Bulletin of the British Museum (Natural History), Geology

Total Page:16

File Type:pdf, Size:1020Kb

Bulletin of the British Museum (Natural History), Geology *-i-S3 Bulletin of the British Museum (Natural History) Geology series Vol 31 1979 British Museum (Natural History) London 1979 Dates of publication of the parts 29 March 1979 No j 29 March 1979 No 2 No3 26 April 1979 No4 31 May 1979 ISSN 0007-1471 Press, Dorchester, Dorset Printed in Great Britain by Henry Ling Ltd, at the Dorset Contents Geology Volume 31 Page No 1 Foraminifera of the Togopi Formation, eastern Sabah, Malaysia. J. E. Whittaker & R. L. Hodgkinson 1 No 2 Cretaceous faunas from Zululand and Natal, South Africa. The ammonite family Gaudryceratidae. W. J. Kennedy & H. C. Klinger 121 No 3 Benthic community organization in the Ludlow Series of the Welsh Borderland. R. Watkins 175 No 4 The ammonites of the English Chalk Rock (Upper Turonian). C. W. Wright 281 _> |o v" - \^ Bulletin of the British Museum (Natural History) Foraminifera of the Togopi Formation, eastern Sabah, Malaysia J. E. Whittaker & R. L. Hodgkinson Geology series Vol 31 No 1 29 March 1979 is issued in four The Bulletin of the British Museum (Natural History), instituted in 1949, Mineralogy) and Zoology, and scientific series, Botany, Entomology, Geology (incorporating an Historical series. will contain about Parts are published at irregular intervals as they become ready. Volumes calendar year. three hundred pages, and will not necessarily be completed within one Subscription orders and enquiries about back issues should be sent to: Publications Sales, England. British Museum (Natural History), Cromwell Road, London SW7 5BD, World List abbreviation: Bull. Br. Mus. nat. Hist. (Geol.) Trustees of the British Museum (Natural History), 1979 ISSN 0007-1471 Geology series Vol 31 No 1 pp 1-120 British Museum (Natural History) Cromwell Road London SW7 5BD Issued 29 March 1979 Foraminifera of the Togopi Formation, eastern Sabah, Malaysia J. E. Whittaker and R. L. Hodgkinson Department of Palaeontology, British Museum (Natural History), Cromwell Road, London SW7 5BD Contents Synopsis 3 Introduction ............ 3 Acknowledgements ........... 4 Methods ............. 4 Biostratigraphy ............ 5 Stratigraphy of the Dent Group 5 Sebahat Formation .......... 5 Ganduman Formation .......... 5 Togopi Formation ........... 5 Distribution and palaeoecology of the Togopi Foraminifera .... 8 Age of the Togopi Formation ......... 9 Planktonic foraminifera .......... 9 Benthic foraminifera .......... 9 Systematics ............. 14 Family Ataxophragmiidae Schwager ........ 15 Textilina Norvang ........... 15 Clavulina d'Orbigny .......... 16 Family Nubeculariidae Jones ......... 16 Edentostomina Collins .......... 16 Spiroloculina d'Orbigny .......... 17 Vertebralina d'Orbigny .......... 19 Family Miliolidae Ehrenberg ......... 20 Quinqueloculina d'Orbigny ......... 20 Pseudomassilina Lacroix .......... 31 Pyrgo Defrance ........... 33 Triloculina d'Orbigny .......... 34 Miliolinella Wiesner .......... 37 Hauerina d'Orbigny in de la Sagra ........ 37 Schlumbergerina Munier-Chalmas ........ 40 Family Soritidae Ehrenberg 41 Peneroplis de Montfort .......... 41 Dendritina d'Orbigny .......... 41 Marginopora de Blainville ......... 42 Family Alveolinidae Ehrenberg 42 Alveolinella Douville .......... 42 Family Nodosariidae Ehrenberg 43 Lagena Walker & Jacob in Kanmacher 43 Pseudonodosaria Boomgaart ......... 48 Family Polymorphinidae d'Orbigny 49 Guttulina d'Orbigny .......... 49 Sigmoidella Cushman & Ozawa ........ 50 Family Glandulinidae Reuss 51 Glandulina d'Orbigny in de la Sagra ........ 51 Oolina d'Orbigny ........... 52 Fissurina Reuss ........... 52 Bull. Br. Mus. nat. Hist. (Geol.) 31 (1): 1-120 Issued 29 March, 1979 J. E. WHITTAKER & R. L. HODGKINSON Family Bolivinitidae Cushman 54 Bolivina d'Orbigny 54 Brizalina Costa ........... 