Paleontological Resources
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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. -
California Vegetation Map in Support of the DRECP
CALIFORNIA VEGETATION MAP IN SUPPORT OF THE DESERT RENEWABLE ENERGY CONSERVATION PLAN (2014-2016 ADDITIONS) John Menke, Edward Reyes, Anne Hepburn, Deborah Johnson, and Janet Reyes Aerial Information Systems, Inc. Prepared for the California Department of Fish and Wildlife Renewable Energy Program and the California Energy Commission Final Report May 2016 Prepared by: Primary Authors John Menke Edward Reyes Anne Hepburn Deborah Johnson Janet Reyes Report Graphics Ben Johnson Cover Page Photo Credits: Joshua Tree: John Fulton Blue Palo Verde: Ed Reyes Mojave Yucca: John Fulton Kingston Range, Pinyon: Arin Glass Aerial Information Systems, Inc. 112 First Street Redlands, CA 92373 (909) 793-9493 [email protected] in collaboration with California Department of Fish and Wildlife Vegetation Classification and Mapping Program 1807 13th Street, Suite 202 Sacramento, CA 95811 and California Native Plant Society 2707 K Street, Suite 1 Sacramento, CA 95816 i ACKNOWLEDGEMENTS Funding for this project was provided by: California Energy Commission US Bureau of Land Management California Wildlife Conservation Board California Department of Fish and Wildlife Personnel involved in developing the methodology and implementing this project included: Aerial Information Systems: Lisa Cotterman, Mark Fox, John Fulton, Arin Glass, Anne Hepburn, Ben Johnson, Debbie Johnson, John Menke, Lisa Morse, Mike Nelson, Ed Reyes, Janet Reyes, Patrick Yiu California Department of Fish and Wildlife: Diana Hickson, Todd Keeler‐Wolf, Anne Klein, Aicha Ougzin, Rosalie Yacoub California -
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. -
The Archaeology and Paleoclimate of the Mud Lake Basin, Nye County, Nevada
University of Nevada, Reno Changing Landscapes During the Terminal Pleistocene/Early Holocene: The Archaeology and Paleoclimate of the Mud Lake Basin, Nye County, Nevada A thesis submitted in partial fulfillment of the requirements for the degree of Masters of Arts in Anthropology By Lindsay A. Fenner Dr. Geoffrey M. Smith/Thesis Advisor May, 2011 © by Lindsay A. Fenner 2011 All Rights Reserved THE GRADUATE SCHOOL We recommend that the thesis prepared under our supervision by LINDSAY A. FENNER entitled Changing Landscapes During The Terminal Pleistocene/Early Holocene: The Archaeology And Paleoclimate Of The Mud Lake Basin, Nye County, Nevada be accepted in partial fulfillment of the requirements for the degree of MASTER OF ARTS Geoffrey M. Smith, Ph.D., Advisor Gary Haynes, Ph.D., Committee Member Kenneth D. Adams, Ph.D., Graduate School Representative Marsha H. Read, Ph. D., Associate Dean, Graduate School May, 2011 i ABSTRACT Archaeological investigation along Pleistocene lakeshores is a longstanding and common approach to prehistoric research in the Great Basin. Continuing in this tradition, this thesis considers the archaeological remains present from pluvial Mud Lake, Nye County, Nevada coupled with an examination of paleoclimatic conditions to assess land-use patters during the terminal Pleistocene/early Holocene. Temporally diagnostic lithic assemblages from 44 localities in the Mud Lake basin provide the framework for which environmental proxy records are considered. Overwhelmingly occupied by Prearchaic groups, comprising 76.6% of all diagnostic artifacts present, Mud Lake was intensively utilized right up to its desiccation after the Younger Dryas, estimated at 9,000 radiocarbon years before present. Intermittently occupied through the remainder of the Holocene, different land-use strategies were employed as a result of shifting subsistence resources reacting to an ever changing environment. -
Mammal Footprints from the Miocene-Pliocene Ogallala
