Mammalia, Chiroptera, Vespertilionidae), in Siberia and the Urals
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Living Lakes Goals 2019 - 2024 Achievements 2012 - 2018
Living Lakes Goals 2019 - 2024 Achievements 2012 - 2018 We save the lakes of the world! 1 Living Lakes Goals 2019-2024 | Achievements 2012-2018 Global Nature Fund (GNF) International Foundation for Environment and Nature Fritz-Reichle-Ring 4 78315 Radolfzell, Germany Phone : +49 (0)7732 99 95-0 Editor in charge : Udo Gattenlöhner Fax : +49 (0)7732 99 95-88 Coordination : David Marchetti, Daniel Natzschka, Bettina Schmidt E-Mail : [email protected] Text : Living Lakes members, Thomas Schaefer Visit us : www.globalnature.org Graphic Design : Didem Senturk Photographs : GNF-Archive, Living Lakes members; Jose Carlo Quintos, SCPW (Page 56) Cover photo : Udo Gattenlöhner, Lake Tota-Colombia 2 Living Lakes Goals 2019-2024 | Achievements 2012-2018 AMERICAS AFRICA Living Lakes Canada; Canada ........................................12 Lake Nokoué, Benin .................................................... 38 Columbia River Wetlands; Canada .................................13 Lake Ossa, Cameroon ..................................................39 Lake Chapala; Mexico ..................................................14 Lake Victoria; Kenya, Tanzania, Uganda ........................40 Ignacio Allende Reservoir, Mexico ................................15 Bujagali Falls; Uganda .................................................41 Lake Zapotlán, Mexico .................................................16 I. Lake Kivu; Democratic Republic of the Congo, Rwanda 42 Laguna de Fúquene; Colombia .....................................17 II. Lake Kivu; Democratic -
Timing and Dynamics of Glaciation in the Ikh Turgen Mountains, Altai T Region, High Asia
Quaternary Geochronology 47 (2018) 54–71 Contents lists available at ScienceDirect Quaternary Geochronology journal homepage: www.elsevier.com/locate/quageo Timing and dynamics of glaciation in the Ikh Turgen Mountains, Altai T region, High Asia ∗ Robin Blomdina,b, , Arjen P. Stroevena,b, Jonathan M. Harbora,b,c, Natacha Gribenskia,b,d, Marc W. Caffeec,e, Jakob Heymanf, Irina Rogozhinag, Mikhail N. Ivanovh, Dmitry A. Petrakovh, Michael Waltheri, Alexei N. Rudoyj, Wei Zhangk, Alexander Orkhonselengel, Clas Hättestranda,b, Nathaniel A. Liftonc,e, Krister N. Janssona,b a Geomorphology and Glaciology, Department of Physical Geography, Stockholm University, Stockholm, Sweden b Bolin Centre for Climate Research, Stockholm University, Stockholm, Sweden c Department of Earth, Atmospheric, and Planetary Sciences, Purdue University, West Lafayette, USA d Institute of Geological Sciences, University of Bern, Bern, Switzerland e Department of Physics and Astronomy, Purdue University, West Lafayette, USA f Department of Earth Sciences, University of Gothenburg, Gothenburg, Sweden g MARUM, University of Bremen, Bremen, Germany h Faculty of Geography, Lomonosov Moscow State University, Moscow, Russia i Institute of Geography and Geoecology, Mongolian Academy of Sciences, Ulaanbaatar, Mongolia j Center of Excellence for Biota, Climate and Research, Tomsk State University, Tomsk, Russia k College of Urban and Environmental Science, Liaoning Normal University, Dalian, China l Laboratory of Geochemistry and Geomorphology, School of Arts and Sciences, National -
NATIONAL PROTECTED AREAS of the RUSSIAN FEDERATION: of the RUSSIAN FEDERATION: AREAS PROTECTED NATIONAL Vladimir Krever, Mikhail Stishov, Irina Onufrenya
