Ammonites from Southern Alaska

Total Page:16

File Type:pdf, Size:1020Kb

Ammonites from Southern Alaska Early and Middle Bajocian (Middle Jurassic) Ammonites from Southern Alaska U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1322 Early and Middle Bajocian (Middle Jurassic) Ammonites from Southern Alaska By RALPH W.IMLAY U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1322 Studies of the early and middle Bajocian ammonites of southern Alaska provide close age determinations and correlations with Europe, Arctic Alaska, Arctic Canada, and the Pacific Coast region in general UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1984 DEPARTMENT OF THE INTERIOR WILLIAM P. CLARK, Secretary U .S. GEOLOGICAL SURVEY Dallas L. Peck, Director Library of Congress Cataloging in Publication Data Imlay, Ralph Willard, 1908- Early and middle Bajocian (Middle Jurassic) ammonites from southern Alaska. (Geological Survey professional paper ; 1322) Bibliography: p. Supt. of Docs. no.: I 19.16:1322 1. Ammonoidea. 2. Paleontology-Jurassic. 3. Paleontology-Alaska. I. Title. 11. Series. QE807.A51584 1984 564l.53 84-600032 For sale by the Distribution Branch, U.S. Geological Survey, 604 South Pickett Street, Alexandria, VA 22304 CONTENTS Pane Paae Abstract ............................................................................................... Systematic descriptions-Continued Introduction ........................................................................................ Family Hildoceratidae Hyatt. 1867-Continued 25 Biological analysis ........................................................................... Genus Asthenoceras Buckman. 1899 ..... Stratigraphic summary ................................................................. Genus Tmetoceras Buckman . 1892 ............................ 27 Wrangell Mountains ................................................................ Family Hammatoceratidae Buckman, 1887 ................... 27 27 Talkeetna Mountains ................................................................ Genus Hammatoceras Hyatt . 1867 ............................ West side of Cook Inlet ............................................................ Genus Erycitoides Westermann . 1964 ..................... 35 Puale Bay area on the Alaska Peninsula ............................ Family Sonniniidae Buckman. 1892 ............................... 35 Wide Bay area on the Alaska Peninsula ............................ Genus Sonninia Bayle. 1879 .................................... 35 Ages and correlations ..................................................................... Genus Fontannesia Buckman, 1902 ....................... 36 Wrangell Mountains ................................................................ Family Oppeliidae Bonavelli. 1894 ................................... 36 Talkeetna Mountains ................................................................ Genus Bradfordia Buckman. 1910 ............................ 36 West side. of Cook Inlet between Tuxedni Bay and Family Otoitidae Mascke, 1907 ......................................... 36 Iniskin Bay .......................................................................... Family Sphaeroceratidae Buckman, 1920 ...................... :I 7 Puale Bay area .......................................................................... Genus Chondroceras Mascke. 1907 ............................ :37 Wide Bay area ............................................................................ Family Stephanoceratidae Neumayr, 1875 ................... 37 Ammonite faunal setting ................................................................ Genus Normannites Munier-Chalmas, 1892 .............. ...37 Geographic distribution .................................................................. Genus Stephanoceras Wadgen, 1869 ............................ 111 Systematic descriptions .................................................................. Genus Teloceras Mascke. 1907 ..................................... 3.7 Family Hildoceratidae Hyatt. 1867 ...................................... References cited .......................................................................... 38 Genus Pseudolioceras Buckman. 1889 ........................ ILLUSTRATIONS [Plates are at back of report1 PLATE1 . Asthenoceras. Tmetoceras. Hammatoceras. Er~jcitoide.~. E . (Kialagi~ikrs).Bradfordin. and Otoites. 2 . Pseudolioceras. Sonninia. Fontannesia. Chondroceras. Normalrirites. Stephalzoceras (Skirroceras).and Trlocerns. Page FIGURE 1. Generalized index map of principal areas of outcrop of Bajocian marine rocks in southern Alaska: (1) Wrangell Mountains; (2) Talkeetna Mountains; (3) peninsula between Tuxedni Bay and Chinitna Bay; (4) Iniskin Peninsula; (5) Puale Bay; and (6) Wide Bay ......................................................................................................................... 