Stratigraphy of Inyan Kara Group and Localization of Uranium Deposits
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A Revised Taxonomy of the Iguanodont Dinosaur Genera and Species
ARTICLE IN PRESS + MODEL Cretaceous Research xx (2007) 1e25 www.elsevier.com/locate/CretRes A revised taxonomy of the iguanodont dinosaur genera and species Gregory S. Paul 3109 North Calvert Station, Side Apartment, Baltimore, MD 21218-3807, USA Received 20 April 2006; accepted in revised form 27 April 2007 Abstract Criteria for designating dinosaur genera are inconsistent; some very similar species are highly split at the generic level, other anatomically disparate species are united at the same rank. Since the mid-1800s the classic genus Iguanodon has become a taxonomic grab-bag containing species spanning most of the Early Cretaceous of the northern hemisphere. Recently the genus was radically redesignated when the type was shifted from nondiagnostic English Valanginian teeth to a complete skull and skeleton of the heavily built, semi-quadrupedal I. bernissartensis from much younger Belgian sediments, even though the latter is very different in form from the gracile skeletal remains described by Mantell. Currently, iguanodont remains from Europe are usually assigned to either robust I. bernissartensis or gracile I. atherfieldensis, regardless of lo- cation or stage. A stratigraphic analysis is combined with a character census that shows the European iguanodonts are markedly more morpho- logically divergent than other dinosaur genera, and some appear phylogenetically more derived than others. Two new genera and a new species have been or are named for the gracile iguanodonts of the Wealden Supergroup; strongly bipedal Mantellisaurus atherfieldensis Paul (2006. Turning the old into the new: a separate genus for the gracile iguanodont from the Wealden of England. In: Carpenter, K. (Ed.), Horns and Beaks: Ceratopsian and Ornithopod Dinosaurs. -
Phylogeny and Biogeography of Iguanodontian Dinosaurs, with Implications from Ontogeny and an Examination of the Function of the Fused Carpal-Digit I Complex
Phylogeny and Biogeography of Iguanodontian Dinosaurs, with Implications from Ontogeny and an Examination of the Function of the Fused Carpal-Digit I Complex By Karen E. Poole B.A. in Geology, May 2004, University of Pennsylvania M.A. in Earth and Planetary Sciences, August 2008, Washington University in St. Louis A Dissertation submitted to The Faculty of The Columbian College of Arts and Sciences of The George Washington University in partial fulfillment of the requirements for the degree of Doctor of Philosophy August 31, 2015 Dissertation Directed by Catherine Forster Professor of Biology The Columbian College of Arts and Sciences of The George Washington University certifies that Karen Poole has passed the Final Examination for the degree of Doctor of Philosophy as of August 10th, 2015. This is the final and approved form of the dissertation. Phylogeny and Biogeography of Iguanodontian Dinosaurs, with Implications from Ontogeny and an Examination of the Function of the Fused Carpal-Digit I Complex Karen E. Poole Dissertation Research Committee: Catherine A. Forster, Professor of Biology, Dissertation Director James M. Clark, Ronald Weintraub Professor of Biology, Committee Member R. Alexander Pyron, Robert F. Griggs Assistant Professor of Biology, Committee Member ii © Copyright 2015 by Karen Poole All rights reserved iii Dedication To Joseph Theis, for his unending support, and for always reminding me what matters most in life. To my parents, who have always encouraged me to pursue my dreams, even those they didn’t understand. iv Acknowledgements First, a heartfelt thank you is due to my advisor, Cathy Forster, for giving me free reign in this dissertation, but always providing valuable commentary on any piece of writing I sent her, no matter how messy. -
A New Species of Baenid Turtle from the Early Cretaceous Lakota Formation of South Dakota
