Using Microfossils to Understand Paleo-Climate
|
|
- Joan Rodgers
- 5 years ago
- Views:
Transcription
1 Using Microfossils to Understand Paleo-Climate Hilary Clement Olson Institute for Geophysics Jackson School of Geosciences The University of Texas at Austin
2 What are fossils? Fossils (from Latin fossus, literally "having been dug up") are the preserved remains or traces of animals, plants, and other organisms from the remote past. (10/14/2010)
3 What do you know about sand dollars? Where do they like to live? Where have you seen them in nature living? (10/14/2010)
4 Here s what we know about living sand dollars (echinoderms) Sand Dollars are widespread in ocean waters of the Northern Hemisphere, from the intertidal zone to deeper water depths. They can be found in temperate and tropical zones. So, what if we found fossil echinoderms from Cretaceous age rocks in Texas? What would we interpret about the environment? Dana-ManGeol/README.htm (10/14/2010)
5 So these fossils would indicate some kind of shallow seaway through Central Texas Fossils can tell us about: Age (=time) Environment Climate
6 Woolly Mammoth what is the significance? The stuffed Beresovka mammoth, in The Museum of Zoology, St. Petersburg (10/14/2010)
7 Example: Spain City of Malaga (10/14/2010) Average Temperatures o F o C (10/14/2010)
8 Sp-map.png (10/14/2010) Iberian sites with Mammuthus primigenius remains (from Álvarez Lao (2007). Padul is represented with a black star. Sites contemporaneous with Padul are represented with black triangles. The Padul mammoth finds On the southernmost record of Mammuthus primigenius in Europe and its southern spread during the Late Pleistocene (Álvarez-Lao et al., 2009) Palaeogeography, Palaeoclimatology, Palaeoecology
9 Sketch of global maximum distribution of the woolly mammoth (Mammuthus primigenius) during the Late Pleistocene. The Padul mammoth finds On the southernmost record of Mammuthus primigenius in Europe and its southern spread during the Late Pleistocene (Álvarez-Lao et al., 2009) Palaeogeography, Palaeoclimatology, Palaeoecology
10 Columbian mammoth Mammuthus columbi Skeleton of Columbian mammoth, Mammuthus columbi, in the George C. Page Museum at the La Brea Tar Pits, Los Angeles, California (
11 F O R A M I N I F E R A What is it? files/paleoceanography.html (10/14/2010) a.php (10/14/2010)
12 CLIMATE ANALYSIS USING PLANKTONIC FORAMINIFERA Neogloboquadrina pachyderma a.php (10/14/2010) Left-coiling (cold) less than 8 C Proxy for marine surface waters temperatures (10/14/2010) Right-coiling (warm) greater than 8 C
13 Complete the chart to normalize the data Work in pairs
14
15 Answer Key
16
17 Gulf Intraslope Basin Project Study Area
18 Globorotalia menardii Prefers warm waters in the Gulf of Mexico interglacial
19
20
21 CORES - STRATIGRAPHY SEISMIC DATA
22 PISTON Core IG 41-11
23
24 Foraminifera and Paleo-Climate Examples: Neogloboquadrina pachyderma coiling direction Globorotalia menardii migration
Looking at Fossils. Fossilized Organisms. Fossils in Rocks. Fossils in Amber
1 Looking at Fossils Key Concept Fossils provide evidence of how life and environmental conditions have changed. What You Will Learn Evidence of past life is preserved as fossils in sedimentary rock and
More informationUnit 10 Lesson 2 What Was Ancient Earth Like? Copyright Houghton Mifflin Harcourt Publishing Company
How Rocks and Fossils Tell a Story Sedimentary rock forms in layers. Many sedimentary rocks contain fossils. The oldest rock layers are at the bottom, and the youngest rock layers are at the top. The relative
More informationOutline 16: The Mesozoic World: Formation of Oil Deposits (with a side trip to the Devonian Marcellus Shale)
Outline 16: The Mesozoic World: Formation of Oil Deposits (with a side trip to the Devonian Marcellus Shale) The first commercial oil well was drilled by Colonel Edwin Drake in Titusville, Pennsylvania,
More information1 Looking at Fossils. What are fossils? How are fossils formed? What can fossils tell us about the history of life on earth?
