Theuniversity Oftexasbulletin 3101 Plate XII 230 the University of Texas Bulletin PLATE XIII Figures— Page 1

Total Page:16

File Type:pdf, Size:1020Kb

Theuniversity Oftexasbulletin 3101 Plate XII 230 the University of Texas Bulletin PLATE XIII Figures— Page 1 TheUniversity of TexasBulletin No. 3101: January 1, 1931 Contributions to Geology, 1931 Bureau of Economic Geology J. A.Udden, Director E. H.Sellards, AssociateDirector PUBLISHED BY THE UNIVERSITY OF TEXAS AUSTIN Publications of The University of Texas Publications Committees GENERAL: Frederic Duncalp Mrs. C. M. Perry J. F.Dobie C. H. Slover J. L.Henderson G. W. Stumberg H. J. Muller A. P.Winston official: E. J. Mathews Killis Campbell C. F. Arrowood C. D.Simmons E. C.H.Bantel Bryant Smith The University publishes bulletins four times a month, so numbered that the first two digits of the number show the year of issue and thelast two the position in the yearly series. (For example, No. 3101 is the first bulletin of the year 1931.) These bulletins comprise the official publica- tions of the University, publications on humanistic and scientific subjects, and bulletins issued from time to time by various divisions of the University. The following bureaus and divisions distribute bulletins issuedby them; communications concerning bulletins in these fields should beaddressed toThe University of Texas,Austin,Texas,care of the bureau or division issuing the bulletin: Bureau of Business Research, Bureau of Economic Geology, Bureau of Engineering Research, Interscholastic League Bureau., andDivision of Extension. Communications concerning all other publications of the University should be addressed toUniversity Publications,TheUniversity of Texas,Austin. Additional copies of this publication may be procured from the Bureau of Economic Geology, The University of Texas, Austin, Texas, at $1.00 per copy The University of Texas Bulletin No. 3101: January 1, 1931 Contributions to Geology, 1931 Bureau of Economic Geology J. A Udden,Director E. H. Sellards, Associate Director PUBLISHED BY THE UNIVERSITY FOUR TIMES A MONTH, AND ENTERED AS SECOND-CLASS MATTER AT THE POSTOFFICE AT AUSTIN, TEXAS, UNDER THE ACT OF AUGUST 24, 1912 The benefits of education and of useful knowledge, generally diffused through a community, are essential to the preservationof a free govern- ment. Sam Houston Cultivated mind is the guardian genius of Democracy,and while guided and controlled by virtue, the noblest attribute of man. Itis the only dictator that freemen acknowledge, and the only security which freemendesire. Mirabeau B. Lamar Contents A. Erratics in the Pennsylvanian of Texas, by E. H.Sellards 9 Introduction 9 The Marathon uplift 11 The erratics 12 The Housetop Mountain locality 13 The Clark Ranch locality 17 Relation to regional geology 17 B. Some Major Structural Features of West Texas, by H. P. Bybee 19 Introduction 19 Major structural features 19 Extreme west Texas 19 The Franklin Mountains 20 The Hueco Bolson 21 The Diablo Plateau 22 The Salt Flat 22 The Guadalupe-Delaware-Apache Mountains 23 Southern end of the PermianBasin 24 The Delaware Basin 24 The Central Basin Platform 24 The Main Permian Basin 25 The Eastern Platform 25 Similarity of major structural features of west Texas 26 C. New Early Fusulinids from Texas, by Norman L. Thomas 27 Introduction and acknowledgements 27 Occurrence of the fossils 27 Age of formation containing the fossils 30 Descriptionof species 31 Fusulina llanoensis n.sp 1 31 Fusulina primaeva Skinner 32 D. Some Upper Cretaceous Ammonites in Western Texas, by W. S. Adkins 35 Description of localities 35 Chispa Summit 35 Southwest flank of Van Horn Mountains 39 West of Glenn Creek 40 Description of species 41 Mantelliceras budaense n. sp 41 Mantelliceras sp. aff. couloni (D'Orbigny) 42 Romanicerascumminsi n. sp 43 Romaniceras loboense n. sp 44 Metacalycoceras (?) sp 45 Coilopoceras eaglefordense n. sp 46 Coilopoceras chispaense n. sp 48 Coilopoceras austinense n. sp 49 Coilopoceras sp. aff. C. springeri Hyatt 51 Pseudaspidoceras (?) chispaense n. sp 51 Pseudaspidoceras(?) sp 53 Pseudaspidoceras (?) n. sp. A 53 Pseudaspidoceraseaglense (Adkins) 53 Pseudaspidoceras sp. aff. footeanum (Stoliczka) 54 Fagesia texana n. sp 55 Fagesia sp. cf. F. haarmani Bose 56 Thomasites sp. '— 56 Neoptychites sp. aff. N. gourguchoni Pervinquiere 57 4 Contents Pseudotissotia (?) n. sp 58 Hoplitoides (?) mirabilisBose (not Pervinquiere) 59 Kanabiceras septem-seriatum (Cragin) 60 Allocriocerasn. sp. 63 Scaphites sp. aff. africanus Pervinquiere 63 Scaphites sp. aff. aequalis Sowerby 64 Baculites sp. aff. gracilis Shumard 64 Metaptychoceras n. sp. aff. M. smithi (H. Woods) 64 Camptonectes sp. i 65 Status of correlationof formations 65 Supplementary statement relating to Neocardioceras 72 E. The Lower Claiborne on the Brazos River, by B. Coleman Renick and H. B. Stenzel 1 73 Introduction 73 Previous investigations 73 Present investigations 74 Geology 76 Mount Selman-CookMountain contact 76 Wilcox formation or group 81 Lower Claiborne group 81 Mount Selman formation 81 Carrizo sand . 81 Reklaw clay 83 Queen City sand 84 Weches clay 84 Cook Mountain formation 90 Sparta sand 90 Crockett clay 91 Upper Claiborne group 96 Yegua formation 96 F. Some Cretaceous foraminifera in Texas, by Helen Jeanne Plummer 109 Introduction 109 "Orbulina rock" 112 Descriptions of outcrops 118 Descriptions of genera and species.. 124 Family Reophacidae 124 Genus Haplostiche— : 124 texana (Conrad) 124 Family Lituolidae 126 Genus Flabellammina 126 alexanderi Cushman 126 Family Textulariidae 127 Genus Textularia 127 washitensis Carsey 127 rioensis Carsey 128 Genus Spiroplectammina 129 semicomplanata (Carsey) 129 Family Valvulinidae 130 Genus Dorothia 130 bulletta (Carsey) 132 Family Verneuilinidae 133 Genus Tritaxia 133 pyramidata Reuss 133 Genus Gaudryina 135 rugosa d'Orbigny 135 gradata Berthelin 136 Contents 5 Genus Gaudryinella 137 delrioensis Plummer 137 Genus Clavulina 138 insignis n. sp 138 Family Trochamminidae 140 Genus Trochammina 140 diagonis (Carsey) 140 Family Lagenidae 140 Genus Lenticulina 141 navarroensis (Plummer) 141 rotulata (Lamarck) 142 washitensis (Carsey) 142 Genus Astacolus 143 taylorensis n. sp 143 dissonus n.sp. 145 Genus Hemicr istellaria 146 ensis (Reuss) 146 silicula n. sp 148 Genus Dentalina 149 communis (d'Orbigny) 149 granti (Plummer) 149 soluta Reuss 150 reussi Neugeboren 151 raristriata (Chapman) 152 obliqua (Linne) 153 alternata (Jones) 153 crinita n. sp 154 Genus Nodosaria 155 radicula (Linne) 155 obscura Reuss 156 zippei Reuss 157 Genus Pseudoglandulina 158 sp. 158 Genus Lagena 159 hispida Reuss 159 sulcata (Walker and Jacob) 159 Genus Vaginulina 160 webbervillensis Carsey 160 simondsi Carsey 161 regina n. sp 162 Genus Flabellina 163 interpunctata yon der Marck 163 projecta ( Carsey) 165 rugosa d'Orbigny 166 Genus Kyphopyxa 168 christneri (Carsey) 168 Genus Frondicularia 171 clarki Bagg 171 Family Polymorphinidae 173 Genus Guttulina 173 problema d'Orbigny 173 Genus Pseudopolymorphina 173 cuyleri n. sp -" 173 Genus Ramulina 174 globulifera H. B. Brady 174 Family Nonionidae 175 Genus Nonionella 175 robustan. sp 175 6 Contents Family Heterohelicidae 176 Genus Giimbelina 176 excolata Cushman 176 globifera (Reuss) 177 Genus Ventilabrella 178 carseyae n. sp 178 Family Buliminidae 179 Genus Buliminella 179 carseyaen. sp 179 Genus Bulimina 180 pupoides d'Orbigny 180 Genus Bolivina 181 decorata Jones 181 Genus Loxostoma 182 plaitum (Carsey) 182 Genus Siphogenerinoides 183 plummeri (Cushman) , 183 Genus Uvigerina 186 seligi Cushman 186 Genus Dentilinopsis : 187 excavata (Reuss) 187 Family Rotaliidae 188 Genus Discorbis 188 correcta Carsey 188 Genus Valvulineria 190 asterigerinoides