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The Rock and Fossil Record
The Rock and Fossil Record

... The Geologic Time Scale B. The Paleozoic Era—Old Life The Paleozoic era lasted from about 543 million to 248 million years ago. It is the first era well represented by fossils. Ended with the largest mass extinction in Earth’s history. C. The Mesozoic Era—The Age of Reptiles The Mesozoic era began ...
History of Life on Earth
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Historical Geology
Historical Geology

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Quaternary Period
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CHICXULUB CRATER - University of Colorado Boulder
CHICXULUB CRATER - University of Colorado Boulder

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Extinction Hypothesis B – Continental Drift
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Learning goals for Geologic Time (Chapter 11)
Learning goals for Geologic Time (Chapter 11)

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Chapter 20 The Origin and Evolution of Life
Chapter 20 The Origin and Evolution of Life

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EarthViewer Questions
EarthViewer Questions

... 9. When  was  the  Cambrian  Explosion?  ___________________________________________________   a. What  %  of  the  atmosphere  was  Oxygen  (O2)?  ________________________________   b. What  %  of  the  atmosphere  is  O2  today?  ______________________ ...
Name______________________ due date ______ period
Name______________________ due date ______ period

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Vocabulary Review - POTOSI SCHOOL DISTRICT
Vocabulary Review - POTOSI SCHOOL DISTRICT

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Earths History - Mrs. Meadows Science
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Part 2 - Mahopac Voyagers!
Part 2 - Mahopac Voyagers!

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... appeared. Several important new types of organisms evolved during the Triassic. For example, the first dinosaurs were among the many types of reptiles that evolved. ...
Earth: An Ever changing planet
Earth: An Ever changing planet

... Eons – Millions and Billions of years • Haden: Earth before life evolved 4.6 to 3.5 Billion years ago (13% of Earth’s history) • Achaean: Earth with only bacteria like cells 3.5 to 2.5 Billion years ago (28% of Earth’s history) • Proterozoic: Multicellular life forms 2.5 BYA to 540 MYA (48% of Eart ...
Chapter 17 The History of Life
Chapter 17 The History of Life

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devonian presentation
devonian presentation

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Phanerozoic

The Phanerozoic /ˌfænərɵˈzoʊɪk/ (British English Phanærozoic) is the current geologic eon in the geologic time scale, and the one during which abundant animal and plant life has existed. It covers 541.0 ± 1.0 million years and goes back to the period when diverse hard-shelled animals first appeared. Its name derives from the Ancient Greek words φανερός (fanerós) and ζωή (zo̱í̱), meaning visible life, since it was once believed that life began in the Cambrian, the first period of this eon. The time before the Phanerozoic, called the Precambrian supereon, is now divided into the Hadean, Archaean and Proterozoic eons. Plant life also appeared from early in the Phanerozoic eon.The time span of the Phanerozoic includes the rapid emergence of a number of animal phyla; the evolution of these phyla into diverse forms; the emergence and development of complex plants; the evolution of fish; the emergence of insects and tetrapods; and the development of modern faunas. During this time span tectonic forces caused the continents to move and eventually collect into a single landmass known as Pangaea, which then separated into the current continental landmasses.
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