Tertiary Fold-And-Thrust Belt of Spitsbergen Svalbard
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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, -
Appendix: Economic Geology: Exploration for Coal, Oil and Minerals
Downloaded from http://mem.lyellcollection.org/ by guest on October 1, 2021 PART 4 Appendix: Economic geology: exploration for coal, oil and Glossary of stratigraphic names, 463 minerals, 449 References, 477 Index of place names, 455 General Index, 515 Alkahornet, a distinctive landmark on the northwest, entrance to Isfjorden, is formed of early Varanger carbonates. The view is from Trygghamna ('Safe Harbour') with CSE motorboats Salterella and Collenia by the shore, with good anchorage and easy access inland. Photo M. J. Hambrey, CSE (SP. 1561). Routine journeys to the fjords of north Spitsbergen and Nordaustlandet pass by the rocky coastline of northwest Spitsbergen. Here is a view of Smeerenburgbreen from Smeerenburgfjordenwhich affords some shelter being protected by outer islands. On one of these was Smeerenburg, the principal base for early whaling, hence the Dutch name for 'blubber town'. Photo N. I. Cox, CSE 1989. Downloaded from http://mem.lyellcollection.org/ by guest on October 1, 2021 The CSE motorboat Salterella in Liefdefjorden looking north towards Erikbreen with largely Devonian rocks in the background unconformably on metamorphic Proterozoic to the left. Photo P. W. Web, CSE 1989. Access to cliffs and a glacier route (up Hannabreen) often necessitates crossing blocky talus (here Devonian in foreground) and then possibly a pleasanter route up the moraine on to hard glacier ice. Moraine generally affords a useful introduction to the rocks to be traversed along the glacial margin. The dots in the sky are geese training their young to fly in V formation for their migration back to the UK at the end of the summer. -
A Contribution to the Knowledge of Bryophytes in Polar Areas Subjected
Ǘ Digitally signed by Piotr Ǘ Otrba Date: 2018.12.31 18:02:17 Z Acta Societatis Botanicorum Poloniae DOI: 10.5586/asbp.3603 ORIGINAL RESEARCH PAPER Publication history Received: 2018-08-10 Accepted: 2018-11-26 A contribution to the knowledge of Published: 2018-12-31 bryophytes in polar areas subjected to Handling editor Michał Ronikier, W. Szafer rapid deglaciation: a case study from Institute of Botany, Polish Academy of Sciences, Poland southeastern Spitsbergen Authors’ contributions AS: designed and coordinated the study, determined the 1 2 3 moss specimens, wrote the Adam Stebel *, Ryszard Ochyra , Nadezhda A. Konstantinova , manuscript; RO: designed Wiesław Ziaja 4, Krzysztof Ostafin 4, Wojciech Maciejowski 5 the study, determined the 1 Department of Pharmaceutical Botany, Faculty of Pharmacy with Division of Laboratory moss specimens, wrote the Medicine, Medical University of Silesia in Katowice, Ostrogórska 30, 41-200 Sosnowiec, Poland manuscript, contributed 2 Department of Bryology, W. Szafer Institute of Botany, Polish Academy of Sciences, Lubicz 46, the distribution maps; NAK: 31-512 Cracow, Poland determined the liverwort 3 Kola Science Center, Russian Academy of Sciences, 184256, Kirovsk, Murmansk District, Russia specimens, wrote the 4 Institute of Geography and Spatial Management, Jagiellonian University, Gronostajowa 7, manuscript; WZ: collected the 30-387 Cracow, Poland specimens, developed the 5 Institute of the Middle and Far East, Jagiellonian University, Gronostajowa 3, 30-387 Cracow, tables, wrote the manuscript; Poland KO: collected the specimens, developed the tables, * Corresponding author. Email: [email protected] contributed the study area map; WM: conceived and coordinated the study, collected the specimens, developed the Abstract tables, wrote the manuscript, e paper provides a list of 54 species of bryophytes (48 mosses and six liverworts) contributed the study area map collected from Spitsbergen, the largest island of the Arctic Svalbard archipelago Funding (Norwegian Arctic), in 2016. -
"Polar Action" of Antoni Bolesław Dobrowolski in the Interwar Period
