[null, null, {"document_url": "http://slideplayer.com/slide/1588977/", "unformatted_src": "/5/1507129/big_thumb.jpg", "src": "https://slideplayer.com/5/1507129/big_thumb.jpg", "formatted_filename": "big thumb", "alt_text": "The Geological Time Scale"}, null, {"document_url": "http://slideplayer.com/slide/1588977/", "unformatted_src": "/5/1507725/big_thumb.jpg", "src": "https://slideplayer.com/5/1507725/big_thumb.jpg", "formatted_filename": "big thumb", "alt_text": "Add this unit to your Table of contents!"}, null, {"document_url": "http://slideplayer.com/slide/1588977/", "unformatted_src": "/5/1588546/big_thumb.jpg", "src": "https://slideplayer.com/5/1588546/big_thumb.jpg", "formatted_filename": "big thumb", "alt_text": "Mr. Karns Biology Fossils."}, null, {"document_url": "http://slideplayer.com/slide/1588977/", "unformatted_src": "/5/1588581/big_thumb.jpg", "src": "https://slideplayer.com/5/1588581/big_thumb.jpg", "formatted_filename": "big thumb", "alt_text": "Outine 17-1: The Fossil Record"}, null, {"document_url": "http://slideplayer.com/slide/1588977/", "unformatted_src": "/5/1589183/big_thumb.jpg", "src": "https://slideplayer.com/5/1589183/big_thumb.jpg", "formatted_filename": "big thumb", "alt_text": "CHAPTER 14 HISTORY OF THE EARTH"}, null, {"document_url": "http://slideplayer.com/slide/1588977/", "unformatted_src": "/5/1598023/big_thumb.jpg", "src": "https://slideplayer.com/5/1598023/big_thumb.jpg", "formatted_filename": "big thumb", "alt_text": "Test Review Test on Thursday!!!! 1. The most powerful Mechanical weathering force is frost wedging. 2."}, null, {"document_url": "http://slideplayer.com/slide/1588977/", "unformatted_src": "/10/2758329/big_thumb.jpg", "src": "https://slideplayer.com/10/2758329/big_thumb.jpg", "formatted_filename": "big thumb", "alt_text": "Chapter 15:5 Geologic Time Scale."}, null, {"document_url": "http://slideplayer.com/slide/1588977/", "unformatted_src": "/14/4449535/big_thumb.jpg", "src": "https://slideplayer.com/14/4449535/big_thumb.jpg", "formatted_filename": "big thumb", "alt_text": "Life and Geologic Time."}, null, {"document_url": "http://slideplayer.com/slide/1588977/", "unformatted_src": "/14/4449540/big_thumb.jpg", "src": "https://slideplayer.com/14/4449540/big_thumb.jpg", "formatted_filename": "big thumb", "alt_text": "The Precambrian Era The Precambrian Era covers seven-eighths of Earth\u2019s history although paleontologists have found very few fossils of Precambrian organisms."}, null, {"document_url": "http://slideplayer.com/slide/1588977/", "unformatted_src": "/14/4449560/big_thumb.jpg", "src": "https://slideplayer.com/14/4449560/big_thumb.jpg", "formatted_filename": "big thumb", "alt_text": "The geologic time scale shows Earth\u2019s past."}, null, {"document_url": "http://slideplayer.com/slide/1588977/", "unformatted_src": "/14/4449566/big_thumb.jpg", "src": "https://slideplayer.com/14/4449566/big_thumb.jpg", "formatted_filename": "big thumb", "alt_text": "The Geologic Time Scale. Geologic Time Scale : Scientists have formed a chronology of Earth\u2019s history based on evidence from the Earth\u2019s rocks and fossils."}, null, {"document_url": "http://slideplayer.com/slide/1588977/", "unformatted_src": "/14/4449871/big_thumb.jpg", "src": "https://slideplayer.com/14/4449871/big_thumb.jpg", "formatted_filename": "big thumb", "alt_text": "Unit 2 Review: History of Life on Earth"}, null, {"document_url": "http://slideplayer.com/slide/1588977/", "unformatted_src": "/14/4449927/big_thumb.jpg", "src": "https://slideplayer.com/14/4449927/big_thumb.jpg", "formatted_filename": "big thumb", "alt_text": "The Geologic Time Scale"}, null, {"document_url": "http://slideplayer.com/slide/1588977/", "unformatted_src": "/14/4449952/big_thumb.jpg", "src": "https://slideplayer.com/14/4449952/big_thumb.jpg", "formatted_filename": "big thumb", "alt_text": "Geologic Time Scale."}, null, {"document_url": "http://slideplayer.com/slide/1588977/", "unformatted_src": "/16/4891819/big_thumb.jpg", "src": "https://slideplayer.com/16/4891819/big_thumb.jpg", "formatted_filename": "big thumb", "alt_text": "CHAPTER 4 Geologic Time."}, null, {"document_url": "http://slideplayer.com/slide/1588977/", "unformatted_src": "/20/6041220/big_thumb.jpg", "src": "https://slideplayer.com/20/6041220/big_thumb.jpg", "formatted_filename": "big thumb", "alt_text": "Events in Your Life \uf09e ___When you started second grade \uf09e ___When you were born \uf09e ___ When you started kindergarten \uf09e ___When you learned to ride a bike."}, null, {"document_url": "http://slideplayer.com/slide/1588977/", "unformatted_src": "/18/6164506/big_thumb.jpg", "src": "https://slideplayer.com/18/6164506/big_thumb.jpg", "formatted_filename": "big thumb", "alt_text": "Geologic Time. Events in Your Life ___When you started second grade ___When you were born ___ When you started kindergarten ___When you learned to ride."}, null, {"document_url": "http://slideplayer.com/slide/1588977/", "unformatted_src": "/23/6676748/big_thumb.jpg", "src": "https://slideplayer.com/23/6676748/big_thumb.jpg", "formatted_filename": "big thumb", "alt_text": "Copyright \u00a9 2014 All rights reserved, Government of Newfoundland and Labrador Earth Systems 3209 Unit: 2 Historical Geology Reference: Chapters 6, 8; Appendix."}, null, {"document_url": "http://slideplayer.com/slide/1588977/", "unformatted_src": "/24/7360515/big_thumb.jpg", "src": "https://slideplayer.com/24/7360515/big_thumb.jpg", "formatted_filename": "big thumb", "alt_text": "Geologic Time Scale (Earth is 4.6 billion years old)"}, null, {"document_url": "http://slideplayer.com/slide/1588977/", "unformatted_src": "/24/7360517/big_thumb.jpg", "src": "https://slideplayer.com/24/7360517/big_thumb.jpg", "formatted_filename": "big thumb", "alt_text": "End Show Slide 1 of 30 Copyright Pearson Prentice Hall Biology."}, null, null]
How do we know when things happened?

