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The Island Monastery of Valaam in Finnish Homeland Tourism: Constructing a “Thirdspace” in the Russian Borderlands
The island monastery of Valaam in Finnish homeland tourism: Constructing a “Thirdspace” in the Russian borderlands MAJA MIKULA Mikula, Maja (2013). The island monastery of Valaam in Finnish homeland tour- ism: Constructing a “Thirdspace” in the Russian borderlands. Fennia 191: 1, pp. 14–24. ISSN 1798-5617. The Orthodox island monastery of Valaam in Russian Karelia is today a popular destination for Finnish tourists visiting Russia’s western borderlands. Many of these tourists are descendants of the Karelians who had evacuated the area fol- lowing World War II. The monastery’s institutionally sanctioned genealogies construct it as the civilizing force, which had brought Christian enlightenment to the local heathen population. This discursive template is played out in the way the place is presented to visitors, with each highlight telling a carefully con- structed story that promotes the monastery’s significance for the Russian reli- gious and national identity. Yet, drawing on lived experience, as well as on popular culture, family lore and meanings from collective memory, the Finnish visitors break the monolithic official discourse and produce a complex “third- space” in their own measure. This paper is based on participant observation and semi-structured interviews conducted during a homeland visit to Ladogan Kare- lia in June 2010. Keywords: homeland tourism, Valaam, Karelia, Finland, Russia, borderlands, “thirdspace” Maja Mikula, Faculty of Arts and Social Sciences, University of Technology Sydney, PO Box 123, Broadway NSW 2007, Australia. E-mail: [email protected]. Introduction A flagship of the budding tourism industry in Russian Karelia (see, e.g., Nilsson 2004), Val- At the northeastern fringes of Europe, Ladogan aam is today a popular destination for Finnish Karelia is a place where visible traces of a trau- tourists visiting Russia’s western borderlands. -
Large Russian Lakes Ladoga, Onega, and Imandra Under Strong Pollution and in the Period of Revitalization: a Review
geosciences Review Large Russian Lakes Ladoga, Onega, and Imandra under Strong Pollution and in the Period of Revitalization: A Review Tatiana Moiseenko 1,* and Andrey Sharov 2 1 Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences, 119991 Moscow, Russia 2 Papanin Institute for Biology of Inland Waters, Russian Academy of Sciences, 152742 Yaroslavl Oblast, Russia; [email protected] * Correspondence: [email protected] Received: 8 October 2019; Accepted: 20 November 2019; Published: 22 November 2019 Abstract: In this paper, retrospective analyses of long-term changes in the aquatic ecosystem of Ladoga, Onega, and Imandra lakes, situated within North-West Russia, are presented. At the beginning of the last century, the lakes were oligotrophic, freshwater and similar in origin in terms of the chemical composition of waters and aquatic fauna. Three stages were identified in this study: reference condition, intensive pollution and degradation, and decreasing pollution and revitalization. Similar changes in polluted bays were detected, for which a significant decrease in their oligotrophic nature, the dominance of eurybiont species, their biodiversity under toxic substances and nutrients, were noted. The lakes have been recolonized by northern species following pollution reduction over the past 20 years. There have been replacements in dominant complexes, an increase in the biodiversity of communities, with the emergence of more southern forms of introduced species. The path of ecosystem transformation during and after the anthropogenic stress compares with the regularities of ecosystem successions: from the natural state through the developmental stage to a more stable mature modification, with significantly different natural characteristics. A peculiarity of the newly formed ecosystems is the change in structure and the higher productivity of biological communities, explained by the stability of the newly formed biogeochemical nutrient cycles, as well as climate warming. -
Agriculture and Land Use in the North of Russia: Case Study of Karelia and Yakutia