POLISH POLAR RESEARCH 19 1-2 31-36 1998 Joanna POPIOŁEK Museum of the Earth Polish Academy of Sciences Al. Na Skarpie 27 00-488 Warszawa, POLAND "Polar Action" of Antoni Bolesław Dobrowolski in the interwar period ABSTRACT: A. B. Dobrowolski, a member of the Belgian expedition in Belgica to West Antarctica (1897-1899), after his return home became a strong supporter of Polish scientific activity in the Polar countries. His patronage - called by him the "Polar Action", was especially well marked during organization of three Polish expeditions to the Svalbard archipelago: to Bear Island during the 2nd Polar Year, 1932-33, and to Spitsbergen in 1934 and 1938. Apart from his scientific achievements in Antarctica, Dobrowolski was also widely known as an author of popular-scientific books on history of discovery and exploration in the Arctic and the Antarctic. Key words: A. B. Dobrowolski, Polish Polar activity. Introduction Apart from scientific studies and pedagogical work, one of the passions of Antoni Bolesław Dobrowolski when he had returned home from the Belgica Expedition to West Antarctica (1897-1899), was the organization of scientific research in Poland. This was first made possible when, in recognition of his great scientific achievement - the monography "Natural history of ice", he was nomi nated deputy-director (in 1924), then director, of the State Meteorological Survey. Considering himself responsible in Poland not only for the meteorology, but also for the geophysics at large, he devoted much time to strengthening the State Meteorological Survey. He had founded the Marine Observatory in Gdynia, the Aerological Observatory at Legionowo near Warsaw, and the Magnetic Obser vatory at Świder near Warsaw. -
Decoupling As an Alternate Model for Transpression During the Initial Opening of the Norwegian-Greenland Sea
Research Note Decoupling as an alternate model for transpression during the initial opening of the Norwegian-Greenland Sea HARMON D. MAHER, JR. AND CAMPBELL CRADDOCK Maher, H. D. Jr. & Craddock, C. 1988: Decoupling as an alternate model for transpression during the initial opening of the Norwegian-Greenland Sea. Polar Research 6, 137-140. Transpressive plate motions during the opening of the Norwegian-Greenland Sea were in somc manner responsible for the development of Spitsbergen’s Tertiary fold-and-thrust belt. A flower model has been proposed for the large-scale structural architecture of Tertiary deformation (Lowell 1972). An alternate model of decoupling, where convergent and transcurrent motions were accommodated in totally or partially separated, subparallel belts is suggested. Harmon D. Maher, Jr., Dept. of Geography and Geology, University of Nebraska. Omaha, Nebraska. 68182, U.S.A.; Campbell Craddock, Dept. of Geology and Geophysics, University of Wisconsin, Madison, Wisconsin, 53706, U.S.A.; April 1988. Folds and thrusts that disrupt both Hecla Hoek probably representing emergence of the trans- basement rocks and the overlying late Paleozoic pression related crustal welt. Also, seismic pro- through Mesozoic platform cover rocks also files indicate that Tertiary structures exist locally deform Tertiary clastic strata (Orvin, 1934; underneath the west limb of the central Tertiary Birkenmajer 1981). These structures are con- basin (N0ttvedt & Rasmussen 1988). These struc- centrated in, but not restricted to (Andresen et tures are probably responsible for the formation al. 1988), a NW trending belt along and parallel of the western limb, and clearly postdate the to Spitsbergen’s west coast. The realization that Paleocene strata that are so tilted (up to 20 these ‘compressive’ structures were coeval with degrees). -
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. -
IASC Workshop on the Dynamics and Mass Budget of Arctic Glaciers