55 Rectobolivina Cushman 56 Family Buliminidae Jones .......... 57 Pavonina d'Orbigny 57 Chrysalidinella Schubert 57 Reussella Galloway 58 Family Uvigerinidae Haeckel ......... 58 Siphogenerina Schlumberger in Milne-Edwards 58 Siphouvigerina Parr 58 Family Discorbidae Ehrenberg 59 Discorbis Lamarck 59 Gavelinopsis Hofker .......... 59 Rosalina d'Orbigny 59 Cancris de Montfort .......... 62 Family Glabratellidae Loeblich & Tappan 63 Schackoinella Weinhandl 63 Family Siphoninidae Cushman 64 Siphoninoides Cushman .......... 64 Family Epistomariidae Hofker ......... 64 Epistomaroides Uchio .......... 64 Pseudoeponides Uchio in Kawai et al. ...... 65 Family Rotaliidae Ehrenberg ......... 66 Ammonia Brunnich .......... 66 Asterorotalia Hofker .......... 72 Pararotalia Le Calvez 76 Pseudorotalia Reiss & Merling ......... 78 Family Calcarinidae Schwager ......... 81 Calcarina d'Orbigny .......... 81 Family Elphidiidae Galloway 81 Elphidium de Montfort . 81 Cellanthus de Montfort 82 Cribroelphidium Cushman & Bronnimann ....... 85 Cribrononion Thalmann .......... 86 Elphidiella Cushman .......... 87 Parrellina Thalmann 88 Family Nummulitidae de Blainville ........ 88 Nummulites Lamarck . 88 Operculina d'Orbigny 89 Heterostegina d'Orbigny .......... 95 Family Hantkeninidae Cushman 95 Hastigerina Thomson in Murray 95 Family Globigerinidae Carpenter, Parker & Jones 96 Globigerina d'Orbigny 96 Globigerinoides Cushman ......... 98 Globigerinita Bronnimann ......... 98 Family Eponididae Hofker 99 Poroeponides Cushman .......... 99 Family Amphisteginidae Cushman 100 Amphistegina d'Orbigny . .100 Family Cibicididae Cushman ......... 100 Caribeanella Bermudez 100 Family Planorbulinidae Schwager ........ 101 Planorbulinella Cushman 101 Family Acervulinidae Schultze ......... 102 Gypsina Carter ........... 102 Family Cymbaloporidae Cushman 102 Cymbaloporetta Cushman . 102 FORAMINIFERA OF THE TOGOPI FORMATION Family Nonionidae Schultze 104 Florilus de Montfort 104 Family Anomalinidae Cushman 105 Anomalinoides Brotzen 105 Hanzawaia Asano . 106 Postscript . 106 References . 107 Index 116 Synopsis One hundred and twenty-five species are described and figured from a section in the upper Togopi River, type-locality of the Togopi Formation, eastern Sabah, Malaysia. Eighty-six per cent of the fauna is living today in the area. The following seven species and one variety are new: Ammonia togopiensis, Bolivina sabahensis, Cellanthus biperforatus, C. hailei, Chbroelphidium dentense, Peneroplis planatus var. annulata, Pseudomassilina medioelata and Textilina subrectangularis. Florilus asanoi is proposed as a new name for Nonion japonicum Asano, 1938. The age of the Togopi Formation is reassessed on the basis of benthic foraminifera and is considered to be mainly of Pliocene age. Introduction The Togopi Formation, the uppermost sequence of mainly marine clays making up the Dent Group, is named after the Togopi River, eastern Sabah, Malaysia. The name was first published by Reinhard & Wenk (1951) but it had previously been used in a Sabah Shell Petroleum Company's (SSPC) internal report as early as 1938. Dr E. Wenk himself made the first collection of fossils (Mollusca) in 1937, some of which were described by Cox (1948). A further collection of macro- fossils was made by P. Collenette in 1950, the Mollusca being listed by Nuttall (1960). Cox dated Wenk's material, which was dominated by gastropods, as Pliocene or possibly U. Miocene, while Nuttall considered Collenette's samples to be almost certainly Pleistocene. The former collection came from the Togopi River, but there is some confusion as to the exact provenance of Collenette's (Nuttall 1965). In 1961 Dr N. S. Haile collected 18 samples from the type area for the Togopi Formation from its supposed boundary with the underlying Ganduman Formation to where it disappears under the coastal alluvia (for details see Haile & Wong 