Activities in Historical Geology with IGO's
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GE OS 1234-101 Historical Geology Lecture Syllabus Instructor
G E OS 1234-101 Historical Geology Lecture Syllabus Instructor: Dr. Jesse Carlucci ([email protected]), (940) 397-4448 Class: MWF, 10am -10:50am, BO 100 Office hours: Bolin Hall 131, MWF, 11am ± 2pm, Tuesday, noon - 2pm. You can arrange to meet with me at any time, by appointment. Textbook: Earth System History by Steven M. Stanley, 3rd edition. I will occasionally post articles and other readings on blackboard. I will also upload Power Point presentations to blackboard before each class, if possible. Course Objectives: Historical Geology provides the student with a comprehensive survey of the history of life, and major events in the physical development of Earth. Most importantly, this class addresses how processes like plate tectonics and climate interact with life, forming an integrated system. The first half of the class focuses on concepts, and the second on a chronologic overview of major biological and physical events in different geologic periods. L E C T UR E SC H E DU L E Aug 27-31: Overview of course; what is science? The Earth as a planet Stanley (pg. 244-247) Sep 5-7: Earth materials, rocks and minerals Stanley (pg. 13-17; 25-34) Sep 10-14: Rocks & minerals continued; plate tectonics. Stanley (pg. 3-12; 35-46; 128-141; 175-186) Sep 17-21: Geological time and dating of the rock record; chemical systems, the climate system through time. Quiz 1 (Sep 19; 5%). Stanley (pg. 187-194; 196-207; 215-223; 232-238) Sep 24-28: Sedimentary environments and life; paleoecology. Stanley (pg. 76-80; 84-96; 99-123) Oct 1-5: Biological evolution and the fossil record. -
GEOL 1104 Historical Geology
Administrative Master Syllabus Course Information Course Title Historical Geology Laboratory Course Prefix, Num. and Title GEOL 1104 Division Life Sciences Department Geology Course Type Academic WCJC Core Course Course Catalog Description This laboratory-based course accompanies GEOL 1304, Historical Geography. Laboratory activities will introduce methods used by scientists to interpret the history of life and major events in the physical development of Earth from rocks and fossils. Pre-Requisites Credit for or concurrent enrollment in GEOL1304 Co-Requisites Enter Co-Requisites Here. Semester Credit Hours Total Semester Credit Hours (SCH): Lecture Hours: 1:0:2 Lab/Other Hours Equated Pay Hours 1.2 Lab/Other Hours Breakdown: Lab Hours 2 Lab/Other Hours Breakdown: Clinical Hours Enter Clinical Hours Here. Lab/Other Hours Breakdown: Practicum Hours Enter Practicum Hours Here. Other Hours Breakdown List Total Lab/Other Hours Here. Approval Signatures Title Signature Date Prepared by: Department Head: Division Chair: Dean/VPI: Approved by CIR: Rev. January 2020 Additional Course Information Topical Outline: Each offering of this course must include the following topics (be sure to include information regarding lab, practicum, and clinical or other non-lecture instruction). 1. The Sedimentary Environment 2. Geochronology Part I: Relative Dating of Strata 3. Geochronology Part II: Absolute or Radiometric Dating of Strata 4. Fossils, Taxonomy, and the Species Concept 5. The Sponges: Early Multi-celled Animals 6. The Corals and their Relatives 7. The Bryozoans: “Lacy Animals” 8. The Brachiopods: Bivalved Lophophorates 9. The Bivalves: Clams, Oysters, and Relatives 10. The Gastropods: Snails, Slugs, and Relativesacticum, and clinical or other non-lecture instruction). -
The Origin and Early Evolution of Dinosaurs
Biol. Rev. (2010), 85, pp. 55–110. 55 doi:10.1111/j.1469-185X.2009.00094.x The origin and early evolution of dinosaurs Max C. Langer1∗,MartinD.Ezcurra2, Jonathas S. Bittencourt1 and Fernando E. Novas2,3 1Departamento de Biologia, FFCLRP, Universidade de S˜ao Paulo; Av. Bandeirantes 3900, Ribeir˜ao Preto-SP, Brazil 2Laboratorio de Anatomia Comparada y Evoluci´on de los Vertebrados, Museo Argentino de Ciencias Naturales ‘‘Bernardino Rivadavia’’, Avda. Angel Gallardo 470, Cdad. de Buenos Aires, Argentina 3CONICET (Consejo Nacional de Investigaciones Cient´ıficas y T´ecnicas); Avda. Rivadavia 1917 - Cdad. de Buenos Aires, Argentina (Received 28 November 2008; revised 09 July 2009; accepted 14 July 2009) ABSTRACT The oldest unequivocal records of Dinosauria