Arctic Coastal Dynamics Report of the International Workshop Vniiokeangeologia, St
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Downloaded Daily to the Geodetic Survey Division in Ottawa, Where They Are Reviewed for Quality Control, Archived, and Uploaded to the International GPS Service
Arctic Coastal Dynamics Report of the 4th International Workshop VNIIOkeangeologia, St. Petersburg (Russia), 10-13 November 2003 Edited by Volker Rachold and Georgy Cherkashov Volker Rachold, Alfred Wegener Institute, Research Unit Potsdam, Telegrafenberg A43, 14473 Potsdam, Germany Georgy Cherkashov, VNIIOkeangeologia (Institute for Geology and Mineral Resources of the Ocean), Angliysky prospect 1, 190121 St. Petersburg, Russia Preface Arctic Coastal Dynamics (ACD) is a joint project of the International Arctic Sciences Committee (IASC) and the International Permafrost Association (IPA) and a regional project of IGBP-LOICZ (International Geosphere-Biosphere Programme – Land- Ocean Interactions in the Coastal Zone). Its overall objective is to improve our understanding of circum-Arctic coastal dynamics as a function of environmental forcing, coastal geology and cryology and morphodynamic behavior. The fourth IASC-sponsored ACD workshop was held in St. Petersburg, Russia, on November 10-13, 2003. Participants from Canada (7), Germany (7), Great Britain (2), the Netherlands (1), Norway (1), Russia (32), Ukraine (1) and the United States (8) attended. During the first part of the workshop, 63 papers dealing with regional and/or circum-Arctic coastal dynamics were presented. Based on the material presented, five thematic working groups were identified: (1) GIS working group to develop of a circum-Arctic coastal GIS system, (2) coastal permafrost working group to discuss processes involved in the transition of onshore to offshore permafrost, (3) biogeochemistry working group with the focus on transport and fate of eroded material (4) biodiversity working group to initiate planning of an Arctic Coastal Biodiversity research agenda, (5) environmental data working group to discuss coastal dynamics as a function of environmental forcing. -
UNITED STATES DEPARTMENT of the INTERIOR H. Mclean, R. Mcmullin, and M . B. Lynch Has Not Been Reviewed for Survey Editorial
UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY HYDROCARBON RESOURCE REPORT FOR PROPOSED OCS SALE NO. 83 NAVARIN BASIN, ALASKA M. S. Marlow, P. Carlson, A. K. Cooper, H. Karl, H. McLean, R. McMullin, and M. B. Lynch This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and nomenclature. Any use of trade names is for descriptive purposes only and does not constitute endorsement by the USGS . TABLE OF CONTENTS Summary I Introduction.................................................... 3 Location of Proposed Lease Area ..............................3 Publicly Available Data ....................................... 3 Framework Geology .........~..~.~~.~.~~~~~~~~..~.~.~~..~~.~.~~..*6 Regional Geologic Setting of the Northwestern Bering Sea Shelf ...................................................6 Geology of Western Alaska .....................................8 Geology of St. Lawrence and St . Matthew Islands ...............9 Geology of Eastern Siberia ..................................... 9 Structural Frame work and Evolution of Navarin Basin ............ 11 Seismic-Reflection Data ......................................I1 Profile A-B ...............................................11 Profile C-D ...............................................I6 Structure Contours ..........................................17 Geologic History .............................................21 Mesozoic Structural Trends ............................2 Cenozoic Subsidence .......................................22 -