n. sp 190 Genus Gyroidina 190 depressa (Alth) 190 nitida (Reuss) 191 Genus Eponides : 192 micheliniana (d'Orbigny) 192 Family Globigerinidae 193 Genus Globigerina 193 washitensis Carsey 193 rugosa Plummer 194 Family Globorotaliidae 195 Genus Globotruncana 195 area (Cushman) 195 fornicata n. sp 198 canaliculatavar. ventricosa White 199 Genus Globorotalia 199 delrioensis n. sp 199 Family Anomalinidae 200 Genus Anomalina 200 pseudopapillosa Carsey 200 grosserugosa (Giimbel) 201 taylorensis -Carsey 202 falcata (Reuss) 202 Index 237 Contents 7 Illustrations Figures Fig. 1. Sketch map of the Marathon region 10 Fig. 2. Hill showing profusion of boulders 14 Fig. 3. Large novaculite boulder 14 Fig. 4. The Haymondformation near the Clark Ranch house. 17 Fig. 5. Map showing the major structural features of west Texas 26 Fig. 6 Bluff on Pfluger Ranch, LlanoRiver 28 Fig. 7. Sketchmap of Chispa Summit 36 Fig. 8. Coilopoceras sp. from Eagle Ford formation 51 Fig. 9. Geologic map of the lower Claiborne in the vicinity of the Brazos River 75 Fig. 10. Columnar section of exposed rocks and characteristic fossils along the Brazos River 79 Fig. 11. Geologic sections along Crockett-Sparta contact in the vicinity of the Brazos River 88 Fig. 12. Map of Austin area showing the Travis County outcrops 120 Plates Following page 203 Plate I. New early fusulinids. Plates IIto V. Upper Cretaceous ammonites.' Plates VI to VII. Tertiary fossils. Plates VIII to XV. Cretaceous foraminifera. The "Contributions to Geology" includes shorter papers of which, in additionto other Bureau publications,usually one volume per year will be issued. Each volume of the "Contributions" bears a bulletin number and is thus a part of the series of The University of Texas bulletinsissued from the Bureau of Economic Geology. E. H. Sellards, AssociateDirector. Erratics in the Pennsylvanian of Texas BY E. H. Sellards Introduction At the meeting of the Geological Society of America in Toronto, Canada, December, 1930, announcement was made of the discovery of erratics of large size in the Haymond formation of Carboniferous age
Recommended publications
  • Handbook of Texas Cretaceous Fossils
    University of Texas Bulletin No. 2838: October 8, 1928 HANDBOOK OF TEXAS CRETACEOUS FOSSILS B y W. S. ADKINS Bureau of Economic Geology J. A. Udden, Director E. H. Sellards, Associate Director PUBLISHED BY THE UNIVERSITY FOUR TIMES A MONTH, AND ENTERED AS SECOND-CLASS MATTER AT THE POSTOFFICE AT AUSTIN, TEXAS. UNDER THE ACT OF AUGUST 24. 1912 The benefits of education and of useful knowledge, generally diffused through a community, are essential to the preservation of a free govern­ m en t. Sam Houston Cultivated mind is the guardian genius of democracy. It is the only dictator that freemen acknowl­ edge and the only security that free­ men desire. Mirabeau В. Lamar CONTENTS P age Introduction __________________________________________________ 5 Summary of Formation Nomenclature_______________________ 6 Zone Markers and Correlation_______________________________ 8 Types of Texas Cretaceous Fossils___________________________ 36 Bibliography ________________________________________________ 39 L ist and Description of Species_________________________________ 46 P lants ______________________________________________________ 46 Thallophytes ______________________________________________ 46 Fungi __________________________________________________ 46 Algae __________________________________________________ 47 Pteridophytes ____________________________________________ 47 Filices __________________________________________________ 47 Spermatophytes __________________________________________ 47 Gymnospermae _________________________________________
    [Show full text]
  • 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]
  • Les Vascoceratinae Et Les Pseudotissotiinae
