Open-File Report Y 1969

Total Page:16

File Type:pdf, Size:1020Kb

Open-File Report Y 1969 UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY CRETACEOUS SEDIMENTATION AND TSCTONISM IN THE SOUTHEASTERN KAIPAROWI1S REGION, UTAH By Fred Peterson Open-file Report _ y 1969 This report is preliraiuary a-..-.u has not been edited or re­ viewed for conformity with U.S. Geological Survey standards and nomenclature. CONTENTS Page Abstract Introduction ------- ------------------ -- --------__-----_---_-. 3 Geography-- --- - --- ------ ----- ------- ---------- 3 Previous work --- ----------- - ----- -_-_ - -- ----- 5 Present investigations --- -- ------- ------- -- 5 Acknowledgments-------------------- ---------------- --------- 6 Methods of study- ------------- --- ------ -_------_--_-_--_-_- 7 Organization------ - ----------- -- --- ------- ------- __--- H Upper Cretaceous formations ---------------------------------------- 12 Dakota Formation------------------------------------------------ 14 Lower member-------------- - ------- ------------------- 15 Middle member---------------------------------------------- 22 Upper member ---------------- -_-____- __-___-_______--.. ?8 Tropic Shale---------------------------------------------------- 34 Straight Cliffs Formation------------------ ------------------- 49 Tibfaet Canyon Member-------------------- ------------------- 49 Smoky Ho 1 lev Member - --------------------------------------- 56 Unconformity---------------- ------------------------------- 60 John Henry Member- ----------------------------------------- 61 Barren zones---------------------------- -------------- 62 Coal zones---- -------------------------------------- 66 Key sandstone beds------------ ------------------------ 71 Marine mudstone tongues------------------------------- 77 General------------------------------------------------ 81 Drip Tank Member ----------------------------------------- 84 Wahweap Formation----------------------------------------------- 88 Formations in northwestern Kaiparowits region------------------- 95 Sedimentary facies ------------------------------------------- ------ 96 Piedmont facies---- ------------ - -----_--_--_----____ ._-» 97 Alluvial plain facies - - -- ---------- ---- ._._ 99. Subdivision A------ --- ------- -----_--_--_---.. 99 Subdivision B--------- -- -------------- _----_-_---___- 103 Subdivision C---------------- ------ __-----__-----_.-« Deltaic plain facies---- ---- - ._._-_ .-_ _-_ Lagoonal-paludal facies-- --------- ------- -_-_ - -_ 125 Barrier sandstone facies ----- --- -- - -- ----- * ----- 132 Offshore marine facies--- - ----- ---- ------- - ------ 141 Distant marine facies------- -- ----------- ---_----_-----_-. 144 CONTENTS Sedimentary facies continued Distribution of facies---- --------------- --- -_-_ ____ Dakota Formation------- - -- ----- - -_ Tropic Shale - --- ----- ------ ---_ -_-__--« ^47 Straight Cliffs Formation -- - ----------- -.--__ ^47 Wahweap Formation ----------------------------------- --- 151 Formations in northwestern Kaiparowits region ------------ 153 Sedimentation and tectonism ---------- ---_-___-.--- -____--__-__ General setting --------- -.....--. ----- -.._-------_-_--- Late Jurassic time---------------------------------------------- 155 Early Cretaceous time---- ------- ------------- ---___-_-_-._ 155 Cenoman ian t irne ------------------ ----------------------------- ^57 Early and middle Turonian time------------------------- --------- 170 Late Turonian to middle Coniacian tine-- --- ----------------- 182 Late Coniacian to earliest Campanian time----------------------- 183 C amp an i an t ime -------------------------------------------------- 198 Maestrichtian and Paleocene time-------------------------------- 206 .Middle and late Cenozoic time---- ---- -- ___---__---__---_-_ 208 General-- ----------------------------------------------------- 210 Economic resources-- ----------------------------------------------- 214 Coal-- .