WWF WWF is one of the world’s largest and most experienced independent conservation WWF-Russia organizations, with almost 5 million supporters and a global network active in more than 19, bld.3 Nikoloyamskaya St., 100 countries. 109240 Moscow WWF’s mission is to stop the degradation of the planet’s natural environment and to build a Russia future in which humans live in harmony with nature, by: Tel.: +7 495 727 09 39 • conserving the world’s biological diversity Fax: +7 495 727 09 38 • ensuring that the use of renewable natural resources is sustainable [email protected] • promoting the reduction of pollution and wasteful consumption. http://www.wwf.ru The Nature Conservancy The Nature Conservancy - the leading conservation organization working around the world to The Nature Conservancy protect ecologically important lands and waters for nature and people. Worldwide Office The mission of The Nature Conservancy is to preserve the plants, animals and natural 4245 North Fairfax Drive, Suite 100 NNATIONALATIONAL PPROTECTEDROTECTED AAREASREAS communities that represent the diversity of life on Earth by protecting the lands and waters Arlington, VA 22203-1606 they need to survive. Tel: +1 (703) 841-5300 http://www.nature.org OOFF TTHEHE RRUSSIANUSSIAN FFEDERATION:EDERATION: MAVA The mission of the Foundation is to contribute to maintaining terrestrial and aquatic Fondation pour la ecosystems, both qualitatively and quantitatively, with a view to preserving their biodiversity. Protection de la Nature GGAPAP AANALYSISNALYSIS To this end, it promotes scientific research, training and integrated management practices Le Petit Essert whose effectiveness has been proved, while securing a future for local populations in cultural, 1147 Montricher, Suisse economic and ecological terms. -
438962 1 En Bookbackmatter 213..218
Index A Average temperature, 4, 53, 55, 57, 87, 111, 162, 185 Accumulation, 12, 26, 27, 33, 44, 66, 109, 113, 140, 141, Average wind speed, 64 144–146, 152, 155, 162 Achit lake, 37, 116, 165, 208 Active layer, 122, 124–126, 130 B Active layer thickness, 124–126 Baatarkhaihan, 35 Adaatsag, 46 Baga Bogd, 3, 38, 43, 188 Agricultural land, 136, 195–199 Baga Buural, 47 Airag lake, 91, 208 Baga Gazriin Chuluu, 46, 47 Air temperature variation, 111 Baga Khavtag, 45 Aj Bogd, 35, 190 Baga Khentii, 39, 80, 110 Alag khairhan, 35 Baga Uul, 47 Alasha Gobi, 163, 165 Baishin Tsav, 46 Algae, 161, 166 Baitag Bogd, 45 Alluvial fans and sediments, 45, 46 Baruun Khuurai depression, 28, 158, 181 Alluvial-proluvial plains, 27, 29 Baruun Saikhan, 33, 43 Alluvial soils, 145, 157 Baruunturuun, 68, 136 Alpine belts, 66, 171, 185 Bayan, 3, 7, 34–36, 40, 69, 79, 88, 89, 91, 106, 109, 113 Alpine-type high mountains, 32 Bayanbor, 43 Alpine type relief, 44 Bayan Bumbun Ranges, 35 Altai region, 5, 28, 35, 42, 65, 144 Bayankhairhan, 39 Altai-Sayan ecoregion, 210 Bayantsagaan, 42, 43, 47, 49 Altai Tavan Bogd, 24, 35 Bayan-Ulgii, 7, 69, 113 Altankhukhii, 35 Biological diversity, 182 Altan Ulgii, 39 Birds, 161, 162, 169–175, 207, 208 Altitudinal belts, 6, 163, 177, 182–185, 187, 190, 192 Bogd, 3, 11, 34, 36, 38, 40, 42, 49, 101–103, 106, 181, Angarkhai, 38 188, 204, 208 Animal, 4, 6, 7, 11, 12, 16, 33, 72, 145, 169, 171, 172, Bogd Ulaan, 49 197, 205 Boreal, 6, 163, 164, 187, 210 Annual precipitation, 53, 60, 61, 71, 86, 92, 121, 186, Bor Khairhan, 39 188, 189, 192 Borzon -
Late Glacial-Holocene Environmental History of the East Sayan Mountains (Southern Siberia, Russia): a Paleolimnological Study of Mountain Lakes
SI: “The 4th International Conference Limnology and Freshwater Biology 2020 (4): 566-567 DOI:10.31951/2658-3518-2020-A-4-566 Palaeolimnology of Northern Eurasia” Short communication Late Glacial-Holocene environmental history of the East Sayan Mountains (Southern Siberia, Russia): a paleolimnological study of mountain lakes Bezrukova E.V.1*, Kulagina N.V.2, Amosova A.A.1, Volchatova E.V.1, Levina O.V.1, Tkachenko L.L.1, Shchetnikov A.A.2, Kerber E.V.1, Filinov I.A.2 1 Vinogradov Institute of Geochemistry, Siberian Branch of the Russian Academy of Sciences, Favorsky Str., 1A, Irkutsk, 664033, Russia 2 Institute of the Earth’s Crust, Siberian Branch of the Russian Academy of Sciences, Lermontov Str., 128, Irkutsk, 664033, Russia ABSTRACT. Palaeoenvironmental changes including vegetation, chemical weathering intensity, lake’s water level fluctuations, and climate dynamics, from the East Sayan Mountains were investigated using multiple proxies such as pollen, mineralogical, petromagnetic, X-ray fluorescence analyses