The Geology of Melville Island, Arctic Canada

Total Page:16

File Type:pdf, Size:1020Kb

The Geology of Melville Island, Arctic Canada GEOLOGICAL SURVEY OF CANADA BULLETIN 450 THE GEOLOGY OF MELVILLE ISLAND, ARCTIC CANADA , ,$".',>pp ;$<':+:>$ * 7i7< cd q .. ..-. .. : ;..-.. *;.%T.~~-,*.< :p,~;< -!: .,. > <-.... &Zr'- j*W&$%% Eg*oisw=lii:l.R $.@<%' ..:;:y;n*...)&* K.L. Christie and N.J. McMillan Natmetl Resources F)eJsowces nakrreHas 1+1 ca,K+& Canada GEOLOGICAL SURVEY OF CANADA BULLETIN 450 THE GEOLOGY OF MELVILLE ISLAND, ARCTIC CANADA Editors R.L. Christie and N.J. McMillan '~inister of Energy, Mines and Resources Canada 1994 Available in Canada through authorized bookstore agents and other bookstores or by mail from Canada Communication Group - Publishing Ottawa, Canada KIA OS9 and from Geological Survey of Canada offices: 601 Booth Street Ottawa, Canada KIA OE8 3303-33rd Street N.W., Calgary, Alberta T2L 2A7 I00 West Pender Street Vancouver, B.C. V6B IR8 A deposit copy of this publication is also available for reference in public libraries across Canada Cat. No. M42-4501E ISBN 0-660- 14982-6 Price subject to change without notice Cover Illustration Naturally carved head of Hecla Bay sandstone, Robertson Anticline locality, eastern Melville Island. Original manuscript received: 86.10.17 to 92.09.14 Approved for publication: 92.06.11 to 92.09.16 PREFACE The earliest geological observations of Melville Island were made between 1819 and 1820, during the search for a northwest passage, by members of Captain Parry's crew. It was concluded correctly that most of the rocks were coaly sandstones. During searches for John Franklin and his crew, several more geological discoveries were made in the mid-1800s. In 1908 and 1909 the Canadian Government sent three expeditions to undertake mapping and to attempt to unravel the geology of parts of the Arctic Archipelago. The Geological Survey of Canada initiated systematic surveys in 1952 in the Arctic. The Survey quickly moved to Melville Island in 1954 to lay the groundwork of stratigraphy and structure as a basis for finding resources. These studies were the geological foundation for oil company exploration. The first wildcat was drilled in I961 and 1962. This venture was followed by 45 more wells, which resulted in the discovery of three gas fields onshore and offshore Melville Island. This bulletin encompasses stratigraphic, paleontological, structural and seismic studies and melds them with industry interpretations. The objective is to consolidate scientific knowledge so that the search for more natural resources in the future can proceed with greater success. Elkanah A. Babcock Assistant Deputy Minister Geological Survey of Canada Les premieres observations gCologiques de l'ile Melville ont CtC faites en 1819-1820 par des membres de 1'Cquipage du capitaine W.E. Parry qui Ctaient a la recherche du passage du Nord-Ouest. 11s ont conclu correctement que la plupart des roches Ctaient des grts charbonneux. Plusieurs autres dCcouvertes gCologiques ont CtC faites durant les annCes 1850, au cours des recherches effectuees dans l'espoir de retrouver Sir John Franklin. En 1908 et 1909, l'expedition du gouvernement canadien menCe par le capitaine J.E. Bernier passait l'hiver sur l'ile Melville, profitant de l'occasion pour ajouter au fonds de connaissances gCologiques de la region. Les premiers levCs systCmatiques dans 1'Arctique ont Cte entrepris par la Commission gkologique du Canada en 1952. La CGC s'est rendue dans l'ile Melville en 1954 afin d'y Ctudier la stratigraphie et la structure en vue de la prospection des ressources pCtrolieres et minCrales. Ces Ctudes ont servi a jeter les bases sur lesquelles se sont par la suite CrigCes les sociCtCs