PALEOZOIC ERA
Transcription
PALEOZOIC ERA
PALEOZOIC ERA ABUNDANT FOSSILS BEGIN START of the PALEOZOIC ERA • Continents separate • North American continent at the equator with the Arctic region facing eastward PALEOZOIC PERIODS Cambrian Ordovician Silurian Devonian Mississippian Pennsylvanian Permian • • • • • • • Trilobites, 1st vertebrates Graptolites, 1st corals Eurypterids, 1st land animals Age of fishes, 1st forests Crinoids & Foraminifera Age of Cockroaches, 1st reptiles Pangaea forms, 1st mammals CAMBRIAN PERIOD • No land plants or animals • Most of North America covered with warm oceans • Burgess Shale forms in the Rocky Mountain region with soft bodied animals • Common fossils – Trilobites (like crabs) - index – Brachiopods (like clams) – Ostracoderms (primitive fish) Cambrian Period – Life in the Oceans Trilobite – Index Fossil of the Cambrian Period Fossil Found in the Burgess Shale ORDOVICIAN PERIOD • All life exists in the oceans • Small plate from northwest Africa collides with eastern North America to form the Green & Taconic mountains • Common fossils – Graptolites (colonial floating animals) - index – Brachiopods, bryozoans, pelecypods, corals, echinoderms, gastropods, cephalopods Ordovician Period – Life in the Oceans Graptolite – Index Fossil of the Ordovician Period SILURIAN PERIOD • 1st land animals – Ancestors of spiders, millipedes, scorpions • Land plants – Club mosses • Eastern North America – Dry climate evaporates the shallow seas leaving large salt & gypsum deposits • Common fossils – Eurypterids (sea scorpions) – index – Coral forming coral reefs, others like Ordovician life Eurypterid – Index Fossil of the Silurian Period (a sea scorpion) DEVONIAN PERIOD • Age of Fishes – Lungfish lived briefly on land • 1st forests – Primitive conifers, ferns, giant rushes • North America – Still at the equator, northwest Africa collides with eastern North America to form the northern Appalachians & White mountains • Common fossils – Coral reefs, jawless & armoured fish Age of Fishes Marine Life of the Devonian Period Formation of the Northern Appalachian Mountains Flooding of the Land – Fertile Soil for Plants Trees Taking Root on Land to Form the 1st Forests Trees of the Devonian Period Extinctions of the Devonian Period MISSISSIPPIAN PERIOD • Common fossils – Crinoids (sea lilies) – starfish attached to the sea floor – Foraminifera (amoeba like single celled animals) – tiny calcite shells • North America – Southern Appalachian mountains form Crinoid Attached to the sea floor Foraminifera Single-celled Calcite shells Animals of the Mississippian Period North America at the Equator – Forming the Southern Appalachian Mountains PENNSYLVANIAN PERIOD • Age of Cockroaches – Insects increase, large dragonflies & cockroaches • 1st reptiles – lizards • North America – Still at the equator – Warm, wet climate floods eastern USA in huge freshwater swamps – forming rich coalfields – Continents continue colliding to form the Appalachian mountains Age of the Cockroaches Swamps Covering Eastern North America – forming coalfields 1st Reptiles – the Lizards North America at the Equator – forming the Appalachian Mountains PERMIAN PERIOD • Dry climate – Shallow inland seas evaporated leaving large deposits of salt & gypsum • Large reefs – Coral, algae, sponges thrived • Great southern ice age – South America, Australia, South Africa, India Dry Climate of the Permian Period - Shallow inland seas Large Coral Reefs Large Reptiles of the Permian Period END of the PALEOZOIC ERA • Pangaea forms – Continental crust welds together into one supercontinent • Mountains form – Appalachian & Ural mountains fully elevate • 96% species extinction – Trilobites, eurypterids, coal forming seed ferns, scale trees & primitive conifers - extinct • 2 important survivors – Cephalopods (oceans) & reptiles (land) Pangaea – the Supercontinent