VII. Magadan and Chukotka Regions Overview of the Regions Josh
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Title Post-Soviet Period Changes in Resource Utilization and Their
Post-Soviet Period Changes in Resource Utilization Title and Their Impact on Population Dynamics: Chukotka Autonomous Okrug Author(s) Litvinenko, Tamara Vitalyevna; Kumo, Kazuhiro Citation Issue Date 2017-08 Type Technical Report Text Version publisher URL http://hdl.handle.net/10086/28761 Right Hitotsubashi University Repository Center for Economic Institutions Working Paper Series No. 2017-3 “Post-Soviet Period Changes in Resource Utilization and Their Impact on Population Dynamics: Chukotka Autonomous Okrug” Tamara Vitalyevna Litvinenko and Kazuhiro Kumo August 2017 Center for Economic Institutions Working Paper Series Institute of Economic Research Hitotsubashi University 2-1 Naka, Kunitachi, Tokyo, 186-8603 JAPAN http://cei.ier.hit-u.ac.jp/English/index.html Tel:+81-42-580-8405/Fax:+81-42-580-8333 Post-Soviet Period Changes in Resource Utilization and Their Impact on Population Dynamics: Chukotka Autonomous Okrug Tamara Vitalyevna Litvinenko Institute of Geography, Russian Academy of Sciences Kazuhiro Kumo Institute of Economic Research, Hitotsubashi University, Japan Abstract This study examines changes that have occurred in the resource utilization sector and the impact of these changes on population dynamics in the Chukotka Autonomous Okrug during the post-Soviet period. This paper sheds light on the sorts of population-dynamics-related differences that have emerged in the region and how these differences relate to the use of natural resources and the ethnic composition of the population. Through this study, it was shown that changes have tended to be small in local areas where indigenous peoples who have engaged in traditional natural resource use for a large proportion of the population, while changes have been relatively large in areas where the proportion of non-indigenous people is high and the mining industry has developed. -
Lake Baikal Russian Federation
LAKE BAIKAL RUSSIAN FEDERATION Lake Baikal is in south central Siberia close to the Mongolian border. It is the largest, oldest by 20 million years, and deepest, at 1,638m, of the world's lakes. It is 3.15 million hectares in size and contains a fifth of the world's unfrozen surface freshwater. Its age and isolation and unusually fertile depths have given it the world's richest and most unusual lacustrine fauna which, like the Galapagos islands’, is of outstanding value to evolutionary science. The exceptional variety of endemic animals and plants make the lake one of the most biologically diverse on earth. Threats to the site: Present threats are the untreated wastes from the river Selenga, potential oil and gas exploration in the Selenga delta, widespread lake-edge pollution and over-hunting of the Baikal seals. However, the threat of an oil pipeline along the lake’s north shore was averted in 2006 by Presidential decree and the pulp and cellulose mill on the southern shore which polluted 200 sq. km of the lake, caused some of the worst air pollution in Russia and genetic mutations in some of the lake’s endemic species, was closed in 2009 as no longer profitable to run. COUNTRY Russian Federation NAME Lake Baikal NATURAL WORLD HERITAGE SERIAL SITE 1996: Inscribed on the World Heritage List under Natural Criteria vii, viii, ix and x. STATEMENT OF OUTSTANDING UNIVERSAL VALUE The UNESCO World Heritage Committee issued the following statement at the time of inscription. Justification for Inscription The Committee inscribed Lake Baikal the most outstanding example of a freshwater ecosystem on the basis of: Criteria (vii), (viii), (ix) and (x). -
Cretaceous Tectonics and Geological Environments in East Russia
