DATA REPOSITORY ITEM
|
|
- Arabella Turner
- 5 years ago
- Views:
Transcription
1 Powell DATA REPOSITORY ITEM 0003 TABLE DR. LITERATURE-DERIVED SAMPLES USED IN THIS STUDY Study Interval* Facies Taxon N # S ** Elias and Young, 8 Ord./Sil. Carbonate Coral 58 0 Elias and Young, 8 Ord./Sil. Carbonate Coral 3 7 Elias and Young, 8 Ord./Sil. Carbonate Coral Elias and Young, 8 Ord./Sil. Carbonate Coral 7 5 erhoff, 9 Penn. Carb./Sil. Crinoid 5 4 erhoff, 9 Penn. Carb./Sil. Crinoid 47 9 erhoff, 9 Penn. Carb./Sil. Crinoid 57 9 erhoff, 9 Penn. Carb./Sil. Crinoid 30 6 erhoff, 9 Penn. Carb./Sil. Crinoid 39 erhoff, 9 Penn. Carb./Sil. Crinoid 63 5 erhoff, 9 Penn. Carb./Sil. Crinoid 47 erhoff, 9 Penn. Carb./Sil. Crinoid 334 erhoff, 9 Penn. Carb./Sil. Crinoid 47 9 erhoff, 9 Penn. Carb./Sil. Crinoid 83 6 erhoff, 9 Penn. Carb./Sil. Crinoid erhoff, 9 Penn. Carb./Sil. Crinoid erhoff, 9 Penn. Carb./Sil. Crinoid 53 8 erhoff, 9 Penn. Carb./Sil. Crinoid 8 8 erhoff, 9 Penn. Carb./Sil. Crinoid 06 erhoff, 9 Penn. Carb./Sil. Crinoid 36 0 erhoff, 9 Penn. Carb./Sil. Crinoid 90 erhoff, 9 Penn. Carb./Sil. Crinoid 7 0 erhoff, 9 Penn. Carb./Sil. Crinoid erhoff, 9 Penn. Carb./Sil. Crinoid 04 5 erhoff, 9 Penn. Carb./Sil. Crinoid 65 erhoff, 9 Penn. Carb./Sil. Crinoid 00 9 erhoff, 9 Penn. Carb./Sil. Crinoid 39 0 erhoff, 9 Penn. Carb./Sil. Crinoid 57 3 ing, 9 Cambrian Mud All 08 7 ing, 9 Cambrian Mud All 63 4 ing, 9 Cambrian Mud All 79 5 ing, 9 Cambrian Mud All ing, 9 Cambrian Mud All 45 9 ing, 9 Cambrian Mud All 6 9 ing, 9 Cambrian Mud All ing, 9 Cambrian Mud All 30 6 Neuman, 4 Ordovician Mud All kowsky, 9 Ordovician Carbonate Brach 6 7 kowsky, 9 Ordovician Carbonate Brach 49 7 kowsky, 9 Ordovician Carbonate Brach 97 5 kowsky, 9 Ordovician Carbonate Brach 5 7 kowsky, 9 Ordovician Carbonate Brach 6 kowsky, 9 Ordovician Carbonate Brach 98 4 kowsky, 9 Ordovician Carbonate Brach 93 kowsky, 9 Ordovician Carbonate Brach 9 5 kowsky, 9 Ordovician Carbonate Brach 09 5 kowsky, 9 Ordovician Carbonate Brach 9 kowsky, 9 Ordovician Carbonate Brach 40 3 kowsky, 9 Ordovician Carbonate All 33 5 kowsky, 9 Ordovician Carbonate All 3 7 kowsky, 9 Ordovician Carbonate All 3 5 kowsky, 9 Ordovician Carbonate All 98 kowsky, 9 Ordovician Carbonate All 03 5 kowsky, 9 Ordovician Carbonate All 50 3 kowsky, 9 Ordovician Carbonate All 40 7 kowsky, 9 Ordovician Carbonate All 7 4
2 kowsky, 9 Ordovician Carbonate All 73 0 kowsky, 9 Ordovician Carbonate All 64 kowsky, 9 Ordovician Carbonate All 84 4 kowsky, 9 Ordovician Carbonate All 88 kowsky, 9 Ordovician Carbonate All 0 kowsky, 9 Ordovician Carbonate All 83 9 Romano and Owen, 3 Ordovician Shale Trilo bert and Bottjer, 9 Triassic Carbonate All 67 4 bert and Bottjer, 9 Triassic Carbonate All 07 6 bert and Bottjer, 9 Triassic Carbonate All 56 6 bert and Bottjer, 9 Triassic Carbonate All 48 8 bert and Bottjer, 9 Triassic Carbonate All 97 8 bert and Bottjer, 9 Triassic Carbonate All 38 bert and Bottjer, 9 Triassic Carbonate All 3 8 bert and Bottjer, 9 Triassic Carbonate All bert and Bottjer, 9 Triassic Carbonate All 46 0 bert and Bottjer, 9 Triassic Carbonate All 0 3 bert and Bottjer, 9 Triassic Carbonate All 4 bert and Bottjer, 9 Triassic Carbonate All 53 7 bert and Bottjer, 9 Triassic Carbonate All bert and Bottjer, 9 Triassic Carbonate All 09 9 Watkins, 3 Silurian Carbonate All Watkins, 3 Silurian Carbonate All Watkins, 3 Silurian Carbonate All 33 Watkins, 3 Silurian Carbonate All West, 976 Ordovician Sand/silt All 80 9 West, 976 Silurian Sand All West, 976 Miss. Shale All West, 976 Permian Mud All 37 3 West, 976 Cretaceous Sand All West, 976 Recent Sand All 5 8 lewski et al., 000 Miocene Mud Moll 47 lewski et al., 000 Miocene