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PALEOZOIC Ch 10 & 11
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AGENDA Geologic Time (7 Periods) Plate Tectonics – “Driving Force”
Geography/Landforms Mountains, Rock Formations Appalachian Mountains Climate Change Sea Level Changes Ice Ages Animal/Plant Evolution Animal/Plant Extinction
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Geologic Time
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Plate Tectonics
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Geological Supercontinents
Vaalbara: Oldest, Formed 3.6 bya Ur: Formed 3.0 bya Nena: Formed 1.8 bya Kenorland: Formed 2.7 bya Columbia: Formed 2.1 bya Rodinia: Formed 1.1 bya Pannotia: Formed 0.6 bya, broke up 0.54 bya Pangea: Formed bya
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Rodinia Breakup Rodinia Breakup (Neoproterozoic) producing 6 large continents: Laurentia (N. America, Greenland, NW Ireland & Scotland) Baltica (Russia & N. Europe) Kazakhstania (Bet. Caspian Sea & China) Siberia (Russia) China (China, Indochina, & Malay) Gondwana (S. America, Africa, India, Australia, & Antarctica) Movements/interactions of these continents responsible for creation of landforms and evolution of lifeforms.
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NEOPROTEROZOIC Laurentia (N. America, Greenland, NW Ireland & Scotland) Baltica (Russia & N. Europe) Kazakhstania (Bet. Caspian Sea & China) Siberia (Russia) China (China, Indochina, & Malay) Gondwana (S. America, Africa, India, Australia, & Antarctica)
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CAMBRIAN f10_04_pg271 f10_04_pg271.jpg f10_04_pg271
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ORDOVICIAN f10_25_pg287 f10_25_pg287.jpg f10_25_pg287
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SILURIAN f10_28_pg289 f10_28_pg289.jpg f10_28_pg289
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DEVONIAN f11_04_pg299 f11_04_pg299.jpg f11_04_pg299
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MISSISSIPPIAN f11_08_pg302 f11_08_pg302.jpg f11_08_pg302
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Mississippian/Pennsylvanian Periods
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PENNSYLVANIAN f11_10_pg304 f11_10_pg304.jpg f11_10_pg304
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PERMIAN f11_17_pg307 f11_17_pg307.jpg f11_17_pg307
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Consequence of Plate Tectonics
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Mountain Building Episodes
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Review Craton: The stable interior of a continent.
2 components of a Craton: Shield: Large area of exposed crystalline rocks. Platforms: Areas surrounding the shields containing flat-lying sedimentary layers.
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Four Orogenic Belts West – Cordilleran North – Franklinian
Northeast – Caledonian/Acadian East - Appalachian
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Mountain Building (Orogenic) Episodes
Break-up of Rodinia (Proterozoic) 7 Continents Iapetus Ocean Formation (Cambrian) Taconic Orogeny (Ordovician) Iapetus Ocean Narrowing, 1st Appalachian Episode Cordilleran Orogeny (Ordovician – Silurian) Rocky Mtns Caledonian Orogeny (Mid Sil. Mid Dev.) Laurasia Formed (N. America/Europe) Acadian (Mid Sil. Mid Dev.) Closing of Iapetus Ocean, 2nd Appalachian Episode Alleghenian Orogeny (MS – Perm) Final Appalachian Episode Ouachita Orogeny (Early Dev – Late MS)
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Appalachian Mountains
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U.S. PHYSIOGRAPHIC REGIONS
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United States Physiographic Regions
Physiographic regions are based on landscape features, which are mostly controlled by the geology of the regions.
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Alabama Physiographic Regions
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Sea Level Changes Epicontinental Seas “Transgressive/Regressive Sequences”
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Transgressive/Regressive Sequences
Sauk (Cambrian – Ordovician) Tippecanoe (Ordovician – Silurian) Kaskaskia (Silurian – Mississippian) Absaroka (Pennsylvanian – Triassic)
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Causes of Sea Level Changes
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Evidence of Sea Level Changes
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Paleozoic Summary
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THE END
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