CHAPTER 9 SECTION The History of Life on Earth 1 Looking at Fossils California Science Standards 7.3.c, 7.4.c, 7.4.e BEFORE YOU READ After you read this section, you should be able to answer these questions:
More informationName: Period: Date: ID: A. Circle the choice that best completes the statement or answers the question and write the letter on the blank.
Name: Period: _ Date: _ ID: A Unit 7 Practice Circle the choice that best completes the statement or answers the question and write the letter on the blank. 1. What term describes the movement of rock
More informationName Class Date. What are fossils? How are fossils formed? What can fossils tell us about the history of life on earth?
CHAPTER 5 2 Looking at Fossils SECTION The Fossil Record BEFORE YOU READ After you read this section, you should be able to answer these questions: What are fossils? How are fossils formed? What can fossils
More informationPaleoclimate indicators
Paleoclimate indicators Rock types as indicators of climate Accumulation of significant thicknesses of limestone and reef-bearing limestone is restricted to ~20º + - equator Gowganda tillite, Ontario
More informationATOC OUR CHANGING ENVIRONMENT
ATOC 1060-002 OUR CHANGING ENVIRONMENT Class 22 (Chp 15, Chp 14 Pages 288-290) Objectives of Today s Class Chp 15 Global Warming, Part 1: Recent and Future Climate: Recent climate: The Holocene Climate
More informationQuiz 12 Bonus 2 (9:30-9:35 AM)
Quiz 12 Bonus 2 (9:30-9:35 AM) UNIVERSITY OF SOUTH ALABAMA GY 112: Earth History Lectures 32 and 33: Mesozoic Sedimentation Instructor: Dr. Douglas W. Haywick Last Time Mesozoic Tectonics A) The Triassic
More informationEarth History & the Fossil Record
Earth History & the Fossil Record The Dynamic Earth Earth s Dynamic Geology Earth is approx. 4.6 billion years old Since its formation, the surface has been unstable Crust and Core rotate as slightly different
More informationSeep Hunt. Middle School - High School Earth s History. Concepts. Objectives. Outline. Duration minutes. Locations La Brea Tar Pits Museum
Middle School - High School Earth s History Duration 30-45 minutes Concepts Southern California is tectonically unique. Locations La Brea Tar Pits Museum Tectonic activity in Southern California helped
More informationCh. 17 Review. Life in the Cretaceous
Ch. 17 Review Life in the Cretaceous Diversification of diatoms, planktonic forams, calcareous nannoplankton Diversification of mobile predators (especially mollusks and teleost fishes) Origin of the angiosperms
More informationThe History of Life. Section 3-2. The Fossil Record
The History of Life Section 3-2 The Fossil Record The History of Life Draw a line that has as many inches as you have years. Mark the years at every inch. For each year, record at least one major event
More informationSurface Circulation. Key Ideas
Surface Circulation The westerlies and the trade winds are two of the winds that drive the ocean s surface currents. 1 Key Ideas Ocean water circulates in currents. Surface currents are caused mainly by
More informationPlease review your abstract submission. If the abstract is final, click "Submit Abstract" below to complete your submission.
Please review your abstract submission. If the abstract is final, click "Submit Abstract" below to complete your submission. SUBMIT ABSTRACT Oxygen isotope stratigraphy in the Gulf of Alaska (IODP Exp.
More informationThe Great Ice Ages. Copyright abcteach.com 2001 Graphics from Art Today
The Great Ice Ages The Great Ice Ages occurred during the Pleistocene epoch. The word epoch means time period. This period began about 2.5 million years ago and ended roughly 10,000 years ago. During the
More informationDiversity, Change and Continuity. History of Life
Diversity, Change and Continuity History of Life Change throughout the history of Life. A summary of content covered 1 2 3 4 Changes in the atmosphere Changes in climate Geological events Biogeography
More informationPLATE 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 informationModule 9: Earth s History Topic 4 Content: Formation of Fossils Notes
Introduction There are a variety of ways in which fossils can form. In this interactivity, click on each of the thumbnail images in the panel to explore the types of fossils and their formation. 1 Tar
More informationBiodiversity Through Earth History. What does the fossil record tell us about past climates and past events?
