Chapter 9 - Paleontology
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Plant Macrofossil Evidence for an Early Onset of the Holocene Summer Thermal Maximum in Northernmost Europe
ARTICLE Received 19 Aug 2014 | Accepted 27 Feb 2015 | Published 10 Apr 2015 DOI: 10.1038/ncomms7809 OPEN Plant macrofossil evidence for an early onset of the Holocene summer thermal maximum in northernmost Europe M. Va¨liranta1, J.S. Salonen2, M. Heikkila¨1, L. Amon3, K. Helmens4, A. Klimaschewski5, P. Kuhry4, S. Kultti2, A. Poska3,6, S. Shala4, S. Veski3 & H.H. Birks7 Holocene summer temperature reconstructions from northern Europe based on sedimentary pollen records suggest an onset of peak summer warmth around 9,000 years ago. However, pollen-based temperature reconstructions are largely driven by changes in the proportions of tree taxa, and thus the early-Holocene warming signal may be delayed due to the geographical disequilibrium between climate and tree populations. Here we show that quantitative summer-temperature estimates in northern Europe based on macrofossils of aquatic plants are in many cases ca.2°C warmer in the early Holocene (11,700–7,500 years ago) than reconstructions based on pollen data. When the lag in potential tree establishment becomes imperceptible in the mid-Holocene (7,500 years ago), the reconstructed temperatures converge at all study sites. We demonstrate that aquatic plant macrofossil records can provide additional and informative insights into early-Holocene temperature evolution in northernmost Europe and suggest further validation of early post-glacial climate development based on multi-proxy data syntheses. 1 Department of Environmental Sciences, ECRU, University of Helsinki, P.O. Box 65, Helsinki FI-00014, Finland. 2 Department of Geosciences and Geography, University of Helsinki, P.O. Box 65, Helsinki FI-00014, Finland. -
Standard Procedures for the Assessment and Mitigation of Adverse Impacts to Paleontological Resources
Standard Procedures for the Assessment and Mitigation of Adverse Impacts to Paleontological Resources Society of Vertebrate Paleontology Impact Mitigation Guidelines Revision Committee Abstract Fossils are nonrenewable paleontological resources that are subject to impacts from land development. Procedures are presented for evaluating the potential for impacts of a proposed action on paleontological resources and for mitigating those impacts. Impact mitigation includes pre-project survey and salvage, monitoring and screen washing during excavation to salvage fossils, conservation and inventory, and final reports and specimen curation. The objective of these procedures is to offer standard methods for assessing potential impacts to fossils and mitigating these impacts. Introduction Fossils are nonrenewable paleontological resources that are afforded protection by federal, state, and local environmental laws and regulations. The Paleontological Resources Preservation Act (PRPA) of 2009 calls for uniform policies and standards that apply to fossils on all federal public lands. All federal land management agencies are required to develop regulations that satisfy the stipulations of the PRPA. Section 6302 of the PRPA mandates that federal agencies "shall manage and protect paleontological resources on Federal land using scientific principles and expertise." Thus, federal agencies need the help of the professional paleontological community in the formulation and implementation of these PRPA- mandated policies and regulations. The potential for destruction or degradation of paleontological resources on both public and private lands selected for development under the jurisdiction of various governmental planning agencies is recognized. The standard procedures below are intended to be applicable to both private and public lands under the jurisdiction of local, city, county, regional, state, and federal agencies. -
PAL-3, Paleontological Resources Mitigation And
