Lithologic Evidence of the Jurassic/Cretaceous Boundary

Total Page:16

File Type:pdf, Size:1020Kb

Lithologic Evidence of the Jurassic/Cretaceous Boundary LITHOLOGIC EVIDENCE OF THE JURASSIC/CRETACEOUS BOUNDARY WITHIN THE NONMARINE CEDAR MOUNTAIN FORMATION, SAN RAFAEL SWELL, UTAH A thesis presented to the faculty of the College of Arts and Sciences of Ohio University In partial fulfillment of the requirements for the degree Master of Science James D. Ayers August 2004 LITHOLOGIC EVIDENCE OF THE JURASSIC/CRETACEOUS BOUNDARY WITHIN THE NONMARINE CEDAR MOUNTAIN FORMATION, SAN RAFAEL SWELL, UTAH BY JAMES D. AYERS has been approved for the Department of Geological Sciences and the College of Arts and Sciences of Ohio University by Gregory C. Nadon Assistant Professor Leslie A. Flemming Dean, College of Arts and Sciences of Ohio University AYERS, JAMES D. M.S. August 2004. Geological Sciences Lithologic Evidence of the Jurassic/Cretaceous Boundary Within the Nonmarine Cedar Mountain Formation, San Rafael Swell, Utah (189 pp.) Director of Thesis: Gregory C. Nadon The Jurassic/Cretaceous boundary in central Utah occurs at a major unconformity within a foreland basin. Paleontological data are absent and the boundary is typically placed at the lower contact of the Buckhorn Conglomerate Member of the Cedar Mountain Formation based on the assumption that this contact represents an erosional unconformity. Lithologic and petrographic evidence from this study indicate the presence of a Stage 6 calcrete and a groundwater silcrete, which both indicate long-term geomorphic stability. These data suggest that the Jurassic/Cretaceous boundary should be placed at the top of the calcrete within the basal Cedar Mountain Shale Member. The fluvial architecture of the strata below and above the boundary suggests that the lower Cedar Mountain Formation records the subtle transition from deposition within the proximal back-bulge depozone during the Late Jurassic to deposition within the distal foredeep depozone during the Early Cretaceous. Approved: Gregory C. Nadon Assistant Professor Acknowledgments I greatly appreciate the patients and support of my committee, family and friends throughout the research and writing of this thesis. To my wonderful girlfriend Kristin, thank you for all the love, understanding, and encouragement. Your faith in my ability to complete this project is greatly appreciated. To Gregory C. Nadon, thank you for your guidance, inspiration, and for providing me the opportunity to work on this exciting project. You have been a wonderful mentor and a great friend. To Xavier Roca, thank you for your assistance and extended discussions in the field. You were a great inspiration. To Elizabeth Gierlowski-Kordesch and David L. Kidder, thank you for your assistance. I benefited greatly from our conversations. 5 Table of Contents Page Abstract…………………………………………………………………………… 3 Acknowledgments…………………………………………………………….….. 4 List of Tables……………………………………………………………………... 7 List of Figures…………………………………………………………………….. 8 Chapter 1. Introduction…………………………………………………………… 11 1.1 Introduction…………………………………………………………… 11 1.2 Purpose....…………………………………………………………….. 17 1.3 Study Area……………………………………………………………. 17 Chapter 2. Previous Work………………………………………………………… 21 2.1 Introduction…………………………………………………………... 21 2.2 Stratigraphy…………………………………………………………… 21 2.2.1 Morrison Formation………………………………………… 21 2.2.2 Cedar Mountain Formation………………………………… 25 2.3 Late Jurassic-Early Cretaceous Foreland Basin Development………. 30 2.4 Nonmarine Sequence-Stratigraphy…………………………………… 33 Chapter 3. Methodology…………………………………………………………. 37 3.1 Fieldwork…………………………………………………………….. 37 3.2 Stratigraphic Data…………………………………………………….. 37 3.3 Sedimentologic Data………………………………………………….. 38 3.4 Petrographic Data……………………………………………………. 38 Chapter 4. Lithofacies Analysis………………………………………………….. 40 4.1 Introduction…………………………………………………………… 40 4.2 Facies A: Conglomerate Facies………………………………………. 