Geology of the Adventdalen Map Area
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- . - - - . -. � ..;/, AGE MILL.YEAR$ ;YE basalt �- OUATERNARY votcanoes CENOZOIC \....t TERTIARY ·· basalt/// 65 CRETACEOUS -� 145 MESOZOIC JURASSIC " 210 � TRIAS SIC 245 " PERMIAN 290 CARBONIFEROUS /I/ Å 360 \....t DEVONIAN � PALEOZOIC � 410 SILURIAN 440 /I/ ranite � ORDOVICIAN T 510 z CAM BRIAN � w :::;: 570 w UPPER (J) PROTEROZOIC � c( " 1000 Ill /// PRECAMBRIAN MIDDLE AND LOWER PROTEROZOIC I /// 2500 ARCHEAN /(/folding \....tfaulting x metamorphism '- subduction POLARHÅNDBOK NO. 7 AUDUN HJELLE GEOLOGY.OF SVALBARD OSLO 1993 Photographs contributed by the following: Dallmann, Winfried: Figs. 12, 21, 24, 25, 31, 33, 35, 48 Heintz, Natascha: Figs. 15, 59 Hisdal, Vidar: Figs. 40, 42, 47, 49 Hjelle, Audun: Figs. 3, 10, 11, 18 , 23, 28, 29, 30, 32, 36, 43, 45, 46, 50, 51, 52, 53, 54, 60, 61, 62, 63, 64, 65, 66, 67, 68, 69, 71, 72, 75 Larsen, Geir B.: Fig. 70 Lytskjold, Bjørn: Fig. 38 Nøttvedt, Arvid: Fig. 34 Paleontologisk Museum, Oslo: Figs. 5, 9 Salvigsen, Otto: Figs. 13, 59 Skogen, Erik: Fig. 39 Store Norske Spitsbergen Kulkompani (SNSK): Fig. 26 © Norsk Polarinstitutt, Middelthuns gate 29, 0301 Oslo English translation: Richard Binns Editor of text and illustrations: Annemor Brekke Graphic design: Vidar Grimshei Omslagsfoto: Erik Skogen Graphic production: Grimshei Grafiske, Lørenskog ISBN 82-7666-057-6 Printed September 1993 CONTENTS PREFACE ............................................6 The Kongsfjorden area ....... ..........97 Smeerenburgfjorden - Magdalene- INTRODUCTION ..... .. .... ....... ........ ....6 fjorden - Liefdefjorden................ 109 Woodfjorden - Bockfjorden........ 116 THE GEOLOGICAL EXPLORATION OF SVALBARD .... ........... ....... .......... ..9 NORTHEASTERN SPITSBERGEN AND NORDAUSTLANDET ........... 123 SVALBARD, PART OF THE Ny Friesland and Olav V Land .. .123 NORTHERN POLAR REGION ...... ... 11 Nordaustlandet and the neigh- bouring islands........................... 126 WHA T TOOK PLACE IN SVALBARD - WHEN? .... -
Checklist of Lichenicolous Fungi and Lichenicolous Lichens of Svalbard, Including New Species, New Records and Revisions
Herzogia 26 (2), 2013: 323 –359 323 Checklist of lichenicolous fungi and lichenicolous lichens of Svalbard, including new species, new records and revisions Mikhail P. Zhurbenko* & Wolfgang von Brackel Abstract: Zhurbenko, M. P. & Brackel, W. v. 2013. Checklist of lichenicolous fungi and lichenicolous lichens of Svalbard, including new species, new records and revisions. – Herzogia 26: 323 –359. Hainesia bryonorae Zhurb. (on Bryonora castanea), Lichenochora caloplacae Zhurb. (on Caloplaca species), Sphaerellothecium epilecanora Zhurb. (on Lecanora epibryon), and Trimmatostroma cetrariae Brackel (on Cetraria is- landica) are described as new to science. Forty four species of lichenicolous fungi (Arthonia apotheciorum, A. aspicili- ae, A. epiphyscia, A. molendoi, A. pannariae, A. peltigerina, Cercidospora ochrolechiae, C. trypetheliza, C. verrucosar- ia, Dacampia engeliana, Dactylospora aeruginosa, D. frigida, Endococcus fusiger, E. sendtneri, Epibryon conductrix, Epilichen glauconigellus, Lichenochora coppinsii, L. weillii, Lichenopeltella peltigericola, L. santessonii, Lichenostigma chlaroterae, L. maureri, Llimoniella vinosa, Merismatium decolorans, M. heterophractum, Muellerella atricola, M. erratica, Pronectria erythrinella, Protothelenella croceae, Skyttella mulleri, Sphaerellothecium parmeliae, Sphaeropezia santessonii, S. thamnoliae, Stigmidium cladoniicola, S. collematis, S. frigidum, S. leucophlebiae, S. mycobilimbiae, S. pseudopeltideae, Taeniolella pertusariicola, Tremella cetrariicola, Xenonectriella lutescens, X. ornamentata, -