1965). From these Nuttall (1965) listed almost 200 species of Mollusca and after a detailed examination of the fauna assigned a Plio-Pleistocene age, equivalent to the Bantamian-Sondian stages of Java, to the Togopi Formation. Haile & Wong (1965 : 83) list identifications of teleostan otoliths by F. Stinton (Stinton 1963) and echino- derms by R. P. S. Jefferies together with a small foraminiferal fauna, identified by SSPC palaeon- tologists. The foraminifera came from samples collected by Wenk and Parsons between 4 and 13 km west and north-west of Dent Haven, but only a few genera and species were recognized. Eleven of Haile's original samples were available for micropalaeontological examination, and in view of the richness of the fauna (125 species) it was decided to describe it fully and to attempt an age determination using the smaller benthic foraminifera. Planktonic foraminifera are un- fortunately few in the Togopi Formation. Since 86% of the fauna still lives in the Indo-Pacific today it has also been possible to correct some common misidentifications of Recent species by referring back to the original collections of Brady, Parker & Jones, Carpenter, Williamson and Heron-Allen & Earland which are preserved in the BM(NH). A number of benthic species are now thought to be extinct and these are listed as of possible biostratigraphic use in the future. Four samples from the small Wenk and Collenette collections have been examined for foramini- fera but yielded no additional species. They are not dealt with any further in this paper. The stratigraphy of the Dent Group is first discussed. The ages of the Sebahat and Ganduman Formations given by Haile & Wong (1965) are revised and the foraminiferal faunas reinterpreted in the light of recent advances in Tertiary biostratigraphy. A description of the Togopi strati- graphy and the material from the type-area which forms the basis of this work
Recommended publications
  • APPLICATIONS of QUANTITATIVE METHODS and CHAOS THEORY in ICHNOLOGY for ANALYSIS of INVERTEBRATE BEHAVIOR and EVOLUTION by James
    APPLICATIONS OF QUANTITATIVE METHODS AND CHAOS THEORY IN ICHNOLOGY FOR ANALYSIS OF INVERTEBRATE BEHAVIOR AND EVOLUTION by James Richard Woodson Lehane A dissertation submitted to the faculty of The University of Utah in partial fulfillment of the requirements for the degree of Doctor of Philosophy in Geology Department of Geology and Geophysics The University of Utah August 2014 Copyright © James Richard Woodson Lehane 2014 All Rights Reserved The University of Utah Graduate School STATEMENT OF DISSERTATION APPROVAL The dissertation of James Richard Woodson Lehane has been approved by the following supervisory committee members: Allan A. Ekdale , Chair May 5th, 2014 Date Approved Randall B. Irmis , Member June 6th, 2014 Date Approved Marjorie A. Chan , Member May 5th, 2014 Date Approved Elena A. Cherkaev , Member June 12th, 2014 Date Approved Leif Tapanila , Member June 6th, 2014 Date Approved and by John M. Bartley , Chair/Dean of the Department/College/School of Geology and Geophysics and by David B. Kieda, Dean of The Graduate School. ABSTRACT Trace fossils are the result of animal behaviors, such as burrowing and feeding, recorded in the rock record. Previous research has been mainly on the systematic description of trace fossils and their paleoenvironmental implications, not how animal behaviors have evolved. This study analyzes behavioral evolution using the quantification of a group of trace fossils, termed graphoglyptids. Graphoglyptids are deep marine trace fossils, typically found preserved as casts on the bottom of turbidite beds. The analytical techniques performed on the graphoglyptids include calculating fractal dimension, branching angles, and tortuosity, among other analyses, for each individual trace fossil and were performed on over 400 trace fossils, ranging from the Cambrian to the modem.
