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A New Troodontid Theropod, Talos Sampsoni Gen. Et Sp. Nov., from the Upper Cretaceous Western Interior Basin of North America
A New Troodontid Theropod, Talos sampsoni gen. et sp. nov., from the Upper Cretaceous Western Interior Basin of North America Lindsay E. Zanno1,2*, David J. Varricchio3, Patrick M. O’Connor4,5, Alan L. Titus6, Michael J. Knell3 1 Field Museum of Natural History, Chicago, Illinois, United States of America, 2 Biological Sciences Department, University of Wisconsin-Parkside, Kenosha, Wisconsin, United States of America, 3 Department of Earth Sciences, Montana State University, Bozeman, Montana, United States of America, 4 Department of Biomedical Sciences, Ohio University College of Osteopathic Medicine, Athens, Ohio, United States of America, 5 Ohio Center for Ecology and Evolutionary Studies, Ohio University, Athens, Ohio, United States of America, 6 Grand Staircase-Escalante National Monument, Bureau of Land Management, Kanab, Utah, United States of America Abstract Background: Troodontids are a predominantly small-bodied group of feathered theropod dinosaurs notable for their close evolutionary relationship with Avialae. Despite a diverse Asian representation with remarkable growth in recent years, the North American record of the clade remains poor, with only one controversial species—Troodon formosus—presently known from substantial skeletal remains. Methodology/Principal Findings: Here we report a gracile new troodontid theropod—Talos sampsoni gen. et sp. nov.— from the Upper Cretaceous Kaiparowits Formation, Utah, USA, representing one of the most complete troodontid skeletons described from North America to date. Histological assessment of the holotype specimen indicates that the adult body size of Talos was notably smaller than that of the contemporary genus Troodon. Phylogenetic analysis recovers Talos as a member of a derived, latest Cretaceous subclade, minimally containing Troodon, Saurornithoides, and Zanabazar. -
Scoping Report: Grand Staircase-Escalante National
CONTENTS 1 Introduction .............................................................................................................................................. 1 2 Scoping Process ....................................................................................................................................... 3 2.1 Purpose of Scoping ........................................................................................................................... 3 2.2 Scoping Outreach .............................................................................................................................. 3 2.2.1 Publication of the Notice of Intent ....................................................................................... 3 2.2.2 Other Outreach Methods ....................................................................................................... 3 2.3 Opportunities for Public Comment ................................................................................................ 3 2.4 Public Scoping Meetings .................................................................................................................. 4 2.5 Cooperating Agency Involvement ................................................................................................... 4 2.6 National Historic Preservation Act and Tribal Consultation ....................................................... 5 3 Submission Processing and Comment Coding .................................................................................... 5 -
Terrestrial Vertebrate Fauna of the Kaiparowits Basin