pCtrolitres. On y a fork le premier puits d'exploration entre 1961 et 1962. Par la suite, 45 autres puits ont CtC forks, ce qui a mend a la dCcouverte de trois champs de gaz dans l'ile Melville et au large de ses c6tes. Le prCsent bulletin regroupe des donnCes d'Ctudes stratigraphiques, palContologiques, structurales et sismiques et des interprktations de l'industrie. Son objectif est de rCunir les connaissances gkoscientifiques actuelles afin de contribuer au travaux futurs de prospection des ressources naturelles. Elkanah A. Babcock Sous-ministre adjoint Commission gCologique du Canada CONTENTS 1 Summary 3 Sommaire INTRODUCTION R.L. Christie 7 Nineteenth century geological discoveries 8 Twentieth century geological discoveries 9 Fieldwork, 1984-1985 9 Acknowledgments 10 References 7 Figure 1 SUMMARY OF STRATIGRAPHY OF MELVILLE ISLAND, ARCTIC CANADA Q.H. Goodbody and R.L. Christie 13 Abstract/RCsumC 13 Introduction 14 Stratigraphic and tectonic units 14 Franklinian successions 17 Sverdrup successions 20 References in text Figures 1 to 5 LOWER AND MIDDLE PALEOZOIC STRATIGRAPHY OF MELVILLE ISLAND Q.H. Goodbody 23 Abstract/RCsumC 24 Introduction 24 Acknowledgments 24 Stratigraphy 24 Ordovician to lower Middle Devonian carbonates and shales 25 Sequences A and B: Lower Ordovician to Upper Silurian or lowermost Devonian carbonates and shales 25 Canrobert Hills 25 Canrobert Formation 28 Ibbett Bay Formation 29 Raglan Range 29 Raglan Range carbonates 3 1 McCormick Inlet 3 1 Cornwallis Group 3 1 Cape Phillips Formation 32 Tingmisut Lake, Weatherall Bay 32 Unnamed carbonates 3 3 Sequence C: Lower to Middle Devonian carbonates and shales 3 3 Canrobert Hills 33 Member 5, Ibbett Bay Formation 33 Eastern and east-central Melville Island 3 3 Upper Cape Phillips Formation 34 Kitson Formation 34 Spencer Range 34 Unnamed carbonates 3 7 Towson Point 37 Unnamed carbonates 39 Middle to Upper Devonian clastic units 39 Hecla Bay wedge 39 Blackley Formation 42 Cape De Bray Formation 44 Weatherall Formation 45 Hecla Bay Formation 56 Beverley Inlet wedge 59 Beverley Inlet Formation 65 Parry Islands Formation 68 Middle to Upper Devonian tectono-stratigraphic setting 68 Summary 69 References in text Figures 1 to 33 39 Table 1 73 Plates 1 to 15 A NOTE ON GRAPTOLITE CORRELATION OF THE CANROBERT AND IBBETT BAY FORMATION BOUNDARY (ORDOVICIAIV) NISBET POINT, NORTHWESTERN MELVILLE ISLAND, ARCTIC CANADA A.C. Lenz and D.J. BorrC 105 Abstract/RCsumC 105 Introduction 105 Acknowledgments 106 Stratigraphy 106 Graptolite faunas 106 Age and correlation 106 Canrobert Formation 106 Ibbett Bay Formation 107 Conclusions 107 References 108 Plate 1 PALYNOLOGICAL CORRELATION OF MIDDLE AND LIPPER DEVONIAN ROCKS OF MELVILLE ISLAND, ARCTIC CANADA D.C. McGregor 111 Abstract/RCsumC 111 Introduction 112 Previous work 114 Age and correlation 114 Spores 116 Marine fossils 120 References in text Figures 1 to 5 in text Tables 1. 2 MELVILLE ISLAND C.L. Riediger and J.C. Harrison 121 Abstract/RCsumC 122 Introduction 122 Previous work 124 Facies analysis 124 Facies association A 127 Interpretation of facies association A 127 Facies association B 127 Interpretation of facies association B 127 Facies association C 129 Interpretation of facies association C 129 Facies association D 129 Interpretation of facies association D 129 Facies association E 13 1 Interpretation of facies association E 132 Stratigraphy and age 132 Lithostratigraphy 133 Biostratigraphy 136 Summary and conclusions 136 Acknowledgments 137 References in text Figures 1 to 10 124 Table 1 UPPERMOST TRIASSIC, JURASSIC, AND LOWERMOST CRETACEOUS STRATIGRAPHY, MELVILLE ISLAND AREA, ARCTIC CANADA A.F. Embry 139 Abstract/RCsumC 140 Introduction 141 Previous work 142 Present work 142 Stratigraphy 