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Paleontological Resources at Grand Teton National Park, Northwestern Wyoming Vincent L
University of Wyoming National Park Service Research Center Annual Report Volume 22 22nd Annual Report, 1998 Article 7 1-1-1998 Paleontological Resources at Grand Teton National Park, Northwestern Wyoming Vincent L. Santucci National Park Service William P. Wall Georgia College and State University Follow this and additional works at: http://repository.uwyo.edu/uwnpsrc_reports Recommended Citation Santucci, Vincent L. and Wall, William P. (1998) "Paleontological Resources at Grand Teton National Park, Northwestern Wyoming," University of Wyoming National Park Service Research Center Annual Report: Vol. 22 , Article 7. Available at: http://repository.uwyo.edu/uwnpsrc_reports/vol22/iss1/7 This Grand Teton National Park Report is brought to you for free and open access by Wyoming Scholars Repository. It has been accepted for inclusion in University of Wyoming National Park Service Research Center Annual Report by an authorized editor of Wyoming Scholars Repository. For more information, please contact [email protected]. Santucci and Wall: Paleontological Resources at Grand Teton National Park, Northwest PALEONTOLOGICAL RESOURCES AT GRAND TETON NATIONAL PARK, NORTHWESTERN WYOMING + VINCENT L. SANTUCCI+ NATIONAL PARK SERVICE KEMMERER + WY WILLIAM P. WALL+ DEPARTMENT OF BIOLOGY GEORGIA COLLEGE AND STATE UNIVERSITY MILLEDGEVILLE + GA + ABSTRACT landscape, and though the last great ice masses melted 15 ,000 years ago, some re-established small Paleontological resources occur throughout glaciers still exist. the formations exposed in Grand Teton National Park. A comprehensive paleontological survey has This report provides a preliminary not been attempted previously at Grand Teton assessment of paleontological resources identified at National Park. Preliminary paleontologic resource Grand Teton National Park. data is given in this report in order to establish baseline data. -
Geological Survey Canada
BULLETIN 119 GEOLOGICAL SURVEY OF CANADA DEPARTMENT OF MINES AND TECHNICAL SURVEYS THE JURASSIC FAUNAS OF THE CANADIAN ARCTIC CADOCERATINAE Hans Frebold Price $2.50 1964 GEOLOGICAL SURVEY OF CANADA BULLE TIN 119 THE JURASSIC FAUNAS OF THE CANADIAN ARCTIC CADOCERATINAE By Hans Frebold DEPARTMENT OF MINES AND TECHNICAL SURVEYS CANADA © Crown Copyrights reserved Available by mail from the Queen's Printer, Ottawa, from Geological Survey of Canada, 601 Booth St., Ottawa, and at the following Canadian Government bookshops: OTTAWA Daly Building, corner Mackenzie and Rideau TORONTO Mackenzie Building, 36 Adelaide St. East MONTREAL JEterna-Vie Building, 1182 St. Catherine St. West or through your bookseller A deposit copy of this publication is also available for reference in public libraries across Canada Price $2.50 Catalogue No. 42-119 Price subject to change without notice ROGER DUHAMEL, F.R.S.C. Queen's Printer and Controller of Stationery Ottawa, Canada 1964 PREFACE This report is based on fossil collections made over a vast area of the Canadian Arctic extending from Axel Heiberg Island in the north to the Aklavik region of the mainland and is a further contribution by the author on the Jurassic faunas of the Canadian Arctic. Detailed study of these ammonite faunas permits correlation of the associated Jurassic rocks and shows their faunal and stratigraphic relation ships with Alaska, East Greenland, and the Arctic areas of Europe and Asia. J. M. HARRISON, Director, Geological Survey of Canada OTTAWA, December 2, 1963 BULLETIN 119 — Die Jurafaunen der kanadischen Acktis CADOCERATINAE. Von Hans Frebold BiojiJieTeHt, 119 — r. <3>pe6ojib,,zT. -
Palaeoecology and Palaeoenvironments of the Middle Jurassic to Lowermost Cretaceous Agardhfjellet Formation (Bathonian–Ryazanian), Spitsbergen, Svalbard
