DOCSLIB.ORG

Glossary of Stratigraphic Names

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read 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. there are no names as yet recommended by the SKS for pre- t Adventfjorden Schichten (Vonderbank 1970)~Firkanten Fm; Carboniferous stratigraphy. Tertiary names were approved by NSK Pg, Pal; 4 20. in December 1995, Carboniferous and Permian names by SKS in Advocat Seam (Orvin 1934) Kongsfjorden Fm, Kolhaugen Mbr; April 1996. They have been cited as Dallmann et al. (1995/96). Pg, Pal; 9 20. $ The Mesozoic names, in draft yet to be recommended by the Agnes-Otelie seam (Orvin 1934)= Otelie Seam. Mesozoic Subcommittee and SKS were available in July 1997 only t Agardhfjellet Fm (Parker 1967) Janusfjellet Subgp; Slottsma- after this text was finalized (Mork et al. in 1997 SKS). noya, Oppdals~ta, Lardyfjellet, Oppdalen mbrs; J2-3, Bth-Tth; All names printed in bold type are favoured in this work. 4, 19. Italic type denotes those names that are not favoured for current t Akademikerbreen Gp (Harland & Wilson 1956; Harland et al. use. However they are included in the list so as to relate to other 1966) Lomfjorden Spgp; Backlundtoppen, Draken, Svanberg- literature. Their equivalent preferred unit is indicated by the symbol fjellet + Grusdievbreen fms; Neptz; 7 12. ~meaning that the relationship may be approximate only. The Akkar Mbr (Mork et al. SKS) Fruholmen Fm in Hammerfest reason for preference or not is not explained in the glossary, but it Basin; Tr3, Nor. may found in the text of the chapters noted at the end of each entry. $ Alge Mbr (Mork et al. SKS) Fuglen Fm in Hammerfest Basin; Names in plain roman type are awaiting consideration. The J3, CIv. upper or lower case initial of the rank term indicates formal or t Alasdairhornet Fm (Harland et al. 1979) Peachflya Gp; V ?Var; informal status. 9, 13. The second part of each entry is the reference to the early use of t Albertbreen Fm (Friend et al. 1997) Siktefjellet Gp; D1, Lok; the name. No further reference is given where a name changes rank 8,16. or status because it is the rock units which retain their name in Albreen Mbr (Wallis 1969) Vildadalen Fm; Neoptz; 7 12. successive schemes. However, where some significant change of Alfred Larson-toppen unit? meaning has been recommended, e.g. by SKS, the reference added. t Alfredfjellet Fm (Krasil'shchikov & Livshits 1974)~Hamberg- The reference is followed by the unit of next higher rank (if any) fjellet Fm; P1, Art; 11, 17. then by the units of next lower rank in it (if any). The penultimate t Alkhorn Fm (Holtedahl 1913; Harland et al. 1979) St Jons- entry is a rough indication only of age. Some are in two parts; a fjorden Gp; six divisions not formalized (Harland et al. 1993) period or era symbol, followed by the three letter stage code. These V1, Varl; 9, 13. [Alkhornet]. conventions generally follow Harland et al. (1990) and are listed Alkhornkalk (Holtedahl 1913)=Alkhorn Fm; V1, Vara; 9, 13. and modified in Chapter 3. This list should not be used as a source t .