Kunnskapsgrunnlag for Nedre Adventdalen

Total Page:16

File Type:pdf, Size:1020Kb

Kunnskapsgrunnlag for Nedre Adventdalen Kunnskapsgrunnlag for Nedre Adventdalen KUNNSKAPSGRUNNLAG FOR NEDRE ADVENTDALEN 1 Kunnskapsgrunnlag for Nedre Adventdalen April 2018 INNHOLD SAMMENDRAG ............................................................................................................................... 5 1. INNLEDNING ............................................................................................................................. 6 1.1 BESKRIVELSE AV OPPDRAGET....................................................................................... 6 1.2 LEVERANSEN OG BEGRENSNINGER .............................................................................. 7 1.3 BIDRAGSYTERE OG LEVERANDØRER ............................................................................ 8 2. FAUNA ...................................................................................................................................... 8 2.1 VANNFUGL ......................................................................................................................... 8 2.1.1 Bakgrunnsdata ................................................................................................................. 8 2.1.2 Rødlistede fuglearter i utredningsområdet ...............................................................10 2.1.3 Områdevis gjennomgang ........................................................................................... 11 2.1.3.1 Adventdalsdeltaet ........................................................................................... 12 2.1.3.2 Hundegårdsområdet på sørsiden Adventdalsdeltaet ................................ 18 2.1.3.3 Fivelflya .......................................................................................................... 22 2.1.3.4 Isdammen med tilstøtende viktige områder for vannfugl ......................... 26 2.1.3.5 Området mellom utløpet av Endalen og Todalen ...................................... 30 2.1.3.6 Området mellom Todalen og Bolterdalen .................................................. 35 2.1.3.7 Området mellom Arctowskifjellet og Janssonhaugen ................................. 39 2.1.4 Vannfugl. Artsvis gjennomgang ..................................................................................41 2.1.4.1 Kortnebbgås ................................................................................................. 42 2.1.4.2 Ringgås ......................................................................................................... 43 2.1.4.3 Hvitkinngås .................................................................................................... 45 2.1.4.4 Stokkand ........................................................................................................ 46 2.1.4.5 Brunnakke...................................................................................................... 47 2.1.4.6 Krikkand ......................................................................................................... 47 2.1.4.7 Stjertand ........................................................................................................ 47 2.1.4.8 Ærfugl ........................................................................................................... 48 2.1.4.9 Praktærfugl .................................................................................................... 48 2.1.4.10 Havelle .......................................................................................................... 50 2.1.4.11 Smålom ......................................................................................................... 52 2.1.4.12 Havhest ......................................................................................................... 53 2 Kunnskapsgrunnlag for Nedre Adventdalen 2.1.4.13 Sandlo ................................................................................................... 53 2.1.4.14 Heilo ....................................................................................................... 53 2.1.4.15 Polarsnipe .............................................................................................. 54 2.1.4.16 Sandløper ............................................................................................... 54 2.1.4.17 Alaskasnipe .............................................................................................. 55 2.1.4.18 Fjæreplytt................................................................................................ 56 2.1.4.19 Myrsnipe ................................................................................................... 58 2.1.4.20 Svømmesnipe .......................................................................................... 59 2.1.4.21 Polarsvømmesnipe .......................................................................................... 60 2.1.4.22 Steinvender ..................................................................................................... 61 2.1.4.23 Tyvjo ................................................................................................................ 61 2.1.4.24 Fjelljo ............................................................................................................... 62 2.1.4.25 Storjo ............................................................................................................... 63 2.1.4.26 Hettemåke ....................................................................................................... 63 2.1.4.27 Fiskemåke ........................................................................................................ 