142 Sequence 1. Rhaetian-Sinemurian 148 Sequence 2. Pliensbachian-Aalenian 150 Sequence 3. Bajocian-Callovian 152 Sequence 4. Oxfordian-Valanginian 155 Geological history 159 References in text Figures 1 to 19 JURASSIC STRATIGRAPHY AND FOSSIL OCCURRENCES - MELVILLE, PRINCE PATRICK, AND BORDEN ISLANDS T.P. Poulton 161 Abstract/RCsumC 161 Introduction 161 Acknowledgments 163 Regional geology 165 Sinemurian 165 Oyster Creek, Borden Island 166 East side of Intrepid Inlet, Prince Patrick Island 167 Pliensbachian 167 Marie Heights, Melville Island 167 Head of Marie Bay, Melville Island 168 East Kitson River, Melville Island 168 Oyster Creek, Borden Island 168 Eastern Prince Patrick Island 168 Toarcian 169 Marie Heights, Melville Island 169 Head of Marie Bay, Melville Island 169 East Kitson River, Melville Island 170 Sabine Peninsula, Melville Island 170 Prince Patrick Island 170 Borden and Mackenzie King islands 171 Aalenian 171 Head of Marie Bay, Melville Island 172 Marie Heights, Melville Island 172 East Kitson River, Melville Island 173 Depot Island-Cape Grassy area, Melville Island 173 Sabine Peninsula, Melville Island 173 Southeastern Prince Patrick Island 174 Mackenzie King Island 174 Early Bajocian 174 Marie Heights, Melville Island 175 West side of Intrepid Inlet, Prince Patrick Island 175 East side of Intrepid Inlet, Prince Patrick Island 176 Late Bajocian and Early or Middle Bathonian 176 Mackenzie King Island 176 Late Bathonian 177 Sproule Peninsula, Melville Island 177 Southeastern Prince Patrick Island 177 Early Callovian 178 East Kitson River, Melville Island 180 Southeastern Prince Patrick Island 180 Oxfordian to Volgian 181 Intrepid Inlet, Prince Patrick Island 18 1 Mould Bay, Prince Patrick Island 181 Volgian 182 East Kitson River, Melville Island 182 Southwestern Melville Island 182 East of Intrepid Inlet, Prince Patrick Island 183 Mould Bay area, Prince Patrick Island 184 Paleogeographic considerations 186 References 189 Appendix: List of GSC fossil localities in text Figures 1 to 25 163 Table 1 CANADA D.A. Russell 195 Abstract/RCsumC 195 Introduction 195 Acknowledgments 195 Systematic Paleontology 195 Order Plesiosauria 195 Family Cryptoclididae 195 cf. Cryptoclidus richardsoni
Recommended publications
  • Post-Carboniferous Stratigraphy, Northeastern Alaska by R
    Post-Carboniferous Stratigraphy, Northeastern Alaska By R. L. DETTERMAN, H. N. REISER, W. P. BROSGE,and]. T. DUTRO,JR. GEOLOGICAL SURVEY PROFESSIONAL PAPER 886 Sedirnentary rocks of Permian to Quaternary age are named, described, and correlated with standard stratigraphic sequences UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON 1975 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress Cataloging in Publication Data Detterman, Robert L. Post-Carboniferous stratigraphy, northeastern Alaska. (Geological Survey Professional Paper 886) Bibliography: p. 45-46. Supt. of Docs. No.: I 19.16:886 1. Geology-Alaska. I. Detterman, Robert L. II. Series: United States. Geological Survey. Professional Paper 886. QE84.N74P67 551.7'6'09798 74-28084 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 Stock Number 024-001-02687-2 CONTENTS Page Page Abstract __ _ _ _ _ __ __ _ _ _ _ _ _ _ _ _ _ _ _ __ __ _ _ _ _ _ _ __ __ _ _ __ __ __ _ _ _ _ __ 1 Stratigraphy__:_Continued Introduction __________ ----------____ ----------------____ __ 1 Kingak Shale ---------------------------------------- 18 Purpose and scope ----------------------~------------- 1 Ignek Formation (abandoned) -------------------------- 20 Geographic setting ------------------------------------ 1 Okpikruak Formation (geographically restricted) ________ 21 Previous work and acknowledgments ------------------ 1 Kongakut Formation ----------------------------------