Journal of Asian Earth Sciences 21 (2003) 967–977 www.elsevier.com/locate/jseaes Cretaceous tectonics and geological environments in East Russia G.L. Kirillova Institute of Tectonics and Geophysics, Far East Branch, Russian Academy of Sciences, 65 Kim Yu Chen Str., Khabarovsk 680000, Russian Federation Received 5 October 2000; revised 7 October 2001; accepted 26 April 2002 Abstract By the Late Jurassic, the northern part of the East Asian continental margin was diversified. Principal structural constituents were the Siberian (or North Asian) craton bounded on the east by a miogeosynclinal fold belt, a system of smaller ancient blocks, and a collage of terranes that had been attached to the craton from the east and southeast at different times. Such a diverse structural environment caused variability of Cretaceous landscapes and related sedimentary systems. Global processes of lithospheric plate interaction and related regional tectonic processes played a leading role in Cretaceous environmental changes in the continental margin of East Russia. During the Early Cretaceous, the oblique plate convergence produced a transform continental margin over a long period of time. During the Middle Albian, a collage of terranes were attached to the continental margin of East Russia. Then during the Late Albian period, the angle of convergence increased, subduction resumed, and a giant East Asian volcanic belt formed along the continental margin. This belt was morphologically represented by a chain of mountain ridges (up to 3000 m), thus creating a sublongitudinal tectonic and climatic zonation. The active continental margin with a typical environmental arrangement of marginal seas–island arcs–the open sea, persisted until the end of the Cretaceous. -
Gap Analysis in Support of Cpan: the Russian Arctic
CAFF Habitat Conservation Report No. 9 GAP ANALYSIS IN SUPPORT OF CPAN: THE RUSSIAN ARCTIC Igor Lysenko and David Henry CAFF INTERNATIONAL SECRETRARIAT 2000 This report, prepared by Igor Lysenko, World Conservation Monitoring Centre (WCMC) and David Henry, United Nations Environment Program (UNEP) Global Resource Information Database (GRID)-Arendal, is a technical account of a Gap Analysis Project conducted for the Russian Arctic in 1997-1999 in support of the Circumpolar Protected Areas Network (CPAN) of CAFF. It updates the status and spatial distribution of protected areas within the CAFF area of the Russian Federation and provides, in 22 GIs based maps and several data sets, a wealth of information relevant for present and future management decisions related to habitat conservation in the Russian Arctic. The present Gap Analysis for the Russian Arctic was undertaken in response to the CPAN Strategy and Action Plan requirement for countries to identify gaps in protected area coverage of ecosystems and species and to select sites for further action. Another important objective was to update the Russian data base. The Analysis used a system of twelve landscape units instead of the previously used vegetation zone system as the basis to classify Russia's ecosystems. A comparison of the terrestrial landscape systems against protected area coverage indicates that 27% of the glacier ecosystem is protected, 9.3% of the tundra (treeless portion) and 4.7% of the forest systems within the Arctic boundaries are under protection, but the most important Arctic forested areas have only 0.1% protection. In general, the analysis indicates a negative relationship between ecosystem productivity and protection, which is consistent with findings in 1996. -
Contemporary State of Glaciers in Chukotka and Kolyma Highlands ISSN 2080-7686
Bulletin of Geography. Physical Geography Series, No. 19 (2020): 5–18 http://dx.doi.org/10.2478/bgeo-2020-0006 Contemporary state of glaciers in Chukotka and Kolyma highlands ISSN 2080-7686 Maria Ananicheva* 1,a, Yury Kononov 1,b, Egor Belozerov2 1 Russian Academy of Science, Institute of Geography, Moscow, Russia 2 Lomonosov State University, Faculty of Geography, Moscow, Russia * Correspondence: Russian Academy of Science, Institute of Geography, Moscow, Russia. E-mail: [email protected] a https://orcid.org/0000-0002-6377-1852, b https://orcid.org/0000-0002-3117-5554 Abstract. The purpose of this work is to assess the main parameters of the Chukotka and Kolyma glaciers (small forms of glaciation, SFG): their size and volume, and changes therein over time. The point as to whether these SFG can be considered glaciers or are in transition into, for example, rock glaciers is also presented. SFG areas