64 2.1.4.28 Sildemåke ......................................................................................................... 64 2.1.4.29 Gråmåke ........................................................................................................... 64 2.1.4.30 Grønlandsmåke ................................................................................................ 65 2.1.4.31 Polarmåke ....................................................................................................... 65 2.1.4.32 Svartbak ........................................................................................................... 67 2.1.4.33 Krykkje .............................................................................................................. 68 2.1.4.34 Ismåke ..............................................................................................................69 2.1.4.35 Rødnebbterne ................................................................................................. 72 2.1.4.36 Polarlomvi ....................................................................................................... 74 2.1.4.37 Teist .................................................................................................................. 75 2.1.4.38 Alkekonge ......................................................................................................... 76 2.1.4.39 Lunde ............................................................................................................... 77 REFERANSER. Vannfugl (inkl. ferdselseffekter på fugl)............................................................ 77 2.2 SVALBARDRYPE ....................................................................................................................... 78 REFERANSER. Svalbardrype (inkl. ferdselseffekter) ................................................................. 82 2.3 FOREKOMST AV ANDRE FUGLEARTER .............................................................................. 83 2.4 SVALBARDREIN ...................................................................................................................... 83 REFERANSER. Svalbardrein (inkl. ferdselseffekter) .................................................................. 85 2.5 FJELLREV ................................................................................................................................ 86 2.6 FOREKOMST AV FREMMEDE ARTER. FAUNA ................................................................... 87 REFERANSER. Fjellrev og fremmede arter (inkl. ferdselseffekter) ........................................... 88 2.7 OMRÅDER SOM ER SPESIELT SÅRBARE FOR MENNESKELIG FERDSEL OG AKTIVITET ....... 89 2.7.1 Vannfugl ................................................................................................................. 89 2.7.2 Svalbardrype ............................................................................................................90 2.7.3 Svalbardrein .............................................................................................................91 2.7.4 Fjellrev ...................................................................................................................... 91 3 Kunnskapsgrunnlag for Nedre Adventdalen 2.8 KUNNSKAPSMANGLER FAUNA .......................................................................................... 92 3. FLORA ............................................................................................................................................. 92 3.1 VEGETASJONSTYPER I OMRÅDET ...................................................................................... 92 3.2 FOREKOMST AV RØDLISTEDE PLANTEARTER .................................................................... 95 3.3. FOREKOMST AV FREMMEDE PLANTEARTER ..................................................................... 96 3.4. OMRÅDER SOM ER SPESIELT
Recommended publications
  • Handbok07.Pdf
    - . - - - . -. � ..;/, 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? ....
    [Show full text]
  • Climate in Svalbard 2100
    M-1242 | 2018 Climate in Svalbard 2100 – a knowledge base for climate adaptation NCCS report no. 1/2019 Photo: Ketil Isaksen, MET Norway Editors I.Hanssen-Bauer, E.J.Førland, H.Hisdal, S.Mayer, A.B.Sandø, A.Sorteberg CLIMATE IN SVALBARD 2100 CLIMATE IN SVALBARD 2100 Commissioned by Title: Date Climate in Svalbard 2100 January 2019 – a knowledge base for climate adaptation ISSN nr. Rapport nr. 2387-3027 1/2019 Authors Classification Editors: I.Hanssen-Bauer1,12, E.J.Førland1,12, H.Hisdal2,12, Free S.Mayer3,12,13, A.B.Sandø5,13, A.Sorteberg4,13 Clients Authors: M.Adakudlu3,13, J.Andresen2, J.Bakke4,13, S.Beldring2,12, R.Benestad1, W. Bilt4,13, J.Bogen2, C.Borstad6, Norwegian Environment Agency (Miljødirektoratet) K.Breili9, Ø.Breivik1,4, K.Y.Børsheim5,13, H.H.Christiansen6, A.Dobler1, R.Engeset2, R.Frauenfelder7, S.Gerland10, H.M.Gjelten1, J.Gundersen2, K.Isaksen1,12, C.Jaedicke7, H.Kierulf9, J.Kohler10, H.Li2,12, J.Lutz1,12, K.Melvold2,12, Client’s reference 1,12 4,6 2,12 5,8,13 A.Mezghani , F.Nilsen , I.B.Nilsen , J.E.Ø.Nilsen , http://www.miljodirektoratet.no/M1242 O. Pavlova10, O.Ravndal9, B.Risebrobakken3,13, T.Saloranta2, S.Sandven6,8,13, T.V.Schuler6,11, M.J.R.Simpson9, M.Skogen5,13, L.H.Smedsrud4,6,13, M.Sund2, D. Vikhamar-Schuler1,2,12, S.Westermann11, W.K.Wong2,12 Affiliations: See Acknowledgements! Abstract The Norwegian Centre for Climate Services (NCCS) is collaboration between the Norwegian Meteorological In- This report was commissioned by the Norwegian Environment Agency in order to provide basic information for use stitute, the Norwegian Water Resources and Energy Directorate, Norwegian Research Centre and the Bjerknes in climate change adaptation in Svalbard.