Mud Moll lewski et al., 000 Miocene Sand Moll lewski et al., 000 Miocene Sand Moll lewski et al., 000 Miocene Sand Moll lewski et al., 000 Miocene Sand Moll lewski et al., 000 Miocene Sand Moll 47 3 lewski et al., 000 Miocene Sand Moll lewski et al., 000 Miocene Mud Moll 9 8 lewski et al., 000 Miocene Mud Moll 3 6 lewski et al., 000 Miocene Sand Moll 7 36 lewski et al., 000 Miocene Sand Moll 38 3 lewski et al., 000 Miocene Sand Moll 5 3 lewski et al., 000 Miocene Sand Moll 38 3 lewski et al., 000 Miocene Mud Moll 5 3 lewski et al., 000 Miocene Mud Moll lewski et al., 000 Miocene Mud Moll 43 0 lewski et al., 000 Miocene Mud Moll lewski et al., 000 Miocene Mud Moll 57 3 lewski et al., 000 Miocene Mud Moll lewski et al., 000 Miocene Mud Moll lewski et al., 000 Miocene Mud Moll 44 7 Budd et al., 9 Plio./Pleis. Carbonate Coral 35 6 Budd et al., 9 Plio./Pleis. Carbonate Coral 45 4 Budd et al., 9 Plio./Pleis. Carbonate Coral 0 Budd et al., 9 Plio./Pleis. Carbonate Coral 94 Peters and Bork, 9 Silurian Shale All Peters and Bork, 9 Silurian Shale All 97 7 Peters and Bork, 9 Silurian Shale All be and Allmon, 4 Eocene Sand Moll be and Allmon, 4 Eocene Sand Moll Powell
3 Powell 3 be and Allmon, 4 Eocene Sand Moll be and Allmon, 4 Eocene Sand Moll be and Allmon, 4 Eocene Sand Moll be and Allmon, 4 Eocene Sand Moll be and Allmon, 4 Eocene Sand Moll be and Allmon, 4 Eocene Sand Moll 4 38 be and Allmon, 4 Eocene Sand Moll be and Allmon, 4 Eocene Sand Moll be and Allmon, 4 Eoc Sand Moll 300 nger, 98 Ord Shale All 8 7 nger, 98 Ord Shale All 67 6 nger, 98 Ord Shale All 05 9 nger, 98 Ord Shale All 0 8 nger, 98 Ord Shale All 50 8 nger, 98 Ord Shale All 4 8 nger, 98 Ord Shale All 00 8 nger, 98 Ord Shale All 85 4 nger, 98 Ord Shale All 7 nger, 98 Ord Shale All 4 nger, 98 Ord Shale All 9 9 nger, 98 Ord Shale All 58 9 nger, 98 Ord Shale All 3 nger, 98 Ord Shale All 34 6 nger, 98 Ord Shale All 50 4 nger, 98 Ord Shale All 00 nger, 98 Ord Shale All 48 5 nger, 98 Ord Sand All 98 3 nger, 98 Ord Sand All 45 5 nger, 98 Ord Sand All 00 8 *Ord. = Ordovician, Sil. = Silurian, Penn. = Pennsylvanian, Miss. = Mississippian, Plio. = Pliocene, Pleis. = Pleistocene. Carb. = Carbonate, Sil. = Siliciclastic. Moll. = Mollusks, Brach. = Brachiopods, Trilo. = Trilobites, All = all preservable taxa. # N = number of specimens collected. **S = number of genera collected. DATA SET REFERENCES Budd, A.F., Johnson, K.G., Stemann, T.A., and Tompkins, B.H., 9, Pliocene to Pleistocene reef coral assemblages in the Limon Group of Costa Rica, in Collins, L.S., and Coates, A.G., eds., A paleobiotic survey of Caribbean faunas from the Neogene of the Isthmus of Panama: Ithaca, NY, Paleontological Research Institution, p be, E.A., and Allmon, W.D., 4, Effects of sampling on paleoecologic and taphonomic analyses in high-diversity fossil accumulations; an example from the Eocene Gosport Sand, Alabama: Lethaia, v. 7, p Elias, R.J., and Young, G.A., 8, Coral diversity, ecology, and provicial structure during a time of crisis; the latest Ordovician to earliest Silurian Edgewood Province in Laurentia: Palaios, v. 3, p 98-. erhoff, P.F., 9, Crinoid biofacies in Upper Carboniferous cyclothems, Midcontinent North America;