Mammalfootprints from the Miocene-Pliocene Ogallala Formation, easternNew Mexico by ThomasE. Williamsonand SpencerG. Lucas, New Mexico Museum of Natural History and Science,1801 Mountain Road NW Albuquerque, New Mexico 87104-7375 Abstract well-develooed mudcracks. The track- ways are diveloped on the mudstone Mammal trackways preserved in the drape but are preserved as infillings at the Miocene-Pliocene Ogallala Formation of base of the overlying conglomerate (Figs. eastern New Mexico represent the first 2-4). Most tracks are preserved on the report of mammal fossils-from this unit in underside of a single, thick conglomerate New Mexico. These trackwavs are Dre- block (Fig. 3). A few isolated mammal served as infillings in a conglomerate near the base of the Ogallala Formation. At least prints were also observed on the under- four mammalian ichnotaxa are represented, side of adjacent blocks.he depth of the including a single trackway of a large camel infillings suggest that tracks were made in (Gambapessp. A), several prints of an uncer- a relatively soft substrate. Some prints are tain family of artiodactyl (Gambapessp B), a accompanied by marks indicating slip- single trackway of a large feloid carnivoran page on a slick, wet substrate (Fig. 5C). (Bestiopeda sp.), and several indistinct im- Infillings of mudcracks and narrow, cylin- pressions, probably representing more than drical burrows and raindrop impressions one trackway of a small canid carnivoran are Dreserved over some areas of the (Chelipus sp ). The footprints are preserved in a channel-margin facies of an Ogallala tracliway slab. Mammal trackways repre- braided stream. sent at least four ichnotaxa. -
Upper Neogene Stratigraphy and Tectonics of Death Valley — a Review
Earth-Science Reviews 73 (2005) 245–270 www.elsevier.com/locate/earscirev Upper Neogene stratigraphy and tectonics of Death Valley — a review J.R. Knott a,*, A.M. Sarna-Wojcicki b, M.N. Machette c, R.E. Klinger d aDepartment of Geological Sciences, California State University Fullerton, Fullerton, CA 92834, United States bU. S. Geological Survey, MS 975, 345 Middlefield Road, Menlo Park, CA 94025, United States cU. S. Geological Survey, MS 966, Box 25046, Denver, CO 80225-0046, United States dTechnical Service Center, U. S. Bureau of Reclamation, P. O. Box 25007, D-8530, Denver, CO 80225-0007, United States Abstract New tephrochronologic, soil-stratigraphic and radiometric-dating studies over the last 10 years have generated a robust numerical stratigraphy for Upper Neogene sedimentary deposits throughout Death Valley. Critical to this improved stratigraphy are correlated or radiometrically-dated tephra beds and tuffs that range in age from N3.58 Ma to b1.1 ka. These tephra beds and tuffs establish relations among the Upper Pliocene to Middle Pleistocene sedimentary deposits at Furnace Creek basin, Nova basin, Ubehebe–Lake Rogers basin, Copper Canyon, Artists Drive, Kit Fox Hills, and Confidence Hills. New geologic formations have been described in the Confidence Hills and at Mormon Point. This new geochronology also establishes maximum and minimum ages for Quaternary alluvial fans and Lake Manly deposits. Facies associated with the tephra beds show that ~3.3 Ma the Furnace Creek basin was a northwest–southeast-trending lake flanked by alluvial fans. This paleolake extended from the Furnace Creek to Ubehebe. Based on the new stratigraphy, the Death Valley fault system can be divided into four main fault zones: the dextral, Quaternary-age Northern Death Valley fault zone; the dextral, pre-Quaternary Furnace Creek fault zone; the oblique–normal Black Mountains fault zone; and the dextral Southern Death Valley fault zone. -
A World Revealed by Language: a New Seri Dictionary and Unapologetic Speculations on Seri Indian Deep History
