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Biogeography is the study of the geographical distribution of living and fossil plants and animals as a result of ecological and evolutionary processes. Biogeography analyzes organism-environment relations through change over space and time, and it often includes human-biota interactions. The main questions explored by biogeographers deal with organism patterns to understand the underlying processes. Biogeographers ponder questions such as why is a species present in a given area? Conversely, if a species is not present, then why is it missing from the area? What are the historical and ecological factors that help determine where a species occurs? What are the effects of evolution and plate tectonics? How have humans altered geographic distribution of organisms? The science of biogeography has been revitalized in the past 60 years due to our understanding of plate tectonics, mechanisms limiting distributions, island biogeography theories, and mathematical and technological tools.

Current work in biogeography uses spatial patterns of organisms, past and present, to determine ecological processes. Biogeographers use experimental testing and quantification of biotic interactions. Vegetation dynamics is the primary focus for approximately half of the biogeographic research conducted by U.S. geographers. Other major focuses include ecosystem structure and function, zoogeography, paleoecology, and development of new biogeographic methodology. In particular, mapping and modeling spatial patterns of abundance and distribution of species of plants and animals have greatly advanced with geographic information systems and remote sensing technology.

Development of Biogeography

To better understand the current field of biogeography, it is important to explore the foundations and history of the science. Biogeography is a synthetic study, which is based in part on the subjects of community ecology, geology, systematics, evolutionary biology, and paleontology. The development of the subject of biogeography may be broken into four historical periods.

1600–1850: The Age of Reason

Early studies of organisms’ geographic distributions were focused on descriptive studies with historical explorations. These scientists focused on documenting spatial patterns of organisms, emphasizing on the effects of climate, latitude, and altitude. Comte de Buffon (1707–1788), also known as Georges-Louis Leclerc, determined that distant regions with similar climate and similar-appearing vegetation have different animal species. This is now referred to as Buffon's Law. He is also the author of Histoire Naturelle, a 44-volume natural history encyclopedia. Carl Linnaeus (1707–1778) studied the plants and animals spread from Mount Ararat in Turkey to explore the idea of the biblical flood. As a result of documenting elevational zones of Ararat, he came up with the idea of biomes defined as major ecological communities. In addition, Carl Linnaeus is considered the father of the science of taxonomy, which is the science of classification.

This time period is also known as a great age for exploration. Johann Reinhold Forster (1729–1798) was the naturalist on James Cook's second Pacific voyage in 1778. He advanced biogeography by creating global biotic regions for plants. Forster noted the higher-species diversity in the tropics, as well as species diversity being correlated with island size. Alexander von Humboldt (1769–1859) created a botanical geography that was foundational to the field of biogeography. He determined that plant vegetation types are strongly correlated with local climate to create latitudinal belts of vegetation. Moreover, he developed elevational vegetation zones for the Andes in South America.

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