The Greatest Challenge to 21St Century Paleontology: When Commercialization of Fossils Threatens the Science
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Illinois Fossils Doc 2005
State of Illinois Illinois Department of Natural Resources Illinois Fossils Illinois Department of Natural Resources he Illinois Fossils activity book from the Illinois Department of Natural Resources’ (IDNR) Division of Education is designed to supplement your curriculum in a vari- ety of ways. The information and activities contained in this publication are targeted toT grades four through eight. The Illinois Fossils resources trunk and lessons can help you T teach about fossils, too. You will find these and other supplemental items through the Web page at https://www2.illinois.gov/dnr/education/Pages/default.aspx. Contact the IDNR Division of Education at 217-524-4126 or [email protected] for more information. Collinson, Charles. 2002. Guide for beginning fossil hunters. Illinois State Geological Survey, Champaign, Illinois. Geoscience Education Series 15. 49 pp. Frankie, Wayne. 2004. Guide to rocks and minerals of Illinois. Illinois State Geological Survey, Champaign, Illinois. Geoscience Education Series 16. 71 pp. Killey, Myrna M. 1998. Illinois’ ice age legacy. Illinois State Geological Survey, Champaign, Illinois. Geoscience Education Series 14. 67 pp. Much of the material in this book is adapted from the Illinois State Geological Survey’s (ISGS) Guide for Beginning Fossil Hunters. Special thanks are given to Charles Collinson, former ISGS geologist, for the use of his fossil illustrations. Equal opportunity to participate in programs of the Illinois Department of Natural Resources (IDNR) and those funded by the U.S. Fish and Wildlife Service and other agencies is available to all individuals regardless of race, sex, national origin, disability, age, reli-gion or other non-merit factors. -
Fossil Collecting Areas in Iowa
FOSSIL COLLECTING AREAS IN IOWA The following list, although far from compete, includes a few of the better fossil collecting areas in Iowa. 1. Rockford, Floyd County (¼ mile south and ¼ mile west of the Rockford Brick and Tile Company pit, on county road “D”). Well preserved brachiopods, gastropods, and corals are most abundant in the yellowish shales that overlie the blue-gray beds. The fossils occurring here are known as the Hackberry fauna and have been described by C.L. and M.A. Fenton in a book entitled, “The Hackberry State of the Upper Devonian,” published by the MacMillan Company in 1924. 2. Bird Hill, Cerro Gordo County This is near the center of the north line of section 24, T 95N, R.19W, about 3½ miles west and ¼ mile south of the Rockford Brick and Tile Company Plant. The Hackberry fauna can be collected here also. 3. Elgin-Clermont area, Fayette County In the Elgin Member of the Maquoketa Formation large trilobites and both straight and coiled cephalopods are found. Fragments of trilobites are common, but whole specimens are rare. Road cuts along the new highway between Clermont and Elgin, the dry stream bed along county road “Y” east of Clermont, and the high-road cuts along the Turkey River southeast of Elgin are all good collecting sites. References for this area are: (1) Slocum, A.W., “Trilobites from the Maquoketa Beds of Fayette County, Iowa,” Iowa Geological Survey Annual Report, Volume 25; (2) Walter, O.T., “Trilobites of Iowa and some Related Paleozoic Forms,” Iowa Geological Survey Annual Report, Volume 31; (3) Ladd, H.S., “Stratigraphy and Paleontology of the Maquoketa Shale of Iowa,” Iowa Geological Survey Annual Report, Volume 34. -
Rowan C. Martindale Curriculum Vitae Associate Professor (Invertebrate Paleontology) at the University of Texas at Austin
ROWAN C. MARTINDALE CURRICULUM VITAE ASSOCIATE PROFESSOR (INVERTEBRATE PALEONTOLOGY) AT THE UNIVERSITY OF TEXAS AT AUSTIN Department of Geological Sciences E-mail: [email protected] Jackson School of Geosciences Website: www.jsg.utexas.edu/martindale/ 2275 Speedway Stop C9000 Orchid ID: 0000-0003-2681-083X Austin, TX 78712-1722 Phone: 512-475-6439 Office: JSG 3.216A RESEARCH INTERESTS The overarching theme of my work is the connection between Earth and life through time, more precisely, understanding ancient (Mesozoic and Cenozoic) ocean ecosystems and the evolutionary and environmental events that shaped them. My research is interdisciplinary, (paleontology, sedimentology, biology, geochemistry, and oceanography) and focuses on: extinctions and carbon cycle perturbation events (e.g., Oceanic Anoxic Events, acidification events); marine (paleo)ecology and reef systems; the evolution of reef builders (e.g., coral photosymbiosis); and exceptionally preserved fossil deposits (Lagerstätten). ACADEMIC APPOINTMENTS Associate Professor, University of Texas at Austin September 2020 to Present Assistant Professor, University of Texas at Austin August 2014 to August 2020 Postdoctoral Researcher, Harvard University August 2012 to July 2014 Department of Organismic and Evolutionary Biology; Mentor: Dr. Andrew H. Knoll. EDUCATION Doctorate, University of Southern California 2007 to 2012 Dissertation: “Paleoecology of Upper Triassic reef ecosystems and their demise at the Triassic-Jurassic extinction, a potential ocean acidification event”. Advisor: Dr. David J. Bottjer, degree conferred August 7th, 2012. Bachelor of Science Honors Degree, Queen’s University 2003 to 2007 Geology major with a general concentration in Biology (Geological Sciences Medal Winner). AWARDS AND RECOGNITION Awards During Tenure at UT Austin • 2019 National Science Foundation CAREER Award: Awarded to candidates who are judged to have the potential to serve as academic role models in research and education. -
Some Philosophical Questions About Paleontology and Their Practica1 Consequences
ACTA GEOLOGICA HISPANICA. Concept and method in Paleontology. 16 (1981) nos 1-2, pags. 7-23 Some philosophical questions about paleontology and their practica1 consequences by Miquel DE RENZI Depto. de Geología, Facultad de Ciencias Biológicas, Universidad de Valencia. Burjassot (Valencia). This papcr attempts to objectively discuss the actual state ofpaleontology. The En aquest treball s'ha intentat fer un balanc d'alguns aspectes de I'estat de la progress of this science stood still somewhat during the latter part of the last paleontologia. La historia de la paleontologia mostra un estancarnent a les century which caused it to develop apart from the biological sciences. an area to darreries del segle passac aquest estancament va Fer que la nostra ciencia s'anes which it is naturally tied. As aconsequence, this bruought a long-term stagnation, allunyant cada cop mes de I'area de les ciencies bii~logiques,amb les qualsestava because biology, dunng this century, has made great progress and paleontology lligada naturalment AixO va portar, com a conseqüencia, un important has not During the last 20 years paleontology as a science hasrecuperatedsome endarreriment, car la biologia, durant aquest segle, ha donat un gran pas of this loss, but we as scientists need to be careful in various aspects of its endavant, mentre que aquest no ha estat el cas de lapaleontologia Al nostre pais development -i possiblement a molts d'altres- la paleontologia es, fonamentalment, un estn per datar estrats. Tanmateix, un mal estri, car la datació es basadaen les especies fossils i la seva determinació es fonamenta en el ccncepte d'especie biolbgica; els fossils pero en moltes ocasions, són utilitzats mes aviat com si fossin segells o monedes. -
Mary Anning of Lyme Regis: 19Th Century Pioneer in British Palaeontology
Headwaters Volume 26 Article 14 2009 Mary Anning of Lyme Regis: 19th Century Pioneer in British Palaeontology Larry E. Davis College of St. Benedict / St. John's University, [email protected] Follow this and additional works at: https://digitalcommons.csbsju.edu/headwaters Part of the Geology Commons, and the Paleontology Commons Recommended Citation Davis, Larry E. (2009) "Mary Anning of Lyme Regis: 19th Century Pioneer in British Palaeontology," Headwaters: Vol. 26, 96-126. Available at: https://digitalcommons.csbsju.edu/headwaters/vol26/iss1/14 This Article is brought to you for free and open access by DigitalCommons@CSB/SJU. It has been accepted for inclusion in Headwaters by an authorized editor of DigitalCommons@CSB/SJU. For more information, please contact [email protected]. LARRY E. DAVIS Mary Anning of Lyme Regis 19th Century Pioneer in British Palaeontology Ludwig Leichhardt, a 19th century German explorer noted in a letter, “… we had the pleasure of making the acquaintance of the Princess of Palaeontology, Miss Anning. She is a strong, energetic spinster of about 28 years of age, tanned and masculine in expression …” (Aurousseau, 1968). Gideon Mantell, a 19th century British palaeontologist, made a less flattering remark when he wrote in his journal, “… sallied out in quest of Mary An- ning, the geological lioness … we found her in a little dirt shop with hundreds of specimens piled around her in the greatest disorder. She, the presiding Deity, a prim, pedantic vinegar looking female; shred, and rather satirical in her conversation” (Curwin, 1940). Who was Mary Anning, this Princess of Palaeontology and Geological Lioness (Fig. -
