Utah Geological Survey Receives Three 1994 NEHRP Grants
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IODP-ICDP Kolloquium 2006 in Greifswald Ernst-Moritz-Arndt-Universität
IODP-ICDP Kolloquium 2006 in Greifswald Ernst-Moritz-Arndt-Universität 27. - 29. März 2006 IODP-ICDP-Kolloquium 2006 27. - 29. März 2006 im Rahmen des 550-jährigen Jubiläums der Ernst-Moritz-Arndt-Universität Greifswald Gemeinsames Kolloquium der DFG-Schwerpunkte IODP - Integrated Ocean Drilling Program und ICDP - International Continental Scientific Drilling Program 27. - 29. März 2006 im Berufsbildungszentrum Greifswald Institut für Geographie und Geologie Friedrich-Ludwig-Jahn-Str. 17a D-17487 Greifswald Tel. 03834 864560 Email: [email protected] IODP-ICDP-Kolloquium Greifswald 27.-29.3.2006 Umgebung Tagungszentrum 500 m . r t S - u a n e h t Friedrich-Ludwig -Jahn-Str a . bft-Tankstelle R - Wolgaster Straße r Geol. e h t l Institut a P W e ß a r Tagungszentrum t S 1: Cafeteria, Icebreaker r e Karl-Liebknecht-Ring u 2: Vortragshalle 3 a h 3: Posterraum c s r (4: Schwimmbad) a Eingang 2 W Pappelallee P Geographie 1 4 Eingang Geologie F.-L.-J.-Str. 17a Makarenkostr. Parkplätze Eingang Geologenkeller Innenstadtplan Ryck Hansering Hansering Roßmühlenstraße Hörsaal Abendvortrag Straße Friedrich-Löffler-Straße J-S-Bach- Knopfstraße Brüggstraße Fischstraße Kuhstraße Steinbeckerstraße Schuhhagen Lange Straße Markt Mensa I Rathaus Dom Mühlenstraße Straße Hansering Domstraße Wolgaster Straße Wall Goethestraße Anklamer Straße Wall Martin-Luther- Stephanistraße Bahnhofstraße 200 m IODP-ICDP-Kolloquium Greifswald 27.-29.3.2006 - Programm 1 Montag, 27. März 2006 11:00 13:00 Registrierung 13:00 14:00 Eröffnung - Oberbürgermeister der Universitäts- und Hansestadt Greifswald, Dr. Arthur König - Prodekan der Mathematisch-Naturwissenschaftlichen Fakultät der Universität Greifswald, Prof. Dr. Reinhard Zölitz-Möller - DFG-Referent Dr. -
The Paleoecology and Biogeography of Ordovician Edrioasteroids
University of Tennessee, Knoxville TRACE: Tennessee Research and Creative Exchange Doctoral Dissertations Graduate School 8-2011 The Paleoecology and Biogeography of Ordovician Edrioasteroids Rene Anne Lewis University of Tennessee - Knoxville, [email protected] Follow this and additional works at: https://trace.tennessee.edu/utk_graddiss Part of the Paleontology Commons Recommended Citation Lewis, Rene Anne, "The Paleoecology and Biogeography of Ordovician Edrioasteroids. " PhD diss., University of Tennessee, 2011. https://trace.tennessee.edu/utk_graddiss/1094 This Dissertation is brought to you for free and open access by the Graduate School at TRACE: Tennessee Research and Creative Exchange. It has been accepted for inclusion in Doctoral Dissertations by an authorized administrator of TRACE: Tennessee Research and Creative Exchange. For more information, please contact [email protected]. To the Graduate Council: I am submitting herewith a dissertation written by Rene Anne Lewis entitled "The Paleoecology and Biogeography of Ordovician Edrioasteroids." I have examined the final electronic copy of this dissertation for form and content and recommend that it be accepted in partial fulfillment of the requirements for the degree of Doctor of Philosophy, with a major in Geology. Michael L. McKinney, Major Professor We have read this dissertation and recommend its acceptance: Colin D. Sumrall, Linda C. Kah, Arthur C. Echternacht Accepted for the Council: Carolyn R. Hodges Vice Provost and Dean of the Graduate School (Original signatures are on file with official studentecor r ds.) THE PALEOECOLOGY AND BIOGEOGRAPHY OF ORDOVICIAN EDRIOASTEROIDS A Dissertation Presented for the Doctor of Philosophy Degree The University of Tennessee, Knoxville René Anne Lewis August 2011 Copyright © 2011 by René Anne Lewis All rights reserved. -
June -·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-1- -I -I -I -I
