
Various biotic and abiotic factors affect the ability of species to reach and establish on islands
Understanding these factors helps explain observed patterns of species distribution and predict future changes
Species dispersal abilities
Organisms with efficient dispersal mechanisms (wind-dispersed seeds, strong flyers) more likely to colonize distant islands
Adaptations for long-distance dispersal (coconuts, floating seeds) enhance colonization success in marine environments
Variation in dispersal abilities leads to disharmonic island biotas, with over-representation of good dispersers
Some taxa develop reduced dispersal abilities over time on islands (flightless birds, large-seeded plants)
Ocean currents and wind patterns
Prevailing ocean currents influence the direction and frequency of species arrivals on islands
Wind patterns affect dispersal of airborne organisms and propagules (spores, seeds, small insects)
Seasonal variations in currents and winds can create temporal windows for colonization
Extreme weather events (hurricanes, storms) may facilitate long-distance dispersal of organisms
Stepping stone islands
Intermediate islands between source and target islands facilitate colonization of distant areas
Allow for gradual range expansion and genetic exchange between populations
Reduce effective isolation, increasing immigration rates to more distant islands
Important for conservation planning, particularly in designing marine protected area networks
Factors affecting extinction
Extinction processes on islands are influenced by various ecological and environmental factors
Understanding these factors is crucial for predicting species persistence and implementing effective conservation strategies
Island characteristics and species interactions play key roles in determining extinction rates
Resource availability
Limited resources on islands increase competition and vulnerability to extinction
Fluctuations in resource abundance (seasonal changes, El Niño events) can lead to population crashes
Specialized species more susceptible to extinction due to narrow resource requirements
Human activities often reduce resource availability, exacerbating extinction risks (habitat destruction, overharvesting)
Habitat diversity
Greater habitat diversity supports more species and reduces extinction risk
Islands with varied topography and microclimates provide more niches and refugia
Habitat diversity buffers against environmental fluctuations and disturbances
Loss of key habitats (wetlands, native forests) can trigger cascading extinctions
Interspecific competition
Increased species richness leads to higher competition for limited resources
Competitive exclusion may cause extinctions, particularly among ecologically similar species
Introduced species often outcompete native island species, lacking coevolutionary history
Competition intensity varies with island size, with stronger effects on smaller islands
Island characteristics
Physical and ecological attributes of islands significantly influence their biodiversity patterns
Island biogeography theory considers these characteristics to explain and predict species richness
Understanding island features helps in comparing and categorizing different island ecosystems
Area vs species richness
Positive correlation between island area and species richness, known as the species-area relationship
Larger islands support more species due to increased habitat diversity and reduced extinction risk
Relationship often expressed as power function: S = cA^z, where S is species number and A is area
z-value (slope) typically ranges from 0.2 to 0.35, varying with taxonomic group and island type
Habitat heterogeneity
Islands with diverse habitats support more species due to niche partitioning
Topographic complexity (mountains, valleys) creates varied microclimates and soil conditions
Habitat diversity often correlates with island area but can vary independently
Heterogeneous habitats provide refugia during environmental fluctuations, reducing extinction risk
Isolation effects
More isolated islands have lower immigration rates and often support fewer species
Isolation promotes endemism through adaptive radiation and reduced gene flow
Remote islands often have disharmonic biotas, lacking certain taxonomic groups
Isolation effects can be modified by factors like ocean currents, wind patterns, and human-mediated dispersal
Applications in conservation
Theory of Island Biogeography provides valuable insights for conservation planning and management
Principles applied to both literal islands and fragmented terrestrial habitats
Informs strategies for preserving biodiversity and mitigating impacts of habitat loss
Marine protected areas
Design of marine reserves incorporates island biogeography principles to maximize biodiversity protection
Size and spacing of protected areas influence species persistence and recolonization rates
Network design considers connectivity through larval dispersal and adult movement
Larger reserves support more species and provide better protection against local extinctions
Habitat fragmentation
Fragmented landscapes viewed as habitat islands within a matrix of unsuitable area
Species-area relationship applied to predict biodiversity loss in fragmented habitats
Edge effects and isolation increase extinction risk in small fragments
Conservation strategies focus on preserving large, contiguous habitat patches where possible
Corridor design
Wildlife corridors connect isolated habitat patches, facilitating species movement and gene flow
Corridor width and quality influence their effectiveness as dispersal routes
Stepping-stone habitats can function as corridors for some species
Corridor networks aim to reduce effective isolation and maintain metapopulation dynamics
Criticisms and limitations
Theory of Island Biogeography, while influential, has faced various criticisms and identified limitations
Ongoing research addresses these concerns and refines the theory's applications
Understanding limitations is crucial for appropriate use of the theory in research and conservation
Oversimplification concerns
Model assumes all species are ecologically equivalent, ignoring functional differences
Does not account for species interactions beyond simple competition
Neglects historical factors and evolutionary processes in shaping island biotas
Simplifies complex ecological dynamics into a few parameters (immigration, extinction rates)
Non-equilibrium scenarios
Some island systems may not reach equilibrium due to frequent disturbances or ongoing environmental changes
Theory less applicable to recently formed islands or those undergoing rapid ecological transitions
Difficulty in determining if observed patterns represent true equilibrium or transient states
Non-equilibrium dynamics may be more common than originally assumed, especially in human-impacted systems
Human impact considerations
Original theory did not explicitly account for human-induced changes to island ecosystems