Great Basin Naturalist Volume 40 Number 4 Article 2 12-31-1980 Terrestrial vertebrate fauna of the Kaiparowits Basin N. Duane Atwood U.S. Forest Service, Provo, Utah Clyde L. Pritchett Brigham Young University Richard D. Porter U.S. Fish and Wildlife Service, Provo, Utah Benjamin W. Wood Brigham Young University Follow this and additional works at: https://scholarsarchive.byu.edu/gbn Recommended Citation Atwood, N. Duane; Pritchett, Clyde L.; Porter, Richard D.; and Wood, Benjamin W. (1980) "Terrestrial vertebrate fauna of the Kaiparowits Basin," Great Basin Naturalist: Vol. 40 : No. 4 , Article 2. Available at: https://scholarsarchive.byu.edu/gbn/vol40/iss4/2 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]. TERRESTRIAL VERTEBRATE FAUNA OF THE KAIPAROWITS BASIN N. Diiane Atwood', Clyde L. Pritchctt', Richard D. Porter', and Benjamin W. Wood' .\bstr^ct.- This report inehides data collected during an investigation by Brighani Young University personnel to 1976, as well as a literature from 1971 review. The fauna of the Kaiparowits Basin is represented by 7 species of salamander, toads, mnphihians (1 5 and 1 tree frog), 29 species of reptiles (1 turtle, 16 lizards, and 12 snakes), 183 species of birds (plus 2 hypothetical), and 74 species of mammals. Geographic distribution of the various species within the basin are discussed. Birds are categorized according to their population and seasonal status. -
A Preliminary Assessment of Archaeological Resources Within the Grand Staircase-Escalante National Monument, Utah
A PRELIMINARY ASSESSMENT OF ARCHAEOLOGICAL RESOURCES WITHIN THE GRAND STAIRCASE-ESCALANTE NATIONAL MONUMENT, UTAH by David B. Madsen Common rock art elements of the Fremont and Anasazi on the Colorado Plateau and the Grand Staircase-Escalante National Monument. ,I!! CIRCULAR 95 . 1997 I~\' UTAH GEOLOGICAL SURVEY ." if;~~ 6EPARTMENT OF NATURAL RESOURCES ISBN 1-55791-605-5 STATE OF UTAH Michael O. Leavitt, Governor DEPARTMENT OF NATURAL RESOURCES Ted Stewart, Executive Director UTAH GEOLOGICAL SURVEY M. Lee Allison~ Director UGS Board Member Representing Russell C. Babcock, Jr. (chairman) .................................................................................................. Mineral Industry D. Cary Smith ................................................................................................................................... Mineral Industry Richard R. Kennedy ....................................................................................................................... Civil Engineering E.H. Deedee O'Brien ......................................................................................................................... Public-at-Large C. William Berge .............................................................................................................................. Mineral Industry Jerry Golden ..................................................................................................................................... Mineral Industry Milton E. Wadsworth ............................................................................................... -
A Large Hadrosaurid Dinosaur from Presa San Antonio, Cerro Del Pueblo Formation, Coahuila, Mexico
A large hadrosaurid dinosaur from Presa San Antonio, Cerro del Pueblo Formation, Coahuila, Mexico ROGELIO ANTONIO REYNA-HERNÁNDEZ, HÉCTOR E. RIVERA-SYLVA, LUIS E. SILVA-MARTÍNEZ, and JOSÉ RUBÉN GUZMAN-GUTIÉRREZ Reyna-Hernández, R.A., Rivera-Sylva, H.E., Silva-Martínez, L.E., and Guzman-Gutiérrez, J.R. 2021. A large hadro- saurid dinosaur from Presa San Antonio, Cerro del Pueblo Formation, Coahuila, Mexico. Acta Palae onto logica Polonica 66 (Supplement to x): xxx–xxx. New hadrosaurid postcranial material is reported, collected near Presa San Antonio, Parras de la Fuente municipality, Coahuila, Mexico, in a sedimentary sequence belonging to the upper Campanian of the Cerro del Pueblo Formation, in the Parras Basin. The skeletal remains include partial elements from the pelvic girdle (left ilium, right pubis, ischium, and incomplete sacrum), a distal end of a left femur, almost complete right and left tibiae, right metatarsals II and IV, cervical and caudal vertebrae. Also, partially complete forelimb elements are present, which are still under preparation. The pubis shows characters of the Lambeosaurinae morphotypes, but the lack of cranial elements does not allow us to directly differentiate this specimen from the already described hadrosaurid taxa from the studied area, such as Velafrons coahuilensis, Latirhinus uitstlani, and Kritosaurus navajovius. This specimen, referred as Lambeosaurinae indet., adds to the fossil record of the hadrosaurids in southern Laramidia during the Campanian. Key words: Dinosauria, Hadrosauridae, Lambeosaurinae, Cretaceous, Campanian, Mexico. Rogelio Antonio Reyna-Hernández [[email protected]], Luis E. Silva-Martínez [[email protected]], Laboratorio de Paleobiología, Facultad de Ciencias Biológicas, Universidad Autónoma de Nuevo León, Av. -
