'Eocene' presentation slideshows

LIFE AFTER JURASSIC PARK: MAMMAL EVOLUTION DURING THE CENOZOIC

LIFE AFTER JURASSIC PARK: MAMMAL EVOLUTION DURING THE CENOZOIC. PALEOGEOGRAPHY AND CLIMATIC CHANGES IN THE CENOZOIC. There were a series of climatic changes during the Cenozoic that were the product of changes in the continental masses.

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IV. Cenozoic (65 - 0 mya)

IV. Cenozoic (65 - 0 mya). IV. Cenozoic (65 - 0 mya). Anthropocene 0.005. IV. Cenozoic (65 - 0 mya) The major groups of mammals had evolved in the Jurassic and Cretaceous. IV. Cenozoic (65 - 0 mya)

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Physical evolution

Physical evolution. Late Proterozoic Era 600ma. Early Cambrian Period 550 ma. Late Cambrian 500 ma. Early Ordivician 485 ma. Late Ordovician 440 ma. Silurian 430 ma. Early Devonian 410 ma. Late Devonian 360 ma. Early Carboniferous 340 ma. Late Carboniferous 290ma. Late Permian 270 ma.

687 views • 45 slides

Western U.S. orogenies

Western U.S. orogenies. Late Cretaceous 75 Ma. K/T boundary 65 Ma. The Paleogene World. Holocene Pleistocene. Pliocene. Two-fold subdivision of Cenozoic: Paleogene , Neogene Previously , Cenozoic was divided into Tertiary (Paleocene-Pliocene) and Quaternary (Pleistocene-Holocene)

326 views • 31 slides

Cenozoic Era

Cenozoic Era. The Epochs. Paleocene Eocene Oligocene Miocene Pliocene Holocene. Paleocene. A geologic epoch that lasted from 66 to 56 million years ago Is the first epoch in the cenozoic era Started with a mass extinction at the end of the cretaceous period.

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Lessons from the Miocene Climatic Optimum

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Eocene Climate Modelling, and the causes of the Palaeocene-Eocene Thermal Maximum (PETM)

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Chiroptera (hand-wing)

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Fossil Turtles of South Dakota

Fossil Turtles of South Dakota. Lilly Sanovia Oglala Lakota College June, 2012. The Oligocene Epoch. 34-24 million years ago Begins with a major extinction event The climate was cooling after a warm, tropical period during the Eocene

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315 views • 23 slides

Early Primates from the Paleocene Through Miocene

166 views • 16 slides

Chapter 5

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Chapter 5

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Cenozoic Mammals

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Geologic Ages

Geologic Ages. Times of deep time. Eons. present. Phanerozoic. 543 Ma. Proterozoic. 2500 Ma. Archean. 3800 Ma. Eras. Phanerozoic. Cenozoic. Proterozoic. Mesozoic. Archean. Paleozoic. Eras. present. Cenozoic. 65 Ma. Mesozoic. 248 Ma. Paleozoic. 543 Ma. Periods. Permian.

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AZUARA BASIN

AZUARA BASIN. ?. an Eocene-Oligocene Impact Structure. -What makes a crater a crater?. 1. Shatter cones 2. Breccias and Breccia Dikes 3. Shock metamorphism 4. Impact melts. - THE CONTROVERSY. NOT A REAL SLIDE (MADE YOU LOOK!). Bottom: left to right: 1. shatter cone

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Depositional environments as represented in classic fields in Norway

This workshop will focus on how to learn development/production strategies from fields that produce in specific depositional environments. The workshop will include presentations and core session.

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