Wasatch Mountain Club JUNE -·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-1- -I -I -I -I I I -·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-· VOLUME 68, NUMBER 6, JUNE 1991 Magdaline Quinlan PROSPECTIVE MEMBER Leslie Mullins INFORMATION Managing Editors IF YOU HA VE MOVED: Please notify the WMC Member COVER LOGO: Knick Knickerbocker ship Director, 888 South 200 East, Suite 111, Salt Lake City, ADVERTISING: Jill Pointer UT 84111, of your new address. ART: Kate Juenger CLASSIFIED ADS: Sue De Vail IF YOU DID NOT RECEIVE YOUR RAMBLER: Con MAILING: Rose Novak, Mark McKenzie, Duke Bush tact the Membership Director to make sure your address is in PRODUCTION: Magdaline Quinlan the Club computer correctly. SKY CALENDAR: Ben Everitt IF YOU WANT TO SUBMIT AN ARTICLE: Articles, preferably typed double spaced, must be received by 6:00 pm THE RAMBLER (USPS 053-410) is published monthly by on the 15th of the month preceding publication. ~fail or de the WASATCH MOUNTAIN CLUB, Inc., 888 South 200 liver to the WMC office or to the Editor. Include your mrne East, Suite 111, Salt Lake City, UT 84111. Telephone: 363- and phone number on all submissions. 7150. Subscription rates of $12.00 per year are paid for by member ship dues only. Second-class Postage paid at Salt IF YOU WANT TO SUBMIT A PHOTO: We wekome Lake City, UT. photos of all kinds: black & white prints, color prints. and slides. Please include captions describing when and whcre POSTMASTER: Send address changes to THE RAM the photo was taken, and the names of the people in it (if you BLER, Membership Director, 888 South 200 East, Suite 111, know). -
This Is an Open Access Document Downloaded from ORCA, Cardiff University's Institutional Repository
This is an Open Access document downloaded from ORCA, Cardiff University's institutional repository: http://orca.cf.ac.uk/93788/ This is the author’s version of a work that was submitted to / accepted for publication. Citation for final published version: Wright, V. Paul and Cherns, Lesley 2016. How far did feedback between biodiversity and early diagenesis affect the nature of early Palaeozoic sea floors? Palaeontology 59 (6) , pp. 753-765. 10.1111/pala.12258 file Publishers page: https://doi.org/10.1111/pala.12258 <https://doi.org/10.1111/pala.12258> Please note: Changes made as a result of publishing processes such as copy-editing, formatting and page numbers may not be reflected in this version. For the definitive version of this publication, please refer to the published source. You are advised to consult the publisher’s version if you wish to cite this paper. This version is being made available in accordance with publisher policies. See http://orca.cf.ac.uk/policies.html for usage policies. Copyright and moral rights for publications made available in ORCA are retained by the copyright holders. SYMPOSIUM How far did feedback between biodiversity and early diagenesis affect the nature of early Palaeozoic sea floors? By V. PAUL WRIGHT1 and LESLEY CHERNS2 1 Natural Sciences, National Museum of Wales, Cathays Park, Cardiff, CF10 3NP, UK; e- mail [email protected] 2 School of Earth and Ocean Sciences, Cardiff University, Main Building, Park Place, Cardiff CF10 3AT, UK; e-mail [email protected] Abstract: Latest Precambrian to Early Palaeozoic biosphere evolution triggered changes in early diagenesis and carbonate precipitation which fed back to biodiversity through colonisation of hard substrates. -
Geologic Mapping Marches Forward
I '- TABLE OF CONTENTS Geologic Mapping Marches Forward ...... ... .. ... .. 1 The Director's Malcolm P. Weiss ... .. ... ..... 3 Geologic Mapping in Dixie . .. .. 7 Perspective Teacher's Comer .. .. .. ... 9 Glad You Asked .......... .. .10 bv 1\1. Lee Allison Survey News .. .... .......12 Energy News . .. .. .. .. .... ..14 Preliminary Analysis: Conoco National Monument Well . ...15 There are at most about 35 geologists in Design by Vicky Clarke the national park system and some of those are not doing geology but collect Cover photo: The old Harrisburg town National Park Service Goes Geologic site, with the Pine Valley Mountains in ing entrance fees or the like, or regulat the distance, Washington County, Utah. Recently, while driving back to Salt ing pre-existing mines and oil wells. Photo by Bob Biek. Lake City from Denver, I stopped in at Contrast that with over 900 biologists in Dinosaur National Monument, one of the park system and you can easily see State of Utah the geologic wonders of the region. Be why individual parks focus on plants, Michael 0 . Leavitt, Governor tween the visitor's center and the quar animals, and biodiversity rather than Department of Natural Resources Ted Stewart, Executive Director ry is a spectacular, nearly vertical layer the rocks, fossils, and minerals. of sandstone with prominent ripple UGS Board The Park Service is recognizing this bias Russell C. Babcock, Jr., Chairman marks. Expecting the sign at the base of and two years ago established the Geo Richard R. Kennedy C. William Berge the outcrop to describe this geologic E.H . Deedee O'Brien Jerry Golden logic Resources Division (GRD), based feature, I was surprised to find instead Craig Nelson D. -