    [Show full text]
  • Terrestrial Inputs Govern Spatial Distribution of Polychlorinated Biphenyls (Pcbs) and Hexachlorobenzene (HCB) in an Arctic Fjord System (Isfjorden, Svalbard)*
    Environmental Pollution 281 (2021) 116963 Contents lists available at ScienceDirect Environmental Pollution journal homepage: www.elsevier.com/locate/envpol Terrestrial inputs govern spatial distribution of polychlorinated biphenyls (PCBs) and hexachlorobenzene (HCB) in an Arctic fjord system (Isfjorden, Svalbard)* * Sverre Johansen a, b, c, Amanda Poste a, Ian Allan c, Anita Evenset d, e, Pernilla Carlsson a, a Norwegian Institute for Water Research, Tromsø, Norway b Norwegian University of Life Sciences, Ås, Norway c Norwegian Institute for Water Research, Oslo, Norway d Akvaplan-niva, Tromsø, Norway e UiT, The Arctic University of Norway, Tromsø, Norway article info abstract Article history: Considerable amounts of previously deposited persistent organic pollutants (POPs) are stored in the Received 20 July 2020 Arctic cryosphere. Transport of freshwater and terrestrial material to the Arctic Ocean is increasing due to Received in revised form ongoing climate change and the impact this has on POPs in marine receiving systems is unknown This 11 March 2021 study has investigated how secondary sources of POPs from land influence the occurrence and fate of Accepted 13 March 2021 POPs in an Arctic coastal marine system. Available online 17 March 2021 Passive sampling of water and sampling of riverine suspended particulate matter (SPM) and marine sediments for analysis of polychlorinated biphenyls (PCBs) and hexachlorobenzene (HCB) was carried out Keywords: Particle transport in rivers and their receiving fjords in Isfjorden system in Svalbard. Riverine SPM had low contaminant < S e Terrestrial runoff concentrations ( level of detection-28 pg/g dw PCB14,16 100 pg/g dw HCB) compared to outer marine Environmental contaminants sediments 630-880 pg/g dw SPCB14,530e770 pg/g dw HCB).