&lryggen Mbr (Wallis 1969) Vildadalen Fm; Neoptz; 7, 12. for the ages of the units. It is intended to be a helpful clue. Ambigua limestone (Andersson 1990)~Kapp Kgtre Fm; C2, In attempting to avoid multiple entries for the same unit Bsh-Mos; 11, 17. separated only by alphabetical sorting many original foreign terms Anasibirites horizon (Buchan et al. 1965) ,.o part of Iskletten Mbr. are put in an English language form. Such terms as French Niveau t Andr~e Land Gp (Harland et al. 1974); Liefde Bay Spgp; Mimer etc., German Schiehten, Kalk etc; Russian Svita; Pashka etc. may be Valley, Wood Bay, Grey Hoek, Wood Bay Fms; D1-D3; translated so as to be listed with related unit names. Pra-Frs; 8 10, 16. For the same reason to streamline the list the proper name is Andr~ebreen Fm (Friend 1961) Red Bay Gp; Buchananhalvoya listed only once with its current rank (e.g. formation) regardless of Mbr; DI: Lok, 8 16. changes in rank (member, group etc.) or earlier terms such as series. t Andvika Mbr (?Birkenmajer 1972) H6ferpynten Fm; Neoptz; Thus later authors introducing a new classification may not be cited 10, 12. if the same package of rock is still identified by the original name. t Angellfjellet Mbr (Birkenmajer & Narebski 1960; Birkenmajer SKS is pressing for all names to be spelled as in current official 1992) Skgtlfjellet Fro; Ptz; 10, 12. maps. This recommendation is followed here for all relatively new t Anhydrite member (Bates & Schwarzacher 1958)~part of names established when the then current official maps were readily Gipshuken Fm; P1, Sak-Art; 4, 17. available. In this work older names, long in use in the literature, t Annabreen Fm (Wilson in Harland 1960; Harland et al. 1979) according to the priority principle are not changed whatever their Comfortlessbreen Gp; V2, ?Edi; 9, 13. grammatical form. It is preferred here only to change a name from t Anservika beds, mbr (Cutbill & Challinor 1965)~Terrierfjellet its first published use when a significant investigation has shown a Mbr; C2, Mos; 4, 17. new scheme to be necessary. The practice of changing a name with Asbestodden unit (?) Chamberlindalen Fm. no more than linguistic justification, and claiming authorship for it, Antaretiefjellet Fm (Armstrong & Smith in press) Ymerdalen is deprecated. Nevertheless in some cases the current place name is Gp; (= Tetradium Limestone of Holtedahl 1920); 03; 11, 14. Downloaded from http://mem.lyellcollection.org/ by guest on September 23, 2021 464 STRATIGRAPHIC GLOSSARY t Arctoceras horizon (Frebold 1930) ~ upper Fish Niveau ~ Sticky * Bayelva Mbr (SKS 1995) Breggerbreen Fm; Pg, Pal; 9, 20. Keep Fm. t Bellsund beds (Smevskiy 1967)~Pleistocene strata at Calypso- t Arctoeeras layers (Stolley 1911) ~ lower Sticky Keep Fm. byen, Kapp Lyell. t Argillite unit (Klubov 1965)N lower Edgeeya Fm. Bellsund dolomite (Hjelle 1962) = Lower member of LAgnesrab- t Ariekammen Fm (Birkenmajer 1958, 1992) Isbjernhamna Gp; bane Fro; Va ?Var; 10, 13. Ptz; 10, 12. t Bellsund Group (Krasil'shchikov & Kovoleva 1976)~all Ven- t Arkfjellet Fm (Major & Winsnes 1955) Sofiekammen Gp; O; dian tilloids in W Spits., includes Early and Late Varanger. 10, 14. t Bellsund-Dunderdalen tillite (Hjelle 1969) ~ all Vendian tilloids N t Arnesodden Bed (Smith et al. 1976) Wilhelmeya Fm in and S of Bellsund, mostly Early Varanger but not distinguished. Svenskoya; Tr3-J1; 5, 18, 19. t Ben Nevis Fm (Kiaer 1916) Red Bay Gp; D1, Lok; 8, 16. Askeladden Seam (Major & Nagy 1972), Firkanten Fm in t Bergnova Fm (Birkenmajer 1975) M. Deilegga Gp; V; 10, 13. E Nordenski61d Land; Pg, Pal. ?CH. t Bergskardet Fm (Birkenmajer 1975) U. Deilegga Gp; V; 10, 13. *t Aspelintoppen Fm (Major & Nagy 1972) Van Mijenfjorden Gp; t Bertel(toppen) Member (Barbaroux 1966)~ lower part Nielsen- Pg; 