2.7 . Detailed index maps of listed early and middle Bajocian ammonite localities in southern Alaska: 2 . In the Wrangell Mountains ............................................................................................................................................ 3 . In the Talkeetna Mountains ................................................................................................................................................. 4 . West side of Cook Inlet between Tuxedni Bay and Chinitna Bay .............................................................................. 5 . West of Cook Inlet on the Iniskin Peninsula ..................................................................................................................... 6 . Northeast of Puale Bay on the Alaska Peninsula .............................................................................................................. 7. At Wide Bay on the Alaska Peninsula ................................................................................................................................ 8-15 . Diagrams showing: 8 . Stratigraphic positions and correlations of Bajocian rocks in southern Alaska .................................................... 9 . Stratigraphic. .positions of some Bajocian ammonite localities west of Cook Inlet between Tuxedni Bay and Inlskln Bay ....................................................................................................................................................... 10. Stratigraphic positions of some Bajocian ammonite localities on the northeast side of Puale Bay on the Alaska Peninsula ......................................................................................................................................................... CONTENTS Page 11. Stratigraphic positions of some Bajocian ammonite localities near Wide Bay on the Alaska Peninsula .... 16 12. Stratigraphic and chronologic correlations of some early and middle Bajocian ammonites present in the Talkeetna Mountains with ammonites present in the Tuxedni Group west of Cook Inlet .................... 13. Stratigraphic and chronologic correlations of some early and middle Bajocian ammonites present along the west side of Cook Inlet between the Fitz Creek and Tuxedni Bay areas ....................................... 14. Stratigraphic and chronologic correlations of some early and middle Bajocian ammonites present near Wide Bay on the Alaska Peninsula ...................................................................................... 15. Correlations and comparisons of Bajocian ammonite faunas in southern Alaska ................................ TABLES Page TABLE1. Early and middle Bajocian (Middle Jurassic) ammonite genera and subgenera in southern Alaska showing biological relationships and relative numbers available for study ................................................................................................ 2. Geographic distribution of early and middle Bajocian ammonites in the Wrangell and Talkeetna Mountains ................ 3. Geographic distribution of early and middle Bajocian ammonites west of Cook Inlet and northeast of Puale Bay on the Alaska Peninsula ...................................................................................................................................................................... 4. Geographic distribution of early and middle Bajocian ammonites near Wide Bay on the Alaska Peninsula .................... 5. Descriptions of middle and Io\ver Bajocian fossil localities in southern Alaska ........................................................ EARLY AND MIDDLE BA JOCIAN (MIDDLE JURASSIC) AMMONITES FROM SOUTHERN ALASKA ABSTRACT were described by the writer in 1964 and by Gerd Westerman in 1964 and 1969 (figs. 1-7). 'The writer at Early and middle Bajocian (Middle Jurassic) ammonites have that time dealt mainly with ammonites collected either been found in six areas in southern Alaska over a distance of about northwest of Cook Inlet between Tuxedni Bay and 500 mi (800 km) from the Wrangell Mountains on the east to the Wide Bay areaof the AlaskaPeninsulaon the west. In the Wrangell Iniskin Bay or in the eastern part of the Nelchina area Mountains, some float obtained near the base of the Nizina Moun- of the Talkeetna Mountains. Gerd Westermann at tain Formation has furnished the ammonites Chondrororrrs. .Vor- those times dealt mainly with ammonites of late early )~rn)r~titp.s,and TrlocPrers,which constitute good evidence for a late to early middle Bajocian age that had been collected middle Bajocian age not older than the upper part of the Stfl)il~n~ro- cc,~,tr.shrtrrrpkrresic~~~rtmm zone. near Wide Bay on the Alaska Peninsula. Most of those In the
Recommended publications
  • 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.
