MASS EXTINCTION. Halesworth & District

Size: px
Start display at page:

Download "MASS EXTINCTION. Halesworth & District"

Transcription

1 MASS EXTINCTION Halesworth & District 1

2 Signs indicate an imminent 6 th Mass Extinction and this time Humans are the cause 2

3 MASS EXTINCTION A Mass Extinction Event is a widespread and rapid decrease in the amount of life (species) on Earth There is a sharp change in diversity and abundance of multi-cellular organisms Rate of extinction increases with respect to the rate of speciation 3

4 MASS EXTINCTION 4

5 MASS EXTINCTION ORDOVICIAN-SILURIAN EVENTS MA two events Killed off 27% of all families 57% of all genera 60-70% of all species Ranked second largest of five mass extinction events 5

6 MASS EXTINCTION LATE DEVONIAN EVENT MA Killed off 19% of all families 50% of all genera 70% of all species 6

7 MASS EXTINCTION PERMIAN-TRIASSIC EVENT 252 MA Killed off 57% of all families 83% of all genera 90-96% of all species Ranked largest of five extinction events 7

8 MASS EXTINCTION TRIASSIC-JURASSIC EVENT 201MA Killed off 23% of all families 48% of all genera 70-75% of all species 8

9 MASS EXTINCTION CRETACEOUS-PALEOGENE EVENT 66MA Killed off 17% of all families 50% of all genera 75% of all species All non-avian dinosaurs became extinct Speculation as to cause but thought to be due to asteroid hit 9

10 RECOVERY Usually only species survive that have the ability to live in diverse habitats Later, species diversify and occupy empty niches Generally biodiversity recovers 5-10 million years after extinction event Recovery may take million years after a severe mass extinction event 10

11 CAUSES Plate tectonic movement Massive volcanism Impact events A nearby nova, supernova or gamma ray burst Geomagnetic reversal Sustained and significant global cooling Sea-level falls Sustained and significant global warming Methane release from continental shelves Hydrogen sulphide emissions from seas Anoxic events Oceanic over-turn Water cycle 11

12 PLATE TECTONIC MOVEMENT Very slow process Ocean floor spreading Some earthquake faults very weak 12

13 MASSIVE VOLCANISM Now, seismic monitoring gives some warning of eruption events Historically Krakatoa in 1883 Mount Tambora in 1815 which led to a year without summer But.. Western half of La Palma could slide causing Tsunami of initial height of 1,000m at island to 50m at Caribbean and Eastern North America 13

14 CAUSES Plate tectonic movement Massive volcanism Impact events A nearby nova, supernova or gamma ray burst Geomagnetic reversal Sustained and significant global cooling Sea-level falls Sustained and significant global warming Methane release from continental shelves Hydrogen sulphide emissions from seas Anoxic events Oceanic over-turn Water cycle 14

15 IMPACT EVENTS Risk comes from asteroid belt which lies between planets Mars and Jupiter Now constant monitoring by NASA Near-Earth Object Programme Office 15

16 IMPACT EVENTS 2008 TC3 exploded 23 miles above Nubian desert on 7 th October

17 IMPACT EVENTS Chelyabinsk meteorite airburst on 15 th February

18 CAUSES Plate tectonic movement Massive volcanism Impact events A nearby nova, supernova or gamma ray burst Geomagnetic reversal Sustained and significant global cooling Sea-level falls Sustained and significant global warming Methane release from continental shelves Hydrogen sulphide emissions from seas Anoxic events Oceanic over-turn Water cycle 18

19 (SUPER)NOVA OR GAMMA RAY Gamma rays are beyond the X-ray spectrum Cause damage similar to radioactivity At the very least, sunspot activity can disrupt satellites 19

20 CAUSES Plate tectonic movement Massive volcanism Impact events A nearby nova, supernova or gamma ray burst Geomagnetic reversal Sustained and significant global cooling Sea-level falls Sustained and significant global warming Methane release from continental shelves Hydrogen sulphide emissions from seas Anoxic events Oceanic over-turn Water cycle 20

21 GEOMAGNETIC REVERSAL A change in earth s magnetic fields such that the positions of magnetic north and magnetic south are interchanged. 21

22 GEOMAGNETIC REVERSAL 22

23 SOUTH ATLANTIC ANOMALY 23

24 SOUTH ATLANTIC ANOMALY 24

25 SOUTH ATLANTIC ANOMALY Increased flux of energy particles dipping to altitude of 200 km Exposes orbiting satellites to higher than usual radiation International Space Station requires extra shielding Hubble Space Telescope does not take observations while passing through the SAA 25

26 CAUSES Plate tectonic movement Massive volcanism Impact events A nearby nova, supernova or gamma ray burst Geomagnetic reversal Sustained and significant global cooling Sea-level falls Sustained and significant global warming Methane release from continental shelves Hydrogen sulphide emissions from seas Anoxic events Oceanic over-turn Water cycle 26

27 ICE AGE CYCLES New data on inter-glacial periods Would expect to be in another ice age 7,000 years ago an ice cycle should have started When planet should have been getting cooler, temperatures started to increase Why? 27

28 ICE AGE CYCLES 12,000 years ago there was an extensive ice sheet over the northern hemisphere (water locked in as ice) 11,000 years ago, farming started in the fertile crescent CO₂ release from burning trees to clear land & CH₄ release from domestic animals Impact was that there was an increased desertification in the fertile crescent Water supply became extremely important 28

29 GLOBAL WARMING GREENHOUSE GASES CO₂ and CH₄ both trap radiation and lead to global warming CH₄ s lifetime in the atmosphere is much shorter than CO 2 CH 4 is more efficient at trapping radiation than CO 2. Pound for pound, the comparative impact of CH 4 on climate change is more than 25 times greater than CO 2 over a 100- year period. 29

30 GLOBAL WARMING Focus has previously been on CO₂ 2015 United Nations Climate Change Conference Agreed to 2% increase in global emissions Wish to pursue efforts to limit the temperature increase to 1.5% The 1.5% goal requires zero emissions sometime between 2030 and