40 4.2.1 Introduction………………………………………………… 40 4.2.2 Facies A1: Buckhorn………………………………………… 40 4.2.3 Facies A2: Buckhorn-equivalent……………………………. 51 4.2.3.1 Introduction………………………………………. 51 4.2.3.2 Indurated A2 Conglomerates……………………… 52 4.2.3.3 Poorly Indurated A2 Conglomerates……………… 54 4.2.4 Facies A3: Red Conglomerate………………………………. 57 4.3 Facies B: Sandstone Facies…………………………………………… 62 4.3.1 Introduction………………………………………………… 62 4.3.2 Facies B1: Buckhorn Sandstones…………………………… 62 4.3.3 Facies B2: Buckhorn-equivalent Sandstones……………….. 70 6 Page 4.3.4 Facies B3: White Sandstone………………………………… 71 4.3.5 Facies B4: Red Conglomerate Sandstones………………….. 78 4.3.6 Facies B5: Isolated Sandstone Bodies………………………. 79 4.4 Facies C: Siltstone Facies…………………………………………….. 80 4.5 Facies D: Mudstone Facies…………………………………………… 81 4.5.1 Facies D1: Mudstone……………………………………….. 81 4.5.2 Facies D2: Pebbly Mudstone……………………………….. 82 4.6 Facies E: Carbonate Facies…………………………………………… 85 4.6.1 Introduction………………………………………………… 85 4.6.2 Facies E1: Lacustrine Carbonate……………………………. 85 4.6.2.1 Lower Carbonate………………………………….. 85 4.6.2.2 Middle Carbonate………………………………… 103 4.6.2.3 Upper Carbonate…………………………………. 104 4.6.3 Facies E2: Calcrete…………………………………………. 106 Chapter 5. Lithofacies Associations and Fluvial Architecture…………………… 119 5.1 Introduction…………………………………………………………… 119 5.2 Lithofacies Associations……………………………………………… 123 5.2.1 Unit 1: The Buckhorn Conglomerate………………………. 123 5.2.2 Unit 2: The Buckhorn-equivalent…………………………… 127 5.2.3 Unit 3: The Lower Carbonate………………………………. 129 5.2.4 Unit 4: The Pedogenic Calcrete Profile…………………….. 130 5.2.5 Unit 5: The White Sandstone………………………………. 136 5.2.6 Unit 6: The Middle Carbonate……………………………… 137 5.2.7 Unit 7: The Red Conglomerate…………………………….. 138 5.2.8 Unit 8: The Upper Carbonate………………………………. 142 5.3 Fluvial Architecture…………………………………………………… 143 Chapter 6. Conclusions…………………………………………………………… 150 References………………………………………………………………………… 152 Appendix A: Measured Sections and Cross-sections…………………………….. 160 Appendix B: Paleocurrent Measurements………………………………………... 180 Appendix C: Point Count and Pebble Count Data……………………………….. 188 7 List of Tables Table Page 5.1 Lithofacies assemblage, lithology, and depositional environment of units…… 120 8 List of Figures Figure Page 1.1 Generalized stratigraphic column…………………………………………….. 12 1.2 Diagrammatic cross-section of Late Jurassic-Late Cretaceous foreland basin.. 13 1.3 Generalized map of the Sevier orogenic belt and its foreland basin…………. 15 1.4 Chart of previous chronostratigraphic interpretations………………………... 16 1.5 Location map of the study area……………………………………………….. 18 1.6 Structural map of the Cedar Mountain region………………………………... 19 2.1 Generalized paleogeographic map of the Albian foreland basin system…….. 34 2.2 Nonmarine sequence-stratigraphic diagram………………………………….. 35 4.1 Diagrammatic cross-section of the facies within the study interval………….. 41 4.2 Map showing the location of measured sections……………………………... 43 4.3 a Outcrop photo of Facies A1 and B1…………………………………………. 44 b Close-up photo of Facies A1………………………………………………... 44 4.4 Paleocurrent map for Facies A1 and B1 as well as Facies A2 and B2………… 46 4.5 “Capping” megaquartz cement……………………………………………….. 48 4.6 Schematic section of a pedogenic silcrete……………………………………. 50 4.7 a Outcrop photo of the Indurated A2 Conglomerates and Facies B2…………. 53 b Close-up photo of the Indurated A2 Conglomerates………………………... 53 4.8 Outcrop photo of the Poorly Indurated A2 Conglomerates…………………... 55 4.9 a Outcrop photo of Facies A3………………………………………………… 58 b Outcrop photo of a well cemented portion of Facies A3…………………… 58 4.10 a Outcrop photo of oncoids within Facies A3……………………………….. 60 b Photo of a carbonate coated extraformational chert clast (oncoid)……….. 60 4.11 Paleocurrent map for Facies A3 and B4……………………………………... 61 4.12 a Ternary diagram of QmFL compositions…………………………………. 