--------.- .--_._-._ __--..---------.__-_ . 214 Dakota Formation--------------------------------- -------- 214 Smoky Hollow Member of Straight Cliffs Formation-------- - 214 John Henry Member of Straight Cliffs Formation------------- 215 Lower coal zone--------------------------------------- 215 Christensen coal zone---- --------------------------- 216 Rees coal zone-------------- ----- --_-__--_- 216 Alvey coal zone -------------------- -_-_---_-__---. 216 Analyses and quality--------------------------------------- 216 Cleats--- ---------------- -- ----.-----_-_----__ 219 Potential resources and production------------------------- 219 Oil and gas exploration--------- -------- --- -_---------_-__ 222 Ground water- --------------------------------- __------_---. 223 Black sandstone deposits---- ---- -- ---- --------- - 223 References cited--------------------------------------------------- 224 Appendix--------- -- ------------- ------- _-_-__-----_ __-_-. 235 Fossil localities -- -- --- ---- ------ -_-__-_-_-__.-_ 235 ILLUSTRATIONS Page Plate 1. Geologic map of southeastern Kaiparowits region ------ in pocket 2. Diagram showing mineralogy of sandstones in Dakota Formation--- - - - -- -- - - " 3. Isopach map of lower and middle members of Dakota Formation- " 4. Fence diagram of Dakota Formation in southeastern Kaiparowits region -- ------------------------------- tf 5. Map shox/ing cross-stratification azimuths for fluvial sandstones in Dakota Formation-- --------_--_-_---.--_ * 6-11. Measured sections of: 6. Dakota Formation in southwestern part of southeastern Kaiparowits region--------------- ------------------ " 7. Dakota Formation in central part of southeastern Kaiparowits region-- ------ ----------------------- " 8. Dakota Formation in northeastern part of southeastern Kaiparowits region----------------------------------- " 9. Straight Cliffs Formation in southwestern part of southeastern Kaiparowits region---------------------- " 10. Straight Cliffs Formation in northeastern part of southeastern Kaiparowits region--- ----------------- " .-.- 11. Straight Cliffs Formation in northwestern and eastern parts of southeastern Kaiparowits region------------- " 12. Diagram showing mineralogy of sandstones in Straight Cliffs Formation, southwestern and central parts of southeastern Kaiparowits region- ----------------------- " 13. Diagram showing mineralogy of sandstones in Straight Cliffs Formation, eastern part of southeastern Kaiparo­ wits region-------------- ------------------ ----- . ' 14. Map showing distribution of coal and muds tone in middle member of Dakota Formation below bentonite marker bed---- " 15. Map showing distribution of coal and mudstone in middle member of Dakota Formation between bentonite marker bed and coal bed No. 4----- ----------- ---- --- ------ » 16. Map showing distribution of coal and partings in coal bed No. 4, middle member of Dakota Formation---- --------- " 17. Diagram of distribution of coal in Smoky Hollow Member of Straight Cliffs Formation- -- - -- ----- ----- « iii ILLUSTRATIONS Plates 18-21. Isopach maps of: 18. Total coal in lower coal zone of John Henry Member----------------------------------- ---- In pocket 19. Total coal in Christensen coal zone of John Henry Member----------------------- ------- -- " 20. Total coal in Rees coal zone of John Henry Member------------------ --------------- 21. John Henry Member of Straight Cliffs Formation--- " Figure 1. Index map--------------------------------------------- -- 4 2. Diagram showing classification of sandstones-------------- 9 3. Photograph showing Dakota Formation in southwestern part of region---- --------- _---_--__-_ --.