Probabilistic Source-To-Sink Analysis of the Provenance of the California Paleoriver: Implications for the Early Eocene Paleog
PROBABILISTIC SOURCE-TO-SINK ANALYSIS OF THE PROVENANCE OF THE CALIFORNIA PALEORIVER: IMPLICATIONS FOR THE EARLY EOCENE PALEOGEOGRAPHY OF WESTERN NORTH AMERICA by Evan Rhys Jones A thesis submitted to the Faculty and the Board of Trustees of the Colorado School of Mines in partial fulfillment of the requirements for the degree of Doctor of Philosophy (Geology). Golden, Colorado Date __________________________ Signed: _____________________________ Evan Jones Signed: _____________________________ Dr. Piret Plink-Björklund Thesis Advisor Golden, Colorado Date __________________________ Signed: _____________________________ Dr. M. Stephen Enders Interim Department Head Department of Geology and Geological Engineering ii ABSTRACT The Latest Paleocene to Early Eocene Colton and Wasatch Formations exposed in the Roan Cliffs on the southern margin of the Uinta Basin, UT make up a genetically related lobate wedge of dominantly fluvial deposits. Estimates of the size of the river that deposited this wedge of sediment vary by more than an order of magnitude. Some authors suggest the sediments are locally derived from Laramide Uplifts that define the southern margin of the Uinta Basin, the local recycling hypotheses. Other authors suggest the sediments were transported by a river system with headwaters 750 km south of the Uinta Basin, the California paleoriver hypothesis. This study uses source-to-sink analysis to constrain the size of the river system that deposited the Colton-Wasatch Fm. We pay particular attention to the what magnitude and recurrence interval of riverine discharge is preserved in the Colton-Wasatch Fm. stratigraphy, and consider the effects this has on scaling discharge to the paleo-catchment area of the system. We develop new scaling relationships between discharge and catchment area using daily gauging data from 415 rivers worldwide. -
Conifers of the San Francisco Mountains, San Rafael Swell, and Roan Plateau Ronald M
Great Basin Naturalist Volume 31 | Number 3 Article 11 9-30-1971 Conifers of the San Francisco Mountains, San Rafael Swell, and Roan Plateau Ronald M. Lanner Utah State University Ronald Warnick Utah State University Follow this and additional works at: https://scholarsarchive.byu.edu/gbn Recommended Citation Lanner, Ronald M. and Warnick, Ronald (1971) "Conifers of the San Francisco Mountains, San Rafael Swell, and Roan Plateau," Great Basin Naturalist: Vol. 31 : No. 3 , Article 11. Available at: https://scholarsarchive.byu.edu/gbn/vol31/iss3/11 This Article is brought to you for free and open access by the Western North American Naturalist Publications at BYU ScholarsArchive. It has been accepted for inclusion in Great Basin Naturalist by an authorized editor of BYU ScholarsArchive. For more information, please contact [email protected], [email protected]. CONIFERS OF THE SAN FRANCISCO MOUNTAINS, SAN RAFAEL SWELL, AND ROAN PLATEAU 1 Ronald M. Lanner2 and Ronald Warnick 2 This is the second in a series of notes on conifer distribution in The Great Basin and adjacent mountain areas. An earlier paper (Lanner, 1971) presented results of field surveys in selected parts of northern Utah. This article will cover three Utah areas further to the south, which represent diverse geological and environmental conditions. The occurrence of previously unrecorded species localities is supported by specimens deposited in the Intermountain Herbarium at Utah State University, Logan, Utah (UTC). San Francisco Mountains The San Francisco Mountains, a typical Great Basin fault-block range, are located in Beaver and Millard counties. The range is ori- ented roughly on a north-south axis and is about 18 miles in length. -
Alleged Cnidarian Sphenothallus in the Late Ordovician of Baltica, Its Mineral Composition and Microstructure