64 b Ternary diagram showing variations in lithic grain proportions………….. 64 4.13 a Outcrop photo of a highly indurated, silica-cemented area of Facies B1…. 66 b Slabbed sample from a highly indurated, silica-cemented area of Facies B1. 66 4.14 a Multiple generations of fracture-filling silica cements……………………. 67 b Multiple generations of fracture-filling silica cements……………………. 67 4.15 a GS-fabric silcrete………………………………………………………….. 69 b F-fabric silcrete……………………………………………………………. 69 4.16 a Outcrop photo of Facies B3……………………………………………….. 72 b Outcrop photo of Facies B3……………………………………………….. 72 4.17 a Outcrop photo of a conglomerate at the base of Facies B3………………... 74 b Outcrop photo of jasper within an intraformational carbonate clast……… 74 4.18 Paleocurrent map for Facies B3……………………………………………... 76 4.19 a Outcrop photo of Facies D2……………………………………………….. 83 b Outcrop photo of a centimeter-scale laminar calcic horizon……………… 83 9 Figure Page 4.20 Isopach map of the Lower Carbonate……………………………………….. 86 4.21 a Outcrop photo of the Lower Carbonate…………………………………… 87 b Outcrop photo of the Lower Carbonate…………………………………… 87 4.22 a Outcrop photo of desiccation breccia……………………………………… 90 b Outcrop photo of desiccation breccia……………………………………… 90 4.23 a Outcrop photo of fault breccia…………………………………………….. 91 b Photo of a slabbed sample of fault breccia………………………………… 91 4.24 a Outcrop photo of a jasper-filled vugs……………………………………… 93 b Close-up photo of a jasper-filled vugs…………………………………….. 93 4.25 a Outcrop photo of a chert-filled vug………………………………………... 94 b Outcrop photo of isopachous jasper cement………………………………. 94 4.26 Outcrop photo of a massive jasper accumulation…………………………… 95 4.27 Outcrop photo of a laminar jasper horizon………………………………….. 95 4.28 a Ostracodes within the Lower Carbonate…………………………………... 96 b Ostracodes within the Lower Carbonate…………………………………... 96 4.29 Map of pedogenic features within
Recommended publications
  • A New Microvertebrate Assemblage from the Mussentuchit
    A new microvertebrate assemblage from the Mussentuchit Member, Cedar Mountain Formation: insights into the paleobiodiversity and paleobiogeography of early Late Cretaceous ecosystems in western North America Haviv M. Avrahami1,2,3, Terry A. Gates1, Andrew B. Heckert3, Peter J. Makovicky4 and Lindsay E. Zanno1,2 1 Department of Biological Sciences, North Carolina State University, Raleigh, NC, USA 2 North Carolina Museum of Natural Sciences, Raleigh, NC, USA 3 Department of Geological and Environmental Sciences, Appalachian State University, Boone, NC, USA 4 Field Museum of Natural History, Chicago, IL, USA ABSTRACT The vertebrate fauna of the Late Cretaceous Mussentuchit Member of the Cedar Mountain Formation has been studied for nearly three decades, yet the fossil-rich unit continues to produce new information about life in western North America approximately 97 million years ago. Here we report on the composition of the Cliffs of Insanity (COI) microvertebrate locality, a newly sampled site containing perhaps one of the densest concentrations of microvertebrate fossils yet discovered in the Mussentuchit Member. The COI locality preserves osteichthyan, lissamphibian, testudinatan, mesoeucrocodylian, dinosaurian, metatherian, and trace fossil remains and is among the most taxonomically rich microvertebrate localities in the Mussentuchit Submitted 30 May 2018 fi fi Accepted 8 October 2018 Member. To better re ne taxonomic identi cations of isolated theropod dinosaur Published 16 November 2018 teeth, we used quantitative analyses of taxonomically comprehensive databases of Corresponding authors theropod tooth measurements, adding new data on theropod tooth morphodiversity in Haviv M. Avrahami, this poorly understood interval. We further provide the first descriptions of [email protected] tyrannosauroid premaxillary teeth and document the earliest North American record of Lindsay E.