Biodiversity Through Earth History What does the fossil record tell us about past climates and past events? Useful terminology: Evolution Natural Selection Adaptation Extinction Taxonomy Logistic Growth
More informationLecture Title ( Fossils ) & Date. Main Ideas/Lecture Topics/Questions. Big Ideas or Chunking the Lecture
Lecture Title ( Fossils ) & Date Main Ideas/Lecture Topics/Questions Big Ideas or Chunking the Lecture Fossil Trilobites Point of View #1 Natural selection provides a scientific explanation for the fossil
More informationDetermining the age of fossils
Sea shells seem to be everywhere. Most of the time you will find them on beaches, but every now and then, you may find them far from the sea. For example, you may have found a shell stuck in a rock high
More informationThermal / Solar. When air is warmed it... Rises. Solar Energy. Evaporation. Condensation Forms Clouds
Thermal / Solar Light from the Sun is transformed into what type of energy when it hits Earth's surface? Rises When air is warmed it... Solar Energy Water moves through the water cycle using what type
More informationGlobal 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 informationnetw rks Guided Reading Activity Essential Question: How does geography influence the way people live? Earth's Physical Geography
Guided Reading Activity Lesson 1 Earth and the Sun Essential Question: How does geography influence the way people live? Looking at Earth Directions: What are the layers that make up Earth? Use your textbook
More informationFossils and EH LT3 & 4
Fossils and EH LT3 & 4 Grade:«grade» Subject:Fossils and EH Date:«date» Dec 3 6:48 AM 1 1 An organism is most likely to become an index fossil if it lived for a A short period of time and was geographically
More informationGY 112 Lecture Notes Significance of Fossils: Paleogeography Interpretations
GY 112 Lecture Notes D. Haywick (2006) 1 GY 112 Lecture Notes Significance of Fossils: Paleogeography Interpretations Lecture Goals: A) What is paleogeography? B) How it works (Late Cambrian fantasy example)
More informationChemostratigraphic and Paleoenvironmental Analysis of Rudist Facies in Cretaceous Strata
Chemostratigraphic and Paleoenvironmental Analysis of Rudist Facies in Cretaceous Strata Luis González, Hernan Santos (UPRM), Robert H. Goldstein, Alvin Bonilla STATUS: Long-term project near completion
More informationLecture 18 Paleoceanography 2
Lecture 18 Paleoceanography 2 May 26, 2010 Trend and Events Climatic evolution in Tertiary Overall drop of sea level General cooling (Figure 9-11) High latitude (deep-water) feature Two major step Middle
More informationPleistocene 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 informationA multi-proxy study of planktonic foraminifera to identify past millennialscale. climate variability in the East Asian Monsoon and the Western Pacific
This pdf file consists of all pages containing figures within: A multi-proxy study of planktonic foraminifera to identify past millennialscale climate variability in the East Asian Monsoon and the Western
More informationPhytoplankton. Zooplankton. Nutrients
Phytoplankton Zooplankton Nutrients Patterns of Productivity There is a large Spring Bloom in the North Atlantic (temperate latitudes remember the Gulf Stream!) What is a bloom? Analogy to terrestrial
More informationStudying The Past. Why Do We Study Fossils Found in Rocks?
I. What is a Fossil? Studying The Past A. Definition: The evidence or remains of once-living plants or animals Why Do We Study Fossils Found in Rocks? QQ#1 what is a fossil? Why are they important? A.
More informationAir sea temperature decoupling in western Europe during the last interglacial glacial transition
María Fernanda Sánchez Goñi, Edouard Bard, Amaelle Landais, Linda Rossignol, Francesco d Errico SUPPLEMENTARY INFORMATION DOI: 10.1038/NGEO1924 Air sea temperature decoupling in western Europe during the
More informationTo understand how we measure ancient temperature, you need to know about oxygen isotopes. Pleistocene Climate. Clouds, rain, and oxygen isotopes
To understand how we measure ancient temperature, you need to know about oxygen isotopes Pleistocene Climate Alan R. Rogers February 20, 2014 There are several types of oxygen atoms, called isotopes The
More informationChapter 15 Millennial Oscillations in Climate
Chapter 15 Millennial Oscillations in Climate This chapter includes millennial oscillations during glaciations, millennial oscillations during the last 8000 years, causes of millennial-scale oscillations,
More information1 What Is Climate? TAKE A LOOK 2. Explain Why do areas near the equator tend to have high temperatures?