Arctic Coastal Dynarnics Report of the 3Rd International Workshop University of Oslo (Norway) 2-5 December 2002
Arctic Coastal Dynarnics Report of the 3rd International Workshop University of Oslo (Norway) 2-5 December 2002 Edited by Volker Rachold, Jerry Brown, Steven Solomon and Johan Ludvig Sollid Ber. Polarforsch. Meeresforsch. 443 (2003) ISSN 1618 - 31 93 Volker Rachold, Alfred Wegener Institute, Research Unit Potsdam, Telegrafenberg A43, 14473 Potsdam, Gerrnany Jerry Brown, Inteinational Pennafrost Association, P.O. Box 7, Woods Hole, MA 02543, USA Steven Solomon, Geological Survey of Canada (Atlantic), Bedford Institute of Oceanography, P.O. Box 1006, 1 Challenger Drive, Dartmouth, NS Canada B2Y 4A2, Canada Johan Ludvig Sollid, Department of Physical Geography, University of Oslo, P.O. Box 1042, Blindem, N-0316 Oslo, Norway Preface Arctic Coastal Dynamics (ACD) is a joint project of the International Arctic Sciences Committee (IASC) and the International Pennafrost Association. Its overall objective is to improve our understanding of circum-Arctic coastal dynamics as a function of environmental forcing, coastal geology and cryology and mosphodynamic behavior. The third IASC-sponsored ACD workshop was held in Oslo, Norway, on December 2-5, 2002. Pasticipants from Canada (3), Germany (3), Great Bsitain (1), the Netherlands (1), Norway (6),Russia (1 l), Switzerland (1) and the United States (2) attended. The objective of the workshop was to review the Status of ACD according to the Science and Implementation Plan, with the main focus on the quantitative assessment of the sediment and organic carbon input to the Arctic Ocean through coastal erosion. Dusing the first past of the workshop, 29 Papers dealing with regional andlor circum-Arctic coastal dynamics were presented. Based on the material presented, three regional working groups and two circum-Arctic working groups were organized. -
Chukotka's Natural Heritage at a Glance
Rough-legged Hawk. for a living planet The Bering Sea Ecoregion CHUKOTKA’S Photo: Peter Grigorovich Chukotka, officially the Chukotsky NATURAL HERITAGE Autonomous Okrug, forms Russia’s north-eastern fron- AT A GLANCE tier. About half of the region’s 737,700 square kilometers lies above the Arctic Circle. The region’s landscape is domi- nated by alpine and arctic tundra, although small larch, pine, birch, poplar, and willow trees can grow in the valleys of larger rivers. More than 900 species of plants grow in Chukotka, The Bering Strait coast. including 400 Photo: Dennis Litovka species of moss and lichen. Polar bears, Thirty fresh- Wrangel Island. water fish species inhabit Chukotka’s inland lakes and streams. Photo: Gennady Smirnov There are 220 bird species in the region. The chilly waters washing the region’s shores provide important habitat for numerous marine mammals, while species such as brown bear, sable, lynx, ermine, mountain hare, and mink can be found in terrestrial habitats. Numerous rare and endangered species inhabit the Chukotsky Autonomous Okrug. Among those listed in the Red Data Book of the Russian Federation are the polar bear, bighorn sheep, narwhal, hump- back whale, finback whale, grey whale, blue whale, razor back, Photo: Arne Nævra, www.naturbilder.no and 24 bird species. Walruses, Wrangel Island. Native hunting party. Siberian dwarf pine. Tumanskaya River. Photo: Gennady Smirnov Photo: Gennady Smirnov Photo: Gennady Smirnov Photo: Gennady Smirnov CHUKOTKA’S PROTECTED AREAS Legend WWF high priority conservation areas Monuments of nature 0 50 100 150 km Subadult white-tailed sea eagle. Lebediny Federal Zoological Wildlife Refuge he Lebediny Federal Zoological Wildlife Refuge, between the Main and Anadyr TRivers, protects almost 400,000 hectares of wetland habitats, as well as the animal species inhabiting them. -