were unearthed from Late Triassic rocks (approximately 230 Ma) accumulated over extensional rift basins in southwestern Pangea. The better known of these are Herrerasaurus ischigualastensis, Pisanosaurus mertii, Eoraptor lunensis,andPanphagia protos from the Ischigualasto Formation, Argentina, and Staurikosaurus pricei and Saturnalia tupiniquim from the Santa Maria Formation, Brazil. No uncontroversial dinosaur body fossils are known from older strata, but the Middle Triassic origin of the lineage may be inferred from both the footprint record and its sister-group relation to Ladinian basal dinosauromorphs. These include the typical Marasuchus lilloensis, more basal forms such as Lagerpeton and Dromomeron, as well as silesaurids: a possibly monophyletic group composed of Mid-Late Triassic forms that may represent immediate sister taxa to dinosaurs. The first phylogenetic definition to fit the current understanding of Dinosauria as a node-based taxon solely composed of mutually exclusive Saurischia and Ornithischia was given as ‘‘all descendants of the most recent common ancestor of birds and Triceratops’’. -
Geologic Timeline
SCIENCE IN THE PARK: GEOLOGY GEOLOGIC TIME SCALE ANALOGY PURPOSE: To show students the order of events and time periods in geologic time and the order of events and ages of the physiographic provinces in Virginia. BACKGROUND: Exact dates for events change as scientists explore geologic time. Dates vary from resource to resource and may not be the same as the dates that appear in your text book. Analogies for geologic time: a 24 hour clock or a yearly calendar. Have students or groups of students come up with their own original analogy. Before you assign this activity, you may want to try it, depending on the age of the student, level of the class, or time constraints, you may want to leave out the events that have a date of less than 1 million years. ! Review conversions in the metric system before you begin this activity ! References L.S. Fichter, 1991 (1997) http://csmres.jmu.edu/geollab/vageol/vahist/images/Vahistry.PDF http://pubs.usgs.gov/gip/geotime/age.html Wicander, Reed. Historical Geology. Fourth Edition. Toronto, Ontario: Brooks/Cole, 2004. Print. VIRGINIA STANDARDS OF LEARNING ES.10 The student will investigate and understand that many aspects of the history and evolution of the Earth can be inferred by studying rocks and fossils. Key concepts include: relative and absolute dating; rocks and fossils from many different geologic periods and epochs are found in Virginia. Developed by C.P. Anderson Page 1 SCIENCE IN THE PARK: GEOLOGY Building a Geologic Time Scale Time: Materials Meter stick, 5 cm adding machine tape, pencil, colored pencils Procedure 1. -
The Bristol Dinosaur Project
Proceedings of the Geologists’ Association 123 (2012) 210–225 Contents lists available at ScienceDirect Proceedings of the Geologists’ Association jo urnal homepage: www.elsevier.com/locate/pgeola Teaching Perspective The Bristol Dinosaur Project Michael J. Benton *, Remmert Schouten, Edward J.A. Drewitt, Pedro Viegas School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, UK A R T I C L E I N F O A B S T R A C T Article history: Dinosaurs have been fascinating to the widest public since the 1840s, and that interest has grown step- Received 18 April 2011 wise ever since. Public interest has been harnessed over the years especially by museums in blockbuster Received in revised form 8 July 2011 exhibitions, and in the form of best-selling books and films. Here we describe a major educational Accepted 8 July 2011 initiative, the Bristol Dinosaur Project, which has run for ten years and has reached tens of thousands of Available online 5 August 2011 children and adults, supported by substantial funding. The Bristol Dinosaur Project focuses on the fourth dinosaur ever named in the world, Thecodontosaurus, discovered in Bristol in 1834, and named in 1836. Keywords: The dinosaur is not in itself spectacular, being only 1–2 m long, but its evolutionary role as one of the first Dinosaurs plant-eating dinosaurs in the world justifies our current research, and provides a strong theme for the Education Engagement public presentation. Further, the fact that the dinosaur is found as disarticulated bones in ancient tropical Outreach cave systems, allows us to develop numerous key themes with all age groups: the geological time scale, Geosciences education continental drift, reconstruction of ancient environments, modern landscape analogues, the rock cycle, evolution, biomechanics, and critical assessment of geological and palaeontological evidence. -
