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Unit 6: Geologic Time
 
Chapter 22: The Precambrian Earth
 
p. 576 Earth’s Earliest History

The Divisions of Precambrian Time
Visit this site by the Museum of Paleontology, University of California, Berkeley to learn more about the Precambrian. There is a nice analogy here that helps you understand how long humans have existed as compared to the length of time Earth has existed. At the top of the page is a timeline showing the divisions of Precambrian time. Click on Archaen to find out more about life on Earth during the time period from 3.8 to 2.5 billion years ago. What are stromatolites?

The Age of the Earth
At this United States Geological Survey (USGS) site you can learn more about the oldest rocks on Earth. Although Earth is between 4.6 and 4.5 billion years old, the oldest rocks have an age of 3.8 to 3.7 billion years. Why haven’t geologists found rocks on Earth that are as old as Earth itself?

The Earliest Atmospher e, Oceans, and Continents
Go to this site by the Space Physics Research Laboratory at the University of Michigan for an explanation of Earth’s early atmosphere, oceans, and continents. What was the source of present-day oceans? Where did this material come from originally?

Introduction to the Cyanobacteria
Visit this Museum of Paleontology, University of California, Berkeley site to learn more about cyanobacteria. Scientists agree that early cyanobacteria probably produced oxygen during the Archaen and Proterozoic eras to form our present-day atmosphere. What is the other great contribution of cyanobacteria to life on Earth?

p. 588 Ozone in Earth’s Atmosphere

Ozone and the Atmosphere
Go to this National Aeronautics and Space Administration (NASA) site to learn about the protective role of ozone in Earth’s stratosphere. Scroll down and click on formation of the ozone layer. What is the origin of the oxygen in the ozone layer?

Reports to the Nation on Our Changing Planet: Our Ozone Shield
At this National Oceanic and Atmospheric Administration (NOAA) site you can find out why the ozone layer is so important to life on Earth, and how human activities have damaged it. This is a comprehensive look at what ozone is and how it protects living things from harmful ultraviolet light. The site also explains how scientists discovered that human activities were harming the ozone layer. This is an excellent site.

The Ozone Depletion Process
Visit this Environmental Protection Agency (EPA) site to learn more about ozone depletion in Earth’s atmosphere. This site explains how chlorofluorocarbons (CFCs) contribute to ozone depletion. Scroll down and click on ultraviolet (UV) light to see how UV light is affected by ozone. Which type of UV light is absorbed by ozone?

Basic Chemistry of Ozone Depletion
At this NASA site you can learn about the basic chemistry of ozone depletion. Although this site does not have fancy graphics, it gives you a relatively simple explanation of how ozone is destroyed in Earth’s atmosphere.

p. 591 Life at Hydrothermal Vents

Ocean Planet: Recently Revealed
Visit this Smithsonian Institution site for information on life at hydrothermal vents. The site includes lots of links to additional information on hydrothermal vents. Scroll down and click on Creatures of the Thermal Vents to open an article from Popular Science magazine on this subject. This article nicely sums up what is known about life at hydrothermal vents. Water pouring out of vents is as hot as 400ºC and contains hydrogen sulfide. Which of these factors supports life around hydrothermal vents?

Hydrothermal Vent Geochemistry
Go to this NOAA site to learn more about the geochemistry of hydrothermal vents. Hydrothermal systems appear to have a major impact on local ocean chemistry. What compounds do hydrothermal vents add to seawater?

The Light at the Bottom of the Ocean
At this site by Science News Online you can find out about a new discovery at hydrothermal vents deep on the ocean floor—faint, but detectible, light. Scientists don’t yet understand the source of this light, but it could be strong enough to allow some photosynthesis deep in the ocean. This discovery is still being examined.

WHOI in Motion
Go to this site by Woods Hole Oceanographic Institution to view images of the organisms found at hydrothermal vents. Click on the slide at the top left of the screen to see a short movie taken at a vent. It takes several minutes to load the movie, so be patient. The movie is very cool.

p. 593 Ediacara Fauna

Edicaran Fauna
Visit this site to read about ediacaran fauna. The article describes a controversy among scientists as to whether the ediacara were ancestral animals. Read the article to form an opinion of your own. Were the ediacara ancestors of today’s animals or were they a completely different form of life?

Learning About the Vendian Animals
At this site by the Museum of Paleontology, University of California, Berkeley you can see images of ten edicaran fossils. Click on any image to see what is known about that fossil. Or you can scroll down and click on Ediacara Hills to see the location in Australia where these fossils were first identified. What does the word ediacara mean?

Ediacara Biota
Go to this site by the Miller Museum of Geology, Queen’s University, Canada to learn about the ediacaran fossils found in Canada. Since the discovery of ediacaran fossils in Australia in 1946, such fossils have been found on every continent except Antarctica. Scroll down to the map of Canada and click on any of the images to learn more about the fossils found at that site.

p. 596 Pseudofossils

False Fossils
At this Geoscience Research Institute site you can read an article about false fossils. Although this is a scientific article, it shows how geologic formations can be mistaken for fossils. What is a pisolite?

Concretions
Visit this site to learn about concretions, compact masses of minerals that at one time were thought to be fossils of plant or animal life. Read about how concretions form. Why did fossil collectors break open concretions?

 


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