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Island biogeography explained

The classic model proposes that immigration tends to add species and local extinction removes them, with island isolation affecting arrival and area affecting persistence. It predicts tendencies and turnover around a dynamic richness, not an exact permanent species list for every island or habitat fragment.

Scope: A worldwide introduction to equilibrium island-biogeography theory and its extensions to oceanic islands and habitat fragments. Area and isolation are central predictors, but habitat diversity, matrix permeability, disturbance, evolutionary history, species traits, and human transport also influence richness and turnover. · Last updated

An aerial view of Anacapa Island's narrow isolated ridges surrounded by the Pacific Ocean.
Image: Anacapa-Island-Aerial by National Park Service · Public domain
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The equilibrium is dynamic

In the classic model, immigration falls as more of the regional species pool arrives, while extinction rises as an island accumulates species with smaller average populations and more interactions. Where the rates cross is an expected richness. Species can continue replacing one another around that value, so equilibrium does not mean ecological stillness or a fixed roster. [1][2]

John Gould's historical plate comparing the differently shaped beaks of four Galápagos finches.
Field frame · Editorial contextA contextual view from Adaptive radiation explained.Image: Darwin's finches by Gould by John Gould · Public domain
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Area and isolation change the odds

Large islands generally offer more habitat and can support larger populations, reducing some extinction risks. Near islands are usually reached by more dispersers than remote ones. The famous species–area and isolation patterns are statistical, however: a small diverse island can exceed a larger uniform one, and strong fliers, windborne spores, rafting reptiles, and human-carried organisms experience distance very differently. [1][3]

Small blue Devils Hole pupfish swimming above pale stones in clear water.
Field frame · Editorial contextA contextual view from What “endemic” means.Image: Joanna Gilkeson / USFWS · Public domain
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Evolution enters on longer timescales

Remote islands may receive few colonists yet generate endemic lineages as populations diverge and diversify. Island age, geological change, climate, and extinction determine how much evolutionary history remains visible. Models that include speciation can better describe oceanic archipelagos, but even those models simplify changing area, connectivity, and environmental conditions through time. [1][2]

Colored spheres illustrating how a small founding sample can shift allele frequencies through genetic drift.
Field frame · Editorial contextA contextual view from Genetic drift and founder effects.Image: Founder effect with drift by Professor marginalia · CC BY-SA 3.0 · Resized and converted to WebP; displayed with a crop.
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Habitat fragments are island-like, not identical

Forest remnants, ponds, and mountaintops can be analyzed as patches surrounded by a contrasting matrix, but that matrix is rarely equivalent to ocean. Some species cross farms or cities; others do not, and edges alter light, wind, predators, and vegetation. Island theory helps frame conservation questions about patch size and connectivity, while local habitat quality and movement data are needed before treating a reserve as a sealed island. [3][4]

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Source-checked editorial guide. Last updated . This guide teaches identification and field skills; it is not a substitute for expert verification when it matters.