31 GLOBAL WARMING 31

32 GLOBAL WARMING & OCEANS Even if the world manages to limit global warming to 2 C sea levels may rise by 6 metres (20 feet) Ice sheets are being warmed from above and below Once the ice sheets start to melt, the changes become irreversible The British Antarctic Survey Station will have to be moved as a huge crack has appeared in the ice sheet The I Newspaper on 11 th May 2016 reported that 5 Pacific Islands have disappeared 32

33 SEAL LEVEL INCREASES 33

34 CAUSES Plate tectonic movement Massive volcanism Impact events A nearby nova, supernova or gamma ray burst Geomagnetic reversal Sustained and significant global cooling Sea-level falls Sustained and significant global warming Methane release from continental shelves Hydrogen sulphide emissions from seas Anoxic events Oceanic over-turn Water cycle 34

35 METHANE RELEASE 35

36 METHANE RELEASE 36

37 CAUSES Plate tectonic movement Massive volcanism Impact events A nearby nova, supernova or gamma ray burst Geomagnetic reversal Sustained and significant global cooling Sea-level falls Sustained and significant global warming Methane release from continental shelves Hydrogen sulphide emissions from seas Anoxic events Oceanic over-turn Water cycle 37

38 H₂S EMISSIONS FROM SEAS Namibian coast has most intense upwelling of fertile deepocean water H₂S Release due to seafloor organic sediments rich in organic matter Late February

39 CAUSES Plate tectonic movement Massive volcanism Impact events A nearby nova, supernova or gamma ray burst Geomagnetic reversal Sustained and significant global cooling Sea-level falls Sustained and significant global warming Methane release from continental shelves Hydrogen sulphide emissions from seas Anoxic events Oceanic over-turn Water cycle 39

40 ANOXIC EFFECTS When water becomes saturated with carbon there is a rise in atmospheric carbon This causes a positive feedback loop The result is a runaway greenhouse effect Increased ocean acidity = survival problems for phytoplankton which use carbon and release oxygen Decrease in atmospheric oxygen 40

41 CAUSES Plate tectonic movement Massive volcanism Impact events A nearby nova, supernova or gamma ray burst Geomagnetic reversal Sustained and significant global cooling Sea-level falls Sustained and significant global warming Methane release from continental shelves Hydrogen sulphide emissions from seas Anoxic events Oceanic over-turn Water cycle 41

42 OCEANIC OVER TURN Ocean currents & wind patterns Ocean currents circulate water throughout the world s oceans Global warming means more fresh water is released into higher latitudes where deep water is formed This reduces the density of surface water Water sinks more slowly than it normally would Slower ocean currents = fewer nutrients = damage to marine ecosystem 42

43 OCEANIC OVER TURN 43

44 Weather OCEANIC OVER TURN Put simply, colder regions would get warmer and warmer regions would get colder Impact on jet stream patterns El Niňo 44

45 CAUSES Plate tectonic movement Massive volcanism Impact events A nearby nova, supernova or gamma ray burst Geomagnetic reversal Sustained and significant global cooling Sea-level falls Sustained and significant global warming Methane release from continental shelves Hydrogen sulphide emissions from seas Anoxic events Oceanic over-turn Water cycle 45

46 WATER CYCLE 2,000 years ago, we intercepted the water cycle 46

47 WATER CYCLE Vast quantities of water are diverted into dams and irrigation channels for farming and human consumption Los Angeles network of aqueducts, canals and pipelines deliver 90% H₂O 5x as much fresh water is stored in reservoirs than flows in the world s rivers If we are to survive, our water usage must change 47

48 HOLOCENE EXTINCTION Dates from 10,000 years ago to the present day. It covers the period since the ice retreated after the last glaciation and it is sometimes regarded as just another interglacial period Humans are driving this extinction event 48

49 IS IT TOO LATE? 2015 United Nations Climate Change Conference Agreed to 2% increase in global emissions Wish to pursue efforts to limit the temperature increase to 1.5% The 1.5% goal requires zero emissions sometime between 2030 and

50 Limit world population IS IT TOO LATE? 50

51 IS IT TOO LATE? Change in agricultural methods Irrigation Crop rotation Widespread acceptance of GM foods Eat less meat 51

52 Carbon capture IS IT TOO LATE? Algae capturing CO₂ Artificial trees to capture CO₂ Plans to use sandstone to absorb CO₂ Pump CO₂ through shale into sandstone Svalbard has the ideal geological structure 52

53 IS IT TOO LATE? National genebanks of seeds held as insurance Nordic Genebank held at an abandoned coalmine at Svalbard on Spitsbergen Island In 2008 became the Svalbard Global Seed Vault Stores duplicates of national genebanks Storing seeds is free to end users Norway and the Global Diversity Trust pays for operational costs Bill & Melinda Gates Foundation 53

54 IS IT TOO LATE? 54

55 IS IT TOO LATE? 55

56 IS IT TOO LATE? 56

57 IS IT TOO LATE? Seed vault is at a constant -18 C Deep enough to withstand a nuclear explosion Aims to store samples Every variety of seed From every stable crop From every country Genetic diversity paramount So far only one withdrawal request Syria in

58 OTHER FACTORS TO CONSIDER Antibiotic resistance Global financial cost of taking no action will be the loss of 10 million lives a year and 69 trillion a year by 2050 New viral infections Zika virus causes microcephaly WHO predicts that 18 European countries at moderate risk in 2016 Highest risk Madeira, Black Sea coast of Russia & Georgia Political hot potato due to mass migration resulting from food shortages 58

HOW GEOGRAPHY AND GEOLOGY AFFECT BIOLOGICAL DIVERSITY

HOW GEOGRAPHY AND GEOLOGY AFFECT BIOLOGICAL DIVERSITY HOW GEOGRAPHY AND GEOLOGY AFFECT BIOLOGICAL DIVERSITY Factors Affecting Extinction Rates Natural Factors Climate change Cataclysmic event (volcano, earthquake) Human Activities Habitat Loss/Fragmentation

More information

Today we will discuss global climate: how it has changed in the past, and how the current status and possible future look.