A World Revealed by Language: A New Seri Dictionary and Unapologetic Speculations on Seri Indian Deep History JIM HILLS AND DAVID YETMAN Comcáac quih Yaza quih Hant Ihíip hac: Diccionario Seri-Español- Ingles, compiled by Mary Beck Moser and Stephen A. Marlett. Illustrated by Cathy Moser Marlett. Published by Plaza y Valdés Editores, Mexico City. 947 pages. ISBN: 970–722–453–3. The philosopher Ludwig Wittgenstein once mentioned that to imagine a language was to imagine a form of life (Wittgenstein 1953: 19). A comprehensive dictionary of any language exemplifies Wittgenstein’s point, but none more than the trilingual dictionary of the Seri language compiled by Mary Beck Moser and Steven Marlett. The work represents more than fifty years of research and over thirty years of living with the Seris in El Desemboque, Sonora, Mexico, in connection with the Summer Institute of Linguistics of the Wycliffe Bible Translators. The entries are in Seri, Spanish, and English, making the work of value to speakers of all three languages. The roughly six hundred Seris are already using the dictionary. Outsiders visiting them would be well advised to use it as well. The authors included Seri consultants at every step of the compilation. Seris reviewed the entries, suggesting changes and additions. Part of the dictionary’s usefulness lies in its incorporation not merely of single-word or phrase translations, but also of sentences or short paragraphs typically generated by Seris. This is critically important, since meanings are frequently so complex that a simple word-by-word translation simply will not do. As Moser and Marlett have realized, JIM HILLS is a longtime Seri hand and trader in Tucson, Arizona. -
UNIVERSITY of CALIFORNIA Los Angeles Southern California
UNIVERSITY OF CALIFORNIA Los Angeles Southern California Climate and Vegetation Over the Past 125,000 Years from Lake Sequences in the San Bernardino Mountains A dissertation submitted in partial satisfaction of the requirements for the degree of Doctor of Philosophy in Geography by Katherine Colby Glover 2016 © Copyright by Katherine Colby Glover 2016 ABSTRACT OF THE DISSERTATION Southern California Climate and Vegetation Over the Past 125,000 Years from Lake Sequences in the San Bernardino Mountains by Katherine Colby Glover Doctor of Philosophy in Geography University of California, Los Angeles, 2016 Professor Glen Michael MacDonald, Chair Long sediment records from offshore and terrestrial basins in California show a history of vegetation and climatic change since the last interglacial (130,000 years BP). Vegetation sensitive to temperature and hydroclimatic change tended to be basin-specific, though the expansion of shrubs and herbs universally signalled arid conditions, and landscpe conversion to steppe. Multi-proxy analyses were conducted on two cores from the Big Bear Valley in the San Bernardino Mountains to reconstruct a 125,000-year history for alpine southern California, at the transition between mediterranean alpine forest and Mojave desert. Age control was based upon radiocarbon and luminescence dating. Loss-on-ignition, magnetic susceptibility, grain size, x-ray fluorescence, pollen, biogenic silica, and charcoal analyses showed that the paleoclimate of the San Bernardino Mountains was highly subject to globally pervasive forcing mechanisms that register in northern hemispheric oceans. Primary productivity in Baldwin Lake during most of its ii history showed a strong correlation to historic fluctuations in local summer solar radiation values. -
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. -
Birds of the California Desert
BIRDS OF THE CALIFORNIA DESERT A. Sidney England and William F. Laudenslayer, Jr. i INTRODUCTION i \ 1 The term, "California desert", as used herein, refers to a politically defined region, most of i which is included in the California Desert Conservation Area (CDCA) designated by the Federal Land ; and Management Act of 1976 (FLPMA). Of the 25 million acres in the CDCA, about one-half are i public lands, most of which are managed by the Bureau of Land Management (BLM) according to the "980 P California Desert Conservation Area Plan mandated by FLPMA. The California desert encompasses those portions of the Great Basin Desert (east of the White and lnyo Mountains and A south of the California-Nevada border), the Mojave Desert, and the Colorado Desert which occur " within California; it does not include areas of riparian, aquatic, urban, and agricultural habitats . adjacent to the Colorado River. (Also see chapters on Geology by Norris and Bioclimatology by E3irdsI4 are the most conspicuous vertebrates found in the California deserts. Records exist for at least 425 species (Garrett and Dunn 1981) from 18 orders and 55 families. These counts far exceed those for mammals, reptiles, amphibians and fish, and they are similar to totals for the entire state -- 542 species from 20 orders and 65 families (Laudenslayer and Grenfell 1983). These figures may seem surprisingly similar considering the harsh, arid climates often believed characteristic of I desert environments. However, habiiats found in the California desert range from open water and h marshes at the Salton Sea to pinyon-juniper woodland and limber pinelbristlecone pine forests on a few mountain ranges. -