    LES VASCOCERATINAE ET LES PSEUDOTISSOTIINAE (AMMONITINA) D'ASHAKA (NE NIGERIA) : RELATIONS AVEC LEUR ENVIRONNEMENT BIOSÉDIMENTAIRE THE VASCOCERATINAEA AND PSEUDOTISSOTIINAEA (AMMONITINA) FROM ASHAKA (NE NIGERIA) : RELATIONSHIPS WlTH THE BIOSEDIMENTARY ENVIRONMENT Philippe COURVILLE COURVILLE Ph. (1992) - Les Vascoceratnae et es Pseudotssotinae (Ammonitina) d'Açhaka (NE Ngera) . relatons avec leur enviannement blosedimentare [The Vaçcoceia1,naea and Psetidotfssoti!naea jAmmon,ti.?s) fiom As,ba,ks (NE Nigeria) relationsh!ps with the biosedimentary enviionment] - Bull. Centres Rech Explof.- Prod EliAquitaine. 16. 2 407~457.8 f~y, 14 p.. Bo~ssensDecember 24, 19'32 - SSN : 0396~2687 CODEN. BCREDP A purdscpnary analyss groupng the sedtmentary yeo,ogy, the sequenta! stratgraphy. !he mcropaleonto1og;cal and nacropaeontologcal aspec!s. allows us 10 renterpret tbe marine çecton of the Gonga Formaton (hypostratotypc Ashaka sect~on).The paleartolag~cal successlonç (benthon~carganiçtrç and Ammonlte papulatons) and the sedmentary unis (ensembles mted by two d!scontinutes) cari now oe deçcrbed accurateiy A dynamc nterpretator of the seres of Ammonte papulatons s proposed for the local framework of the Ashaka ste some taxa coud beong to .. autochthonous ,, neages (Vascoceratnae and Pseudotsçatnae) others are corsdered ta be ., exo~ ric ,. elements (Fagesra and Pseodaspidoceras) The settements of the Cer,omanan and Turonan marne envronments seem to be w~th~na few steps reach. Fi'çt of a. tïe progreçslve settng of subplatycone 01 paty~spheroconetethysan Vascoceratds (Nigeiiceras and V gr cauv!ni) can be obçerved Ths ç folowed by the suaden .. appearance .. of cad-serperllcone Ammontes, whch quicky dr~fttowards cad-spherocone forms (frst morphologcal c:sls) Then a second morpnolagica crlsls occurç.
    [Show full text]
  • Vita Scientia Revista De Ciências Biológicas Do CCBS
    Volume III - Encarte especial - 2020 Vita Scientia Revista de Ciências Biológicas do CCBS © 2020 Universidade Presbiteriana Mackenzie Os direitos de publicação desta revista são da Universidade Presbiteriana Mackenzie. Os textos publicados na revista são de inteira responsabilidade de seus autores. Permite-se a reprodução desde que citada a fonte. A revista Vita Scientia está disponível em: http://vitascientiaweb.wordpress.com Dados Internacionais de Catalogação na Publicação (CIP) Vita Scientia: Revista Mackenzista de Ciências Biológi- cas/Universidade Presbiteriana Mackenzie. Semestral ISSN:2595-7325 UNIVERSIDADE PRESBITERIANA MACKENZIE Reitor: Marco Túllio de Castro Vasconcelos Chanceler: Robinson Granjeiro Pro-Reitoria de Graduação: Janette Brunstein Pro-Reitoria de Extensão e Cultura: Marcelo Martins Bueno Pro-Reitoria de Pesquisa e Pós-Graduação: Felipe Chiarello de Souza Pinto Diretora do Centro de Ciências Biológicas e da Saúde: Berenice Carpigiani Coordenador do Curso de Ciências Biológicas: Adriano Monteiro de Castro Endereço para correspondência Revista Vita Scientia Centro de Ciências Biológicas e da Saúde Universidade Presbiteriana Mackenzie Rua da Consolação 930, São Paulo (SP) CEP 01302907 E-mail: [email protected] Revista Vita Scientia CONSELHO EDITORIAL Adriano Monteiro de Castro Camila Sachelli Ramos Fabiano Fonseca da Silva Leandro Tavares Azevedo Vieira Patrícia Fiorino Roberta Monterazzo Cysneiros Vera de Moura Azevedo Farah Carlos Eduardo Martins EDITORES Magno Botelho Castelo Branco Waldir Stefano CAPA Bruna Araujo PERIDIOCIDADE Publicação semestral IDIOMAS Artigos publicados em português ou inglês Universidade Presbiteriana Mackenzie, Revista Vita Scientia Rua da Consolaçãoo 930, Edíficio João Calvino, Mezanino Higienópolis, São Paulo (SP) CEP 01302-907 (11)2766-7364 Apresentação A revista Vita Scientia publica semestralmente textos das diferentes áreas da Biologia, escritos em por- tuguês ou inglês: Artigo resultados científicos originais.