Alaska Interagency Sampling Plan
SAMPLING PROTOCOL FOR HIGHLY PATHOGENIC ASIAN H5N1 AVIAN INFLUENZA IN MIGRATORY BIRDS IN ALASKA Alaska Interagency HPAI Bird Surveillance Working Group March 1, 2006 Suggested citation: Alaska Interagency HPAI Bird Surveillance Working Group. 2006. Sampling protocol for highly pathogenic Asian H5N1 avian influenza in migratory birds in Alaska. Interagency planning report, Anchorage, AK. Interagency Avian Influenza Working Group Members: U.S. Geological Survey – Alaska Science Center, Anchorage, AK Craig Ely Paul Flint Thomas Fondell Robert Gill Colleen Handel Jerry Hupp John Pearce Margaret Petersen Joel Schmutz Lee Tibbitts David Ward U.S. Fish and Wildlife Service, Anchorage, AK Vernon Byrd Julian Fischer David Irons Richard Lanctot Robert Leedy Steve Matsuoka Russell Oates Robert Platte Deborah Rocque Kent Wohl Alaska Department of Fish and Game, Anchorage, AK Tom Rothe Photo credits: Front cover: Steller’s eider: Jeff Wasley; Dunlin: Robert Gill; Arctic Warbler and Glaucous Gull: Ted Swem; Inside cover: Spectacled eiders: William Larned Back cover: Northern pintail: Jeff Wasley INDEX Introduction 1 Rock Sandpiper 69 Steller’s Eider 4 Pacific Golden Plover 72 Northern Pintail 7 Buff-breasted Sandpiper 75 Lesser Snow Goose 11 Aleutian Tern 79 Emperor Goose 15 Glaucous-winged Gull 82 Spectacled Eider 18 Glaucous Gull 85 Black Brant 21 Gyrfalcon 88 Lesser Sandhill Crane 25 Eastern Yellow Wagtail 92 Tundra Swan 28 Arctic Warbler 96 Long-tailed Duck 31 Gray-cheeked Thrush 99 Aleutian Canada Goose 34 Pacific Common Eider 37 King Eider 41 Dunlin 44 Sharp-tailed Sandpiper 49 Bar-tailed Godwit 53 Ruddy Turnstone 56 Pectoral Sandpiper 59 Red Knot 63 Long-billed Dowitcher 66 SAMPLING PROTOCOL FOR HIGHLY PATHOGENIC ASIAN H5N1 AVIAN INFLUENZA IN MIGRATORY BIRDS IN ALASKA INTRODUCTION The highly pathogenic avian influenza referred to as Asian H5N1 continues to spread across the Asian continent. -
Summer-Temperature Evolution on the Kamchatka Peninsula, Russian Far East, During the Past 20,000 Years
Clim. Past Discuss., doi:10.5194/cp-2016-21, 2016 Manuscript under review for journal Clim. Past Published: 6 April 2016 c Author(s) 2016. CC-BY 3.0 License. Summer-temperature evolution on the Kamchatka Peninsula, Russian Far East, during the past 20,000 years Vera D. Meyer1,2, Jens Hefter1, Gerrit Lohmann1, Ralf Tiedemann1 and Gesine Mollenhauer1,2,3 1 Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Bremerhaven, 27570, Germany 5 2 Department of Geosciences University of Bremen, Bremen, 28359, Germany 3 MARUM- Centre for Environmental Sciences, University of Bremen, Bremen, 28359, Germany Correspondence to: V. D. Meyer ([email protected]) 10 Abstract. Little is known about the climate evolution on the Kamchatka Peninsula during the last deglaciation as existing climate records do not reach beyond 12 ka BP. In this study, a summer-temperature record for the past 20 ka is presented. Branched Glycerol Dialkyl Glycerol Tetraethers, terrigenous biomarkers suitable for continental air temperature reconstructions, were analyzed in a sediment core from the western continental margin off Kamchatka/marginal Northwest Pacific (NW Pacific). The record reveals that summer temperatures on Kamchatka during the Last Glacial Maximum (LGM) 15 equaled modern. We suggest that strong southerly winds associated with a pronounced North Pacific High pressure system over the subarctic NW Pacific accounted for the warm conditions. A comparison with outputs from an Earth System Model reveals discrepancies between model and proxy-based reconstructions for the LGM-temperature and atmospheric circulation in the NW Pacific realm. The deglacial temperature development is characterized by abrupt millennial-scale temperature oscillations. -