    [Show full text]
  • Mongolian Geoscientist 50 (2020) 2-10
    Yun, Mongolian Geoscientist 50 (2020) 2-10 https://doi.org/10.5564/mgs.v50i0.1325 Mongolian Geoscientist Original article A Carcharodontosaurid tooth from the Hasandong Formation (Lower Cretaceous) of South Korea Chan-gyu Yun1,2* 1Vertebrate Paleontological Institute of Incheon, Incheon 21974, Republic of Korea 2Biological Sciences, Inha University, Incheon 22212, Republic of Korea *Corresponding author: [email protected] ARTICLE INFO ABSTRACT Article history: A large tooth of theropod dinosaur that was recovered from the Hasandong Received 04 April, 2020 Formation (Lower Cretaceous; Aptian-Albian) in Daedo island, Hadong Couty, South Gyeongsang Province of South Korea is redescribed. Although the tooth was Accepted 12 May, 2020 misidentified as a "Prodeinodon"-like megalosaurid theropod at the first time, detailed comparisons with known theropod dentition anatomy strongly indicate that this tooth belongs to an Acrocanthosaurus-like basal carcharodontosaurid theropod. This referral is supported by its combination of large size, ovoid-shaped cervix outline, mesial carina that does not reach the cervix, labially displaced distal carina and large number of denticles. This tooth is different from other carcharodontosaurid teeth from the same formation in several anatomical aspects (e.g., smaller overall size, presence of transverse lines adjacent to the distal carina, presence of interdenticular sulci in distal carina, denticle densities, crown basal ratio), indicating that carcharodontosaurid diversity in the Early Cretaceous of Korea could have been higher, although these differences may represent positional or individual variations. The presence of Acrocanthosaurus-like theropod teeth (e.g., "Prodeinodon", "Wakinosaurus") from early Cretaceous deposits (Valanginian-Cenomanian) of South Korea, Japan, Mongolia and China indicates that North American Acrocanthosaurus atokensis possibly represents a form that immigrated from the Asia.
    [Show full text]
  • Small Pterosaur Tracks in the Jinju Formation (Early Cretaceous), Gyeongsang Basin, South Korea: Abundance of Tiny Pterosaur Tracks in the East Asia
    Geophysical Research Abstracts Vol. 21, EGU2019-3245, 2019 EGU General Assembly 2019 © Author(s) 2019. CC Attribution 4.0 license. Small pterosaur tracks in the Jinju Formation (Early Cretaceous), Gyeongsang Basin, South Korea: abundance of tiny pterosaur tracks in the East Asia Sujin Ha (1), Kyung Soo Kim (2), Jong Deock Lim (3), and Hyoun Soo Lim (1) (1) Department of Geological Sciences, Pusan National University, Busan 46241, South Korea, (2) Department of Science Education, Chinju National University of Education, Jinju, Gyeongnam 52673, South Korea, (3) Cultural Heritage Administration, Daejeon 35208, South Korea So far, many vertebrate footprints (avian, nonavian dinosaur, pterosaur, crocodilian and mammal tracks) have been found in the Early Cretaceous Jinju Formation, Gyeongsang Basin, South Korea, and Jinju Innovation City is one of the most outstanding tracksite. Particularly noteworthy is that pterosaur tracks are commonly found in this area, although pterosaur tracks are generally rare compared to dinosaur tracks in other areas. Besides, the pterosaur tracks in this site vary widely in their morphology, size, and degree of preservation. Here we report new pterosaur tracks and trackway which are very small and well-preserved among various pterosaur tracks. Manus imprints have average values of 27.8 mm long, 9.0 mm wide, and 3.2 length/width ra- tio. Pes prints show average values of 27.7 mm long, 13.2 mm wide, and 2.1 length/width ratio. Small-sized (< 5 cm) footprints of pterosaur are rarely occurred around the world. At present, only four ichnospecies reported in the East Asia and Europe are valid: Pteraichnus koreanensis (Hasandong Formation, Korea), P.