DOCKETED Docket Number: 16-AFC-01C Project Title: Stanton Energy Reliability Center - Compliance TN #: 226417 PAL-3, Paleontological Resources Mitigation and Monitoring Program Document Title: (PRMMP) Description: N/A Filer: Marichka Haws Organization: California Energy Commission Submitter Role: Commission Staff Submission Date: 1/31/2019 11:24:15 AM Docketed Date: 1/31/2019 STATE OF CALIFORNIA – NATURAL RESOURCES AGENCY GAVIN NEWSOM, Governor CALIFORNIA ENERGY COMMISSION 1516 NINTH STREET SACRAMENTO, CA 95814-5512 www.energy.ca.gov January 14, 2019 Greg Lamberg Compliance Manager W Power 650 Bercut Drive, Suite A Sacramento, CA 95811 SUBJECT: Stanton Energy Reliability Center (16-AFC-01C), PAL-3, Paleontological Resources Mitigation and Monitoring Program (PRMMP) Dear Mr. Lamberg, In accordance with PAL-3, the CPM has reviewed and approved the Paleontological Resources Mitigation and Monitoring Plan (PRMMP). If you have any questions or concerns, please contact John Heiser, Compliance Project Manager, at (916) 653-8236, or by fax to (916) 654-3882, or via e-mail at [email protected]. Sincerely, John Heiser Compliance Office Manager Siting, Transmission, & Environmental Protection Division CONDITION OF CERTIFICATION PAL- 3 Stanton Energy Reliability Center (16-AFC-01) Paleontological Resources Mitigation and Monitoring Plan Prepared for California Energy Commission November 2018 Orange County Office 27001 La Paz Road, Suite 230 Mission Viejo, CA 92691 The undersigned is the primary author of this document: Dr. W. Geoffrey Spaulding -
Databases in Vertebrate Paleontology Mark D
This article was downloaded by: [University of California, Berkeley] On: 08 January 2013, At: 09:29 Publisher: Taylor & Francis Informa Ltd Registered in England and Wales Registered Number: 1072954 Registered office: Mortimer House, 37-41 Mortimer Street, London W1T 3JH, UK Journal of Vertebrate Paleontology Publication details, including instructions for authors and subscription information: http://www.tandfonline.com/loi/ujvp20 From card catalogs to computers: databases in vertebrate paleontology Mark D. Uhen a , Anthony D. Barnosky b , Brian Bills c , Jessica Blois d , Matthew T. Carrano e , Marc A. Carrasco b , Gregory M. Erickson f , Jussi T. Eronen g h , Mikael Fortelius g , Russell W. Graham i , Eric C. Grimm j , Maureen A. O’Leary k , Austin Mast f l , William H. Piel m , P. David Polly n & Laura K. Säilä g a Department of Atmospheric, Oceanic and Earth Sciences, George Mason University, Fairfax, Virginia, 22030, U.S.A. b Department of Integrative Biology and Museum of Paleontology, University of California, Berkeley, California, 94720, U.S.A. c Center for Environmental Informatics, Pennsylvania State University, University Park, Pennsylvania, 16802, U.S.A. d Center for Climate Research, University of Wisconsin, Madison, Wisconsin, 53706, U.S.A. e Department of Paleobiology, National Museum of Natural History, Smithsonian Institution, Washington, D.C., 20013, U.S.A. f Department of Biological Science, The Florida State University, Tallahassee, Florida, 32306, U.S.A. g Department of Geosciences and Geography, HY-00014, University of Helsinki, Finland h Senckenberg Research Institute und Nature Museum, Biodiversity and Climate Research Centre LOEWE BiK-F, Senckenberganlage 25, D-60325 Frankfurt am Main, Germany i Department of Geosciences, The Pennsylvania State University, University Park, Pennsylvania, 16802, U.S.A. -
PALEONTOLOGICAL TECHNICAL REPORT: 6Th AVENUE and WADSWORTH BOULEVARD INTERCHANGE PHASE II ENVIRONMENTAL ASSESSMENT, CITY of LAKEWOOD, JEFFERSON COUNTY, COLORADO