Published byDamien Weekly Modified over 4 years ago


Presentation on theme: "How do we know when things happened?"— Presentation transcript:

1 How do we know when things happened?
Geologic time How do we know when things happened?

2 Goals Students will write about, talk about, and understand the principles of relative dating and original horizontality(7A) Students will write about, talk about, and understand the principle of Radiometric dating 7B) Students will write about, talk about, and understand the scale and scope of the Geologic time scale

3 Part 1 With a partner of your choosing, answer the questions from the end of the packet I hand out. Alternate answering the questions on you answer page. Skip questions 1 and 15. Match vocabulary words to the questions to help find answers if you are having trouble with one. 5. 266 17, , 281

4 Events in Your Life ___When you started second grade
Construct a timeline of the important events in your life. Be sure to include all of the events listed below and any other events you feel are important. Your timeline should be constructed TWO ways: Numerical Order (use actual dates) Sequential Order (most recent at top) ___When you started second grade ___When you were born ___ When you started kindergarten ___When you learned to ride a bike. ___ When you learned to walk. ___ When you learned to read. ___ When you lost your first tooth. ___ Today’s date.


6 What is the Earth’s time scale?
The Geological time scale is a record of the life forms and geological events in Earth’s history. Scientists developed the time scale by studying rock layers and fossils world wide. Radioactive dating helped determine the absolute divisions in the time scale.

7 Divisions of Geologic Time
Eras are subdivided into periods...periods are subdivided into epochs. Era Period Epoch E + P = EP

8 Divisions of Geologic Time
Geological time begins with Precambrian Time. Precambrian time covers approximately 88% of Earth’s history.


10 FOUR Eras… PRE-CAMBRIAN – 88% of earth’s history
Paleozoic (ancient life) 544 million years ago…lasted 300 million yrs Mesozoic (middle life) 245 million years ago…lasted 180 million yrs Cenozoic (recent life) 65 million years ago…continues through present day

11 Today… Today we are in the Holocene Epoch of the Quaternary Period of the Cenozoic Era. Which unit is the largest? Which unit is the smallest?


13 Paleozoic Era (Ancient Life)
The Cambrian period is the 1st period of the Paleozoic Era. “Age of the Trilobites” Explosion of life in the oceans began during this era. Most of the continents were covered in warm, shallow seas. Invertebrates were dominant - Trilobites Fish emerged during this time Fish led to the arrival of amphibians The end of the Paleozoic era is called the “Age of Amphibians” Early land plants including mosses, ferns and cone-bearing plants. The early coal forming forests were also formed during this time.

14 Trilobites Lived in Earth’s ancient seas
Extinct before the dinosaurs came into existence Cambrian Period is know as the “Age of the Trilobites”

15 Paleozoic Era Much of the limestone quarried for building and industrial purposes, as well as the coal deposits of western Europe and the eastern United States, were formed during the Paleozoic. The Cambrian (beginning) opened with the breakup of the world-continent Rodinia and closed with the formation of Pangaea, as the Earth's continents came together once again. This event is thought to have caused the climate changes that led to mass extinction event. The Appalachian mountains were formed during this time.

