THE TREE OF LIFE Gustav Klimt, 1909. OFTEN, THE RELATIONSHIP BETWEEN SPECIES THROUGH EVOLUTION IS PICTURED AS A TREE WITH THE ANCESTOR SPECIES LOWER ON.

Slides:



Advertisements
Similar presentations
Add this unit to your Table of contents!
Advertisements

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
Geologic Time Scale.
The Cladogram The cladogram is used to show evolutionary relationships between organisms, NOT ancestry. The human shares more DNA with the Chimpanzee than.
Fossils and Earth’s History Notes
Monday December 9,2013 Do Now: Iron oxides are chemicals composed of iron and oxygen. Scientist found that sedimentary rocks prior to 3.5 billion years.
8-1 Notes - Geologic Time and Mass Extinctions
HISTORY OF LIFE Chapter 14. The Record of Life Ch. 14, Sec 1.
A history including how life evolved, how the geosphere changed and major extinction events.
Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Earth Systems 3209 Unit: 2 Historical Geology Reference: Chapters 6, 8; Appendix.
La nuova biologia.blu Le cellule e i viventi David Sadava, David M. Hillis, H. Craig Heller, May R. Berenbaum.
Chapter 19 The History of Life.
Unit 5: Formation of the Earth Objectives: E5.3B - Explain the process of radioactive decay and explain how radioactive elements are used to date the rocks.
- A scale that subdivides the 4.5- billion-year history of Earth into many different units and provides a meaningful time frame within which the events.
Earth History: Geologic Time
Scientists have developed a model of the history of life on Earth called the geologic time scale. The geological time scale is based on studies of Earth’s.
14.1 Fossil Evidence of Change Land Environments The History of Life Chapter 14  Earth formed about 4.6 billion years ago.  Gravity pulled the densest.
Section 1: Geologic Time
The History of Life on Earth
I. Early Life on Earth Earth formed about 4.6 billion years ago Earth was very hot Atmosphere - little Oxygen. Mostly water vapor, CO, CO 2, and N 2.
Geologic Time and Mass Extinctions
17-3 Evolution of Multicellular Life
Examining layers of sedimentary rock, scientists have put together a chronology of Earth’s history. Divided into 4 Eras: 1.Precambrian (3.5 bya mya)
Earth History.
Fossil Evidence of Change Part 2 Chapter 14 Section 1.
Ch 14.1 The record of life You will … 1. examine how rocks and fossils provide evidence of changes in Earth’s organisms 2. correlate the geographic time.
EVOLUTION The History of Life Lecture 11 Southern Boone County HS College Biology Mr. Palmer.
Geologic Time Scale Spring th Grade.
I. What was it like on early Earth ? Very hot Meteorites colliding into earth Frequent volcanic activity Atmosphere with little oxygen & lots of nitrogen.
 Section 8 The Cambrian Explosion and the Diversification of Animals
Early Earth Chapter 15. Earth Forms Scientists hypothesize that Earth formed about 4.6 billion years ago. They also believe that Earth started as a ball.
Copyright © by Holt, Rinehart and Winston. All rights reserved. ResourcesChapter menu CH. 9 - EARTH’S HISTORY Students know the evidence from geological.
17-3 Evolution of Multicellular Life How multicellular life evolved from its earliest forms to its present day diversity.
History of Life Chapter 26. What you need to know! The age of the Earth and when prokaryotic and eukaryotic life emerged. Characteristics of the early.
17-1 The fossil Record 17-2 Earth’s Early History 17-3 Evolution of Multicellular life 17-4 Patterns of Evolution.
Evolutionary History Chapter 15. What you need to know! The age of the Earth and when prokaryotic and eukaryotic life emerged. Characteristics of the.
Chapter billion years ago, the Earth was born. Consider that the Earth formed, life arose: - the first tectonic plates arose and began to move.
Warm-up 3/19/13 The Earth is an estimated 4.6 billion years old. 1. How did scientists come up with this estimate? 2. Describe an organism you would expect.
Precambrian Times Occurred from 4.6 BYA to 542 MYA The period of Earth history known as the “Precambrian Times” is broken up into three eons, which are.
GEOLOGIC TIME The Earth is about 4.6 billion years old.
Time Marches On Chapter 3 Section 5 p Vocabulalry: 1. geologic time scale 2. eon 3. era 4. period 5. epoch 6. extinction.
Early Earth Introduction.
Geologic Time Scale. Imagine putting everything that has happened on Earth into a one hour time frame!
Unit 1 Lesson 4 The History of Life on Earth Copyright © Houghton Mifflin Harcourt Publishing Company.
Geographic Time 8.E.6A.1Develop and use models to organize Earth’s history (including era, period, and epoch) according to the geologic time scale using.
By the end of class, you need to be able to
Early Earth Guided Notes
Geologic Timescale.
Geological timeline events
Geological Time 9.1.
Geologic Time Geologists have their own system of defining and
Introduction- WHEN H DAWG WAS BORN
DO NOW Turn in Review #1. Pick up notes sheet and Review #2.
DO NOW Pick up notes and Review #6 Turn in Review #5.
GEOLOGIC TIME SCALE. GEOLOGIC TIME SCALE The GEOLOGIC TIME SCALE is a record of the history of the Earth, based major geologic & biologic events.
Personal Timeline Create a visual timeline of your life.
4/28 & 4/29 7th Grade Agenda Learning Objective: Learn about Radioactive Dating Collect HW: Reading & Reading & Notetaking p Video: Monsters.
History of our Earth Geologic Time Scale.
Earth formed about 4.6 billion years ago.
A Quick Look at the History of Life on Earth
Geological Time Scale.
Geologic Time Ch. 30.
Human Activities and Biodiversity
The Geologic Time Scale
Notes #6: Geologic Timescale
2/24 & 2/25- 7th Grade Agenda Learning Objective: Learn about other students’ Science Fair Projects Collect HW: Reading & Reading & Notetaking p. 143.
Geologic time is a difficult concept to grasp. 12 hours
2014 Mrs. Hughes 8th Grade Science Geologic Time Shows Earth’s History.
Presentation transcript:

THE TREE OF LIFE Gustav Klimt, 1909

OFTEN, THE RELATIONSHIP BETWEEN SPECIES THROUGH EVOLUTION IS PICTURED AS A TREE WITH THE ANCESTOR SPECIES LOWER ON THE TREE AND THE MORE RECENT SPECIES AS THE NEWER SMALL BRANCHES. WHERE A BRANCH OCCURS INDICATES A COMMON ANCESTOR.

Assyrian, 1000 BCE

GEOLOGIC TIME HADEAN ERA billion years ago to 3.8 bya ARCHAEN ERA- 3.8 bya to 2.5 bya PROTEROZOIC ERA bya to 543 mya PALEOZOIC ERA mya to 248 mya MESOZOIC ERA mya to 65 mya CENOZOIC ERA - 65 mya to today WE’LL ALSO BE CONCERNED WITH SOME OF THE SMALLER DIVISIONS, PERIODS, IN THE PALEOZOIC AND MESOZOIC ERAS.

DURING THE HADEAN ERA, THE EARTH WAS STILL PICKING UP MATERIAL FROM SPACE, AND THE SURFACE WAS MOLTEN FOR MUCH OF THIS PERIOD. SOME TIME DURING THIS PERIOD, THE SURFACE SOLIDIFIED. THERE ARE NO ROCKS ON EARTH THIS OLD. THE OLDEST ROCKS DATE TO ABOUT 3.8 BYA AT THE START OF THE ARCHAEN ERA. DURING THE ARCHAEN ERA, LIFE FIRST APPEARS ON EARTH IN THE FORM OF PRIMITIVE BACTERIA.