    [Show full text]
  • Cretaceous Ammonites from the Lower Part of the Matanuska Formation Southern Alaska
    Cretaceous Ammonites From the Lower Part of The Matanuska Formation Southern Alaska By DAVID L. JONES With a STRATIGRAPHIC SUMMARY By ARTHUR GRANT2 GEOLOGICAL SURVEY PROFESSIONAL PAPER 547 UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1967 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director Library of Congress catalog-card No. GS 66-286 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price $1.25 (paper cover) CONTENTS Page Abstract-----------__-------------------------------- 1 Stratigraphic summary of the lower part of the Matanuska Introduction--------------------------------------- 1 Formation-Continued Mid-Cretaceous faunal sequence in southern Alaska- - - - .. 2 Unit B, sandstone of Cenomanian age-- _---------- 3 Unit C, strata of Cenomanian to Santonian(?) age--- Cenomanian - - - - - - _ - - - - - - - - - - - - - - - - - - - - - - - - - - - - 4 Unit Gl, lutite of Cenomanian to Coniacian or Stratigraphic summary of the lower part of the Matanuska Santonian age-____----------------------- Formation, by Arthur Grants -------_______--------- Unit G2, composite sequence of Coniacian and Unit A, strata of Albian age ...................... Santonian(?) age .......................... Limestone Hills area- - ----____-------------- Regional correlation of the lower part of the Matanuska North front of the Chugach Mountains--- - - - - - Forrnation_____---------------------------------- Matanuska Valley---------_-____---------
    [Show full text]
  • Paleofloristic and Paleoenvironmental Information from a Late Cretaceous
    Palaeogeography, Palaeoclimatology, Palaeoecology 295 (2010) 389–408 Contents lists available at ScienceDirect Palaeogeography, Palaeoclimatology, Palaeoecology journal homepage: www.elsevier.com/locate/palaeo Paleofloristic and paleoenvironmental information from a Late Cretaceous (Maastrichtian) flora of the lower Cantwell Formation near Sable Mountain, Denali National Park, Alaska Carla Susanne Tomsich a,⁎, Paul J. McCarthy a, Sarah J. Fowell a, David Sunderlin b a University of Alaska, Dept. of Geology and Geophysics, P.O. Box 755780, Fairbanks, AK 99775-5780, United States b Lafayette College, Dept. of Geology and Environmental Geosciences, Easton, PA 18042-1768, United States article info abstract Article history: The lower Cantwell Formation in Denali National Park, Alaska, is a Late Cretaceous high-latitude fluvial succession Received 28 June 2009 that contains dinosaur and bird footprints, diverse invertebrate traces, and plant fossils. New fossil discoveries Received in revised form 21 January 2010 and stratigraphic descriptions in the Sable Mountain area allow for refined paleoenvironmental reconstructions Accepted 18 February 2010 and age interpretations. The formation consists of well-indurated conglomerate, sandstone, siltstone, and shale Available online 24 February 2010 interpreted as gravelly and sandy channel, levee, crevasse splay, sheetflood, lacustrine, and floodplain sediments with interspersed debris flows. The overall depositional environment is interpreted as a braided river floodplain Keywords: that interfingered with distal alluvial fan sedimentation. Plant fossils include leaves, branches, cones and rare Late Cretaceous Lower Cantwell Formation seeds of taxodiaceous and other conifer taxa, fern fronds, rhizomes and stem segments of Equisetites,linearand High-latitude paleoenvironments broad-lanceolate monocot leaf fragments, cf. Kenella, and impressions of diverse angiosperm broad-leaf Paleobotany morphotypes likely belonging to menispermoid, platanoid and several Late Cretaceous hamamelid groups.