PALEONTOLOGICAL TECHNICAL REPORT: 6th AVENUE AND WADSWORTH BOULEVARD INTERCHANGE PHASE II ENVIRONMENTAL ASSESSMENT, CITY OF LAKEWOOD, JEFFERSON COUNTY, COLORADO Prepared for: TEC Inc. 1746 Cole Boulevard, Suite 265 Golden, CO 80401 Prepared by: Paul C. Murphey, Ph.D. and David Daitch M.S. Rocky Mountain Paleontology 4614 Lonespur Court Oceanside, CA 92056 303-514-1095; 760-758-4019 www.rockymountainpaleontology.com Prepared under State of Colorado Paleontological Permit 2007-33 January, 2007 TABLE OF CONTENTS 1.0 SUMMARY............................................................................................................................. 3 2.0 INTRODUCTION ................................................................................................................... 4 2.1 DEFINITION AND SIGNIFICANCE OF PALEONTOLOGICAL RESOURCES........... 4 3.0 METHODS .............................................................................................................................. 6 4.0. LAWS, ORDINANCES, REGULATIONS AND STANDARDS......................................... 7 4.1. Federal................................................................................................................................. 7 4.2. State..................................................................................................................................... 8 4.3. County................................................................................................................................. 8 4.4. City..................................................................................................................................... -
Grand Canyon National Park Centennial Paleontological Resource Inventory (Non-Sensitive Version)
Grand Canyon National Park Centennial Paleontological Resource Inventory (Non-Sensitive Version) Natural Resource Report NPS/GRCA/NRR—2020/2103 Vincent L. Santucci1 and Justin S. Tweet,2 editors 1National Park Service Geologic Resources Division 1849 “C” Street, NW Washington, D.C. 20240 2National Park Service 9149 79th St. S. Cottage Grove, Minnesota 55016 March 2020 U.S. Department of the Interior National Park Service Natural Resource Stewardship and Science Fort Collins, Colorado Chapter 1. Introduction and Summary: The Paleontological Heritage of Grand Canyon National Park By Vincent L. Santucci1 1National Park Service Geologic Resources Division 1849 “C” Street, NW Washington, D.C. 20240 Throughout my life I have been bestowed the privilege of experiencing the world-renowned landscape and resources of the Grand Canyon from many perspectives and viewsheds (Figure 1-1). My first views were standing and taking photos from the many vantage points and overlooks along the North and South rims. I have enjoyed many hikes into the canyon with colleagues from the National Park Service (NPS) or with academic geologists and paleontologists. On a few occasions I ventured down and then back up the trails of the canyon with my children Sarah, Bethany, Luke, Jacob, Brianna and Abigail, often carrying one or more in my arms on the climb against gravity. I traversed by foot to the base of the canyon at Phantom Ranch and gained a greater appreciation for the geologic story preserved in the park strata. I have gazed intensely out the window of many commercial aircraft from above this geologic wonder of Earth, contemplating the geomorphic “grandeur” created over "Deep Time" and the artistry of processes perfected by “Mother Nature.” I pinch myself when I recall the opportunity when my friend Justin Tweet and I were granted permission to fly into the western portion of the Grand Canyon on a small NPS plane operated by a pilot from Lake Mead National Recreation Area. -
Phylum Arthropod Silvia Rondon, and Mary Corp, OSU Extension Entomologist and Agronomist, Respectively Hermiston Research and Extension Center, Hermiston, Oregon
Phylum Arthropod Silvia Rondon, and Mary Corp, OSU Extension Entomologist and Agronomist, respectively Hermiston Research and Extension Center, Hermiston, Oregon Member of the Phyllum Arthropoda can be found in the seas, in fresh water, on land, or even flying freely; a group with amazing differences of structure, and so abundant that all the other animals taken together are less than 1/6 as many as the arthropods. Well-known members of this group are the Kingdom lobsters, crayfish and crabs; scorpions, spiders, mites, ticks, Phylum Phylum Phylum Class the centipedes and millipedes; and last, but not least, the Order most abundant of all, the insects. Family Genus The Phylum Arthropods consist of the