RAP 3/14 pg. 42 1. How old is the Earth? 2. How do we know? TOPIC: Geologic History 29.1 Fossils 29.2 Relative Time 29.3 Absolute Time Paleontology The study of life that existed in prehistoric times I. Fossils -Preserved remains or traces of once living organisms A. Types 1. Original Remains -preserved in its entirety Ex: Wooly mammoths in ice and soil Insect in amber 2. Replaced remains -Soft parts replaced by minerals Ex: Petrified wood 3. Molds and Casts -Mold: hollow depression (cupcake pan) -Cast: copy of original fossil (cupcake) 4. Trace -indirect evidence of life Ex: trails footprints burrows bite marks Trace fossils And one more example... coprolite 5. Carbonaceous Remains -thin carbon film Ex. Fern print What do we know about this animal? Fossil Formation Fossil formed? 1 2 3 4 5 6 7 Type No Why/Why not? not deep enough Yes Original Remains frozen No too deep No too much pressure Yes replaced remains Yes mould cast Yes trace fused with minerals minerals filled in uplifted Fossil Formation Burying Bodies Making Fossils Who dung it? RAP 1. 2. 3/15 pg. 42 What type of rock do most fossils occur in? What is one method of preserving a fossil? B 3. In the picture, which letter represents the mold? Which letter represents the cast? A II. Relative Time- placing events in the sequence in which they occurred **Does not identify actual dates ** A. Principle of Uniform Processes 1. processes that occurred in past produce same results as today B. Principle of Superposition Deposited sediments are compressed into layers, or strata 1. Oldest layer at bottom; youngest at top Deciphering relative time is like detective work... Who Dunnit?! Someone took the last cookie in the cookie jar last night. The last person to leave is the culprit! Clues: The Butler walks to work The Handyman rides a bike The Cook rides a motorcycle The Maid drives a car The Nephew has a seeing-eye dog Sequences on pg. 44 3 2 1 4 1 2 3 C. Principle of Cross-Cutting Relationships 1. Igneous intrusion is always younger than rock it intrudes 4 2 1 3 5 Gaps in Relative Time D. Unconformity 1. indicates where layers of rock are missing a. Exist because -Lack of deposition -Erosion Example E. Index Fossils 1. Four characteristics a. Easily recognizable b. Abundant c. Widespread in occurrence d. Existed only for a brief period When did I live? Who’s On First?: Period 6 Groups Lab Table 1 Lab Table 4 Shannon Jake Jenny Mitchell Lab Table 2 With Ms. Renwick Devin Group 7 Jordan C. Chrissy Kaitlin Bennett Kaitlyn Bishop Dylan Wimer Chase Brice Lab Table 5 Lab Table 3 Ashtyn Alex Daniel Dylan S. Trey Anandhu Davon Lab Table 6 Josue Yony Ben Luke Group 8 Zach Robert Jordan B. Put it all together... Decoding geologic history... And… RAP 3/19 pg. 42 1. Select the fossil you think would be the best index fossil and explain why. B A D C 2. Put the following events in the correct order. F. Correlation 1. Matching of rock layers from one area to another Practice! unconformity Section 1 Section 2 What AnWhich unconformity islayers the sequence (buried ofsame? rock erosional Of E and F,the which islayer oldest? layers are from surface) oldest is to represented youngest? by the interface between which two layers? III. Absolute Time A. Use ACTUAL dates to order events B. Methods 1. Tree rings 2. Varves- layer of sediment representing summer and winter RAP 3/20 1. 2. pg. 46 What is the difference between relative and absolute time? What type of fossil shows evidence of an organism but not the organism itself? RAP 3/21 pg. 46 **QUIZ ON FOSSILS, Relative and Absolute Time 1. 2. 3. What is the relative age of layer C and D? What two things can cause an unconformity? Which letter to the right represents an unconformity? 3. Radiometric dating Compares ratio of naturally occurring unstable isotope (parent) and its decay products (daughter) Pb Ur Parent = original element Daughter = the product of the decay • Example: uranium-238 decays to lead-206 i. Half-life -Time it takes for half the radioactive atoms to decay =1 half-life =2 half-lives In each half-life, the amount of atoms gets cut in half. =parent =daughter One half-life. =parent =daughter Two half-lives. =parent =daughter Three half-lives. =parent =daughter Four half-lives. =parent =daughter Don’t worry about the last atom. You start with so many trillions that you never really get there. (It will just decay and then they’re all gone.) =parent =daughter About how many students would have had to sit down if we started with twice as many students? What about if we only had half as many in this class? What does that tell you about how the quantity of "radioactive isotopes" affects the number that decay? Can you predict which of you is going to be the first to sit down? Why or why not? Keys to radioactivity **Decay at constant rates regardless of time or climate** **Decay begins as soon as rock crystallizes or organism dies** **Ratio of amount of radioactive element left to the amount of stable product is used to determine the absolute age** RAP 1. 3/22 pg. 46 What is the definition of a half life? Since you don’t know how many atoms you started with, a ratio between parent to daughter will tell you how many half-lives have gone by. 100% parent 0% daughter 0 half lives One half-life. 50% parent 50% daughter 1 half-life Two half-lives. 25% parent 75% daughter 2 half-lives Three half-lives. 12.5% parent 87.5% daughter 3 half-lives Four half-lives. 6.25% parent 93.75% daughter 4 half-lives Half-lives range from a fraction of a second to billions of years • Protactinium-234 has • half-life of ~1 min Uranium-238 has half-life of 4.5 by Radiocarbon limitations Only for once living organisms Half-life=5730 years meaning the limit to dating is about 70,000 years 17190 RAP 3/14 pg. 45 1. 2. 3. RAP 3/13 pg. 43 1. 2. 3. What is a half life? You find a piece of wood and use carbon dating to determine the age. The ratio of parent to daughter is 1:1. How many half lives have passed? How do varves help geologists understand the past? Quiz Relative Time, Fossils and Absolute Time Web quest Let’s get a little more complicated…