4 Powell 4 faunal tracking and the role of regional processes in biofacies recurrence: Palaeogeogrpahy, Palaeoclimatology, Palaeoecology, v. 7, p lewski, M., Gürs, K., Nebelsick, J.H., Oschmann, W., Piller, W.E., and Hoffmeister, A.P., 00, Multivariate hierarchical analyses of Miocene mollusk assemblages of Europe: Paleogeographic, paleoecological, and biostratigraphic implications: Geological Society of America Bulletin, v. 4, in press. ing, E., 9, Upper Placentian-Branchian series of mainland Nova Scotia (Middle-Upper Lower Cambrian); faunas, paleoenvironments, and stratigraphic revision: Journal of Paleontology, v. 69, p Neuman, R.B., 4, Late Ordovician (Ashgill) Foliomena fauna brachiopods from northeastern Maine: Journal of Paleontology, v. 68, p kowsky, M.E., 9, Gradient analysis of Middle Ordovician brachiopod biofacies; biostratigraphic, biogeographic, and macroevolutionary implications: Palaios, v. 0, p kowsky, M.E., 9, Biofacies replacement in a sequence stratigraphic framework; Middle and Upper Ordovician of the Nashville Dome, Tennessee, USA: Palaios, v. 4, p 30, 37. Peters, S.E., and Bork, K.B., 9, Species-abundance models; an ecological approach to inferring paleoenvironment and resolving paleoecological change in the Waldron Shale (Silurian): Palaios, v. 4, p Romano, M., and Owen, A.W., 3, Early Caradoc trilobites of eastern Ireland and their palaeogeographical significance: Palaeontology, v. 36, p bert, J.K., and Bottjer, D.J., 9, Aftermath of the Permian-Triassic mass extinction event; paleoecology of Lower Triassic carbonates in the Western USA: Palaeogeography, Palaeoclimatology, Palaeoecology, v. 6, p -39. nger, D.A., 98, Community gradients in the Martinsburg formation (Ordovician), southwestern Virginia, [Ph.D. Thesis]: Virginia Polytechnic Institute and State University, pp 36. Watkins, R., 3, The Silurian (Wenlockian) reef fauna of southeastern Wisconsin: Palaios, v. 8, p West, R.R., 976, Comparison of seven lingulid communities, in Scott, R. W., and West, R. R., eds., Structure and classification of paleocommunities: Stroudsburg, PA, Dowden, Hutchinson & Ross, Inc., p 7-9.
5 Powell 5 FIGURE DR 90 Cumulative Abundance A B C Cumulative Diversity Figure DR. Example of mean abundance vs. diversity curve (MAD) for taxa in one sample. A: Mean curve constructed from 000 subsamples. B: Maximum evenness curve. C: Maximum deviation of mean curve from maximum evenness curve (Kolmogorov-Smirnov D statistic). TABLE DR. RAW DATA SETS ABBREVIATED BY FIRST 4 LETTERS OF CITATION AND LAST TWO DIGITS OF PUBLICATION YEAR. NUMBERS REPRESENT COUNTS OF SPECIMENS FOR EACH GENUS. GENERA ARRANGED ACCORDING TO THEIR RELATIVE ABUNDANCE (E.G., FIRST ROW OF NUMBERS REPRESENTS THE MOST ABUNDANT GENUS IN A GIVEN DATA SET AND SO ON). Elia 98 Elia 98 Elia 98 Elia
6 Powell
7 Powell 7 Neum
8 Powell Roma
9 Powell 9 Watk 93 Watk 93 Watk 93 Watk 93 West 76 West 76 West 76 West 76 West 76 West
10 Powell 0
11 Powell
12 Powell Budd Budd Budd Budd Pete Pete Pete
13 Powell
14 Powell
Geographic coordinates (longitude and latitude) of terrestrial and marine fossil collections of
1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 DATA REPOSITORY Recurrent Hierarchical Patterns and the Fractal Distribution of Fossil Localities Materials and Methods Geographic coordinates
More informationGeologic Time. Geologic Events
Geologic Time Much of geology is focused on understanding Earth's history. The physical characteristics of rocks and minerals offer clues to the processes and conditions on and within Earth in the past.
More informationTIME LINE OF LIFE. Strip for Clock of Eras representing the circumference. 1. Review the eras represented on the Clock of Eras:
TIME LINE OF LIFE Material Time Line of Life Working Time Line of Life Clock of Eras Strip for Clock of Eras representing the circumference Elastic strip for Clock of Eras Presentation 1: Overview 1. Review
More informationTHE 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 informationTIME. Does not give the. Places events in sequencee 1 st, 2 nd, 3 rd. Gives a. exact date of an event. event. Radioactive Dating.