__---___-____. 15 4. Photograph showing Dakota Formation in central part of region----------- ------ ----- __---------_---------_ ]_y 5. Photograph showing Dakota Formation in northeastern pare of region----------------------------------------------- 18 6. Stratigraphic section showing southwestward regional beveling of Jurassic formations and upiifu of ancestral Cedar Mountain anticline prior to deposition of Dakota Formation--------- ------------------------------------ 21 7. Measured sections showing relations of members and units in Dakota Formation------------------------------------- 26 8. Correlation of Cretaceous formations in Kaiparowits region, Utah, and Black Mesa region, Arizona------------ 35 9. Correlation of Cretaceous formations in Kaiparowits region, Utah, and San Juan Basin, N. Mex---------------- 36 10. Photograph showing Tropic Shale about 1 mile west of Warm Creek--------- --- ------------------------- 37 11. Photograph showing texture on weathered surface of Tropic Shale 38 12. Diagram showing mineralogy of Tropic Shale at measured section Tl------ --- --- ---------------------- 40 13. Selected measured sections of Tropic Shale and parts of Dakota and Straight Cliffs Formations showing thickness changes over ancestral folds--- ----------------------- 43 14. Photograph showing Straight Cliffs Formation in south­ western part of region in Warm Creek canyon----------- 50 15. Photograph showing Straight Cliffs Formation at east end of Kaiparowits Plateau above Fiftymile Point - - -- 51 ILLUSTRATIONS Page Figure 16. Diagram showing relations of members and units in Straight Cliffs Formation------------- --- -- - 54 17. Photograph showing black sandstone bed at top of B sand­ stone bed in John Henry Member of Straight Cliffs Formation --------------- --------- -- _--__--_--_- 74 18. Photograph showing basal conglomerate of John Henry Member--- -------- -------- ..-_-_-.--_-_- -- -- 79 19. Photograph showing Wahweap Formation on northeast side of Drip Tank Canyon-----------------
Recommended publications
  • Stratigraphy and Paleontology of Mid-Cretaceous Rocks in Minnesota and Contiguous Areas
    Stratigraphy and Paleontology of Mid-Cretaceous Rocks in Minnesota and Contiguous Areas GEOLOGICAL SURVEY PROFESSIONAL PAPER 1253 Stratigraphy and Paleontology of Mid-Cretaceous Rocks in Minnesota and Contiguous Areas By WILLIAM A. COBBAN and E. A. MEREWETHER Molluscan Fossil Record from the Northeastern Part of the Upper Cretaceous Seaway, Western Interior By WILLIAM A. COBBAN Lower Upper Cretaceous Strata in Minnesota and Adjacent Areas-Time-Stratigraphic Correlations. and Structural Attitudes By E. A. M EREWETHER GEOLOGICAL SURVEY PROFESSIONAL PAPER 1 2 53 UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON 1983 UNITED STATES DEPARTMENT OF THE INTERIOR JAMES G. WATT, Secretary GEOLOGICAL SURVEY Dallas L. Peck, Director Library of Congress Cataloging in Publication Data Cobban, William Aubrey, 1916 Stratigraphy and paleontology of mid-Cretaceous rocks in Minnesota and contiguous areas. (Geological Survey Professional Paper 1253) Bibliography: 52 p. Supt. of Docs. no.: I 19.16 A. Molluscan fossil record from the northeastern part of the Upper Cretaceous seaway, Western Interior by William A. Cobban. B. Lower Upper Cretaceous strata in Minnesota and adjacent areas-time-stratigraphic correlations and structural attitudes by E. A. Merewether. I. Mollusks, Fossil-Middle West. 2. Geology, Stratigraphic-Cretaceous. 3. Geology-Middle West. 4. Paleontology-Cretaceous. 5. Paleontology-Middle West. I. Merewether, E. A. (Edward Allen), 1930. II. Title. III. Series. QE687.C6 551.7'7'09776 81--607803 AACR2 For sale by the Distribution Branch, U.S.