Today we will discuss global climate: how it has changed in the past, and how the current status and possible future look. Global Climate Change Today we will discuss global climate: how it has changed in the past, and how the current status and possible future look. If you live in an area such as the Mississippi delta (pictured)

More information

STAAR Science Tutorial 48 TEK 8.11C: Effects of Environmental Change

STAAR Science Tutorial 48 TEK 8.11C: Effects of Environmental Change Name: Teacher: Pd. Date: STAAR Science Tutorial 48 TEK 8.11C: Effects of Environmental Change TEK 8.11C: Explore how short- and long-term environmental changes affect organisms and traits in subsequent

More information

Climate Changes due to Natural Processes

Climate Changes due to Natural Processes Climate Changes due to Natural Processes 2.6.2a Summarize natural processes that can and have affected global climate (particularly El Niño/La Niña, volcanic eruptions, sunspots, shifts in Earth's orbit,

More information

Chapter Introduction. Earth. Change. Chapter Wrap-Up

Chapter Introduction. Earth. Change. Chapter Wrap-Up Chapter Introduction Lesson 1 Lesson 2 Lesson 3 Climates of Earth Chapter Wrap-Up Climate Cycles Recent Climate Change What is climate and how does it impact life on Earth? What do you think? Before you

More information

4 Changes in Climate. TAKE A LOOK 2. Explain Why is more land exposed during glacial periods than at other times?

4 Changes in Climate. TAKE A LOOK 2. Explain Why is more land exposed during glacial periods than at other times? Name Class CHAPTER 3 Date Climate 4 Changes in Climate SECTION National Science Education Standards BEFORE YOU READ After you read this section, you should be able to answer these questions: ES 1k, 2a

More information

NATS 101 Section 13: Lecture 32. Paleoclimate

NATS 101 Section 13: Lecture 32. Paleoclimate NATS 101 Section 13: Lecture 32 Paleoclimate Natural changes in the Earth s climate also occur at much longer timescales The study of prehistoric climates and their variability is called paleoclimate.

More information

Global climate change

Global climate change Global climate change What is climate change? This winter was really cold! Temp difference ( C): Jan 2004 vs. Jan 2002-2003 Make your own maps at: http://www.giss.nasa.gov/data/update/gistemp/maps/ 1 What

More information

ESA's Rosetta spacecraft What are habitable exoplanets? Is there an Earth 2.0?

ESA's Rosetta spacecraft What are habitable exoplanets? Is there an Earth 2.0? ESA's Rosetta spacecraft - 2009 What are habitable exoplanets? Is there an Earth 2.0? Christina Hedges (Institute of Astronomy) For the past 20 years, since the discovery of planets outside our solar system,

More information

Carbon Cycling Internal

Carbon Cycling Internal Carbon Cycling Internal The 4 subcycles Atmosphere The Earth s Atmosphere The Earth has a radius of some 6400 km. Ninety-nine percent of the earth's atmosphere is contained within a layer approximately

More information

History of life on Earth Mass Extinctions.

History of life on Earth Mass Extinctions. History of life on Earth Mass Extinctions. Agenda or Summary Layout A summary of the topics discussed 1 2 3 4 Explanation of Mass extinctions The five major mass extinctions Two particular extinctions

More information

The surface of the ocean floor is as varied as the land. The five major oceans, from largest to smallest, are

The surface of the ocean floor is as varied as the land. The five major oceans, from largest to smallest, are 11.1 Ocean Basins The surface of the ocean floor is as varied as the land. The five major oceans, from largest to smallest, are w the Pacific w the Atlantic w the Indian w the Southern w the Arctic The

More information

Chapter 2: Physical Geography

Chapter 2: Physical Geography Chapter 2: Physical Geography Pg. 39-68 Learning Goals for Chp2: q q q q q Explain how the Earth moves in space and why seasons change. Outline the factors that influence climate and recognize different

More information

Website Lecture 3 The Physical Environment Part 1

Website   Lecture 3 The Physical Environment Part 1 Website http://websites.rcc.edu/halama Lecture 3 The Physical Environment Part 1 1 Lectures 3 & 4 1. Biogeochemical Cycling 2. Solar Radiation 3. The Atmosphere 4. The Global Ocean 5. Weather and Climate

More information

6. What has been the most effective erosive agent in the climate system? a. Water b. Ice c. Wind

6. What has been the most effective erosive agent in the climate system? a. Water b. Ice c. Wind Multiple Choice. 1. Heinrich Events a. Show increased abundance of warm-water species of planktic foraminifera b. Show greater intensity since the last deglaciation c. Show increased accumulation of ice-rafted

More information

Weather Forecasts and Climate AOSC 200 Tim Canty. Class Web Site: Lecture 27 Dec

Weather Forecasts and Climate AOSC 200 Tim Canty. Class Web Site:   Lecture 27 Dec Weather Forecasts and Climate AOSC 200 Tim Canty Class Web Site: http://www.atmos.umd.edu/~tcanty/aosc200 Topics for today: Climate Natural Variations Feedback Mechanisms Lecture 27 Dec 4 2018 1 Climate

More information

THE ORDOVICIAN EXTINCTION. 444 million years ago

THE ORDOVICIAN EXTINCTION. 444 million years ago THE ORDOVICIAN EXTINCTION 444 million years ago TOTAL GENERA THROUGH THE PHANEROZOIC ERA The Cambrian to the Present PERMIAN TRIASSIC CRETACEOUS Holocene The Present Miocene DEVONIAN ORDOVICIAN Mississippian

More information

Greenhouse Effect & Global Warming

Greenhouse Effect & Global Warming Chemical Cycles: Greenhouse Effect: Cause and effect Chemical Cycles: CO 2 and O 2 Chemical Fluxes: CO 2 and O 2 Proxies for climate change: Isotopes Greenhouse Effect & Global Warming Global Warming World

More information

Natural Climate Variability: Longer Term

Natural Climate Variability: Longer Term Natural Climate Variability: Longer Term Natural Climate Change Today: Natural Climate Change-2: Ice Ages, and Deep Time Geologic Time Scale background: Need a system for talking about unimaginable lengths

More information

Use models to describe the sun s place in space in relation to the Milky Way Galaxy and the distribution of galaxy clusters in the universe.