The Paleontology Synthesis Project and Establishing a Framework for Managing National Park Service Paleontological Resource Archives and Data
Lucas, S.G. and Sullivan, R.M., eds., 2018, Fossil Record 6. New Mexico Museum of Natural History and Science Bulletin 79. 589 THE PALEONTOLOGY SYNTHESIS PROJECT AND ESTABLISHING A FRAMEWORK FOR MANAGING NATIONAL PARK SERVICE PALEONTOLOGICAL RESOURCE ARCHIVES AND DATA VINCENT L. SANTUCCI1, JUSTIN S. TWEET2 and TIMOTHY B. CONNORS3 1National Park Service, Geologic Resources Division, 1849 “C” Street, NW, Washington, D.C. 20240, [email protected]; 2National Park Service, 9149 79th Street S., Cottage Grove, MN 55016, [email protected]; 3National Park Service, Geologic Resources Division, 12795 W. Alameda Parkway, Lakewood, CO 80225, [email protected] Abstract—The National Park Service Paleontology Program maintains an extensive collection of digital and hard copy documents, publications, photographs and other archives associated with the paleontological resources documented in 268 parks. The organization and preservation of the NPS paleontology archives has been the focus of intensive data management activities by a small and dedicated team of NPS staff. The data preservation strategy complemented the NPS servicewide inventories for paleontological resources. The first phase of the data management, referred to as the NPS Paleontology Synthesis Project, compiled servicewide paleontological resource data pertaining to geologic time, taxonomy, museum repositories, holotype fossil specimens, and numerous other topics. In 2015, the second phase of data management was implemented with the creation and organization of a multi-faceted digital data system known as the NPS Paleontology Archives and NPS Paleontology Library. Two components of the NPS Paleontology Archives were designed for the preservation of both park specific and servicewide paleontological resource archives and data. A third component, the NPS Paleontology Library, is a repository for electronic copies of geology and paleontology publications, reports, and other media. -
SVP's Letter to Editors of Journals and Publishers on Burmese Amber And
Society of Vertebrate Paleontology 7918 Jones Branch Drive, Suite 300 McLean, VA 22102 USA Phone: (301) 634-7024 Email: [email protected] Web: www.vertpaleo.org FEIN: 06-0906643 April 21, 2020 Subject: Fossils from conflict zones and reproducibility of fossil-based scientific data Dear Editors, We are writing you today to promote the awareness of a couple of troubling matters in our scientific discipline, paleontology, because we value your professional academic publication as an important ‘gatekeeper’ to set high ethical standards in our scientific field. We represent the Society of Vertebrate Paleontology (SVP: http://vertpaleo.org/), a non-profit international scientific organization with over 2,000 researchers, educators, students, and enthusiasts, to advance the science of vertebrate palaeontology and to support and encourage the discovery, preservation, and protection of vertebrate fossils, fossil sites, and their geological and paleontological contexts. The first troubling matter concerns situations surrounding fossils in and from conflict zones. One particularly alarming example is with the so-called ‘Burmese amber’ that contains exquisitely well-preserved fossils trapped in 100-million-year-old (Cretaceous) tree sap from Myanmar. They include insects and plants, as well as various vertebrates such as lizards, snakes, birds, and dinosaurs, which have provided a wealth of biological information about the ‘dinosaur-era’ terrestrial ecosystem. Yet, the scientific value of these specimens comes at a cost (https://www.nytimes.com/2020/03/11/science/amber-myanmar-paleontologists.html). Where Burmese amber is mined in hazardous conditions, smuggled out of the country, and sold as gemstones, the most disheartening issue is that the recent surge of exciting scientific discoveries, particularly involving vertebrate fossils, has in part fueled the commercial trading of amber. -
Fossil Collecting in Ohio