CHAPTER 17 1 What Is Climate? SECTION Climate BEFORE YOU READ After you read this section, you should be able to answer these questions: What is climate? What factors affect climate? How do climates differ
More informationPaleoclimatology ATMS/ESS/OCEAN 589. Abrupt Climate Change During the Last Glacial Period
Paleoclimatology ATMS/ESS/OCEAN 589 Ice Age Cycles Are they fundamentaly about ice, about CO2, or both? Abrupt Climate Change During the Last Glacial Period Lessons for the future? The Holocene Early Holocene
More informationModule 11: Meteorology Topic 3 Content: Climate Zones Notes
Introduction Latitude is such an important climate factor that you can make generalizations about a location's climate based on its latitude. Areas near the equator or the low latitudes are generally hot
More informationOcean s Influence on Weather and Climate
Earth is often called the Blue Planet because so much of its surface (about 71%) is covered by water. Of all the water on Earth, about 96.5%, is held in the world s oceans. As you can imagine, these oceans
More informationA Trip Through Geologic Time
Date Class _ A Trip Through Geologic Time Chapter Test A Multiple Choice Write the letter of the correct answer on the line at the left. 1. Late in the Paleozoic Era, the supercontinent Pangaea formed.
More information(Brown & Loucks, 2009)
SECARB Phase 3, Task 15 Geological CO 2 Sequestration Capacity Estimate Offshore Northern Gulf of Mexico March 9, 2011 Prepared by David L. Carr Project Team: Cari Breton, GIS Analyst David L. Carr, Reservoir
More informationUnit 2: Geology of Tsikw aye (Mesa Prieta)
Unit 2 page 9 Name: Date: GEOLOGIC HISTORY OF MESA PRIETA: Student Information Sheet: Activity 2 Looking at Mesa Prieta today, with its tumbled black basalt boulders, prickly pear cacti and an occasional
More informationOrganisms in the Ocean
Oceans Objective 8.E.1.2 Summarize evidence that Earth's oceans are a reservoir of nutrients, minerals, dissolved gases, and life forms: estuaries, marine ecosystems, upwelling, and behavior of gases in
More informationFOSSIL "FUN"DAMENTALS
NAME DATE PARTNER(S) FOSSIL "FUN"DAMENTALS You are taking a stroll on a beach in Calvert or southern Charles County when you come across a shark s tooth laying in the sand at the water s edge. You pick
More informationCredit: Adapted from NASA/JPL Caltech
Credit: Adapted from NASA/JPL Caltech Three Puzzling Ice Age Mysteries 1. Sudden return of Ice Age temperatures 12,800 years ago After about 1400 years of warming, temperatures plunged 10 C (50 F) That
More informationlecture 12 Paleoclimate
lecture 12 Paleoclimate OVERVIEW OF EARTH S CLIMATIC HISTORY Geologic time scales http://www.snowballearth.org/index.html Features of the climate during the Cretaceous period the land-sea distribution
More informationJoides Resolution at Hong-Kong
Report from Iván Hernández-Almeida, post-doc at the Oeschger Centre for Climate Change Research/Institute of Geography, University of Bern. Shipboard Micropaleontologist (radiolarian specialist) on IODP
More informationMOR SEAWAY TEACHERS. A CHANGING LANDSCAPE Activity Overview BIG IDEA
MOR SEAWAY 03 Activity Overview BIG IDEA The Earth and its landscapes change over time. Scientists use the fossil record to understand the Earth s environments and climates millions of years ago. OBJECTIVE
More information4th Grade U.S. Regional Geography
4th Grade U.S. Regional Geography Multiple Choice Identify the choice that best completes the statement or answers the question. What does the term mainland mean in the sentence above? A the continent
More informationWe re living in the Ice Age!
