The Early Paleozoic

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The Early Paleozoic

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Title: The Early Paleozoic


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The Paleozoic
  • (544-250 million years)

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Initial formation of the Appalachian Mountains
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Early Paleozoic PaleogeographyWarm shallow seas
over central part of North American
continentThe Taconian Orogeny has resulted in
the formation of the ancestral Appalachian
Mountains
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By middle Paleozoic timethe Appalachian
Mountains have experienced another episode of
uplift, the Acadian OrogenyThe Antler Orogeny
has resulted in uplift of the western part of the
continent
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Early Paleozoic LifeSponges, bryzoans, tabulate
corals, brachiopods, and trilobites thrived in
warm shallow seas. Graptolites dominate the
surface waters.
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Phylum Cnidaria (Corals)
  • Organization of cells into primitive tissue
  • Cells that secret enzymes for digestion
  • Nerve sensory cells (cnidoblasts)
  • Mobility
  • Free-swimming larvae
  • Sexual and asexual reporduction
  • Colonial and solitary
  • Tabulate and Rugose

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Phylum Bryzoa (moss animals)
  • U-shaped digestive system
  • Primitive muscles
  • Circulatory and nervous system

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Phylum Arthropoda
  • 3/4 of all living organisms-includes insects,
    spiders, crabs, etc.
  • Jointed appendages, segmented bodies, chitonous
    exoskeleton, sensory organs
  • Fly, crawl, swim
  • The trilobites and Eurypterids-cominated early
    Paleozoic seas

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Eurypterids
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Phylum Brachiopoda
  • Bivalves with bilateral symmetry
  • Complex digestive system, circulatory system, and
    nervous system

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Brachiopods - first organisms with internal
skeletal elements
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Graptolites
  • Planktonic
  • Black shales
  • Index fossil for early Paleozoic

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Late PaleozoicRugose corals, bryzoans,
brachiopods and mollusks dominate the sea floor
benthic community while fish become dominant in
the pelagic realm
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Mississippian Paleogeography
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Solitary Rugose corals
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Phylum Mullusca
  • Gastropods (snails)
  • Bivalves (clams and oysters)
  • Cephalopods (squid, octopi, nautiloids)

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Cephalopods (squid, octopi, nautiloids)First
true pelagic organisms with eyes, jaws and
tentacles-adapted for hunting
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Coiled Cephalopods
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Crinoids - were abundant during the late
Paleozoic and typically comprise the main
component of Late Paleozoic limestones (crinoidal
limestones)
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Evolution Gone Wild
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Pennslvanian Coal Forests (Gymnosperms- plants
with cones)
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West Texas Permian Reefs
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Evolution of Fish, Reptilesand Amphibians
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Permian Reptiles (amniotic egg, cold-blooded)
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The Great Permian Extenction
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The Mesozoic
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The TriassicA time of Mountain building
(orogeny)in the western U.S
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The Sonoma Orogeny
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The Sevier Orogeny (Nevada and Utah)Imbricated
Thrust Faults -crustal shortning, melanges
(jumble) and decollement (unsticking).
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Triassic Conifers(The petrified forest of
Arizona)
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Triassic reptiles in conifer/cycad forest
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Jurassic Dinosaurs
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Seismosaurus and flying Pterosaurs
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Jurassic bird Archaeopteryx and Raptors
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The CretaceousThe Western InteriorSeaway
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AmmonitesImportant indexfossils for the
Cretaceous
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Sassafras Leaf fossil from Cretaceous, one of the
early angiosperms (flowering plants). Other
Cretaceous angiosperms included the birch,
sycamore, magnolia, holly, palm, maple and beech
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Large marine reptiles (Plesiosaurs)
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Sunset for the Dinosaurs
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Late Cretaceous Extenction
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Giant meteor impact - possible cause of
Cretaceous extinctions
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