Late Quaternary Glaciations in Far NE Russia; Combining Moraines, Topography and Chronology to Assess Regional and Global Glaciation Synchrony
Late Quaternary glaciations in Far NE Russia; combining moraines, topography and chronology to assess regional and global glaciation synchrony Iestyn D. Barr & Chris D. Clark School of Geography, Queen Mary University of London, Mile End Road, London E1 4NS, UK Department of Geography, University of Sheffield, Winter Street, Sheffield S10 2TN, UK This is an author produced version of a paper published in Quaternary Science Reviews Published paper Barr, ID., Clark, CD. (2012) Late Quaternary glaciations in Far NE Russia; combining moraines, topography and chronology to assess regional and global glaciation synchrony. Quaternary Science Reviews, 53, 72-87. doi: 10.1016/j.quascirev.2012.08.004 http://www.sciencedirect.com/science/article/pii/S0277379112003046 1 Abstract During various periods of Late Quaternary glaciation, small ice-sheets, -caps, -fields and valley glaciers, occupied the mountains and uplands of Far NE Russia (including the Verkhoyansk, Suntar-Khayata, and Chersky Mountains; the Kolyma-Anyuy and Koryak Highlands; and much of the Kamchatka and Chukchi peninsulas). Here, the margins of former glaciers across this region are constrained through the comprehensive mapping of moraines from remote sensing data (Landsat 7 ETM+ satellite images; ASTER Global Digital Elevation Model (GDEM2); and Viewfinder Panorama DEM data). A total of 8414 moraines are mapped, and this record is integrated with a series of published age-estimates (n = 25), considered to chronologically-constrain former ice-margin positions. Geomorphological and chronological data are compiled in a Geographic Information System (GIS) to produce ‘best estimate’ reconstructions of ice extent during the global Last Glacial Maximum (gLGM) and, to a lesser degree, during earlier phases of glaciation. -
Geoberlin 2015 4—7 October 2015 | Annual Meeting of DGGV · DMG DYNAMIC EARTH · from Alfred Wegener to Today and Beyond
GeoBerlin 2015 4—7 October 2015 | Annual Meeting of DGGV · DMG DYNAMIC EARTH · from Alfred Wegener to today and beyond Abstracts Recommended Citation Wagner, J.; Elger, K. [Eds.] (2015) GeoBerlin2015 - Dynamic Earth from Alfred Wegener to today and beyond - Abstracts. Annual Meeting of DGGV and DMG, 4-7 October 2015, Berlin: GFZ German Research Centre for Geosciences. DOI: http://doi.org/10.2312/GFZ.LIS.2015.003 Disclaimer and Copyright Each author is responsible for the content of his or her abstract and has the copyright for his or her figures. Imprint Publisher Helmholtz Centre Potsdam GFZ German Research Centre for Geosciences Telegrafenberg 14473 Potsdam Published in Potsdam, Germany Editors Johannes Wagner Kirsten Elger DOI: http://doi.org/10.2312/GFZ.LIS.2015.003 Contents Welcome 1 Scientific Committee . 3 Plenary Lectures4 Dan McKenzie . The Lithospheric Structure of Pangea and Central Asia: The rules of craton assembly . 4 Maureen Raymo . Sea Level During Past Warm Periods - Rethinking the Bathtub Model 4 Barbara Romanowicz . Global mantle imaging in the age of high speed wavefield computations 5 Trond H. Torsvik . Paleomagnetism and Plate Tectonics . 5 Faszination Alfred Wegener: Leben, Aktivitäten und wissenschaftliche Leistungen7 A. M. Celâl Şengör . Das Weltbild der Geowissenschaften – von Alfred Wegener bis heute . 7 Kurt Stuewe . The Wegener Memorial Expedition to the Greenland Caledonides . 8 Wolfgang Jacoby . Wie dachte Alfred Wegener über die Ursachen der Kontinentalver- schiebung? . 8 Günther Schönharting . Die Wahrnehmung der Ideen von Alfred Wegener und Wladimir Köppen in der Öffentlichkeit – ein Stück Wissenschaftsgeschichte . 9 I Jörn Thiede . Waldimir Köppen, Alfred Wegener and Milutin Milankovitch, Early Pioneers and Partners in Paleoclimate Researchs . -