    [Show full text]
  • Seasonal Dynamics of the Marine CO System in Adventfjorden, a West
    RESEARCH ARTICLE Seasonal dynamics of the marine CO2 system in Adventfjorden, a west Spitsbergen fjord Ylva Ericson1,2, Melissa Chierici1,3, Eva Falck1,2, Agneta Fransson4, Elizabeth Jones3 & Svein Kristiansen5 1Department of Arctic Geophysics, University Centre in Svalbard, Longyearbyen, Norway; 2Geophysical Institute, University of Bergen, Bergen, Norway; 3Institute of Marine Research, Fram Centre, Tromsø, Norway; 4Norwegian Polar Institute, Fram Centre, Tromsø, Norway; 5Department of Arctic and Marine Biology, UiT—The Arctic University of Norway, Tromsø, Norway Abstract Keywords Marine carbonate system; aragonite; Time series of the marine CO2 system and related parameters at the IsA Sta- net community production; Arctic fjord tion, by Adventfjorden, Svalbard, were investigated between March 2015 biogeochemistry; Svalbard and November 2017. The physical and biogeochemical processes that govern changes in total alkalinity (TA), total dissolved inorganic carbon (DIC) and the Correspondence Ylva Ericson, Department of Arctic saturation state of the calcium carbonate mineral aragonite (ΩAr) were assessed on a monthly timescale. The major driver for TA and DIC was changes in salin- Geophysics, University Centre in Svalbard, ity, caused by river runoff, mixing and advection. This accounted for 77 and PO Box 156, NO-9171 Longyearbyen, Norway. E-mail: [email protected] 45%, respectively, of the overall variability. It contributed minimally to the variability in ΩAr (5%); instead, biological activity was responsible for 60% of Abbreviations the monthly variations. For DIC, the biological activity was also important, con- ArW: Arctic water; AW: Atlantic water; tributing 44%. The monthly effect of air–sea CO2 fluxes accounted for 11 and CC: coastal current; CTD: conductivity– temperature–depth instrument; DIC: 15% of the total changes in DIC and ΩAr, respectively.
    [Show full text]
  • Heavy Rain Events in Svalbard Summer and Autumn of 2016 to 2018
    Heavy Rain Events in Svalbard Summer and Autumn of 2016 to 2018 Ola Bakke Aashamar Thesis submitted for the degree of Master of Science in Meteorology Department of Geosciences Faculty of Mathematics and Natural Sciences University of Oslo Department of Arctic Geophysics The University Centre in Svalbard August 15, 2019 2 “ Når merket vel dere byfolk her i deres stengte gater selv det minste pust av den frihet som tindrer over Ishavets veldige rom? Sto en eneste av dere noensinne ensom under Herrens øyne i et øde av snø og natt? Stirret dere noen gang opp i polarlandets flammende nordlys og forstod de tause toner som strømmet under stjernene? Hva vet dere om de makter som taler i stormer, som roper i snøløsningens skred og som jubler i fuglefjellenes vårskrik? Ingenting. “ - Fritt etter John Giæver, Ishavets glade borgere (1956) ​ 3 Acknowledgements First of all, I am forever grateful to my main supervisor Marius Jonassen, who with his great insight and supportive comments gave me all the motivation and help I needed along the way towards this master thesis. Big round of applause to all the amazing students and staff at UNIS who I was lucky to meet during my stays in Svalbard, and the people at MetOs in Oslo. The times shared with you inspire me both personally and professionally, and I will always keep the memories! Then I want to thank Grete Stavik-Døvle, Terje Berntsen, Frode Stordal and Karl-Johan Ullavik Bakken for ​ ​ admitting and guiding two lost NTNU students into studies at UiO. If not for you, who knows what would have happened.
    [Show full text]
  • Springtime Nitrogen Oxides and Tropospheric Ozone in Svalbard: Local and Long-Range Transported Air Pollution
    EGU21-9126 https://doi.org/10.5194/egusphere-egu21-9126 EGU General Assembly 2021 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Springtime nitrogen oxides and tropospheric ozone in Svalbard: local and long-range transported air pollution Alena Dekhtyareva1, Mark Hermanson2, Anna Nikulina3, Ove Hermansen4, Tove Svendby5, Kim Holmén6, and Rune Graversen7 1Geophysical Institute, University of Bergen and Bjerknes Centre for Climate Research, Bergen, Norway ([email protected]) 2Hermanson and Associates LLC, Minneapolis, USA 3Department of Research Coordination and Planning, Arctic and Antarctic Research Institute, Russia 4Department of Monitoring and Information Technology, NILU - Norwegian Institute for Air Research, Norway 5Department of Atmosphere and Climate, NILU - Norwegian Institute for Air Research, Norway 6International director, Norwegian Polar Institute, Longyearbyen, Norway 7Department of Physics and Technology, UiT The Arctic University of Norway, Tromsø, Norway Svalbard is a near pristine Arctic environment, where long-range transport from mid-latitudes is an important air pollution source. Thus, several previous studies investigated the background nitrogen oxides (NOx) and tropospheric ozone (O3) springtime chemistry in the region. However, there are also local anthropogenic emission sources on the archipelago such as coal power plants, ships and snowmobiles, which may significantly alter in situ atmospheric composition. Measurement results from three independent research projects were combined to identify the effect of emissions from various local sources on the background concentration of NOx and O3 in Svalbard. The hourly meteorological and chemical data from the ground-based stations in Adventdalen, Ny-Ålesund and Barentsburg were analysed along with daily radiosonde soundings and weekly data from O3 sondes.