Use models to describe the sun s place in space in relation to the Milky Way Galaxy and the distribution of galaxy clusters in the universe. The Milky Way Galaxy consists of more than two hundred billion stars, the sun being one of them, and is one of hundreds of billions of galaxies in the known universe. s of the formation and structure of

More information

Weather and Climate Change

Weather and Climate Change Weather and Climate Change What if the environmental lapse rate falls between the moist and dry adiabatic lapse rates? The atmosphere is unstable for saturated air parcels but stable for unsaturated air

More information

Introduction to Climate Change

Introduction to Climate Change Ch 19 Climate Change Introduction to Climate Change Throughout time, the earth's climate has always been changing produced ice ages Hence, climate variations have been noted in the past what physical processes

More information

Website Lecture 3 The Physical Environment Part 1

Website   Lecture 3 The Physical Environment Part 1 Website http://websites.rcc.edu/halama Lecture 3 The Physical Environment Part 1 1 Lectures 3 & 4 1. Biogeochemical Cycling 2. Solar Radiation 3. The Atmosphere 4. The Global Ocean 5. Weather and Climate

More information

Development of the Global Environment

Development of the Global Environment Development of the Global Environment G302: Spring 2004 A course focused on exploration of changes in the Earth system through geological history Simon C. Brassell Geological Sciences simon@indiana.edu

More information

What is Climate? Understanding and predicting climatic changes are the basic goals of climatology.

What is Climate? Understanding and predicting climatic changes are the basic goals of climatology. What is Climate? Understanding and predicting climatic changes are the basic goals of climatology. Climatology is the study of Earth s climate and the factors that affect past, present, and future climatic

More information

Day 1 of Global Warming. Copyright 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings

Day 1 of Global Warming. Copyright 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Day 1 of Global Warming Copyright 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings The Atmosphere Atmosphere = the thin layer (1/100 th of Earth s diameter) of gases that surrounds

More information

Climate Regulation. - What stabilizes the climate - Greenhouse effect

Climate Regulation. - What stabilizes the climate - Greenhouse effect Climate Regulation - What stabilizes the climate - Greenhouse effect Last time! Processes that shaped Earth: Volcanism, tectonics! How we retain atmospheric molecules ( escape speed )! A magnetic field

More information

8. Climate changes Short-term regional variations

8. Climate changes Short-term regional variations 8. Climate changes 8.1. Short-term regional variations By short-term climate changes, we refer here to changes occurring over years to decades. Over this timescale, climate is influenced by interactions

More information

Chapter 2 Planet Earth

Chapter 2 Planet Earth Chapter 2 Planet Earth Section Notes Earth and the Sun s Energy Water on Earth The Land Close-up The Water Cycle World Almanac Major Eruptions in the Ring of Fire Quick Facts Chapter 2 Visual Summary Video

More information

Extinctions & Climate Change Student Activity. Diagram interpretation and using research data

Extinctions & Climate Change Student Activity. Diagram interpretation and using research data Diagram interpretation and using research data Biodiversity relates to the variety of life found in an area. The number and variety of species is a simple measure of its health i.e. its ability to respond

More information

Oceanography Quiz 2. Multiple Choice Identify the choice that best completes the statement or answers the question.

Oceanography Quiz 2. Multiple Choice Identify the choice that best completes the statement or answers the question. Oceanography Quiz 2 Multiple Choice Identify the choice that best completes the statement or answers the question. 1. The highest and lowest tides are known as the spring tides. When do these occur? a.

More information

LECTURE #25: Mega Disasters - Mass Extinctions, Meteorite Impacts...

LECTURE #25: Mega Disasters - Mass Extinctions, Meteorite Impacts... GEOL 0820 Ramsey Natural Disasters Spring, 2018 LECTURE #25: Mega Disasters - Mass Extinctions, Meteorite Impacts... Date: 19 April 2018 I. Time & Life on Earth geologic time scale o divided into named

More information

0 questions at random and keep in order

0 questions at random and keep in order Page 1 of 5 This chapter has 48 questions. Scroll down to see and select individual questions or narrow the list using the checkboxes below. 0 questions at random and keep in order s - (23) Odd Numbered

More information

Lesson 2. Antarctic Oceanography: Component I - Ice/Glaciers Component II - Marine Snow

Lesson 2. Antarctic Oceanography: Component I - Ice/Glaciers Component II - Marine Snow Lesson 2. Antarctic Oceanography: Component I - Ice/Glaciers Component II - Marine Snow Lesson Objectives: Introduces students to the different kinds of ice found in Antarctica, Students will become familiar

More information

Grades 9-12: Earth Sciences

Grades 9-12: Earth Sciences Grades 9-12: Earth Sciences Earth Sciences...1 Earth s Place in the Universe...1 Dynamic Earth Processes...2 Energy in the Earth System...2 Biogeochemical cycles...4 Structure and Composition of the Atmosphere...4

More information

CLIMATE. SECTION 14.1 Defining Climate

CLIMATE. SECTION 14.1 Defining Climate Date Period Name CLIMATE SECTION.1 Defining Climate In your textbook, read about climate and different types of climate data. Put a check ( ) next to the types of data that describe climate. 1. annual

More information

History. Late 18 th /early 19 th century Europeans observed that erratic boulders dispersed due to the retention of glaciers caused by climate chance