No. 17 OHIOGeoFacts DEPARTMENT OF NATURAL RESOURCES • DIVISION OF GEOLOGICAL SURVEY FOSSIL COLLECTING IN OHIO Hobbyists have long known about Ohio’s great abundance and WHERE FOSSILS ARE FOUND IN OHIO diversity of fossils. Many world-famous paleontologists—geologists who study fossils—began their careers as youngsters collecting fossils Ordovician rocks in Ohio are world famous for in their native Ohio. Fossils from Ohio are important constituents the abundance, variety, and excellent preserva- of museum collections throughout the United States and Europe. tion of the fossils they contain. The limestones and shales exposed in almost every road cut or WHY OHIO HAS FOSSILS stream bed in southwestern Ohio, southeastern Indiana, and north-central Kentucky provide The area that is now Ohio was not always dry land as it is today. the opportunity to collect a bonanza of fossils. Approximately 510 million years ago (m.y.a.), Ohio was south of the Among the more abundant types of fossils col- Equator. As the North American Plate moved to its current position ORDOVICIAN lected from Ordovician rocks are brachiopods, 508–438 m.y.a. through the process of plate tectonics, tropical to subtropical seas bryozoans, gastropods, and trilobites. repeatedly transgressed over the plate. It is because of those warm Silurian rocks of western Ohio are not known seas that Ohio has the abundant fossils that people collect today. for their fossils. When the limestones and shales The seas that covered Ohio during the Ordovician, Silurian, and were fi rst deposited they were quite fossilifer- most of the Devonian Periods of the Paleozoic Era were the site of ous. -
A Concise Dictionary of Paleontology Second Edition
springer.com Life Sciences : Evolutionary Biology Carlton, Robert L. A Concise Dictionary of Paleontology Second Edition Presents a unique English language dictionary of paleontological terms, taxa, localities, and concepts Focuses on the most common orders, genera, and species, paying careful attention to overall historical significance in terms of turning points such as mass extinctions Written for students, libraries, museums, and general readers of scientific literature This new and significantly updated authored dictionary is a unique glossary of paleontological Springer terms, taxa, localities, and concepts. It focuses primarily on identifying the most significant 2nd ed. 2019, XII, 469 p. groups of fossil animals and plants in relation to their evolution and phylogeny. It also focuses 2nd on mass extinctions, on taxa that are problematic in some significant way, on the principal edition fossil-Lagerstätten of the world, and on historical turning points marked by index fossils. Although there are many current resources on the subject, none contains an accurate representation of the paleontological lexicon. Although well aware that the fast-changing field Printed book of paleontology will always defy any attempt at complete description, the author has attempted Hardcover to provide an accurate and comprehensive set of about 4,000 entries that will be useful to professionals as well as to general readers of scientific literature without a background in Printed book paleontology. Hardcover ISBN 978-3-030-25585-5 £ 149,99 | CHF 200,50 | 169,99 € | Order online at springer.com/booksellers Springer Nature Customer Service Center GmbH 186,99 € (A) | 181,89 € (D) Customer Service Available Tiergartenstrasse 15-17 Discount group 69121 Heidelberg Standard (0) Germany T: +49 (0)6221 345-4301 Product category [email protected] Dictionary Other renditions Softcover ISBN 978-3-030-25588-6 Softcover ISBN 978-3-030-25587-9 Prices and other details are subject to change without notice. -
Raymond M. Alf Museum of Paleontology EDUCATOR's GUIDE
Raymond M. Alf Museum of Paleontology EDUCATOR’S GUIDE Dear Educator: This guide is recommended for educators of grades K-4 and is designed to help you prepare students for their Alf Museum visit, as well as to provide resources to enhance your classroom curriculum. This packet includes background information about the Alf Museum and the science of paleontology, a summary of our museum guidelines and what to expect, a pre-visit checklist, a series of content standard-aligned activities/exercises for classroom use before and/or after your visit, and a list of relevant terms and additional resources. Please complete and return the enclosed evaluation form to help us improve this guide to better serve your needs. Thank you! Paleontology: The Study of Ancient Life Paleontology is the study of ancient life. The history of past life on Earth is interpreted by scientists through the examination of fossils, the preserved remains of organisms which lived in the geologic past (more than 10,000 years ago). There are two main types of fossils: body fossils, the preserved remains of actual organisms (e.g. shells/hard parts, teeth, bones, leaves, etc.) and trace fossils, the preserved evidence of activity by organisms (e.g. footprints, burrows, fossil dung). Chances for fossil preservation are enhanced by (1) the presence of hard parts (since soft parts generally rot or are eaten, preventing preservation) and (2) rapid burial (preventing disturbance by bio- logical or physical actions). Many body fossils are skeletal remains (e.g. bones, teeth, shells, exoskel- etons). Most form when an animal or plant dies and then is buried by sediment (e.g. -
