Copyright Pearson Prentice Hall

Slides:



Advertisements
Similar presentations
Chapter 17: The History of Life Calif. Science standards 8e
Advertisements

Mr. Karns Biology Fossils.
Outine 17-1: The Fossil Record
17-1 The Fossil Record. A fossil is defined as any evidence of life that existed long ago. A fossil can be a plant, an animal, a footprint, an egg, a.
Copyright Pearson Prentice Hall
The Fossil Record Section 17–1
Chapter 17 – Miller · Levine
Chapter 17: History of Life.
How do we know the age of the Earth?
17.1 The Fossil Record Fossils and Ancient Life Paleontologists – scientists who collect and study fossils. Fossil – any evidence of an organism that.
Chapter 19 The History of Life.
Fossils and Geologic Time Scale Chapter 17. What’s It All About Essential Question: Can relative dating and relative frequency be a trusted thing? Objectives:
How do scientists know evolution has occurred?. Paleontologists: scientists who study fossils Geologists: scientists who study rock layers.
Chapter Paleontologists- scientists who collect and study fossils 2. Fossil Record- evidence about the history of life on Earth & shows how.
14.1 Fossil Evidence of Change Land Environments The History of Life Chapter 14  Earth formed about 4.6 billion years ago.  Gravity pulled the densest.
End Show Slide 1 of 40 Copyright Pearson Prentice Hall 17-1 The Fossil Record.
End Show Slide 1 of 40 Copyright Pearson Prentice Hall 17-1 The Fossil Record.
What are fossils? The remains, imprints or traces of an organism that lived long ago. Preserved in rock. – Typically sedimentary rock – Must be buried.
17-1 The fossil record. Fossils Remains of once-living things Appear in a particular order Provide evidence for evolution.
Fossils and Geologic Time
Key Concepts: Why is the geological time scale used to show Earth’s history? What are the different units of the geological time scale? Key Terms: geological.
History of Biological Diversity 14.1 The History of Life.
Chapter 4 A trip Through Geologic Time
Section 10:3 Radioactive Decay.
 Fossils are preserved remains or traces of living things  Most fossils form when living things die and are buried by sediments. The sediments slowly.
Fossils & The Geologic Time Scale. Fossils Preserved remains or traces of an organism that lived in the past. Fossils are formed when organisms die and.
1/28/13 - QOTD In the picture below, where is the oldest rock? A B.
End Show Slide 1 of The Fossil Record. End Show 17-1 The Fossil Record Slide 2 of 40 Fossils and Ancient Life What is the fossil record?
17-1 The fossil Record 17-2 Earth’s Early History 17-3 Evolution of Multicellular life 17-4 Patterns of Evolution.
Slide 1 of 40 The Fossil Record. Slide 2 of 40 Fossils and Ancient Life What are fossils? What are fossils? Preserved remains of ancient organisms Preserved.
Evolutionary History Chapter 15. What you need to know! The age of the Earth and when prokaryotic and eukaryotic life emerged. Characteristics of the.
Chapter 17 Section 1 paleontologists- scientists who study fossils -they infer what past life forms were like -arrange fossils according to time in which.
The History of Life Chapter 17. Fossils and Ancient Life Fossil → Any part of, trace of, or preserved remains of ancient life –Fossils may be all, part,
Chapter 19: The History Of Life Ridgewood High School
17-1: The Fossil Record Biology 2. Studying history of life is fascinating and challenging Scientists can study ancient rocks, sap from trees, bogs and.
CHAPTER 6 History of the Earth. Origins of the Universe What does the Bible say about the origins of the universe? What have scientist learned about the.
CHAPTER 17 THE HISTORY OF LIFE
The history of life on Earth is filled with mystery and violence.
LE1 – 06 – Life in Geological Time
Fossils & The Geologic Time Scale
Earth’s Geologic History based on fossils
The Geologic Time Scale
Copyright Pearson Prentice Hall
Copyright Pearson Prentice Hall
Science 9 Review for the Earth History
Fossils & The Geologic Time Scale
Geological time, Fossils, & Dinosaurs
Earths History: Geological Time, Rocks, Fossils
Section 14.1 Summary – pages
Fossils & The Geologic Time Scale
Fossils FOSSIL: Any preserved evidence of life from a past geological age, such as the impressions and remains of organisms embedded in sedimentary rock.
Fossils & The Geologic Time Scale
Good Morning!!! Today we will be finishing up GATTACA and starting some new stuff! To prepare for class please… Please get out your GATTACA question sheets.
The History of Life Ch. 17.
The Geologic Time Scale
The Fossil Record (Ch 19.1) Unit 5: Evolution.
Chapter 17 The History of Life
The Fossil Record Section 3
Copyright Pearson Prentice Hall
Unit 8 A: The Geologic Time Scale and Fossils
Earth’s Structure Earth’s History
Chapter 17: History of Life.
Copyright Pearson Prentice Hall
The Age of Earth Ch 19.2 Biology.
Copyright Pearson Prentice Hall
Fossils & The Geologic Time Scale
Fossil Evidence of Change
The Fossil Record.
The Fossil Record.
The Rock and Fossil Record
Presentation transcript:

Copyright Pearson Prentice Hall 17-1 The Fossil Record Photo credit: Jackie Beckett/American Museum of Natural History Copyright Pearson Prentice Hall

Fossils and Ancient Life __________________are scientists who collect and study fossils. All information about past life is called the________ ____________. The fossil record includes information about the structure of organisms, what they ate, what ate them, in what environment they lived, and the order in which they lived. Copyright Pearson Prentice Hall

Fossils and Ancient Life The fossil record provides evidence about the history of__________on Earth. It also shows how different groups of organisms, including species, have_______________________. The fossil record provides____________information about the history of life. Over ________of all species that have lived on Earth have become______, which means that the species has died out. Copyright Pearson Prentice Hall

Copyright Pearson Prentice Hall How Fossils Form How Fossils Form Fossils can be as large as a complete, preserved animals, or as small as a fragment. Most fossils form in_____________________rock. Sedimentary rock forms when exposure to the elements breaks down existing rock into small particles of sand, silt, and clay. Copyright Pearson Prentice Hall

Copyright Pearson Prentice Hall How Fossils Form Fossil Formation __________carries small rock particles to lakes and seas. The fossil record provides evidence about the history of life on Earth. Most fossils are formed in sedimentary rock. Copyright Pearson Prentice Hall

Copyright Pearson Prentice Hall How Fossils Form Dead organisms are buried by layers of sediment, which forms________________. The fossil record provides evidence about the history of life on Earth. Most fossils are formed in sedimentary rock. Copyright Pearson Prentice Hall

Copyright Pearson Prentice Hall How Fossils Form The____________remains may be later discovered and studied. The fossil record provides evidence about the history of life on Earth. Most fossil formed in sedimentary rock. Copyright Pearson Prentice Hall

Interpreting Fossil Evidence Paleontologists determine the age of fossils using relative dating or radioactive dating. Relative Dating In_____________, the age of a fossil is determined by comparing its placement with that of fossils in other layers of rock. Rock layers form in order by age—the oldest on the __________, with more recent layers on_______. Copyright Pearson Prentice Hall

Interpreting Fossil Evidence Relative Dating In relative dating, a paleontologist estimates a fossil’s age in comparison with that of other fossils. Each of these fossils is an index fossil. It enables scientists to date the rock layer in which it is found. Scientists can also use index fossils to date rocks from different locations. Photo credit: l. ©David Hanson/Stone; r. ©CORBIS Copyright Pearson Prentice Hall

Interpreting Fossil Evidence Index fossils are used to compare the relative ages of fossils. An__________is a species that is recognizable and that existed for a short period but had a wide geographic range. Relative dating allows paleontologists to estimate a fossil's age compared with that of other fossils. Copyright Pearson Prentice Hall