IASCIASC Workshop Workshop onon the the dynamics dynamics and and mass mass budgetbudget of of Arctic Arctic glaciers glaciers AbstractsAbstracts andand Programme Programme IASCIASC Workshop, Workshop, 25-27 25-27 January January 2016 2016 BenasqueBenasque (Spain) (Spain) IASC Network on Arctic Glaciology IASC Workshop on the dynamics and mass budget of Arctic glaciers Abstracts and program IASC Workshop & Network on Arctic Glaciology annual meeting, 25-27 January 2016, Benasque (Spain) Organised by C.H. Tijm-Reijmer, F. Navarro and M. Sharp Local organizing committee: F. Navarro (Chair), E. de Andrés (Secretary), C. Recio-Blitz, J. Lapazaran, J. Otero Network on Arctic Glaciology Cover photo: Nordenskiöldbreen 2011. Photo by A. Waxegard. ISBN: 978-90-393-6605-9 Contents Preface ............................................. 4 Program ............................................ 5 Posters ............................................. 9 Participants ......................................... 10 Minutes of the Open Forum meeting ....................... 12 Abstracts ........................................... 15 Observed changes in the runoff regime of the West Greenland ice sheet from a 40-year discharge time series ........................ 15 A.P. Ahlstrøm, D. Petersen Flow velocity abnormal and altitude variation of Austre Lovénbreen in Sval- bard: a comparison of observation and simulation . 15 S. Ai, Z. Wang, M. Yan An attempt to distinguish glacier facies on Vestfonna (Nordaustlandet), Svalbard based on SAR and GPR data ........................ 16 B. Barzycka, M. Blaszczyk, M. Grabiec, J.A. Jania Greenlands outlet-glacier sensitivity to submarine melting . 16 J. Beckmann Potential of Pléiades stereo images for measurement of snow accumula- tion in Drangajökull Ice Cap (NW Iceland) ...................... 17 J.M.C. Belart, E. Berthier, E. Magnuússon, L. Anderson, A.H. Jarosch, T. Thorsteins- son, F. Pálsson Area, elevation and mass changes of the two southernmost ice caps of the Canadian Arctic Archipelago between 1952 and 2014 . -
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. -
Polish Polar Station at Hornsund (Svalbard)
PolarPolar Research Research Department Department InstituteInstitute ofof GeophysicsGeophysics PolishPolish AcademyAcademy ofof SciencesSciences Title Piotr GŁOWACKI „Polish logistic potential at Svalbard – contribution to SIOS” (Svalbard Integrated Arctic Earth Observing System) Svalbard Integrated Arctic Earth Observing System (SIOS) The goal of SIOS Establish an Arctic Earth Observing System in and around Svalbard that integrates the studies of geophysical, chemical, hydrological and biological processes from all research and monitoring platforms. SIOS is an opportunity for Europe to establish the central node in the global monitoring of the High Arctic. ESFRI Environmental Sciences Svalbard Integrated Arctic Earth Observing System (SIOS) Map of the European Arctic and the area covered by SIOS Svalbard Integrated Arctic Earth Observing System (SIAEOS SIOS) Svalbard Integrated Arctic Earth Observing System (SIOS) Access to Project (preparatory phase) 45 partners from 15 countrys : Norway – 24 EU – 13 (Great Britain - 3, Poland - 2, Finland - 2, Danish, France, Netherlands, Germany, Sweden and Italy) non EU – 7 (Russia - 4, China, Korea, Japan) Svalbard Integrated Arctic Earth Observing System Polish activity on the Svalbard Kinnvika HonsundHonsund areaarea Polish Polar Station Photo by courtesy of the University of Leeds Hornsund area Polish vessel HORYZONT II PolishBaza Polar StationHornsund in Hornsund area PolishBaza Polar StationHornsund in Hornsund area Scientific - training vessel Horyzont II Scientific - training vessel Horyzont -
Meddelelser139.Pdf
MEDDELELSER NR. 139 Soviet Geological Research in Svalbard 1962-1992 Extended abstracts of unpublished reports Edited by: A.A. Krasil'scikov Polar Marine Geological Research Expedition NORSK POLARINSTITUTT OSLO 1996 Sponsored by: Russian-Norwegian Joint Venture "SEVOTEAM", St.Petersburg lAse Secretariat, Oslo ©Norsk Polarinstitutt, Oslo 1996 Compilation: AAKrasil'sCikov, M.Ju.Miloslavskij, AV.Pavlov, T.M.Pcelina, D.V.Semevskij, AN.Sirotkin, AM.Teben'kov and E.p.Skatov: Poljamaja morskaja geologorazvedocnaja ekspedicija, Lomonosov - St-Peterburg (Polar Marine Geological Research Expedition, Lomonosov - St.Petersburg) 189510, g. Lomonosov, ul. Pobedy, 24, RUSSIA Figures drawn by: N.G.Krasnova and L.S.Semenova Translated from Russian by: R.V.Fursenko Editor of English text: L.E.Craig Layout: W.K.Dallmann Printed February 1996 Cover photo: AM. Teben'kov: Field camp in Møllerfjorden, northwestem Spitsbergen, summer 1991. ISBN 82-7666-102-5 2 CONTENTS INTRODUCTORY REMARKS by W.K.DALLMANN 6 PREFACE by A.A.KRASIL'SCIKOV 7 1. MAIN FEATURES OF THE GEOLOGY OF SVALBARD 8 KRASIL'SCIKOV ET 1986: Explanatory notes to a series of geological maps of Spitsbergen 8 AL. 2. THE FOLDED BASEMENT 16 KRASIL'SCIKOV& LOPA 1963: Preliminary results ofthe study ofCaledonian granitoids and Hecla TIN Hoek gneis ses in northernSvalbard 16 KRASIL'SCIKOV& ABAKUMOV 1964: Preliminary results ofthe study of the sedimentary-metamorphic Hecla Hoek Complex and Paleozoic granitoids in centralSpitsbergen and northern Nordaustlandet 17 ABAKUMOV 1965: Metamorphic rocks of the Lower -