    [Show full text]
  • Seismic Reflection Profiles from Kane to Hall Basin, Nares Strait: Evidence for Faulting
    Polarforschung 74 (1-3), 21 – 39, 2004 (erschienen 2006) Seismic Reflection Profiles from Kane to Hall Basin, Nares Strait: Evidence for Faulting by H. Ruth Jackson1, Tim Hannon1, Sönke Neben2, Karsten Piepjohn2 and Tom Brent3 Abstract: Three major tectonic boundaries are predicted to be present beneath durch eine folgende kompressive Phase reaktiviert wurde. Als Arbeitshypo- the waters of this segment of Nares Strait: (1) the orogenic front of the Paleo- these fassen wir die oberflächennahen Teile dieses Systems als Stirn der Plat- zoic Ellesmerian Foldbelt between thrust sheets on Ellesmere Island and flat- tengrenze zwischen Nordamerika und Grönland auf. lying foreland rocks on Greenland, (2) the supposed sinistral strike-slip plate boundary of Paleocene age between the Ellemere Island section of the North America plate and the Greenland plate, and (3) the orogenic front of the Eocene to Oligocene Eurekan Foldbelt that must lie between thrust tectonics INTRODUCTION on Ellesmere Island and undeformed rocks of Greenland. To understand this complicated situation and to look for direct evidence of the plate boundary, The Late Cretaceous and Tertiary deformation on Ellesmere new seismic reflection profiles were collected and, together with industry data in the south, interpreted. The profiles are clustered in three areas controlled by Island (Fig. 1) called the Eurekan Orogeny has been attributed the distribution of the sea ice. Bathymetry is used to extrapolate seismic to the counter clockwise rotation of Greenland (e.g., OKULITCH features with a topographic expression between the regions. Based on high- & TRETTIN 1991). However reconciling the geology on oppo- resolution boomer and deeper penetration airgun profiles five seismic units are mapped.
    [Show full text]
  • (Late Tertiary) As Seen from Prince Patrick Island, Arctic Canada’ JOHN G
    ARCTIC WL. 43, NO. 4 (DECEMBER 1990) P. 393-403 Beaufort Formation (Late Tertiary) as Seen from Prince Patrick Island, Arctic Canada’ JOHN G. FYLES’ (Received 20 March 1990; accepted in revked form 14 June 1990) ABSTRACT. The Beaufort Formation, in its typearea on Prince Patrick Island, is a single lithostratigraphicunit, a few tens of metres thick, consisting of unlithified sandy deposits of braided rivers. Organicbeds in the sand have yielded more than 200 species of plants and insects and probably originated during the Pliocene, when the area supported coniferous forest. ThisBeaufort unit forms the thin eastern edge of a northwest-thickeningwedge of sand and gravel beneath the western part of the island. These largely unexposed beds,up to several hundred metres thick, include the Beaufort unit and perhaps other older or younger deposits.On the islands northeast and southwest of PrincePatrick Island (MeighenIsland to Banks Island),the name BeaufortFormation has been appliedto similar deposits of late Rrtiary age. Most recorded Beaufort beds on these islands are stratigraphically and paleontologically equivalentto the “type” Beaufort, but a few sites that have been called Beaufort (suchas Duck Hawk Bluffsand the lower unit at Ballast Brook,on Banks Island) differ stratigraphicallyand paleontologically from the “type” Beaufort. This paper recommends that these deposits (probably middle Miocene) and others like them be assigned new stratigraphic names and not be included in the Beaufort Formation as now defined. Informal names Mary Sachs gravel (Duck HawkBluffs) and Ballast Brookbeds are proposed as an initial step. Formal use of the name Beaufort Formation shouldrestricted be to the western Arctic Islands.