GEOLOGY THEME STUDY Page 1
NATIONAL HISTORIC LANDMARKS Dr. Harry A. Butowsky GEOLOGY THEME STUDY Page 1 Geology National Historic Landmark Theme Study (Draft 1990) Introduction by Dr. Harry A. Butowsky Historian, History Division National Park Service, Washington, DC The Geology National Historic Landmark Theme Study represents the second phase of the National Park Service's thematic study of the history of American science. Phase one of this study, Astronomy and Astrophysics: A National Historic Landmark Theme Study was completed in l989. Subsequent phases of the science theme study will include the disciplines of biology, chemistry, mathematics, physics and other related sciences. The Science Theme Study is being completed by the National Historic Landmarks Survey of the National Park Service in compliance with the requirements of the Historic Sites Act of l935. The Historic Sites Act established "a national policy to preserve for public use historic sites, buildings and objects of national significance for the inspiration and benefit of the American people." Under the terms of the Act, the service is required to survey, study, protect, preserve, maintain, or operate nationally significant historic buildings, sites & objects. The National Historic Landmarks Survey of the National Park Service is charged with the responsibility of identifying America's nationally significant historic property. The survey meets this obligation through a comprehensive process involving thematic study of the facets of American History. In recent years, the survey has completed National Historic Landmark theme studies on topics as diverse as the American space program, World War II in the Pacific, the US Constitution, recreation in the United States and architecture in the National Parks. -
GEOL 5 Historical Geology & Paleontology(C-ID GEOL 111)
Lassen Community College Course Outline GEOL-5 Historical Geology & Paleontology 4.0 Units I. Catalog Description This course is designed to provide a descriptive geological history of the earth using the principles and methods of interpretation and reconstruction of the changes that have occurred on the earth in the fossil record. Recommended Preparation: Successful completion of ENGL105 or equivalent multiple measures placement. Transfers to both UC/CSU General Education Area: A CSU GE Area: B1 & B3 IGETC GE Area: 5A & 5C C-ID GEOL 111 51 Hours Lecture, 51 Hours Lab Scheduled: Spring II. Coding Information Repeatability: Not Repeatable, Take 1 Time Grading Option: Graded or Pass/No Pass Credit Type: Credit - Degree Applicable TOP Code: 191400 III. Course Objectives A. Course Student Learning Outcomes Upon completion of this course the student will be able to: 1. Outline the earth's history through construction of a geological time scale and evolution of organisms. 2. Apply proper lab techniques and knowledge of theoretical concepts in geology to acquire and interpret geologic data and formulate new questions in a laboratory setting. B. Course Objectives Upon completion of this course the student will be able to: 1. Explain and practically apply the principles of the scientific method. 2. Discuss earth's origin and evolution. 3. Identify the basic physical features of the earth. 4. Describe how the record of the past is expressed in the sedimentary rocks of the earth. 5. Examine and interpret evidence of geologic activity and the presence of life in the major areas of geologic time. 6. Discuss how the past is the key to the present. -
Historical Geology Course Design 2020-2021
