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MEDDELELSER NR. 120 IAN GJERTZ & BERIT MØRKVED Environmental Studies from Franz Josef Land, with Emphasis on Tikhaia Bay, Hooker Island '-,.J��!c �"'oo..--------' MikhalSkakuj NORSK POLARINSTITUTT OSLO 1992 ISBN 82-7666-043-6 lan Gjertz and Berit Mørkved Printed J uly 1992 Norsk Polarinstitutt Cover picture: Postboks 158 Iceberg of Franz Josef Land N-1330 Oslo Lufthavn (Ian Gjertz) Norway INTRODUCTION The Russian high Arctic archipelago Franz Josef Land has long been closed to foreign scientists. The political changes which occurred in the former Soviet Union in the last part of the 1980s resulted in the opening of this area to foreigners. Director Gennady Matishov of Murmansk Marine Biological Institute deserves much of the credit for this. In 1990 an international cooperation was established between the Murmansk Marine Biological Institute (MMBI); the Arctic Ecology Group of the Institute of Oceanology, Gdansk; and the Norwegian Polar Research Institute, Oslo. The purpose of this cooperation is to develope scientific cooperation in the Arctic thorugh joint expeditions, the establishment of a high Arctic scientific station, and the exchange of scientific information. So far the results of this cooperation are two scientific cruises with the RV "Pomor", a vessel belonging to the MMBI. The cruises have been named Sov Nor-Poll and Sov-Nor-Po12. A third cruise is planned for August-September 1992. In addition the MMBI has undertaken to establish a scientific station at Tikhaia Bay on Hooker Island. This is the site of a former Soviet meteorological base from 1929-1958, and some of the buildings are now being restored by MMBI. -
Palynological Investigations of Miocene Deposits on the New Siberian Archipelago (U.S.S.R.)
ARCTIC VOL. 45, NO.3 (SEPTEMBER 1992) P. 285-294 Palynological Investigationsof Miocene Deposits on the New Siberian Archipelago(U.S.S.R.)’ EUGENE v. ZYRYANOV~ (Received 12 February 1990; accepted in revised form23 January 1992) ABSTRACT. New paleobotanical data (mainly palynological) are reported from Miocene beds of the New Siberian Islands. The palynoflora has a number of distinctive features: the presence of typical hypoarctic forms, the high content taxa representing dark coniferous assemblages and the con- siderable proportion of small-leaved forms. Floristic comparison with the paleofloras of the Beaufort Formation in arctic Canada allows interpreta- tion of the evolution of the Arctic as a landscape region during Miocene-Pliocene time. This paper is a preliminary analysis of the mechanisms of arctic florogenesis. The model of an “adaptive landscape” is considered in relation to the active eustaticdrying of polar shelves. Key words: palynology, U.S.S.R., NewSiberian Islands, Miocene,Arctic, florogenesis RÉSUMÉ. On rapporte de nouvelles données paléobotaniques (principalement palynologiques) venant de couches datant du miocène situées dans l’archipel de la Nouvelle-Sibérie. La palynoflore possède un nombre de caractéristiques particulières, parmi lesquelles, la présence de formes hypoarctiques typiques, la grande quantité de taxons représentant des assemblages de conifires sombres, ainsi qu’une collection considérable de formes à petites feuilles. Une comparaison floristique avec les paléoflores de la formationde Beaufort dans l’Arctique canadien permet d’interpréter I’évolution de l’Arctique en tant que zone peuplée d’espèces végetales durant le miocbne et le pliocène. Cet article est une analyse préliminaire des mécanismes de la genèse de la flore arctique. -
The Jackson-Harmsworth North Polar Expedition