    [Show full text]
  • High-Resolution Correlation of the Upper Cretaceous Stratigraphy Between the Book Cliffs and the Western Henry Mountains Syncline, Utah, U.S.A
    University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Dissertations & Theses in Earth and Atmospheric Earth and Atmospheric Sciences, Department of Sciences 5-2012 HIGH-RESOLUTION CORRELATION OF THE UPPER CRETACEOUS STRATIGRAPHY BETWEEN THE BOOK CLIFFS AND THE WESTERN HENRY MOUNTAINS SYNCLINE, UTAH, U.S.A. Drew L. Seymour University of Nebraska, [email protected] Follow this and additional works at: http://digitalcommons.unl.edu/geoscidiss Part of the Geology Commons, Sedimentology Commons, and the Stratigraphy Commons Seymour, Drew L., "HIGH-RESOLUTION CORRELATION OF THE UPPER CRETACEOUS STRATIGRAPHY BETWEEN THE BOOK CLIFFS AND THE WESTERN HENRY MOUNTAINS SYNCLINE, UTAH, U.S.A." (2012). Dissertations & Theses in Earth and Atmospheric Sciences. 88. http://digitalcommons.unl.edu/geoscidiss/88 This Article is brought to you for free and open access by the Earth and Atmospheric Sciences, Department of at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Dissertations & Theses in Earth and Atmospheric Sciences by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. HIGH-RESOLUTION CORRELATION OF THE UPPER CRETACEOUS STRATIGRAPHY BETWEEN THE BOOK CLIFFS AND THE WESTERN HENRY MOUNTAINS SYNCLINE, UTAH, U.S.A. By Drew L. Seymour A THESIS Presented to the Faculty of The Graduate College at the University of Nebraska In Partial Fulfillment of Requirements For Degree of Master of Science Major: Earth and Atmospheric Sciences Under the Supervision of Professor Christopher R. Fielding Lincoln, NE May, 2012 HIGH-RESOLUTION CORRELATION OF THE UPPER CRETACEOUS STRATIGRAPHY BETWEEN THE BOOK CLIFFS AND THE WESTERN HENRY MOUNTAINS SYNCLINE, UTAH. U.S.A. Drew L. Seymour, M.S.
    [Show full text]
  • Hydrogeology and Stratigraphy of the Dakota Formation in Northwest Iowa
    WATER SUPPLY HYDROGEOLOGY AND J.A. MUNTER BULLETIN G.A. LUDVIGSON NUMBER 13 STRATIGRAPHY OF THE B.J. BUNKER 1983 DAKOTA FORMATION IN NORTHWEST IOWA Iowa Geological Survey Donald L. Koch State Geologist and Director 123 North Capitol Street Iowa City, Iowa 52242 IOWA GEOLOGICAL SURVEY WATER-SUPPLY BULLETIN NO. 13 1983 HYDROGEOLOGY AND STRATIGRAPHY OF THE DAKOTA FORMATION IN NORTHWEST IOWA J. A. Munter G. A. Ludvigson B. J. Bunker Iowa Geological Survey Iowa Geological Survey Donald L. Koch Director and State Geologist 123 North Capitol Street Iowa City, Iowa 52242 Foreword An assessment of the quantity and quality of water available from the Dakota (Sandstone) Formation 1n northwest Iowa is presented in this report. The as sessment was undertaken to provide quantitative information on the hydrology of the Dakota aquifer system to the Iowa Natural Resources Council for alloca tion of water for irrigation, largely as a consequence of the 1976-77 drought. Most area wells for domestic, livestock, and irrigation purposes only partial ly penetrated the Dakota Formation. Consequently, the long-term effects of significant increases in water withdrawals could not be assessed on the basis of existing wells. Acquisition of new data was based upon a drilling program designed to penetrate the entire sequence of Dakota sediments at key loca tions, after a thorough inventory and analysis of existing data. Definition of the distribution, thickness, and lateral and vertical changes in composition of the Dakota Formation has permitted the recognition of two mem bers. Additionally, Identification of the rock units that underlie the Dakota Formation has contributed greatly to our knowledge of the regional geology of northwest Iowa and the upper midwest.
