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The Galápagos Islands: Part 1 - Environmental Setting
BIO 53 Fall 2007
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Geography 13 large islands (>10 km2), 6 smaller islands of 1-2 km2
Many islets, rocks Total land area: ~8,000 km2 (SC: ~77,700 km2) Mainland Ecuador ~960 km to east Costa Rica ~1100 km away
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Geology http://alpha.dickinson.edu/departments/geol/gal_2003.htm
Fernandina
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Cocos Plate Galápagos Pacific Plate Nazca Plate
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The Galápagos Platform
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Hot Spots and Volcanic Island Formation
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Lava flows (basalt)
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Eroding tuff formation
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Uplifted areas may include fossil-bearing (calcareous) rocks
Baltra Island
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Climate of the Galápagos
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Climate patterns
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Climate patterns
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Climate patterns
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The Galápagos Islands: Part 2 – Darwin’s visit
Darwin’s voyage on the H.M.S. Beagle ( )
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Charles Darwin (1809 - 1882) Darwin at age 31
(1840 portrait by Richmond)
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Jean Baptist de Lamarck :
( ) Belief in gradual changes in organisms over long time periods Recognized the environment as an important influence on evolution: Inheritance of acquired characters Published theory in 1809
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Charles Lyell: author of Principles of Geology (1830)
Proponent of uniformitarianism Slow, steady, gradual changes have shaped earth surface Earth at least millions (not thousands) of years old
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Figure 23.1 Darwin and the Voyage of the Beagle (Part 2)
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Sep. 17: Chatham (San Cristobal)
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Arid lowlands and tortoises
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Sep. 23: Charles (Floreana)
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Moist Uplands
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Sep. 29: Albemarle (Isabela)
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Iguanas
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Oct. 8: James (Santiago/San Salvador)
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Moist Uplands
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Other observations Galapagos Dove
25 of 26 land bird species unique to the islands Galapagos Dove
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Finches
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Mockingbirds http://oikos.villanova.edu/Nesomimus/melanotis.html
San Cristóbal Mockingbird Nesomimus melanotis
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Tortoises Saddleback Dome-shaped
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Plants: number of species confined to the islands
James: 38 of 71 Albemarle: 26 of 46 Chatham: 16 of 32 Charles: 29 of 68 in modern terms: high levels of endemism
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