The Jackson-Harmsworth North Polar Expedition: An Account of Its First Winter and of Some Discoveries in Franz Josef Land Author(s): Arthur Montefiore Source: The Geographical Journal, Vol. 6, No. 6 (Dec., 1895), pp. 499-519 Published by: geographicalj Stable URL: http://www.jstor.org/stable/1774008 Accessed: 26-06-2016 20:45 UTC Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at http://about.jstor.org/terms JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact [email protected]. The Royal Geographical Society (with the Institute of British Geographers), Wiley are collaborating with JSTOR to digitize, preserve and extend access to The Geographical Journal This content downloaded from 129.219.247.33 on Sun, 26 Jun 2016 20:45:14 UTC All use subject to http://about.jstor.org/terms THE JACESON--HARMSWORTH NORTH POL AR EXPEDITION. 499 session, after their adventurous journey in Tibet. We also anticipate the reception of several important papers of a more specially scientific character and the afternoon meetings in the Society's map-room, which were commenced in the last session, will bei continued. As President of the International Geographical Congress, it has becotne my duty, in compliance with the terms of a resolution, to re- present the importance of Antarctic exploration to the First Lord of the Admiralty. -
New Siberian Islands Archipelago)
Detrital zircon ages and provenance of the Upper Paleozoic successions of Kotel’ny Island (New Siberian Islands archipelago) Victoria B. Ershova1,*, Andrei V. Prokopiev2, Andrei K. Khudoley1, Nikolay N. Sobolev3, and Eugeny O. Petrov3 1INSTITUTE OF EARTH SCIENCE, ST. PETERSBURG STATE UNIVERSITY, UNIVERSITETSKAYA NAB. 7/9, ST. PETERSBURG 199034, RUSSIA 2DIAMOND AND PRECIOUS METAL GEOLOGY INSTITUTE, SIBERIAN BRANCH, RUSSIAN ACADEMY OF SCIENCES, LENIN PROSPECT 39, YAKUTSK 677980, RUSSIA 3RUSSIAN GEOLOGICAL RESEARCH INSTITUTE (VSEGEI), SREDNIY PROSPECT 74, ST. PETERSBURG 199106, RUSSIA ABSTRACT Plate-tectonic models for the Paleozoic evolution of the Arctic are numerous and diverse. Our detrital zircon provenance study of Upper Paleozoic sandstones from Kotel’ny Island (New Siberian Island archipelago) provides new data on the provenance of clastic sediments and crustal affinity of the New Siberian Islands. Upper Devonian–Lower Carboniferous deposits yield detrital zircon populations that are consistent with the age of magmatic and metamorphic rocks within the Grenvillian-Sveconorwegian, Timanian, and Caledonian orogenic belts, but not with the Siberian craton. The Kolmogorov-Smirnov test reveals a strong similarity between detrital zircon populations within Devonian–Permian clastics of the New Siberian Islands, Wrangel Island (and possibly Chukotka), and the Severnaya Zemlya Archipelago. These results suggest that the New Siberian Islands, along with Wrangel Island and the Severnaya Zemlya Archipelago, were located along the northern margin of Laurentia-Baltica in the Late Devonian–Mississippian and possibly made up a single tectonic block. Detrital zircon populations from the Permian clastics record a dramatic shift to a Uralian provenance. The data and results presented here provide vital information to aid Paleozoic tectonic reconstructions of the Arctic region prior to opening of the Mesozoic oceanic basins. -
A Newly Discovered Glacial Trough on the East Siberian Continental Margin
Clim. Past Discuss., doi:10.5194/cp-2017-56, 2017 Manuscript under review for journal Clim. Past Discussion started: 20 April 2017 c Author(s) 2017. CC-BY 3.0 License. De Long Trough: A newly discovered glacial trough on the East Siberian Continental Margin Matt O’Regan1,2, Jan Backman1,2, Natalia Barrientos1,2, Thomas M. Cronin3, Laura Gemery3, Nina 2,4 5 2,6 7 1,2,8 9,10 5 Kirchner , Larry A. Mayer , Johan Nilsson , Riko Noormets , Christof Pearce , Igor Semilietov , Christian Stranne1,2,5, Martin Jakobsson1,2. 1 Department of Geological Sciences, Stockholm University, Stockholm, 106 91, Sweden 2 Bolin Centre for Climate Research, Stockholm University, Stockholm, Sweden 10 3 US Geological Survey MS926A, Reston, Virginia, 20192, USA 4 Department of Physical Geography (NG), Stockholm University, SE-106 91 Stockholm, Sweden 5 Center for Coastal and Ocean Mapping, University of New Hampshire, New Hampshire 03824, USA 6 Department of Meteorology, Stockholm University, Stockholm, 106 91, Sweden 7 University Centre in Svalbard (UNIS), P O Box 156, N-9171 Longyearbyen, Svalbard 15 8 Department of Geoscience, Aarhus University, Aarhus, 8000, Denmark 9 Pacific Oceanological Institute, Far Eastern Branch of the Russian Academy of Sciences, 690041 Vladivostok, Russia 10 Tomsk National Research Polytechnic University, Tomsk, Russia Correspondence to: Matt O’Regan ([email protected]) 20 Abstract. Ice sheets extending over parts of the East Siberian continental shelf have been proposed during the last glacial period, and during the larger Pleistocene glaciations. The sparse data available over this sector of the Arctic Ocean has left the timing, extent and even existence of these ice sheets largely unresolved. -