    [Show full text]
  • Geology, Fossils and Mapperton
    GEOLOGY, FOSSILS AND ROCKWATCH MAPPERTON EVENT SERIES 2020 Exploring fossils, geology and the bubonic plague at Mapperton Quarry in Dorset Dr. Robert Chandler Geology, Fossils and Mapperton Mapperton is a small village between Bridport and Beaminster in Dorset. In this area there is a quarry previously known as ‘Sheepwash quarry’ that is of considerable geological interest. As the name suggests the quarry used to be used to wash sheep. There was a gate with a pit to keep the animals free of disease by bathing them in disinfectant. In early times many village residents were killed by the plague. Question: When did the Bubonic Plague happen? Until recently a tree stood near the quarry reminding The ‘posy tree’ remembering plague us of those who lost their lives. The tree has now victims at Mapperton gone having rotted and become unstable over the years. We will make a virtual visit to the quarry, now known as Coombe quarry commemorating those who died and highlighting some interesting history of the area. This is rather relevant now as our visit has been postponed by Corona virus. Hopefully we can return at a later time? The quarry we will visit stands on some of the highest ground in the area. It consists of limestone deposited as part of the Jurassic System (the rocks deposited during the Jurassic Period) around 175 million years old. The limestones are called ‘Inferior Oolite’. In this case ‘Inferior’ means below the rocks of the Great Oolite commonly seen around Bath. Coombe Quarry viewed from the air 1 Question: What is an oolite? Now look it up! In the 1990s the site was purchased to house farm buildings and this involved clearing the faces of the old quarry.
    [Show full text]
  • Text of Draft
    Reconnaissance bedrock geologic map for the northern Alaska Peninsula area, southwest Alaska Including the Dillingham, Iliamna, Lake Clark, Taylor Mountains and the western part of the Kenai and Seldovia 1:250,000-scale quadrangles Compiled by Frederic H. Wilson, Robert B. Blodgett, Charles D. Blomé, Solmaz Mohadjer, Cindi C. Preller, Edward P. Klimasauskas, Bruce M. Gamble, and Warren L. Coonrad DISCLAIMER This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards or with the North American Stratigraphic Code. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. This World-Wide-Web publication was prepared by an agency of the United States Government. Neither the United States Government nor any agency thereof, nor any of their employees, makes any warranty, expressed or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed in this report, or represents that its use would not infringe privately owned rights. Reference therein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise does not necessarily constitute or imply its endorsement, recommendation, or favoring by the United States Government or any agency thereof. Although all data and software published on this Web-site have been used by the USGS, no warranty, expressed or implied, is made by the USGS as to the accuracy of the data and related materials and (or) the functioning of the software. The act of distribution shall not constitute any such warranty, and no responsibility is assumed by the USGS in the use of this data, software, or related materials.
    [Show full text]
  • Ammonites and Stratigraphy of the Upper Bajocian Garantiana Garantiana Zone in the Interfluve Between the Kuban and Urup Rivers (Northern Caucasus) V
    ISSN 0031-0301, Paleontological Journal, 2019, Vol. 53, No. 11, pp. 1188–1202. © Pleiades Publishing, Ltd., 2019. Ammonites and Stratigraphy of the Upper Bajocian Garantiana garantiana Zone in the Interfluve between the Kuban and Urup Rivers (Northern Caucasus) V. V. Mittaa, b, * aBorissiak Paleontological Institute, Russian Academy of Sciences, Moscow, 117647 Russia bCherepovets State University, Cherepovets, 162600 Russia *e-mail: [email protected] Received March 12, 2019; revised March 29, 2019; accepted April 1, 2019 Abstract—This paper presents the results of the study of the Upper Bajocian Garantiana garantiana Zone (Middle Jurassic) and characteristic ammonites in sections of the basin of the Kuban River (Karachay-Cher- kessia). The assemblage contains species of the genera Garantiana, Pseudogarantiana, Paragarantiana, Djanaliparkinsonia (all family Stephanoceratidae) and Vermisphinctes (family Perisphinctidae). A section of the Garantiana Zone on the Kyafar River contains (from bottom to top) Beds with Djanaliparkinsonia alanica (also recognized on the Kuban River), Beds with Garantiana subgaranti and Beds with Paragarantiana, approximately corresponding to the Dichotoma, Garantiana, and Tetragona subzones of the standard scale. Garantiana subgaranti Wetzel and Vermisphinctes martiusii (d’Orbigny) are described. Prorsisphinctes Buck- man, 1921 is proposed as a junior subjective synonym of Vermisphinctes Buckman, 1920. Keywords: Upper Bajocian, ammonites, Garantiana, Paragarantiana, Djanaliparkinsonia, Vermisphinctes, biostratigraphy, Northern Caucasus DOI: 10.1134/S0031030119110066 INTRODUCTION lished records of representatives of Garantianinae in the Garantiana Zone in the Northern Caucasus The Garantiana garantiana Zone is located (Ob”yasnitelnaya…, 1973; Yura…, 1992) are not sup- between the Upper Bajocian Strenoceras niortense and ported by figures or collections, and are mostly based Parkinsonia parkinsoni zones of the standard scale and on field identifications.