    [Show full text]
  • Pterosaur Distribution in Time and Space: an Atlas 61
    Zitteliana An International Journal of Palaeontology and Geobiology Series B/Reihe B Abhandlungen der Bayerischen Staatssammlung für Pa lä on to lo gie und Geologie B28 DAVID W. E. HONE & ERIC BUFFETAUT (Eds) Flugsaurier: pterosaur papers in honour of Peter Wellnhofer CONTENTS/INHALT Dedication 3 PETER WELLNHOFER A short history of pterosaur research 7 KEVIN PADIAN Were pterosaur ancestors bipedal or quadrupedal?: Morphometric, functional, and phylogenetic considerations 21 DAVID W. E. HONE & MICHAEL J. BENTON Contrasting supertree and total-evidence methods: the origin of the pterosaurs 35 PAUL M. BARRETT, RICHARD J. BUTLER, NICHOLAS P. EDWARDS & ANDREW R. MILNER Pterosaur distribution in time and space: an atlas 61 LORNA STEEL The palaeohistology of pterosaur bone: an overview 109 S. CHRISTOPHER BENNETT Morphological evolution of the wing of pterosaurs: myology and function 127 MARK P. WITTON A new approach to determining pterosaur body mass and its implications for pterosaur fl ight 143 MICHAEL B. HABIB Comparative evidence for quadrupedal launch in pterosaurs 159 ROSS A. ELGIN, CARLOS A. GRAU, COLIN PALMER, DAVID W. E. HONE, DOUGLAS GREENWELL & MICHAEL J. BENTON Aerodynamic characters of the cranial crest in Pteranodon 167 DAVID M. MARTILL & MARK P. WITTON Catastrophic failure in a pterosaur skull from the Cretaceous Santana Formation of Brazil 175 MARTIN LOCKLEY, JERALD D. HARRIS & LAURA MITCHELL A global overview of pterosaur ichnology: tracksite distribution in space and time 185 DAVID M. UNWIN & D. CHARLES DEEMING Pterosaur eggshell structure and its implications for pterosaur reproductive biology 199 DAVID M. MARTILL, MARK P. WITTON & ANDREW GALE Possible azhdarchoid pterosaur remains from the Coniacian (Late Cretaceous) of England 209 TAISSA RODRIGUES & ALEXANDER W.
    [Show full text]
  • Oil and Gas Plays Ute Moutnain Ute Reservation, Colorado and New Mexico
    Ute Mountain Ute Indian Reservation Cortez R18W Karle Key Xu R17W T General Setting Mine Xu Xcu 36 Can y on N Xcu McElmo WIND RIVER 32 INDIAN MABEL The Ute Mountain Ute Reservation is located in the northwest RESERVATION MOUNTAIN FT HALL IND RES Little Moude Mine Xcu T N ern portion of New Mexico and the southwestern corner of Colorado UTE PEAK 35 N R16W (Fig. UM-1). The reservation consists of 553,008 acres in Montezu BLACK 666 T W Y O M I N G MOUNTAIN 35 R20W SLEEPING UTE MOUNTAIN N ma and La Plata Counties, Colorado, and San Juan County, New R19W Coche T Mexico. All of these lands belong to the tribe but are held in trust by NORTHWESTERN 34 SHOSHONI HERMANO the U.S. Government. Individually owned lands, or allotments, are IND RES Desert Canyon PEAK N MESA VERDE R14W NATIONAL GREAT SALT LAKE W Marble SENTINEL located at Allen Canyon and White Mesa, San Juan County, Utah, Wash Towaoc PARK PEAK T and cover 8,499 acres. Tribal lands held in trust within this area cov Towaoc River M E S A 33 1/2 N er 3,597 acres. An additional forty acres are defined as U.S. Govern THE MOUND R15W SKULL VALLEY ment lands in San Juan County, Utah, and are utilized for school pur TEXAS PACIFIC 6-INCH OIL PIPELINE IND RES UNITAH AND OURAY INDIAN RESERVATION Navajo poses. W Ramona GOSHUTE 789 The Allen Canyon allotments are located twelve miles west of IND RES T UTAH 33 Blanding, Utah, and adjacent to the Manti-La Sal National Forest.