    [Show full text]
  • The Wunstorf Drilling Project
    Progress Reports The Wunstorf Drilling Project: Coring a Global Stratigraphic Reference Section of the Oceanic Anoxic Event 2 by Jochen Erbacher, Jörg Mutterlose, Markus Wilmsen, Thomas Wonik, and the Wunstorf Drilling Scientific Party doi:10.0/iodp.sd..0.007 section. Disciplines involved include micropaleontology Introduction and Goals (calcareous nannofossils, planktonic foraminifera), macro- paleontology (ammonites, inoceramids), stable isotopes and The mid-Cretaceous greenhouse world (Albian–Turonian) cyclostratigraphy mainly based on borehole logging, multi was characterized by high atmospheric carbon dioxide sensor core logging���������������������������������������,�������������������������������������� and x-ray fluorescence (XRF) scanning levels, much higher global temperatures than at present�����,���� and data. The combination of geochemical, paleontological�����,���� and a lack of permanent ice caps at the poles (Bice et al., 2006; logging data will allow high resolution chemo- and biostra- Huber et al., 2002; Wilson et al., 2002). A characteristic tigraphy for the CTB�������������������������������������I������������������������������������ which may in ����������������������the future������������������ serve as an feature of this greenhouse world was the deposition of black international standard. shales during the Cenomanian / Turonian boundary interval (CTBI; Schlanger and Jenkyns, 1976; Arthur et al., 1990). The Wunstorf Core These carbon�����������������������������������������������-����������������������������������������������rich
    [Show full text]
  • Annotated Checklist of Fossil Fishes from the Smoky Hill Chalk of the Niobrara Chalk (Upper Cretaceous) in Kansas
    Lucas, S. G. and Sullivan, R.M., eds., 2006, Late Cretaceous vertebrates from the Western Interior. New Mexico Museum of Natural History and Science Bulletin 35. 193 ANNOTATED CHECKLIST OF FOSSIL FISHES FROM THE SMOKY HILL CHALK OF THE NIOBRARA CHALK (UPPER CRETACEOUS) IN KANSAS KENSHU SHIMADA1 AND CHRISTOPHER FIELITZ2 1Environmental Science Program and Department of Biological Sciences, DePaul University,2325 North Clifton Avenue, Chicago, Illinois 60614; and Sternberg Museum of Natural History, Fort Hays State University, 3000 Sternberg Drive, Hays, Kansas 67601;2Department of Biology, Emory & Henry College, P.O. Box 947, Emory, Virginia 24327 Abstract—The Smoky Hill Chalk Member of the Niobrara Chalk is an Upper Cretaceous marine deposit found in Kansas and adjacent states in North America. The rock, which was formed under the Western Interior Sea, has a long history of yielding spectacular fossil marine vertebrates, including fishes. Here, we present an annotated taxo- nomic list of fossil fishes (= non-tetrapod vertebrates) described from the Smoky Hill Chalk based on published records. Our study shows that there are a total of 643 referable paleoichthyological specimens from the Smoky Hill Chalk documented in literature of which 133 belong to chondrichthyans and 510 to osteichthyans. These 643 specimens support the occurrence of a minimum of 70 species, comprising at least 16 chondrichthyans and 54 osteichthyans. Of these 70 species, 44 are represented by type specimens from the Smoky Hill Chalk. However, it must be noted that the fossil record of Niobrara fishes shows evidence of preservation, collecting, and research biases, and that the paleofauna is a time-averaged assemblage over five million years of chalk deposition.
    [Show full text]
  • OFR21 a Guide to Fossil Sharks, Skates, and Rays from The
    STATE OF DELAWARE UNIVERSITY OF DELAWARE DELAWARE GEOLOGICAL SURVEY OPEN FILE REPORT No. 21 A GUIDE TO FOSSIL SHARKS J SKATES J AND RAYS FROM THE CHESAPEAKE ANU DELAWARE CANAL AREA) DELAWARE BY EDWARD M. LAUGINIGER AND EUGENE F. HARTSTEIN NEWARK) DELAWARE MAY 1983 Reprinted 6-95 FOREWORD The authors of this paper are serious avocational students of paleontology. We are pleased to present their work on vertebrate fossils found in Delaware, a subject that has not before been adequately investigated. Edward M. Lauginiger of Wilmington, Delaware teaches biology at Academy Park High School in Sharon Hill, Pennsyl­ vania. He is especially interested in fossils from the Cretaceous. Eugene F. Hartstein, also of Wilmington, is a chemical engineer with a particular interest in echinoderm and vertebrate fossils. Their combined efforts on this study total 13 years. They have pursued the subject in New Jersey, Maryland, and Texas as well as in Delaware. Both authors are members of the Mid-America Paleontology Society, the Delaware Valley Paleontology Society, and the Delaware Mineralogical Society. We believe that Messrs. Lauginiger and Hartstein have made a significant technical contribution that will be of interest to both professional and amateur paleontologists. Robert R. Jordan State Geologist A GUIDE TO FOSSIL SHARKS, SKATES, AND RAYS FROM THE CHESAPEAKE AND DELAWARE CANAL AREA, DELAWARE Edward M. Lauginiger and Eugene F. Hartstein INTRODUCTION In recent years there has been a renewed interest by both amateur and professional paleontologists in the rich upper Cretaceous exposures along the Chesapeake and Delaware Canal, Delaware (Fig. 1). Large quantities of fossil material, mostly clams, oysters, and snails have been collected as a result of this activity.