Nanostructure of Biogenic Versus Abiogenic Calcium Carbonate Crystals
Nanostructure of biogenic versus abiogenic calcium carbonate crystals JAROSŁAW STOLARSKI and MACIEJ MAZUR Stolarski, J. and Mazur, M. 2005. Nanostructure of biogenic versus abiogenic calcium carbonate crystals. Acta Palae− ontologica Polonica 50 (4): 847–865. The mineral phase of the aragonite skeletal fibers of extant scleractinians (Favia, Goniastrea) examined with Atomic Force Microscope (AFM) consists entirely of grains ca. 50–100 nm in diameter separated from each other by spaces of a few nanometers. A similar pattern of nanograin arrangement was observed in basal calcite skeleton of extant calcareous sponges (Petrobiona) and aragonitic extant stylasterid coralla (Adelopora). Aragonite fibers of the fossil scleractinians: Neogene Paracyathus (Korytnica, Poland), Cretaceous Rennensismilia (Gosau, Austria), Trochocyathus (Black Hills, South Dakota, USA), Jurassic Isastraea (Ostromice, Poland), and unidentified Triassic tropiastraeid (Alpe di Specie, It− aly) are also nanogranular, though boundaries between individual grains occasionally are not well resolved. On the other hand, in diagenetically altered coralla (fibrous skeleton beside aragonite bears distinct calcite signals) of the Triassic cor− als from Alakir Cay, Turkey (Pachysolenia), a typical nanogranular pattern is not recognizable. Also aragonite crystals produced synthetically in sterile environment did not exhibit a nanogranular pattern. Unexpectedly, nanograins were rec− ognized in some crystals of sparry calcite regarded as abiotically precipitated. Our findings support the idea that nanogranular organization of calcium carbonate fibers is not, per se, evidence of their biogenic versus abiogenic origin or their aragonitic versus calcitic composition but rather, a feature of CaCO3 formed in an aqueous solution in the presence of organic molecules that control nanograin formation. Consistent orientation of crystalographic axes of polycrystalline skeletal fibers in extant or fossil coralla, suggests that nanograins are monocrystalline and crystallographically ordered (at least after deposition). -
Vertebrate Paleontology of the Cretaceous/Tertiary Transition of Big Bend National Park, Texas (Lancian, Puercan, Mammalia, Dinosauria, Paleomagnetism)
Louisiana State University LSU Digital Commons LSU Historical Dissertations and Theses Graduate School 1986 Vertebrate Paleontology of the Cretaceous/Tertiary Transition of Big Bend National Park, Texas (Lancian, Puercan, Mammalia, Dinosauria, Paleomagnetism). Barbara R. Standhardt Louisiana State University and Agricultural & Mechanical College Follow this and additional works at: https://digitalcommons.lsu.edu/gradschool_disstheses Recommended Citation Standhardt, Barbara R., "Vertebrate Paleontology of the Cretaceous/Tertiary Transition of Big Bend National Park, Texas (Lancian, Puercan, Mammalia, Dinosauria, Paleomagnetism)." (1986). LSU Historical Dissertations and Theses. 4209. https://digitalcommons.lsu.edu/gradschool_disstheses/4209 This Dissertation is brought to you for free and open access by the Graduate School at LSU Digital Commons. It has been accepted for inclusion in LSU Historical Dissertations and Theses by an authorized administrator of LSU Digital Commons. For more information, please contact [email protected]. INFORMATION TO USERS This reproduction was made from a copy of a manuscript sent to us for publication and microfilming. While the most advanced technology has been used to pho tograph and reproduce this manuscript, the quality of the reproduction is heavily dependent upon the quality of the material submitted. Pages in any manuscript may have indistinct print. In all cases the best available copy has been filmed. The following explanation of techniques is provided to help clarify notations which may appear on this reproduction. 1. Manuscripts may not always be complete. When it is not possible to obtain missing pages, a note appears to indicate this. 2. When copyrighted materials are removed from the manuscript, a note ap pears to indicate this. 3.