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Earth History GEOL 2110 The Paleozoic Era Late Ordovician Period Limestone, Limestone, and more Limestone and The Emergence of the Appalachians

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Earth History GEOL 2110. The Paleozoic Era Late Ordovician Period Limestone, Limestone, and more Limestone and The Emergence of the Appalachians. Major Concepts. - PowerPoint PPT Presentation

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Page 1: Earth History  GEOL 2110

Earth History GEOL 2110

The Paleozoic EraLate Ordovician Period

Limestone, Limestone, and more Limestone and The Emergence of the Appalachians

Page 2: Earth History  GEOL 2110

Major Concepts• The great Sauk sea retreated to the edge of the NA craton about

480 Ma, when it transgressed the craton again (the Tippecanoe Transgression) over the next 50 million years, a whole new diversity of marine live came with it.

• While Cambrian sands were initially spread over the craton as the Tippecanoe beach trangressed over the land, creating another ultrapure quartz sandstone formation – the St. Peter, this was quickly followed extensive deposition of fossil-rich limestone.

• In the late Ordovician, the eastern margin of Laurentia transformed from a passive continental slope margin to a tectonically active volcanic arc – the Taconic.

• Immature sediments shed westward from this arc accumulated between the continent and the volcanic arc and eventually became deformed and metamorphosed when the arc eventually collided and was thrust onto the continental edge –Penokean-like.

Page 3: Earth History  GEOL 2110

The Tippecanoe TransgressionMid- to Late Ordovician

Page 4: Earth History  GEOL 2110

The Ordovician “Explosion”Changes in Ordovician from Cambrian Fauna

• more complex food chain

• extend higher above the seabed

• hard part made of calcite rather than phosphate

Page 5: Earth History  GEOL 2110

Ecological Diversification of Ordovician FaunaIncreasingly Complex Food Web

Page 6: Earth History  GEOL 2110

Multi-tiered Feeding Levels

Page 7: Earth History  GEOL 2110

Arrival of Classic “Paleozoic” FaunaArticulated

BrachiopodsBryzoans Crinoids

“Sea Lillies”

Sea Shells Twigs Cheerios

Page 8: Earth History  GEOL 2110

…and the world’s best Index fossils!

Conodonts Graptolites Ostracodes

Page 9: Earth History  GEOL 2110

New Kids on the BlockJa

wle

ss B

ony

Fish

Carniverous Nautiloid

Page 10: Earth History  GEOL 2110

Nautiloid fragment found last year on field trip

Page 11: Earth History  GEOL 2110

Why This Explosive Radiation?An Early Ordovician regression followed by the most extensive transgression up to that point in Earth historyEnormous areas of shallow marine environments - niches

Atmospheric oxygen reaches modern-day levels

Page 12: Earth History  GEOL 2110

The Tippecanoe Trangression

St Peter SS – Platteville LS, St. Paul

Page 13: Earth History  GEOL 2110

Capping the Craton in Limestone

Except Here

Page 14: Earth History  GEOL 2110

The Taconic Orogeny

Page 15: Earth History  GEOL 2110

The Taconic Orogeny

Page 16: Earth History  GEOL 2110

The Taconic Orogeny

Page 17: Earth History  GEOL 2110

Modern-Day Analog

Page 18: Earth History  GEOL 2110

Prior-Day Analog1.85 Ga Penokean Orogeny

Page 19: Earth History  GEOL 2110

Next Lecture

The Paleozoic EraCambrian and Ordovician History

of Minnesota and WisconsinHave a Great Spring Break!!!