Harvard Alumni Association Worldwide Travel Programs
HARVARD ALUMNI ASSOCIATION WORLDWIDE TRAVEL PROGRAMS 2015 39836_stamp_art.indd 1 9/22/11 1:54 AM ° Expert Harvard faculty and study leaders ° More than 80 destinations on all seven continents ° Choice of land & rail, cruises, rivers & lakes, and spring break & family adventures ° Travel with fellow Harvard alumni ° Local culture, history, and cuisine at each stop ° Friendships that outlast your trip “ELBE RIVER” 2014 WITH PROFESSOR WERNER SOLLORS BOOK YOUR NEXT JOURNEY WITH THE HAA TODAY! CALL 800-422-1636 OR VISIT US AT ALUMNI.HARVARD.EDU/CATALOG Trip information is current as of August 22, 2014 COVER PHOTOGRAPHY: CHRISTOPHER MICHEL MBA ’98, PRAYER FLAGS IN BHUTAN (SEE PAGE 17 FOR TRIP DETAILS) 39836_stamp_art.indd 2 9/22/11 1:55 AM 2015 TRIPS LAND & RAIL RIVERS & LAKES CENTRAL AMERICA: CROSSING COSTA RICA, A BALKAN MOSAIC 24 GARDEN ISLES & GRAND ESTATES FROM WATERWAYS OF RUSSIA: MOSCOW TO NICARAGUA & EL SALVADOR 3 OCTOBER 1–14, 2015 HONFLEUR TO PORTSMOUTH ON SEA CLOUD II 17 ST. PETERSBURG ON VOLGA DREAM II 19 FEBRUARY 2–13, 2015 LEGENDARY TURKEY 25 JUNE 6–14, 2015 JUNE 11–21, 2015 ART, ARCHAEOLOGICAL & ARCHITECTURAL OCTOBER 3–17, 2015 WILD GALÁPAGOS ON ISABELA II 18 THE GREAT JOURNEY THROUGH EUROPE: THE TREASURES OF MEXICO CITY 4 MYSTICAL INDIA 25 JUNE 8–16, 2015 NETHERLANDS, GERMANY, FRANCE & SWITZERLAND 19 FEBRUARY 18–23, 2015 OCTOBER 8–25, 2015 MACHU PICCHU TO THE GALÁPAGOS ON CORAL II 18 JUNE 26–JULY 6, 2015 A HISTORY OF EUROPEAN FASHION EXPLORING AUSTRALIA & NEW ZEALAND 27 JUNE 9–23, 2015 THE ENCHANTING DOURO RIVER ON AMAVIDA 24 IN LONDON & PARIS 4 OCTOBER 17–NOVEMBER 7, 2015 THE BALTIC’S AMBER COAST: COPENHAGEN SEPTEMBER 26–OCTOBER 6, 2015 MARCH 13–21, 2015 EASTERN & ORIENTAL EXPRESS: BANGKOK TO ST. -
Arctic Explorer - Franz Josef Land, Spitsbergen & East Greenland Expedition
ARCTIC EXPLORER - FRANZ JOSEF LAND, SPITSBERGEN & EAST GREENLAND EXPEDITION Get away from it all on our 19-day Arctic Explorer cruise from Norway to Iceland via the remote Russian archipelago of Franz Josef Land in the Russian High Arctic where pioneers and scientists stepped ashore. This remarkable journey takes you past Spitsbergen’s towering glaciers calving spectacular icebergs across the Greenland Sea to Iceland, the land of fire and ice. Watch polar bears carrying their cubs and fluking whales in the icy waters. Join us on our voyage of discovery as we sail from ice-bound islands to hot springs, spouting geysers and gushing waterfalls. ITINERARY DAY 1, TROMSO Known as the Arctic gateway, Tromso is a remote Norwegian city at 69° north, 250 miles above the Arctic Circle, where you can take in the soft glow of the midnight sun. Make time to attend a midnight concert at Tromso’s distinctive Arctic Cathedral or learn more about early polar explorations at the Polar Museum. Famed for the Northern Lights on winter nights, you can find out more about this natural spectacle at the Science Centre. DAY 2 - DAY 3, AT SEA As you cruise to your next port of call, spend the day at sea savouring the ship’s facilities and learning about your destination’s many facets from the knowledgeable onboard experts. Listen to an enriching talk, indulge in a relaxing treatment at the spa, work out in the well-equipped gym, enjoy some down- time in your cabin, share travel reminiscences with newly found friends: the options are numerous. -
Smithsonian Miscellaneous Collections
