Permian

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13 Terms

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Permian glaciation

Permian glaciation
• Global disconformity in marine sediments
• Fossils allow global correlation.

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Rates of Origination and Extinction

Rates of Origination and Extinction
• Marine mass extinction most extensive, ever
• Recovery (origination) lagged, was slow compared to extinction

• During ice age, new species were adapted to seasonal climatic changes, broadly distributed in Panthallasic Ocean
• Resistant to extinction, and also speciation during the ice age

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Permian glaciation

Permian glaciation
• At the end of the ice age, massive mass
extinction – again, due to climate change.
• Life is fragile!

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Permian Paleogeography

Permian Paleogeography
-Pangaea nearly complete
-Ural Mountains
-Large supercontinent produces strong climate gradients
overland between temperate coastal, extreme

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Interior Pangaea

Interior Pangaea

-Low moisture
-Evaporites and dunes
-Reduced carbon burial
-Led to higher atmospheric CO2
-Global warming ended glaciation

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At end of ice age, two mass extinctions:

At end of ice age, two mass extinctions
1) Guadalupian; mostly marine
2) Terminal Permian extinction; affected many terrestrial animals
-Probably caused by Asian vulcanism

-By the end Permian mass extinction, 60% marine genera, 80% marine species died out
-Largest ever for a Phanerozoic mass extinction!!

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Terminal Permian mass extinction killed:

Terminal Permian mass extinction killed:
-Trilobites! Oh no!
-Tabulate and rugose corals
-Ammonids, crinoids, bryozoans hang in there
-Most Therapsids killed, but not all
-Lystrosaurus survives, dominated Therapsids in Triassic; pig-like herbivore thrived in absence of predators
-terrestrial plants: gymnosperms and woody conifers mostly
died, replaced by small, non-woody lycopods
—> FORESTS DISAPPEARED

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What caused the two Permian mass extinctions?

What caused the two Permian mass extinctions?
-Stagnation of deep ocean probably reflects warming of polar regions due to global warming
-Terrestrial sediments also reflect warming, drying climate
-Eruption of Siberian Traps probably caused terminal Permian warming, mass extinction

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Marine extinctions: Why global ocean anoxia?

Strictly temperature-driven extinction; conodont
d18O records indicate 8 deg. C (14 deg. F!) increase;
would kill shallow-water marine (and deep) species, as
well as terrestrial

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Did permain mass extinction kill all life?

It didn’t kill ALL LIFE

-90 marine animal orders that persisted, with significant anatomical, physiological, ecological diversity, and gave rise to marine life that flourished in Mesozoic

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Regional geologic events of Late Paleozoic

Regional geologic events of Late Paleozoic
• Mountain building in both Western (Sonoma) and Eastern (Allegheny and Ouachita) US
• Reef formation in Western US
Alleghenian Orogeny
• Mountain building in
Eastern US
• Valley and Ridge
– Thrust faults
• Blue Ridge
– Grenville

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Ouachita Mountains

Ouachita Mountains
– Westward continuation of Appalachians
– Fold and thrust belt of offshore deposits

• Ouachita Mountains
– Flysch deposits, deep black shales shoved on top of carbonates of Ordovician to Carboniferous age; offshore deformation with high rate of deposition; unusual, very deep offshore basin

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Coal-bearing cyclothems

Coal-bearing cyclothems (coal measures, in Britain) accumulated in marginal marine environments in the midcontinent

• Cycles in thin coal beds that contain marine sediments
– Slight change in sea level
– Alternating transgressions and regressions


• Transgression
– Think Everglades! Large, swampy area with slowly flowing water
—> Coal swamps form over non-marine deposits during a transgression, carbonate on top