Chapter 18. Coping with the Weather: Causes and Consequences of Naturally Induce Climate Change 지구시스템의이해 We re living in the Ice Age! 1 Phanerozoic Climate 서늘해지고 더웠고 따뜻했고 3 Climate Rollercoaster 4 2 Time
More informationChatham Rise Phosphorite. Observations from the literature
Chatham Rise Phosphorite Observations from the literature Content 1. Where is it? 2. Why is it there? i. Stratigraphy ii. Structure iii. GONDWANA iv. Ocean circulation v. Ocean fronts 3. The answer...
More informationTopic 5: The Dynamic Crust (workbook p ) Evidence that Earth s crust has shifted and changed in both the past and the present is shown by:
Topic 5: The Dynamic Crust (workbook p. 65-85) Evidence that Earth s crust has shifted and changed in both the past and the present is shown by: --sedimentary horizontal rock layers (strata) are found
More informationOcean Currents and Climate
Ocean Currents and Climate Ocean water contains streamlike movements of water called ocean currents. Currents are influenced by a number of factors, including weather, the Earth's rotation, and the position
More informationFossils. Presented by Kesler Science
Presented by Kesler Science Essential Questions: 1. What are fossils? 2. What are some different types of fossilization? 3. What is the difference between relative and absolute age? 4. What does the fossil
More information3. 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 informationFossils & The Geologic Time Scale
Fossils & The Geologic Time Scale Fossils Preserved remains or traces of an organism that lived in the past. Fossils are formed when organisms die and are buried in sediment. Eventually the sediment builds
More informationWhat happened Before. reflect
reflect Sea shells seem to be everywhere. Most of the time, you will find them on beaches. But every now and then, you might find them far from the sea. For example, you might find a shell stuck in a rock
More informationChapter: Clues to Earth s Past
Table of Contents Chapter: Clues to Earth s Past Section : Section 2: Relative Ages of Rocks Section 3: Absolute Ages of Rocks Traces of the Distant Past Paleontologists, scientists who study fossils,
More informationQuaternary Geology For Geology BSc. Students, Tanta University, Ali Soliman 1
Quaternary Geology For Geology BSc. Students, Tanta University, Ali Soliman 1 Elements of Quaternary Geology Quaternary Geology For Geology BSc. Students, Tanta University, Ali Soliman 2 Quaternary Geology
More informationLatest Press Release. sarah palin leg show
corp@stantec.com Latest Press Release sarah palin leg show S The South Texas Sand Sheet, also known as the Coastal Sand Plains and the Llano Mesteño, occupies more than two million acres at the southern
More informationQuarterly Assessment 4 Review answers
Quarterly Assessment 4 Review answers Metric Conversions (Review from QA 1, 2 and 3) Directions: Fill in the missing parts to the chart below. Kilo Hecto UNIT Deci Centi 1000 100 10 1 0.1 0.01 0.001 Km
More informationGeologic History of Texas: The Making of Texas Over 1.5 Billion Years
# 4 Geologic History of Texas: The Making of Texas Over 1.5 Billion Years Dr. Richard Kyle March 24, 2000 Produced by and for Hot Science - Cool Talks by the Environmental Science Institute. We request
More informationLatitude and Longitude
Seafloor Magnetism, Seafloor Spreading: Developing the Theory of Plate Tectonics Graphics: (top) Earth topography, (bottom) Garrison, Fig. 3.14. Earthquakes and the Dynamic Earth The Earth is not entirely
More information2. Can you describe how temperature and dissolved solids changes the density of water?
Unit 4: Oceanography LT 4.1 Density: I can explain the role density plays to help form some currents. #1 Yes I can: 1. Can you explain what density is and how you calculate it? 2. Can you describe how
More informationKIPP: Inspire Academy Social Studies Benchmark 1 PART I. Use the map of Missouri to answer questions 7-9.