Guadalupian, Middle Permian) Mass Extinction in NW Pangea (Borup Fiord, Arctic Canada): a Global Crisis Driven by Volcanism and Anoxia
The Capitanian (Guadalupian, Middle Permian) mass extinction in NW Pangea (Borup Fiord, Arctic Canada): A global crisis driven by volcanism and anoxia David P.G. Bond1†, Paul B. Wignall2, and Stephen E. Grasby3,4 1Department of Geography, Geology and Environment, University of Hull, Hull, HU6 7RX, UK 2School of Earth and Environment, University of Leeds, Leeds, LS2 9JT, UK 3Geological Survey of Canada, 3303 33rd Street N.W., Calgary, Alberta, T2L 2A7, Canada 4Department of Geoscience, University of Calgary, 2500 University Drive N.W., Calgary Alberta, T2N 1N4, Canada ABSTRACT ing gun of eruptions in the distant Emeishan 2009; Wignall et al., 2009a, 2009b; Bond et al., large igneous province, which drove high- 2010a, 2010b), making this a mid-Capitanian Until recently, the biotic crisis that oc- latitude anoxia via global warming. Although crisis of short duration, fulfilling the second cri- curred within the Capitanian Stage (Middle the global Capitanian extinction might have terion. Several other marine groups were badly Permian, ca. 262 Ma) was known only from had different regional mechanisms, like the affected in equatorial eastern Tethys Ocean, in- equatorial (Tethyan) latitudes, and its global more famous extinction at the end of the cluding corals, bryozoans, and giant alatocon- extent was poorly resolved. The discovery of Permian, each had its roots in large igneous chid bivalves (e.g., Wang and Sugiyama, 2000; a Boreal Capitanian crisis in Spitsbergen, province volcanism. Weidlich, 2002; Bond et al., 2010a; Chen et al., with losses of similar magnitude to those in 2018). In contrast, pelagic elements of the fauna low latitudes, indicated that the event was INTRODUCTION (ammonoids and conodonts) suffered a later, geographically widespread, but further non- ecologically distinct, extinction crisis in the ear- Tethyan records are needed to confirm this as The Capitanian (Guadalupian Series, Middle liest Lopingian (Huang et al., 2019). -
The History of Exploration and Stratigraphy of the Early to Middle Triassic Vertebrate-Bearing Strata of Svalbard (Sassendalen Group, Spitsbergen)
NORWEGIAN JOURNAL OF GEOLOGY Vol 98 Nr. 2 https://dx.doi.org/10.17850/njg98-2-04 The history of exploration and stratigraphy of the Early to Middle Triassic vertebrate-bearing strata of Svalbard (Sassendalen Group, Spitsbergen) Jørn H. Hurum1, Victoria S. Engelschiøn3,1, Inghild Økland1, Janne Bratvold1, Christina P. Ekeheien1, Aubrey J. Roberts1,2, Lene L. Delsett1, Bitten B. Hansen1, Atle Mørk3, Hans A. Nakrem1, Patrick S. Druckenmiller4 & Øyvind Hammer1 1Natural History Museum, P.O. Box 1172 Blindern, NO–0318 Oslo, Norway. 2The Natural History Museum, Earth Sciences, Cromwell Road, London SW7 5BD, UK. 3Department of Geoscience and Petroleum, Norwegian University of Sciences and Technology, NO–7491 Trondheim, Norway. 4University of Alaska Museum and Department of Geology and Geophysics, University of Alaska Fairbanks, 907 Yukon Dr., Fairbanks, Alaska, 99775, USA. E-mail corresponding author (Jørn H. Hurum): [email protected] The palaeontology of the Lower to Middle Triassic succession in Spitsbergen has been studied for more than a century and a half. Our ability to properly interpret the evolutionary and ecological implications of the faunas requires precise stratigraphic control that has only recently become available. Within such a detailed stratigraphic framework, the Spitsbergen fossil material promises to contribute to our understanding of the faunal recovery after the end-Permian mass extinction. Keywords: Triassic stratigraphy, Boreal, Spitsbergen, Svalbard, Ichthyopterygia, Sedimentology, Mass extinction, Marmierfjellet, Vikinghøgda, Deltadalen, Botneheia, Olenekian, Anisian, Smithian, Spathian Received 23. November 2017 / Accepted 7. August 2018 / Published online 4. October 2018 Introduction waning stages of the Palaeozoic (Burgess et al., 2017). A direct result of this was the formation of the Siberian Traps (Yin & Song, 2013; Burgess et al., 2017). -