    [Show full text]
  • AALENIAN TMETOCERAS (AMMONOIDEA) from IBERIA Taxonomy, Habitats, and Evolution
    AALENIAN TMETOCERAS (AMMONOIDEA) FROM IBERIA Taxonomy, Habitats, and Evolution 1 2 3 S. R. Femandez-L6pez, M. H. Henriques, A. Linares, 1. Sandovae and M. S. Ureta1 'Dept. y UEI de Paleontologia Facultad de Ciencias Geo16gicas (UCM) elnstitutode Geologia Econ6mica (CSIC-UCM) 28040-Madrid, Spain 2Dept. Ci€mcias da Terra Centro de Geociencias Universidade de Coimbra 3049-Coimbra Codex, Portugal 3Dept. de Estratigrafia y Paleontologia Facultad de Ciencias Universidad de Granada 18071 Granada, Spain Abstract Several hundred Aalenian Tmetoceras from the Iberian Peninsula (N Lusitanian Basin, As­ turias, Basque-Cantabrian Basin, NE Cameros, NW Iberian Basin, Aragonese Platform, Tortosa Platform, Castilian Platform, Majorca and Betic Basin) have been reviewed. Two species of Aalenian Tmetoceras have been identified on the basis of morphological, bio­ chronological and palaeobiogeographical data: T. scissum and T. regleyi. T. scissum was dominant among the Tmetoceras populations developed in the Betic and Lusitanian basins during Opalinum, Murchisonae and Bradfordensis biochrons. Popu­ lations coniposed by evolute individuals of T. scissum inhabited shelfal or oceanic envi­ ronments. A chronocline, from rectiradiate and primitive forms to flexicostate and derived forms, can be recognized in these populations of T. scissum. In contrast, shallow epiconti­ nental platforms were inhabited by involute individuals of T. regleyi. This second species was phyletically derived from T. scissum, representing an adaptive radiation from popula­ tions of shelfal or oceanic basins to populations of epicontinental platforms. Asturias L��---:T NW Iberian Basin 14--=--�- Aragonese Platform +--Tortosa Platform 0� q@ Majorca SE Castilian Platform Central Castilian Platform Oriental sector of Median Subbetic Basin 250 km I Central sector with condensed sections of Median Subbetic Basin External Subbetic Basin Central sector with expanded sections of Median Subbetic Basin Figure 1.
    [Show full text]
  • Palaeoclimatic and Biotic Changes During the Aalenian (Middle ]Urassic) at the Southern Laurasian Seaway (Basque-Cantabrian Basin, Northern Spain)
    Palaeoclimatic and biotic changes during the Aalenian (Middle ]urassic) at the southern Laurasian Seaway (Basque-Cantabrian Basin, northern Spain) a,*, L. b, b, b Juan J. Gomez Maria Canales Soled ad Ureta Antonio Goy • Dpto, de Estratigrafia, Facultad de Ciencias Ge%gicas (UCM) and Instituto de Geologfa Econ6mica (CSIC-UCM), 28040 Madrid, Spain b Dpto, de Paleonto[ogia, Facultad de Ciencias Ge%gicas (UCM) and Instituto de Geologia Econ6mica (CSIC-UCM),28040 Madrid, Spain ABSTRACT The uppermost Toarcian-lowermost 8ajocian deposits have been studied in 10 sections located in the western part of the Basque-Cantabrian Basin (northern Spain). The studied 276 successive recorded ammonite assemblages allowed detailed biostratigraphical subdivision and the correlation of the sections at the ammonite zone and subzone scale. The foraminifers were studied in 96 samples and 55 diagenetically screened belemnite rostra were analyzed for C and 0 isotope. Keywords: Facies and thickness distribution of the Aalenian sediments suggest that deposition took place in a nearly Palaeoc1imate symmetrical sub-basin included into an intra plate shallow platform, developed over continental crust, on Biotic changes Foraminifers which flexure was the main control responsible for subsidence and basin evolution. Ammonoids Noteworthy negative 613Cb�1 excursions, coinciding with seawater temperature changes, were recorded Stable isotopes during the Bradfordensis Biochron, around the Concavum-Limitatum biochron boundary, and around the Paiaeoceanography Aalenian-Bajocian boundary. A close relationship between the changes in seawater temperature and the biotic changes observed in the foraminiferal and in the ammonoids assemblages has been evidenced. During the Comptum Biochron, the 6180�1-based palaeotemperature shows a remarkable cooling interval with an average seawater temperature of 15.7 QC.