    [Show full text]
  • A Historical and Legal Study of Sovereignty in the Canadian North : Terrestrial Sovereignty, 1870–1939
    University of Calgary PRISM: University of Calgary's Digital Repository University of Calgary Press University of Calgary Press Open Access Books 2014 A historical and legal study of sovereignty in the Canadian north : terrestrial sovereignty, 1870–1939 Smith, Gordon W. University of Calgary Press "A historical and legal study of sovereignty in the Canadian north : terrestrial sovereignty, 1870–1939", Gordon W. Smith; edited by P. Whitney Lackenbauer. University of Calgary Press, Calgary, Alberta, 2014 http://hdl.handle.net/1880/50251 book http://creativecommons.org/licenses/by-nc-nd/4.0/ Attribution Non-Commercial No Derivatives 4.0 International Downloaded from PRISM: https://prism.ucalgary.ca A HISTORICAL AND LEGAL STUDY OF SOVEREIGNTY IN THE CANADIAN NORTH: TERRESTRIAL SOVEREIGNTY, 1870–1939 By Gordon W. Smith, Edited by P. Whitney Lackenbauer ISBN 978-1-55238-774-0 THIS BOOK IS AN OPEN ACCESS E-BOOK. It is an electronic version of a book that can be purchased in physical form through any bookseller or on-line retailer, or from our distributors. Please support this open access publication by requesting that your university purchase a print copy of this book, or by purchasing a copy yourself. If you have any questions, please contact us at ucpress@ ucalgary.ca Cover Art: The artwork on the cover of this book is not open access and falls under traditional copyright provisions; it cannot be reproduced in any way without written permission of the artists and their agents. The cover can be displayed as a complete cover image for the purposes of publicizing this work, but the artwork cannot be extracted from the context of the cover of this specificwork without breaching the artist’s copyright.
    [Show full text]
  • Beaufort Sea Oil Spills State of Knowledge Review and Identification of Key Issues
    Environmental Studies Research Funds 177 Beaufort Sea Oil Spills State of Knowledge Review and Identification of Key Issues November 2010 Correct citation for this report is: SL Ross Environmental Research Ltd., DF Dickins Associates LLC., Envision Planning Solutions Inc. 2010. Beaufort Sea Oil Spills State of Knowledge Review and Identification of Key Issues. Environmental Studies Research Funds Report No. 177. Calgary. 126p. The Environmental Studies Research Funds are financed from special levies on the oil and gas industry and administered by Natural Resources Canada for the Minister of Natural Resources Canada and the Minister of Indian Affairs and Northern Development. The Environmental Studies Research Funds and any person acting on their behalf assume no liability arising from the use of the information contained in this document. The opinions expressed are those of the authors and do not necessarily reflect those of the Environmental Studies Research Funds agencies. The use of trade names or identification of specific products does not constitute an endorsement or recommendation for use. Published under the auspices of the Environmental Studies Research Funds NE22-4/177E-PDF Environmental Research Studies Funds Report No. 177 November 2010 Beaufort Sea Oil Spills State of Knowledge Review and Identification of Key Issues by SL Ross Environmental Research Ltd. Ottawa, ON with DF Dickins Associates LLC La Jolla, CA and Envision Planning Solutions Inc. Calgary, AB Table of Contents Table of Contents...........................................................................................................................
    [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]
  • 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.
    [Show full text]
  • Joint Industry Programme
    CETACEAN STOCK ASSESSMENT IN RELATION TO EXPLORATION AND PRODUCTION INDUSTRY SOUND by Prepared for Joint Industry Programme 30 September 2009 LGL Report TA4582-1 CETACEAN STOCK ASSESSMENT IN RELATION TO EXPLORATION AND PRODUCTION INDUSTRY SOUND by LGL Limited, environmental research associates 22 Fisher Street, POB 280 King City, Ontario, Canada L7B 1A6 9768 Second Street Sidney, British Columbia, Canada V8L 3Y8 and LGL Alaska Research Associates Inc. 1101 East 76th Avenue, Suite B Anchorage, Alaska, United States 99518 Prepared for Joint Industry Programme 30 September 2009 LGL Report TA4582-1 Executive Summary Purpose and Objectives This project investigated the relationship between the oil industry‘s offshore E&P activities and trends in the distribution, abundance and rates of increase of key cetacean stocks found in three areas where E&P activities are intensive. The approach taken was to compare the status and population trends of stocks of key cetacean species in three areas with E&P activities―Alaska (subdivided into three regions, the Beaufort, Bering and Chukchi seas), Australia (Western and southeast regions), and Sakhalin Island, Russia―with corresponding parameters for stocks of the same species (where possible) in areas where E&P activities were absent or greatly reduced. The project involved a critical review of existing and historical data on cetacean stocks, and a compilation of data on E&P activities and non-industry factors that may have influenced stocks, in the areas of interest. Data were assessed in terms of quality, quantity, and temporal and spatial coverage to determine whether sufficient data were available for a reasonable assessment of correlations between cetacean populations and E&P activities.