EASTERN ARIZONA COLLEGE Historical Geology Course Design 2020-2021 Course Information Division Science Course Number GLG 102 (SUN# GLG1102) Title Historical Geology Credits 4 Developed by David Morris Lecture/Lab Ratio 3 Lecture/3 Lab Transfer Status ASU NAU UA GLG 102 (3) & GLG GLG 102; Science GEOS 255 104 (1) , Natural & Applied Science Science - General [SAS] --and-- GLG (SG), Historical 104L; Lab Science Awareness (H), [LAB] Natural Science - General (SG) Activity Course No CIP Code 40.0601 Assessment Mode Pre/Post Test (100 Questions/100 Points) Semester Taught Spring GE Category Lab Science Separate Lab Yes Awareness Course No Intensive Writing Course No Diversity and Inclusion Course No Prerequisites ENG 091 with a grade of “C” or higher or reading placement test score as established by District policy. Educational Value This course meets the general education, lab science requirement for graduation and transfer, and is part of the required curriculum for many astronomy majors. Description This course is an introduction to the principles and interpretation of geologic history. It emphasizes the evolution of the earth's lithosphere (crust), atmosphere, and biosphere through geologic time. It includes consideration of the historical aspects of plate tectonics, the geologic development of North America, and important events in biological evolution and the resulting assembly of fossils. It provides an appreciation for the vast extent of geologic time, the natural processes affecting change on the earth, and the identification of common fossil types. EASTERN ARIZONA COLLEGE - 1 - Historical Geology Equal Opportunity Employer and Educator Supplies None Competencies and Performance Standards 1. Compare the contributions made in the past with the advanced methods used today in the field of geology. -
GEOLOGY Geology Major GEO. GEOLOGY
GEOLOGY 14 Geology Major Fifth Semester The major leading to the B.S. degree emphasizes the fundamental of the [[CE-346]] Rock Engineering 3 science of geology with upper-level courses that provide both breadth and [[ENV-321]] Hydrology 3 depth in the curriculum. The program is designed to optimize classroom, [[ENV-323]] Hydrology Lab 1 lab, and field experiences and prepare students for the modern demands of [[GEO-345]] Stratigraphy and 4 a geoscientist or entry into graduate school. Total credits - 122 Sedimentation Geology B.S. Degree- Required Courses [[GIS-271]] Intro to GPS & GIS 3 and Recommended Course Sequence 14 First Semester Credits Sixth Semester [[CHM-115]] Elements & 3 [[EES-302]] Literature Methods 1 Compounds [[EES-304]] Environmental Data 2 [[CHM-113]] Elements & 1 Analysis Compounds Lab [[GEO-349]] Structure and 4 [[ENG-101]] Composition 4 Tectonics [[FYF-101]] First-Year Foundations 3 [[GEO-351]] Paleoclimatology 3 [[MTH-111]] Calculus I 4 [[GEO-352]] Hydrogeology 3 15 [[GIS-272]] Advanced GIS & 3 Remote Sensing Second Semester 16 [[CHM-116]] The Chemical 3 Reaction Summer Session [[CHM-114]] The Chemical 1 [[GEO-380]] Geology Field Camp 4 Reaction Lab [[GEO-101]] Intro to Geology 3 [[GEO-103]] Intro to Geology Lab 1 Seventh Semester [[MTH-112]] Calculus II 4 [[GEO-390]] Applied Geophysics 3 Distribution Requirement 3 [[GEO-391]] Senior Projects I 1 15 Distribution Requirements 6 Third Semester Program Elective 3 13 [[GEO-212]] Historical Geology 3 [[GEO-281]] Mineralogy 4 Eighth Semester [[MTH-150]] Elementary Statistics 3 [[GEO-370]] Geomorphology 3 [[PHY-171]] Principles of Classical 4 [[GEO-392]] Senior Projects II 2 and Modern Physics Distribution Requirements 3 Distribution Requirement 3 Free Elective 3 17 Program Elective 3 Fourth Semester 14 [[EES-240]] Principles of 3 Environmental Engineering & GEO. -
GEOL 02: Historical Geology Lab 7: Discovery of Plate Tectonics 1
GEOL 02: Historical Geology Lab 7: Discovery of Plate Tectonics Name: ________________________________________ Date: _______________ (Adapted by Jason R. Patton from Dale Sawyer, Rice University and Richard Sedlock, San Jose State University) In the early 1960s, the emergence of the theory of plate tectonics started a revolution in the earth sciences. Subsequent verification and refinement of the theory has led scientists to recognize that, directly or indirectly, plate tectonics influences nearly all geologic processes. The theory of plate tectonics states that the Earth's outermost layer is fragmented into a dozen or more shell‐like plates that are moving relative to one another as they ride atop hotter underlying rock. In this lab, we will investigate the locations and types of plate boundaries around the globe by using several types of scientific data. We'll do this as a kind of role play exercise, so consider yourself transported back in time to the 1960's. The data types we'll use today are the same ones used by scientists in the late 1950’s and 1960’s to develop the theory of plate tectonics. These data continue to be collected to better understand how plate tectonics works. Today you will work in groups of "specialists" in one type of data and propose how to locate and classify different types of plate boundaries. Then, you will work with students who are specialists in the other data types to collaborate on an improved classification scheme and apply it to at least one major plate. Finally, you'll receive input from the instructor on plate boundary types and apply that to your final rendition of plate boundaries. -