    [Show full text]
  • THE BIBLIOGRAPHY of HADROSAURIAN DINOSAURS the First 150 Years: 1856 - 2006
    THE BIBLIOGRAPHY OF HADROSAURIAN DINOSAURS The First 150 Years: 1856 - 2006. complied by M.K. Brett-Surman © Smithsonian Institution 1985-2008 The Department of Paleobiology of the National Museum of Natural History, Smithsonian Institution, currently houses approximately 44 million fossil plant, invertebrate, and vertebrate fossils in more than 480 separate collections. In addition, Paleobiology also maintains a reference collection of over 120,000 stratigraphic and sediment samples. This listing represents a service provided to the public as part of our Outreach Program and as part of the Smithsonian Institution’s mission "for the increase and diffusion of knowledge...". Papers are listed by author and year. Author's names are capitalized. The viewer should be aware of any searches that are case sensitive. The papers listed here, in a majority of instances, do NOT contain abstracts, papers on ichnites, or popular articles or books, unless they present new information or cover an aspect of the history of dinosaur paleontology. At present, some of the legacy software that was used to maintain this list only allowed basic ASCII characters, therefore foreign accents (such as in French and Spanish) did not translate. This will be fixed at a later date. The Bibliography of Hadrosaurian Dinosaurs was written, compiled, and maintained by M.K. Brett-Surman, (Museum Specialist), P.O. Box 37012, Department of Paleobiology, National Museum of Natural History, MRC-121, Washington, DC 20013-7012. He can be reached electronically at: [email protected]., and by FAX at 202-786-2832. Please send all corrections and additions to the e-mail address. This file will be no longer be updated, except for entries prior to 2007.
    [Show full text]
  • Synoptic Taxonomy of Major Fossil Groups
    APPENDIX Synoptic Taxonomy of Major Fossil Groups Important fossil taxa are listed down to the lowest practical taxonomic level; in most cases, this will be the ordinal or subordinallevel. Abbreviated stratigraphic units in parentheses (e.g., UCamb-Ree) indicate maximum range known for the group; units followed by question marks are isolated occurrences followed generally by an interval with no known representatives. Taxa with ranges to "Ree" are extant. Data are extracted principally from Harland et al. (1967), Moore et al. (1956 et seq.), Sepkoski (1982), Romer (1966), Colbert (1980), Moy-Thomas and Miles (1971), Taylor (1981), and Brasier (1980). KINGDOM MONERA Class Ciliata (cont.) Order Spirotrichia (Tintinnida) (UOrd-Rec) DIVISION CYANOPHYTA ?Class [mertae sedis Order Chitinozoa (Proterozoic?, LOrd-UDev) Class Cyanophyceae Class Actinopoda Order Chroococcales (Archean-Rec) Subclass Radiolaria Order Nostocales (Archean-Ree) Order Polycystina Order Spongiostromales (Archean-Ree) Suborder Spumellaria (MCamb-Rec) Order Stigonematales (LDev-Rec) Suborder Nasselaria (Dev-Ree) Three minor orders KINGDOM ANIMALIA KINGDOM PROTISTA PHYLUM PORIFERA PHYLUM PROTOZOA Class Hexactinellida Order Amphidiscophora (Miss-Ree) Class Rhizopodea Order Hexactinosida (MTrias-Rec) Order Foraminiferida* Order Lyssacinosida (LCamb-Rec) Suborder Allogromiina (UCamb-Ree) Order Lychniscosida (UTrias-Rec) Suborder Textulariina (LCamb-Ree) Class Demospongia Suborder Fusulinina (Ord-Perm) Order Monaxonida (MCamb-Ree) Suborder Miliolina (Sil-Ree) Order Lithistida
    [Show full text]
  • Contributions in Science, 523:37–65 21 August 2015
    Contributions in Science, 523:37–65 21 August 2015 PACIFIC SLOPE OF NORTH AMERICA RECORD OF THE CRETACEOUS APORRHAID GASTROPOD TESSAROLAX:EVOLUTIONARY TRENDS, MODE OF LIFE, AND PALEOBIOGEOGRAPHY OF THE GENUS1 LOUELLA R. SAUL2 AND RICHARD L. SQUIRES3 ABSTRACT. The Cretaceous aporrhaid Tessarolax Gabb, 1864, is a widespread but uncommon marine gastropod whose mature shell is very distinctive with four long and narrow digitations. Its most species-rich record is from the Pacific slope of North America (PSNA), where it has been found from southern Alaska to northern Baja California, Mexico. Its longest geologic range (late Hauterivian to early late Maastrichtian) occurs in the PSNA and is represented by 10 species, five of them new: Tessarolax alaskana, late Turonian to early Coniacian; Tessarolax bullardi, middle Coniacian to early Campanian; Tessarolax grahami, early Campanian; Tessarolax louellae, middle late Campanian; and Tessarolax teleos, ‘‘mid’’ Maastrichtian. Nondigitate immature specimens of Tessarolax were infaunal, whereas digitate mature specimens were epifaunal. In maturity, shells also developed a callus coat, partial in Early Cretaceous and becoming overall by Late Cretaceous. Through time, part of the mature ventral surface thickened into a projecting stabilizer (herein newly termed ‘‘fictavarix’’), and other distinctive callus structures developed dorsally and ventrally on the shell. Some exceptional specimens provide three-dimensional views of fragile projecting features, thereby allowing for the first insights as to mode of life. In the PSNA region, specimens are most common in fine-grained offshore (outer sublittoral) siliciclastics, where warm-temperate waters were deeper/calmer and slightly cooler relative to more nearshore environments. Tessarolax gabbi new name is provided for Helicaulax bicarinata Gabb, 1869, a junior secondary homonym of Tessarolax bicarinata (Deshayes in Leymerie, 1842).
    [Show full text]
  • Tertiary Stratigraphy and Paleobotany of the Cook Inlet Region, Alaska
    Tertiary Stratigraphy and Paleobotany of the Cook Inlet Region, Alaska By JACK A. WOLFE, D. M. HOPKINS, and ESTELLA B. LEOPOLD TERTIARY BIOSTRATIGRAPHY OF THE COOK INLET REGION, ALASKA GEOLOGICAL SURVEY PROFESSIONAL PAPER 398-A Discussion of stratigraphic signrJicance of fossil plants from the Chichaloon, Kenai, and TsadzKa Formations Property of District Library Alaska District UNITED STATES GOVERNMENT PRINTING OFFICE. WASHINGTON : 1966 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price 70 cents (paper cover) CONTENTS Abstract--,---------------------------------------- Geology-Continued Introduction,-------------------------------------- Neogene stratigraphy-Continued Previous geologic studies......................... Kenai and Tsadaka Formations-Continued Acknowledgments----- - - - - - - - - - - - - - - - - - - - - - - - - - - Provincial stages-Continued Evolution of stratigraphic nomenclature and age assign- Seldovian Stage-Continued ments------------------------------------------- Mollusks-- - - - - - - .- - - - - - - - - - - - - - Age ------------..-------------- Gwlogy------------------------------------------- Homerian Stage-, - --- - - - - - - - - - - - -- - Paleogene stratigraphy .......................... Definition ---,-- - - - - - - - - - - - - - - - - Chickaloon Formation -,,----- ------ ---- --- -- Flora andage-------------------------- Fresh-water mollusks-----,---
    [Show full text]
  • SQUIRES—PACIFIC CRETACEOUS PALEOCENE BIVALVES 913 Gyrodes and Biplica Are the Only Gastropods Commonly Found (Squires, 2003)
    SQUIRES—PACIFIC CRETACEOUS PALEOCENE BIVALVES 913 Gyrodes and Biplica are the only gastropods commonly found (Squires, 2003). These paleoclimates are in keeping with the in abundance in these assemblages. Saul and Popenoe (1962, climatic conditions of modern glycymeridids, which are mostly p. 323) suggested a shallow (7-40 m) water depth for these restricted to tropical and temperate waters, but, at least one assemblages, and Saul (1973) reported that they inhabited species extends into boreal waters (Matsukuma, 1986; Coan et inner sublittoral, current-disturbed, muddy sand substrates. al., 2000). The late Paleocene Glycymerita major is found with common to abundant shallow-marine bivalves (e.g., Crassatella, Vener- PALEOBIOGEOGRAPHY OF THE STUDIED GLYCYMERIDIDS icardia) and common to abundant shallow-marine gastropods Saul (1986, fig. 1) depicted the relative-ocean temperatures (e.g., Turritella). and the global cycles of sea-level changes for the northeast The shallow-marine paleoenvironment of the studied species Pacific area during the Cretaceous. A warming trend and the is in keeping with the environment of modern glycymeridids. high sea-level stand during the Turonian help explain the first Modern species burrow in sand and other sediments with large occurrence of glycymeridids and the widespread distribution particles (Coan et al., 2000). They never live in brackish waters of Glycymeris pacifica in the study area during that time. The or in deep oceans. They are suspension feeders with large Coniacian and Santonian were cooler and associated with filibranch gills. Lacking siphons, their shells are normally just lower sea levels, thus probably accounting for the restriction covered by the sediment, with their posterior-ventral margin of Glycymerita veatchii to just northern California during this exposed at the sediment surface.