    [Show full text]
  • Classification of Ammonitic Sutures Using Gis
    Palaeontologia Electronica http://palaeo-electronica.org PATTERN MATCHING: CLASSIFICATION OF AMMONITIC SUTURES USING GIS Lori L. Manship ABSTRACT Geographic Information Systems (GIS) is utilized to apply spatial analysis tech- niques to visually and quantitatively match ammonoid suture patterns for classification. The Turonian ammonite family Coilopoceratidae was chosen as the basis for this project, because the similar suture patterns within the family make species-level identi- fication a challenge. A Coilopoceras springeri suture template was created by overlay- ing 10 different Coilopoceras springeri suture patterns, using the right holotype suture pattern as the basal or designation guide. Templates for Coilopoceras colleti and Hopli- toides sandovalensis sutures were constructed in the same manner. Sutures of known and unknown specimens were tested within the templates in order to identify species. The sutures of known specimens matched with the correct templates and did not com- pare well with other species’ templates. Sutures of unknown specimens clearly fit within one template better than within others and, hence, could be reliably classified to the species level. In addition to species classification, the GIS method provides a mechanism for both visual and quantitative comparisons of individual sutures. This GIS method will aid professional and avocational paleontologists, biostratigraphers, and geologists in classifying ammonite species, and may help further our understanding of suture morphogenesis and function by providing a standard basis for morphological comparison of complex sutural patterns. Department of Geosciences, Texas Tech University, Lubbock, Texas, 79409-1053, USA. [email protected] KEY WORDS: ammonite; Geographic Information Systems (GIS); suture pattern; Turonian; Cretaceous PE Article Number: 7.2.5A Copyright: Paleontological Society.
    [Show full text]
  • Phylogeny, Diversity, and Ecology of the Ammonoid Superfamily Acanthoceratoidea Through the Cenomanian and Turonian
    PHYLOGENY, DIVERSITY, AND ECOLOGY OF THE AMMONOID SUPERFAMILY ACANTHOCERATOIDEA THROUGH THE CENOMANIAN AND TURONIAN DAVID A.A. MERTZ A Thesis Submitted to the Graduate College of Bowling Green State University in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE August 2017 Committee: Margaret Yacobucci, Advisor Andrew Gregory Keith Mann © 2017 David Mertz All Rights Reserved iii ABSTRACT Margaret Yacobucci Both increased extinction and decreased origination, caused by rising oceanic anoxia and decreased provincialism, respectively, have been proposed as the cause of the Cenomanian Turonian (C/T) extinction event for ammonoids. Conflicting evidence exists for whether diversity actually dropped across the C/T. This study used the ammonoid superfamily Acanthoceratoidea as a proxy for ammonoids as a whole, particularly focusing on genera found in the Western Interior Seaway (WIS) of North America, including Texas. Ultimately, this study set out to determine 1) whether standing diversity decreased across the C/T boundary in the WIS, 2) whether decreased speciation or increased extinction in ammonoids led to a drop in diversity in the C/T extinction event, 3) how ecology of acanthoceratoid genera changed in relation to the C/T extinction event, and 4) whether these ecological changes indicate rising anoxia as the cause of the extinction. In answering these questions, three phylogenetic analyses were run that recovered the families Acanthoceratidae, Collignoniceratidae, and Vascoceratidae. Pseudotissotiidae was not recovered at all, while Coilopoceratidae was recovered but reclassified as a subfamily of Vascoceratidae. Seven genera were reclassified into new families and one genus into a new subfamily. After calibrating the trees with stratigraphy, I was able to determine that standing diversity dropped modestly across the C/T boundary and the Early/Middle Turonian boundary.