Palaeogene Deposits and the Platform Structure of Svalbard
NORSK POLARINSTITUTT SKRIFTER NR. 159 v JU. JA. LIVSIC Palaeogene deposits and the platform structure of Svalbard NORSK POLARINSTITUTT OSLO 1974 DET KONGEUGE DEPARTEMENT FOR INDUSTRI OG IlANDVERK NORSK POLARINSTITUTT Rolfstangveien 12, Snareya, 1330 Oslo Lufthavn, Norway SALG AV B0KER SALE OF BOOKS Bekene selges gjennom bokhandlere, eller The books are sold through bookshops, or bestilles direkte fra : may be ordered directly from: UNlVERSITETSFORLAGET Postboks 307 16 Pall Mall P.O.Box 142 Blindem, Oslo 3 London SW 1 Boston, Mass. 02113 Norway England USA Publikasjonsliste, som ogsa omfatter land List of publications, including maps and og sjekart, kan sendes pa anmodning. charts, wiZ be sent on request. NORSK POLARINSTITUTT SKRIFTER NR.159 JU. JA. LIVSIC Palaeogene deposits and the platform structure of Svalbard NORSK POLARINSTITUTT OSLO 1974 Manuscript received March 1971 Published April 1974 Contents Abstract ........................ 5 The eastern marginal fault zone 25 The Sassendalen monocline ...... 25 AHHOTaU;HH (Russian abstract) 5 The east Svalbard horst-like uplift 25 The Olgastretet trough .. .. .. .. 26 Introduction 7 The Kong Karls Land uplift .... 26 Stratigraphy ..................... 10 The main stages of formation of the A. Interpretation of sections ac- platform structure of the archipelago 26 cording to areas ............ 11 The Central Basin ........... 11 The Forlandsundet area ..... 13 The importance of Palaeogene depo- The Kongsfjorden area ....... 14 sits for oil and gas prospecting in The Renardodden area ...... 14 Svalbard .. .. .. .. .. .. .. 30 B. Correlation of sections ....... 15 Bituminosity and reservoir rock C. Svalbard Palaeogene deposits properties in Palaeogene deposits 30 as part of the Palaeogene depo- Hydrogeological criteria testifying sits of the Polar Basin ...... 15 to gas and oil content of the rocks 34 Tectonic criteria of oil and gas con- Mineral composition and conditions of tent . -
Svalbard 2015–2016 Meld
Norwegian Ministry of Justice and Public Security Published by: Norwegian Ministry of Justice and Public Security Public institutions may order additional copies from: Norwegian Government Security and Service Organisation E-mail: [email protected] Internet: www.publikasjoner.dep.no KET T Meld. St. 32 (2015–2016) Report to the Storting (white paper) Telephone: + 47 222 40 000 ER RY M K Ø K J E L R I I Photo: Longyearbyen, Tommy Dahl Markussen M 0 Print: 07 PrintMedia AS 7 9 7 P 3 R 0 I 1 08/2017 – Impression 1000 N 4 TM 0 EDIA – 2 Svalbard 2015–2016 Meld. St. 32 (2015–2016) Report to the Storting (white paper) 1 Svalbard Meld. St. 32 (2015–2016) Report to the Storting (white paper) Svalbard Translation from Norwegian. For information only. Table of Contents 1 Summary ........................................ 5 6Longyearbyen .............................. 39 1.1 A predictable Svalbard policy ........ 5 6.1 Introduction .................................... 39 1.2 Contents of each chapter ............... 6 6.2 Areas for further development ..... 40 1.3 Full overview of measures ............. 8 6.2.1 Tourism: Longyearbyen and surrounding areas .......................... 41 2Background .................................. 11 6.2.2 Relocation of public-sector jobs .... 43 2.1 Introduction .................................... 11 6.2.3 Port development ........................... 44 2.2 Main policy objectives for Svalbard 11 6.2.4 Svalbard Science Centre ............... 45 2.3 Svalbard in general ........................ 12 6.2.5 Land development in Longyearbyen ................................ 46 3 Framework under international 6.2.6 Energy supply ................................ 46 law .................................................... 17 6.2.7 Water supply .................................. 47 3.1 Norwegian sovereignty .................. 17 6.3 Provision of services ..................... -