    [Show full text]
  • 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.
    [Show full text]
  • Traditional Knowledge About Polar Bears (Ursus Maritimus) in Northwestern Alaska HANNAH VOORHEES,1 RHONDA SPARKS, 2 HENRY P
    ARCTIC VOL. 67, NO. 4 (DECEMBER 2014) P. 523 – 536 http://dx.doi.org/10.14430/arctic4425 Traditional Knowledge about Polar Bears (Ursus maritimus) in Northwestern Alaska HANNAH VOORHEES,1 RHONDA SPARKS, 2 HENRY P. HUNTINGTON3 and KARYN D. RODE4 (Received 3 July 2013; accepted in revised form 4 April 2014) ABSTRACT. Polar bears (Ursus maritimus) are an iconic Arctic species, but residents of Arctic coastal communities are among the few who have opportunities to observe their behavior for extended periods of time. Documenting traditional knowledge about polar bears is thus an important research approach, especially in light of recent rapid changes to summer sea ice extent. We interviewed polar bear hunters in seven Alaska Native communities along the coast of the northern Bering Sea and Chukchi Sea. Our study confirmed findings from similar research conducted in the mid-1990s and added information about the responses of polar bears to more recent environmental change. The distribution and local abundance of polar bears have changed over time, though different communities report different patterns. Polar bears arrive from the north later in fall than previously. Despite substantial changes in sea ice and other aspects of polar bear habitat, the animals generally appear to be in good body condition, and cubs continue to be observed regularly. While polar bears continue to feed primarily on seals, they have been observed eating a diverse range of foods, including eggs, greens, fish, berries, and other foods as available. Reduction in harvest levels due to environmental, economic, and social factors is the overriding trend; however, in years when bears are particularly abundant around villages, this pattern is temporarily reversed.
    [Show full text]
  • Pacific Walrus (Odobenus Rosmaurs Divergens) As a Threatened Or Endangered Species Under the Endangered Species Act
    BEFORE THE SECRETARY OF INTERIOR PETITION TO LIST THE PACIFIC WALRUS (ODOBENUS ROSMAURS DIVERGENS) AS A THREATENED OR ENDANGERED SPECIES UNDER THE ENDANGERED SPECIES ACT © BILL HICKEY, USFWS CENTER FOR BIOLOGICAL DIVERSITY FEBRUARY 7, 2008 Notice of Petition____________________________________________________ Dirk Kempthorne, Secretary Department of the Interior 1849 C Street, N.W. Washington. D.C. 20240 Tom Melius, Regional Director U.S. Fish and Wildlife Service Alaska Regional Office 1011 East Tudor Road Anchorage, Alaska 99503 PETITIONER The Center for Biological Diversity 1095 Market Street, Suite 511 San Francisco, CA 94103 ph: (415) 436-9682 ext 301 fax: (415) 436-9683 __________________________ Date: this 7th day of February, 2008 Shaye Wolf, Ph.D. Kassie Siegel Brendan Cummings Center for Biological Diversity Pursuant to Section 4(b) of the Endangered Species Act (“ESA”), 16 U.S.C. §1533(b), Section 553(3) of the Administrative Procedures Act, 5 U.S.C. § 553(e), and 50 C.F.R. § 424.14(a), the Center for Biological Diversity hereby petitions the Secretary of the Interior, through the United States Fish and Wildlife Service (“USFWS”), to list the Pacific walrus (Odobenus rosmarus divergens) as a threatened or endangered species and to designate critical habitat to ensure its survival and recovery. The Center for Biological Diversity works through science, law, and policy to secure a future for all species, great or small, hovering on the brink of extinction. The Center has over 40,000 members throughout Alaska and the United States. The Center and its members are concerned with the conservation of endangered species, including the Pacific walrus, and the effective implementation of the ESA.
    [Show full text]
  • 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.
    [Show full text]