NORWEGIAN JOURNAL OF GEOLOGY Vol 99 Nr. 1 https://dx.doi.org/10.17850/njg99-1-02 Palaeoecology and palaeoenvironments of the Middle Jurassic to lowermost Cretaceous Agardhfjellet Formation (Bathonian–Ryazanian), Spitsbergen, Svalbard Maayke J. Koevoets1, Øyvind Hammer1 & Crispin T.S. Little2 1Natural History Museum, University of Oslo, P.O. Box 1172 Blindern, 0318 Oslo, Norway. 2School of Earth and Environment, University of Leeds, Leeds LS2 9JT, United Kingdom. E-mail corresponding author (Maayke J. Koevoets): [email protected] We describe the invertebrate assemblages in the Middle Jurassic to lowermost Cretaceous of the Agardhfjellet Formation present in the DH2 rock-core material of Central Spitsbergen (Svalbard). Previous studies of the Agardhfjellet Formation do not accurately reflect the distribution of invertebrates throughout the unit as they were limited to sampling discontinuous intervals at outcrop. The rock-core material shows the benthic bivalve fauna to reflect dysoxic, but not anoxic environments for the Oxfordian–Lower Kimmeridgian interval with sporadic monospecific assemblages of epifaunal bivalves, and more favourable conditions in the Volgian, with major increases in abundance and diversity of Hartwellia sp. assemblages. Overall, the new information from cores shows that abundance, diversity and stratigraphic continuity of the fossil record in the Upper Jurassic of Spitsbergen are considerably higher than indicated in outcrop studies. The inferred life positions and feeding habits of the benthic fauna refine our understanding of the depositional environments of the Agardhfjellet Formation. The pattern of occurrence of the bivalve genera is correlated with published studies of Arctic localities in East Greenland and northern Siberia and shows similarities in palaeoecology with the former but not the latter. -
Characteristic Jurassic Mollusks from Northern Alaska
Characteristic Jurassic Mollusks From Northern Alaska GEOLOGICAL SURVEY PROFESSIONAL PAPER 274-D Characteristic Jurassic Mollusks From Northern Alaska By RALPH W. IMLAY A SHORTER CONTRIBUTION TO GENERAL GEOLOGY GEOLOGICAL SURVEY PROFESSIONAL PAPER 274-D A study showing that the northern Alaskan faunal succession agrees with that elsewhere in the Boreal region and in other parts of North America and in northwest Europe UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1955 UNITED STATES DEPARTMENT OF THE INTERIOR Douglas McKay, Secretary GEOLOGICAL SURVEY W. E. Wrather, Director For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. - BMMH§ts (paper cover) Price $1.00 CONTENTS Page Abstract_________________ 69 Introduction _________________ 69 Biologic analysis____________ 69 Stratigraphic summary. _______ 70 Ages of fossils________________ 73 Comparisons with other faunas. 75 Ecological considerations___ _ 75 Geographic distribution____. 78 Summary of results ___________ 81 Systematic descriptions__ _. 82 Literature cited____________ 92 Index_____________________ 95 ILLUSTRATIONS [Plates &-13 follow Index] PLATE 8. Inoceramus and Gryphaea 9. Aucella 10. Amaltheus, Dactylioceras, "Arietites," Phylloceras, and Posidonia 11. Ludwigella, Dactylioceras, and Harpoceras. 12. Pseudocadoceras, Arcticoceras, Amoeboceras, Tmetoceras, Coeloceras, and Pseudolioceras 13. Reineckeia, Erycites, and Cylindroteuthis. Page FIGXTKE 20. Index map showing Jurassic fossil collection localities in northern Alaska. -
Geology of the Prince William Sound and Kenai Peninsula Region, Alaska
Geology of the Prince William Sound and Kenai Peninsula Region, Alaska Including the Kenai, Seldovia, Seward, Blying Sound, Cordova, and Middleton Island 1:250,000-scale quadrangles By Frederic H. Wilson and Chad P. Hults Pamphlet to accompany Scientific Investigations Map 3110 View looking east down Harriman Fiord at Serpentine Glacier and Mount Gilbert. (photograph by M.L. Miller) 2012 U.S. Department of the Interior U.S. Geological Survey Contents Abstract ..........................................................................................................................................................1 Introduction ....................................................................................................................................................1 Geographic, Physiographic, and Geologic Framework ..........................................................................1 Description of Map Units .............................................................................................................................3 Unconsolidated deposits ....................................................................................................................3 Surficial deposits ........................................................................................................................3 Rock Units West of the Border Ranges Fault System ....................................................................5 Bedded rocks ...............................................................................................................................5 -