History. Late 18 th /early 19 th century Europeans observed that erratic boulders dispersed due to the retention of glaciers caused by climate chance Ice ages What is an ice age? Geological period of long-term reduction in the temperature of the Earth's surface and atmosphere which results in the formation and expansion of continental ice sheets, polar

More information

SAMPLE PAGE. pulses. The Ice Age By: Sue Peterson

SAMPLE PAGE. pulses. The Ice Age By: Sue Peterson Page 61 Objective sight words (pulses, intermittent, isotopes, chronicle, methane, tectonic plates, volcanism, configurations, land-locked, erratic); concepts (geological evidence and specific terminology

More information

The History of Life on Earth

The History of Life on Earth 8 The History of Life on Earth lesson 1 Geologic Time and Mass Extinctions Grade Seven Science Content Standard. 4.b. Students know the history of life on Earth has been disrupted by major catastrophic

More information

Please be ready for today by:

Please be ready for today by: Please be ready for today by: 1. HW out for a stamp 2. Paper and pencil/pen for notes 3. Be ready to discuss what you know about El Nino after you view the video clip What is El Nino? El Nino Basics El

More information

Unit 2 Meteorology Test **Please do not write on this test** 5. El Nino & La Nina 6. Photosynthesis 7. Coriolis Effect 8.

Unit 2 Meteorology Test **Please do not write on this test** 5. El Nino & La Nina 6. Photosynthesis 7. Coriolis Effect 8. Matching (2 points each) 1. weather 2. climate 3. Greenhouse Effect 4. Convection Unit 2 Meteorology Test **Please do not write on this test** 5. El Nino & La Nina 6. Photosynthesis 7. Coriolis Effect

More information

Pleistocene Glaciation (Ch.14) Geologic evidence Milankovitch cycles Glacial climate feedbacks

Pleistocene Glaciation (Ch.14) Geologic evidence Milankovitch cycles Glacial climate feedbacks Pleistocene Glaciation (Ch.14) Geologic evidence Milankovitch cycles Glacial climate feedbacks End of last ice-age rise of human civilization Modern ice-ages begin Asteroid impact end of dinosaurs Cambrian

More information

Name Date Class. growth rings of trees, fossilized pollen, and ocean. in the northern hemisphere.

Name Date Class. growth rings of trees, fossilized pollen, and ocean. in the northern hemisphere. Lesson Outline LESSON 2 A. Long-Term Cycles 1. A(n) climate cycle takes much longer than a lifetime to complete. a. To learn about long-term climate cycles, scientists study natural records, such as growth

More information

Climate. What is climate? STUDY GUIDE FOR CONTENT MASTERY. Name Class Date

Climate. What is climate? STUDY GUIDE FOR CONTENT MASTERY. Name Class Date Climate SECTION 14.1 What is climate? In your textbook, read about climate and different types of climate data. Put a check ( ) next to the types of data that describe climate. 1. annual wind speed 4.

More information

Welcome to ATMS 111 Global Warming.

Welcome to ATMS 111 Global Warming. Welcome to ATMS 111 Global Warming http://www.atmos.washington.edu/2010q1/111 Isotopic Evidence 16 O isotopes "light 18 O isotopes "heavy" Evaporation favors light Rain favors heavy Cloud above ice is

More information

Causes of Extinction

Causes of Extinction Causes of Extinction Extinction the process through which a species disappears from Earth, when the birth rate is less than the death rate. When a species becomes extinct, it no longer exists, which can

More information

Phanerozoic (last 0.54 by) Tectonics Climate Life

Phanerozoic (last 0.54 by) Tectonics Climate Life Phanerozoic (last 0.54 by) Tectonics Climate Life Tools for Locating Past Continent Positions Fossils depending on climate Alignment of geological features Geometrical fit of continental margins Similarity

More information

3. The diagram below shows how scientists think some of Earth's continents were joined together in the geologic past.

3. The diagram below shows how scientists think some of Earth's continents were joined together in the geologic past. 1. The map below shows the present-day locations of South America and Africa. Remains of Mesosaurus, an extinct freshwater reptile, have been found in similarly aged bedrock formed from lake sediments

More information

The Distribution of Cold Environments

The Distribution of Cold Environments The Distribution of Cold Environments Over 25% of the surface of our planet can be said to have a cold environment, but defining what we actually mean by that can be very challenging. This is because cold

More information

Understanding past climate change

Understanding past climate change Steven J. Phipps ARC Centre of Excellence for Climate System Science Climate Change Research Centre University of New South Wales CLIM1001 Introduction to Climate Change 3 September 2013 1 Why past climates

More information

Weather Vs. Climate. Weather Vs. Climate. Chapter 14

Weather Vs. Climate. Weather Vs. Climate. Chapter 14 Weather Vs. Climate Chapter 14 Weather: Conditions of the atmosphere at a particular time and place, for short periods of time (days). Climate: Long-term averages of weather (Averaged over 30 yrs). Weather

More information

The bar chart shows the composition of a sample of dry air from the Earth s atmosphere. Name the three gases shown in the bar chart.

The bar chart shows the composition of a sample of dry air from the Earth s atmosphere. Name the three gases shown in the bar chart. Q1. (a) The diagram shows the Earth s layered structure. Name parts (i) and (ii). (b) The bar chart shows the composition of a sample of dry air from the Earth s atmosphere. Name the three gases shown

More information

The Dynamic Earth Section 3. Chapter 3 The Dynamic Earth Section 3: The Hydrosphere and Biosphere DAY 1

The Dynamic Earth Section 3. Chapter 3 The Dynamic Earth Section 3: The Hydrosphere and Biosphere DAY 1 Chapter 3 The Dynamic Earth Section 3: The Hydrosphere and Biosphere DAY 1 The Hydrosphere The hydrosphere includes all of the water on or near the Earth s surface. This includes water in the oceans, lakes,

More information

World Geography Chapter 3

World Geography Chapter 3 World Geography Chapter 3 Section 1 A. Introduction a. Weather b. Climate c. Both weather and climate are influenced by i. direct sunlight. ii. iii. iv. the features of the earth s surface. B. The Greenhouse

More information

Long-term Climate Change. We are in a period of relative warmth right now but on the time scale of the Earth s history, the planet is cold.