    [Show full text]
  • Written Exam SH-201 the History of Svalbard the University Centre in Svalbard, Monday 6 February 2012
    Written exam SH-201 The History of Svalbard The University Centre in Svalbard, Monday 6 February 2012 The exam is a 3 hour written test. It consists of two parts: Part I is a multiple choice test of factual knowledge. Note: This sheet with answers to part I shall be handed in. Part II (see below) is an essay part where you write extensively about one of two alternative subjects. No aids except dictionary are permitted. You may answer in English, Norwegian, Swedish or Danish. 1 2 Part I counts approximately /3 and part II counts /3 of the grade at the evaluation, but adjustment may take place. Both parts must be passed in order to pass the whole exam. Part I: Multiple choice test. Make only one cross for each question. In what year was Bjørnøya discovered by Willem 1. 1569 1596 1603 Barentsz? 2. When did land-based whaling end on Svalbard? ca. 1630 ca. 1680 ca. 1720 Which geographical region did most Russian 3. Pechora Murmansk White Sea hunters and trappers come from? When did Norwegian hunters and trappers start 4. ca. 1700 the 1750s the 1820s going to Svalbard regularly? From when dates the first map to show the whole 5. 1598 1714 1872 Svalbard archipelago? A famous scientific expedition visited Svalbard in 6. Chichagov Fram 1838–39. Which name is it known under? Recherche Svalbard was for a long time a no man’s land. In 7. Norway Sweden Russia 1871, who took an initiative to annex the islands? 8. When did Norway formally take over sovereignty? 1916 1920 1925 When was the Sysselmann (Governor of Svalbard) 9.
    [Show full text]
  • Sess Report 2018
    SESS REPORT 2018 The State of Environmental Science in Svalbard – an annual report Xxx 1 SESS report 2018 The State of Environmental Science in Svalbard – an annual report ISSN 2535-6321 ISBN 978-82-691528-0-7 Publisher: Svalbard Integrated Arctic Earth Observing System (SIOS) Editors: Elizabeth Orr, Georg Hansen, Hanna Lappalainen, Christiane Hübner, Heikki Lihavainen Editor popular science summaries: Janet Holmén Layout: Melkeveien designkontor, Oslo Citation: Orr et al (eds) 2019: SESS report 2018, Longyearbyen, Svalbard Integrated Arctic Earth Observing System The report is published as electronic document, available from SIOS web site www.sios-svalbard.org/SESSreport Contents Foreword .................................................................................................................................................4 Authors from following institutions contributed to this report ...................................................6 Summaries for stakeholders ................................................................................................................8 Permafrost thermal snapshot and active-layer thickness in Svalbard 2016–2017 .................................................................................................................... 26 Microbial activity monitoring by the Integrated Arctic Earth Observing System (MamSIOS) .................................................................................. 48 Snow research in Svalbard: current status and knowledge gaps ............................................