Wetlands in Russia
WETLANDS IN RUSSIA Volume 4 Wetlands in Northeastern Russia Compiled by A.V.Andreev Moscow 2004 © Wetlands International, 2004 All rights reserved. Apart from any fair dealing for the purpose of private study, research, criticism, or review (as permitted under the Copyright Designs and Patents Act 1988) no part of this publication may be reproduced, stored in a retrieval system or transmitted in any form or by any means, electronic, electrical, chemical, mechanical, optical, photocopying, recording or otherwise, without prior permission of the copyright holder. The production of this publication has been generously supported by the Ministry of Agriculture, Nature and Food Quality, The Netherlands Citation: Andreev, A.V. 2004. Wetlands in Russia, Volume 4: Wetlands in Northeastern Russia. Wetlands International–Russia Programme.198 pp. ISBN 90-5882-024-6 Editorial Board: V.O.Avdanin, V.G.Vinogradov, V.Yu. Iliashenko, I.E.Kamennova, V.G.Krivenko, V.A.Orlov, V.S.Ostapenko, V.E.Flint Translation: Yu.V.Morozov Editing of English text: D. Engelbrecht Layout: M.A.Kiryushkin Cover photograph: A.V.Andreev Designed and produced by KMK Scientific Press Available from: Wetlands International-Russia Programme Nikoloyamskaya Ulitsa, 19, stroeniye 3 Moscow 109240, Russia Fax: + 7 095 7270938; E-mail: [email protected] The presentation of material in this publication and the geographical designations employed do not imply the expression of any opinion whatsoever on the part of Wetlands International, concerning the legal status of any territory or area, -
USEFUL TERMS Josh Newell, Siberia Hotspot Program, Friends of the Earth - Japan
第3章 ロシア極東地域の森林保護地域の現状と課題 USEFUL TERMS Josh Newell, Siberia Hotspot Program, Friends of the Earth - Japan Siberia The term stems from the Tartar word sibir or sleeping land. To foreigners, the name usually refers to the vast stretch of Russia from the Ural Mountains in the west to the Pacific seacoast in the east. Russians, however, generally consider Siberia’s eastern edge to be a series of mountain ranges stretching from western Chita Oblast northward through western Yakutia to the Arctic Ocean. Beyond that lies what Russians call Dalniy vostok, the Far East. Russian Far East Geographers disagree on the exact boundaries of the Russian Far East. Some limit the region to areas affected by the monsoon climate and the Pacific Ocean, i.e., Primorskiy, Khabarovsk, Amur, Sakhalin, Magadan, Chukotka, and Kamchatka. Others, defining the RFE according to economic ties with the Pacific Rim, include the Republic of Yakutia and Chita Oblast. For this study, we have chosen to base our definition on areas that have strong economic ties to the Pacific Rim; therefore, we have included Yakutia, but not Chita Oblast. Krai, Oblast, Republic, Okrug Administrative divisions of the Russian Federation, similar to states in the U.S. A republic (such as the Republic of Yakutia) has, however, more autonomy from Moscow and greater leeway in paying taxes and fees to the capital. Republics are usually set up in regions that have a significant non-Russian indigenous population. All krais and oblasts technically have the same status with respect to the federal government, but, in practice, some regions have more autonomy from Moscow than do others. -
