Hard Parts of Organisms: Bones Shells Hard Parts of Insects Woody Material (trunks) Fossils provide evidence of how life has changed over time.

Similar documents
FOSSILS. Book G Chapter 4 Section 1

Section 1 Darwin s theory

Chapter: Clues to Earth s Past

A Trip Through Geologic Time

The History of Life. Section 3-2. The Fossil Record

Module 9: Earth s History Topic 4 Content: Formation of Fossils Notes

Fossils. Who studies fossils? How do fossils form? Fossils are the preserved remains or traces of living things.

NOTES 1. Fossils. The BIG Idea Rocks, fossils, and other types of natural evidence tell Earth s story.

Name Class Date. What are fossils? How are fossils formed? What can fossils tell us about the history of life on earth?

1 Looking at Fossils. What are fossils? How are fossils formed? What can fossils tell us about the history of life on earth?

Body Fossils are preserved remains where an organism's body tissue, or parts thereof, become fossilized in an altered or actual state.

Lecture Title ( Fossils ) & Date. Main Ideas/Lecture Topics/Questions. Big Ideas or Chunking the Lecture

Tales of the Past. Source: Sci-ber Text with the Utah State Office of Education

There are actually 5 processes

What we will learn about Fossils?

Do Now HW due Friday 9/30

Fossils. Presented by Kesler Science

Earth s Changing Surface Chapter 4

A fossil is the preserved remains of a once-living organism.

Looking at Fossils. Fossilized Organisms. Fossils in Rocks. Fossils in Amber

Evolution Evidence of Change

Fossils and EH LT 1 and 2

Directed Reading. Section: The Fossil Record. Skills Worksheet

7.1 Life in the past. Fossil formation

NOTES: The Fossil Record and Geologic Time

Paleo Lab #5 - Fossilization and Fossil Identification

Geo 302D: Age of Dinosaurs. LAB 3: Fossils and Fossilization

Program Objectives. Fossil Casting 1. Science: Building with a Variety of Materials

Lesson Checkpoint: Name one animal that you know is extinct.

Chapter 6. Life on Earth: What do Fossils Reveal?

Hot Sync. Materials Needed Today

Final Revision G8 Biology ( ) Multiple Choice Identify the choice that best completes the statement or answers the question.

Studying The Past. II. Why Do We Study Fossils Found in Rocks?

FoSSil Puzzler (1 Hour)

The Significance of the Fossil Record ( Susan Matthews and Graeme Lindbeck)

Clues to Earth s Past. Fossils and Geologic Time

The Environment and Change Over Time

Objectives: Define Relative Age, Absolute Age

Fossils. Name Date Class. A Trip Through Geologic Time Section Summary

Online Fossil Lab Fossil Formation How Fossils Form 1. Describe the process in which fossils form.

Spilsbu Engag e Literacy Fo ssil Hunters

Studying The Past. II. Why Do We Study Fossils Found in Rocks?

Evidence for Evolution Notes:

11/5/2015. Creating a Time Scale - Relative Dating Principles. Creating a Time Scale - Relative Dating Principles. The Geologic Time Scale

Marquette County in the ICE AGE and before

Studying The Past. Why Do We Study Fossils Found in Rocks?

Mineral - a naturally occurring, inorganic solid that has a crystalline structure and a definite chemical composition For the Love of God

THE PRESERVATION OF FOSSILS

Fun with Fossils. Ask a Fossil

PALEONTOLOGY - the study of the history of life as reflected in the fossil record

5 total items = 10 points

3rd-4th Grade. The Fossilization Process Flip Chart

Relative aging, fossils, natural disasters

and Fuels OSSIIS Vocabulary Process Skill

Geologic Time. What is Age? Absolute Age The number of years since the rock formed. (150 million years old, 10 thousand years old.

Unit 2 Lesson 1 Geologic Change over Time. Copyright Houghton Mifflin Harcourt Publishing Company

Digging into the Past Pre-Visit Materials

Chapter 7- Changes Over Time. Section 2 Evidence of Evolution

Ecology and Paleoecology. A brief review

Focus on Fossils. Third - Fifth. Earth Science TEKS. Vocabulary

Directed Reading. Section: Determining Relative Age. conclusions? UNIFORMITARIANISM. geology? of Earth? Skills Worksheet

A Trip Through Geologic Time

Fossils & The Geologic Time Scale

The Fossil Record. CELLS and HEREDITY, CHAPTER 5, SECTION 3, PAGES 155 to 163

Determining the age of fossils

Name Class Date. 1. In your own words, write a definition for each of the following terms: superposition, geologic column, and geologic time scale.

Topic 7: Historical Geology

Processing Activities

What Can We Learn From The Rock Record?

Clues to Earth s Past

Unit 9 Lesson 3 How Can Rocks Be Classified? Copyright Houghton Mifflin Harcourt Publishing Company

Rock cycle diagram. Relative dating. Placing rocks and events in proper sequence of formation Deciphering Earth s history from clues in the rocks

What happened Before. reflect

My Goal 1. The Dinosaur Who Lived In My Backyard. Dinosaur Tracking. Dinosaur Fossils Why Did the Dinosaurs. Monster Tracks Let s Go

Fossils: evidence of past life

Name Test Date Hour. forms that lived only during certain periods. abundant and widespread geographically. changes to the surface of Earth.

Common Fossils in Pennsylvania

test date Name date Review: Geologic Time & Geologic Procesess-: You will record 1-38 answers on the scan sheet! These are worth 1.