    [Show full text]
  • Contributions in BIOLOGY and GEOLOGY
    MILWAUKEE PUBLIC MUSEUM Contributions In BIOLOGY and GEOLOGY Number 51 November 29, 1982 A Compendium of Fossil Marine Families J. John Sepkoski, Jr. MILWAUKEE PUBLIC MUSEUM Contributions in BIOLOGY and GEOLOGY Number 51 November 29, 1982 A COMPENDIUM OF FOSSIL MARINE FAMILIES J. JOHN SEPKOSKI, JR. Department of the Geophysical Sciences University of Chicago REVIEWERS FOR THIS PUBLICATION: Robert Gernant, University of Wisconsin-Milwaukee David M. Raup, Field Museum of Natural History Frederick R. Schram, San Diego Natural History Museum Peter M. Sheehan, Milwaukee Public Museum ISBN 0-893260-081-9 Milwaukee Public Museum Press Published by the Order of the Board of Trustees CONTENTS Abstract ---- ---------- -- - ----------------------- 2 Introduction -- --- -- ------ - - - ------- - ----------- - - - 2 Compendium ----------------------------- -- ------ 6 Protozoa ----- - ------- - - - -- -- - -------- - ------ - 6 Porifera------------- --- ---------------------- 9 Archaeocyatha -- - ------ - ------ - - -- ---------- - - - - 14 Coelenterata -- - -- --- -- - - -- - - - - -- - -- - -- - - -- -- - -- 17 Platyhelminthes - - -- - - - -- - - -- - -- - -- - -- -- --- - - - - - - 24 Rhynchocoela - ---- - - - - ---- --- ---- - - ----------- - 24 Priapulida ------ ---- - - - - -- - - -- - ------ - -- ------ 24 Nematoda - -- - --- --- -- - -- --- - -- --- ---- -- - - -- -- 24 Mollusca ------------- --- --------------- ------ 24 Sipunculida ---------- --- ------------ ---- -- --- - 46 Echiurida ------ - --- - - - - - --- --- - -- --- - -- - - ---
    [Show full text]
  • 06 Pavia.Pmd
    Bollettino della Società Paleontologica Italiana, 45 (2-3), 2006, 217-226. Modena, 15 gennaio 2007217 Lissoceras monachum (Gemmellaro), a ghost Ammonitida of the Tethyan Bathonian Giulio PAVIA G. Pavia, Dipartimento di Scienze della Terra, via Valperga Caluso 35, I-10124 Torino (Italy); [email protected] KEY-WORDS - Systematics, Ammonitida, Lissoceras, Bathonian, Tethys. ABSTRACT - L. monachum has been frequently recorded in the Upper Bajocian and Lower Bathonian, but references in literature differ in morphological details as they are based on a juvenile and poorly-preserved holotype. In addition, the type of L. monachum comes from a bed affected by taphonomical condensation mixing fossils from Early and Middle Bathonian times, i.e. the biochronological meaning of Gemmellaro’s taxon cannot be specified with biostratigraphic criteria from the type-locality. These references are here revised and refused on the basis of two topotypes recently sampled at Monte Erice in western Sicily, which allow a precise morphological definition of L. monachum by means of architectural and sutural characteristics. The only acceptable biostratigraphic datum comes from a Lower Bathonian specimen from southern France. The differences from L. ferrifex, L. magnum, and L. ventriplanum are discussed. Finally, the suture-line of topotype PU111502 of L. monachum and those specimens from the Upper Bajocian of the Venetian Alps, here named L. aff. monachum, support the phyletic relationships between L. ferrifex and L. magnum through transitional forms of L. monachum aged for the Tethyan Early Bathonian. RIASSUNTO - [Lissoceras monachum (Gemmellaro), un Ammonitida fantasma del Batoniano Tetideo] - L’ammonite Lissoceras monachum, della famiglia medio- e tardo-giurassica Lissoceratidae, risulta ripetutamente citata nella letteratura sistematica relativa al Baiociano superiore e al Batoniano inferiore.