-&? SMITHSONIAN MISCELLANEOUS COLLECTIONS VOLUME 82. NUMBER 6 THE PAST CLIMATE OF THE NORTH POLAR REGION BY EDWARD W. BERRY The Johns Hopkins University (Publication 3061) CITY OF WASHINGTON PUBLISHED BY THE SMITHSONIAN INSTITUTION APRIL 9, 1930 SMITHSONIAN MISCELLANEOUS COLLECTIONS VOLUME 82, NUMBER 6 THE PAST CLIMATE OF THE NORTH POLAR REGION BY EDWARD W. BERRY The Johns Hopkins University Publication 306i i CITY OF WASHINGTON PUBLISHED BY THE SMITHSONIAN INSTITUTION APRIL 9, 1930 ZU £or& (gafttmore (prees BALTIMORE, MD., U. S. A. THE PAST CLIMATE OF THE NORTH POLAR REGION 1 By EDWARD W. BERRY THE JOHNS HOPKINS UNIVERSITY The plants, coal beds, hairy mammoth and woolly rhinoceros ; the corals, ammonites and the host of other marine organisms, chiefly invertebrate but including ichthyosaurs and other saurians, that have been discovered beneath the snow and ice of boreal lands have always made a most powerful appeal to the imagination of explorers and geologists. We forget entirely the modern whales, reindeer, musk ox, polar bear, and abundant Arctic marine life, and remember only the seemingly great contrast between the present and this subjective past. Nowhere on the earth is there such an apparent contrast between the present and geologic climates as in the polar regions and the mental pictures which have been aroused and the theories by means of which it has been sought to explain the fancied conditions of the past are all, at least in large part, highly imaginary. Occasionally a student like Nathorst (1911) has refused to be carried away by his imagination and has called to mind the mar- velously rich life of the present day Arctic seas, but for the most part those who have speculated on former climates have entirely ignored the results of Arctic oceanography. -
Redacted for Privacy Abstract Approved: John V
AN ABSTRACT OF THE THESIS OF MIAH ALLAN BEAL for the Doctor of Philosophy (Name) (Degree) in Oceanography presented on August 12.1968 (Major) (Date) Title:Batymety and_Strictuof_thp..4rctic_Ocean Redacted for Privacy Abstract approved: John V. The history of the explordtion of the Central Arctic Ocean is reviewed.It has been only within the last 15 years that any signifi- cant number of depth-sounding data have been collected.The present study uses seven million echo soundings collected by U. S. Navy nuclear submarines along nearly 40, 000 km of track to construct, for the first time, a reasonably complete picture of the physiography of the basin of the Arctic Ocean.The use of nuclear submarines as under-ice survey ships is discussed. The physiography of the entire Arctic basin and of each of the major features in the basin are described, illustrated and named. The dominant ocean floor features are three mountain ranges, generally paralleling each other and the 40°E. 140°W. meridian. From the Pacific- side of the Arctic basin toward the Atlantic, they are: The Alpha Cordillera; The Lomonosov Ridge; andThe Nansen Cordillera. The Alpha Cordillera is the widest of the three mountain ranges. It abuts the continental slopes off the Canadian Archipelago and off Asia across more than550of longitude on each slope.Its minimum width of about 300 km is located midway between North America and Asia.In cross section, the Alpha Cordillera is a broad arch rising about two km, above the floor of the basin.The arch is marked by volcanoes and regions of "high fractured plateau, and by scarps500to 1000 meters high.The small number of data from seismology, heat flow, magnetics and gravity studies are reviewed.The Alpha Cordillera is interpreted to be an inactive mid-ocean ridge which has undergone some subsidence. -
Arctic Report Card 2017
Arctic Report Card 2017 Arctic Report Card 2017 Arctic shows no sign of returning to reliably frozen region of recent past decades 2017 Headlines 2017 Headlines Video Executive Summary Contacts Arctic shows no sign of returning to reliably frozen Vital Signs region of recent past decades Surface Air Temperature Despite relatively cool summer temperatures, Terrestrial Snow Cover observations in 2017 continue to indicate that the Greenland Ice Sheet Arctic environmental system has reached a 'new Sea Ice normal', characterized by long-term losses in the Sea Surface Temperature extent and thickness of the sea ice cover, the extent Arctic Ocean Primary Productivity and duration of the winter snow cover and the mass of ice in the Greenland Ice Sheet and Arctic glaciers, Tundra Greenness and warming sea surface and permafrost Other Indicators temperatures. Terrestrial Permafrost Groundfish Fisheries in the Highlights Eastern Bering Sea Wildland Fire in High Latitudes • The average surface air temperature for the year ending September 2017 is the 2nd warmest since 1900; however, cooler spring and summer temperatures contributed to a rebound in snow cover in the Eurasian Arctic, slower summer sea ice loss, Frostbites and below-average melt extent for the Greenland ice sheet. Paleoceanographic Perspectives • The sea ice cover continues to be relatively young and thin with older, thicker ice comprising only 21% of the ice cover in on Arctic Ocean Change 2017 compared to 45% in 1985. Collecting Environmental • In August 2017, sea surface temperatures in the Barents and Chukchi seas were up to 4° C warmer than average, Intelligence in the New Arctic contributing to a delay in the autumn freeze-up in these regions. -