Open-File/Color For
Questions about Lake Manly’s age, extent, and source Michael N. Machette, Ralph E. Klinger, and Jeffrey R. Knott ABSTRACT extent to form more than a shallow n this paper, we grapple with the timing of Lake Manly, an inconstant lake. A search for traces of any ancient lake that inundated Death Valley in the Pleistocene upper lines [shorelines] around the slopes Iepoch. The pluvial lake(s) of Death Valley are known col- leading into Death Valley has failed to lectively as Lake Manly (Hooke, 1999), just as the term Lake reveal evidence that any considerable lake Bonneville is used for the recurring deep-water Pleistocene lake has ever existed there.” (Gale, 1914, p. in northern Utah. As with other closed basins in the western 401, as cited in Hunt and Mabey, 1966, U.S., Death Valley may have been occupied by a shallow to p. A69.) deep lake during marine oxygen-isotope stages II (Tioga glacia- So, almost 20 years after Russell’s inference of tion), IV (Tenaya glaciation), and/or VI (Tahoe glaciation), as a lake in Death Valley, the pot was just start- well as other times earlier in the Quaternary. Geomorphic ing to simmer. C arguments and uranium-series disequilibrium dating of lacus- trine tufas suggest that most prominent high-level features of RECOGNITION AND NAMING OF Lake Manly, such as shorelines, strandlines, spits, bars, and tufa LAKE MANLY H deposits, are related to marine oxygen-isotope stage VI (OIS6, In 1924, Levi Noble—who would go on to 128-180 ka), whereas other geomorphic arguments and limited have a long and distinguished career in Death radiocarbon and luminescence age determinations suggest a Valley—discovered the first evidence for a younger lake phase (OIS 2 or 4). -
Episodes 149 September 2009 Published by the International Union of Geological Sciences Vol.32, No.3
Contents Episodes 149 September 2009 Published by the International Union of Geological Sciences Vol.32, No.3 Editorial 150 IUGS: 2008-2009 Status Report by Alberto Riccardi Articles 152 The Global Stratotype Section and Point (GSSP) of the Serravallian Stage (Middle Miocene) by F.J. Hilgen, H.A. Abels, S. Iaccarino, W. Krijgsman, I. Raffi, R. Sprovieri, E. Turco and W.J. Zachariasse 167 Using carbon, hydrogen and helium isotopes to unravel the origin of hydrocarbons in the Wujiaweizi area of the Songliao Basin, China by Zhijun Jin, Liuping Zhang, Yang Wang, Yongqiang Cui and Katherine Milla 177 Geoconservation of Springs in Poland by Maria Bascik, Wojciech Chelmicki and Jan Urban 186 Worldwide outlook of geology journals: Challenges in South America by Susana E. Damborenea 194 The 20th International Geological Congress, Mexico (1956) by Luis Felipe Mazadiego Martínez and Octavio Puche Riart English translation by John Stevenson Conference Reports 208 The Third and Final Workshop of IGCP-524: Continent-Island Arc Collisions: How Anomalous is the Macquarie Arc? 210 Pre-congress Meeting of the Fifth Conference of the African Association of Women in Geosciences entitled “Women and Geosciences for Peace”. 212 World Summit on Ancient Microfossils. 214 News from the Geological Society of Africa. Book Reviews 216 The Geology of India. 217 Reservoir Geomechanics. 218 Calendar Cover The Ras il Pellegrin section on Malta. The Global Stratotype Section and Point (GSSP) of the Serravallian Stage (Miocene) is now formally defined at the boundary between the more indurated yellowish limestones of the Globigerina Limestone Formation at the base of the section and the softer greyish marls and clays of the Blue Clay Formation.