4, 20. fjellet Fm. Astarte horizon (Feyling-Hanssen 1955); Holocene raised beach t Billejyorden beds (Semevskiy 1967)~ Quaternary, older than his deposits in Billefjorden; 21. Bellsund beds. t Atomfjella Complex (Krasil'shchikov 1970) Stubendorffbreen Billefjorden Stage (Boulton et al. 1982) Quaternary equivalent to Spgp; Harkerbreen + Finnlandveggen gps. Paleoptz; 7, 12. Semevskiy's (1967) Bellsund Beds. t Aucella Shale (Hagerman 1925)~ Janusfjellet Subgp; JK; 4, 19. *t Billefjorden Gp (Cutbill & Challinor 1965) Btinsow Land Spgp; t Austfjorden gneisses (Harland & Wilson 1956),-~Eskolabreen Mumien, Herbyebreen, Vegardfjella, Orustdalen, Sergeijevfjel- Fm; Palptz; 7, 12. let, Hornsundneset, Adriabukta, Nordkapp, Reedvika fms; Austfjorden Mbr (Vogt 1929) Wood Bay Fm, D1, Pra-Ems; D3-C1; Fam-Tou-Vis; 4, 17. 8, 16. * Birger Johnsonfjellet Mbr (SKS 1996) Mumien Fro; C1, Vis; 4, t Austfjorden series (Harland & Wilson 1956)~ coastal completof 17. Harkerbreen § Finnlandveggen gps; Palptz; 7, 12. Biskayerfonna Subgp (Friend et al. 1997) Krossfjorden Gp; t Ausffonna Fm (Flood et al. 1969) in E Brennevinsfjorden Gp; Biskayerhuken + Montblane fms; Ptz; 8, 12. revised (Gee & Teben'kov 1996) in middle Nordaustlandet, t Biskayerhuken Fm (Harland et al. 1966; Hjelle & Lauritzen 1982 ?equiv. Lower Franklinsundet Gp. in W; Neoptz; 6, 12. after Gee) Biskayerfonna Subgp; Ptz; 8, 12.
Load more

Recommended publications
  • Taxonomy, Stratigraphy and Phylogeny of the Ne\T Genus Lanceoptychites (Ammonoidea, Anisian)
    Rivìsta Italiana di Paleontologia e Stratigrafia pagine 143-i66 TAXONOMY, STRATIGRAPHY AND PHYLOGENY OF THE NE\T GENUS LANCEOPTYCHITES (AMMONOIDEA, ANISIAN) MARCO BALINI Receìoed February 10, 1998; accepted ApriL 3, 1998 Key-zuords: Ammonoidea, Population analysis, Triassic, Ani- Damit kann bewiesen werden, dafl das Auftreten einer subakuten./fa- sien, Biostratigraphy, Phylogeny, Northern Alps, Southern Alps. stigaten Externseite unci eines lanzettfórmigen \'Vindungsquerschnitts wlhrend des lVachstums, bei flachen Ptychitidae, eine normale onto- Riassunto. Viene effettuato per la prima volta uno studio po- genetische Entwicklung darstellt und dass es sich dabei nicht um 'Va- polazionistico degli Ptychitidae compressi (Ammonoidea) raccolti chstumsanomalien handelt, wie rnanchrnal rn der Literatur vermutet strato-per-strxto nel Calcare dr Prezzo (Anisico superiore, Alpi meri- wurde. Ammonoideen mit einer solch eigentùmlicher Ontogenese dionali). Si dimostra come in alcune popolazioni di Ptychitidi com- werden nun aus der Gattung Flexoptychites, zt d.er nur noch flache pressi durante I'ontogenesi si possa verificare una modificazione del Ptychitiden mit gerundeter Externseite gerechnet werden, ;rusgeglie- ventre, che diventa subacuto/Íastigato mentre la sezione deì giro di- den und zur neuen Gattung Lanceoptychìtes gestellt. Die neue Gat- venta lanceolata. Questo particolare sviluppo della zona ventrale non tung ist eine sekundàre Abspeltung von F/exoptychires und umfasst è dovuto ad anomalie di crescita, come talvolta riponato in letteratu- zur Zett aus vier Arten: Lanceoptycbites telox sp. n, (Typusrrt), l sryx ra, ma è un normale sviluppo ontogenetico. Gli Ammonoidi con que- sp. n., l. indistinctus (Mojsisovics, 1882) und L. cbarlyanus (Diener, sto tipo particolare di ontogenesi sono separati dal genere Flexoptychi- 1900). Z. sllx und seine peramorphe Abspaltung L.