Catalogue of Place Names in Northern East Greenland
Catalogue of place names in northern East Greenland In this section all officially approved, and many Greenlandic names are spelt according to the unapproved, names are listed, together with explana- modern Greenland orthography (spelling reform tions where known. Approved names are listed in 1973), with cross-references from the old-style normal type or bold type, whereas unapproved spelling still to be found on many published maps. names are always given in italics. Names of ships are Prospectors place names used only in confidential given in small CAPITALS. Individual name entries are company reports are not found in this volume. In listed in Danish alphabetical order, such that names general, only selected unapproved names introduced beginning with the Danish letters Æ, Ø and Å come by scientific or climbing expeditions are included. after Z. This means that Danish names beginning Incomplete documentation of climbing activities with Å or Aa (e.g. Aage Bertelsen Gletscher, Aage de by expeditions claiming ‘first ascents’ on Milne Land Lemos Dal, Åkerblom Ø, Ålborg Fjord etc) are found and in nunatak regions such as Dronning Louise towards the end of this catalogue. Å replaced aa in Land, has led to a decision to exclude them. Many Danish spelling for most purposes in 1948, but aa is recent expeditions to Dronning Louise Land, and commonly retained in personal names, and is option- other nunatak areas, have gained access to their al in some Danish town names (e.g. Ålborg or Aalborg region of interest using Twin Otter aircraft, such that are both correct). However, Greenlandic names be - the remaining ‘climb’ to the summits of some peaks ginning with aa following the spelling reform dating may be as little as a few hundred metres; this raises from 1973 (a long vowel sound rather than short) are the question of what constitutes an ‘ascent’? treated as two consecutive ‘a’s. -
A Sedimentological Study of the De Geerdalen Formation with Focus on the Isfjorden Member and Palaeosols
A Sedimentological Study of the De Geerdalen Formation with Focus on the Isfjorden Member and Palaeosols Turid Haugen Geology Submission date: August 2016 Supervisor: Atle Mørk, IGB Co-supervisor: Snorre Olaussen, UNIS Norwegian University of Science and Technology Department of Geology and Mineral Resources Engineering Abstract In this study sedimentological depositional environments of the Upper Triassic De Geerdalen Formation in Svalbard have been investigated. Facies and facies associations of the whole formation are presented, however the main focus has been on delta top sediments and in particular palaeosols. Special attention has been paid to the Isfjorden Member, which constitutes the uppermost part of the De Geerdalen Formation. The purpose of the study has been to identify palaeosols, and relate them to the overall depositional environments. The palaeosols have been identified by three main characteristics: roots, soil horizons and soil structure. Based on field observations an attempt to classify the palaeosols has been made. There are notable differences between brown and yellow palaeosols found in the middle and upper parts of the De Geerdalen Formation and the red and green palaeosols restricted to the Isfjorden Member. The yellow and brown palaeosols are in general immature compared to the green and red palaeosols of the Isfjorden Member. Thin sections from the Isfjorden Member on Deltaneset show excellent examples of calcrete, with clear biogenetic indicators. Distinct and alternating green and red colours might be related to fluctuations in groundwater level and reduction and oxidation of the soil profile. The palaeosols are found on floodplains, interdistributary areas and on top of proximal shoreface deposits. -