Russia (Eastern)
Important Bird Areas in Asia – Russia (Eastern) ■ RUSSIA (Eastern) LAND AREA1 10,339,000 km2 HUMAN POPULATION2 16,828,000 (2 per km2) NUMBER OF IBAs 169 TOTAL AREA OF IBAs c.345,000 km2 STATUS OF IBAs 41 protected; 29 partially protected; 99 unprotected Arctic tundra in northern Russia is immensely rich in breeding waterbirds, in particular waterfowl and shorebirds, for example on Belyaka spit at the mouth of Kolyuchin bay (IBA 87). (PHOTO: MINORU KASHIWAGI) KEY HABITATS AND BIRDS • Many coastal and inland wetlands in eastern Russia support large congregations of waterbirds on passage from their • The Arctic tundra in northern Russia (Biome AS01: Arctic tundra northern breeding grounds to their wintering areas, and certain and SA 087: Chukotski peninsula) is immensely rich in breeding wetlands in the tundra support large flocks of moulting waterbirds, in particular waterfowl and shorebirds, most of which waterfowl in late summer. The coastal wetlands around the Sea migrate to other parts of Asia and to Australasia outside the of Okhotsk and the northern Sea of Japan are the only breeding breeding season. Many waterbird species nest only in the tundra grounds of the threatened Steller’s Sea-eagle Haliaeetus pelagicus zone (and its interface with the taiga zone), including the and Spotted Greenshank Tringa guttifer, and the lower Amur threatened Lesser White-fronted Goose Anser erythropus, Red- and Ussuri floodplains in south-east Russia are important breasted Goose Branta ruficollis, Siberian Crane Grus leucogeranus breeding grounds for the threatened Oriental Stork Ciconia and Spoon-billed Sandpiper Eurynorhynchus pygmeus. boyciana, Baer’s Pochard Aythya baeri, Red-crowned Crane • The vast expanse of coniferous taiga forest (and associated Grus japonensis and probably Swinhoe’s Rail Coturnicops wetlands) that extends across Eastern Siberia, and the temperate exquisitus. -
A Review of Postglacial Emergence on Svalbard, Franz Josef Land and Novaya Zemlya, Northern Eurasia S.L
ARTICLE IN PRESS Quaternary Science Reviews 23 (2004) 1391–1434 A review of postglacial emergence on Svalbard, Franz Josef Land and Novaya Zemlya, northern Eurasia S.L. Formana,*, D.J. Lubinskib, O.! Ingolfsson! c, J.J. Zeebergd, J.A. Snydere, M.J. Siegertf, G.G. Matishovg a Department of Earth and Environmental Sciences, University of Illinois, Chicago, IL 60607, USA b Institute of Arctic and Alpine Research, The University of Colorado, Boulder, CO 80309-0450, USA c Department of Geology and Geography, University of Iceland, Is-101 Reykjav!ık, Iceland d Netherlands Institute for Fisheries Research, Haringkade 1, P.O. Box 68 1970 AB IJmuiden, The Netherlands e Department of Geology, Bowling Green State University, Bowling Green, OH 43403, USA f Bristol Glaciology Centre, School of Geographical Sciences University of Bristol, University Road, Bristol BSS 1SS, UK g Murmansk Marine Biological Institute, 17 Vladimirskaya Street, Murmansk 183010, Russia Abstract The pattern of postglacial emergence in the Barents Sea is pivotal to constraining the timing of deglaciation and extent and thickness of the last ice sheet in northern Eurasia. This review unites records of Holocene relative sea level from Svalbard, Franz Josef Land, and Novaya Zemlya to better understand the geometries of past ice sheet loads. Emergence data from northern Eurasia confine the maximum area of glacier loading to the northwestern Barents Sea, where >100 m of emergence is measured on Kongs^ya. Deglacial unloading commenced on western and northern Spitsbergen c. 13–12 14C ka ago, and by c. 10.5 14Cka on eastern Svalbard and more distal sites on Franz Josef Land and Novaya Zemlya.