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Published byBernadette Terry Modified over 9 years ago
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Paleozoic Era Life starts in the seas and moves onto land
570,000,000 years ago to 225,000,000 years ago Six periods: Cambrian Ordovician Silurian Devonian Carboniferous Permian
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Cambrian Period (570-500 MYA)
Cambrian Explosion – Most major animal phyla are found in the fossil record (mostly aquatic invertebrates with exoskeletons). Burgess Shale – major fossil site located in Canadian Rockies
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Ordovician Period (500-435 MYA)
1st vertebrates - jawless fish (filter feeders) The vertebrate protects the spinal cord, which carries signals from the brain throughout the body. The lamprey of today is a parasite. The hagfish is a scavenger.
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Silurian Period (435-395 MYA)
1st jawed fish (later evolved into sharks-made of cartilage). Ozone (O3) layer formed which blocks harmful UV radiation; life could evolve on land. 1st land plants (mosses & ferns) followed by 1st land animals (arthropods-spiders & scorpions).
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Devonian Period (395-345 MYA)
“Age of the Fish” (giant armored fish). 1st bony fish (scales and swim bladder for buoyancy).
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Devonian Period (395-345 MYA)
1st vertebrates on land – amphibians Evolved from the lobed-fin fish which include some species of lungfish.
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Carboniferous Period (345-280 MYA)
North America is at the equator (tropical swamps form coal deposits) Amphibians & insects dominate and become large (dragon flies-1m wing span; cockroaches-10 cm long). 1st reptiles
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Permian Period (280-225 MYA) Reptiles dominate.
Pangaea begins to form (Appalachian Mnts; dry climate; ice age in the southern hemisphere) Mass Extinction (90% of all species go extinct-mostly marine invertebrates). Early Permian reptiles, Cacops in front & Casea in back. The middle Permian reptile, Anteosaurus.
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Mass Extinction One of the Big FIVE Mass Extinctions
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