and radio- carbon dating. Keywords: vegetation and chemical weathering history, climate, Late Glacial-Holocene, Oka Plateau, southern Siberia 1. Introduction 3. Results and discussion Climate is the major environmental factor that Multiproxy records from lakes Kaskadnoe (Ksk) influences lake geosystems, directly and indirectly and Khikushka (Khk) demonstrate distinct changes in (O’Sullivan, Reynolds, 2005). At the end of the last gla- regional vegetation, environment and climate since 14.6 ciation, there was a general climate warming although ka BP (calibrated thousands years before present). The it included fluctuations such as warmer Allerød or pollen record indicates a considerable development of cooler Younger Dryas (Rasmussen et al., 2014). -
Defining Territories and Empires: from Mongol Ulus to Russian Siberia1200-1800 Stephen Kotkin
Defining Territories and Empires: from Mongol Ulus to Russian Siberia1200-1800 Stephen Kotkin (Princeton University) Copyright (c) 1996 by the Slavic Research Center All rights reserved. The Russian empire's eventual displacement of the thirteenth-century Mongol ulus in Eurasia seems self-evident. The overthrow of the foreign yoke, defeat of various khanates, and conquest of Siberia constitute core aspects of the narratives on the formation of Russia's identity and political institutions. To those who disavow the Mongol influence, the Byzantine tradition serves as a counterweight. But the geopolitical turnabout is not a matter of dispute. Where Chingis Khan and his many descendants once held sway, the Riurikids (succeeded by the Romanovs) moved in. *1 Rather than the shortlived but ramified Mongol hegemony, which was mostly limited to the middle and southern parts of Eurasia, longterm overviews of the lands that became known as Siberia, or of its various subregions, typically begin with a chapter on "pre-history," which extends from the paleolithic to the moment of Russian arrival in the late sixteenth, early seventeenth centuries. *2 The goal is usually to enable the reader to understand what "human material" the Russians found and what "progress" was then achieved. Inherent in the narratives -- however sympathetic they may or may not be to the native peoples -- are assumptions about the historical advance deriving from the Russian arrival and socio-economic transformation. In short, the narratives are involved in legitimating Russia's conquest without any notion of alternatives. Of course, history can also be used to show that what seems natural did not exist forever but came into being; to reveal that there were other modes of existence, which were either pushed aside or folded into what then came to seem irreversible. -
Naming Practices and Ethnic Identity in Tuva K
Naming Practices and Ethnic Identity in Tuva K. David Harrison 1 Yale University 1 Introduction Indigenous peoples of Siberia maintain a tenuous identity pummeled by forces of linguistic and cultural assimilation on the one hand, and empowered by a discourse of self-determination on the other. Language, even at the level of individual words, may serve as an arena where such opposing ideologies of identity and exclusion play themselves out (Bakhtin 1981). This paper is based on recent fieldwork by the author among the Tuvans (also Tyvans), an indigenous Turkic people of south central Siberia. We investigate two recent trends in Tuvan anthroponymic praxis (i.e. choice and use of given names, nicknames and kinship terms). First, we look at the rise and decline in the use of Russian (and other non- Tuvan) given names for Tuvan children after 1944. This trend reveals perceived values of native vs. non-native names in a community where two languages of unequal social value are spoken. Secondly, we explore how the Russian naming system imposed on Tuvans after 1944 fused with the existing Tuvan system, giving rise to a new symbiosis. The new system adds Russian elements, preserves key elements of Tuvan naming, and also introduces some innovations not found in either system. For comparative purposes, we cite recent studies of Xakas names (Butanayev, n.d.) and Lithuanian naming practices (Lawson and Butkus 1999). We situate naming trends within a historical and sociolinguistic context of Tuvan as the majority language of a minority people of Russia. We also offer an interpretation of these two trends that addresses larger questions of the relation between naming and name use on the one hand and construction of ethno-linguistic identity on the other. -
