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Study of distribution of organisms
Biogeography Study of distribution of organisms
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Biogeography Comparative observational science Experiments – limited utility Multiple scales Comparative has uses, though Synthetic science
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Subjects Used in Biogeography
Anatomy Physiology Taxonomy Developmental Evolution Geology Geography Ecology Climatology, Paleontology……
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Relevance of Biogeography
What enables a species to live where it doe, and what prevents it from colonizing other areas? What are a species closest relatives and where can they be found? Where did its ancestors live? How have historical events shaped a species’ distribution?
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Overarching question: What shapes global patterns of biodiversity?
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The Importance of Time Historical biogeography Ecological biogeography Paleoecology
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“While the process of science owes much to admirable human traits……
“While the process of science owes much to admirable human traits……..it is also retarded by characteristics such as prejudice, jealousy, short-sightedness, and stupidity.”
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History of Biogeography
Roots from questions that developed during the “Age of Exploration” Shares common lineage with ecology Early questions From where did life come? How did it diversify across the planet?
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Persistent Themes in Biogeography
Classifying geographic regions based on their biota Reconstructing historical development or lineages and biota, including their origin, spread, and diversification Explaining differences in numbers and types of species among geographic areas, and along geographic gradients Explaining geographic variation in characteristics of individuals and populations of closely related species
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Age of Exploration 250 yr ago, only 1% of species known today identified Mission – reveal mysteries of creation by learning of the diversity of life Prevailing view – stasis With increasing identification of species, was a clear need for organization
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Carolus Linneaus (1707 – 1778) Understanding organization would lead to knowing Creator’s plan Took static view of Earth Explain origin and spread of life Challenge was to explain diversity and distribution
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Carolus Linneaus (1707 – 1778) How could life have spread from Paradise then landing spot of the Ark Linnaeus – “Paradisical Mountain” – a mountain island life along the slopes, perfectly adapted for biotic and abiotic conditions at their “station” Based on known conditions of tropical mountains Later formation of land allowed spread
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Comte de Buffon (1707 – 1788) Contemporary of Linaeus
Disagreed with his view of spread of life (living and fossil specimens) Places with same climate had different species Inhospitable environment around Mount Ararat Proposed origin in northern Europe
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Buffon’s hypothesis – climate was cooler at time allowing species to move to new areas and change
Key points – climate and species were dynamic (central to modern biogeographic theory and precursor to development of evolutionary theory)
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Comte de Buffon (1707 – 1788) Buffon’s Law – Environmentally similar but separated regions have different species of birds and mammals Considered first principle of biogeography Later studies by Joseph Banks and Johann Forster found Buffon’s Law applied to plants
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Phytogeography End of 18th century – natural theology still primary biological theory Willdenow ( ) and Humboldt ( ) – phytogeography – geographic distribution of plants Studies of plant distribution on Andes mountain (5,600 m elevation Mt. Chimbaruzo
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Phytogeography Identified floristic belts from tropical to arctic
Observed plant communities closely associated with local climate Hints at competition (Candolle) Mt. Chimbaruzo
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Biogeography of 19th Century
First three themes established Classifying geographic regions based on their biota Reconstructing historical development or lineages and biota, including their origin, spread, and diversification Explaining differences in numbers and types of species among geographic areas, and along geographic gradients
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Biogeography of 19th Century
Buffon’s Law Early biogeographers tested Classify regions based on biota (theme 1) Reconstructing origin and spread of life (theme 2) Changes along gradients (theme 3) Established approachs still used Perception of static earth and life to dynamic
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WHY?????? Number of local species increased with area
Limitations Number of local species increased with area Number of species decreased from equator Needed to move to next step (rigorous testing) but first needed WHY??????
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Needs for Better Understanding
Better estimate of age of Earth (natural theology and 6,000 yr) Understanding of dynamic nature of continents and oceans Understanding of spread and diversification – dispersal, vicariance, extinction, evolution)
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Early Advances of 19th Century
Borngniart – father of paleobotany Lyell – father of geology Both used fossil record to conclude climate changes over time (life forms of tropical climates in northern Europe Lyell – changes in sea level and the lifting and erosion of mountains; extinction New species arose through new creations after extinctions; new species created for new climate
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Early Advances of 19th Century
Lyell proposed uniformitarianism Also, realization that processes occur slowly (gradualism) Time needed for geological processes + continual replacement of biota = Earth much older than 6,000 years
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Four British Scientists
Charles Darwin, Joseph Hooker, Philip Sclater, Alfred Russell Wallace Naturalists, traveling the world and discovering diversity Shared their observations, building a broader image of life Did not agree on all points
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Darwin Origin of Species – contribution is obvious Proposed ideas on dispersal of life (countering Agassiz’s view of point near creation) The “dispersalist” view made dispersal dynamic Disagreement then moved to mechanisms of dispersal (dispersalists vs. extensionists)
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Extensionists & Land Bridges
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Further Contributions
Hooker – study of southern hemisphere plant distributions lead to development of vicariance biogeography Sclater – used distribution of passerine (perching) birds to develop a system of six biogeographic regions still used today Also developed zones based on marine mammals (Fig. 2.8)
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Wallace Greatest contributions to biogeography (father of zoogeography) Expanded view provided by Sclater’s zones Established many of the basic principles of biogeography (see Box 2.1) Observed a distinct change in fauna of Southeast Asia and Australasia (Wallace Line)
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Other 19th Century Contributions
Bergmann’s rule – homeotherms, body size, and surface-to-volume ratio from poles Allen’s rule – limbs of birds and mammals become shorter and stouter as move from equator. Cope’s rule – groups tend to increase in size during their evolution Limitation of generalities but open new thoughts Cope’s tend to go to extinction but replaced by taxa that begin to increase
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Other 19th Century Contributions
Merriam’s life zones Study of elevational changes – found vegetation types and species composition are similar to longitudinal patterns Confirmed Humboldt’s work Cope’s tend to go to extinction but replaced by taxa that begin to increase
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Burdgeoning info from paleontology
Twentieth Century Burdgeoning info from paleontology Origin, dispersal, radiation, and decline of terrestrial vertebrates Development of phylogenies New groups rise Increase in number of species Radiate to fill niches and expand range Still – question of how dispersed Cope’s tend to go to extinction but replaced by taxa that begin to increase
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Patterns of morphological variation Coincided with Modern Synthesis
Twentieth Century Relationships between geological and ecological properties of environment Patterns of morphological variation Coincided with Modern Synthesis Linking lead to formulation of biological species concept (Ernst Mayr) Also identified allopatric speciation Cope’s tend to go to extinction but replaced by taxa that begin to increase
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Earth’s crust believed fixed until 1960s
Continental Drift Earth’s crust believed fixed until 1960s Continental drift 1st proposed 1858 Resurfaced by Wegener and Taylor using geological and ecological evidence Criticized and denied until evidence became overwhelming Changed dispersal from land bridges to movements of continents Cope’s tend to go to extinction but replaced by taxa that begin to increase
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New Phylogenetic Methods
Continental drift lead to study of disjunctions Vicariance biogeography Examination and revision of phylogenies Cope’s tend to go to extinction but replaced by taxa that begin to increase
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Geographic information systems Geostatistics
Further Aids Computers Geographic information systems Geostatistics Cope’s tend to go to extinction but replaced by taxa that begin to increase
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