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Earth History GEOL 2110 The Paleozoic Era
Part 4A: The Silurian and Devonian Periods Time of Fish, Amphibians and Forests
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Major Concepts Biodiversity on the seafloor continued in Silurian and Devonian times. Ammonites replaced Nautiloids; Bony fish diversified to skeletal fish. Land began to be populated with burrowing animals, spiders, scorpians and later amphibians Spore-bearing vascular plants took root in the form of club moss, ferns, horsetails and seed ferns. The proliferation of coral reefs caused restricted basins wherein great thickness of limestone and evaporites were deposited.
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Silurian – Devonian Major Events
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Marine Biodiversity Recovers from Ordovician Extinction
Trilobites get big and defensive 1’ Spirifer Brachiopods Thick-walled, “winged” Brachs
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Marine Biodiversity Recovers from Ordovician Extinction
Coiled Ammonoid Cephalopods Replace Straight Nautiloids
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The Age of Fishes Jawed Spiny Acanthodians
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Invasion of the Land Vascular Plants take Root
Lycopsids (Club Moss) Rhynia – leaf-less tubes Sphenopsids (Horsetail) Psilophyton –Rooted , strong bundled stalks
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Invasion of the Land Late Devonian – Seeded Plants and Trees
Plants colonize the land! Late Devonian Seed Fern Stumps, Catskill Mtns, NY Modern-day spore tree fern as existed in the Late Devonian Fossilized Seeds from a Seed Fern
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Invasion of the Land Vascular Plants take Root
Plants colonize the land! Invasion of the Land Vascular Plants take Root
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Invasion of the Land Bugs and Slimy Creatures Follow
Plants colonize the land! Devonian centipede claw and head Devonian compound insect eye Millipede fossil
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Invasion of the Land Bugs and Slimy Creatures Follow
Plants colonize the land! Invasion of the Land Bugs and Slimy Creatures Follow
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Proliferation of Reefs
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Silurian-Devonian Coral Reefs
Huge reefs in the Silurian and Devonian, made of: Tabulate Chain Coral Sponges Rugose Corals Heliophyllum Hexagoneria
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Silurian-Devonian Coral Reefs
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Ecological Zonation of Coral Reefs
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Reef Facies Devonian Reef Complex, W. Australia
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Modern-day Reef Environment
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Silurian Reef Thorton Quarry, South of Chicago
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Late Devonian Extinction Another Cool Down?
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Part 4b: Stratigraphy and Tectonics of Silurian and Devonian Periods
Next Lecture The Paleozoic Era Part 4b: Stratigraphy and Tectonics of Silurian and Devonian Periods
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