Alleged cnidarian Sphenothallus in the Late Ordovician of Baltica, its mineral composition and microstructure OLEV VINN and KALLE KIRSIMÄE Vinn, O. and Kirsimäe, K. 2015. Alleged cnidarian Sphenothallus in the Late Ordovician of Baltica, its mineral compo- sition and microstructure. Acta Palaeontologica Polonica 60 (4): 1001–1008. Sphenothallus is a problematic fossil with possible cnidarian affinities. Two species of Sphenothallus, S. aff. longissimus and S. kukersianus, occur in the normal marine sediments of the Late Ordovician of Estonia. S. longissimus is more common than S. kukersianus and has a range from early Sandbian to middle Katian. Sphenothallus had a wide paleo- biogeographic distribution in the Late Ordovician. The tubes of Sphenothallus are composed of lamellae with a homo- geneous microstructure. The homogeneous microstructure could represent a diagenetic fabric, based on the similarity to diagenetic structures in Torellella (Cnidaria?, Hyolithelminthes). Tubes of Sphenothallus have an apatitic composition, but one tube contains lamellae of diagenetic calcite within the apatitic structure. Sphenothallus presumably had origi- nally biomineralized apatitic tubes. Different lattice parameters of the apatite indicate that biomineralization systems of phosphatic cnidarians Sphenothallus and Conularia sp. may have been different. Key words: Cnidaria?, Sphenothallus, apatite, microstructure, Ordovician, Sandbian, Katian, Estonia. Olev Vinn [[email protected]] and Kalle Kirsimäe [[email protected]], Department of Geology, University of Tartu, Ravila 14A, 50411 Tartu, Estonia. Copyright © 2015 O. Vinn and K. Kirsimäe. This is an open-access article distributed under the terms of the Creative Commons Attribution License (for details please see http://creativecommons.org/licenses/by/4.0/), which permits un- restricted use, distribution, and reproduction in any medium, provided the original author and source are credited. -
Geological Survey
DBPABTMBHT OF THE INTERIOR BULLETIN OF THK UNITED STATES GEOLOGICAL SURVEY No. 166 WASHINGTON GOVERNMENT PRINTING- OFFICE 1.900 UNITED STATES GEOLOGICAL SURVEY (JHAKLES D. WALCOTT, DIKECTOK QAZETTEEE OF UTAH BY HENRY G-ANNETT WASHINGTON GOVERNMENT rilTNTING OFFICE 1900 ' \ CONTENTS Page. Letter of transmittal........................................................ 7 General description of the State ..........-................. -..- - ---- 9 Political history and area ............................................... 9 Exploration............................................................ 10 Settlement.......................................;..................... 12 Topography ........................................................... 12 Rivers................................................................. 13 Great Salt Lake ........................................................ 14 Elevation.............................................................. 15 Climate................................................................. 16 Population............................................................. 16 Industries .............................................................. 18 Counties.........'.............................................-......... 20 Gazetteer of the State....................................................... 21 ILLUSTRATIONS. PLATE I. Map of Utah...................................................... 9 FIG. 1. Historical map...................................................... 10 - 5 LETTER OF TRANSMITTAL. DEPARTMENT -
Organism-Sediment Relationships in Silurian Marine Environments
ORGANISM-SEDIMENT RELATIONSHIPS IN SILURIAN MARINE ENVIRONMENTS by C. E. BRETT ABSTRACT.Organisms pIayed major roles as producers and modifiers of sediments in many Silurian marine env~ronments.Pelrnarozoan skeietal debris famed extensive shoals and banks in many high-enerw, tropical environments : algae. bvozoans. tabulate corals. and strematoporoids were the major skeieral contributors to reeial buridups common in mid and late SiIunan subtropical shelves. ArtlcuIare brachiopods and Lesser numben oiosrracodes, trilobites, and molluscs formed extensive. although reIatively !Em (5-15 mi. shell beds in shaIloiv shelf fac~es:pefagc. cephalopod limestones characrerized the circum-Gondwana region. Skeletd hard substrates and hardgrounds supported relarively complex eprfaunal suspenaan-feeding communities. The apparent scarclry of encollthic sponges and bivalves indicates thac rates of hard subsrrare bioerosron were far below those of post-Palaeozolc times. Substra~eselection. spatial compeotion. anc porarlry of c:Tpnc versus exposed subcommun~tiesare clearly evidenr. for the first rzme. in Ordovician to latesr Siiurian hard substrate cornrnuniries. Unconsoi~datedsediments displayed a wide variety of characrerisrtc trace and body fossd assoclatlons that were. to some degree. subsrrare conrrolled. Sand and silt subsrrates mpporred a low die'ersltv oi shelly organisms bur preserved abundant rraccs, nngmg from fkoiirhas ana .