Foss. Rec., 23, 1–13, 2020 https://doi.org/10.5194/fr-23-1-2020 © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. A new species of baenid turtle from the Early Cretaceous Lakota Formation of South Dakota Walter G. Joyce1, Yann Rollot1, and Richard L. Cifelli2 1Department of Geosciences, University of Fribourg, 1700 Fribourg, Switzerland 2Oklahoma Museum of Natural History, Norman, OK 73072, USA Correspondence: Walter G. Joyce ([email protected]) Received: 27 September 2019 – Revised: 6 January 2020 – Accepted: 22 January 2020 – Published: 12 February 2020 Abstract. Baenidae is a clade of paracryptodiran turtles (e.g., Lyson et al., 2011, 2019). Only little is known, by con- known from the late Early Cretaceous to Eocene of North trast, about the early evolution of the group, mostly due to America. The proposed sister-group relationship of Baenidae a lack of fossils. At present, only three unambiguous baenid to Pleurosternidae, a group of turtles known from sediments fossils are known from the Early Cretaceous, in particular dated as early as the Late Jurassic, suggests a ghost lin- the holotype specimens of Arundelemys dardeni Lipka et eage that crosses the early Early Cretaceous. We here doc- al., 2006, Trinitichelys hiatti Gaffney, 1972, and Protobaena ument a new species of paracryptodiran turtle, Lakotemys wyomingensis (Gilmore, 1919) from the Aptian–Albian of australodakotensis gen. and sp. nov., from the Early Creta- Maryland, Texas, and Wyoming, respectively. A broad set of ceous (Berriasian to Valanginian) Lakota Formation of South mostly unfigured fragmentary remains from the Early Creta- Dakota based on a poorly preserved skull and two partial ceous of Nevada (Bonde et al., 2008), Montana (Oreska et al., shells. -
The Professional Geologist Jan.Feb.Mar 2016
Volume 53, Number 1 THE PROFESSIONAL GEOLOGIST Jan.Feb.Mar 2016 TPG Volume 53 Number 1 Jan.Feb.Mar 2016 INSIDE THIS STUDENT ISSUE DEPARTMENTS FEATURES 6 Students in Action INTRAW Project Michael Lawless, CPG-09224 3 25/26 Student Chapters Field Camp in Ireland-International Studies 27 Editor’s Corner Jessica Davey, SA-4424 4 28 Test Your Knowledge The Best Geologist is the One Who Has Seen the Most Rocks Allison Richards, SA-5323 5 29 President’s Message Sailing the Seven C’s of Loss Prevention 30 Test Your Knowledge Answers Lawrence C. Weber, CPG-7120 8 31 Professional Ethics and Practices Undergraduate Education Beyond the Classes: The Importance of Research Experience 34 In Memory Brittany Kime, SA-3259 9 Your Senior Year Starts When You Enter College 35 Hydrothink Diane Burns, MEM-2471 10 35 Membership Totals Do You Have a Mentor? William J. Elliott, CPG-04194 12 36 Educator’s Page The Silver Market in 2014 40 Letter to the Editor Jim Burnell, CPG-11609 12 41 Student’s Voice The Success of Your Project Determines Your Future Oludamilola Alalade 13 42 Student’s Voice Two-and Three-Dimensional Finite Element Groundwater 43 Letter to the Editor Flow Models with Isothermal Freezing and Thawing H.D. McInvale, T.V. Hromadka II, M. Phillips, and B. Landry 14 44 Professional Services Directory Predicting Thaw Degradation in Algid Climates along Highway 46 Online Courses Embankments using a Boundary Element Method A.N. Johnson, T.V. Hromadka II, M. Phillips, and J. Williams 16 Development of a Multifunction Best Fit Computer Program to Model Sediment Transport Data in Rivers Bisti/De-Na-Zin Wilderness located in San Juan T.V. -
Insight on the Anatomy, Systematic Relationships, and Age of the Early Cretaceous Ankylopollexian Dinosaur Dakotadon Lakotaensis Clint A
Insight on the anatomy, systematic relationships, and age of the Early Cretaceous ankylopollexian dinosaur Dakotadon lakotaensis Clint A. Boyd1 and Darrin C. Pagnac2 1 North Dakota Geological Survey, Bismarck, North Dakota, USA 2 Department of Geology and Geological Engineering, South Dakota School of Mines and Technology, Rapid City, South Dakota, USA ABSTRACT Knowledge regarding the early evolution within the dinosaurian clade Ankylopollexia drastically increased over the past two decades, in part because of an increase in described taxa from the Early Cretaceous of North America. These advances motivated the recent completion of extensive preparation and conservation work on the holotype and only known specimen of Dakotadon lakotaensis, a basal ankylopollexian from the Lakota Formation of South Dakota. That specimen (SDSM 8656) preserves a partial skull, lower jaws, a single dorsal vertebra, and two caudal vertebrae. That new preparation work exposed several bones not included in the original description and revealed that other bones were previously misidentified. The presence of extensive deformation in areas of the skull is also noted that influenced inaccuracies in prior descriptions and reconstructions of this taxon. In addition to providing an extensive re-description of D. lakotaensis, this study reviews previously proposed diagnoses for this taxon, identifies two autapomorphies, and provides an extensive diVerential diagnosis. Dakotadon lakotaensis is distinct from the only other ankylopollexian taxon known from the Lakota Formation, Osmakasaurus depressus, in the presence of two prominent, anteroposteriorly oriented ridges on the ventral surfaces of the caudal vertebrae, the only overlapping material preserved Submitted 28 May 2015 Accepted 3 September 2015 between these taxa. The systematic relationships of D. -