Palaeontology and Biostratigraphy of the Lower Cretaceous Qihulin
Dissertation Submitted to the Combined Faculties for the Natural Sciences and for Mathematics of the Ruperto-Carola University of Heidelberg, Germany for the degree of Doctor of Natural Sciences presented by Master of Science: Gang Li Born in: Heilongjiang, China Oral examination: 30 November 2001 Gedruckt mit Unterstützung des Deutschen Akademischen Austauschdienstes (Printed with the support of German Academic Exchange Service) Palaeontology and biostratigraphy of the Lower Cretaceous Qihulin Formation in eastern Heilongjiang, northeastern China Referees: Prof. Dr. Peter Bengtson Prof. Pei-ji Chen This manuscript is produced only for examination as a doctoral dissertation and is not intended as a permanent scientific record. It is therefore not a publication in the sense of the International Code of Zoological Nomenclature. Abstract The purpose of the study was to provide conclusive evidence for a chronostratigraphical assignment of the Qihulin Formation of the Longzhaogou Group exposed in Mishan and Hulin counties of eastern Heilongjiang, northeastern China. To develop an integrated view of the formation, all collected fossil groups, i.e. the macrofossils (ammonites and bivalves) and microfossils (agglutinated foraminifers and radiolarians) have been studied. The low-diversity ammonite fauna consists of Pseudohaploceras Hyatt, 1900, and Eogaudryceras Spath, 1927, which indicate a Barremian–Aptian age. The bivalve fauna consists of eight genera and 16 species. The occurrence of Thracia rotundata (J. de C: Sowerby) suggests an Aptian age. The agglutinated foraminifers comprise ten genera and 16 species, including common Lower Cretaceous species such as Ammodiscus rotalarius Loeblich & Tappan, 1949, Cribrostomoides? nonioninoides (Reuss, 1836), Haplophragmoides concavus (Chapman, 1892), Trochommina depressa Lozo, 1944. The radiolarians comprise ten genera and 17 species, where Novixitus sp., Xitus cf. -
Composition and Origin of Jurassic Ammonite Concretions at Gerzen, Germany
JURASSIC AMMONITE CONCRETIONS COMPOSITION AND ORIGIN OF JURASSIC AMMONITE CONCRETIONS AT GERZEN, GERMANY. By MICHAEL DAVID GERAGHTY, B.Sc. A Thesis Submitted to the School of Graduate Studies in Partial Fulfilment of the Requirements for the Degree Master of Science McMaster University (c) Copyright by Michael David Geraghty, April 1990 MASTER OF SCIENCE (1990) McMaster University (Geology) Hamilton, Ontario TITLE: Composition and Origin of Jurassic Ammonite Concretions at Gerzen, Germany. AUTHOR: Michael David Geraghty, B. Sc. (University of Guelph) SUPERVISOR: Professor G.E.G. Westermann NUMBER OF PAGES: xiii, 154, 17 Figs., 10 Pls. ii ACKNOWLEDGEMENTS I would like to express my sincere gratitude to Dr. Gerd Westermann for allowing me the privilege of studying under his supervision on a most interesting research project. His advice, support and patience were greatly appreciated. I deeply indebted to Mr. Klaus Banike of Gottingen, F. R. Germany for opening his home and his collection of concretions to me and also for his help and friendship. To Erhardt Trute and Family of Gerzen, F.R. Germany, I owe many thanks for their warm hospitality and assistance with my field work. Also Dr. Hans Jahnke of Georg-August University, Gottingen deserves thanks for his assistance and guidance. Jack Whorwood's photographic expertise was invaluable and Len Zwicker did an excellent job of preparing my thin sections. Also, Kathie Wright did a great job helping me prepare my figures. Lastly, I would like to thank all those people, they know who they are, from whom I begged and borrowed time, equipment and advice. iii ABSTRACT Study of the ecology of concretion and host sediment fossils from a shell bed in middle Bajocian clays of northwestern Germany indicates a predominantly epifaunal suspension-feeding community living on a firm mud bottom. -
The Evolution of the Jurassic Ammonite Family Cardioceratidae