    [Show full text]
  • A Fossil Locality Predictive Model for the Early Cretaceous Cedar Mountain Formation, Utah, Usa
    A FOSSIL LOCALITY PREDICTIVE MODEL FOR THE EARLY CRETACEOUS CEDAR MOUNTAIN FORMATION, UTAH, USA A THESIS PRESENTED TO THE DEPARTMENT OF HUMANITIES AND SOCIAL SCIENCE IN CANDIDACY FOR THE DEGREE OF MASTER OF SCIENCE By DANIEL BURK NORTHWEST MISSOURI STATE UNIVERSITY MARYVILLE, MISSOURI OCTOBER, 2014 FOSSIL LOCALITY PREDICTIVE MODEL A Fossil Locality Predictive Model for the Early Cretaceous Cedar Mountain Formation, Utah, USA Daniel Burk Northwest Missouri State University THESIS APPROVED Thesis Advisor, Dr. Yi-Hwa Wu Date Dr. Ming-Chih Hung Date Dr. John P. Pope Date Dean of Graduate School Date A Fossil Locality Predictive Model for the Early Cretaceous Cedar Mountain Formation, Utah, USA Abstract Hard work and chance are nearly always among the deciding factors in finding new, important, and productive paleontological localities. Fossil locality predictive models have the potential to reduce unproductive field time and maximize hard work thus increasing the chances researchers have to find important localities. This study uses remotely sensed data to design and test a fossil locality predictive model for the Early Cretaceous Cedar Mountain Formation. Landsat 8 OLI/TIRS data from known localities were summarized, reclassified and used in a weighted suitability analysis to categorize fossil locality potential of the study area. Field work was conducted to test model functionality. Field observations were used to refine the weighted suitability analysis. Landsat 8 OLI/TIRS data alone offers a less accurate prescription of fossil locality potential. Additional physical and environmental factors play a role in determining the chance of finding fossils. Slope degree and aspect data from known localities were summarized and analyzed to further refine the model.
    [Show full text]
  • Dinosaur Track-Bearing Deposits of the Cretaceous Gyeongsang Su- Pergroup, Korea: Stratigraphic Occurrences and Paleoecological Implications
    Hallesches Jahrbuch für Geowissenschaften, Beiheft 46 (2019) 77 Dinosaur track-bearing deposits of the Cretaceous Gyeongsang Su- pergroup, Korea: Stratigraphic occurrences and paleoecological implications IN SUNG PAIK1* & HYUN JOO KIM1 1 Department of Earth and Environmental Sciences, Pukyong National University, Address, 83516 Busan, Korea *presenting author, [email protected] Abstract: Dinosaur track-bearing deposits are common in the Cretaceous Gyeongsang Supergroup (Hauteri-vi- an to Maastrichtian) (Fig. 1), Korea. The Gyeongsang Supergroup consists of alluvial fan, fluvial plain, and lacustrine deposits and is composed of a variety of siliciclastic and tuffaceous rocks, some car- bonates and evaporites. The dinosaur track-bearing deposits of the Gyeongsang Supergroup show variation in stratigraphic occurrences. Whereas dinosaur bone fossils occur in the lowermost Nak- dong Formation (alluvial fan with some ponds) and are common in the overlying Hasandong For- mation (fluvial with some lakes), dinosaur tracks are absent in the Nakdong Formation and scarcely present in the Hasandong Formation. Body fossils of dinosaurs are very rare throughout the Gyeo- ngsang Supergroup except the Hasandong Formation, however, dinosaur tracks are common in the upper part of the Jinju Formation (lacustrine), the Haman Formation (alluvial plain with some ponds) and the Jindong Formation (alluvial plain and playa lakes). It is unusual that dinosaur tracks are ab- sent in the Chilgok Formation overlying the Jinju Formation in spite of its similar depositional setting to that of the Haman Foramtion. In the pyroclastic deposit-dominated Yucheon Group (the upper- most Group) overlying the Jindong Formation dinosaur tracks are very rare. In summary the occur- rences of dinosaur tracks in the Gyeongsang Supergroup shows the recurrent pattern of increase and decrease in abundance and a preferred occurrence in lake-related deposits rather than in alluvial fan and fluvial sediments.