Long-term Climate Change. We are in a period of relative warmth right now but on the time scale of the Earth s history, the planet is cold. Long-term Climate Change We are in a period of relative warmth right now but on the time scale of the Earth s history, the planet is cold. Long-term Climate Change The Archean is thought to have been warmer,

More information

PLATE TECTONICS THEORY

PLATE TECTONICS THEORY PLATE TECTONICS THEORY Continental drift Sea floor spreading CONTINENTAL DRIFT CONTINENTAL DRIFT 1. The fitness of continents and Continental Reconstruction Earth ~200 million years ago 1.1 Geometrical

More information

Formation of the Earth and Solar System. Radiometric dating of moon rocks, minerals, and meteorites. Size and composition of solar system objects

Formation of the Earth and Solar System. Radiometric dating of moon rocks, minerals, and meteorites. Size and composition of solar system objects Environmental Science: NGSS Curriculum Map 2016 - S. Kraemer, J. Crane, M. Thorn, S. Marz Time/Interval Essential Question Content Skills Assessment Standards Days: Unit 1: History of the Earth Crosscutting:

More information

COMPUTER METHODS AND MODELING IN GEOLOGY THE GLOBAL PHOSPHORUS CYCLE

COMPUTER METHODS AND MODELING IN GEOLOGY THE GLOBAL PHOSPHORUS CYCLE COMPUTER METHODS AND MODELING IN GEOLOGY THE GLOBAL PHOSPHORUS CYCLE Phosphorous (P) is an essential nutrient for life. It is found in the RNA and DNA of all organisms, as well as in the adenosine triphosphate

More information

Water percolating through hot lava dissolves soluble minerals containing chlorine, bromine and sulphur compounds

Water percolating through hot lava dissolves soluble minerals containing chlorine, bromine and sulphur compounds Figure 5 The sources of dissolved ions in sea water. Water falls as rain Compounds containing mainly calcium, magnesium, carbonate and silicate ions are leached from the soil Rivers carry ions in solution

More information

Summary. The Ice Ages and Global Climate

Summary. The Ice Ages and Global Climate The Ice Ages and Global Climate Summary Earth s climate system involves the atmosphere, hydrosphere, lithosphere, and biosphere. Changes affecting it operate on time scales ranging from decades to millions

More information

Monday, December 4, 2017 The Pleistocene Glaciations (Chapter 14) Week 14 Assessment, closes Wednesday Dec 6

Monday, December 4, 2017 The Pleistocene Glaciations (Chapter 14) Week 14 Assessment, closes Wednesday Dec 6 Monday, December 4, 2017 The Pleistocene Glaciations (Chapter 14) Week 14 Assessment, closes Wednesday Dec 6 Week 15 Assessment will be last one, closes Wednesday Dec 13 Homework 5 due Wednesday, Dec 6

More information

Last Time. Submarine Canyons and Fans. Turbidites. MAS 603: Geological Oceanography. Lecture 16: Greenhouse vs. Icehouse Earths

Last Time. Submarine Canyons and Fans. Turbidites. MAS 603: Geological Oceanography. Lecture 16: Greenhouse vs. Icehouse Earths UNIVERSITY OF SOUTH ALABAMA Last Time MAS 603: Geological Oceanography Lecture 16: Greenhouse vs. Icehouse Earths Submarine Fans Definition and morphology Transport mechanisms (density currents) Submarine

More information

Chapter 1 Section 2. Land, Water, and Climate

Chapter 1 Section 2. Land, Water, and Climate Chapter 1 Section 2 Land, Water, and Climate Vocabulary 1. Landforms- natural features of the Earth s land surface 2. Elevation- height above sea level 3. Relief- changes in height 4. Core- most inner

More information

1. Oceans. Example 2. oxygen.

1. Oceans. Example 2. oxygen. 1. Oceans a) Basic facts: There are five oceans on earth, making up about 72% of the planet s surface and holding 97% of the hydrosphere. Oceans supply the planet with most of its oxygen, play a vital

More information

Earth & Earthlike Planets. David Spergel

Earth & Earthlike Planets. David Spergel Earth & Earthlike Planets David Spergel Course Logistics Life Everywhere and Rare Earths are now in the U-Store Each precept will be divided into two teams (at this week s s precept). Debate topic: Are

More information

Plate Tectonics Tutoiral. Questions. Teacher: Mrs. Zimmerman. Plate Tectonics and Mountains Practice Test

Plate Tectonics Tutoiral. Questions. Teacher: Mrs. Zimmerman. Plate Tectonics and Mountains Practice Test Teacher: Mrs. Zimmerman Print Close Plate Tectonics and Mountains Practice Test Plate Tectonics Tutoiral URL: http://www.hartrao.ac.za/geodesy/tectonics.html Questions 1. Fossils of organisms that lived

More information

PTYS 214 Spring Announcements Midterm #4: two weeks from today!

PTYS 214 Spring Announcements Midterm #4: two weeks from today! PTYS 214 Spring 2018 Announcements Midterm #4: two weeks from today! 1 Previously Radiometric Dating Compare parent / daughter to determine # of half lives 14C, 40K, 238U, 232Th, 87Ru Evidence for Early

More information

GO ON. Directions: Use the diagram below to answer question 1.