Geologic History TIME Places events in sequencee 1 st, 2 nd, 3 rd Does not give the exact date of an event Gives a date or time of an event Uses the Law of Superposition Radioactive Dating Youngest Law
More informationField trip to Racine Reef Complex, Thornton Quarry, Illinois
Field trip to Racine Reef Complex, Thornton Quarry, Illinois Primary objectives for this fieldtrip 1) Collect and identify the fossils of the Racine Reef Complex. 2) Discuss procedures for collecting fossil
More informationOrdovician. The Cincinnatian and the Richmondian Invasion
Ordovician The Cincinnatian and the Richmondian Invasion P. David Polly Department of Geological Sciences Indiana University Bloomington, Indiana 47405 USA pdpolly@indiana.edu The Cincinnatian (painting
More informationDroser, M., Bottjer, D.J., A semiquantitative field classification of ichnofabric. Journal of Sedimentary Petrology 56,
GSA Data Repository 2015329 Chemosymbiont-dominated seafloor communities in modern and Cretaceous upwelling systems support a new, high-productivity variant of standard low-oxygen models Y. Edelman-Furstenberg
More informationSAMPLE QUESTIONS FOR GEOLOGY 103, TEST 1
SAMPLE QUESTIONS FOR GEOLOGY 103, TEST 1 The correct answers are listed at the bottom (no peeking!). These questions are to give you an idea of the type of questions that will be asked. They are not a
More informationGenus-level versus species-level extinction rates
Acta Geologica Polonica, Vol. 66 (2016), No. 3, pp. 261 265 DOI: 10.1515/agp-2016-0012 Genus-level versus species-level extinction rates JERZY TRAMMER Faculty of Geology, University of Warsaw, ul. Żwirki
More informationScience Data Representation Questions: Strategies and Sample Questions
Science Data Representation Questions: Strategies and Sample Questions Focus on understanding what information is given. Review any additional information given (descriptive paragraphs, headings, scale
More informationThe Significance of the Fossil Record ( Susan Matthews and Graeme Lindbeck)
The Significance of the Fossil Record ( Susan Matthews and Graeme Lindbeck) The fossil record indicates the evolutionary history of life. Many events together, including: continental drift, changes in
More informationEarth s s Geologic History
The Earth s s Geologic History and The Earth s s Interior Earth s s Geologic History Geologic timescale Divides Earth s s history into relative time periods Relative dating based on: (apply for entire
More informationPhanerozoic Diversity and Mass Extinctions
Phanerozoic Diversity and Mass Extinctions Measuring Diversity John Phillips produced the first estimates of Phanerozoic diversity in 1860, based on the British fossil record Intuitively it seems simple
More informationL.O: HOW GEOLOGISTS SEQUENCE EVENTS IN EARTH'S GEOLOGIC HISTORY IF NOT OVERTURNED, OLDEST ON BOTTOM, YOUNGEST ON TOP
L.O: HOW GEOLOGISTS SEQUENCE EVENTS IN EARTH'S GEOLOGIC HISTORY IF NOT OVERTURNED, OLDEST ON BOTTOM, YOUNGEST ON TOP 1. Unless a series of sedimentary rock layers has been overturned, the bottom rock layer
More informationGY 111: Physical Geology
UNIVERSITY OF SOUTH ALABAMA GY 111: Physical Geology Lecture 21: Rock Deformation Instructor: Dr. Douglas W. Haywick Last Time A) How long is long? B) Geological time divisions Web notes 20 Geological
More informationPackage velociraptr. February 15, 2017
Type Package Title Fossil Analysis Version 1.0 Author Package velociraptr February 15, 2017 Maintainer Andrew A Zaffos Functions for downloading, reshaping, culling, cleaning, and analyzing
More informationFossils, Environments, and Geologic Time
Fossils, Environments, and Geologic Time By Rachel Dolbier, W.M. Keck Earth Science and Mineral Engineering Museum & D.D. LaPointe, Nevada Bureau of Mines and Geology In this activity, we will evaluate
More informationModule 9: Earth's History Topic 3 Content: A Tour of Geologic Time Notes
The geologic time scale holds secrets to the life that has existed on Earth since the beginning of time. It is time for you to take a journey through the history of Earth. 1 Click on each of the segments
More informationThe terrestrial rock record
The terrestrial rock record Stratigraphy, vertebrate biostratigraphy and phylogenetics The Cretaceous-Paleogene boundary at Hell Creek, Montana. Hell Creek Fm. lower, Tullock Fm. upper. (P. David Polly,
More informationBiology. Slide 1 of 40. End Show. Copyright Pearson Prentice Hall
Biology 1 of 40 2 of 40 Fossils and Ancient Life What is the fossil record? 3 of 40 Fossils and Ancient Life The fossil record provides evidence about the history of life on Earth. It also shows how different
More informationGeological Time Scale UG Hons.1 st Year) DR. CHANDAN SURABHI DAS ASST. PROF. IN GEOGRAPHY BARASAT GOVT. COLLEGE
Geological Time Scale UG Hons.1 st Year) 1 DR. CHANDAN SURABHI DAS ASST. PROF. IN GEOGRAPHY BARASAT GOVT. COLLEGE 2 Imagine putting everything that has happened on Earth into a one hour time frame! 3 12:00am
More informationPaleoceanography II Telluric Effects on Oceanography
Paleoceanography II Telluric Effects on Oceanography Geological Oceanography OCN 622 Gary McMurtry Telluric Effects Tellus = Earth Distribution of Continents at 100 Ma BP and Present Comparison of Earth
More informationGY 112: Earth History. Fossils Part:
UNIVERSITY OF SOUTH ALABAMA GY 112: Earth History Fossils Part: Telling Time Predicting Paleoenvironments Instructor: Dr. Douglas W. Haywick Last Time 1. Chronostratigraphy versus biostratigraphy 2. Paleontological
More informationHow do we learn about ancient life? Fossil- a trace or imprint of a living thing that is preserved by geological processes.
Unit 1B Lesson 4 History of Life on Earth How do we learn about ancient life? Paleontologists scientists that studies fossils Fossil- a trace or imprint of a living thing that is preserved by geological
More informationTeam members (First and Last Names): Fossil lab
Team members (First and Last Names): Period: Group #: Fossil lab Background: Fossils are traces of organisms that lived in the past. When fossils are found, they are carefully excavated and then analyzed.