NO ONE KNOWS EXACTLY HOW LIFE FIRST BEGAN ON EARTH, BUT MOST AGREE IT BEGAN IN THE OCEANS THAT FIRST FORMED AFTER THE SURFACE COOLED AROUND 3.8 BILLION YEARS AGO. THE EARLY OCEANS WERE LIKELY A SOUP OF CHEMICALS. SOME OF THESE CHEMICALS EVEN CAME FROM OUTER SPACE IN THE FORM OF CHONDRITES, CARBON-CONTAINING METEORITES. AN EXAMPLE WOULD BE THE MURCHESON METEORITE FOUND IN AUSTRALIA.

UNDER THE RIGHT CIRCUMSTANCES, CERTAIN CHEMICALS ARE SELF ORGANIZING. AN EXAMPLE WOULD BE FATTY ACIDS AND LIPIDS. WHEN SHAKEN IN WATER, THEY CAN FORM SPHERICAL DROPLETS OF LIPID BILAYERS WHICH COULD SERVE AS PRIMITIVE CELL WALLS. SCIENTISTS HAVE ALSO DISCOVERED THAT RNA CAN SERVE AS CHEMICAL CATALYSTS AS WELL AS CONTAINERS OF GENETIC INFORMATION.

GEOLOGISTS HAVE DISCOVERED MICRO- FOSSILS AND CHEMICAL EVIDENCE DATING TO AROUND 3.5 BILLION YEARS AGO. THESE WERE FOUND IN ROCKS FROM MARINE SEDIMENTS.

DURING THE PROTEROZOIC ERA (2.5 bya to 543 mya), EUKARYOTIC CELLS APPEAR - PROBABLY AROUND 1.8 bya. SOME OF THESE HAVE THE ABILITY TO PRODUCE OXYGEN AS A WASTE PRODUCT, SO OXYGEN BUILDUP BEGINS IN THE ATMOSPHERE. OXYGEN EQUILIBRIUM WAS PROBABLY REACHED AROUND 2 bya.

THE PALEOZOIC ERA FOLLOWED (543 mya to 248 mya. TWO MAJOR EVENTS CHARACTERIZED THIS ERA. AT THE BEGINNING, A LARGE EXPLOSION IN MULTICELLULAR ORGANISMS OCCURRED. ALMOST ALL LIVING ANIMAL PHYLA APPEARED WITHIN A FEW MILLION YEARS. SOME 400 mya PLANTS AND ANIMALS EMERGED ON LAND.

AT THE END OF THIS ERA, THE LARGEST MASS EXTINCTION IN THE HISTORY OF THE EARTH OCCURRED, THE PERMIAN EXTINCTION. 90% OF ALL LIFE WAS DESTROYED. THE MESOZOIC ERA FOLLOWED (248 mya to 65 mya). DINOSAURS, AS WELL AS MAMMALS, APPEARED DURING THIS ERA, AND PLANTS UNDERWENT A GREAT CHANGE. THE EARLY MESOZOIC WAS DOMINATED BY FERNS AND CYCADS. MODERN GYMNOSPERMS SUCH AS CONIFERS APPEARED IN THE MIDDLE OF THE ERA. BY THE END, MODERN ANGIOSPERMS APPEARED.

THE MESOZOIC ERA ENDED WITH ANOTHER LARGE MASS EXTINCTION - THE END OF THE AGE OF DINOSAURS. THE CENOZOIC ERA GOES FROM 65 mya TO THE PRESENT AND IS OFTEN REFERRED TO AS THE AGE OF MAMMALS. THE LAST 11,000 YEARS ARE CALLED THE HOLOCENE EPOCH. THIS REPRESENTS THE TIME SINCE THE LAST ICE AGE.

