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THE DEVONIAN Life in the Devonian Sponges with glass skeleton Hydnoceras left Hindia above
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THE DEVONIAN Life in the Devonian Sponges and tabulate coral reefs
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THE DEVONIAN Life in the Devonian Devonian corals Rugose Corals Petoskey Stone Tabulate coral State fossil of Michigan
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THE DEVONIAN Life in the Devonian Spiriferid brachiopods
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THE DEVONIAN Life in the Devonian Goniatite cephalopods Suture pattern more complex than Nautiloid
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THE DEVONIAN Life in the Devonian Fish Placoderms expanded rapidly in Devonian Dunkleosteus Arthrodires - carnivorous
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THE DEVONIAN Life in the Devonian Fish Placoderms expanded rapidly in Devonian Antiarchs – mud-grubbers Pterichthyoides above Bothriolepis right
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THE DEVONIAN Life in the Devonian Fish Chondrichthyan fish – cartilagenous fish Cladoselache
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THE DEVONIAN Life in the Devonian Fish Osteichthyan fish – bony or ray-finned fish Cheirolepis
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THE DEVONIAN Life in the Devonian Fish Osteichthyan fish – lobe-finned fish Led to tetrapods Dipterus
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THE DEVONIAN Life in the Devonian Eurypterids Eurypterus remipes
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THE DEVONIAN Life in the Devonian Plants Aglaophyton left Rhynia center Horneophyton right
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THE DEVONIAN Life in the Devonian Plants Lycopsids Pteridophytes (seed ferns) Sphenopsids (Calamites)
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THE DEVONIAN Life in the Devonian Plants
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THE DEVONIAN Life in the Devonian Plants
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THE MISSISSIPPIAN The Age of Crinoids Mississippian named by Alexander Winchell in 1870 Named for carbonate rocks deposited in the Upper Mississippi River valley Lower Carboniferous in Europe and Canada
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THE MISSISSIPPIAN
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The Age of Crinoids Acadia highlands reduced Decrease in muddy sediments Paleozoic flooding by epeiric seas
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THE MISSISSIPPIAN The Age of Crinoids
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THE MISSISSIPPIAN Mississippian Tectonics
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THE MISSISSIPPIAN Mississippian Tectonics
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THE MISSISSIPPIAN The Age of Crinoids Acadia highlands reduced Decrease in muddy sediments Paleozoic flooding by epeiric seas
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THE MISSISSIPPIAN The Age of Crinoids Crinoids abundant Ooids abundant Clear, shallow marine water Salinity higher than normal Mississippian Lime Bank
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THE MISSISSIPPIAN The Age of Crinoids Late Mississippian the Kaskaskia sea retreated
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THE MISSISSIPPIAN The Age of Crinoids Late Mississippian the Kaskaskia sea retreated Detrital muds and limestones formed. Petroleum reservoirs Nonmarine shales and sandstones from erosion of Acadian highlands
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THE MISSISSIPPIAN The Age of Crinoids Erosion of Acadian highland produced Pocono Ss. Forms resistant ridges of the Pocono Mtns. Forms third clastic wedge
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THE MISSISSIPPIAN The Age of Crinoids Erosion of Acadian highland produced Pocono Ss.
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THE MISSISSIPPIAN The Age of Crinoids Life in the Mississippian Rugose corals common
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THE MISSISSIPPIAN The Age of Crinoids Life in the Mississippian Archimedes common bryozoan
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THE MISSISSIPPIAN The Age of Crinoids Life in the Mississippian Bivalves uncommon Goniatite cephalopods Graptolites go extinct
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THE MISSISSIPPIAN The Age of Crinoids Life in the Mississippian Crinoids abundant
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THE MISSISSIPPIAN The Age of Crinoids Life in the Mississippian Insects become abundant Forests include Seed ferns (Pteridospermae) Lycopsids Sphenopsids
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THE PENNSYLVANIAN The Age of Coal Swamps Pennsylvanian named by Henry S. Williams in 1891 Named for coal-bearing rocks deposited in Pennsylvanian Upper Carboniferous in Europe and Canada
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THE PENNSYLVANIAN
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The Age of Coal Swamps
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THE PENNSYLVANIAN Orogenic Events Hercynian Orogeny
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THE PENNSYLVANIAN Orogenic Events Alleghenian Orogeny
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THE PENNSYLVANIAN The Age of Coal Swamps Alleghenian Orogeny
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THE PENNSYLVANIAN Orogenic Events Alleghenian Orogeny Begins formation of Pangaea Laurentia and Baltica collide to form LAURASIA Laurasia and Gondwana collide to form PANGAEA
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THE PENNSYLVANIAN Orogenic Events Alleghenian Orogeny
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THE PENNSYLVANIAN Orogenic Events Alleghenian Orogeny
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