    [Show full text]
  • Professional Paper 1760F
    Studies by the U.S. Geological Survey in Alaska, 2007 Detrital Zircon Geochronology of Cretaceous and Paleogene Strata Across the South-Central Alaskan Convergent Margin Professional Paper 1760–F U.S. Department of the Interior U.S. Geological Survey This page intentionally left blank Studies by the U.S. Geological Survey in Alaska, 2007 Detrital Zircon Geochronology of Cretaceous and Paleogene Strata Across the South-Central Alaskan Convergent Margin By Dwight Bradley, Peter Haeussler, Paul O’Sullivan, Rich Friedman, Alison Till, Dan Bradley, and Jeff Trop Professional Paper 1760–F U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Suzette M. Kimball, Acting Director U.S. Geological Survey, Reston, Virginia: 2009 This report and any updates to it are available online at: http://pubs.usgs.gov/pp/1760/f/ For more information about the USGS and its products: Telephone: 1–888–ASK–USGS (1-888-275-8747) World Wide Web: http://www.usgs.gov/ Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, it may contain copyrighted materials that are noted in the text. Permission to reproduce those items must be secured from the individual copyright owners. Produced in the Western Region, Menlo Park, California Manuscript approved for publication, August 20, 2009 Text edited by Peter H. Stauffer Layout and design by Stephen L. Scott Suggested citation: Bradley, D., Haeussler, P., O’Sullivan, P., Friedman, R., Till, A., Bradley, D., and Trop, J., 2009, Detrital zircon geochronol- ogy of Cretaceous and Paleogene strata across the south-central Alaskan convergent margin, in Haeussler, P.J., and Galloway, J.P., Studies by the U.S.
    [Show full text]
  • Zakharov, Y. D., Y. Shigeta, A. Popov, T. A. Velivetskaya & T. Afanasyeva
    Author's personal copy Sedimentary Geology 235 (2011) 122–131 Contents lists available at ScienceDirect Sedimentary Geology journal homepage: www.elsevier.com/locate/sedgeo Cretaceous climatic oscillations in the Bering area (Alaska and Koryak Upland): Isotopic and palaeontological evidence Yuri D. Zakharov a,⁎, Yasunari Shigeta b, Alexander M. Popov a, Tatiana A. Velivetskaya a, Tamara B. Afanasyeva a a Far Eastern Geological Institute, Far Eastern Branch, Russian Academy of Sciences, Stoletiya Prospect 159, Vladivostok, 690022, Russia b Department of Geology, National Museum of Nature and Science, 3-23-1 Hyakunincho, Shinjuku-ku, Tokyo 169-0073, Japan article info abstract Article history: New isotopic palaeotemperatures, estimated from δ18O values of Early Albian, latest Campanian and Early Received 17 April 2009 Maastrichtian ammonoid shells of Southern Alaska, as well as our previously published data on the Received in revised form 5 March 2010 Cretaceous of the Koryak Upland, have been used to reconstruct palaeonvironmental changes in the Bering Accepted 19 March 2010 area. Significant seasonal contrast, marked in Alaska and the adjacent area during the Early Albian, as well as Available online 9 April 2010 the Coniacian, was partly connected apparently with the possible penetration of cooler waters from the polar area via the Strait of Alaska. Data suggest that the Bering Land Bridge existed during the post-Aptian Keywords: Cretaceous, with the exception of the Early Albian and Coniacian. Both the stable isotope and the floral data Cretaceous Isotopes on the post-Aptian Cretaceous of the Bering area suggest the existence of warm climatic conditions in the Palaeotemperatures Late Albian, latest Cenomanian, Coniacian, Santonian to Early Campanian, latest Campanian, and also late Palaeogeography Early Maastrichtian.