Open Geosciences 2020; 12: 1497–1511 Transformation of Traditional Cultural Landscapes - Koper 2019 Alexey Naumov*, Varvara Akimova, Daria Sidorova, and Mikhail Topnikov Agriculture and land use in the North of Russia: Case study of Karelia and Yakutia https://doi.org/10.1515/geo-2020-0210 Keywords: Northern regions, land use, changes, agricul- received December 31, 2019; accepted November 03, 2020 tural development, agriculture, Russia, Karelia, Yakutia Abstract: Despite harsh climate, agriculture on the northern margins of Russia still remains the backbone of food security. Historically, in both regions studied in this article – the Republic of Karelia and the Republic 1 Introduction of Sakha (Yakutia) – agricultural activities as dairy - farming and even cropping were well adapted to local This article is based on the case study of two large admin – conditions including traditional activities such as horse istrative regions of Russian Federation the Republic of ( ) breeding typical for Yakutia. Using three different Karelia furthermore Karelia and the Republic of Sakha sources of information – official statistics, expert inter- (Yakutia). Territory of both regions is officially considered views, and field observations – allowed us to draw a in Russia as the Extreme North. This notion applies to the conclusion that there are both similarities and differ- whole territory of Yakutia, the largest unit of Russian ences in agricultural development and land use of these Federation and also the largest administrative region two studied regions. The differences arise from agro- worldwide with 3,084 thousand km2 land area. Five ad- climate conditions, settlement history, specialization, ministrative districts (uluses) of Yakutia have an access and spatial pattern of economy. -
Fish and Fishing in Karelia Удк 597.2/.5+639.2(470.2) Ббк 28.693.32.(2Рос.Кар.) I-54
FISH AND FISHING IN KARELIA УДК 597.2/.5+639.2(470.2) ББК 28.693.32.(2Рос.Кар.) I-54 ISBN 978-5-9274-0651-7 © Karelian research centre RAS, 2014 FISH AND FISHING IN KARELIA N.V. ILMAST, O.P. STERLIGOVA, D.S. SAVOSIN PETROZAVODSK 2014 CHARACTERISTICS OF THE FRESHWATER FISH FAUNA OF KARELIA Karelian waters belong to drainage basins of two seas: the Baltic and the White Sea. The watershed between them runs across the central part of the republic. The hydrographic network is made up of numerous rivers and lakes grouped together into lake-river systems. The republic comprises nearly 50% of the water area of Lake Ladoga and 80% of Lake Onega, which are the biggest freshwater bodies in Europe. If lakes Onega and Ladoga are included, the lake cover of the territory (the ratio of the surface area of all lakes and the land area) is 21%. This is one of the highest values in the world. Migratory and salt-water fishes in Karelian waters are of marine origin, and the rest are of freshwater origin. Colonization of the region by freshwater fish fauna proceeded from south to north as the glacier was retreating. More thermophilic species (cyprinids, percids, etc.) colonized the waters some 10000 years B.P., and cold-loving species (salmons, chars, whitefishes, etc.) – even earlier. Contemporary freshwater fish fauna in Karelia comprises 44 fish species, excluding the typically marine species that enter the lower reaches of the rivers emptying into the White Sea (European plaice, Arctic flounder, navaga), farm-reared species (pink salmon, common carp, rainbow trout, longnose sucker, muksun, Arctic cisco, broad whitefish, northern (peled) whitefish, nelma/inconnu), as well as some accidental species (European flounder). -
Translation Series No.2137
FISHERIES RESEARCH BOARD OF CANADA Translation Series No. 2137 • Salmon of Lake Onega • by YU. A. Smirnov -Original title: •Losost onezhskogo ozera Biologiya vosproiFvodstvo ispOliziovapie From: Lososi onezhskogo ozera Biolop.iya vosproizvodstvc* ispoll .zovanie (Salmon of Lake Onega), : 1-143, 1Q71 Translated by the Translation Bureau-( PH) . Foreign Languages Division Department of the Secretary of . State of Canada Department of the-Environment- Fisheries Research Board of Canada Biological Station. Nanaimd, b... Biological Station, St. Andrews, X. S. Biological Station, St. John's, Nfld. 19 72 195 & pages typescript lleibliography 7:7 1 OF THE SECRETARY OF STATE s E DEPAR'RENT c R F.Pr r; D'iT A T • TRANSLATION BUREAU bUREAU DES RADUCTIONS N iq E DES, E LANGUES GAN A DA. 1C D!.\fî5i N L. TA9SLATED FROM — TRADUCTION DE INTO — EN Fusq .d. P.n Elish AU rtiop. AuTuun rnov Yu. "FITLE FI•LISH — TITRE ANGLAIS salmon of Lake Onega l bioloy reprouction - utilizetion Title in foreign language (transliterate foreign characters) Loos' onezhskoiy) ozera biolos,j_ya vosproizvoCts1;vo ispol";:.ovP.nie ------ RE'FrE..