Geological Time Scale Lecture Notes
Geological Time Scale Lecture Notes dewansEddy remains validly. ill-judged: Lefty is unhelpable: she leaf her she reinsurers phrases mediates inattentively too artfully?and postmarks Ruthenic her and annual. closed-door Fabio still crenellate his Seventh grade Lesson Geologic Time Mini Project. If i miss a lecture and primitive to copy a classmate's notes find a photocopying. Geologic Time Scale Age of free Earth subdivided into named and dated intervals. The Quaternary is even most recent geological period for time in trek's history spanning the unique two million. Geologic Time and Earth Science Lumen Learning. Explaining Events Study arrangement 3 in Figure B Note that. Do not get notified when each lecture notes to be taken in fact depends on plate boundaries in lecture notes with it was convinced from? Coloured minerals introduction to mining geology lecture notes ppt Mining. The geologic record indicates several ice surges interspersed with periods of. Lecture Notes Geologic Eras Geologic Timescale The geologic timetable is divided into 4 major eras The oldest era is called the Pre-Cambrian Era. 4 Mb Over long periods of debate many rocks change shape and ease as salary are. A Geologic Time Scale Measures the Evolution of Life system Review NotesHighlights Image Attributions ShowHide Details. Lecture notes lecture 26 Geological time scale StuDocu. You are encouraged to work together and review notes from lectures to flex on. These lecture notes you slip and indirect evidence of rocks, and phases and geological time scale lecture notes made by which help you? Index fossil any homicide or plant preserved in the department record write the bond that is characteristic of behavior particular complain of geologic time sensitive environment but useful index. -
Competition Structured a Late Cretaceous Megaherbivorous Dinosaur Assemblage Jordan C
www.nature.com/scientificreports OPEN Competition structured a Late Cretaceous megaherbivorous dinosaur assemblage Jordan C. Mallon 1,2 Modern megaherbivore community richness is limited by bottom-up controls, such as resource limitation and resultant dietary competition. However, the extent to which these same controls impacted the richness of fossil megaherbivore communities is poorly understood. The present study investigates the matter with reference to the megaherbivorous dinosaur assemblage from the middle to upper Campanian Dinosaur Park Formation of Alberta, Canada. Using a meta-analysis of 21 ecomorphological variables measured across 14 genera, contemporaneous taxa are demonstrably well-separated in ecomorphospace at the family/subfamily level. Moreover, this pattern is persistent through the approximately 1.5 Myr timespan of the formation, despite continual species turnover, indicative of underlying structural principles imposed by long-term ecological competition. After considering the implications of ecomorphology for megaherbivorous dinosaur diet, it is concluded that competition structured comparable megaherbivorous dinosaur communities throughout the Late Cretaceous of western North America. Te question of which mechanisms regulate species coexistence is fundamental to understanding the evolution of biodiversity1. Te standing diversity (richness) of extant megaherbivore (herbivores weighing ≥1,000 kg) com- munities appears to be mainly regulated by bottom-up controls2–4 as these animals are virtually invulnerable to top-down down processes (e.g., predation) when fully grown. Tus, while the young may occasionally succumb to predation, fully-grown African elephants (Loxodonta africana), rhinoceroses (Ceratotherium simum and Diceros bicornis), hippopotamuses (Hippopotamus amphibius), and girafes (Girafa camelopardalis) are rarely targeted by predators, and ofen show indiference to their presence in the wild5.