were defined from the early 1980s (data from the catalogue of the glaciers compiled by R.V. Sedov) to 2005, and up to 2017: these data were retrieved from sat- Key words: ellite images. The maximum of the SGF reduction occurred in the Chantalsky Range, Iskaten Range, Chukotka Peninsula, and in the northern part of Chukotka Peninsula. The smallest retreat by this time relates to the gla- Kolyma Highlands, ciers of the southern part of the peninsula. Glacier volumes are determined by the formula of S.A. satellite image, Nikitin for corrie glaciers, based on in-situ volume measurements, and by our own method: the av- climate change, erage glacier thickness is calculated from isogypsum patterns, constructed using DEMs of individu- glacier reduction, al glaciers based on images taken from a drone during field work, and using ArcticDEM for others. -
Helicobacter Pylori's Historical Journey Through Siberia and the Americas
Helicobacter pylori’s historical journey through Siberia and the Americas Yoshan Moodleya,1,2, Andrea Brunellib,1, Silvia Ghirottoc,1, Andrey Klyubind, Ayas S. Maadye, William Tynef, Zilia Y. Muñoz-Ramirezg, Zhemin Zhouf, Andrea Manicah, Bodo Linzi, and Mark Achtmanf aDepartment of Zoology, University of Venda, Thohoyandou 0950, Republic of South Africa; bDepartment of Life Sciences and Biotechnology, University of Ferrara, 44121 Ferrara, Italy; cDepartment of Mathematics and Computer Science, University of Ferrara, 44121 Ferrara, Italy; dDepartment of Molecular Biology and Genetics, Research Institute for Physical-Chemical Medicine, 119435 Moscow, Russia; eDepartment of Diagnostic and Operative Endoscopy, Pirogov National Medical and Surgical Center, 105203 Moscow, Russia; fWarwick Medical School, University of Warwick, Coventry CV4 7AL, United Kingdom; gLaboratorio de Bioinformática y Biotecnología Genómica, Escuela Nacional de Ciencias Biológicas, Unidad Profesional Lázaro Cárdenas, Instituto Politécnico Nacional, 11340 Mexico City, Mexico; hDepartment of Zoology, University of Cambridge, Cambridge CB2 3EJ, United Kingdom; and iDepartment of Biology, Division of Microbiology, Friedrich Alexander University Erlangen-Nuremberg, 91058 Erlangen, Germany Edited by Daniel Falush, University of Bath, Bath, United Kingdom, and accepted by Editorial Board Member W. F. Doolittle April 30, 2021 (received for review July 22, 2020) The gastric bacterium Helicobacter pylori shares a coevolutionary speakers). However, H. pylori’s presence, diversity, and structure history with humans that predates the out-of-Africa diaspora, and in northern Eurasia are still unknown. This vast region, hereafter the geographical specificities of H. pylori populations reflect mul- Siberia, extends from the Ural Mountains in the west to the tiple well-known human migrations. We extensively sampled H. -
Sources and Pathways 4.1
Chapter 4 Persistant toxic substances (PTS) sources and pathways 4.1. Introduction Chapter 4 4.1. Introduction 4.2. Assessment of distant sources: In general, the human environment is a combination Longrange atmospheric transport of the physical, chemical, biological, social and cultur- Due to the nature of atmospheric circulation, emission al factors that affect human health. It should be recog- sources located within the Northern Hemisphere, par- nized that exposure of humans to PTS can, to certain ticularly those in Europe and Asia, play a dominant extent, be dependant on each of these factors. The pre- role in the contamination of the Arctic. Given the spa- cise role differs depending on the contaminant con- tial distribution of PTS emission sources, and their cerned, however, with respect to human intake, the potential for ‘global’ transport, evaluation of long- chain consisting of ‘source – pathway – biological avail- range atmospheric transport of PTS to the Arctic ability’ applies to all contaminants. Leaving aside the region necessarily involves modeling on the hemi- biological aspect of the problem, this chapter focuses spheric/global scale using a multi-compartment on PTS sources, and their physical transport pathways. approach. To meet these requirements, appropriate modeling tools have been developed. Contaminant sources can be provisionally separated into three categories: Extensive efforts were made in the collection and • Distant sources: Located far from receptor sites in preparation of input data for modeling. This included the Arctic. Contaminants can reach receptor areas the required meteorological and geophysical informa- via air currents, riverine flow, and ocean currents. tion, and data on the physical and chemical properties During their transport, contaminants are affected by of both the selected substances and of their emissions. -