    [Show full text]
  • Sucesión De Amonitas Del Cretácico Superior (Cenomaniano – Coniaciano) De La Parte Más Alta De La Formación Hondita Y De L
    Boletín de Geología Vol. 33, N° 1, enero-junio de 2011 SUCESIÓN DE AMONITAS DEL CRETÁCICO SUPERIOR (CENOMANIANO – CONIACIANO) DE LA PARTE MÁS ALTA DE LA FORMACIÓN HONDITA Y DE LA FORMACIÓN LOMA GORDA EN LA QUEBRADA BAMBUCÁ, AIPE - HUILA (COLOMBIA, S. A.) Pedro Patarroyo1 RESUMEN La sección de la quebrada Bambucá (Aipe - Huila) posee una buena exposición de los depósitos del Cretácico del Valle Superior del Magdalena. De la parte alta de la Formación Hondita se recolectaron Acanthoceras sp. y Rhynchostreon sp. del Cenomaniano superior. Dentro del segmento inferior de la Formación Loma Gorda se hallaron Choffaticeras (C.) cf. segne, Fagesia cf. catinus, Neoptychites cf. andinus, Mitonia gracilis, Morrowites sp., Nannovascoceras ? sp., Quitmaniceras ? sp., Benueites ? sp. junto con Mytiloides kossmati, M. goppelnensis y Anomia sp. del Turoniano inferior. Estratigráficamente arriba aparecen Paramammites ? sp., Hoplitoides sp. H. ingens, H. cf. lagiraldae, Codazziceras ospinae, Allocrioceras sp., que pueden estar representando entre el Turoniano inferior y medio. Para la parte alta de este segmento se encontraron Prionocycloceras sp. P. guayabanum, Reesidites subtuberculatum, Subprionotropis colombianus, Mytiloides scupini, Dydimotis sp., Gauthiericeras sp., Anagaudryceras ? sp., Eulophoceras jacobi, Paralenticeras sieversi, Hauericeras cf. madagascarensis, Peroniceras (P.) subtricarinatum, Forresteria (F.) sp., Barroisiceras cf. onilahyense, Ankinatsytes venezolanus que abarcan entre el Turoniano superior y el Coniaciano. Con base en la fauna colectada no es posible establecer los límites Cenomaniano/Turoniano y Turoniano/Coniaciano. Palabras clave: Amonitas, Cretácico superior, Valle Superior del Magdalena, Aipe-Huila-Colombia. UPPER CRETACEOUS AMMONITE SUCCESSION (CENOMANIAN – CONIACIAN) RELATED TO THE UPPER HONDITA AND LOMA GORDA FORMATIONS ALONG THE BAMBUCÁ CREEK, AIPE - HUILA (COLOMBIA, S.A.) ABSTRACT The Bambucá creek section (Aipe - Huila) shows a very good exposition of the Upper Magdalena Valley Cretaceous deposits.
    [Show full text]
  • Mid-Cretaceous Ammonite Sequence for Western New Mexico Iv
    iii Contents ABSTRACT 5 Genus Morrowites Cobban and Hook, n. gen. 9 Morrowites wingi (Morrow) 9 INTRODUCTION 5 M. depressus (Powell) 11 COMPOSITION OF MOLLUSCAN FAUNA 5 M. subdepressus Cobban and Hook, n. sp. 11 OCCURRENCE AND PRESERVATION OF FOSSILS 6 M. cf. M. dixeyi (Reyment) 12 STRATIGRAPHIC POSITION OF FOSSILS 6 Subfamily Euomphaloceratinae Cooper 13 COLLECTION LOCALITIES 7 Genus Kamerunoceras Reyment 13 Kamerunoceras turoniense (d'Orbigny) 13 FAMILY VASCOCERATIDAE H. Douvillé 14 SYSTEMATIC PALEONTOLOGY 7 Subfamily Vascoceratinae H. Douvillé 14 FAMILY BACULITIDAE GILL 7 Genus Neoptychites Kossmat 14 Genus Baculites Lamarck 7 Neoptychites cephalotus (Courtiller) 14 Baculites yokoyamai Tokunaga and Shimizu 7 Genus Fagesia Pervinquière 15 FAMILY MUNIERICERATIDAE WRIGHT 7 Fagesia superstes (Kossmat) 16 Genus Tragodesmoceras Spath 7 FAMILY C OLLIGNONICERATIDAE WRIGHT AND WRIGHT 16 Tragodesmoceras socorroense Cobban and Hook 7 Subfamily Barroisiceratinae Basse 16 FAMILY PLACENTICERATIDAE HYATT 8 Genus Cibolaites Cobban and Hook, n. gen. 16 Genus Placenticeras Spath 8 Cibolaites molenaari Cobban and Hook, n. sp. 16 Placenticeras cumminsi Cragin 8 REFERENCES 18 FAMILY ACANTHOCERATIDAE DE GROSSOUVRE 8 Subfamily Mammitinae Hyatt 8 Genus Mammites PLATES 1-14 21 Laube and Bruder 8 INDEX 50 Mammites nodosoides (Schluter) 8 TABLE 1—Mid-Cretaceous ammonite sequence for western New Mexico iv FIGURES 1—Location of study area 5 9—Histogram of size and body chambers of Neoptychites 2—External sutures of Mammites nodosoides (Schluter) 9 3— cephalotus (Courtiller) 14 Whorl sections of Morrowites wingi (Morrow) 10 4—External 10—Scatter diagram of breadth to diameter ratio of Neop- suture of Morrowites wingi (Morrow) 10 5—Whorl section and tychites 14 suture of Morrowites depressus 11—External sutures of Neoptychites cephalotus (Cour-tiller) 15 (Powell) 11 12—External suture of Fagesia superstes (Kossmat) 16 13— 6—External sutures of Morrowites subdepressus Cobban and Histogram of size of body chambers of Cibolaites molenaari Hook, n.