- RENCE IN FOREIGN LANGUAGE (NAME OF BOOK OR PUBLICATION) IN FULL. TRANSLITERATE FOREIG4 CHA.RACTERS. rzr,-FE,.PENCE EN LANGUE ÉTRANGÉRE (NOM DU LIVRE OU PUBLICATION), AU COMPLET. TRANSCRIRE EN CARACTÉFiES PHONÉTIQUES. • REFERENcE IN ENGLISH — RÉFÉRENCE EN ANGLAIS Ao above PUBLISH ER —.ÉDITEUR PAGE NUMBERS IN ORIGINAL DATE OF PUBLICATION NUMÉROS DES PAGES DANS DATE DE PUBLICATION L'ORIGINAL yauka Press 3 143 YEAR ISSUE NO. VOLUME ANNÉE NUMERO PLACE OF PUBLICATION NUMBER OF TYPED PAGES LIEU DE PUBLICATION NOMBRE DE-PAGES DAÇTYLOGRAPHIÉEs 195 (exclusive of Lenirw.rad IWR 1971 Bibliographmj REQUESTING DEPARTMENT Environment TRANSLATION BUREAU NO. -
The Ponto-Caspian Basin As a Final Trap for Southeastern Scandinavian Ice-Sheet Meltwater
Quaternary Science Reviews 148 (2016) 29e43 Contents lists available at ScienceDirect Quaternary Science Reviews journal homepage: www.elsevier.com/locate/quascirev The Ponto-Caspian basin as a final trap for southeastern Scandinavian Ice-Sheet meltwater * Alina Tudryn a, , Suzanne A.G. Leroy b, Samuel Toucanne c, Elisabeth Gibert-Brunet a, Piotr Tucholka a, Yuri A. Lavrushin d, Olivier Dufaure a, Serge Miska a, Germain Bayon c a GEOPS, Univ. Paris-Sud, CNRS, Universite Paris-Saclay, Rue du Belvedere, Bat.^ 504-509, 91405, Orsay, France b Environmental Science, Brunel University London, Uxbridge, UB8 3PH, London, UK c Institut Français de Recherche pour l’Exploitation de la Mer (IFREMER), Unite de Recherche Geosciences Marines, F-29280, Plouzane, France d Geological Institute (GIN), Russian Academy of Sciences, Pyzhevskii per. 7, Moscow, 117036, Russia article info abstract Article history: This paper provides new data on the evolution of the Caspian Sea and Black Sea from the Last Glacial Received 23 December 2015 Maximum until ca. 12 cal kyr BP. We present new analyses (clay mineralogy, grain-size, Nd isotopes and Received in revised form pollen) applied to sediments from the river terraces in the lower Volga, from the middle Caspian Sea and 23 June 2016 from the western part of the Black Sea. The results show that during the last deglaciation, the Ponto- Accepted 29 June 2016 Caspian basin collected meltwater and fine-grained sediment from the southern margin of the Scandi- navian Ice Sheet (SIS) via the Dniepr and Volga Rivers. It induced the deposition of characteristic red- brownish/chocolate-coloured illite-rich sediments (Red Layers in the Black Sea and Chocolate Clays in Keywords: Caspian sea the Caspian Sea) that originated from the Baltic Shield area according to Nd data. -
Distribution and Significance of Alien Amphipods and Decapods in The
IS.RIVERS 2012 C1 – INVASIVES / INVASIVE SPECIES Distribution and significance of alien amphipods and decapods in the Neva river basin (North-western Russia) Répartition et effets des espèces exotiques amphipodes et décapodes dans le bassin du Neva Nadezhda Berezina 1, 2, Viktor Petryashev1, Natalia Kalinkina2 and 2 Andrey Sharov 1 - Zoological Institute of the Russian Academy of sciences, Universitetskaya emb. 1, Saint Petersburg 199034, Russia ([email protected]; [email protected]); 2 - Northern Water Problems Institute, Karelian Research Centre, Russian Academy of sciences, Alexander Nevskyi prospect 50, Petrozavodsk 185003 ([email protected]; [email protected]) RÉSUMÉ Le fleuve Neva, en reliant le bassin Ponto-Caspien au sud et la mer Baltique et les écosystemes aquatiques du nord de la Russie, fait partie du corridor nord des invasions biologiques. Ce papier est centré sur l’histoire récente des invasions par les crustacés malacostracés (Amphipodes et Décapodes) dans le bassin du Neva (le plus grand fleuve du nord-est de la Russie). Ce papier analyse nos données et celles de la littérature concernant la distribution géographique des invasifs dans le bassin du Neva (essentiellement six espèces Chelicorophium curvispinum, Pontogammarus robustoides, Gmelinoides fasciatus, Gammarus tigrinus, Eriocheir sinensis et Astacus leptodactylus). Nous discutons également de l’histoire des invasions par ces espèces exotiques, les vecteurs possibles de leur extension à partir de leur aire d’origine mais aussi l’effet potentiel des interactions trophiques entre les amphipodes et les décapodes exotiques et les espèces natives. Les principales voies d’invasions dans la mer Baltique à partir des différents bassins sont liées aux activités humaines (principalement liées à la création de continuum rivières-canaux/corridors d’invasions et introduction volontaire/commerce). -