    [Show full text]
  • Order LAMNIFORMES ODONTASPIDIDAE Sand Tiger Sharks Iagnostic Characters: Large Sharks
    click for previous page Lamniformes: Odontaspididae 419 Order LAMNIFORMES ODONTASPIDIDAE Sand tiger sharks iagnostic characters: Large sharks. Head with 5 medium-sized gill slits, all in front of pectoral-fin bases, Dtheir upper ends not extending onto dorsal surface of head; eyes small or moderately large, with- out nictitating eyelids; no nasal barbels or nasoral grooves; snout conical or moderately depressed, not blade-like;mouth very long and angular, extending well behind eyes when jaws are not protruded;lower labial furrows present at mouth corners; anterior teeth enlarged, with long, narrow, sharp-edged but unserrated cusps and small basal cusplets (absent in young of at least 1 species), the upper anteriors separated from the laterals by a gap and tiny intermediate teeth; gill arches without rakers; spiracles present but very small. Two moderately large high dorsal fins, the first dorsal fin originating well in advance of the pelvic fins, the second dorsal fin as large as or somewhat smaller than the first dorsal fin;anal fin as large as second dorsal fin or slightly smaller; caudal fin short, asymmetrical, with a strong subterminal notch and a short but well marked ventral lobe. Caudal peduncle not depressed, without keels; a deep upper precaudal pit present but no lower pit. Intestinal valve of ring type, with turns closely packed like a stack of washers. Colour: grey or grey-brown to blackish above, blackish to light grey or white, with round or oval dark spots and blotches vari- ably present on 2 species. high dorsal fins upper precaudal eyes without pit present nictitating eyelids intestinal valve of ring type Habitat, biology, and fisheries: Wide-ranging, tropical to cool-temperate sharks, found inshore and down to moderate depths on the edge of the continental shelves and around some oceanic islands, and in the open ocean.
    [Show full text]
  • The Cretaceous System in Central Sierra County, New Mexico
    The Cretaceous System in central Sierra County, New Mexico Spencer G. Lucas, New Mexico Museum of Natural History, Albuquerque, NM 87104, [email protected] W. John Nelson, Illinois State Geological Survey, Champaign, IL 61820, [email protected] Karl Krainer, Institute of Geology, Innsbruck University, Innsbruck, A-6020 Austria, [email protected] Scott D. Elrick, Illinois State Geological Survey, Champaign, IL 61820, [email protected] Abstract (part of the Dakota Formation, Campana (Fig. 1). This is the most extensive outcrop Member of the Tres Hermanos Formation, area of Cretaceous rocks in southern New Upper Cretaceous sedimentary rocks are Flying Eagle Canyon Formation, Ash Canyon Mexico, and the exposed Cretaceous sec- Formation, and the entire McRae Group). A exposed in central Sierra County, southern tion is very thick, at about 2.5 km. First comprehensive understanding of the Cretaceous New Mexico, in the Fra Cristobal Mountains, recognized in 1860, these Cretaceous Caballo Mountains and in the topographically strata in Sierra County allows a more detailed inter- pretation of local geologic events in the context strata have been the subject of diverse, but low Cutter sag between the two ranges. The ~2.5 generally restricted, studies for more than km thick Cretaceous section is assigned to the of broad, transgressive-regressive (T-R) cycles of 150 years. (ascending order) Dakota Formation (locally deposition in the Western Interior Seaway, and includes the Oak Canyon [?] and Paguate also in terms of Laramide orogenic
    [Show full text]