Transboudary Cooperation of Russian Cooperation Of
MINISTRY OF NATURAL RESOURCES AND ENVIRONMENT OF THE RUSSIAN FEDERATION Dauria International Protected TRANSBOUDARY Area Daursky Biosphere Reserve COOPERATION OF RUSSIAN OLGA KIRILYUK [email protected] PROTECTED AREAS TRANSBOUDARY COOPERATION OF RUSSIAN PROTECTED AREAS RF 2 The Russian Federation has a longest national borders in the World and https://en.wikipedia.org/wiki/Protected_area cross the different types of ecosystems Russia (Russian Federation) is one of the largest country in the world. RF shares land and maritime borders with more than 15 countries. Total length of borders is 62, 269 km. State borders cross several terrestrial and marine ecosystem types: from arctic to subtropical. Total area of all Russian PA is about 207 million hectares (11,4% ). Along Russian border territories are a lot of Protected areas among them about 30 are federal level PAs of I-IV categories of IUCN classification. Many of them have international significance (status). TRANSBOUDARY COOPERATION OF RUSSIAN PROTECTED AREAS 1 3 5 3 2 4 3. Only 5 official 1. “Friendship” (USSR-Finland), 1989; 2. Dauria (Russia-Mongolia-China), 1994; transboundary protected 3. “Ubsunur Hollow” (Russia-Mongolia), areas were created by 2003; intergovernmental 4. “Khanka Lake” (Russia-China), 2006; agreement: 5. “Altay” (Russia-Kazahstan), 2011. TRANSBOUDARY COOPERATION OF RUSSIAN PROTECTED AREAS 4 Russian - Finnish zapovednik «Friendship» Protects the boreal forest ecosystems •Kostomukshsky zapovednik (Russia), •Metsahalitus Forstyrelsen PA (Finland) Main aim of creation: -
Migration: on the Move in Alaska
National Park Service U.S. Department of the Interior Alaska Park Science Alaska Region Migration: On the Move in Alaska Volume 17, Issue 1 Alaska Park Science Volume 17, Issue 1 June 2018 Editorial Board: Leigh Welling Jim Lawler Jason J. Taylor Jennifer Pederson Weinberger Guest Editor: Laura Phillips Managing Editor: Nina Chambers Contributing Editor: Stacia Backensto Design: Nina Chambers Contact Alaska Park Science at: [email protected] Alaska Park Science is the semi-annual science journal of the National Park Service Alaska Region. Each issue highlights research and scholarship important to the stewardship of Alaska’s parks. Publication in Alaska Park Science does not signify that the contents reflect the views or policies of the National Park Service, nor does mention of trade names or commercial products constitute National Park Service endorsement or recommendation. Alaska Park Science is found online at: www.nps.gov/subjects/alaskaparkscience/index.htm Table of Contents Migration: On the Move in Alaska ...............1 Future Challenges for Salmon and the Statewide Movements of Non-territorial Freshwater Ecosystems of Southeast Alaska Golden Eagles in Alaska During the A Survey of Human Migration in Alaska's .......................................................................41 Breeding Season: Information for National Parks through Time .......................5 Developing Effective Conservation Plans ..65 History, Purpose, and Status of Caribou Duck-billed Dinosaurs (Hadrosauridae), Movements in Northwest -
Living in Two Places : Permanent Transiency In