    [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]
  • 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,
    [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]
  • Tertiary Fold-And-Thrust Belt of Spitsbergen Svalbard
    Winfried K. Dallmann • Arild Andersen • Steffen G. Bergh • Harmond D. Maher Jr. • Yoshihide Ohta Tertiary fold-and-thrust belt of Spitsbergen Svalbard ' ~dl... ,, !!~"\\ MEDDELELSER NR.128 9,.~,f OSLO 1993 k ·pOlARll'l'>'\ MEDDELELSER NR. 128 WINFRIED K. DALLMANN, ARILD ANDRESEN, STEFFEN G. BERGH, HARMON D. MAHER Jr. & YOSHIHIDE OHTA Tertiary f old-and-thrust belt of Spitsbergen Svalbard COMPILATION MAP, SUMMARY AND BIBLIOGRAPHY NORSK POLARINSTITUTT OSLO 1993 Andresen, Arild: Univ. Oslo, Institutt for geologi, Pb. 1047 Blindern, N-0316 Oslo Bergh, Steffen G.: Univ. Tromsø, Institutt for biologi og geologi, N-9037 Tromsø Dallmann, Winfried K.: Norsk Polarinstitutt, Pb. 5072 Majorstua, N-0301 Oslo Maher, Harmon D., Jr.: Univ. Nebraska, Dept. of Geography and Geology, Omaha, USA-Nebraska 68182-0199 Ohta, Yoshihide: Norsk Polarinstitutt, Pb. 5072 Majorstua, N-0301 Oslo ISBN 82-7666-065-7 Printed December 1993 Cover photo by W. K. Dallmann: Folded Triassic sandstones and shales within the interior part of the Tertiary fold-and-thrust belt at Curie­ Sklodowskafjellet, Wedel Jarlsberg Land, Svalbard. CONTENTS: Introduction 5 Map data and explanatory remarks 6 Sources, compilation and accuracy of the geological base map 7 Explanation of map elements 7 Stratigraphy 7 Structure 8 Outline of the Tertiary fold-and-thrust belt of Spitsbergen 10 Tectonic setting 10 Dimensions and directions 11 Structural subdivision and characteristics 13 Interior part of foldbelt 13 Western Basement High 15 Forlandsundet Graben 16 Central Tertiary Basin 16 Billefjorden Fault Zone 17 Lomfjorden Fault Zone 17 Structural descriptions (including explanation of cross sections) 17 Sørkapp-Hornsund area 17 Interior Wedel Jarlsberg Land/Torell Land - Bellsund 19 Western and Central Nordenskiold Land 21 Oscar li Land 22 Brøggerhalvøya 24 Billefjorden - Eastern Nordenskiold Land 24 Agardhbukta - Negribreen 25 Bibliography 29 Maps and map descriptions 29 Proceedings of symposia etc.