PART I 1) A physical map key shows: A. Climate B. Cities and borders C. Elevation and water depth D. Geographic features Use the map of Missouri to answer questions 7-9. 2) Lines of latitude: A. Are parallel
More informationStudent Workbook California Education and the Environment Initiative. Science Standard 7.4.g. Extinction: Past and Present
7 Student Workbook California Education and the Environment Initiative Science Standard 7.4.g. Extinction: Past and Present California Education and the Environment Initiative Approved by the California
More informationUNIT 5: ECOLOGY Chapter 15: The Biosphere
CORNELL NOTES Directions: You must create a minimum of 5 questions in this column per page (average). Use these to study your notes and prepare for tests and quizzes. Notes will be stamped after each assigned
More informationOffshore Geosequestration Potential in the Gulf of Mexico. Carbon Sequestration Opportunities in the North Sea Conference March, 2010
Offshore Geosequestration Potential in the Gulf of Mexico Presenter: Ramón Treviño Gulf Coast Carbon Center Bureau of Economic Geology University of Texas at Austin, Carbon Sequestration Opportunities
More informationScience 20. Unit C: The Changing Earth. Assignment Booklet C3
Science 20 Unit C: The Changing Earth Assignment Booklet C3 FOR TEACHER S USE ONLY Summary Teacher s Comments Chapter 3 Assignment Total Possible Marks 45 Your Mark Science 20 Unit C: The Changing Earth
More informationWhat is the Earth s time scale?
Earth History 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 fossils world wide.
More informationDecoupling Allogenic Forcing from Autogenic Processes: Experimental Stratigraphy. Wonsuck Kim
Decoupling Allogenic Forcing from Autogenic Processes: Experimental Stratigraphy Wonsuck Kim Department of Geological Sciences and Institute for Geophysics, Jackson School of Geosciences, University of
More informationObjective 3: Earth and Space Systems
Name Class Period: Objective 3: Earth and Space Systems 1. The diagram above shows the orbit of the moon around Earth. At which point in the moon s orbit will a person standing on Earth see a waxing crescent
More informationNatural 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 informationObserved changes in climate and their effects
1 1.1 Observations of climate change Since the TAR, progress in understanding how climate is changing in space and time has been gained through improvements and extensions of numerous datasets and data
More informationMASTERY ASSIGNMENT 2015
Climate & Meteorology MASTERY ASSIGNMENT 2015 Directions: You must submit this document via Google Docs to lzimmerman@wcpss.net. The document must include the questions and pictures must be hand drawn
More informationNAME: GEL 109 Final Winter 2010
GEL 109 Final Winter 2010 1. The following stratigraphic sections represents a single event followed by the slow accumulation of background sedimentation of shale. Describe the flows that produced the
More informationActivity #2 - Major Ocean Surface Currents
Activity #2 - Major Ocean Surface Currents Concepts # 3 & 6 # 3 Atmospheric cells and ocean gyres redistribute heat from low to high latitudes, which influences climate, weather, and ocean temperature.
More informationStudying The Past. II. Why Do We Study Fossils Found in Rocks?
Studying The Past I. What is a Fossil? A. Definition: The evidence or remains of once-living plants or animals II. Why Do We Study Fossils Found in Rocks? A. To provide evidence of the past existence of
More informationSedimentation. Ocean Sediments Chapter 5. Paleoceanography. Lecture #6 Week #4. A.K. Morris, Ph.D.
Sedimentation Ocean Sediments Chapter 5 A time capsule to the past Principle of superposition going deeper in the sediment means looking further into the past Oceanography Lecture #6 1 2 Fig. 5.1 Paleoceanography
More informationExtinctions & 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 informationSupplementary Figure 1. New downcore data from this study. Triangles represent the depth of radiocarbon dates. Error bars represent 2 standard error
Supplementary Figure 1. New downcore data from this study. Triangles represent the depth of radiocarbon dates. Error bars represent 2 standard error of measurement (s.e.m.). 1 Supplementary Figure 2. Particle
More informationBiogeography. An ecological and evolutionary approach SEVENTH EDITION. C. Barry Cox MA, PhD, DSc and Peter D. Moore PhD
Biogeography An ecological and evolutionary approach C. Barry Cox MA, PhD, DSc and Peter D. Moore PhD Division of Life Sciences, King's College London, Fmnklin-Wilkins Building, Stamford Street, London
More informationReading Material. See class website. Sediments, from Oceanography M.G. Gross, Prentice-Hall
Reading Material See class website Sediments, from Oceanography M.G. Gross, Prentice-Hall Materials filling ocean basins Dissolved chemicals especially from rivers and mid-ocean ridges (volcanic eruptions)
More informationWELCOME TO PERIOD 14:CLIMATE CHANGE. Homework #13 is due today.