MAJOR EXTINCTIONS LATE CAMBRIAN - APPROX. 500 mya - A SERIES OF EXTINCTIONS AS A RESULT OF A CHANGE IN SEA LEVEL LATE ORDOVICIAN - APPROX 440 mya - TWO PEAK EXTINCTIONS - THE FIRST AS A RESULT OF GLACIATION AND THE SECOND AS A RESULT OF RISE IN SEA LEVEL AT THE END OF GLACIATION LATE DEVONIAN - OVER A PERIOD OF ABOUT 3 MILLION YEARS, 365 mya 70% OF ALL SPECIES WERE LOST - FACTORS SUGGESTED INCLUDE GLOBAL COOLING AND A DROP IN OXYGEN LEVELS IN THE SHALLOW SEAS.

PERMIAN EXTINCTION - LARGEST EXTINCTION EVENT - EXTIMATED THAT AS MANY AS 96% OF ALL MARINE SPECIES WERE LOST AND 75% OF ALL VERTEBRATE FAMILIES ON LAND - THE MOST IMPORTANT FACTOR SEEMS TO BE CLIMATE CHANGE. END CRETACEOUS EXTINCTION (KT EXTINCTION)- 85% OF ALL SPECIES DISAPPEARED, INCLUDING THE DINOSAURS - THEORIES SUGGEST A LARGE METEORITE.

WHY SHOULD WE BE CONCERNED ABOUT PAST EXTINCTIONS?

1.WHAT HAPPENED IN THE PAST COULD HAPPEN IN THE FUTURE. A.CLIMATE CHANGE B.ASTEROID/COMET COLLISION 2. GIVES CLUES AS TO HOW EXTINCTIONS DROVE EVOLUTION 3. PROVIDES INFORMATION AS TO HOW LIFE MIGHT DEVELOP ON OTHER WORLDS

SCIENTISTS NOW TALK ABOUT A SIXTH EXTINCTION THAT COULD BE TAKING PLACE NOW. WHILE NOT IN TOTAL AGREEMENT, SCIENTISTS ESTIMATE THAT BETWEEN 17,000 AND 100,000 SPECIES ARE LOST EACH YEAR. IF WE ASSUME A MID-RANGE NUMBER OF 50,000, THAT WOULD MEAN A LOSS OF 50% OF EARTH’S SPECIES IN 100 YEARS.

RICHARD LEAKEY AND ROGER LEWIN IN THEIR BOOK “THE SIXTH EXTINCTION” GIVE THREE REASONS WHY THIS IS OCCURING: 1.DIRECT EXPLOITATION 2.DESTRUCTION AND FRAGMENTATION OF HABITAT 3.INTRODUCTION OF ALIEN SPECIES WE SHOULD PROBABLY ADD A FOURTH FACTOR - CLIMATE CHANGE.

WHAT IS DRIVING THE 6 TH EXTINCTION?

1 DOT = 7,500 PEOPLE

IT SHOULD BE POINTED OUT THAT THE COMPOSITION OF OUR ATMOSPHERE IS NOT AN ACCIDENT. IT IS A RESULT OF A NUMBER OF BIOLOGICAL FACTORS WORKING TOGETHER TO PRODUCE THE ATMOSPHERIC COMPOSITION THAT WE HAVE NOW. 1.GREEN PLANTS PRODUCING OXYGEN AND USING CARBON DIOXIDE 2.A CERTAIN AMOUNT OF CARBON TIED UP IN ORGANIC MATERIAL 3.A CERTAIN AMOUNT OF CARBON TIED UP IN ROCKS

THERE ARE POSSIBLY TWO FACTORS THAT CONTROL THE FATE OF LIFE ON EARTH: 1.THE SURFACE TEMPERATURE 2.THE CONCENTRATION OF CARBON DIOXIDE GAS IN THE ATMOSPHERE

FIRE AND ICE Some say the world will end in fire, Some say in ice. From what I’ve tasted of desire I hold with those who favor fire. But if it had to perish twice, I think I know enough of hate To know that for destruction ice Is also great And would suffice. - Robert Frost -