More informationAbsolute Time. Part 8 Geochronology and the Time Scale
Absolute Time Part 8 Geochronology and the Time Scale Unless otherwise noted the artwork and photographs in this slide show are original and by Burt Carter. Permission is granted to use them for non-commercial,
More informationChapter 12. Life of the Paleozoic
Chapter 12 Life of the Paleozoic Paleozoic Invertebrates Representatives of most major invertebrate phyla were present during Paleozoic, including sponges, corals, bryozoans, brachiopods, mollusks, arthropods,
More informationShield was above sea-level during the Cambrian and provided the sediment for the basins.
Name: Answers Geology 1023 Lab #8, Winter 2014 Platforms and Paleozoic life-forms Lab day: Tu W Th 1. Schematic geologic cross-sections A-B and C-D (shown below) cross the edge of the continental platform
More informationTime. How we achieved a modern sense of time. Yearly Calendars are Ancient
Time How we achieved a modern sense of time. Yearly Calendars are Ancient Stonehenge is 2000+ BC and indicates that ancient cultures counted days and knew precisely the repeat cycle of the seasons. 1 Renaissance
More informationChapter 3 Time and Geology
Chapter 3 Time and Geology Methods of Dating Rocks 1. Relative dating - Using fundamental principles of geology (Steno's Laws, Fossil Succession, etc.) to determine the relative ages of rocks (which rocks
More informationPERSISTENT PREDATOR-PREY DYNAMICS REVEALED BY MASS EXTINCTION.
1 Supporting Information Appendix for PERSISTENT PREDATOR-PREY DYNAMICS REVEALED BY MASS EXTINCTION. Lauren Cole Sallan, Thomas W. Kammer, William I. Ausich, Lewis A. Cook 1 2 Illustration - A Viséan Euramerican
More informationGEOLOGY 12 CHAPTER 8 WS #3 GEOLOGIC TIME & THE FOSSIL RECORD
GEOLOGY 12 CHAPTER 8 WS #3 GEOLOGIC TIME & THE FOSSIL RECORD NAME Multiple Choice 1. Fossils are most commonly found in A. sedimentary rocks. B. metamorphic rocks. C. igneous rocks. D. all kinds of rocks.
More informationThe Fossil Record. CELLS and HEREDITY, CHAPTER 5, SECTION 3, PAGES 155 to 163
The Fossil Record CELLS and HEREDITY, CHAPTER 5, SECTION 3, PAGES 155 to 163 Objectives 1. Describe how most fossils form. 2. Explain how scientists can determine a fossil s age. 3. Identify some unanswered
More informationDirected Reading. Section: Precambrian Time and the Paleozoic Era EVOLUTION. beginning of life is called. to. PRECAMBRIAN TIME.
Skills Worksheet Directed Reading Section: Precambrian Time and the Paleozoic Era 1. Where is the geologic history of Earth recorded? 2. What kind of information can scientists get from the types of rock
More informationA sampling-standardized analysis of Phanerozoic marine diversification and extinction. A Working Group proposed by
A sampling-standardized analysis of Phanerozoic marine diversification and extinction A Working Group proposed by John Alroy Department of Paleobiology Smithsonian Institution MRC 121 Washington, DC 20560
More informationCURRICULUM VITAE. CURRENT POSITION Postdoctoral fellow, Department of Ecology & Evolutionary Biology, University of Michigan EDUCATION
CURRICULUM VITAE Katharine M. Loughney Department of Ecology & Evolutionary Biology Museum of Paleontology University of Michigan 1105 North University Ave., Ann Arbor, MI 48109 loughney@umich.edu CURRENT
More informationPhanerozoic (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 informationClues to the Past. Grades 6-8 Educational Program Guide
Clues to the Past Grades 6-8 Educational Program Guide OAS Science Practices: 1, 2, 3, 4, 6, 7, 8 Program Overview The Clues to the Past program will introduce students to several 300 million years old
More informationTuesday 10 June 2014 Afternoon
Tuesday 10 June 2014 Afternoon A2 GCE GEOLOGY F795/01 Evolution of Life, Earth and Climate *1242977619* Candidates answer on the Question Paper. OCR supplied materials: None Other materials required: Electronic
More information251 Million years. 299 Million years. 318 Million years. 359 Million years
The Late Paleozoic 251 Million years 299 Million years 318 Million years 359 Million years Major Questions How did marine life of late Paleozoic time differ from that of middle Paleozoic time? How did
More informationChapter 10. Early Paleozoic Events
Chapter 10 Early Paleozoic Events The Phanerozoic Eon Consists of three eras (from oldest to youngest): Paleozoic = "ancient life" (542-251 m.y. ago) Mesozoic = "middle life" (251-65.5 m.y. ago) Cenozoic
More informationMatthew G. Powell. Student Grants (supervised)
Matthew G. Powell DEPARTMENT OF GEOLOGY, JUNIATA COLLEGE, 1700 MOORE ST., HUNTINGDON, PA 16652 WORK (814) 641-3602 HOME (443) 802-6300 EMAIL POWELL@JUNIATA.EDU Education Ph.D. Earth and Planetary Sciences.
More informationMass Extinctions &Their Consequences
Mass Extinctions &Their Consequences Microevolution and macroevolution Microevolution: evolution occurring within populations p Adaptive and neutral changes in allele frequencies Macroevolution: evolution
More informationWhy is it called the "Inland Basins" Region?
