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Definitions
For biogeographical purposes, an insular environment or "island" is any area of habitat suitable for a specific ecosystem, surrounded by an expanse of unsuitable habitat. While this may be a traditional island—a mass of land surrounded by water—the term may also be applied to many nontraditional "islands", such as the peaks of mountains, isolated springs or lakes, and non-contiguous woodlands. The concept is often applied to natural habitats surrounded by human-altered landscapes, such as expanses of grassland surrounded by highways or housing tracts, and national parks. Additionally, what is an insular for one organism may not be so for others, some organisms located on mountaintops may also be found in the valleys, while others may be restricted to the peaks.

Definitions
For biogeographical purposes, an insular environment or "island" is any area of habitat suitable for a specific ecosystem that is surrounded by an expanse of unsuitable habitat. While this may be a traditional island—a land mass surrounded by water—the term may also be applied to many nontraditional "islands", such as the peaks of mountains or island ranges that are separate from larger mountain range chains, isolated springs or lakes, and non-contiguous woodlands. The concept is often applied to natural habitats that have been fragmented due human-altered landscapes, such as grasslands and forests utilized for industrial purposes, and national parks. Additionally, what is an insular for one organism may not be so for others, some organisms located on mountaintops may also be found in the valleys, while others may be restricted to the peaks.

Historical record
The theory can be studied through the fossils, which provide a record of life on Earth. 300 million years ago, Europe and North America lay on the equator and were covered by steamy tropical rainforests. Climate change devastated these tropical rainforests during the Carboniferous Period and as the climate grew drier, rainforests fragmented. Shrunken islands of forest were uninhabitable for amphibians but were well suited to reptiles, which became more diverse and even varied their diet in the rapidly changing environment; this Carboniferous rainforest collapse event triggered an evolutionary burst among reptiles.

Historical record
The theory can be studied through the fossils, which provide a record of life on Earth. 300 million years ago, Europe and North America lay on the equator and were covered by steamy tropical rainforests. Climate change devastated these tropical rainforests during the Carboniferous Period and as the climate grew drier, rainforests fragmented. Shrunken islands of forest were uninhabitable for amphibians but were well suited to reptiles, which became more diverse and even varied their diet in the rapidly changing environment; this Carboniferous rainforest collapse event triggered an evolutionary burst among reptiles, which researchers determined by analyzing two databases of tetrapod diversity.

Research experiments
The theory of island biogeography was experimentally tested by E. O. Wilson and his student Daniel Simberloff in the mangrove islands in the Florida Keys. Species richness on several small mangroves islands were surveyed. The islands were fumigated with methyl bromide to clear their arthropod communities. Following fumigation, the immigration of species onto the islands was monitored. Within a year the islands had been recolonized to pre-fumigation levels. However, Simberloff and Wilson contended this final species richness was oscillating in quasi-equilibrium. Islands closer to the mainland recovered faster as predicted by the Theory of Island Biogeography. The effect of island size was not tested, since all islands were of approximately equal size.

Research conducted at the rainforest research station on Barro Colorado Island has yielded a large number of publications concerning the ecological changes following the formation of islands, such as the local extinction of large predators and the subsequent changes in prey populations.

Research experiments
The theory of island biogeography was experimentally tested by E. O. Wilson and his student Daniel Simberloff in the mangrove islands in the Florida Keys. Species richness on several small mangroves islands were surveyed. The islands were fumigated with methyl bromide to clear their arthropod communities. Following fumigation, the immigration of species onto the islands was monitored. Within a year the islands had been recolonized to pre-fumigation levels. However, Simberloff and Wilson contended this final species richness was oscillating in quasi-equilibrium. Islands closer to the mainland recovered faster as predicted by the Theory of Island Biogeography. The effect of island size was not tested, since all islands were of approximately equal size.

Research conducted at the rainforest research station on Barro Colorado Island has yielded a large number of publications concerning the ecological changes following the formation of islands, such as the local extinction of large predators and the subsequent changes in prey populations.

Recent research demonstrates how during the Anthropocene, it is becoming ever more important to consider how human influences impact island biogeography. For example, a study on how shipping trade between Caribbean islands impacted anole lizard populations found that the economic isolation of human populations played a significant role in increasing the magnitude of the species-area effect and decreasing that of the rescue effect for those islands.