16 Paleozoic Era At the end of the Paleozoic, the largest mass extinction in history wiped out approximately 90% of all marine animal species and 70% of land animals. Possible causes of this Mass Extinction Event Lowering of sea levels when the continents were rejoined as Pangaea (convergent boundary) Increased volcanic activity (ash and dust) Climate changes – cooler climate

17 Brachiopods Marine animals that resemble clams.

18 Early Fish Early fish did not have jaws.
Some species of sharks were in existence at this time.

19 Frilled Shark that was found in Japan in January 2007
Frilled Shark that was found in Japan in January This shark was considered a “living fossil”

20 Early Land Plants Mosses Cone bearing plants Ferns

21 Mesozoic Era – Middle Life
At the beginning of this era the continents were joined as Pangaea. Pangaea broke up around the middle of this era. Reptiles became the most abundant animals because of their ability to adapt to the drier climate of the Mesozoic Era. Skin maintains body fluids Embryos live in shells

22 Mesozoic Era Dinosaurs were also very active in this era.
First small dinosaurs appeared in the Triassic Period. Larger and more abundant dinosaurs appeared in the Jurassic Period. Small mammals and birds also appeared during this era. The mammals were small, warm-blooded animals. Hair covering their bodies. These characteristics help them survive in changing environments.




26 Mesozoic Era The main plant life of this time were Gymnosperms or plants that produce seeds, but no flowers. Pine Trees Flowering plants appeared during the END of this era.

27 Mesozoic Era This era ended with a mass extinction event about 65 million years ago. Many groups of animals, including the dinosaurs disappeared suddenly at this time. Many scientists believe that this event was caused by a comet or asteroid colliding with the Earth.





32 Mesozoic Era – Mass Extinction Event
Asteroid or Comet collides with Earth. Huge cloud of smoke and dust fills the air Blocks out sunlight Plants die Animals that eat plants die Animals that eat plant-eaters die. However, not all forms of life died during this event. Many animals that you see today are descendants from the survivors of this extinction event.

33 Dinosaurs

34 Mesozoic Reptiles

35 Mesozoic Mammals


37 Mesozoic Plants Flowering plants evolved towards the end of the Mesozoic Era.

38 Cenozoic Era – Recent Life
Began about 65 million years ago and continues today!!!!! Climate was warm and mild. Marine animals such as whales and dolphins evolved. Mammals began to increase and evolve adaptations that allowed them to live in many different environments – land, air and the sea. Grasses increased and provided a food source for grazing animals Many mountain ranges formed during the Cenozoic Era Alps in Europe and Himalayas in India; Rocky Mountains in the USA

39 Cenozoic Era Growth of these mountains may have helped to cool down the climate Ice Ages occurred late in the Cenozoic Era (Quaternary Period). As the climate changed, the animals had to adapt to the rise and fall of the oceans caused by melting glaciers. This era is sometimes called the “Age of Mammals”

40 Cenozoic Era Marine animal examples: Land animal examples:
Algae, Mollusks, Fish and Mammals Land animal examples: Bats, Cats, Dogs, Cattle and Humans Humans are thought to have appeared around 3.5 million years ago (during the most recent period – Quaternary). Flowering plants were now the most common plant life.

41 Cenozoic Mammals

42 Flowering Plants were common during the Cenozoic Era

43 Test Thursday We will spend tomorrow reviewing the material from the last 3 weeks.

Download ppt "How do we know when things happened?"
 The Geological Time Scale Add this unit to your Table of contents! Mr. Karns Biology Fossils. Outine 17-1: The Fossil Record Test Review Test on Thursday!!!! 1. The most powerful Mechanical weathering force is frost wedging. 2. Chapter 15:5 Geologic Time Scale. Life and Geologic Time. The geologic time scale shows Earth’s past. The Geologic Time Scale. Geologic Time Scale : Scientists have formed a chronology of Earth’s history based on evidence from the Earth’s rocks and fossils. Unit 2 Review: History of Life on Earth The Geologic Time Scale Geologic Time Scale. CHAPTER 4 Geologic Time. Events in Your Life  ___When you started second grade  ___When you were born  ___ When you started kindergarten  ___When you learned to ride a bike. Geologic Time. Events in Your Life ___When you started second grade ___When you were born ___ When you started kindergarten ___When you learned to ride. Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Earth Systems 3209 Unit: 2 Historical Geology Reference: Chapters 6, 8; Appendix. Geologic Time Scale (Earth is 4.6 billion years old) End Show Slide 1 of 30 Copyright Pearson Prentice Hall Biology.

 READING THE ROCK RECORD. relative time: events are in sequence, but no actual dates absolute time: identifies actual date of event.