Article (SCP) Deposition Rates, Based on Snowpack Analyses of a Formerly Unexplored Siberian Mountain Region
Biogeosciences, 18, 1601–1618, 2021 https://doi.org/10.5194/bg-18-1601-2021 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Winter atmospheric nutrient and pollutant deposition on Western Sayan Mountain lakes (Siberia) Daniel Diaz-de-Quijano1, Aleksander Vladimirovich Ageev1, Elena Anatolevna Ivanova1, and Olesia Valerevna Anishchenko1,2 1Siberian Federal University, 79, Svobondyi prospekt, Krasnoyarsk, 660041, Krasnoyarsk Krai, Russian Federation 2Institute of Biophysics, Siberian Branch, Russian Academy of Sciences, 50/50, Akademgorodok, Krasnoyarsk, 660036, Krasnoyarsk Krai, Russian Federation Correspondence: Daniel Diaz-de-Quijano ([email protected], [email protected]) Received: 6 April 2020 – Discussion started: 21 September 2020 Revised: 30 December 2020 – Accepted: 12 January 2021 – Published: 5 March 2021 Abstract. The world map of anthropogenic atmospheric ni- temperature-inhibited responses of phytoplankton to nutrient trogen deposition and its effects on natural ecosystems is not shifts. described with equal precision everywhere. In this paper, we report atmospheric nutrient, sulfate and spheroidal carbona- ceous particle (SCP) deposition rates, based on snowpack analyses of a formerly unexplored Siberian mountain region. 1 Introduction Then, we discuss their potential effects on lake phytoplank- ton biomass limitation. Worldwide nitrogen cycle perturbation is the second most We estimate that the nutrient depositions observed important global environmental concern, just after mas- −2 in the late-season snowpack (40 ± 16 mg NO3-N m sive extinction of species and even more important than and 0.58 ± 0.13 mg TP-P m−2; TP for total phospho- global warming (Rockström et al., 2009; Steffen et al., rous) would correspond to yearly depositions lower 2015). -
Mongolia the Private Collection
Big Five Presents Mongolia The Private Collection Ancient monasteries, the haunting natural beauty of the Gobi Desert, wild horses and intriguing cultures - Mongolia offers extraordinary opportunities to see and experience the living history that is Mongolia. In our own rapid-fire, always changing world, Mongolia is one of those increasingly rare places that seems to belong to another time; somewhere far off on the edges of what we know. It calls up images of nomadic tribesmen on the wind-swept Mongolian steppes, the Silk Road stations in the Gobi Desert and herds of rugged wild horses. Beneath such simplistic images, however, are a legendary past and people that once dominated the world stage in the 13th and 14th centuries. At its peak, the Mongol Empire was the largest contiguous land empire in human history! It reached across central Asia to encompass lands from Eastern Europe to the Sea of Japan and south into India. By the 17th century, Tibetan Buddhism became the dominant religion in Mongolia, replacing, for the most part, indigenous shaman practices. In the Mongolia of today, modernity is beginning to remodel the country as high-rise buildings crop up next to 18th-century monasteries. By the same token, Mongolians respect their history, traditions and the deep roots put down by their ancestors. Around the country, reconstruction and preservation projects are underway to preserve that history. Priceless artifacts that were so long hidden away for safekeeping are now being returned to monasteries. And it is still possible to set out on a journey that encounters nomadic clans, exquisite landscapes and unique wildlife. -