NSF 03-048, Arctic Research in the United States, Volume 17, Spring
This document has been archived. The Russian–American Initiative for Land–Shelf Environments in the Arctic Contributions to Arctic System Science This article was prepared The Russian–American Initiative for Land– projects involving both U.S. and Russian scien- by Lee W. Cooper, Shelf Environments (RAISE) is unique among tists have been initiated. Summaries of many of Department of Ecology research program and project components sup- these projects, both Russian and U.S. based, are and Evolutionary Biolo- ported by the National Science Foundation’s also available at http://arctic.bio.utk.edu/#raise, gy, University of Tennes- see, with assistance from (NSF) Arctic System Science Program (ARCSS). and a summary in written form has also been RAISE principal RAISE project implementation has been explicitly recently published. investigators. international, and the program is the only cooper- Despite this progress, the scale of research ative, bilateral research program supported by supported through RAISE has been limited by the both NSF and its Russian counterpart agency, the complexities of undertaking bilateral research in Russian Foundation for Basic Research (RFBR). the Russian Federation. Changing political reali- The goal of RAISE is to facilitate bilateral ties in both the United States and Russia, eco- (U.S.–Russian) research at the land–sea margin nomic dislocations that have affected the abilities in the Eurasian Arctic, focusing on the scientific of Russian scientists to pursue their vocations, challenges of environmental change in human logistical challenges in the Russian Arctic, and and biological communities and related physical the lack of high-level governmental agreements and chemical systems. -
Proceedings of a Workshop on The
97 Select References Anonymous. [1901.] “Biographical Sketches of the Members and Crew of the Baldwin- Ziegler Polar Expedition. S.S. America.” E.B. Baldwin Papers. Washington, D.C.: Library of Congress, Manuscript Division: Box 8, Folder “Biographies—Baldwin-Ziegler Expedition.” (Hereafter cited as “Baldwin Papers: Box, etc.”) Baldwin, Evelyn Briggs. 2004. The Franz Josef Land Archipelago: E.B. Journal of the Wellman Polar Expedition, 1898-1899. P.J. Capelotti, editor. Jefferson, North Carolina: McFarland & Company, Inc. __________. 1903. “The Baldwin-Ziegler Polar Expedition, Parts I, II, and III.” Wide World Magazine 10 (58):396-402; 10 (59): 432-436; 10 (60): 587-593. __________. 1901. “Meterological Observations of the Second Wellman Expedition,” Report of the Chief of the Weather Bureau, 1899-1900, Part VII. Washington: Government Printing Office. __________. n.d. [1901]. “Short Autobiographical Sketch—Evelyn Briggs Baldwin, for William Ziegler, Esq.” Seven pp. Baldwin Papers. Washington, D.C.: Library of Congress, Manuscript Division. __________. n.d. [1899a]. “Report on Auroras.” Thirty-six pp. Baldwin Papers. Washington, D.C.: Library of Congress, Manuscript Division. __________. n.d. [1899b]. “Discovery of Graham Bell Land.” Fifty-six pp. Baldwin Papers. Washington, D.C.: Library of Congress, Manuscript Division. __________. 1899. Journal of the Wellman Polar Expedition. (unpublished typescript). Badwin Papers. Washington, D.C.: Library of Congress, Manuscript Division. __________. 1896. The Search for the North Pole. Chicago: Privately printed. __________. Papers. Manuscript Division. Library of Congress. Washington. Barnard, Leon F. Papers. Scott Polar Research Institute, MS 1514. Barr, Susan, editor. 1995. Franz Josef Land. Oslo: Norsk Polarinstitutt. Barr, Susan. 1995. “The History of Western Activity in Franz Josef Land,” in Franz Josef Land, Susan Barr, ed.