Summary of Early Paleozoic Earth History
Early Paleozoic Earth History
Introduction
1815: William Smith published first geological map of England.
Rocks record geological changes due to plate tectonics and glaciation.
Smith mapped coal mines, contributing to descriptions of Paleozoic periods.
Paleozoic Eras and Major Events
Cambrian (488-542 Ma): First fish and land plants.
Ordovician (444-488 Ma): First reptiles; glaciations in Gondwana.
Silurian (416-444 Ma): First amphibians; coral and sponge reefs became abundant.
Devonian (359-416 Ma): Age of fishes; extensive barrier reef formation.
Carboniferous (299-359 Ma): Major coal swamps; significant mountain-building.
Paleozoic Paleogeography
Reconstruction through paleoclimates, paleomagnetics, fossils, etc.
Major continental movements shaped early Paleozoic landscapes.
Late Cambrian: Epeiric seas; passive continental margins dominate.
Pangea Formation
By end of Permian (251 Ma); changes in ocean and atmosphere circulation patterns.
Continental Developments
Cratons and mobile belts characterized the early Paleozoic architecture.
Cratonic sequences: Major transgressive-regressive cycles due to tectonics/glaciation.
Paleozoic Mineral Resources
Important resources: coal, oil, limestone, gypsum; influenced industrial development.
Climatic and Geological Changes
Late Paleozoic glacial cycles affected Gondwana; coal deposits formed.
Major orogenic events shaped modern landscapes and climates.
Evolution of North America
Dynamic sedimentary record during periods of mountain-building and marine transgressions.
Orogenies: Taconic, Acadian, and Alleghenian.
Significant black shale and coal formations mark various periods.
Cyclothem Deposition
Cyclothems represent alternating marine and nonmarine sedimentation; indicate sea level changes.
Characterized by coal deposits under marine shales.
End of Paleozoic
Transition marked by Pangaea formation and the largest mass extinction event affecting marine and terrestrial life.