Prioriterte Kulturminner Og Kulturmiljøer Pa Svalbard
KATALOG PRIORITERTE KULTURMINNER OG KULTURMILJØER PA SVALBARD Versjon 1.1 (2013) Irene Skauen Sandodden Sysselmannen på Svalbard Katalog prioriterte kulturminner og kulturmiljøer på Svalbard, versjon 1.1 Side 1 Telefon 79 02 43 00 Internett Adresse Telefaks 79 02 11 66 www.sysselmannen.no Sysselmannen på Svalbard, E-post [email protected] Pb. 633, 9171 Longyearbyen ISBN: Tilgjengelighet Internett: www.sysselmannen.no Opplag: Trykkes ikke, kun digitalt Utgiver Årstall: 2013 Sysselmannen på Svalbard, miljøvernavdelingen Sider: 220 Forfattere Irene Skauen Sandodden. Tekt er hentet fra ulike kilder. Per Kyrre Reymert, Tora Hultgreen, Marit Anne Hauan og Thor Bjørn Arlov har skrevet artikler om de ulike fasene i Svalbard historie (kapittel 2). Deltakende institusjoner Sysselmannen på Svalbard Tittel Title Katalog prioriterte kulturminner og kulturmiljøer på Svalbard. Versjon Catalogue of the cultural heritage sites with high priority in Svalbard. 1.1 (2013). Version 1.1 (2013). Referanse Katalog prioriterte kulturminner og kulturmiljøer på Svalbard. Versjon 1.1 (2013). Tilgjengelig på Internett: www.sysselmannen.no. Sammendrag Katalogen gir et kort innblikk i historien til Svalbard og representative kulturminner. Videre beskrives de om lag 100 prioriterte kulturminnene og kulturmiljøene som er valgt ut i Kulturminneplan for Svalbard 2013 – 2023. Katalogen er utarbeidet som et vedlegg til kulturminneplanen, men kan revideres ved behov. Emneord norsk Keywords English - Kulturminner og kulturmiljø - Cultural heritage (monuments and cultural -
Crinoids from Svalbard in the Aftermath of the End-Permian Mass Extinction
Title: Crinoids from Svalbard in the aftermath of the end-Permian mass extinction Author: Mariusz Salamon, Przemysław Gorzelak, Nils-Martin Hanken, Henrik Erevik Riise, Bruno Ferre Citation style: Salamon Mariusz, Gorzelak Przemysław, Hanken Nils-Martin, Riise Henrik Erevik, Ferre Bruno. (2015). Crinoids from Svalbard in the aftermath of the end-Permian mass extinction. "Polish Polar Research" (Vol. 36, no. 3 (2015), s. 225-238), doi 10.1515/popore−2015−0015 vol. 36, no. 3, pp. 225–238, 2015 doi: 10.1515/popore−2015−0015 Crinoids from Svalbard in the aftermath of the end−Permian mass extinction Mariusz A. SALAMON 1, Przemysław GORZELAK2*, Nils−Martin HANKEN 3, Henrik Erevik RIISE 3,4 and Bruno FERRÉ 5 1 Wydział Nauk o Ziemi, Uniwersytet Śląski, ul. Będzińska 60, 41−200 Sosnowiec, Poland <[email protected]> 2 Instytut Paleobiologii, Polska Akademia Nauk, ul. Twarda 51/55, 00−818 Warszawa, Poland <[email protected]> * corresponding author 3 Department of Geology, UiT – The Arctic University of Norway, NO−9037 Tromsø, Norway <nils−[email protected]> 4 Present address: Halliburton, Sperry Drilling, P.O. Box 200, NO−4065 Stavanger, Norway <[email protected]> 5 Dame du Lac 213, 3 rue Henri Barbusse, F−76300 Sotteville−lès−Rouen, France <[email protected]> Abstract: The end−Permian mass extinction constituted a major event in the history of cri− noids. It led to the demise of the major Paleozoic crinoid groups including cladids, disparids, flexibles and camerates. It is widely accepted that a single lineage, derived from a late Paleo− zoic cladid ancestor (Ampelocrinidae), survived this mass extinction. -