Monthly Discharges for 2400 Rivers and Streams of the Former Soviet Union [FSU]
Annotations for Monthly Discharges for 2400 Rivers and Streams of the former Soviet Union [FSU] v1.1, September, 2001 Byron A. Bodo [email protected] Toronto, Canada Disclaimer Users assume responsibility for errors in the river and stream discharge data, associated metadata [river names, gauge names, drainage areas, & geographic coordinates], and the annotations contained herein. No doubt errors and discrepancies remain in the metadata and discharge records. Anyone data set users who uncover further errors and other discrepancies are invited to report them to NCAR. Acknowledgement Most discharge records in this compilation originated from the State Hydrological Institute [SHI] in St. Petersburg, Russia. Problems with some discharge records and metadata notwithstanding; this compilation could not have been created were it not for the efforts of SHI. The University of New Hampshire’s Global Hydrology Group is credited for making the SHI Arctic Basin data available. Foreword This document was prepared for on-screen viewing, not printing !!! Printed output can be very messy. To ensure wide accessibility, this document was prepared as an MS Word 6 doc file. The www addresses are not active hyperlinks. They have to be copied and pasted into www browsers. Clicking on a page number in the Table of Contents will jump the cursor to the beginning of that section of text [in the MS Word version, not the pdf file]. Distribution Files Files in the distribution package are listed below: Contents File name short abstract abstract.txt ascii description of -
Contacts and Networks in the Baltic Sea Region
11 CROSSING BOUNDARIES Bertell, Frog & Willson (eds) Contacts and Networks in the Baltic Sea Region Sea Baltic the in Networks and Contacts Edited by Maths Bertell, Frog, and Kendra Willson Contacts and Networks in the Baltic Sea Region Austmarr as a Northern mare nostrum, ca. 500-1500 ad FOR PRIVATE AND NON-COMMERCIAL USE AMSTERDAM UNIVERSITY PRESS Contacts and Networks in the Baltic Sea Region FOR PRIVATE AND NON-COMMERCIAL USE AMSTERDAM UNIVERSITY PRESS Crossing Boundaries Turku Medieval and Early Modern Studies The series from the Turku Centre for Medieval and Early Modern Studies (TUCEMEMS) publishes monographs and collective volumes placed at the intersection of disciplinary boundaries, introducing fresh connections between established fields of study. The series especially welcomes research combining or juxtaposing different kinds of primary sources and new methodological solutions to deal with problems presented by them. Encouraged themes and approaches include, but are not limited to, identity formation in medieval/early modern communities and the analysis of texts and other cultural products as a communicative process comprising shared symbols and meanings. Series Editor Matti Peikola, University of Turku, Finland Editorial Board Matti Peikola, Department of Modern Languages, University of Turku (Editor- in-chief) Janne Harjula, Adjunct Professor of Historical Archaeology, University of Turku Johanna Ilmakunnas, Acting Professor of Finnish History, School of History, Culture and Arts Studies, University of Turku Hemmo Laiho, Postdoctoral Researchers, Department of Philosophy, University of Turku Satu Lidman, Adjunct Professor of History of Criminal law, Faculty of Law/Legal History, University of Turku Aino Mäkikalli, Postdoctoral Researcher, Department of Comparative Literature, University of Turku Kirsi-Maria Nummila, Adjunct Professor of Finnish language, University of Turku; University Lecturer of Finnish, University of Helsinki. -
2Ndexcurtion Day. August 22 TRIP to GIRVAS Shelekhova, T.S., Svetov