  • (Chondrichthyes, Elasmobranchii) from the Upper Cretaceous of South America
    A ptychodontid (Chondrichthyes, Elasmobranchii) from the Upper Cretaceous of South America Paulo M. BRITO Departamento de Biologia Animal e Vegetal, Universidade do Estado do Rio de Janeiro, rua São Francisco Xavier, 524, Rio de Janeiro (Brazil) [email protected] Philippe JANVIER UMR 8569 du CNRS, Département Histoire de la Terre, Muséum national d’Histoire naturelle, 8 rue Buffon, F-75231 Paris cedex 05 (France) [email protected] Brito P. M. & Janvier P. 2002. — A ptychodontid (Chondrichthyes, Elasmobranchii) from the Upper Cretaceous of South America. Geodiversitas 24 (4) : 785-790. ABSTRACT An articulated assemblage of chondrichthyan teeth remain, previously described by Larrazet (1886) as selachian dermal scutes from the Carboniferous of New Granada, is re-described as a Ptychodus sp. and turns out to be Cretaceous in age, presumably from the La Luna Formation of Colombia or Venezuela. This Ptychodus species seems to differ from all the other known ptychodon- KEY WORDS tids by its homodontous dentition, tooth morphology and ornamentation, Chondrichthyes, however we prefer not to erect a new taxon here until tooth morphology Ptychodontidae, Upper Cretaceous, morphoclines become better known and help in the understanding of the South America. phylogenetic relationships among chondrichthyans. RÉSUMÉ Un ptychodontidé (Chondrichthyes, Elasmobranchii) du Crétacé supérieur d’Amérique du Sud. Une plaque dentaire de Chondrichthyes, précédemment décrite par Larrazet (1886) comme des plaques dermiques d’un Sélacien du Carbonifère de la Nouvelle
    [Show full text]
  • Cranial Anatomy and Taxonomy of Dolichorhynchops Bonneri New
    Marshall University Marshall Digital Scholar Biological Sciences Faculty Research Biological Sciences 2008 Cranial anatomy and taxonomy of Dolichorhynchops bonneri new combination, a polycotylid (Sauropterygia: Plesiosauria) from the Pierre Shale of Wyoming and South Dakota F. Robin O’Keefe Marshall University, [email protected] Follow this and additional works at: http://mds.marshall.edu/bio_sciences_faculty Part of the Animal Sciences Commons, and the Ecology and Evolutionary Biology Commons Recommended Citation O'Keefe, F. R. (2008). Cranial anatomy and taxonomy of Dolichorhynchops bonneri new combination, a polycotylid (Sauropterygia: Plesiosauria) from the Pierre Shale of Wyoming and South Dakota. Journal of Vertebrate Paleontology, 28(3), 664-676. This Article is brought to you for free and open access by the Biological Sciences at Marshall Digital Scholar. It has been accepted for inclusion in Biological Sciences Faculty Research by an authorized administrator of Marshall Digital Scholar. For more information, please contact [email protected], [email protected]. CRANIAL ANATOMY AND TAXONOMY OF DOLICHORHYNCHOPS BONNERI NEW COMBINATION, A POLYCOTYLID (SAUROPTERYGIA: PLESIOSAURIA) FROM THE PIERRE SHALE OF WYOMING AND SOUTH DAKOTA F. ROBIN O’KEEFE ABSTRACT The taxonomic identity of two well-preserved polycotylid plesiosaur skeletons from the Pierre Shale of far northern Wyoming and southern South Dakota has been controversial since their discovery. Originally referred to Dolichorhynchops osborni, the material was almost immediate-ly christened Trinacromerum bonneri Adams 1997; more recently the material has been referred to Polycotylus. Recent preparation of the well-preserved skull of one specimen permits detailed examination of the cranial morphology of this animal for the first time, and allows for its inclusion in a cladistic analysis of the Polycotylidae.
