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Early Paleozoic Earth History
http://jan.ucc.nau.edu/~rcb7/510NAt.jpg
North American Paleogeography
• Broke away from supercontinent ~600 Ma
• Configuration of supercontinent not well-understood
• How do we know?– Evidence of rifting (divergent margin)– Basalt– Subsidence – cooling and thinning of lithosphere
Early Paleozoic Climate of NA
• North America in tropical location
• End of Snowball Earth
• Warmer in Cambrian and Ordovician
• Location of continents and ocean basins constantly changes
• Historical geology provides past geologic and paleogeographic reconstruction of the world
• Paleogeographic maps show – distribution of land and sea– possible climate regimes– geographic features (mountain ranges,
swamps, glaciers)
Paleogeography
• Cambrian world consisted of six major continents at low tropical latitudes
• Water circulated freely among ocean basins, and the polar regions were mostly ice free
Early Paleozoic Global History
• For the Late Cambrian Period
Paleogeography of the World
• For the Late Ordovician Period
Paleogeography of the World
• For the Middle Silurian Period
Paleogeography of the World
• The geologic history of the North American craton may be divided into two parts– relatively stable continental interior over
which epeiric seas transgressed and regressed
– mobile belts where mountain building occurred
• Sedimentary-rock record of NA subdivided into six cratonic sequences
Early Paleozoic Evolution of North America
• The Paleozoic history of most continents – major mountain-building activity along
margins
– numerous shallow-water marine transgressions and regressions
• These transgressions and regressions – caused by global changes in sea level
– related to plate activity and glaciation
Paleozoic History
• A cratonic sequence is – large-scale lithostratigraphic unit – represents a major transgressive-
regressive cycle – bounded by unconformities
• The six unconformities extend across the North American craton
Cratonic Sequence
Cratonic Sequences of N. America
• Rocks of the Sauk Sequence– Late Proterozoic-Early Ordovician– record the first major transgression onto
the North American craton
• Deposition of marine sediments limited to the shelf areas of the craton
• The craton itself was above sea level
The Sauk Sequence
• By the Late Cambrian, Sauk Sea had covered most of North America, leaving above sea level only – a portion of the Canadian Shield – and a few large islands, the Transcontinental
Arch, • extended from New Mexico to Minnesota and the
Lake Superior region
Transcontinental Arch
• During this time North America straddled the equator
• Trans-continental Arch
Cambrian Paleogeography of North America
Cambrian Facies
Cambrian Facies• Sediment derived from craton
• Sandy facies occur closest to craton
• Quartz-rich sand derived from craton– craton surface weathered and eroded for
half a billion years!– no land plants yet – erosion by wind more
common– Mature sandstone: well-rounded, well-
sorted, 99% Qtz,
Where were they deposited?
• Fossils suggest marine environment
• No land animals at this time
• How do we interpret environment?
Use sedimentary structures!
Cross-stratification
• Formed by wind or water
• Wind – dunes > 1 m high
• Water – typically smaller
Cross-stratification
www.env.duke.edu/eos/geo41/win2.htm and homepage.ntlworld.com/donald.mcintyre/menu_files/stones_files/crossbeds_files/peddie_230.jpg
2 m
WIND!
End of Cambrian• Most of North America underwater
• Sauk Transgression
• Epeiric sea– shallow inland sea (over continent)– < 200 m deep
• Cambrian strata exposed in the Grand Canyon
Cambrian Transgression
Beginning of Ordovician• Very little land remaining above SL
• Little terrigenous clastic sedimentation
• Shift to carbonate deposition– limestones formed from shell debris– clear, shallow water
Stromatolites• Constrain water depth
– need sunlight for photosynthesis– Photic zone – 150-200 m
• All evidence suggests very shallow Sauk Sea
http://www.mlssa.asn.au/journals/1999Journal.htm
Shark Bay, Australia
• As the Sauk Sea regressed during the Early Ordovician, it revealed a landscape of low relief
• The rocks exposed were predominately limestones
• The resulting craton-wide unconformity marks the boundary between the Sauk and Tippecanoe sequences
Regression and Unconformity
• Paleogeography of North America showing change in the position of the the equator
Ordovician Period
What North American mountain range began to form
in the Ordovician?
Appalachians
Orogeny
• Named after present-day Taconic Mountains of– eastern New York– central Massachusetts– and Vermont
• First of several orogenies to affect the Appalachian region
The Taconic Orogeny
Appalachian Area
• East coast was passive margin in Early Ordovician – like modern Gulf of Mexico
• Changed to active margin in Middle Ordovician
• Collision with microcontinent or volcanic arc
• Middle Ordovician transition to convergence resulted in orogenic activity
Appalachian Mobile Belt
Ordovician Plate Tectonics
• Volcanic rocks from present-day Georgia to Newfoundland
• Clustering of radiometric ages between 440 to 480 million years ago
• In addition, regional metamorphism coincides with the radiometric dates
Orogeny Timing
Clastic Wedge
Debris eroded from mountains into adjacent basinThick layer of sediment adjacent to source
• Reefs developed in the Michigan, Ohio, and Indiana-Illinois-Kentucky areas
Silurian Period
Silurian Sedimentation