St.Meld. Nr. 9 (1999)
St.meld. nr. 9 (1999) Svalbard Tilråding fra Justis- og politidepartementet av 29. oktober 1999, godkjent i statsråd samme dag. Forklaring på forkortinger LL Longyearbyen lokalstyre SND Statens nærings- og distriktsutviklingsfond SNU Svalbard Næringsutvikling AS SSD Svalbard Samfunnsdrift AS SSS Svalbard ServiceSenter AS Store Norske Store Norske Spitsbergen Kulkompani AS St.meld. nr. 39 Stortingsmelding nr. 39 (1974–75) Vedrørende Sval- bard St.meld. nr. 40 Stortingsmelding nr. 40 (1985–86) Svalbard St.meld. nr. 50 Stortingsmelding nr. 50 (1990–91) Næringstiltak for Svalbard St.meld. nr. 42 Stortingsmelding nr. 42 (1992–93) Norsk polarfors- kning St.meld. nr. 22 Stortingsmelding nr. 22 (1994–95) Om miljøvern på Svalbard UNIS Universitetsstudiene på Svalbard Kapittel 1 St.meld. nr. 9 3 Svalbard 1 Bakgrunn Ved behandlingen av St.meld. nr. 22 (1994–95) Miljøvern på Svalbard ba Stor- tinget regjeringen om å foreta en helhetlig vurdering av svalbardsamfunnet der miljø, kulldrift og annen næringsvirksomhet, utenrikspolitiske og andre relevante forhold ble sett i sammenheng. I tillegg ble regjeringen i Dokument nr. 8:85 (1994–1995) bedt om å legge opp til en styringsmodell for Longyear- byen som gir befolkningen muligheter til demokratisk innflytelse i lokalsam- funnet i den helhetlige gjennomgangen av svalbardsamfunnet Stortinget har bedt om. I forbindelse med utarbeidelsen av stortingsmeldingen om Svalbard har det vært nedsatt en interdepartemental styringsgruppe bestående av repre- sentanter fra Finansdepartementet, Justisdepartementet, Kirke, utdannings- og forskningsdepartementet, Kommunal- og regionaldepartementet, Miljø- verndepartementet, Nærings- og handelsdepartementet og Utenriksdeparte- mentet. Som ledd i arbeidet med meldingen har det også vært nedsatt to arbeids- grupper, som har utredet spørsmålet om lokaldemokrati nærmere. -
Navarro, F., Möller, R., Vasilenko, E., Martin Espanol, A., Finkelnburg, R., & Möller, M
Navarro, F., Möller, R., Vasilenko, E., Martin Espanol, A., Finkelnburg, R., & Möller, M. (2015). Ice thickness distribution and hydrothermal structure of Elfenbeinbreen and Sveigbreen, eastern Spitsbergen, Svalbard. Journal of Glaciology, 61(229), 1015-1018. https://doi.org/10.3189/2015JoG15J141 Publisher's PDF, also known as Version of record Link to published version (if available): 10.3189/2015JoG15J141 Link to publication record in Explore Bristol Research PDF-document University of Bristol - Explore Bristol Research General rights This document is made available in accordance with publisher policies. Please cite only the published version using the reference above. Full terms of use are available: http://www.bristol.ac.uk/red/research-policy/pure/user-guides/ebr-terms/ Journal of Glaciology, Vol. 61, No. 229, 2015 doi: 10.3189/2015JoG15J141 1015 Ice thickness distribution and hydrothermal structure of The radio-echo sounding campaign was carried out on Elfenbeinbreen and Sveigbreen, eastern Spitsbergen, 5–7 April 2015, before the onset of spring melting. The radar Svalbard equipment used was a VIRL-7 ground-penetrating radar (GPR) (Vasilenko and others, 2011) with central frequency of 25 MHz. Transmitter and receiver (including control unit and INTRODUCTION recording system) were installed on separate plastic sledges, In recent decades, Svalbard glaciers have been widely radio- pulled by a snow scooter, with a separation between the echo sounded. The earliest extensive surveys of ice thickness antenna centres of 11.8 m (antennas were resistively loaded were the airborne echo soundings carried out in the 1970s dipoles, each 4.5 m in length). A total of 105 km of radar and 1980s (Macheret and Zhuravlev, 1982; Dowdeswell and profiles were collected on Elfenbeinbreen, and 36 km on others, 1984).