2nd excurtion day. August 22 TRIP TO GIRVAS Shelekhova, T.S., Svetov, S.A., Medvedev, P.V. FIC KarRC RAS Institute of Geology, Karelian Research Centre, RAS, Petrozavodsk, Pushkinskaya str., 11, RUSSIA E-mail: [email protected] Stop 1. Sulazhgora (Sulazh Hill) glaciofluvial delta The delta is located in the northern environs of Petrozavodsk. Standing on the top of the hill, a visitor will enjoy a spectacular view of the Shuya Lowland (40-75 m.a.s.l.) and the Solomennoye denudation ridge (122m.a.s.l.). The delta consists dominantly of ca.40 m thick sandy, occasionally gravel sediments. In the southern part of the delta, deltaic sediments are covered by ablation till. The laminae dip at 15 to 40 degrees. The material was transported from west to east. This big delta evolved in Middle Dryas (Neva cold stage) - early Allerod time, when the ice front rimmed the northern and eastern slopes of the so-called Olonets denudation uplift at an altitude of 120-313 m.a.s.l. The Shuya Lowland was already ice-free at this time and was covered by meltwater from Shuya Ice Lake. The lake had an outlet to the east into Onega Ice Lake located in the southern part of modern Lake Onega and adjacent lowlands. Delta was formed between the ice front on the north and bedrock uplift on the south. It looks like a glaciofluvial terrace, 3 km in length and up to 2 km in width. The maximum altitude of the delta is 117 m.a.s.l. It shows the maximal level of Onega Ice Lake at this time. -
Waterways of Russia St
distinguished travel for more than 35 years OF Waterways Russia St. Petersburg u Moscow FINLAND Kizhi Island Lake Lake Ladoga Onega Svirstroy iver R St. Petersburg ir Lake Beloye v S Gulf of Finland Neva River Goritsy Sheksna River Volga-Baltic Waterway Lake Rybinskoye Yaroslavl lga River RUSSIA Vo Uglich UNESCO World Moscow Canal Heritage Site Cruise Itinerary Air Routing Moscow Moscow River July 21 to August 1, 2021 Experience the legendary traditional folklore of Russia, St. Petersburg u Svirstroy u Kizhi Island as it unfolds along the picturesque rivers, lakes and Goritsy u Yaroslavl u Uglich u Moscow canals that link St. Petersburg with Moscow. Cruise for 1 Depart the U.S. six nights aboard the exclusively chartered, deluxe, 2-4 St. Petersburg, Russia 90 passenger Volga Dream. Spend three nights in 5 St. Petersburg/Embark Volga Dream Five‑Star accommodations in St. Petersburg and one night 6 Neva River/Lake Ladoga/Svirstroy/ in Moscow. Enjoy an early entrance guided tour of the Svir River/Lake Onega State Hermitage Museum and visits to Catherine 7 Kizhi Island/Lake Onega Palace in Pushkin and Peterhof. Explore Russia’s 8 Lake Beloye/Goritsy/Sheksna River heartland in 10th‑century Uglich and medieval Yaroslavl, 9 Lake Rybinskoye/Yaroslavl the 14th‑century Kirillo‑Belozersky monastery near Goritsy and the open‑air museum of Kizhi Island. 10 Uglich/Volga River Savor traditional Russian tea and cakes in a Svirstroy 11 Moscow/Disembark ship villager’s home. Moscow Post‑Program Option. 12 Moscow/Return to the U.S. Itinerary is subject to change. Exclusively Chartered Deluxe River Ship Volga Dream Waterways of Russia Included Features* In St. -
Amended Draft Decision 44 COM 8B.44
World Heritage 44 COM AMENDMENT WHC/21/44.COM/8B Nominations to Item of the Agenda the World Heritage List Amended Draft Decision 44 COM 8B.44 Amendment submitted Saudi Arabia by the Delegation of…. Date of submission 15/07/2021 TEXT Draft Decision: 44 COM 8B.44 The World Heritage Committee, 1. Having examined Documents WHC/21/44.COM/8B and WHC/21/44.COM/INF.8B1, 2. Inscribes the Petroglyphs of Lake Onega and the White Sea, Russian Federation, on the World Heritage List on the basis of criterion (iii), 3. Adopts the following Statement of Outstanding Universal Value: Brief synthesis The Petroglyphs of Lake Onega and the White Sea are located in the north-west of Russia in the Republic of Karelia and include two component parts located 300 km from each other: the petroglyphs of Lake Onega in the south-east part of the Republic of Karelia and those of the White Sea in the north-east part. The petroglyphs of Lake Onega and the White Sea represent one of the largest independent centres of Neolithic rock art in Europe, dating to between circa 4,500 BC to 3,500 BC. The property comprises a total of over 4,500 petroglyphs concentrated in 33 sites within the two component parts, including a total of 22 sites at Lake Onega and 11 located at the White Sea. The petroglyphs are also associated with more than 100 archeological sites including settlements, camp sites and one burial ground dated as contemporary with the rock art. The rock art at Lake Onega mostly represents birds, symbols, half human and half animal figures, as well as figures interpreted as demon, burbot and otter, while the petroglyphs of the White Sea are mostly composed of carvings depicting boats, sea and forest hunting, scenes including their related equipment as well as animal and human footprints.