following Species classes: arachnids, chilopods, diplopods, crustaceans and hexapods (insects). All arthropods possess: • Exoskeleton. A hard protective covering around the outside of the body (divided by sutures into plates called sclerites). An insect's exoskeleton (integument) serves as a protective covering over the body, but also as a surface for muscle attachment, a water-tight barrier against desiccation, and a sensory interface with the environment. It is a multi-layered structure with four functional regions: epicuticle (top layer), procuticle, epidermis, and basement membrane. • Segmented body • Jointed limbs and jointed mouthparts that allow extensive specialization • Bilateral symmetry, whereby a central line can divide the body Insect molting or removing its into two identical halves, left and right exoesqueleton • Ventral nerve -
The Strawberry Bank Lagerstätte Reveals Insights Into Early Jurassic Lifematt Williams, Michael J
XXX10.1144/jgs2014-144M. Williams et al.Early Jurassic Strawberry Bank Lagerstätte 2015 Downloaded from http://jgs.lyellcollection.org/ by guest on September 27, 2021 2014-144review-articleReview focus10.1144/jgs2014-144The Strawberry Bank Lagerstätte reveals insights into Early Jurassic lifeMatt Williams, Michael J. Benton &, Andrew Ross Review focus Journal of the Geological Society Published Online First doi:10.1144/jgs2014-144 The Strawberry Bank Lagerstätte reveals insights into Early Jurassic life Matt Williams1, Michael J. Benton2* & Andrew Ross3 1 Bath Royal Literary and Scientific Institution, 16–18 Queen Square, Bath BA1 2HN, UK 2 School of Earth Sciences, University of Bristol, Bristol BS8 2BU, UK 3 National Museum of Scotland, Chambers Street, Edinburgh EH1 1JF, UK * Correspondence: [email protected] Abstract: The Strawberry Bank Lagerstätte provides a rich insight into Early Jurassic marine vertebrate life, revealing exquisite anatomical detail of marine reptiles and large pachycormid fishes thanks to exceptional preservation, and especially the uncrushed, 3D nature of the fossils. The site documents a fauna of Early Jurassic nektonic marine animals (five species of fishes, one species of marine crocodilian, two species of ichthyosaurs, cephalopods and crustaceans), but also over 20 spe- cies of insects. Unlike other fossil sites of similar age, the 3D preservation at Strawberry Bank provides unique evidence on palatal and braincase structures in the fishes and reptiles. The age of the site is important, documenting a marine ecosystem during recovery from the end-Triassic mass extinction, but also exactly coincident with the height of the Toarcian Oceanic Anoxic Event, a further time of turmoil in evolution. -
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. -
71St Annual Meeting Society of Vertebrate Paleontology Paris Las Vegas Las Vegas, Nevada, USA November 2 – 5, 2011 SESSION CONCURRENT SESSION CONCURRENT
ISSN 1937-2809 online Journal of Supplement to the November 2011 Vertebrate Paleontology Vertebrate Society of Vertebrate Paleontology Society of Vertebrate 71st Annual Meeting Paleontology Society of Vertebrate Las Vegas Paris Nevada, USA Las Vegas, November 2 – 5, 2011 Program and Abstracts Society of Vertebrate Paleontology 71st Annual Meeting Program and Abstracts COMMITTEE MEETING ROOM POSTER SESSION/ CONCURRENT CONCURRENT SESSION EXHIBITS SESSION COMMITTEE MEETING ROOMS AUCTION EVENT REGISTRATION, CONCURRENT MERCHANDISE SESSION LOUNGE, EDUCATION & OUTREACH SPEAKER READY COMMITTEE MEETING POSTER SESSION ROOM ROOM SOCIETY OF VERTEBRATE PALEONTOLOGY ABSTRACTS OF PAPERS SEVENTY-FIRST ANNUAL MEETING PARIS LAS VEGAS HOTEL LAS VEGAS, NV, USA NOVEMBER 2–5, 2011 HOST COMMITTEE Stephen Rowland, Co-Chair; Aubrey Bonde, Co-Chair; Joshua Bonde; David Elliott; Lee Hall; Jerry Harris; Andrew Milner; Eric Roberts EXECUTIVE COMMITTEE Philip Currie, President; Blaire Van Valkenburgh, Past President; Catherine Forster, Vice President; Christopher Bell, Secretary; Ted Vlamis, Treasurer; Julia Clarke, Member at Large; Kristina Curry Rogers, Member at Large; Lars