    [Show full text]
  • Glossary of Stratigraphic Names
    Downloaded from http://mem.lyellcollection.org/ by guest on September 23, 2021 Glossary of stratigraphic names This index attempts to list in alphabetical order all proper strati- completed here in square brackets where it differs. Constituent graphic names from Svalbard literature. It cannot be complete, units are listed generally from the top down. although most names encountered during work on this book have As explained in Sections 18.3 and 19.3.2 correlated units in the an entry. Each entry begins with the name and its stratigraphic rank Hammerfest Basin have been included. abbreviated. The name occurs and may be defined in the translation of the Aavatsmarkbreen Fm (Harland et al. 1993) Comfortlessbreen Russian Publication of Gramberg et al. (1990, Dallmann & Mork Gp; V2, Edi; 9 13. 1991 (eds)). This is a valuable source of further information which * Aberdeenflya Fm (SKS 1996, after Rye Larsen ) McVitiepynten supplements this work. Gramberg et al. is indeed especially valu- Sbgp; Pg; 9 20. able because the Russian entries are interpreted by the authors' *t Adriabukta Fro. (Birkenmajer & Turnau 1962) Billefjorden Gp; colleagues. However, the presently recommended equivalents of Meranfjellet, Julhogda, Haitanna mbrs; Cl,Tou-Vis; 10, 17. many named units are different from that work. :~t Adventdalen Gp (Parker 1967) Janusfjellet Subgp; Carolinefjel- * Names have been recommended for use by the Stratigrafisk let, Helvetiafjellet, Rurikfjellet, Agardhfjellet, Kong Karls Komite for Svalbard (SKS) of Norsk Stratigrafisk Komite (NSK). Land, Kongsoya fms; J2-K~; 4 5, 19; it has been suggested to At the time of collation of this book the SKS had provisionally include Kolmule, Kolje, Knurr, Hekkingen and Fuglen fms of agreed only on post-Devonian stratigraphic nomenclature, hence Hammerfest Basin.
    [Show full text]
  • Winning Coal at 78° North : Mining, Contingency and the Chaîne Opératoire in Old Longyear City
    Michigan Technological University Digital Commons @ Michigan Tech Dissertations, Master's Theses and Master's Dissertations, Master's Theses and Master's Reports - Open Reports 2009 Winning coal at 78° North : mining, contingency and the Chaîne Opératoire in old Longyear City Seth C. DePasqual Michigan Technological University Follow this and additional works at: https://digitalcommons.mtu.edu/etds Part of the Archaeological Anthropology Commons Copyright 2009 Seth C. DePasqual Recommended Citation DePasqual, Seth C., "Winning coal at 78° North : mining, contingency and the Chaîne Opératoire in old Longyear City", Master's Thesis, Michigan Technological University, 2009. https://doi.org/10.37099/mtu.dc.etds/308 Follow this and additional works at: https://digitalcommons.mtu.edu/etds Part of the Archaeological Anthropology Commons Winning Coal at 78˚ North: Mining, Contingency and the Chaîne Opératoire in Old Longyear City By Seth C. DePasqual A THESIS Submitted in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE IN INDUSTRIAL ARCHAEOLOGY MICHIGAN TECHNOLOGICAL UNIVERSITY 2009 This thesis, “Winning Coal at 78˚ North: Mining, Contingency and the Chaîne Opératoire in Old Longyear City” is hereby approved in partial fulfillment of the requirements for the Degree of MASTER OF SCIENCE IN INDUSTRIAL ARCHAEOLOGY. DEPARTMENT: Social Sciences Signatures: Thesis Advisor: ________________________________ Dr. Patrick E. Martin Department Chair: ______________________________ Dr. Patrick E. Martin Date: ______________________________ Acknowledgements This thesis would not have been possible without the encouraging words and guidance of my advisor Patrick Martin. His unremitting support saw me through a number of matters both academic and personal. I’d like to thank Carol MacLennan, who fostered my attention to socialized aspects of the Arctic Coal Company mining system and those related to the environment.