GO ON. Directions: Use the diagram below to answer question 1. d i a g n o s t i c t e s t : e a r t h a n d s p a c e s c i e n c e question 1. 1. What is the correct order (starting from the surface) of Earth s layers? A crust, outer core, inner core, mantle B mantle,

More information

Plate Tectonics. By Destiny, Jarrek, Kaidence, and Autumn

Plate Tectonics. By Destiny, Jarrek, Kaidence, and Autumn Plate Tectonics By Destiny, Jarrek, Kaidence, and Autumn .The Denali Fault and San Andreas Fault - The San Andreas Fault is a continental transform fault that extends roughly 1300 km (810 miles) through

More information

4 Changes in Climate. TAKE A LOOK 2. Explain Why is more land exposed during glacial periods than at other times?

4 Changes in Climate. TAKE A LOOK 2. Explain Why is more land exposed during glacial periods than at other times? Name Class CHAPTER 17 Date Climate SECTION 4 Changes in Climate National Science Education Standards BEFORE YOU READ After you read this section, you should be able to answer these questions: ES 1k, 2a

More information

Environmental Science Chapter 13 Atmosphere and Climate Change Review

Environmental Science Chapter 13 Atmosphere and Climate Change Review Environmental Science Chapter 13 Atmosphere and Climate Change Review Multiple Choice Identify the choice that best completes the statement or answers the question. 1. Climate in a region is a. the long-term,

More information

MAR110 LECTURE #28 Climate Change I

MAR110 LECTURE #28 Climate Change I 25 November 2007 MAR 110 Lec28 Climate Change I 1 MAR110 LECTURE #28 Climate Change I Figure 28.1 Climate Change Diagnostics Drought and flooding represent just a couple of hazards related to climate variability

More information

Almost of Earth is covered by water. On a map, the continents appear as huge islands surrounded by a vast global ocean.

Almost of Earth is covered by water. On a map, the continents appear as huge islands surrounded by a vast global ocean. Earth s Oceans & Ocean Floor Date: Feelin Blue What are Earth s five main oceans? Almost of Earth is covered by water. On a map, the continents appear as huge islands surrounded by a vast global ocean.

More information

Lithosphere: (Rocky Sphere) Solid, rocky, outer layer of the Earth. Includes the crust and part of the upper mantle. Lithosphere

Lithosphere: (Rocky Sphere) Solid, rocky, outer layer of the Earth. Includes the crust and part of the upper mantle. Lithosphere Lithosphere: (Rocky Sphere) Solid, rocky, outer layer of the Earth. Includes the crust and part of the upper mantle. Lithosphere Permafrost Permafrost Ground that is at a temperature of 0 or below for

More information

1. In the block diagram shown here, which is the oldest rock unit?

1. In the block diagram shown here, which is the oldest rock unit? Pre/Post GCI Name (print) 1. In the block diagram shown here, which is the oldest rock unit? 2. Referring to the same diagram as the previous question, which of the labeled rock units is the youngest?

More information

Section 1: How Did Life Begin? Chapter 19: History of Life on Earth. Section 2: The Age of Earth

Section 1: How Did Life Begin? Chapter 19: History of Life on Earth. Section 2: The Age of Earth Chapter 19: History of Life on Earth Section 1: How Did Life Begin? I. The Basic Chemicals of Life A. 1920s B. Earth s early oceans contained large amounts of organic molecules C. Molecules formed spontaneously

More information

Topic 6: Insolation and the Seasons

Topic 6: Insolation and the Seasons Topic 6: Insolation and the Seasons Solar Radiation and Insolation Insolation: In Sol ation The Sun is the primary source of energy for the earth. The rate at which energy is radiated is called Intensity

More information

Please take out your fill-in notes again, and we will continue learning about extinct creatures.

Please take out your fill-in notes again, and we will continue learning about extinct creatures. Today s Topic Evolution: Extinction Learning Goal: SWBAT explain why creatures go extinct from Earth, and why some recently-extinct creatures have gone extinct. Please take out your fill-in notes again,

More information

2. Fargo, North Dakota receives more snow than Charleston, South Carolina.

2. Fargo, North Dakota receives more snow than Charleston, South Carolina. 2015 National Tournament Division B Meteorology Section 1: Weather versus Climate Chose the answer that best answers the question 1. The sky is partly cloudy this morning in Lincoln, Nebraska. 2. Fargo,

More information

Name Date Class. Directions: Use the diagram below to answer question Florida Progress Monitoring and Benchmark Assessments

Name Date Class. Directions: Use the diagram below to answer question Florida Progress Monitoring and Benchmark Assessments b e n c h m a r k t e s t : e a r t h a n d s p a c e s c i e n c e Multiple Choice 1. Geologists obtain indirect evidence about Earth s interior by A measuring pressure differences at Earth s surface.

More information

Climate vs. Weather. Weather: Short term state of the atmosphere. Climate: The average weather conditions in an area over a long period of time

Climate vs. Weather. Weather: Short term state of the atmosphere. Climate: The average weather conditions in an area over a long period of time Weather and Climate Climate vs. Weather Weather: Short term state of the atmosphere. Temperature, humidity, cloud cover, precipitation, winds, visibility, air pressure, air pollution, etc Climate: The

More information

Global Weather Trade Winds etc.notebook February 17, 2017

Global Weather Trade Winds etc.notebook February 17, 2017 Global Weather 1 north pole northern hemisphere equator southern hemisphere south pole 2 We have seasons because of the Earth's tilt The seasons are opposite in the northern and southern hemispheres winter

More information

Weather & Ocean Currents

Weather & Ocean Currents Weather & Ocean Currents Earth is heated unevenly Causes: Earth is round Earth is tilted on an axis Earth s orbit is eliptical Effects: Convection = vertical circular currents caused by temperature differences

More information

Impacts of Climate on the Corn Belt

Impacts of Climate on the Corn Belt Impacts of Climate on the Corn Belt Great Lakes Crop Summit 2015 2015 Evelyn Browning Garriss Conclusions Climate change is not linear. It ebbs and flows. Recent polar volcano eruptions created a cool

More information

Lecture 8. The Holocene and Recent Climate Change

Lecture 8. The Holocene and Recent Climate Change Lecture 8 The Holocene and Recent Climate Change Recovery from the last ice age About 15,000 years ago, the earth began to warm and the huge ice sheets covering much of North America and Eurasia began