Werdelin, Member at Large SYMPOSIUM CONVENORS Roger B.J. Benson, Richard J. Butler, Nadia B. Fröbisch, Hans C.E. Larsson, Mark A. Loewen, Philip D. Mannion, Jim I. Mead, Eric M. Roberts, Scott D. Sampson, Eric D. Scott, Kathleen Springer PROGRAM COMMITTEE Jonathan Bloch, Co-Chair; Anjali Goswami, Co-Chair; Jason Anderson; Paul Barrett; Brian Beatty; Kerin Claeson; Kristina Curry Rogers; Ted Daeschler; David Evans; David Fox; Nadia B. Fröbisch; Christian Kammerer; Johannes Müller; Emily Rayfield; William Sanders; Bruce Shockey; Mary Silcox; Michelle Stocker; Rebecca Terry November 2011—PROGRAM AND ABSTRACTS 1 Members and Friends of the Society of Vertebrate Paleontology, The Host Committee cordially welcomes you to the 71st Annual Meeting of the Society of Vertebrate Paleontology in Las Vegas. -
Active Research Grants
Linda C. Ivany Professor Department of Earth and Environmental Sciences Heroy Geology Laboratory,Syracuse University, Syracuse, NY 13244 phone: (315) 443-3626 / fax: (315) 443-3363 / email: [email protected] http://thecollege.syr.edu/people/faculty/pages/ear/Ivany-Linda.html https://orcid.org/0000-0002-4692-3455 Education Ph.D. in Earth and Planetary Sciences, 1997, Harvard University Advisor: Stephen Jay Gould M.S. in Geology, minor in Zoology, 1990, University of Florida-Gainesville Advisor: Douglas S. Jones B.S. in Geology, minor in Zoology, 1988, Syracuse University Advisor: Cathryn R. Newton Academic Positions 2012-present Professor of Earth Sciences, Syracuse University 2005-2012 Associate Professor of Earth Sciences, Syracuse University 2001-2005 Assistant Professor of Earth Sciences, Syracuse University 2000-2001 Visiting Assistant Professor of Earth Sciences, Syracuse University 1997-2000 Michigan Society Fellow and Visiting Assistant Professor of Geological Sciences, University of Michigan General Research Interests Evolutionary Paleoecology, Paleoclimatology, Stable Isotopes in Paleobiology I am a marine paleoecologist and paleoclimatologist. My interests lie broadly in the evolution of the Earth-life system and how ecosystems and their component taxa evolve and respond to changes in the physical environment. Specific areas of interest include biotic and climatic change during the Paleogene (~65-24 million years ago); use of geochemical data, particularly stable isotopes, derived from accretionary biogenic materials for inference -
Vertebrates and Invertebrates
Vertebrates and invertebrates The animal kingdom is divided into two groups: vertebrates and invertebrates. Vertebrates have been around for millions of years but have evolved and changed over time. The word vertebrate means “having a backbone." Many animals have backbones. You have a backbone. So does a cow, a whale, a fish, a frog, and a bird. Vertebrates are animals that have a backbone. Most animals have a backbone that is made of bones joined together to form a skeleton. Our skeleton gives us our shape and allows us to move. Mammals, fish, birds, reptiles, and amphibians have Vertebrae backbones so they are all vertebrates. Each bone that makes up the backbone Scientists classify vertebrates into five classes: is called a vertebra. These are the • Mammals building blacks that form the backbone, • Fish also known as the spinal cord. The • Birds vertebrae protect and support your • Reptiles spine. Without a backbone, you would not • Amphibians be able to move any part of your body. Animals without a backbone are called invertebrates. Most The human animals are invertebrates. In fact, 95% of all living creatures backbone has 26 on Earth are invertebrates. vertebrae. Arthropods are the largest group of invertebrates. Insects make up a large part of this group. All insects, such as ladybugs, ants, grasshoppers, and bumblebees have three body sections and six legs. Most arthropods live on land, but some of these fascinating creatures live in water. Lobsters, crabs, and shrimp are arthropods that live in the oceans. Many invertebrates have skeletons on the outside of their A frog only has bodies called exoskeletons.