Stratigraphy, Paleotectonics and Paleoenvironments of the Morrison Formation in the Bighorn Basin of Wyoming and Montana Dibakar Goswami Iowa State University
Iowa State University Capstones, Theses and Retrospective Theses and Dissertations Dissertations 1993 Stratigraphy, paleotectonics and paleoenvironments of the Morrison Formation in the Bighorn Basin of Wyoming and Montana Dibakar Goswami Iowa State University Follow this and additional works at: https://lib.dr.iastate.edu/rtd Part of the Geology Commons Recommended Citation Goswami, Dibakar, "Stratigraphy, paleotectonics and paleoenvironments of the Morrison Formation in the Bighorn Basin of Wyoming and Montana " (1993). Retrospective Theses and Dissertations. 10434. https://lib.dr.iastate.edu/rtd/10434 This Dissertation is brought to you for free and open access by the Iowa State University Capstones, Theses and Dissertations at Iowa State University Digital Repository. It has been accepted for inclusion in Retrospective Theses and Dissertations by an authorized administrator of Iowa State University Digital Repository. For more information, please contact [email protected]. INFORMATION TO USERS This manuscript has been reproduced from the microfilm master. UMI films the text directly from the original or copy submitted. Thus, some thesis and dissertation copies are in typewriter face, while others may be from any type of computer printer. The quality of this reproduction is dependent upon the quality of the copy submitted. Broken or indistinct print, colored or poor quality illustrations and photographs, print bleedthrough, substandard margins, and improper alignment can adversely afiect reproduction. In the unlikely event that the author did not send UMI a complete manuscript and there are missing pages, these will be noted. Also, if unauthorized copyright material had to be removed, a note will indicate the deletion. Oversize materials (e.g., maps, drawings, charts) are reproduced by sectioning the original, beginning at the upper left-hand corner and continuing from left to right in equal sections with small overlaps. -
THE LOWER CRETACEOUS in EAST-CENTRAL UTAH—THE CEDAR MOUNTAIN FORMATION and ITS BOUNDING STRATA James I
GEOLOGY OF THE INTERMOUNTAIN WEST an open-access journal of the Utah Geological Association Volume 3 2016 THE LOWER CRETACEOUS IN EAST-CENTRAL UTAH—THE CEDAR MOUNTAIN FORMATION AND ITS BOUNDING STRATA James I. Kirkland, Marina Suarez, Celina Suarez, and ReBecca Hunt-Foster A Field Guide Prepared For SOCIETY OF VERTEBRATE PALEONTOLOGY Annual Meeting, October 26 – 29, 2016 Grand America Hotel Salt Lake City, Utah, USA Pre-Meeting Field Trip October 23–25, 2016 © 2016 Utah Geological Association. All rights reserved. For permission to copy and distribute, see the following page or visit the UGA website at www.utahgeology.org for information. Email inquiries to [email protected]. GEOLOGY OF THE INTERMOUNTAIN WEST an open-access journal of the Utah Geological Association Volume 3 2016 Editors UGA Board Douglas A. Sprinkel Thomas C. Chidsey, Jr. 2016 President Bill Loughlin [email protected] 435.649.4005 Utah Geological Survey Utah Geological Survey 2016 President-Elect Paul Inkenbrandt [email protected] 801.537.3361 801.391.1977 801.537.3364 2016 Program Chair Andrew Rupke [email protected] 801.537.3366 [email protected] [email protected] 2016 Treasurer Robert Ressetar [email protected] 801.949.3312 2016 Secretary Tom Nicolaysen [email protected] 801.538.5360 Bart J. Kowallis Steven Schamel 2016 Past-President Jason Blake [email protected] 435.658.3423 Brigham Young University GeoX Consulting, Inc. 801.422.2467 801.583-1146 UGA Committees [email protected] [email protected] Education/Scholarship Loren Morton -
Geology of the Fort Hill Quadrangle Lincoln County Wyoming
