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Paleobiogeography Biogeography (ENVR333) Fall 2007 5 October 2006
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PaleoBiogeography Time Scale Theory of Continental Drift and Plate Tectonics The Breakup of Pangea Biogeographic Implications of a Dynamic Geography
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Geologic Time Scale (Fig 7.1 MacDonald 2003)
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Theory of Continental Drift Alfred Wegener (1880-1930) 1915 The Origin of Continents and Oceans Pangea = supercontinent
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Evidence for Continental Drift Matching shapes Similar rock types and structures Continuity of plant and animal fossils Glacial deposits
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Plate Tectonics Fig 7.5 MacDonald 2003)
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Plate Tectonics
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Pangea 200 million km 2 or 40% of earth’s surface connectivity
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Break up of Pangea Laurasia Gondwanaland Tethyan Seaway
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Break up of Pangea
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Cenozoic Changes India rafts into Asia (45 mya) Africa and Europe rejoin (17 mya) Stepping Stone Islands created (15 mya) Central American Landbridge (6mya) Epicontinental seas disappear
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http://www.clearlight.com/%7Emhieb/WVFossils/continents.html
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Biogeographic Implications Speciation
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Biogeographic Implications Corridors and Barriers Great American Interchange
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Biogeographic Implications Corridors and Barriers 12,000 ybp today Beringia
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Biogeographic Implications Marine-Climate effects
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