Learning Series: Rocks of the Southeastern U. S. The BIG Picture Why is it called the "Inland Basins" Region? Inland from the mountains, the Earth s crust was buckled (downwarped) into a series of depressions
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 informationMass Extinctions &Their Consequences
Mass Extinctions &Their Consequences Taxonomic diversity of skeletonized marine animal families during the Phanerozoic Spindle diagram of family diversification/extinction PNAS 1994. 91:6758-6763. Background
More informationOrdovician. System. Cambrian. System
443 495 543 Late Middle Early Late Middle Early Ordovician System Cambrian System Earth History, Ch. 13 1 Ch. 13 Review: Early Paleozoic life & Burgess Shale fauna Most animal phyla originated in Cambrian;
More informationThe Pennsylvania State University. The Graduate School. Department of Geosciences TAXIC AND PHYLOGENETIC APPROACHES TO UNDERSTANDING THE
The Pennsylvania State University The Graduate School Department of Geosciences TAXIC AND PHYLOGENETIC APPROACHES TO UNDERSTANDING THE LATE ORDOVICIAN MASS EXTINCTION AND EARLY SILURIAN RECOVERY A Thesis
More informationEARTH S HISTORY. What is Geology? logy: science. Geology is the scientific study of the Earth, including its:
EARTH S HISTORY 1 What is Geology? Geo: earth logy: science Geology is the scientific study of the Earth, including its: composition, structure, and physical properties. 2 1 Geologists study: the origin
More informationName: Date: Period: Page 1
Name: Date: Period: Base your answers to questions 1 through 4 on the three bedrock outcrops below and on your knowledge of Earth science. The outcrops, labeled I, II, and III, are located within 15 kilometers
More informationDOWNLOAD PDF THE NEOGENE MARINE BIOTA OF TROPICAL AMERICA (/
Chapter 1 : Neogene - Wikipedia The Neogene Marine Biota of Tropical America ("NMITA") database: Accounting for biodiversity in paleontology - Volume 75 Issue 3 - Ann F. Budd, Charles T. Foster, John P.
More information5 Time Marches On. TAKE A LOOK 1. Identify What kinds of organisms formed the fossils in the picture?
CHAPTER 6 5 Time Marches On SECTION The Rock and Fossil Record BEFORE YOU READ After you read this section, you should be able to answer these questions: How do geologists measure time? How has life changed
More informationGeologic History. A. Basic Geologic Principles The relative age of rock formations relies on the following basic geologic principles:
Geologic History I. Relative Age Dating of Rocks Relative age of rocks does not rely on an exact date of a rock, but relates its age relative to other rock formations or layers. A. Basic Geologic Principles
More informationSize differences of the post-anoxia, biotic recovery brachiopod, Dyoros sp., in Hughes Creek Shale (Carboniferous), Richardson County, Nebraska.
Size differences of the post-anoxia, biotic recovery brachiopod, Dyoros sp., in Hughes Creek Shale (Carboniferous), Richardson County, Nebraska. Daryl Johnson and Rex Hanger Dept. of Geography & Geology
More informationDO NOT WRITE ON THIS EXAM ONLY WRITE ON THE ANSWER SHEET!
DO NOT WRITE ON THIS EXAM ONLY WRITE ON THE ANSWER SHEET! Multiple Choice Questions (30 points) for each question, please choose the best answer and circle your answer on the answer sheet (do not write
More information17-1 The Fossil Record Slide 2 of 40
2 of 40 Fossils and Ancient Life What is the fossil record? 3 of 40 Fossils and Ancient Life Fossils and Ancient Life Paleontologists are scientists who collect and study fossils. All information about
More informationPetroleum Systems (Part One) Source, Generation, and Migration
Petroleum Systems (Part One) Source, Generation, and Migration GEOL 4233 Class January 2008 Petroleum Systems Elements Source Rock Migration Route Reservoir Rock Seal Rock Trap Processes Generation Migration
More informationLinks to help understand the immensity of the Geologic Time Scale
Links to help understand the immensity of the Geologic Time Scale http://www.bonnechere.ca/naturalhistory.htm http://comp.uark.edu/~sboss/geotime.htm http://www.britannica.com/ebchecked/media/1650/the-geologic-time-scale-from-650-million-years-ago-to
More information1. Identify this organism (it is 1mm in diameter) 2. The shell or of this organism is made of 3. How do these one-celled organism feed? 4.