Pluridisciplinary Evidence for Burial for the La Ferrassie 8 Neandertal Child
Pluridisciplinary evidence for burial for the La Ferrassie 8 Neandertal child Balzeau, Antoine; Turq, Alain; Talamo, Sahra; Daujeard, Camille; Guérin, Guillaume; Welker, Frido; Crevecoeur, Isabelle; Fewlass, Helen; Hublin, Jean-Jacques; Lahaye, Christelle; Maureille, Bruno; Meyer, Matthias; Schwab, Catherine; Gómez-Olivencia, Asier Published in: Scientific Reports DOI: 10.1038/s41598-020-77611-z Publication date: 2020 Document version Publisher's PDF, also known as Version of record Document license: CC BY Citation for published version (APA): Balzeau, A., Turq, A., Talamo, S., Daujeard, C., Guérin, G., Welker, F., Crevecoeur, I., Fewlass, H., Hublin, J-J., Lahaye, C., Maureille, B., Meyer, M., Schwab, C., & Gómez-Olivencia, A. (2020). Pluridisciplinary evidence for burial for the La Ferrassie 8 Neandertal child. Scientific Reports, 10(1), [21230]. https://doi.org/10.1038/s41598- 020-77611-z Download date: 24. sep.. 2021 www.nature.com/scientificreports OPEN Pluridisciplinary evidence for burial for the La Ferrassie 8 Neandertal child Antoine Balzeau1,2*, Alain Turq3, Sahra Talamo4,5, Camille Daujeard1, Guillaume Guérin6,7, Frido Welker8,9, Isabelle Crevecoeur10, Helen Fewlass 4, Jean‑Jacques Hublin 4, Christelle Lahaye6, Bruno Maureille10, Matthias Meyer11, Catherine Schwab12 & Asier Gómez‑Olivencia13,14,15* The origin of funerary practices has important implications for the emergence of so‑called modern cognitive capacities and behaviour. We provide new multidisciplinary information on the archaeological context of the La Ferrassie 8 Neandertal skeleton (grand abri of La Ferrassie, Dordogne, France), including geochronological data ‑14C and OSL‑, ZooMS and ancient DNA data, geological and stratigraphic information from the surrounding context, complete taphonomic study of the skeleton and associated remains, spatial information from the 1968–1973 excavations, and new (2014) feldwork data. -
38-Simpson Et Al (Wahweap Fm).P65
Sullivan et al., eds., 2011, Fossil Record 3. New Mexico Museum of Natural History and Science, Bulletin 53. 380 UPPER CRETACEOUS DINOSAUR TRACKS FROM THE UPPER AND CAPPING SANDSTONE MEMBERS OF THE WAHWEAP FORMATION, GRAND STAIRCASE-ESCALANTE NATIONAL MONUMENT, UTAH, U.S.A. EDWARD L. SIMPSON1, H. FITZGERALD MALENDA1, MATTATHIAS NEEDLE1, HANNAH L. HILBERT-WOLF2, ALEX STEULLET3, KEN BOLING3, MICHAEL C. WIZEVICH3 AND SARAH E. TINDALL1 1 Department of Physical Sciences, Kutztown University, Kutztown, PA 19530; 2 Department of Geology, Carleton College, Northfield, MN, 55057; 3 Central Connecticut State University, Department of Physics and Earth Sciences, New Britain, Connecticut 06050, USA Abstract—Tridactyl tracks were identified in the fluvial strata of the Upper Cretaceous Wahweap Formation in Grand Staircase-Escalante National Monument, southern Utah, U.S.A. An isolated track and a trackway are located within the upper member at the Cockscomb, and an isolated track is in the capping sandstone member at Wesses Canyon. The upper member tracks are tridactyl pes imprints consisting of a longer, blunt digit III and shorter, blunt digits II-IV. This trace corresponds well to an ornithropod dinosaur as the trackmaker. The capping sandstone member track is a tridactyl pes with an elongate digit III and shorter digits II-IV. Claw impressions are present on the terminus of digits II and III. This trace is consistent with the pes impression of a one meter tall theropod. The tracks further highlight the diversity of dinosaurs in the capping sandstone of the Wahweap Formation. INTRODUCTION During the Late Cretaceous, North America, in particular the west- ern United States, was the site of a radiation of new dinosaurian genera. -
Implications for Predatory Dinosaur Macroecology and Ontogeny in Later Late Cretaceous Asiamerica