    [Show full text]
  • Supplement of Solid Earth, 12, 1025–1049, 2021 © Author(S) 2021
    Supplement of Solid Earth, 12, 1025–1049, 2021 https://doi.org/10.5194/se-12-1025-2021-supplement © Author(s) 2021. CC BY 4.0 License. Supplement of Early Cenozoic Eurekan strain partitioning and decoupling in central Spitsbergen, Svalbard Jean-Baptiste P. Koehl Correspondence to: Jean-Baptiste P. Koehl ([email protected]) The copyright of individual parts of the supplement might differ from the article licence. 1 S1: (a) Photographs in non-polarized and (b) polarized light of a thick section in Devonian sandstone including fractured quartz (qz) crosscut by healed fractures (hf) showing no displacement and by quartz-rich cataclastic fault rock filled with calcite cement (upper part); (c) Photographs in non-polarized and (d) polarized light of cataclased Devonian sandstone comprised of quartz crystals showing mild undulose extinction (ue) and grainsize reduction along the subvertical, east-dipping fault in the gully under the coal mine in Pyramiden (see Figure 2 for the location of the fault). Brittle cracks incorporate clasts of quartz, and a matrix of quartz, calcite and brownish, iron-rich clay minerals. 2 S2: Uninterpreted seismic sections in Sassenfjorden–Tempelfjorden (a–f) and Reindalspasset (g). See Figure 1b for location. 3 S3: Field photograph of steeply east-dipping, partly overturned Lower Devonian dark sandstone near the bottom of the gully below the mine entrance. 4 S4: Uninterpreted field photograph of Figure 3b in Pyramiden. 5 S5: (a) Interpreted and (b) uninterpreted field photograph along the northern shore of Sassenfjorden showing uppermost Pennsylvanian–lower Permian strata of the Wordiekammen and Gipshuken formations thrusted and folded top-west by a low-angle Eurekan thrust.
    [Show full text]
  • Alien Vascular Plants Recorded from the Barentsburg and Pyramiden Settlements, Svalbard
    Preslia, Praha, 76: 279–290, 2004 279 Alien vascular plants recorded from the Barentsburg and Pyramiden settlements, Svalbard Nepůvodní taxony cévnatých rostlin v okolí sídel Barentsburg a Pyramiden, Špicberky Jiří L i š k a1 & Zdeněk S o l d á n2 Dedicated to Professor Emil Hadač, a pioneer of Czech botanical research in the Arctic 1Institute of Botany, Academy of Sciences, CZ-252 43 Průhonice, Czech Republic, e-mail: [email protected]; 2Department of Botany, Charles University, Benátská 2, CZ-128 01 Praha 2, Czech Republic, e-mail: [email protected] Liška J. & Soldán Z. (2004): Alien vascular plants recorded from Barentsburg and Pyramiden settle- ments, Svalbard. – Preslia, Praha, 76: 279–290. A list of alien plant species recorded from Svalbard in the summer of 1988 is presented. Two locali- ties, the Russian settlements of Barentsburg and Pyramiden on the Isfjorden, Spitsbergen, were studied. Prior to this study, almost 60 alien species were recorded from Svalbard by other investiga- tors. During the research reported here, 44 taxa were found, 14 of which are new records for the Svalbard archipelago. Six species are considered to be possibly naturalized; however, it is difficult to assess their naturalization status because of the severity of the climate in the study area. A com- plete list of species is presented, with information on height and phenological stage of particular specimens. Most of the alien plants recorded at the two settlements belong to the family Brassicaceae. K e y w o r d s : adventive, allochtonous, Arctic, flora, introduced, non-indigenous, plant invasions, Spitsbergen, Svalbard Introduction The expedition “Svalbard 1988”, 13 July to 10 August 1988, funded by the former Czechoslovak Academy of Sciences, focused on cryptogamology, in particular algology, lichenology, and bryology.
    [Show full text]