Cenozoic Mammals and the Modern World. Cenozoic 65-0 Myr.

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Cenozoic Mammals and the Modern World
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Transcript of Cenozoic Mammals and the Modern World. Cenozoic 65-0 Myr.

Page 1: Cenozoic Mammals and the Modern World. Cenozoic 65-0 Myr.

Cenozoic

Mammals and the Modern World

Page 2: Cenozoic Mammals and the Modern World. Cenozoic 65-0 Myr.

Era Age (Myrs) Epoch

0.01Holocene

1.8Pleistocene

5.3Pliocene

23.8Miocene

33.6Oligocene

54.8Eocene

65Paleocene

144

206

248

290

323

354

417

443

490

543

2500

3800

Precambrian

Phanerozoic

Eon

Proterozoic

Archean

Hadean

Period

Quaternary

Tertiary

Neogene

Paleocene

Mississippian

Cenozoic

Mesozoic

Paleozoic

Cretaceous

Jurassic

Age of the Earth 4600 Myrs (4.6 Byrs)Source: Geological Society of America (1999)

Geologic Time Scale

Devonian

Silurian

Ordivician

Cambrian

Triassic

Permian

Pennsylvanian

Cenozoic

65-0 Myr

Page 3: Cenozoic Mammals and the Modern World. Cenozoic 65-0 Myr.

Highlights of the Cenozoic:Geology

1. Continents move into their current configurations. (Western NA remains active.)

2. Tethys Sea closes with the Alpine/Himalayan Orogeny.

3. Minor sea level fluctuations4. Temperature peaks in the Eocene

and drops through the Pliocene/Pleistocene Ice Age.

Page 4: Cenozoic Mammals and the Modern World. Cenozoic 65-0 Myr.

Highlights of the Cenozoic:

Life1. Mammals and angiosperms

(including grasses) diversify and dominate.

2. Mammals return to the sea.3. Two minor mass extinctions -

Eocene and Pleistocene/Holocene.4. Humans appear in the Pliocene

and by the late Holocene become a “geologic force”.

Page 5: Cenozoic Mammals and the Modern World. Cenozoic 65-0 Myr.

Cenozoic Geology

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Late Cretaceous

Page 7: Cenozoic Mammals and the Modern World. Cenozoic 65-0 Myr.

Early Eocene

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Late Eocene

Page 9: Cenozoic Mammals and the Modern World. Cenozoic 65-0 Myr.

Early Miocene

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Late Miocene

Page 11: Cenozoic Mammals and the Modern World. Cenozoic 65-0 Myr.

Separation of

Antarctica&

Climate

Page 12: Cenozoic Mammals and the Modern World. Cenozoic 65-0 Myr.

Alpine/Himalayan Orogeny & the Closing

of the Tethys Sea

Page 13: Cenozoic Mammals and the Modern World. Cenozoic 65-0 Myr.

The Rise and Fallof the Western US

Subduction to San Andreas

Laramide Orogeny to Basin and Range

Page 14: Cenozoic Mammals and the Modern World. Cenozoic 65-0 Myr.

Subduction of the

Farallon Plate:

Origin of the San Andreas

Fault and the Gulf of California

Page 15: Cenozoic Mammals and the Modern World. Cenozoic 65-0 Myr.

Subduction of a

Spreading Ridge

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The Laramide Orogeny(Rocky Mountains)

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The Basin and Range

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The Basin and Range

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Curiosities: The Grand Canyon

<5 Myr Old!

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Curiosities: Yellowstone

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Curiosities: The Olympics

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Curiosities:

Chesapeake Bay

Late Eocene

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Curiosities: Central America

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Central American Land Bridge

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Climate - Hot

to Cold

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Sea Level

Fluctuations

Transgression Regression

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The Pliocene/Pleistocene

Ice Age

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The Final

Ice Age

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What Causes Ice Ages?

1. Position of the Continents• Changes to Ocean Currents• Closer o Poles

2. Orogenies / Uplift of Land Surface• Changes in air circulation• Increased erosion

3. Changes in Greenhouse Gases

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Glacial Cycles within an Ice Age

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What Cause

s Cycles?

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Some Effects of the Ice

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Changing Ecosystems