    [Show full text]
  • Late Jurassic Ammonites from Alaska
    Late Jurassic Ammonites From Alaska GEOLOGICAL SURVEY PROFESSIONAL PAPER 1190 Late Jurassic Ammonites From Alaska By RALPH W. IMLAY GEOLOGICAL SURVEY PROFESSIONAL PAPER 1190 Studies of the Late jurassic ammonites of Alaska enables fairly close age determinations and correlations to be made with Upper Jurassic ammonite and stratigraphic sequences elsewhere in the world UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON 1981 UNITED STATES DEPARTMENT OF THE INTERIOR JAMES G. WATT, Secretary GEOLOGICAL SURVEY Dallas L. Peck, Director Library of Congress catalog-card No. 81-600164 For sale by the Distribution Branch, U.S. Geological Survey, 604 South Pickett Street, Alexandria, VA 22304 CONTENTS Page Page Abstract ----------------------------------------- 1 Ages and correlations -----------------------------­ 19 19 Introduction -------------------------------------- 2 Early to early middle Oxfordian --------------­ Biologic analysis _________________________________ _ 14 Late middle Oxfordian to early late Kimmeridgian 20 Latest Kimmeridgian and early Tithonian _____ _ 21 Biostratigraphic summary ------------------------- 14 Late Tithonian ______________________________ _ 21 ~ortheastern Alaska -------------------------­ 14 Ammonite faunal setting --------------------------­ 22 Wrangell Mountains -------------------------- 15 Geographic distribution ---------------------------- 23 Talkeetna Mountains -------------------------­ 17 Systematic descriptions ___________________________ _ 28 Tuxedni Bay-Iniskin Bay area ----------------- 17 References
    [Show full text]
  • Ammonites from Bathonian and Callovian (Middle Jurassic)
    View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Universität München: Elektronischen Publikationen 253 Zitteliana 89 Ammonites from Bathonian and Callovian (Middle Jurassic) North of Damghan, Paläontologie Bayerische EasternGeoBio- Alborz, North Iran & Geobiologie Staatssammlung Center LMU München LMU München für Paläontologie und Geologie Kazem Seyed-Emami1* & Ahmad Raoufian2 München, 01.07.2017 1School of Mining Engineering, University College of Engineering, University of Tehran, Manuscript received P.O. Box 11365-4563, Tehran, Iran 2 26.09.2016; revision Daneshvar Center, Farhangian University, Neyshapour, Iran accepted 30.10.2016 *Corresponding author; E-mail: [email protected] ISSN 0373-9627 ISBN 978-3-946705-00-0 Zitteliana 89, 253–270. Abstract The following Middle Jurassic ammonite families (subfamilies) are described from the Dalichai Formation north of Damghan (eastern Alborz), some of them for the first time: Phylloceratidae, Lytoceratidae, Oppeliidae (Hecticoceratinae), Stephanoceratidae (Cadomitinae), Tulitidae and Reineckeiidae. The fauna is typically Northwest-Tethyan and closely related to Central Europe (Subboreal – Submediterra- nean Provinces). Key words: Ammonites, Dalichai Formation, Middle Jurassic, Alborz, Iran Zusammenfassung Aus der Dalichai Formation nördlich von Damghan (Ostalborz) werden einige mitteljurassische Ammoniten, teils zum ersten Mal, beschrieben. Folgende Familien und Unterfamilien sind vertreten: Phylloceratidae, Lytoceratidae, Oppeliidae (Hecticoceratinae), Steph- anoceratidae (Cadomitinae), Tulitidae und Reineckeiidae. Die Fauna ist typisch für die Nordwest-Tethys und zeigt enge Beziehungen zu Zentraleuropa (Subboreale und Submediterrane Faunenprovinz). Schlüsselwörter: Ammoniten, Dalichai Formation, Mittlerer Jura, Alborz, Iran Introduction the frame of a MSc. thesis. For the present study, a new section nearby was chosen and collections The present study is a continuation of a larger re- were made by A.
    [Show full text]
  • 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.
    [Show full text]
  • 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
    [Show full text]