J OURNAL #26 Describe carbon dating and how it used to determine the numerical age of a rock layers.

Slides:



Advertisements
Similar presentations
The remains or evidence of a
Advertisements

Earth’s Past.
Fossils Mr. Skirbst Earth Science Topic 24. Fossils The preserved remains or evidence of a living thing.
A Little Bit of History… The history of geologic time begins with the human interest in mining. Interests in rock units began to flourish with commercial.
Clues from Fossils Fossils give us information about living things in the past.
FOSSILS.
The study of ancient life!
Chapter 8.  itarianism  A principle that geologic processes that occurred in the past can be explained by current geologic processes.  Volcanism and.
Rock Record Spring 2013.
By: Colby Lacks.  Without such fossils, scientists would know very little about the history of life on earth.  The answers we get from rocks often cause.
The History of Earth.
Relative dating superposition Clues in Igneous rock Index Fossils
Fossils.
FOSSILS. OVERVIEW Explain what fossils are and how most fossils form. Explain what fossils are and how most fossils form. Describe what fossils tell about.
IN: How do you think fossils form?
Chapter 3 Section 4 Looking at Fossils.
The Fossil Record Def: the traces or remains of animals or plants from a previous geologic time.
Quick-write What is a fossil?. Fossils Fossils are remains, or evidence, of living organisms that have been preserved over millions of years.
How do we know that there was life millions of years ago??
A Trip through Geologic Time:
{ Looking at Fossils Chapter 2.1.  If the half-life of Uranium-232 is 70 years, how many half lives will it take for 10g to be reduced to 1.25g?  Mercury-197.
DO NOW Geologic Time. DO NOW 1. Superposition –C–C 2. Absolute dating –B–B 3. Relative dating –A–A 4. Geologic column –D–D A. Finding if a rock layer.
Fossils.
Define: Fossil Carbon film (carbonization) Petrified fossil (mineralization) Solid Cast Mold Trace Fossil.
Fossils Ch. 13 Section1. Fossils  Remains, imprints, or traces of prehistoric organisms  Scientists who study fossils are paleontologists.  Fossils.
THIS IS With Host... Your Relative Dating Absolute Dating Radiometric Dating Fossils Vocabulary 1 Vocabulary 2.
The Rock Record Chapter 8 James Hutton  18 th Century Scottish physician  Observed geologic changes that took place on his farm  By studying the present,
Today’s Objective (learning goal) To identify how fossils are used as evidence in changes within a species.
Inside the Restless Earth Chapter 3 Section 4
WHAT’S IN THE ROCKS!. Bell Work If you were to put the following events in to a time sequence of first to last, how would you do it? What else would you.
Welcome to Class How do we determine the age of something?
Earth’s History Chapters 29 & 30. Paleontology is the study of the life that existed in Prehistoric times. Traces of ancient life (fossils) are the basis.
Begin Earth’s Past 3/28/12 What do you know about Fossils?
Fossils and the Rock Record
Fossils …old dead stuff… How old is old?
Fossils and the Rock Record The Rock Record  Rocks record geological events and changing life forms of the past  Planet Earth was formed 4.6 billion.
Fossils. Essential Question How can fossils be used to help explain what happened in the past?
The Rock Record Section 3 Section 3: The Fossil Record Preview Objectives Interpreting the Fossil Record Fossilization Types of Fossils Index Fossils Index.
What Era and Period did it come from?. Describes timing and relationships between events that have occurred during the history of the Earth Divided into.
The Fossil Record. 1. Fossils are the remains of organisms that lived in a previous geologic time. 2. The study of these fossils is called paleontology.
Earth’s Past. Determining Relative age Relative age – the age of the object in relation to the age of other objects – No actual age in years given Law.
Looking at Fossils Chapter 3 Section 4 p Vocabulary:
Chapter 15, Section 4 Vocabulary Pages fossil The remains or physical evidence of an organism preserved by geological processes Coprolite (Preserved.
Fossils are the remains, imprints, or traces of prehistoric organisms. Fossils have helped determine approximately when life first appeared, when plants.
REMAINS OR TRACES OF PREHISTORIC LIFE Inclusions found in sediment & sedimentary rocks A Tool for interpreting the geologic past Important time indicators.
Created By Gina Wike. Fossils A fossil is evidence such as remains, imprints or traces of once living organisms preserved in rock A fossil is evidence.
PALEONTOLOGY. Paleontology—The Study of Past Life The history of the Earth would be incomplete without knowledge of the organisms that have inhabited.
Topic: Fossils PSSA: A / S8.D.1.1. Objective: TLW explain what a fossil is and compare different ways living things can be fossilized. TLW explain.
Chapter 8. Fossil - the preserved remains or traces of a living thing. Mold - the hollow space that is left. Cast - forms when dissolved minerals fill.
Chapter 15 Section 4 Fossils. Fossil Preservation Five main ways fossils are preserved: o Rocks o Amber o Petrifaction o Asphalt o Ice.
Fossils The remains or imprints of living things of the past found in Sedimentary rocks or turned into rocks.
Methods of Fossilization
Fossils!.
Chapter 8 The Rock Record.
Fossils.
Specific conditions are needed for fossilization.
PALEONTOLOGY.
Fossil Records – Clues to the Past
Fossils!.
Fossil Notes 8.E.2 Understand the history of Earth and its life forms based on evidence of change recorded in fossil records and landforms.
The Fossil Record
FOSSILS.
What is a fossil? What do fossils tell us?
The fossil record Chapter 8 section 3.
Fossil Types and Conditions
Chapter 8 The Rock Record
Chapter F3 Fossilized Organisms
Looking at Fossils Chapter 3 Section 4 p Vocabulary:
Fossils Ch. 13 Section1.
The Fossil Record 16-1.
Presentation transcript:

J OURNAL #26 Describe carbon dating and how it used to determine the numerical age of a rock layers.

The Fossil Record

L EARNING G OAL Today we will describe 4 ways in which entire organisms can be preserved as fossils and learn 5 examples of fossilized traces of organisms

T HE F OSSIL R ECORD Fossils- the remains of animals or plants that lived in a previous geologic time Paleontology- the study of fossils. Almost all fossils are discovered in sedimentary rock. The sediments that cover the fossils slow or stop the process of decay and protect the dead body from damage

T HE F OSSIL R ECORD The fossil record provides information about the geologic history of Earth. These dead organisms have changed throughout the geologic past and provide cluse to the environmental changes that occurred in Earth’s past. Example: marine animal fossils have been discovered in areas far from any ocean. This means that the area was previously covered by ocean in the past.

F OSSILIZATION Normally, dead plants and animals are eaten by other animals or decomposed by bacteria. If left unprotected, even the hard parts such as bones decay and leave no trace of the organism. Only dead organisms that buried quickly can become fossils. There are many ways fossils form.

H OW FOSSILS FORM : Mummification Amber (tree sap) Tar Seeps Freezing Petrification Imprints Molds and Casts Coprolites Gastroliths

T YPES OF F OSSILS Sometimes, no part of the original organism survives in fossil form. Trace fossils- a fossilized mark that formed in sedimentary rock by the movement of an animal on or within soft sediment. A trace fossil such as a footprint is an important clue to the animal’s appearance and activities.

T YPES OF F OSSILS Index fossils- a fossil that is used to establish the age of rock layers because it is distinct, abundant and widespread and existed for only a short span of geologic time. It must be present in rocks scattered over a large region It must have features that clearly distinguish it form other fossils. The organisms from which the fossil formed must have lived during a short span of geologic time. The fossil must occur in fairly large numbers within the rock layers.

L ET ’ S R EVIEW : What is a fossil? Name 4 ways in which an entire organism can be preserved as a fossil. The trace or remains of an organism that lived long ago, most commonly preserved in sedimentary rock

L ET ’ S R EVIEW : What is paleontology? What are trace fossils? How do trace fossils help date sedimentary rock layers? The study of fossils A fossilized mark that formed by the movement of an animal on or within soft sediment. They occur only in rock layers of a particular geologic age