    [Show full text]
  • Information to Users
    Evidence For A Northern Transitional Continental Margin Flora In The Cretaceous (Campanian To Maastrichtian) Matanuska Formation, Talkeetna Mountains, Southcentral Alaska Item Type Thesis Authors Reid, Sabra Louise Download date 09/10/2021 10:03:13 Link to Item http://hdl.handle.net/11122/8942 INFORMATION TO USERS This manuscript has been reproduced from the microfilm master. UMI films the text directly from the original or copy submitted. Thus, some thesis and dissertation copies are in typewriter face, while others may be from any type of computer printer. The quality of this reproduction is dependent upon the quality of the copy submitted. Broken or indistinct print, colored or poor quality illustrations and photographs, print bleedthrough, substandard margins, and improper alignment can adversely affect reproduction. In the unlikely event that the author did not send UMI a complete manuscript and there are missing pages, these will be noted. Also, if unauthorized copyright material had to be removed, a note will indicate the deletion. Oversize materials (e.g., maps, drawings, charts) are reproduced by sectioning the original, beginning at the upper left-hand corner and continuing from left to right in equal sections with small overlaps. ProQuest Information and Learning 300 North Zeeb Road, Ann Arbor, Ml 48106-1346 USA 800-521-0600 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. EVIDENCE FOR A NORTHERN TRANSITIONAL CONTINENTAL MARGIN FLORA IN THE CRETACEOUS (CAMPANIAN TO MAASTRICHTIAN) MATANUSKA FORMATION, TALKEETNA MOUNTAINS, SOUTHCENTRAL ALASKA A DISSERTATION Presented to the Faculty of the University of Alaska Fairbanks in Partial Fulfillment of the Requirements for the Degree of DOCTOR OF PHILOSOPHY by Sabra Louise Reid, B.S., M.L.A.
    [Show full text]
  • Cretaceous Ammonites from the Lower Part of the Matanuska Formation Southern Alaska
    Cretaceous Ammonites From the Lower Part of The Matanuska Formation Southern Alaska GEOLOGICAL SURVEY PROFESSIONAL PAPER 547 Cretaceous Ammonites From the Lower Part of The Matanuska Formation Southern Alaska By DAVID L. JONES With a STRATIGRAPHIC SUMMARY By ARTHUR GRANTZ GEOLOGICAL SURVEY PROFESSIONAL PAPER 547 UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1967 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director Library of Congress catalog-card No. GS 66-286 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price $1.25 (paper cover) CONTENTS Page Page Abstract_ ________________________________________ 1 Stratigraphic summary of the lower part of the Matanuska Introduction. ______________________________________ 1 Formation Continued Mid-Cretaceous faunal sequence in southern Alaska. 2 Unit B, sandstone of Cenomanian age_____________ 9 Albian _________________________________________ 3 Unit C, strata of Cenomanian to Santonian(?) age _ 10 Cenomanian_ __________________________________ 4 Unit C 1, lutite of Cenomanian to Coniacian or Stratigraphic summary of the lower part of the Matanuska Santonian age__-___________-__---_-_---__ 10 Formation, by Arthur Grantz______________________ 4 Unit C-2, composite sequence of Coniacian and Unit A, strata of Albian age____________________ 6 Santonian(?) age-_------_--_-_------------ 11 Limestone Hills area._______________________ 7 Regional correlation of the lower part of the Matanuska North front of the Chugach Mountains.------- 7 Formation _______________________________________ 12 Matanuska Valley______________________ 7 Geographic distribution of ammonites___-__--__----_-- 15 Nelchina area and southwest Copper River Systematic descriptions..---------------------------- 21 lowland__ __________________________ References--___--_--_-_-_--_-_---------_----------- 44 Correlation within the Matanuska Valley- Index.
    [Show full text]