chapter 5, section 2 the fossil record monday, january 11, 2010 pages 157 -- 164

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Chapter 5, Section 2 The Fossil Record Monday, January 11, 2010 Pages 157 -- 164

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Page 1: Chapter 5, Section 2 The Fossil Record Monday, January 11, 2010 Pages 157 -- 164

Chapter 5, Section 2The Fossil Record

Monday, January 11, 2010

Pages 157 -- 164

Page 2: Chapter 5, Section 2 The Fossil Record Monday, January 11, 2010 Pages 157 -- 164

Objectives

Describe how most fossils formExplain how a scientist determines a fossil’s age.Explain what fossils reveal.Describe the main events of the Geologic Time Scale.Distinguish between gradualism and punctuated equilibria.

Page 3: Chapter 5, Section 2 The Fossil Record Monday, January 11, 2010 Pages 157 -- 164

Vocabulary Words

Fossil

Sedimentary rock

Petrified fossil

Mold

Cast

Relative dating

Absolute dating

Radioactive element

Half-life

Fossil record

Extinct

Gradualism

Punctuated equilibria

Page 4: Chapter 5, Section 2 The Fossil Record Monday, January 11, 2010 Pages 157 -- 164

What is a fossil?

A fossil is the preserved remains or traces of an organism that lived in the past.Other fossils include things like footprints or burrows left in mud that later turned to stone.

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Fossil of a spider.

Page 5: Chapter 5, Section 2 The Fossil Record Monday, January 11, 2010 Pages 157 -- 164

How Do Fossils Form?

Fossils can form from bones, tooth, shell, or other part of an organism.Most fossils form when organisms that die become buried in sediments.Over millions of years, the sediments build up and layers harden to become sedimentary rock.

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Page 6: Chapter 5, Section 2 The Fossil Record Monday, January 11, 2010 Pages 157 -- 164

Petrified Fossils

Petrified fossils come from remains that are buried in sediments that eventually turns to rock.Gradually, the minerals replace the remains, changing them into rock.

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Petrified wood from Arizona.

Page 7: Chapter 5, Section 2 The Fossil Record Monday, January 11, 2010 Pages 157 -- 164

Molds and Casts

Sometimes shells or other parts that are buried by sediments are gradually dissolved.

The empty space that remains in its place in the shape of the organism is a mold.

A cast is a copy of the shape of the organism that made the mold.

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Amonite mold - left and mold - right.

Page 8: Chapter 5, Section 2 The Fossil Record Monday, January 11, 2010 Pages 157 -- 164

Preserved Remains

Entire organisms have been found preserved in substances other than sediments.

Low temperatures preserved the animal’s soft parts.

Other ancient animals have been preservd in tar pits (tar is a sticky form of oil).

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Preserved remains of an elephant that fell in ice.

Page 9: Chapter 5, Section 2 The Fossil Record Monday, January 11, 2010 Pages 157 -- 164

Determining a Fossil’s Age

The age of a fossil can be determined in two ways:

Relative Dating

Absolute Dating

Page 10: Chapter 5, Section 2 The Fossil Record Monday, January 11, 2010 Pages 157 -- 164

Relative Dating

Relative dating is used to scientists to determine which of two fossils is older.

Mainly used when looking a various layers.

The layers closest to the outside are younger.

Relative dating will not determine the actual age of the fossil.

Page 11: Chapter 5, Section 2 The Fossil Record Monday, January 11, 2010 Pages 157 -- 164

Absolute Dating

Absolute dating allows scientists to determine the actual age of a fossil.Fossils are found near rocks that contain radioactive elements.

Radioactive elements are unstable and break down to form other elements.The half-life of a radioactive element is the time it takes for half of the atoms in a sample to decay.The amount of radioactive element in a sample is compared to the amount of the element into which it breaks down.

Page 12: Chapter 5, Section 2 The Fossil Record Monday, January 11, 2010 Pages 157 -- 164

Fossil Record

Fossil record is the millions of fossils that scientists have collected.

The fossil record is incomplete.

Fossil records provide clues about how and when new groups of organisms evolved.

Most of the species preserved as fossils are now extinct.

Members of this species are no longer alive.

Page 13: Chapter 5, Section 2 The Fossil Record Monday, January 11, 2010 Pages 157 -- 164

Geologic Time Scale

The geologic time scale is also known as the calendar of Earth’s history.

Largest span is the Precambrian Time.

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Page 14: Chapter 5, Section 2 The Fossil Record Monday, January 11, 2010 Pages 157 -- 164

Gradualism

Gradualism is the process that evolution occurs slowly but steadily.According to this theory, tiny changes in a species gradually add up to major changes over very long periods of time.This is what Charles Darwin believed.

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Page 15: Chapter 5, Section 2 The Fossil Record Monday, January 11, 2010 Pages 157 -- 164

Punctuated Equilibria

Species evolve during short periods of rapid change.Periods of rapid change are separated by long periods of little or no change.According to this theory, species evolve quickly when groups are isolated and adapt to new environments.

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Page 16: Chapter 5, Section 2 The Fossil Record Monday, January 11, 2010 Pages 157 -- 164

Homework

Workbook 5.2 (1/13)

Worksheet 5.2 (1/13)

Vocabulary quiz 5.2 (1/14)