Canadian Journal of Earth Sciences Theropod Guild Structure and the Tyrannosaurid Niche Assimilation Hypothesis: Implications for Predatory Dinosaur Macroecology and Ontogeny in later Late Cretaceous Asiamerica Journal: Canadian Journal of Earth Sciences Manuscript ID cjes-2020-0174.R1 Manuscript Type: Article Date Submitted by the 04-Jan-2021 Author: Complete List of Authors: Holtz, Thomas; University of Maryland at College Park, Department of Geology; NationalDraft Museum of Natural History, Department of Geology Keyword: Dinosaur, Ontogeny, Theropod, Paleocology, Mesozoic, Tyrannosauridae Is the invited manuscript for consideration in a Special Tribute to Dale Russell Issue? : © The Author(s) or their Institution(s) Page 1 of 91 Canadian Journal of Earth Sciences 1 Theropod Guild Structure and the Tyrannosaurid Niche Assimilation Hypothesis: 2 Implications for Predatory Dinosaur Macroecology and Ontogeny in later Late Cretaceous 3 Asiamerica 4 5 6 Thomas R. Holtz, Jr. 7 8 Department of Geology, University of Maryland, College Park, MD 20742 USA 9 Department of Paleobiology, National Museum of Natural History, Washington, DC 20013 USA 10 Email address: [email protected] 11 ORCID: 0000-0002-2906-4900 Draft 12 13 Thomas R. Holtz, Jr. 14 Department of Geology 15 8000 Regents Drive 16 University of Maryland 17 College Park, MD 20742 18 USA 19 Phone: 1-301-405-4084 20 Fax: 1-301-314-9661 21 Email address: [email protected] 22 23 1 © The Author(s) or their Institution(s) Canadian Journal of Earth Sciences Page 2 of 91 24 ABSTRACT 25 Well-sampled dinosaur communities from the Jurassic through the early Late Cretaceous show 26 greater taxonomic diversity among larger (>50kg) theropod taxa than communities of the 27 Campano-Maastrichtian, particularly to those of eastern/central Asia and Laramidia. -
Giant Raptor Dinosaur Discovered in Utah Monument 3 April 2006
Giant Raptor Dinosaur Discovered in Utah Monument 3 April 2006 and published in the latest issue of the Journal of Vertebrate Paleontology, was authored by Lindsay Zanno, a graduate student in the Department of Geology and Geophysics, and Scott Sampson, chief curator at the Utah Museum of Natural History (UMNH), and associate professor in the Department of Geology and Geophysics. The new dinosaur, formally dubbed Hagryphus giganteus, which means "giant four-footed, bird-like god of the western desert” in reference to the animal's outward resemblance to a large land bird, its giant stature, and its discovery in the Utah desert. Hagryphus is a member of the oviraptorosaurs, a group of bird-like feathered dinosaurs with toothless beaks, powerful arms and formidable claws. These enigmatic animals are thought by some paleontologists to have been omnivorous, feeding on a mixture of meat and plants. Although only the hands and feet of The fleshed-out rendering by artist Michael Skrepnick Hagryphus are known, the scientists were able to best represents what the new dinosaur, called Hagryphus, looked like. Photo Credit: copyright Michael use the animal"s close relatives to estimate the size W. Skrepnick 1999 of the skeleton. The researchers say they do not know why this dinosaur was so much larger than its northern cousins but speculate that it may have been related to different environmental conditions Scientists from the University of Utah and the Utah in the south. Museum of Natural History have discovered the remains of a new bird-like, meat-eating dinosaur in Ruthless Thief or Protective Parent? Grand Staircase-Escalante National Monument (GSENM), southern Utah. -
Of Coal in the Kaiparowits Plateau, Southern Utah
Chapter T National Coal Resource Geologic Overview and Resource Assessment Assessment of Coal in the Kaiparowits Plateau, Southern Utah Click here to return to Disc 1 By Robert D. Hettinger,1 Laura N.R. Roberts,1 Volume Table of Contents Laura R.H. Biewick,1 and Mark A. Kirschbaum1 Chapter T of Geologic Assessment of Coal in the Colorado Plateau: Arizona, Colorado, New Mexico, and Utah Edited by M.A. Kirschbaum, L.N.R. Roberts, and L.R.H. Biewick U.S. Geological Survey Professional Paper 1625–B* Chapter T supersedes U.S. Geological Survey Open-File Report 96-539 1 U.S. Geological Survey, Denver, Colorado 80225 * This report, although in the USGS Professional Paper series, is available only on CD-ROM and is not available separately U.S. Department of the Interior U.S. Geological Survey Contents Abstract........................................................................................................................................................ T1 Introduction ................................................................................................................................................... 2 Purpose and Scope ............................................................................................................................. 2 Methods ................................................................................................................................................ 2 Lithologic and Stratigraphic Data ............................................................................................ 2 -