Geology of the Fort Hill Quadrangle Lincoln County Wyoming I GEOLOGICAL SURVEY PROFESSIONAL PAPER 594-M - Geology of the Fort Hill Quadrangle Lincoln County Wyoming By STEVEN S. ORIEL SHORTER CONTRIBUTIONS TO GENERAL GEOLOGY GEOLOGICAL SURVEY PROFESSIONAL PAPER 594-M Surface and subsurface data of an area along the eastern margin of the Idaho-JI7joming thrust belt establish the geometry and times of movement of two ma;"or frontal thrust faults UNITED STATES GOVERNMENT PRINTING OFFICE. WASHINGTON 1969 UNITED STATES DEPARTMENT OF THE INTERIOR WALTER J. HICKEL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Page Stratigraphy-Continued Page Abstract __________________________________________ _ M1 Cretaceous System_____________________________ - M10 Introduction ______________________________________ _ 1 Gannett Group ____________________________ _ 10 Purpose of report ______________________________ _ 2 Bear River Formation ______________________ _ 11 Previous work _________________________________ _ 2 Aspen Formation __________________________ _ 11 Present work and methods ______________________ _ 2 Frontier Formation ________________________ _ 11 Acknowledgments ______________________________ _ 3 Cretaceous rocks below the Hogsback fault ________ _ 12 Geography________________________________________ _ Gannett Group ____________________________ _ 3 12 Location ______________________________________ _ 3 Bear River and Aspen -
Early and “Middle” Cretaceous Iguanodonts in Time and Space
ISSN (print): 1698-6180. ISSN (online): 1886-7995 www.ucm.es/info/estratig/journal.htm Journal of Iberian Geology 36 (2) 2010: 145-164 doi:10.5209/rev_JIGE.2010.v36.n2.3 Early and “Middle” Cretaceous Iguanodonts in Time and Space Iguanodontes del Cretácico temprano y “medio” en el tiempo y en el espacio K. Carpenter1*, Y. Ishida,2 1USU-CEU Prehistoric Museum, 155 East Main Street, Price, UT 84501, USA 2Department of Natural History Sciences, Hokkaido University, Sapporo 06-0810, Japan *[email protected] Received: 28/11/09 / Accepted: 30/06/10 Abstract Recent discoveries of diverse iguanodonts throughout the Cedar Mountain Formation (Utah, USA) have led us to assess the global diversity of Early Cretaceous iguanodonts. The record in England is more diverse than previously recognized due to Iguanodon being a wastebasket genus throughout the Twentieth Century. Several new taxa, previously recognized as generically distinct by Harry Grovier Seeley, are named. The spatial and temporal distributions of iguanodonts are plotted on global maps as a key to un- derstanding the origin of the Cedar Mountain Formation iguanodonts. Keywords: Early Cretaceous, Iguanodonts, Dinosauria Resumen Los recientes descubrimientos de diversos iguanodontes en la Formación Cedar Mountain (Utah, EE.UU.) nos han llevado a valo- rar la diversidad global de los iguanodontes del Cretácico temprano. El registro en Inglaterra es más diverso de lo que previamente se ha reconocido, debido a que Iguanodon ha sido tratado como un género “cajón de sastre” a lo largo de todo el siglo XX. Varios de los nuevos taxones, previamente reconocidos como genéricamente distintos por Harry Seeley Grovier, se denominan. -
North American Geology, Paleontology Petrology, and Mineralogy
Bulletin No. 221 Series G, Miscellaneous, 25 DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY CHARLES D. WALCOTT, DIRECTOR OF NORTH AMERICAN GEOLOGY, PALEONTOLOGY PETROLOGY, AND MINERALOGY FOR BY 3FJRJEJD BOUGHHXCMV WEEKS WASHINGTON @QVEE,NMENT PRINTING OFFICE 1 9 0 3 O'Q.S. Pago. Letter of transrnittal...................................................... 5 Introduction...............................:............................. 7 List of publications examined............................................. 9 Bibliography............................................................. 13 Addenda to bibliographies for previous years............................... 124 Classified key to the index................................................ 125 Index................................................................... 133 £3373 LETTER OF TRANSMITTAL. DEPARTMENT OF THE INTERIOR, UNITED STATES GEOLOGICAL SURVEY, Washington, D. C., October 20, 1903. SIR: I have the honor to transmit herewith the manuscript) of a bibliography and index of North American geology, paleontology, petrology, and mineralogy for the year 1902, and to request that it be published as a bulletin of the Survey. Very respectfully, F. B. WEEKS. Hon. CHARLES D. WALCOTT, Director United States Geological Survey. 5 BIBLIOaRAPHY AND INDEX OF NORTH AMERICAN GEOLOGY, PALEONTOLOGY, PETROLOGY, AND MINERALOGY FOR THE YEAR 1902. By FRED BOUGHTON WEEKS. INTRODUCTION. The arrangement of the material of the Bibliography and Index for 1902 is similar to that adopted for the previous publications (Bulletins Nos. 130, 135, 146, 149, 156, 162, 172, 188, 189, and 203). Several papers that should have been entered in the previous bulletins are here recorded, and the date of publication is given with each entry. Bibliography. The bibliography consists of full titles of separate papers, arranged alphabetically by authors' names, an abbreviated reference to the publication in which the paper is printed, and a brief description of the contents, each r>aper being numbered for index reference. -