living in two places: permanent transiency in the magadan region Elena Khlinovskaya Rockhill Scott Polar Research Institute, University of Cambridge, Lensfield Road, Cambridge CB2 1ER, UK; [email protected] abstract Some individuals in the Kolyma region of Northeast Russia describe their way of life as “permanently temporary.” This mode of living involves constant movements and the work of imagination while liv- ing between two places, the “island” of Kolyma and the materik, or mainland. In the Soviet era people maintained connections to the materik through visits, correspondence and telephone conversations. Today, living in the Kolyma means living in some distant future, constantly keeping the materik in mind, without fully inhabiting the Kolyma. People’s lives embody various mythologies that have been at work throughout Soviet Kolyma history. Some of these models are being transformed, while oth- ers persist. Underlying the opportunities afforded by high mobility, both government practices and individual plans reveal an ideal of permanency and rootedness. KEYWORDS: Siberia, gulag, Soviet Union, industrialism, migration, mobility, post-Soviet The Magadan oblast’1 has enjoyed only modest attention the mid-seventeenth century, the history of its prishloye in arctic anthropology. Located in northeast Russia, it be- naseleniye3 started in the 1920s when the Kolyma region longs to the Far Eastern Federal Okrug along with eight became known for gold mining and Stalinist forced-labor other regions, okrugs and krais. Among these, Magadan camps. oblast' is somewhat peculiar. First, although this territory These regional peculiarities—a small indigenous pop- has been inhabited by various Native groups for centu- ulation and a distinct industrial Soviet history—partly ries, compared to neighboring Chukotka and the Sakha account for the dearth of anthropological research con- Republic (Yakutia), the Magadan oblast' does not have a ducted in Magadan. -
Spanning the Bering Strait
National Park service shared beringian heritage Program U.s. Department of the interior Spanning the Bering Strait 20 years of collaborative research s U b s i s t e N c e h UN t e r i N c h UK o t K a , r U s s i a i N t r o DU c t i o N cean Arctic O N O R T H E L A Chu a e S T kchi Se n R A LASKA a SIBERIA er U C h v u B R i k R S otk S a e i a P v I A en r e m in i n USA r y s M l u l g o a a S K S ew la c ard Peninsu r k t e e r Riv n a n z uko i i Y e t R i v e r ering Sea la B u s n i CANADA n e P la u a ns k ni t Pe a ka N h las c A lf of Alaska m u a G K W E 0 250 500 Pacific Ocean miles S USA The Shared Beringian Heritage Program has been fortunate enough to have had a sustained source of funds to support 3 community based projects and research since its creation in 1991. Presidents George H.W. Bush and Mikhail Gorbachev expanded their cooperation in the field of environmental protection and the study of global change to create the Shared Beringian Heritage Program. -
Arctic Marine Aviation Transportation
SARA FRENCh, WAlTER AND DuNCAN GORDON FOundation Response CapacityandSustainableDevelopment Arctic Transportation Infrastructure: Transportation Arctic 3-6 December 2012 | Reykjavik, Iceland 3-6 December2012|Reykjavik, Prepared for the Sustainable Development Working Group Prepared fortheSustainableDevelopment Working By InstituteoftheNorth,Anchorage, Alaska,USA PROCEEDINGS: 20 Decem B er 2012 ICElANDIC coast GuARD INSTITuTE OF ThE NORTh INSTITuTE OF ThE NORTh SARA FRENCh, WAlTER AND DuNCAN GORDON FOundation Table of Contents Introduction ................................................................................ 5 Acknowledgments ......................................................................... 6 Abbreviations and Acronyms .......................................................... 7 Executive Summary ....................................................................... 8 Chapters—Workshop Proceedings................................................. 10 1. Current infrastructure and response 2. Current and future activity 3. Infrastructure and investment 4. Infrastructure and sustainable development 5. Conclusions: What’s next? Appendices ................................................................................ 21 A. Arctic vignettes—innovative best practices B. Case studies—showcasing Arctic infrastructure C. Workshop materials 1) Workshop agenda 2) Workshop participants 3) Project-related terminology 4) List of data points and definitions 5) List of Arctic marine and aviation infrastructure AlASkA DepartmENT OF ENvIRONmental