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Chapter 17 The History of Life. Section 17-1 The Fossil Record. Fossils & Ancient Life. Paleontologists Scientists Who Study Fossils Infer What Past Life Looked Like What They Ate & What Ate Them Behavior Environment They Lived In. What They Looked Like. What They Ate.
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Chapter 17The History of Life Section 17-1 The Fossil Record
Fossils & Ancient Life • Paleontologists • Scientists Who Study Fossils • Infer What Past Life • Looked Like • What They Ate & What Ate Them • Behavior • Environment They Lived In
Behavior & Environment 3.6 MYA
Fossils & Ancient Life • Fossil Record • Organization Of Fossils From Oldest To Newest Including Supporting Information Of Other Life Forms In Their Environment
Fossils & Ancient Life Key Concept The Fossil Record Provides Evidence About The History Of Life On Earth. It Also Shows How Different Groups of Organisms Have Changed Over Time.
Fossils & Ancient Life • Each Fossil Is Found Only In It’s Particular Time Period or Layer • A Kind Of Fossil Clock • Of All The Life Forms That Have Ever Lived On Earth ----- • 99% Are Extinct • No Longer Alive
How Fossils Are Formed • Most Form In Sedimentary Rock • Plants & Animals Die In A Water Environment And Are Covered With Silt • Others Covered With Fine Sand or Volcanic Ash • Compressed Into Rock
How Fossils Are Formed • Organic Materials Are Replaced By Minerals • Quality Of Preservation Varies • Fossils Include: • Bones • Eggs • Footprints • Skin Impressions, etc.
Interpreting Fossil Evidence • Fossils Are Released By • Tectonic Forces • Erosion • Mining • Construction
Interpreting Fossil Evidence • Most Fossils Disarticulated • Predation • Scavengers • Rot • Catastrophic Events May Bury & Preserve Whole Animals and/or Ecosystems
Dating Fossils Two Types of Dating • Relative Dating Organizes Fossils By Order (1st, 2nd, 3rd, etc.) Tells You Which Organisms Lived In What Order Does Not Give You Actual Years • Absolute Dating Gives You Age In Years Before Present e.g. 150 Million Years Ago
Relative Dating • The Age of a Fossil Is Determined By Comparing Its Placement With Other Fossils In Other Layers Of Sedimentary Rock • Allows Comparison Of Layers World Wide
Relative Dating • Index Fossils • Easily Recognized • Existed For A Short Period • Wide Geographic Distribution • Does Not Give Absolute Age
Relative Dating Key Concept: Relative Dating Allows Paleontologists To Estimate A Fossils Age Compared With That Of Other Fossils
Radioactive Dating Uses The Half Lives Of Certain Radioactive Isotopes In Igneous Rocks To Calculate The Age Of A Fossil Half Life The Length Of Time Required For Half Of The Radioactive Atoms In A Sample To Decay
Radioactive Dating Key Concept: In Radioactive Dating, Scientists Calculate The Age Of A Sample Based On The Amount Of Remaining Radioactive Isotopes It Contains
Radioactive Dating Different Radioactive Elements Have Different “tick rates” Carbon-14 Half-life = 5,730 years Decays to Nitrogen-14 Useful Back 60,000 years
Geologic Time Scale Developed By Paleontologists To Classify Geologic And Biologic Events Rock Layers Fossils Present
Chapter 17The History of Life Section 17- 4 Patterns of Evolution
Macroevolution • Large Scale Evolutionary Changes That Take Place Over Long Periods of Time
Macroevolution Key Concept: There Are Six Important Patterns of Macroevolution: • Mass Extinctions • Adaptive Radiation • Convergent Evolution • Coevolution • Punctuated Equilibrium • Developmental Gene Changes
Mass Extinctions • Extinction • Occurs Constantly • 99% Earths Life Forms Extinct • Mass Extinctions • Wipe Out Ecosystems • Disrupt Energy Flow • Collapse Food Webs
Mass Extinctions • Causes? • Asteroids? • Volcanic/Geologic Activity? • Effects • Habitats Left Unoccupied • Ecological Opportunity • Evolution Explosion
Adaptive Radiation • Single Species or Small Group of Species Evolve Into Several Different Forms That Live In Different Ways • Darwin’s Finches • Age of Reptiles • Age of Mammals
Convergent Evolution • Unrelated Species That Look And Act Remarkably Similar To Each Other But Are Not Related: • Fish - Whales • Dolphins - Sharks • Seals - Penguins
Coevolution • The Process By Which Two Species Evolve In Response To Changes In Each Other • Figs & Wasp • Yucca & Bats • Orchids & Moths
Punctuated Equilibrium • Evolution Is Sometimes Gradual & Slow (Gradualism, Darwin) • Horseshoe Crabs • Sharks • Cockroaches • BUT When Ecological Equilibrium Is Upset, Evolution Can Become Quite “Rapid
Punctuated Equilibrium • Occurs Due To • Small Populations Become Reproductively Isolated • Mass Extinctions
Punctuated Equilibrium • Brief Periods of Rapid Evolutionary Change That Interrupt Long Periods of Gradual Evolution • Still Controversial
Developmental Genes & Body Plans Small Changes In Timing of Genetic Control During Embryonic Development, Make Big Changes In The Resulting Organism
Click on the links below • Evolution videos: http://www.pbs.org/wgbh/evolution/educators/teachstuds/svideos.html • Fossil article: http://news.bbc.co.uk/2/hi/science/nature/4879672.stm • Games: http://www.abc.net.au/beasts/fossilfun/ • http://www.ucmp.berkeley.edu/education/explorations/tours/fossil/index.html • http://www.abc.net.au/beasts/fossilfun/makingfossils/default.htm