    [Show full text]
  • Mississippian Cephalopods of Northern and Eastern Alaska
    Mississippian Cephalopods of Northern and Eastern Alaska By MACKENZIE GORDON, JR. GEOLOGICAL SURVEY PROFESSIONAL PAPER 283 Descr9tions and illustrations of nautiloids and ammonoids and correlation of the assemblages with European Carbonferous goniatite zones UNITED STATES GOVERNMENT PRINTING OF,FICE, WASHINGTON : 1957 UNITED STATES DEPARTMENT OF THE INTERIOR FRED A. SEATON, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. - Price $1.50 (paper cover) CONTENTS Pane Page 1 Stratigraphic and geographic distribution-Continued Introduction - - - - - - .. - - - - ... - - - - - - - - - - - - .. - - - - - - - - - - - - - 1 Brooks Range-Continued Previous work-------------------------------------- 1 Kiruktagiak River basin--Chandler Lake area- - Composition of the cephalopod fauna ------------------ 2 Siksikpuk River basin ------- ---------- ------ Stratigraphic and geographic distribution of the cepha- Anaktuvuk River basin _------------..-..------ lopods------------------------------------------- Nanushuk River basin ...................... - Brooks Range---------------------------------- Echooka River basin --------- ----- - Cape Lisburne region ------- -- --- --------- - - - Eagle-Circle district ---__ _ -___ _- --- --- - - ---- - -- - - Lower Noatak Rlver basin -----------------..- Age and correlation of the cephalopod-bearing beds- ---- Western De Long Mountains_--__----- .------ Mississippian cephalopod-collecting localities in Alaska- -
    [Show full text]
  • A Preliminary Assessment of Paleontological Resources at Bighorn Canyon National Recreation Area, Montana and Wyoming
    A PRELIMINARY ASSESSMENT OF PALEONTOLOGICAL RESOURCES AT BIGHORN CANYON NATIONAL RECREATION AREA, MONTANA AND WYOMING Vincent L. Santucci1, David Hays2, James Staebler2 And Michael Milstein3 1National Park Service, P.O. Box 592, Kemmerer, WY 83101 2Bighorn Canyon National Recreation Area, P.O. Box 7458, Fort Smith, MT 59035 3P.O. Box 821, Cody, WY 82414 ____________________ ABSTRACT - Paleontological resources occur throughout the Paleozoic and Mesozoic formations exposed in Bighorn Canyon National Recreation Area. Isolated research on specific geologic units within Bighorn Canyon has yielded data on a wide diversity of fossil forms. A comprehensive paleonotological survey has not been previously undertaken at Bighorn Canyon. Preliminary paleontologic resource data is presented in this report as an effort to establish baseline data. ____________________ INTRODUCTION ighorn Canyon National Recreation Area (BICA) consists of approximately 120,000 acres within the Bighorn Mountains of north-central Wyoming and south-central Montana B (Figure 1). The northwestern trending Bighorn Mountains consist of over 9,000 feet of sedimentary rock. The predominantly marine and near shore sedimentary units range from the Cambrian through the Lower Cretaceous. Many of these formations are extremely fossiliferous. The Bighorn Mountains were uplifted during the Laramide Orogeny beginning approximately 70 million years ago. Large volumes of sediments, rich in early Tertiary paleontological resources, were deposited in the adjoining basins. This report provides a preliminary assessment of paleontological resources identified at Bighorn Canyon National Recreation Area. STRATIGRAPHY The stratigraphic record at Bighorn Canyon National Recreation Area extends from the Cambrian through the Cretaceous (Figure 2). The only time period during this interval that is not represented is the Silurian.
