THE PENNSYLVANIAN The Age of Coal Swamps Beginning of Absaroka Sequence Regression of Kaskaskia Erosion took place Large regional unconformity.

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Presentation transcript:

THE PENNSYLVANIAN The Age of Coal Swamps Beginning of Absaroka Sequence Regression of Kaskaskia Erosion took place Large regional unconformity

THE PENNSYLVANIAN The Age of Coal Swamps Beginning of Absaroka Sequence Seas of Absaroka encroach in in Middle Penns. Deposits to east are thicker Terrestrial ss, sh, coal beds

THE PENNSYLVANIAN The Age of Coal Swamps Pennsylvanian Cyclothems Transgressive-regressive events Alternation between marine and nonmarine sediments Represents a change in depositional environment caused by a single advance and retreat of sea

THE PENNSYLVANIAN The Age of Coal Swamps Pennsylvanian Cyclothems

THE PENNSYLVANIAN The Age of Coal Swamps Pennsylvanian Cyclothems Correlated over large areas 50 cyclothems recorded in Missouri and Kansas All about 750 m in thickness, 1000’s of kilometers 2 Eustatic sea level change caused by advance and retreat of continental glaciers

THE PENNSYLVANIAN The Age of Coal Swamps Southwest Portion of Craton Ancestral Rockies

THE PENNSYLVANIAN The Age of Coal Swamps Southwest Portion of Craton Ancestral Rockies Fountain Formation – Flatirons, Boulder, CO

THE PENNSYLVANIAN The Age of Coal Swamps Southwest Portion of Craton Ancestral Rockies

THE PENNSYLVANIAN The Age of Coal Swamps Southwest Portion of Craton Ancestral Rockies

THE PENNSYLVANIAN The Age of Coal Swamps Southwest Portion of Craton Ancestral Rockies Paradox Valley CO-UT

THE PENNSYLVANIAN The Age of Coal Swamps Southwest Portion of Craton Ancestral Rockies

THE PENNSYLVANIAN The Age of Coal Swamps Southwest Portion of Craton Ancestral Rockies

THE PENNSYLVANIAN The Age of Coal Swamps Southwest Portion of Craton Ancestral Rockies

THE PENNSYLVANIAN The Age of Coal Swamps Southwest Portion of Craton Ouachita Mountains

THE PENNSYLVANIAN The Age of Coal Swamps Southwest Portion of Craton Ouachita Mountains

THE PENNSYLVANIAN The Age of Coal Swamps Southwest Portion of Craton Ouachita Mountains Mississippi Embayment Southern Appalachians

THE PENNSYLVANIAN The Age of Coal Swamps Life in the Pennsylvanian Calamites, L Lepidodendron, M Sigillaria, A

Reconstructions of Lepidodendron (far left, Late Carboniferous, ~50 m tall), Sigillaria (left, Late Carboniferous, ~40 m,), Valmeyerodendron (middle top, Early Carboniferous, 0.6 m), Protolepidodendron (top right, Middle Devonian, 0.2 m), Chaloneria (bottom middle, Late Carboniferous, 2 m), Pleuromeia (bottom right, Triassic, 2 m) and Isoetes (bottom far right, extant, 30 cm).

THE PENNSYLVANIAN The Age of Coal Swamps Life in the Pennsylvanian

THE PENNSYLVANIAN The Age of Coal Swamps Life in the Pennsylvanian

THE PENNSYLVANIAN The Age of Coal Swamps Life in the Pennsylvanian Insects

THE PENNSYLVANIAN The Age of Coal Swamps Life in the Pennsylvanian Lagerstatten Mazon Creek IL Fern Lepidodendron

THE PENNSYLVANIAN The Age of Coal Swamps Life in the Pennsylvanian Lagerstatten Joggins, NS

THE PENNSYLVANIAN The Age of Coal Swamps Life in the Pennsylvanian Lagerstatten Joggins, NS plants

THE PENNSYLVANIAN The Age of Coal Swamps Life in the Pennsylvanian Lagerstatten Joggins, NS first reptiles

THE PENNSYLVANIAN The Age of Coal Swamps Life in the Pennsylvanian Lagerstatten Joggins, NS insects

THE PENNSYLVANIAN The Age of Coal Swamps Life in the Pennsylvanian Lagerstatten Joggins, NS First terrestrial gastropods

THE PERMIAN The Age of Pangaea Named for Permia, an ancient kingdom between the Urals and the Volga River Named by Murchison in 1841

THE PERMIAN

Alleghenian Orogeny continues

THE PERMIAN Sonoman Orogeny

THE PERMIAN

El Capitan Capitan Ls. Guadalupe Mountains, TX

THE PERMIAN Castille Fm. evaporited Guadalupe Mountains, TX

THE PERMIAN Reptiles Dimetrodon Mammal-like Reptiles

THE PERMIAN Eggs Amniotic egg allowed Organisms to become terrestrial

THE PERMIAN Plants Glossopteris

THE PERMIAN Permian Extinction

THE TRIASSIC The Break-up of Pangaea Three-fold division of rocks in Germany Named by Frederich von Alberti in 1834

THE TRIASSIC

Absaroka Sea continues to retreat Triassic is very terrestrial Period

THE TRIASSIC

Joshua Chamberlain, left Little Round Top, Battle of Gettysburg 3 July, 1863

THE TRIASSIC Chinle Formation, Petrified Forest National Park

THE TRIASSIC Chinle Formation, Painted Desert

THE TRIASSIC Triassic Reptiles Mammal-like

THE TRIASSIC Triassic Reptiles Diversification of dinosaurs Coelophysis Dilophosaurus

THE TRIASSIC First Marine Reptiles

THE TRIASSIC Mammals Evolve