SVALBARD 31. AUGUST – 4. SEPTEMBER Vi Meldte Oss På En Tur Til Svalbard Som Ble Arrangert Av Stavanger Aftenblad I Samarbeid Med Unik Travel
SVALBARD 31. AUGUST – 4. SEPTEMBER Vi meldte oss på en tur til Svalbard som ble arrangert av Stavanger Aftenblad i samarbeid med Unik Travel. Det var Norwegian som skulle fly fra Gardermoen til Longyearbyen. Svalbard Flagg Våpen Ifølge Wikipedia så er Svalbard første gang nevnt i islandske annaler fra 1194. I den islandske landnåmsboken fra 1200-tallet er Svalbard også nevnt, men det er usikkert om dette er det samme som dagens Svalbard. I 1596 oppdaget frisisk-nederlandske Willem Barents øyene, men Danmark-Norges overhøyhet ble respektert og forsvart. I 1671 gjorde den tyske legen Friedrich Martens nøyaktige observasjoner av øygruppens flora og fauna. Fra 1890-årene da Norge ble bedt om å gjøre krav på øygruppen, tok det 30 år før Norges regjering tildels motvillig til slutt godtok et fransk utkast til traktat ved Paris-konferansen i 1920. Den 17. juli 1925 ble loven om Svalbard sanksjonert av Kongen i statsråd, og 14. august samme år ble øygruppen Svalbard offisielt overtatt av Norge. Linker: Visit Svalbard – Wikipedia – Spitsbergen Travel – Store Norske Leksikon – Statistisk Sentralbyrå Flyet skulle gå klokka 09:00 og vi burde være på flyplassen klokka 07:15. For å slippe å reise så tidlig fra Kongsvinger, reiste vi kvelden før og overnattet på Radisson Blu Airport Hotel, Gardermoen. Sist gang vi bodde der var det dårlig rengjort. Vi klaget, og som plaster på såret så fikk vi overnatte gratis denne gangen. I en svær suite. Ikke verst. Da vi kom kom til Svalbard la vi først merke til fjellformasjonene som vi tok masse bilder av. Her er noen få av dem på syd- og vestsiden av Spitsbergen. -
A Diverse Trackway-Dominated Marine Ichnoassemblage from the Lower
Palaeogeography, Palaeoclimatology, Palaeoecology 519 (2019) 124–140 Contents lists available at ScienceDirect Palaeogeography, Palaeoclimatology, Palaeoecology journal homepage: www.elsevier.com/locate/palaeo A diverse trackway-dominated marine ichnoassemblage from the Lower Triassic in the northern Paleotethys: Ichnology and implications for biotic T recovery ⁎ Xueqian Fenga, Zhong-Qiang Chena, , Michael J. Bentonb, Siqi Wua, David J. Bottjerc, Jeffrey R. Thompsonc a State Key Laboratory of Biogeology and Environmental Geology, School of Earth Science, China University of Geosciences (Wuhan), Wuhan 430074, China b School of Earth Sciences, University of Bristol, Bristol BS8 1RJ, UK c Department of Earth Sciences, University of Southern California, Los Angeles, California 90089, USA ARTICLE INFO ABSTRACT Keywords: We document a diverse ichnoassemblage from marine interbeds of the Lower Triassic terrestrial succession in the Griesbachian Houzhougongmiao (HZGM) section of Shaanxi Province, northwestern China. Integrated biostratigraphic data Shallow tiers (bivalve, palynology and conchostracan) reveals that the ichnofossil-bearing marine beds are Griesbachian Ophiuroids (Induan, Early Triassic) in age. The marine interbeds are interpreted to be the result of the earliest Triassic Arthropods transgression of the Paleotethys Ocean northward onto the southern margin of the North China Craton. The Opportunistic organisms HZGM ichnoassemblage includes 17 ichnospecies in 16 ichnogenera and is dominated by shallow-tier Asteriacites North China and Biformites produced by ophiuroids, the scratch marks or trackways Dimorphichnus, Diplichnites, and Monomorphichnus produced by arthropods, and a rare occurrence of the fish swimming trace Undichna. Of these, the hook-shaped imprints Biformites, representing the moving arm impressions of ophiuroids, are reported for the first time from the Lower Triassic. These trace-makers are interpreted to have lived in a low energy, semi- restricted, shallow embayment environment.