-~rthropir~cus-aomina~ed nensshore sed~mentsro offshore diverse ichnolicles. Some Silur~annearshore sediments display b~orurbat~on up to Im deep and contaln very Fen epifaunal organisms. susgesting destabiiizat~onof substrares. However. b1ogentc disturbance of offsfshore, soft substrates rematned relat~velyresrricted In the Sllur~anwnh tnfauna extenarng onlv abour 1C-15 cm tnro the sediment. Silunan epthunai organlrrns dispIayea varled morpnolo_eical ad~ptationsrs soft substrates. -
Decoupled Evolution of Soft and Hard Substrate Communities During the Cambrian Explosion and Great Ordovician Biodiversification Event
Decoupled evolution of soft and hard substrate communities during the Cambrian Explosion and Great Ordovician Biodiversification Event Luis A. Buatoisa,1, Maria G. Mánganoa, Ricardo A. Oleab, and Mark A. Wilsonc aDepartment of Geological Sciences, University of Saskatchewan, Saskatoon, SK, Canada S7N 5E2; bEastern Energy Resources Science Center, US Geological Survey, Reston, VA 20192; and cDepartment of Geology, The College of Wooster, Wooster, OH 44691 Edited by Steven M. Holland, University of Georgia, Athens, GA, and accepted by Editorial Board Member David Jablonski May 6, 2016 (received for review November 21, 2015) Contrasts between the Cambrian Explosion (CE) and the Great shed light on the natures of both radiations. Because there is still Ordovician Biodiversification Event (GOBE) have long been recog- controversy regarding Sepkoski’s nonstandardized curves of nized. Whereas the vast majority of body plans were established Phanerozoic taxonomic diversity (13–15), a rarefaction analysis as a result of the CE, taxonomic increases during the GOBE were was performed in an attempt to standardize diversity data. The manifested at lower taxonomic levels. Assessing changes of ichno- aims of this paper are to document the contrasting ichnodiversity diversity and ichnodisparity as a result of these two evolutionary and ichnodisparity trajectories in soft and hard substrate com- events may shed light on the dynamics of both radiations. The early munities during these two evolutionary events and to discuss the Cambrian (series 1 and 2) displayed a dramatic increase in ichnodi- possible underlying causes of this decoupled evolution. versity and ichnodisparity in softground communities. In contrast to this evolutionary explosion in bioturbation structures, only a few Results Cambrian bioerosion structures are known. -
Energy Trail Colorado River Loma DOUGLAS PASS Rangely White River Oil Dinosaur ENERGY TRAIL River Shale 70
Did you know miners and oilmen have been working BOUNDLESS LANDSCAPES & SPIRITED PEOPLE in northwest Colorado for generations? Douglas Pass Green Energy Trail Colorado River Loma DOUGLAS PASS Rangely White River Oil Dinosaur ENERGY TRAIL River Shale 70 Section on RD 139* Mancos Shale In the 1930s, technology enabled oilmen to drill over a mile down to oil pockets and open Colorado’s most productive oil field; just south of Douglas Pass look for Green River shale. Roan Plateau Energy Trail Color photo: courtesy Mary Lee Morlang; historical Colorado River Grand Junction BOOK CLIFFS ROAN CLIFFS CALLAHAN MT. Parachute ROAN CLIFFS Rifle GRAND HOGBACK 70 photo: courtesy CHS History Collection ca. MCC-2568 1910 Section parallel to I-70 70 FAULT Mancos Shale It is estimated that 1.8 trillion barrels of oil exists in the waxy compound or kerogen of the shale of the Roan Cliffs—the world’s largest known source. Axial to Yampa Energy Trail Oil Field Tow Creek Tow Craig Hayden Milner Steamboat Springs Did you know a wealth of natural resources are found 70 Section on U.S. 40* in northwest Colorado? Shale Mancos Deep below northwest Colorado’s canyons and rivers, forests and wilderness, mountains and parks, mesas and plateaus—lie Starting in the 1870s, coal enticed miners to this region and geological expanses of fossil fuels and minerals. For centuries, continues as a way of life today; and in other geological layers coal, oil, natural gas, and oil shale have lured men to open cut oil is pumped from a depth of 2,500 feet.