    [Show full text]
  • Rediscovery of the Holotypes of the Cenomanian (Upper Cretaceous) Ammonites Vascoceras Gamai Choffat, 1898, and Vascoceras Barcoicense (Choffat, 1898)
    Cretaceous Research 56 (2015) 647e650 Contents lists available at ScienceDirect Cretaceous Research journal homepage: www.elsevier.com/locate/CretRes Short communication Rediscovery of the holotypes of the Cenomanian (Upper Cretaceous) ammonites Vascoceras gamai Choffat, 1898, and Vascoceras barcoicense (Choffat, 1898) * Fernando Barroso-Barcenilla a, b, , Jose Manuel Brandao~ c, Pedro Miguel Callapez d, e, Vanda Faria dos Santos e, f a Grupo de Investigacion IberCreta, Departamento de Geología y Geografía, Facultad de Ciencias, Universidad de Alcala de Henares, 28871 Alcalade Henares, Spain b Grupo de Investigacion Procesos Bioticos Mesozoicos, Departamento de Paleontología, Facultad de Ciencias Geologicas, Universidad Complutense de Madrid, 28040 Madrid, Spain c Instituto de Historia Contemporanea,^ Centro de Estudos de Historia e FilosofiadaCi^encia, Universidade de Evora, 7000-554 Evora, Portugal d Departamento de Ci^encias da Terra, Faculdade de Ci^encias e Tecnologia, Universidade de Coimbra, 3030-790 Coimbra, Portugal e Centro de Investigaçao~ da Terra e do Espaço, Universidade de Coimbra, 3000-134 Coimbra, Portugal f Museu Nacional de Historia Natural e da Ci^encia, Universidade de Lisboa, 1250-102 Lisboa, Portugal article info abstract Article history: The historical holotypes of the Cenomanian (Upper Cretaceous) ammonites Vascoceras gamai Choffat, Received 23 January 2015 1898 (type of the genus), and Vascoceras barcoicense (Choffat, 1898), thought to be destroyed by the fire of Received in revised form March 1978 at the National Museum of Natural History, Lisbon, Portugal, have been rediscovered in good 10 June 2015 state of preservation. Based on the study of the originals, these upper Cenomanian specimens can be Accepted in revised form 27 June 2015 rehabilitated as holotypes, maintaining and justifying the status of both taxa as well as of Vascoceras Available online 30 July 2015 cauvini Chudeau, 1909.
    [Show full text]
  • Theuniversity Oftexasbulletin 3101 Plate XII 230 the University of Texas Bulletin PLATE XIII Figures— Page 1
    TheUniversity of TexasBulletin No. 3101: January 1, 1931 Contributions to Geology, 1931 Bureau of Economic Geology J. A.Udden, Director E. H.Sellards, AssociateDirector PUBLISHED BY THE UNIVERSITY OF TEXAS AUSTIN Publications of The University of Texas Publications Committees GENERAL: Frederic Duncalp Mrs. C. M. Perry J. F.Dobie C. H. Slover J. L.Henderson G. W. Stumberg H. J. Muller A. P.Winston official: E. J. Mathews Killis Campbell C. F. Arrowood C. D.Simmons E. C.H.Bantel Bryant Smith The University publishes bulletins four times a month, so numbered that the first two digits of the number show the year of issue and thelast two the position in the yearly series. (For example, No. 3101 is the first bulletin of the year 1931.) These bulletins comprise the official publica- tions of the University, publications on humanistic and scientific subjects, and bulletins issued from time to time by various divisions of the University. The following bureaus and divisions distribute bulletins issuedby them; communications concerning bulletins in these fields should beaddressed toThe University of Texas,Austin,Texas,care of the bureau or division issuing the bulletin: Bureau of Business Research, Bureau of Economic Geology, Bureau of Engineering Research, Interscholastic League Bureau., andDivision of Extension. Communications concerning all other publications of the University should be addressed toUniversity Publications,TheUniversity of Texas,Austin. Additional copies of this publication may be procured from the Bureau of Economic Geology, The University of Texas, Austin, Texas, at $1.00 per copy The University of Texas Bulletin No. 3101: January 1, 1931 Contributions to Geology, 1931 Bureau of Economic Geology J.
    [Show full text]