Geology, Taphonomy, and Paleoecology of a Unique Upper Cretaceous Bonebed Near the Cretaceous-Tertiary Boundary in South Dakota
GEOLOGY, TAPHONOMY, AND PALEOECOLOGY OF A UNIQUE UPPER CRETACEOUS BONEBED NEAR THE CRETACEOUS-TERTIARY BOUNDARY IN SOUTH DAKOTA By © 2010 Robert A. DePalma II B.A., Florida Atlantic University, 2007 Submitted to the Department of Geology and the Faculty of the Graduate School of the University of Kansas In partial fulfillment of the requirements for the degree of Master of Science Advisory Committee: Co-Chairman: Larry D. Martin Co-Chairman: Paul Selden David Burnham Michael Engel David Fowle Date Defended: 21 April 2010 The thesis committee for Robert A. DePalma II certifies that this is the approved version of the following thesis: GEOLOGY, TAPHONOMY, AND PALEOECOLOGY OF A UNIQUE UPPER CRETACEOUS BONEBED NEAR THE CRETACEOUS-TERTIARY BOUNDARY IN SOUTH DAKOTA Advisory Committee: Co-Chairman: Larry D. Martin Co-Chairman: Paul Selden David Burnham Michael Engel David Fowle Date approved: 21 April 2010 i ABSTRACT Robert A. DePalma II Department of Geology, April 2010 University of Kansas This research examines a Konzentrat-Lagerstätte, the Bone Butte site, in the Upper Cretaceous Hell Creek Formation of South Dakota. Field data from a diverse multispecific bonebed in Harding County, South Dakota, including sedimentologic, stratigraphic, taphonomic, floral, and faunal observations, are used to reconstruct the depositional history, depositional environment, and paleoecology of the site, while comparing it to other sites within the Hell Creek Formation. Taphonomic analyses of bone completeness, abrasion, and sorting reveal the presence of autochthonous and allochthonous faunas, and demonstrate the heterogeneity of the Hell Creek dinosaurian fauna. Particularly noteworthy components of the Bone Butte ecology are undescribed insect and ornithurine bird faunas. -
Geological Society of America
BRIGHAM YOUNG UNIVERSITY GEOJ (3GY GEOLOGICAL SOCIETY OF AMERICA 1997 ANNUAL MEETING SALT LAKE CITY, UTAH PART2 TWO EDITED BY PAUL KARL LINK AND BART J. KOWALLIS VOLUME 42 1997 MESOZOIC TO RECENT GEOLOGY OF UTAH Edited by Paul Karl Link and Bart J. Kowallis BRIGHAM YOUNG UNIVERSITY GEOLOGY STUDIES Volume 42, Part 11, 1997 CONTENTS Triassic and Jurassic Macroinvertebrate Faunas of Utah: Field Relationships and Paleobiologic Significance ........................................ Carol M. Tang and David J. Bottjer Part 2: Trace fossils, hardgrounds and ostreoliths in the Carmel Formation (Middle Jurassic) of southwestern Utah ...........................................Mark A. Wilson Part 3: Low-diversity faunas of the Middle Jurassic Carmel Formation and their paleobiological implications ................................Carol M. Tang and David J. Bottjer Part 4: Paleoecology of Lower Triassic marine carbonates in the southwestern USA ....................... ......................................................David J. Bottjer and Jennifer K. Schubert Structure and Kinematics of a Complex Impact Crater, Upheaval Dome, Southeast Utah .........................Bryan J. Kriens, Eugene M. Shoemaker, and Ken E. Herkenhoff Stratigraphy, and structure of the Sevier thrust belt, and proximal foreland-basin system in central Utah: A transect from the Sevier Desert to the Wasatch Plateau ...................T. E Lawton, D. A. Sprinkel, F! G. DeCelles, G. Mitra, A. J. Sussman,, and M. l? Weiss Lower to Middle Cretaceous Dinosaur Faunas of the Central Colorado Plateau: A Key to Understanding 35 Million Years of Tectonics, Sedimentology, Evolution, and Biogeography ..................... James I. Kirkland, Brooks Britt, Donald L. Burge, Ken Carpenter, Richard Cifelli, Frank DeCourten, Jeffrey Eaton, Steve Hasiotis, and Tim Lawton Sequence Architecture, and Stacking Patterns in the Cretaceous Foreland Basin, Utah: Tectonism versus Eustasy ........................................