WELCOME TO PERIOD 14:CLIMATE CHANGE Homework #13 is due today. Note: Homework #14 due on Thursday or Friday includes using a web site to calculate your carbon footprint. You should complete this homework
More informationA fossil is the preserved remains of a once-living organism.
What is a fossil? A fossil is the preserved remains of a once-living organism. What do fossils tell us? Fossils give clues about organisms that lived long ago. They help to show that evolution has occurred.
More informationGlobal Climate Change
Global Climate Change Overview: Students will learn about global climate change, what causes global warming, and scientific projections about climate change in the near future. Levels V-VI Grades 9-12
More informationHOW 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 informationPaleobotanical Estimates of Climate in Deep Time: Two Examples From the Late Cretaceous of Western North America
Paleobotanical Estimates of Climate in Deep Time: Two Examples From the Late Cretaceous of Western North America Garland Upchurch 1, Ann Marie Prue 1, Joan Parrott 1, Emilio Estrada-Ruiz 2, and Dori Contreras
More informationReservoirs and Production
Lesson Plan Page 1 Topic: Reservoirs and production Topic Overview: Porosity refers to the percentage of holes (pores) in the rock. Permeability is the ability of fluids to travel through porous rocks.
More informationEcosystems Chapter 4. What is an Ecosystem? Section 4-1
Ecosystems Chapter 4 What is an Ecosystem? Section 4-1 Ecosystems Key Idea: An ecosystem includes a community of organisms and their physical environment. A community is a group of various species that
More informationOnline Fossil Lab Fossil Formation How Fossils Form 1. Describe the process in which fossils form.
Name: Online Fossil Lab Fossil Formation How Fossils Form 1. Describe the process in which fossils form. Period: 2. What is a Mold? 3. What is a cast? Getting into the Fossil Record 4. What is the fossil
More informationDevelopment 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 informationFossil Clues Teacher s Notes
Fossils are the remains of living things which have been changed into rock. The father of modern geology, James Hutton, said that we can interpret the nature of creatures from the past and the environment
More informationVirginia Standards of Learning correlated to Reading Essentials in Science Perfection Learning Corporation
Earthquakes Floods Tornadoes Hurricanes Volcanoes Erosion Forecasting Natural Disasters Records and Oddities Seasons and Patterns Are We Alone? The Case for Extraterrestrial Life Inside a Star Lights in
More informationEQ: Discuss main geographic landforms of the U.S. & Canada and examine varied landforms in relation to their lifestyles.
EQ: Discuss main geographic landforms of the U.S. & Canada and examine varied landforms in relation to their lifestyles. Places & Terms for Discussion Appalachian Mountains Great Plains Canadian Shield
More informationFascinating Fossils Grades 4-8
Fascinating Fossils Grades 4-8 This activity introduces students to a variety of fossils: large animal bones, small fragment pieces, and microfossils. Students will analyze fossils like that of a field
More informationGulf of México Mapping NATCARB Atlas
Gulf of México Mapping NATCARB Atlas Presenter: Ramón Treviño Gulf Coast Carbon Center University of Texas at Austin, Bureau of Economic Geology NACAP Cuernavaca, Morelos, México March 9, 2010 Acknowledgements
More informationWorld Geography. BY MARK STANGE and REBECCA LARATTA
BY MARK STANGE and REBECCA LARATTA COPYRIGHT 2002 Mark Twain Media, Inc. ISBN 1-58037-205-8 Printing No. CD-1551 Mark Twain Media, Inc., Publishers Distributed by Carson-Dellosa Publishing Company, Inc.
More informationUnit 5 Possible Test Questions Mesozoic and Cenozoic Eras HISTORICAL GEOLOGY
Revised 8/16 Unit 5 Possible Test Questions Mesozoic and Cenozoic Eras HISTORICAL GEOLOGY Mesozoic Era Eons, Eras and Periods 1. List the Mesozoic periods in order (oldest to youngest). End of the Paleozoic
More information