    [Show full text]
  • Upper Cretaceous Chondrichthyes Teeth Record in Phosphorites of the Loma Gorda Formation•
    BOLETIN DE CIENCIAS DE LA TIERRA http://www.revistas.unal.edu.co/index.php/rbct Upper Cretaceous chondrichthyes teeth record in phosphorites of the • Loma Gorda formation Alejandro Niño-Garcia, Juan Diego Parra-Mosquera & Peter Anthony Macias-Villarraga Departamento de Geociencias, Facultad de Ciencias Naturales y Exactas, Universidad de Caldas, Manizales, Colombia. [email protected], [email protected], [email protected] Received: April 26th, 2019. Received in revised form: May 17th, 2019. Accepted: June 04th, 2019. Abstract In layers of phosphorites and gray calcareous mudstones of the Loma Gorda Formation, in the vicinity of the municipal seat of Yaguará in Huila department, Colombia, were found fossils teeth of chondrichthyes, these were extracted from the rocks by mechanical means, to be compared with the species in the bibliography in order to indentify them. The species were: Ptychodus mortoni (order Hybodontiformes), were found, Squalicorax falcatus and Cretodus crassidens (order Lamniformes). This finding constitutes the first record of these species in the Colombian territory; which allows to extend its paleogeographic distribution to the northern region of South America, which until now was limited to Africa, Europe, Asia and North America, except for the Ptychodus mortoni that has been described before in Venezuela. Keywords: first record; sharks; upper Cretaceous; fossil teeth; Colombia. Registro de dientes de condrictios del Cretácico Superior en fosforitas de la formación Loma Gorda Resumen En capas de fosforitas y lodolitas calcáreas grises de la Formación Loma Gorda, en cercanías de la cabecera municipal de Yaguará en el departamento del Huila, Colombia, se encontraron dientes fósiles de condrictios; estos fueron extraídos de la roca por medios mecánicos, para ser comparados con las especies encontradas en la bibliografía e identificarlos.
    [Show full text]
  • Paleoecology of Late Cretaceous Methane Cold-Seeps of the Pierre Shale, South Dakota
    City University of New York (CUNY) CUNY Academic Works All Dissertations, Theses, and Capstone Projects Dissertations, Theses, and Capstone Projects 10-2014 Paleoecology of Late Cretaceous methane cold-seeps of the Pierre Shale, South Dakota Kimberly Cynthia Handle Graduate Center, City University of New York How does access to this work benefit ou?y Let us know! More information about this work at: https://academicworks.cuny.edu/gc_etds/355 Discover additional works at: https://academicworks.cuny.edu This work is made publicly available by the City University of New York (CUNY). Contact: [email protected] Paleoecology of Late Cretaceous methane cold-seeps of the Pierre Shale, South Dakota by Kimberly Cynthia Handle A dissertation submitted to the Graduate Faculty in Earth and Environmental Sciences in partial fulfillment of the requirements for the degree of Doctor of Philosophy, The City University of New York 2014 i © 2014 Kimberly Cynthia Handle All Rights Reserved ii This manuscript has been read and accepted for the Graduate Faculty in Earth and Environmental Sciences in satisfaction of the dissertation requirement for the degree of Doctor of Philosophy. Neil H. Landman____________________________ __________________ __________________________________________ Date Chair of Examining Committee Harold C. Connolly, Jr.___ ____________________ __________________ __________________________________________ Date Deputy - Executive Officer Supervising Committee Harold C. Connolly, Jr John A. Chamberlain Robert F. Rockwell The City University of New York iii ABSTRACT The Paleoecology of Late Cretaceous methane cold-seeps of the Pierre Shale, South Dakota By Kimberly Cynthia Handle Adviser: Neil H. Landman Most investigations of ancient methane seeps focus on either the geologic or paleontological aspects of these extreme environments.
    [Show full text]