THE EVOLUTION OF THE JURASSIC AMMONITE FAMILY CARDIOCERATIDAE by J. H. CALLOMON ABSTRACT.The beginnings of the Jurassic ammonite family Cardioceratidae can be traced back rather precisely to the sudden colonization of a largely land-locked Boreal Sea devoid of ammonites by North Pacific Sphaer- oceras (Defonticeras) in the Upper Bajocian. Thereafter the evolution of the family can be followed in great detail up to its equally abrupt extinction at the top of the Lower Kimmeridgian (sensu onglico). Over a hundred successive assemblages have been recognized, spanning some four and a half stages, twenty-eight standard ammonite zones and sixty-two subzones, equivalent on average to time-intervals of perhaps 250,000 years. Material at most levels is sufficiently abundant to delineate intraspecific variability and dimorphism. Both vary with time and can be very large. They point strongly to an important conclusion, that the assemblages found at any one level and place are monospecific. Morphological overlap between successive assemblages then identifies phyletic lineages. Evolution was on the whole gradualistic, with noise, although the principal lineage can be seen to have undergone phylogenetic division at least twice, followed by a major geographic migration of one or both branches. At other times, considerable mierations. which could be eeologicallv tns~antancous,did not lead to phylogenetic rpeciation. Thc habxtat 07 the famtly remaned broadly 'Horeil thro~phout,local endemlsmr hrinz infrequent and short-livcd Mot~holoeicall\,- .~the family evolved through almost the complete spectrum ofcoiling and sculpture to be found in ammonites as a whole, excluding heteromorphs. The nature of the selection-pressure, if any, remains totally obscure. -
MEDDELELSER OM GR0NLAND UDGIVNE AF KOMMISSIONEN for VIDENSKABELIGE UNDERS0GELSER I GR0NLAND Bd
MEDDELELSER OM GR0NLAND UDGIVNE AF KOMMISSIONEN FOR VIDENSKABELIGE UNDERS0GELSER I GR0NLAND Bd. 168 ■ N r. 3 AN ANNOTATED MAP OF THE PERMIAN AND MESOZOIC FORMATIONS OF EAST GREENLAND BY JOHN H. CALLOMON, DESMOND T. DONOVAN and RUDOLF TROMPY WITH 9 FIGURES IN THE TEXT, AND 1 MAP K0BENHAVN C. A. REITZELS FORLAG BIANCO LUNOS BOGTRYKKEHI A/S 1972 A map has been compiled on the scale of 1:1 million showing Permian and Mesozoic rocks of East Greenland from 70° to 77° north latitude. The accompanying text briefly summarizes the existing knowledge of these rocks. Lower Permian (not shown on the map) is represented by non-marine formations which lie conformably on Upper Carboniferous. Upper Permian lies unconformably on Lower Permian and earlier rocks with a basal conglomerate. The remaining Upper Permian rocks include marine strata with arich fauna. The lowest Triassic beds are marine with an abundant fauna which enables six ammonoid zones to be recognized. The rest of the Trias is almost entirely non marine, a mainly clastic redbed sequence with some evaporites. The Trias closes with deltaic beds with an abundant flora, which span the interval from Rhaetian to earliest Jurassic (Hettangian). The Jurassic succession is incomplete. The Middle Jurassic has yielded important ammonite faunas which make it a zonal standard for the boreal Jurassic, very differ ent from that of Europe. Upper Jurassic rocks, mainly Upper Oxfordian and Lower Kimmeridgian, are widespread. Still higher Jurassic rocks are preserved in Milne Land. Lowest Cretaceous (Berriasian and Yalanginian) rocks have yielded important faunas, which in the Valanginian include both North European and Mediterranean elements. -
The Upper Bajocian–Lower Bathonian Boundary Section in the Outskirts of Saratov: Molluscan Characteristics and Biostratigraphy V
ISSN 08695938, Stratigraphy and Geological Correlation, 2011, Vol. 19, No. 5, pp. 502–514. © Pleiades Publishing, Ltd., 2011. Original Russian Text © V.V. Mitta, V.A. Zakharov, I.S. Barskov, V.B. Sel’tser, A.V. Ivanov, 2011, published in Stratigrafiya Geologicheskaya Korrelyatsiya, 2011, Vol. 19, No. 5, pp. 32–45. The Upper Bajocian–Lower Bathonian Boundary Section in the Outskirts of Saratov: Molluscan Characteristics and Biostratigraphy V. V. Mittaa, V. A. Zakharovb, I. S. Barskova, V. B. Sel’tserc, and A. V. Ivanovc a Borissiak Paleontological Institute, Russian Academy of Sciences, Profsoyuznaya ul. 123, Moscow, 117647 Russia email: [email protected] b Geological Institute (GIN), Russian Academy of Sciences, Pyzhevskii per. 7, Moscow, 119017 Russia c Chernyshevskii Saratov State University, Astrakhanskaya ul. 83, Saratov. 