    [Show full text]
  • A Jurassic Basal Eusauropod Clade from Iberia Finds Refuge In
    View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by UCL Discovery Descendants of the Jurassic turiasaurs from Iberia found refuge in the Early Cretaceous of western USA Rafael Royo-Torres, Paul Upchurch, James I. Kirkland, Donald D. DeBlieux, John R. Foster, Alberto Cobos, Luis Alcalá Supplementary Information: I. Abbreviations section II. Geological setting of the Doelling’s Bowl bonebed III. Phylogenetic analyses and list of synapomorphies IV. Holotype of Mierasaurus V. Measurements VI. References I. Abbreviations section BYU (Museum of Paleontology of Brigham Young University, Provo, Utah USA). DBBB Doelling’s Bowl bonebed; DBGI Doelling’s Bowl site; J-K Jurassic- Cretaceous transition; Ma million years ago; My million years; MPT most parsimonious trees; RD name for every dinosaur site from Riodeva in Teruel (Spain); TL Tree length; UMNH the Natural History Museum of Utah (USA); UGS Utah Geological Survey (USA). Anatomical abbreviations: bt basal tubera; bo basioccipital; bpt basipterygoid process; ca crista antotica; ct crista tuberalis; f frontal; fme fenestra metotic; fv fenestra vestivuli (=fenestra ovalis); osc otosphenoidal crest (= crista prootica); p parietal; pa parapophysis; prf prefontal; stf supratemporal fossa; so supraoccipital; eo exoccipital- opisthotic; bo basioccipital; popr paraoccipital process; cranial nerves: I olfactory nerve; II optic nerve; III oculomotor nerve; IV trochlear nerve; V trigeminal nerve (ophthalmic, maxillary, mandibular); VI abductor or abducens nerve; VII facialis nerve; VIII vestibulocochlear nerve. Abbreviations for laminae vertebral: acpl anterior centroparapophyseal lamina; ant. spdl anterior spinodiapophyseal lamina; cprl 1 centroprezygapophyseal lamina; cpol centropostzygapophyseal lamina; pcdl posterior centrodiapophyseal lamina; post. spdl posterior spinodiapophyseal lamina; ppdl paradiapophyseal lamina; prdl prezygodiapophyseal lamina; spol spinopostzygapophyseal lamina.
    [Show full text]
  • The End of the Sauropod Dinosaur Hiatus in North America
    Palaeogeography, Palaeoclimatology, Palaeoecology 297 (2010) 486–490 Contents lists available at ScienceDirect Palaeogeography, Palaeoclimatology, Palaeoecology journal homepage: www.elsevier.com/locate/palaeo The end of the sauropod dinosaur hiatus in North America Michael D. D'Emic a,⁎, Jeffrey A. Wilson a, Richard Thompson b a Museum of Paleontology and Department of Geological Sciences, University of Michigan, 1109 Geddes Avenue, Ann Arbor, MI 48109–1079, USA b Department of Geosciences, University of Arizona, 1040 E 4th St, Tucson, AZ, 85721-0077, USA article info abstract Article history: Sauropod dinosaurs reached their acme in abundance and diversity in North America during the Late Received 4 February 2010 Jurassic. Persisting in lesser numbers into the Early Cretaceous, sauropods disappeared from the North Received in revised form 16 August 2010 American fossil record from the Cenomanian until the Campanian or Maastrichtian stage of the Late Accepted 30 August 2010 Cretaceous. This ca. 25–30 million-year long sauropod hiatus has been attributed to either a true extinction, Available online 19 September 2010 perhaps due to competition with ornithischian dinosaurs, or a false extinction, due to non-preservation of sediments bearing sauropods. The duration of the sauropod hiatus remains in question due to uncertainty in Keywords: fi Dinosaur the ages and af nities of the specimens bounding the observed gap. In this paper, we re-examine the Sauropod phylogenetic affinity of materials from Campanian-aged sediments of Adobe Canyon, Arizona that currently Titanosaur mark the end of the sauropod hiatus. Based on the original description of those remains and new specimens Alamosaurus from the same formation, we conclude that the Adobe Canyon vertebrae do not pertain to titanosaurs, but to Hadrosaur hadrosaurid dinosaurs.
    [Show full text]
  • A New Ornithischian–Dominated and Theropod Footprint Assemblage from the Lower Jurassic Lufeng Formation of Yunnan Province, China
    Sullivan, R.M. and Lucas, S.G., eds., 2016, Fossil Record 5. New Mexico Museum of Natural History and Science Bulletin 74. 331 A NEW ORNITHISCHIAN–DOMINATED AND THEROPOD FOOTPRINT ASSEMBLAGE FROM THE LOWER JURASSIC LUFENG FORMATION OF YUNNAN PROVINCE, CHINA LIDA XING1, MARTIN G. LOCKLEY2, HENDRIK KLEIN3, JIANPING ZHANG1, and W. SCOTT PERSONS IV4 1School of the Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China; -email: [email protected]; 2Dinosaur Tracks Museum, University of Colorado Denver, P.O. Box 173364, Denver, CO 80217; 3Saurierwelt Paläontologisches Museum Alte Richt 7, D-92318 Neumarkt, Germany; 4Department of Biological Sciences, University of Alberta, 11455 Saskatchewan Drive, Edmonton, Alberta T6G 2E9, Canada Abstract—Ornithischian- and theropod-dominated footprint assemblages from the Lower Jurassic Lufeng Formation of Yunnan Province, China, differ significantly from the skeletal record of the same region. Ornithischian tracks assigned to Shenmuichnus wangi are the most common track type (52%), while small Anomoepus-type tracks account for 31%. Large Eubrontes-like theropod tracks make up about 17% of the assemblage. The track record of the Lufeng Basin currently lacks evidence corresponding to basal sauropodomorphs and basal sauropods, even though they are the most abundant skeletal fossils. INTRODUCTION Diplocraterion belongs to the Skolithos ichnofacies, which is The Lufeng Basin of China contains many wide exposures of mainly preserved in high energy, shallow marine substrates (Cornish, Mesozoic continental red beds rich in dinosaur and other vertebrate 1986; Šimo and Olšavský, 2007). In southern Sweden, Diplocraterion fossils, making the Lufeng Basin among the most famous dinosaur field is also associated with some Early Jurassic tracks (Gierliński and research sites in the world (Dong, 1992; Luo and Wu, 1995).