Interpreting Fossil Evidence Radioactive Dating  Scientists use radioactive decay to assign an __________________________to rocks. Some elements are radioactive and steadily break down into nonradioactive elements. A_______is the length of time required for half of the radioactive atoms in a sample to decay. Radioactive dating is the use of half-lives to determine the age of a sample. Scientists calculate the age of a sample based on the amount of remaining radioactive________it contains. Copyright Pearson Prentice Hall

Interpreting Fossil Evidence Carbon-___begins to decay when an organism dies. Carbon-___is not radioactive and does not decay. By comparing the amounts of carbon-14 and carbon-12 in a fossil, researchers can determine_______the organism lived. Copyright Pearson Prentice Hall

Interpreting Fossil Evidence Radioactive dating involves measuring the amounts of radioactive isotopes in a sample to determine its actual age. Such measurements enable scientists to determine the absolute age of rocks and the fossils they contain. Copyright Pearson Prentice Hall

Copyright Pearson Prentice Hall Geologic Time Scale Geologic Time Scale Paleontologists use a scale called the geologic time scale to represent evolutionary time. Scientists first developed the geologic time scale by studying rock layers and index fossils worldwide. The basic divisions of the geologic time scale are _____________________________. Copyright Pearson Prentice Hall

Copyright Pearson Prentice Hall Geologic Time Scale Geologic time begins with_______________Time, which covers about _____% of Earth’s history. The basic units of the geologic time scale after Precambrian Time are eras and periods. Each era is divided into periods. Vendian 650–544 Copyright Pearson Prentice Hall

Copyright Pearson Prentice Hall Geologic Time Scale Eras  Geologists divide the time between Precambrian time and the present into three eras: Paleozoic Era Mesozoic Era Cenozoic Era The____________began about____million years ago. Many vertebrates and invertebrates lived during this time. Copyright Pearson Prentice Hall

Copyright Pearson Prentice Hall Geologic Time Scale Permian 290–245 Carboniferous 360–290 Devonian 410–360 The basic units of the geologic time scale after Precambrian Time are eras and periods. Each era is divided into periods. Silurian 440–410 Ordovician 505–440 Cambrian 544–505 Copyright Pearson Prentice Hall

Copyright Pearson Prentice Hall Geologic Time Scale The Mesozoic began about______million years ago. Dinosaurs lived during this time so it is sometimes called the_________________________. ________________began to evolve during this era. Copyright Pearson Prentice Hall

Copyright Pearson Prentice Hall Geologic Time Scale Cretaceous 145–65 Jurassic 208–145 The basic units of the geologic time scale after Precambrian Time are eras and periods. Each era is divided into periods. Triassic 245–208 Copyright Pearson Prentice Hall

Copyright Pearson Prentice Hall Geologic Time Scale The Cenozoic began about___million years ago and continues to the present. Mammals became common during the Cenozoic so it is often called the________________________. Copyright Pearson Prentice Hall

Copyright Pearson Prentice Hall Geologic Time Scale The basic units of the geologic time scale after Precambrian Time are eras and periods. Each era is divided into periods. Copyright Pearson Prentice Hall

Copyright Pearson Prentice Hall Geologic Time Scale Periods  Eras are subdivided into periods, which range in length from tens of millions of years to less than two million years. Many periods are named for places around the world where geologists first discovered the rocks and fossils of that period. Cambrian refers to Cambria, the old Roman name for ______; Jurassic refers to the Jura Mountains in ___________. Copyright Pearson Prentice Hall

Copyright Pearson Prentice Hall Geologic Time Scale Clock Model of Earth’s History First humans Radiation of mammals First land plants First prokaryotes First multicellular organisms Cenozoic Era Mesozoic Era Paleozoic Era Precambrian Time Earth’s history is often compared to a familiar measurement, such as the twelve hours between noon and midnight. In such a comparison, notice that Precambrian Time lasts from noon until after 10:30 pm. First eukaryotes Accumulation of atmospheric oxygen Copyright Pearson Prentice Hall