University of Birmingham Deep-Time Biodiversity Patterns and The
University of Birmingham Deep-time biodiversity patterns and the dinosaurian fossil record of the Late Cretaceous Western Interior, North America Maidment, Susannah; Dean, Christopher; Mansergh, Robert; Butler, Richard DOI: 10.1098/rspb.2021.0692 License: None: All rights reserved Document Version Peer reviewed version Citation for published version (Harvard): Maidment, S, Dean, C, Mansergh, R & Butler, R 2021, 'Deep-time biodiversity patterns and the dinosaurian fossil record of the Late Cretaceous Western Interior, North America', Royal Society of London. Proceedings B. Biological Sciences, vol. 288, no. 1953, 20210692. https://doi.org/10.1098/rspb.2021.0692 Link to publication on Research at Birmingham portal General rights Unless a licence is specified above, all rights (including copyright and moral rights) in this document are retained by the authors and/or the copyright holders. The express permission of the copyright holder must be obtained for any use of this material other than for purposes permitted by law. •Users may freely distribute the URL that is used to identify this publication. •Users may download and/or print one copy of the publication from the University of Birmingham research portal for the purpose of private study or non-commercial research. •User may use extracts from the document in line with the concept of ‘fair dealing’ under the Copyright, Designs and Patents Act 1988 (?) •Users may not further distribute the material nor use it for the purposes of commercial gain. Where a licence is displayed above, please note the terms and conditions of the licence govern your use of this document. When citing, please reference the published version. -
A New Late Permian Burnetiamorph from Zambia Confirms Exceptional
fevo-09-685244 June 19, 2021 Time: 17:19 # 1 ORIGINAL RESEARCH published: 24 June 2021 doi: 10.3389/fevo.2021.685244 A New Late Permian Burnetiamorph From Zambia Confirms Exceptional Levels of Endemism in Burnetiamorpha (Therapsida: Biarmosuchia) and an Updated Paleoenvironmental Interpretation of the Upper Madumabisa Mudstone Formation Edited by: 1 † 2 3,4† Mark Joseph MacDougall, Christian A. Sidor * , Neil J. Tabor and Roger M. H. Smith Museum of Natural History Berlin 1 Burke Museum and Department of Biology, University of Washington, Seattle, WA, United States, 2 Roy M. Huffington (MfN), Germany Department of Earth Sciences, Southern Methodist University, Dallas, TX, United States, 3 Evolutionary Studies Institute, Reviewed by: University of the Witwatersrand, Johannesburg, South Africa, 4 Iziko South African Museum, Cape Town, South Africa Sean P. Modesto, Cape Breton University, Canada Michael Oliver Day, A new burnetiamorph therapsid, Isengops luangwensis, gen. et sp. nov., is described Natural History Museum, on the basis of a partial skull from the upper Madumabisa Mudstone Formation of the United Kingdom Luangwa Basin of northeastern Zambia. Isengops is diagnosed by reduced palatal *Correspondence: Christian A. Sidor dentition, a ridge-like palatine-pterygoid boss, a palatal exposure of the jugal that [email protected] extends far anteriorly, a tall trigonal pyramid-shaped supraorbital boss, and a recess †ORCID: along the dorsal margin of the lateral temporal fenestra. The upper Madumabisa Christian A. Sidor Mudstone Formation was deposited in a rift basin with lithofacies characterized orcid.org/0000-0003-0742-4829 Roger M. H. Smith by unchannelized flow, periods of subaerial desiccation and non-deposition, and orcid.org/0000-0001-6806-1983 pedogenesis, and can be biostratigraphically tied to the upper Cistecephalus Assemblage Zone of South Africa, suggesting a Wuchiapingian age.