    [Show full text]
  • DINOSAURS Contents the Director’S Perspective the Thumb-Spiked Iguanodontians—Dinosaurian Cows of the Early Cretaceous
    UTAH GEOLOGICAL SURVEY SURVEY NOTES Volume 45, Number 1 January 2013 UTAH'S NEW IGUANODONTIAN DINOSAURS Contents The Director’s Perspective The Thumb-Spiked Iguanodontians—Dinosaurian Cows of the Early Cretaceous ...........................1 Each year, the Utah Geological Survey of proven reserves Using Aquifers for Water Storage provides two chapters for the “Economic (barrels) to annual in Cache Valley ................................................ 4 Report to the Governor,” which is pub- oil production (bar- Establishing Baseline Water Quality in the lished by the Governor’s Office of Man- rels per year) has Southeastern Uinta Basin ............................. 6 agement and Budget in January. The two increased from GeoSights ............................................................. 8 chapters address energy and mineral typically 6 to 8 Glad You Asked .................................................... 9 industry trends in Utah during the past years of supply Energy News .......................................................10 year. The UGS also summarizes Utah’s prior to 2000, to Teacher’s Corner ................................................ 12 extractive resource industry trends in 18 years over the Survey News .......................................................13 an annual publication (recently pub- past three years. lished UGS Circular 115 summarizes 2011 In addition, annual New Publications ................................................13 trends). A key indicator we use to mea- oil production has sure the overall
    [Show full text]
  • ¿Saurópodos Asiáticos En El Barremiense Inferior (Cretácico Inferior) De España?
    AMEGHINIANA (Rev. Asoc. Paleontol. Argent.) - 39 (4): 443-452. Buenos Aires, 30-12-2002 ISSN0002-7014 ¿Saurópodos asiáticos en el Barremiense inferior (Cretácico Inferior) de España? José Ignacio CANUDO1, José Ignacio RUIZ-OMEÑACA1,2José Luis BARCO 1,2 y Rafael ROYO TORRES 1,3 Abstract.ASIANSAUROPODSINTHELOWERBARREMIAN(LOWERCRETACEOUS) OFSPAIN?We describe here three sauropod teeth from the Lower Cretaceous (lower Barremian) of La Cantalera (Josa, Teruel, Spain). The te- eth are spoon-shaped with a lingual cingulum-like structure. The general morphology is closer to Camarasauridae, but the presence of cingular structure indicates a different group, more derived that this family. The problematic genus Euhelopusfrom the Upper Jurassic or Lower Cretaceous of China and some isolated teeth from the Lower Cretaceous of China, Russia and Mongolia are the only sauropods with si- milar teeth. We suggest the presence of a sauropod group in Asian and European Lower Cretaceous. This group is included in the family Euhelopodidae and the Titanosauriformes clade. This European - Asian Lower Cretaceous geographic connection has been previously observed with mammals and ornithopod dinosaurs. Resumen. Se describen tres dientes de dinosaurios saurópodos recogidos en el Cretácico Inferior (Barremiense inferior) del yacimiento de La Cantalera (Josa, Teruel , España). Los dientes tienen forma de cuchara con una estructura cingular en el lado lingual. La morfología general es parecida a las de Camarasauridae, pero la presencia de la estructura cingular nos indica un grupo más derivado que esta familia. El problemático género Euhelopusdel Jurásico superior o Cretácico inferior de China y algunos dientes aislados del Cretácico inferior de China, Rusia y Mongolia son los únicos saurópodos con esta es- tructura cingular.
    [Show full text]