410012 Saratov Received February 4, 2011; in final form April 13, 2011 Abstract—The analysis of all available data on the structure of the Bajocian–Bathonian boundary section in the outskirts of Saratov (Sokur quarry) and the taxonomic composition of its ammonites, belemnites, and bivalves revealed a continuous succession of the Pseudocosmoceras michalskii (Upper Bajocian), Oraniceras besnosovi, and Arcticoceras ishmae (Lower Bathonian) zones. In connection with the critique by Meledina et al. (2009), correlation of Bajocian and Bathonian boundary strata of the Central Russia and Northern Siberia is discussed. The inconsistency of Siberian bivalve and belemnite assemblages with Central Russian ammonite zones is explained by heterochronous invasions of different molluscan groups. Keywords: Saratov Volga region, ammonites, Bajocian, Bathonian, biostratigraphy, zones, Boreal–Tethyan correlation. DOI: 10.1134/S086959381105008X INTRODUCTION sediments in the Saratov–Volgograd region (Lower Volga River). -
Paleontological Contributions
THE UNIVERSITY OF KANSAS PALEONTOLOGICAL CONTRIBUTIONS May 15, 1970 Paper 47 SIGNIFICANCE OF SUTURES IN PHYLOGENY OF AMMONOIDEA JURGEN KULLMANN AND JOST WIEDMANN Universinit Tubingen, Germany ABSTRACT Because of their complex structure ammonoid sutures offer best possibilities for the recognition of homologies. Sutures comprise a set of individual elements, which may be changed during the course of ontogeny and phylogeny as a result of heterotopy, hetero- morphy, and heterochrony. By means of a morphogenetic symbol terminology, sutural formulas may be established which show the composition of adult sutures as well as their ontogenetic development. WEDEKIND ' S terminology system is preferred because it is the oldest and morphogenetically the most consequent, whereas RUZHENTSEV ' S system seems to be inadequate because of its usage of different symbols for homologous elements. WEDEKIND ' S system includes only five symbols: E (for external lobe), L (for lateral lobe), I (for internal lobe), A (for adventitious lobe), U (for umbilical lobe). Investigations on ontogenetic development show that all taxonomic groups of the entire superorder Ammonoidea can be compared one with another by means of their sutural development, expressed by their sutural formulas. Most of the higher and many of the lower taxa can be solely characterized and arranged in phylogenetic relationship by use of their sutural formulas. INTRODUCTION Today very few ammonoid workers doubt the (e.g., conch shape, sculpture, growth lines) rep- importance of sutures as indication of ammonoid resent less complicated structures; therefore, phylogeny. The considerable advances in our numerous homeomorphs restrict the usefulness of knowledge of ammonoid evolution during recent these features for phylogenetic investigations. -
Geological Survey Canada
GEOLOGICAL BULLETIN 74 SURVEY 1 p OF CANADA DEPARTMENT OF MINES AND TECHNICAL SURVEYS THE JURASSIC FAUNAS OF THE CANADIAN ARCTIC MIDDLE AND UPPER JURASSIC AMMONITES Hans Frebold 5" Price, $2.00 1961 THE JURASSIC FAUNAS OF THE CANADIAN ARCTIC Middle and Upper Jurassic Ammonites 3,000—1960—1789 89772-8—li GEOLOGICAL SURVEY OF CANADA BULLETIN 74 THE JURASSIC FAUNAS OF THE CANADIAN ARCTIC MIDDLE AND UPPER JURASSIC AMMONITES By Hans Frebold DEPARTMENT OF MINES AND TECHNICAL SURVEYS CANADA ROGER DUHAMEL, F.R.S.C. QUEEN'S PRINTER AND CONTROLLER OF STATIONERY OTTAWA, 1961 Price $2.00 Cat. No. M42-74 PREFACE This report is based on fossil collections made over a vast area of the Canadian Arctic extending from Ellesmere Island in the north to the Aklavik region of the mainland. Detailed study of these ammonite faunas permits correla tion of the associated Jurassic rocks and shows their faunal and stratigraphic relationships with East Greenland and Siberia. J. M. HARRISON, Director, Geological Survey of Canada OTTAWA, June 22, 1960 CONTENTS PAGE Introduction 1 Fossil localities 2 Richardson and British Mountains region 2 Canadian Arctic islands 3 Description of ammonites 5 Age and correlation 25 The zoogeographical position of the Middle and Upper Jurassic ammonite faunas of the Canadian Arctic 32 The time of the manifestation of the Jurassic boreal realm 35 The Arctic seas in Middle and Late Jurassic times 37 References 41 Table I. Correlation chart of the Middle and Upper Jurassic of the Canadian Arctic with other Arctic regions Facing p. 26 Illustrations Plates I—XXI.