    [Show full text]
  • First Record of the Upper Illyrian Ammonoid Subzone Marker Reitziites Reitzi in the Karst Dinarides
    75 The Mining-Geology-Petroleum Engineering Bulletin First record of the upper Illyrian UDC: 551.7:551.8 ammonoid subzone marker DOI: 10.17794/rgn.2020.2.7 Reitziites reitzi in the Karst Dinarides Original scientific paper Duje Smirčić1; Dražen Japundžić2; Nikolina GaberšeK1, Dunja Aljinović1, Nediljka Prlj-Šimić2, Katarina Krizmanić2, Uroš Barudžija1, Ivor Pavić1 1Faculty of Mining, Geology and Petroleum Engineering, University of Zagreb, Pierottijeva 6, HR10000 Zagreb 2Croatian Natural History Museum, Demetrova 1, HR10000 Zagreb Abstract Middle Triassic deposits in the Karst Dinarides (south Lika area, near Gračac) were investigated for petrological, sedi- mentological and biostratigraphic determinations. Within two continuously recorded sections of sedimentary carbon- ates and interlayered pyroclastic rocks (Mali Kunovac and Kunovac sections) reflecting variable sedimentary-magmatic environments, valuable cephalopod fauna ranging from the middle Illyrian to the upper Illyrian age was found. The most significant was the recovery of the ammonoids Asseretoceras sp., indicating the upper part of the Illyrian Paraceratites trinodosus Zone, and Reitziites reitzi species which marks the upper part of the Illyrian Reitziites reitzi Zone. The dis- covery of the Reitziites reitzi species was not known from the Karst Dinarides until this finding. Keywords: Karst Dinarides, Croatia, Middle Triassic, biostratigraphy, ammonoids 1. Introduction 2. Geological setting Biostratigraphic zonation according to ammonoids The investigated area is located in the southern part of has a very high resolution and is still considered one of Lika, in Croatia. In a geological sense, the area represents the best correlative principles for the Middle Triassic. the central part of the Karst Dinarides. The wider area of There are many recent works that consider ammonoids as Kunovac has been investigated in the frame of basic geo- the important correlative marker in spite of the wide use logical mapping, and the area of our interest covers the of conodonts in biostratigraphic correlations.
    [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]
  • 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.
    [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]
  • "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.
    [Show full text]
  • The Dynamics and Mass Budget of Aretic Glaciers
    DA NM ARKS OG GRØN L ANDS GEO L OG I SKE UNDERSØGELSE RAP P ORT 2013/3 The Dynamics and Mass Budget of Aretic Glaciers Abstracts, IASC Network of Aretic Glaciology, 9 - 12 January 2012, Zieleniec (Poland) A. P. Ahlstrøm, C. Tijm-Reijmer & M. Sharp (eds) • GEOLOGICAL SURVEY OF D EN MARK AND GREENLAND DANISH MINISTAV OF CLIMATE, ENEAGY AND BUILDING ~ G E U S DANMARKS OG GRØNLANDS GEOLOGISKE UNDERSØGELSE RAPPORT 201 3 / 3 The Dynamics and Mass Budget of Arctic Glaciers Abstracts, IASC Network of Arctic Glaciology, 9 - 12 January 2012, Zieleniec (Poland) A. P. Ahlstrøm, C. Tijm-Reijmer & M. Sharp (eds) GEOLOGICAL SURVEY OF DENMARK AND GREENLAND DANISH MINISTRY OF CLIMATE, ENERGY AND BUILDING Indhold Preface 5 Programme 6 List of participants 11 Minutes from a special session on tidewater glaciers research in the Arctic 14 Abstracts 17 Seasonal and multi-year fluctuations of tidewater glaciers cliffson Southern Spitsbergen 18 Recent changes in elevation across the Devon Ice Cap, Canada 19 Estimation of iceberg to the Hansbukta (Southern Spitsbergen) based on time-lapse photos 20 Seasonal and interannual velocity variations of two outlet glaciers of Austfonna, Svalbard, inferred by continuous GPS measurements 21 Discharge from the Werenskiold Glacier catchment based upon measurements and surface ablation in summer 2011 22 The mass balance of Austfonna Ice Cap, 2004-2010 23 Overview on radon measurements in glacier meltwater 24 Permafrost distribution in coastal zone in Hornsund (Southern Spitsbergen) 25 Glacial environment of De Long Archipelago
    [Show full text]
  • 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 .
    [Show full text]