More information

1 Earth s Oceans. TAKE A LOOK 2. Identify What are the five main oceans?

1 Earth s Oceans. TAKE A LOOK 2. Identify What are the five main oceans? CHAPTER 13 1 Earth s Oceans SECTION Exploring the Oceans BEFORE YOU READ After you read this section, you should be able to answer these questions: What affects the salinity of ocean water? What affects

More information

MAR110 LECTURE #22 Climate Change

MAR110 LECTURE #22 Climate Change MAR 110: Lecture 22 Outline Climate Change 1 MAR110 LECTURE #22 Climate Change Climate Change Diagnostics Drought and flooding represent just a couple of hazards related to climate variability (O) The

More information

Earth History. What is the Earth s time scale? Geological time Scale. Pre-Cambrian. FOUR Eras

Earth History. What is the Earth s time scale? Geological time Scale. Pre-Cambrian. FOUR Eras The Earth is 4.6 billion years old! Earth History Mrs. Burkey ESS Cy Creek HS 17-18 If the Earth formed at midnight 6:00 am First life appears 10:00 pm First animals/plants on land 11:59 pm First humans

More information

Hydrologic System. What is a Natural System? Hydrologic System

Hydrologic System. What is a Natural System? Hydrologic System 31 The Changing Face of the Earth Before After Flooding of Mississippi & Illinois Rivers 1993 According to plate tectonic theory, which of these should have the most violent earthquakes, on average? 1.

More information

Plate Climatology Theory* by James Edward Kamis 21 October 2014

Plate Climatology Theory* by James Edward Kamis 21 October 2014 Plate Climatology Theory* by James Edward Kamis 21 October 2014 Synopsis The Sun, quite obviously, is the first order driver of Earth s climate, but a much neglected second order driver can contribute

More information

Chapter 10 Planetary Atmospheres Earth and the Other Terrestrial Worlds. What is an atmosphere? Planetary Atmospheres

Chapter 10 Planetary Atmospheres Earth and the Other Terrestrial Worlds. What is an atmosphere? Planetary Atmospheres Chapter 10 Planetary Atmospheres Earth and the Other Terrestrial Worlds What is an atmosphere? Planetary Atmospheres Pressure Composition Greenhouse effect Atmospheric structure Color of the sky 1 Atmospheres

More information

Factors That Affect Climate

Factors That Affect Climate Factors That Affect Climate Factors That Affect Climate Latitude As latitude (horizontal lines) increases, the intensity of solar energy decreases. The tropical zone is between the tropic of Cancer and

More information

The Dynamic Crust 2) 4) Which diagram represents the most probable result of these forces? 1)

The Dynamic Crust 2) 4) Which diagram represents the most probable result of these forces? 1) 1. The diagrams below show cross sections of exposed bedrock. Which cross section shows the least evidence of crustal movement? 1) 3) 4. The diagram below represents a section of the Earth's bedrock. The

More information

Extent of Periglacial = Global Permafrost Permafrost: Soil and/or rock where temperatures remain below 0 degrees C for 2 or more years.

Extent of Periglacial = Global Permafrost Permafrost: Soil and/or rock where temperatures remain below 0 degrees C for 2 or more years. Geog 1000 - Lecture 34 Periglacial Environments and Paleoclimatology http://scholar.ulethbridge.ca/chasmer/classes/ Today s Lecture (Pgs 422-434) 1. Exam questions from last week, and today 2. Extent of

More information

Global Climate Systems

Global Climate Systems Global Climate Systems I. Earth s Climate A. Past Climate B. Present Climate and Classification 1. Climate components 2. Classification 3. Köppen Climate Classification 4. El Nino III. Global Climate Change

More information

Origins of Life and Extinction

Origins of Life and Extinction Origins of Life and Extinction What is evolution? What is evolution? The change in the genetic makeup of a population over time Evolution accounts for the diversity of life on Earth Natural selection is

More information

Short-Term Climate Variability (Ch.15) Volcanos and Climate Other Causes of Holocene Climate Change

Short-Term Climate Variability (Ch.15) Volcanos and Climate Other Causes of Holocene Climate Change Short-Term Climate Variability (Ch.15) Volcanos and Climate Other Causes of Holocene Climate Change Volcanos and Climate We learned in Chapter 12 that the volanos play an important role in Earth s climate

More information

The Phanerozoic Eon. 542 mya Present. Divided into 3 Eras The Paleozoic, Mesozoic, and Cenozoic Eras

The Phanerozoic Eon. 542 mya Present. Divided into 3 Eras The Paleozoic, Mesozoic, and Cenozoic Eras 542 mya Present The Phanerozoic Eon Divided into 3 Eras The Paleozoic, Mesozoic, and Cenozoic Eras The ends of the Paleozoic and Mesozoic Eras were marked by mass extinctions The Cenozoic Era is still

More information

Land Surface Sea Ice Land Ice. (from Our Changing Planet)

Land Surface Sea Ice Land Ice. (from Our Changing Planet) Lecture 5: Land Surface and Cryosphere (Outline) Land Surface Sea Ice Land Ice (from Our Changing Planet) Earth s s Climate System Solar forcing Atmosphere Ocean Land Solid Earth Energy, Water, and Biochemistry

More information

Earth s Climate System. Surface Albedo. Climate Roles of Land Surface. Lecture 5: Land Surface and Cryosphere (Outline) Land Surface Sea Ice Land Ice

Earth s Climate System. Surface Albedo. Climate Roles of Land Surface. Lecture 5: Land Surface and Cryosphere (Outline) Land Surface Sea Ice Land Ice Lecture 5: Land Surface and Cryosphere (Outline) Earth s Climate System Solar forcing Land Surface Sea Ice Land Ice Atmosphere Ocean Land Solid Earth Energy, Water, and Biochemistry Cycles (from Our Changing

More information