Fossil Test 2 1. Identify this organism (it is 1mm in diameter) 2. The shell or of this organism is made of 3. How do these one-celled organism feed? 4. Describe the biological and geological importance
More informationQuiz Four (9:30-9:35 AM)
Quiz Four (9:30-9:35 AM) UNIVERSITY OF SOUTH ALABAMA GY 112: Earth History Fossils Part 1: Telling Time Instructor: Dr. Douglas W. Haywick Last Time A) Stable isotopes of use to geology (fractionation)
More informationMesozoic rock formations in the NY region. The Geologic History of New York State. The Mesozoic. Mesozoic Rock Formations in the NY Region
The eologic History of New York State The Mesozoic eologic Provinces NY Region Timescale and geologic provinces of NY-NJ Mesozoic Rock Formations in the NY Region Mesozoic rock formations in the NY region
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 informationEvenness of Cambrian Ordovician benthic marine communities in North America
Paleobiology, 30(3), 2004, pp. 325 346 Evenness of Cambrian Ordovician benthic marine communities in North America Shanan E. Peters Abstract. Biodiversity has two principal components: richness (the number
More informationFossils, Geologic Time, Absolute & Relative Dating, and Natural Resources. Chapters 5 & 6
Fossils, Geologic Time, Absolute & Relative Dating, and Natural Resources Chapters 5 & 6 How Do Fossils Form? Fossils are found in sedimentary rocks like sandstone, limestone, and shale In Virginia, most
More informationChapter 3 Time and Geology
Chapter 3 Time and Geology Finding the age of rocks: Relative versus Actual Dating The science that deals with determining the ages of rocks is called geochronology. Methods of Dating Rocks 1. Relative
More informationEarth Science 105 Geologic Time Chapter 11
Correlation of rock layers Earth Science 105 Geologic Time Chapter 11 Earth Science 11 th ed. Tarbuck & Lutgens Matching same age rocks In local area Across wide area In different regions Grand Canyon
More informationEarth Science 105. Geologic Time Chapter 11. Earth Science 11 th ed. Tarbuck & Lutgens
Earth Science 105 Geologic Time Chapter 11 Earth Science 11 th ed. Tarbuck & Lutgens Correlation of rock layers Matching same age rocks In local area Across wide area In different regions Grand Canyon
More informationGSA DATA REPOSITORY
GSA DATA REPOSITORY 2015274 Saltzman "Persistent oceanic anoxia..." Part I. NOTES ON CAMBRO-ORDOVICIAN CARBON ISOTOPE COMPOSITE CURVE IN FIG. 1 CAMBRIAN COMPOSITE REFERENCES FOR FIG.1 Data all originally
More informationGeological Time How old is the Earth
Geological Time How old is the Earth How old is everything? Universe? Universe ~ 14 Billion Years Old Milky Way Galaxy? Milky Way Galaxy - 10 Billion Years Old Solar System? Solar System -4.6 Billion Years
More informationPage 143: Geologic Time
Page 143: Geologic Time Divide pages 144-147 in 6 One for each box: Hadeon Eon Archeon Eon Cambrian Period Ordovician Period Silurian Period Devonian Period Carboniferous Period Mississipian Period Pennsylvanian
More informationCambrian Sedimentary Deposits - The Sauk Sequence
Cambrian Sedimentary Deposits - The Sauk Sequence During Cambrian, there were no vascular plants on the land, so the landscape was barren. Erosion was active and severe without plant roots to hold the
More informationPlan of Development Mountain Valley Pipeline Project. APPENDIX P Plan for Unanticipated Discovery of Paleontological Resources
APPENDIX P Plan for Unanticipated Discovery of Paleontological Resources Appendix P Plan for Unanticipated Discovery of Paleontological Resources Prepared by: TABLE OF CONTENTS 1.0 INTRODUCTION... 1 1.1
More informationUnit 5: Earth s History Practice Problems
Name: Date: 1. Which bedrock would be most likely to contain fossils? A. Precambrian granite B. Cambrian shale C. Pleistocene basalt D. Middle-Proterozoic quartzite 6. Base your answer(s) to the following
More informationSpring th Grade
Spring 2015 8 th Grade The geologic time scale is a record of the major events and diversity of life forms present in Earth s history. The geologic time scale began when Earth was formed and goes on until
More informationEGAS. Ministry of Petroleum
EGAS Ministry of Petroleum EGAS Ministry of Petroleum About The Block Location: N. Thekah offshore block is located at about 56 km to the north of the Mediterranean shore line, 85 km to the north west
More informationThe Evolution of Biological Diversity. All living organisms are descended from an ancestor that arose between 3 and 4 billion years ago.
The Evolution of Biological Diversity All living organisms are descended from an ancestor that arose between 3 and 4 billion years ago. The diversity of life on earth currently includes some 5 to 50 million
More information17-1 The Fossil Record Slide 1 of 40
1 of 40 Fossils and Ancient Life Fossils and Ancient Life Paleontologists are scientists who collect and study fossils. All information about past life is called the fossil record. The fossil record includes
More informationG331: The Nature and Adequacy of the Fossil Record
1 G331: The Nature and Adequacy of the Fossil Record Approaches: Rarefaction Logarithmic Decay Model How many species might have been alive in the past? What percentage are fossilized? How many skeletonized
More informationvary spuriously with preservation rate, but this spurious variation is largely eliminated and true rates are reasonably well estimated.