Your quiz will have some multiple-choice questions, matching, fill-in-the-blank questions, and short answer. To review, study DQs, notes from class,

HISTORICAL GEOLOGY. Relative & Absolute age, fossils and geologic time

8. GEOLOGIC TIME LAST NAME (ALL IN CAPS): FIRST NAME: Instructions

Fossils, Fossils Everywhere

Integrated Science. Geologic Time Notes. Section 1: Geologic Time

Presented to grade 5-7; appropriate for grades 1-9 with age appropriate modifications Duration of lesson: 1 hour Notes:

FOSSIL "FUN"DAMENTALS

(c) 4 1. correct derivation of children s genotypes 1. identification of children with cystic fibrosis (dd) 1

Darwin s Conclusions. The Theory of Evolution

Remains or traces of prehistoric life

CHAPTER 2: EVOLUTION- CHANGE ACROSS TIME. Examining the evidence of change across time.

THE HISTORY OF THE EARTH EARTH SCIENCE

Rock cycle diagram. Principle of Original Horizontality. Sediment is deposited horizontally

Amber is a solid, glass-like material. Amber is formed from a thick, sticky liquid which oozes out of pine trees.

6/30/2018. Geologic Time. Earth, Chapter 9 Chapter 9 Geologic Time

Lesson Eight The Meeting of the Dinosaurs Evidence Given by Dinosaur Footprints

Station 8 Station Station 9 Station Station 10 Station Sample 9 Station

Lecture Outline Friday Feb. 21 Wednesday Feb. 28, 2018

1 The origin of life (pp )

LECTURE 2: Taphonomy and Time

THIRD GRADE PAST LIFE

FOSSILS Uncovering Clues to the Earth s Past

Transcription:

PLEASE, PICK UP OUTLINE FROM THE FRONT TABLE! *recommend adding the extra stuff to the notes Fossus - means to dig up Fossils are preserved remains or traces of living things. Most fossils form when living things die and are buried by sediments. The sediments slowly harden into rock and preserve the shapes of the organisms. Paleontologists are scientists who study fossils. Hard Parts of Organisms: Bones Shells Hard Parts of Insects Woody Material (trunks) Soft or Easily Decayed Parts of Organisms: Internal Organs Skin Hair Feathers Leaves Almost exclusively in sedimentary rocks Heat of melting or metamorphism would destroy almost every type of fossil Rare Exceptions: Some fossils in low-grade metamorphic rocks Trees buried by lava flow To be preserved, organisms have to be: Buried rapidly after death Preserved from decay Fossils provide evidence of how life has changed over time. Fossils help scientists infer how Earth s surface has changed. Fossils are clues to what past environments were like. 1

The fossil record provides evidence about the history of life on Earth. The fossil record also shows that different groups of organisms have changed over time. Evolution is the gradual change in living things over long periods of time. Extinct means an organism no longer exists and will never again live on Earth. Petrified fossils Molds and casts Carbon films Trace fossils Preserved remains No need to write Fossils in which minerals replace all or part of an organism. How does this happen? Water rich in dissolved minerals seeped into spaces, evaporated, leaving the hardened minerals behind. Example petrified wood Permineralization Mineral matter from percolating ground waters is added to pores and cavities in bones, shell, teeth, etc. The original material is still present with new mineral matter added to the void spaces. Many dinosaur bones are preserved by this method. 2

Replacement Original hard parts are replaced with new mineral matter of a different composition than the original Silica (SiO 2 ), iron oxide (Fe 2 O 3 ), and calcium carbonate (CaCO 3 ) are common replacement minerals Many dinosaur bones are both permineralized and partially replaced. Recrystallization The original mineral crystals grow larger and fill most of the void space. More common in invertebrate fossils (clams, brachiopods, gastropods, etc.) than in vertebrate fossils. Usually destroys or partially obscures the original microstructure of the skeletal material. Most common type of fossil. Both copy the shape of the organism. A mold is a hollow area of sediment in the shape of the organism. A cast is a copy of the shape of an organism. 3

Mold Natural casts of shelled invertebrates Cast Mold Carbon film is an extremely thin coating of carbon on rock. How does this happen? All organisms are made of carbon. When they are buried, the materials that make up the organism evaporate. These gases escape leaving carbon behind. Carbon film Trace fossils provide evidence of the activities of ancient organisms. Examples A footprint provides clues about the size and behavior, the speed, how many legs it walked on, if lived alone or with others. A trail or burrow can give clues about the size and shape of the organism, Worm trails where it lived, and how it obtained food. 4

A dinosaur footprint Dinosaur Valley State Park Dinosaur tracks 113 mya Preservation of remains with little or no change. Preservation material; Tar The sticky oil that seeps from Earth s surface. Tar soaks into the organisms bones, preserving the bones from decay. Amber The hardened resin, or sap, of trees. The amber seals the organism from the air protecting it from decay. Ice 49 million years old frog 25 million year old flying ants 10,000 years old 5

Is Dinosaur bone Mammoth frozen in ice Dinosaur tracks Ancient shark tooth Egyptian mummy Dinosaur excrement Roman Skull Insect trapped in amber Petrified wood Cast of a shell in rock Leaf imprint in rock Piece of dinosaur egg shell Is not Sedimentary rock Air trapped in ice Prehistoric cave drawing Prehistoric tool Hardened lava A 1 byo rock Old carved gravestone Ancient arrowhead 6