606 MICHAEL FOOTE Figure 1 shows results of an experiment with simulated data. Rates of origination, extinction, and preservation were varied in a pulsed pattern, in which a background level was punctuated
More informationAnswers to Section G: Time and the Fossil Record (Relative Dating)
Answers to Section G: Time and the Fossil Record (Relative Dating) Use the following sketch of a geological cross section to answer questions 1 to 3. 1. The most important principle used to determine the
More informationGEOLOGY - GL4 INTERPRETING THE GEOLOGICAL RECORD
Candidate Name Centre Number 2 Candidate Number GCE A level 1214/01 GEOLOGY - GL4 INTERPRETING THE GEOLOGICAL RECORD A.M. MONDAY, 21 June 2010 2 hours Section A 1. 2. 3. 15 15 15 1214 01 01 4. 15 Section
More information2010 National Science Olympiad Fossil Test Final Qs & A s
2010 National Science Olympiad Fossil Test Final Qs & A s Note: Fossil pictures are unavailable (consider using the internet for samples) Station 1 Specimens A and B. DO NOT WRITE ON THIS SHEET USE YOUR
More informationEGAS. Ministry of Petroleum
EGAS Ministry of Petroleum EGAS Ministry of Petroleum About The Block Location: N. El Arish offshore block is located in the extreme eastern part of the Egypt s economic water border and bounded from the
More informationControls on facies distributions in the Charlie Lake Formation, Peace River Arch, Alberta
Controls on facies distributions in the Charlie Lake Formation, Peace River Arch, Alberta E.L. Percy 12, C. Frostad 2, A. Juska 2, C. Schmidt 2, C. Sitzler 2, and J.P. Zonneveld 3 University of Calgary,
More informationAge of Earth/Geologic Time. Vocabulary
Age of Earth/Geologic Time Vocabulary Big Ideas Geologic Time Earth Structures Identify current methods for measuring the age of Earth and its parts, including the law of superposition and radioactive
More informationQuiz Nine (9:30-9:35 AM)
Quiz Nine (9:30-9:35 AM) UNIVERSITY OF SOUTH ALAAMA GY 112: Earth History Lecture 25: Paleozoic 2: More Laurentia! Instructor: Dr. Douglas W. Haywick Last Time The Paleozoic of North America 1) Laurentian
More informationEras of Earth's History Lesson 6
Eras of Earth's History Lesson 6 May 24 8:42 PM What happened in the Paleozoic Era? What happened in the Mesozoic Era? What happened in the Cenozoic Era? May 24 8:55 PM 1 I. What happened in the Paleozoic
More information2009 Colorado Science Olympiad Fossils Test Station 1:
2009 Colorado Science Olympiad Fossils Test Station 1: 1. Identify the genus for these specimens (diameters range from 2.5 to 5 mm). 2. In which Kingdom do these organisms belong? 3. What famous structures
More informationPaleontology Muhittin Görmüş Department of Geology Lecture 12
Paleontology http://www.biltek.tubitak. gov.tr/bilgipaket/jeolojik /index.htm Muhittin Görmüş Department of Geology http://members.cox.net/jdmount/paleont.html http://www.ucmp.berkeley.edu/arthropoda/arthropoda.html
More informationLate 20 th Century Tests of the Continental Drift Hypothesis
Late 20 th Century Tests of the Continental Drift Hypothesis 7 Biogeography Revisited Unless otherwise noted the artwork and photographs in this slide show are original and by Burt Carter. Permission is
More informationSkeletal grains. Pores. Matrix <20 m) Cement. Non-skeletal grains. 1 cm
Components of a Carbonate rock Skeletal grains Pores Matrix
More informationBiodiversity in the Phanerozoic: a reinterpretation
Paleobiology, 27(4), 2001, pp. 583 601 Biodiversity in the Phanerozoic: a reinterpretation Shanan E. Peters and Michael Foote Abstract. Many features of global diversity compilations have proven robust
More informationPALEONTOLOGY. Muhittin Görmüş Department of Geology. Lecture gov.tr/bilgipaket/jeolojik /index.htm
PALEONTOLOGY http://www.biltek.tubitak. gov.tr/bilgipaket/jeolojik /index.htm Muhittin Görmüş Department of Geology http://members.cox.net/jdmount/paleont.html 1. Hemicordata General characteristics Classification
More informationPALEONTOLOGY MUSEUM MICHELE GORTANI
PALEONTOLOGY MUSEUM MICHELE GORTANI Paleontology exhibition The evolution of life through fossils Luciano Tiraboschi --- Antonio Foscheri (photos) Paleontology Museum Michele Gortani Portogruaro Paleontology
More informationLate Cretaceous biostratigraphy and adaptive radiation of the calcareous nannofossil genus Eiffellithus
Ms Jamie Shamrock was born in Pennsylvania; she has earned already a B.A. in anthropology and a B.Sc. in geology. Ms. Shamrock is now going for her Master s degree at the University of Nebraska-Lincoln.
More informationFossils. Ch. 29 and 30 Overview
Ch. 29 and 30 Overview What you need to know: Chapter 29: Fossils, Relative Time, Absolute Time Chapter 30: Geologic Time Fossils Study of fossils called paleontology Original remains rare usually dead
More informationLab 4 Identifying metazoan phyla and plant groups
Geol G308 Paleontology and Geology of Indiana Name: Lab 4 Identifying metazoan phyla and plant groups The objective of this lab is to classify all of the fossils from your site to phylum (or to plant group)
More informationAre Sigurdsen. Master Thesis, Department of Biology
Size change in brachiopods and trilobites of the Oslo Region during the Ordovician and during the Ordovician-Silurian transition. Evidence of Cope s Rule and the Lilliput Effect? Master Thesis, Department
More informationComparative Taphonomy of the Vendian Genera. Beltanelloides and Nemiana as a Key to their True. Nature
Comparative Taphonomy of the Vendian Genera Beltanelloides and Nemiana as a Key to their True Nature M. V. Leonov Paleontological Institute, Russian Academy of Science, 123 Profsoyuznaya, Moscow, 117868,
More information