The Complex Admixture History and Recent Southern Origins of Siberian Populations
bioRxiv preprint doi: https://doi.org/10.1101/018770; this version posted April 30, 2015. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC-ND 4.0 International license. The complex admixture history and recent southern origins of Siberian populations Short title: The complex admixture history of Siberians Irina Pugach1*, Rostislav Matveev2, Viktor Spitsyn3, Sergey Makarov3, Innokentiy Novgorodov4, Vladimir Osakovsky5, Mark Stoneking1, Brigitte Pakendorf6* 1 Department of Evolutionary Genetics, Max Planck Institute for Evolutionary Anthropology, Leipzig, Germany 2 Max Planck Institute for Mathematics in the Sciences, Leipzig, Germany 3 Research Centre for Medical Genetics, Federal State Budgetary Institution, Moscow, Russian Federation 4 Institute of Foreign Philology and Regional Studies, North-Eastern Federal University, Yakutsk, Russian Federation 5 Institute of Health, North-Eastern Federal University, Yakutsk, Russian Federation 6 Laboratoire Dynamique du Langage, UMR5596, CNRS and Université Lyon Lumière 2, Lyon, France. *Corresponding authors: [email protected] (IP), [email protected] (BP) 1 bioRxiv preprint doi: https://doi.org/10.1101/018770; this version posted April 30, 2015. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC-ND 4.0 International license. Abstract Although Siberia was inhabited by modern humans at an early stage, there is still debate over whether this area remained habitable during the extremely cold period of the Last Glacial Maximum or whether it was subsequently repopulated by peoples with a recent shared ancestry. -
Gap Eng 1.Pdf
PARTICIPATION IN MINING RELATED DECISION MAKING REPORT Project: Give people a voice! Strengthen public participation in mining Investment planning to ensure the health of people, livestock and the environment of Mongolia. Client: WWF (Mongolia) Contractor: Green Focus Contract No. EIDH/2015-369-258 funded under European Instrument for Democracy and Human Rights (EIDHR) - Country-Based Support Schemes (CBSS), Mongolia Disclaimer This document is issued for the party which commissioned it and for the specific purposes connected with the above-captioned project only. It should not be relied upon by any other party or used for any other purpose. Neither the authors nor the client accept responsibility for the consequences of this document being relied upon by any other party, or being used for any other purpose, or containing any error or omission which is due to an error or omission in data supplied to us by other parties This document contains confidential information and proprietary intellectual property. It should not be shown to other parties without consent from the authors and from the party which commissioned it. PARTICIPATION IN MINING RELATED DECISION MAKING TABLE OF CONTENTS Executive Summary 4 Abbreviations 6 Mongolian Terminology 8 Definitions 8 Acknowlegements 11 Project Team 11 Goals and Objectives 12 Methodology 13 1. Introduction 15 2. The Development of Mongolia’s Mining Sector 16 3. International Initiatives and Benchmarks 19 4. Implementing International Standards in Mongolia 21 5. The Challenges of Public Participation in EIA Processes. 23 a. Persistent Poor Practices in Community Engagement in Mining Projects. 24 b. Emerging Good Practice for Community Engagement in Mining Projects. -
WWF-Mongolia: WWF-Mongolia: the Way Forward • 1 WWF-Mongolia Achievement Summary and Landmark Dates
WWF-Mongolia: WWF-MONGOLIA: THE WAY FORWARD • 1 WWF-Mongolia achieveMent suMMary and landMark dates • WWF starts its first project towards designing • As part of the WWF initiative, entitled “Gift to and expanding PA networks with WWF-Germany’s the Earth”, the Mongolian President pledges support and opened a project office with three to put 30% of the nation under protected staff members. Prior to WWF’s arrival, Mon- status, which is formalized by parliamentary golia had established only 13 protected areas, approval of the National Programme on Pro- encompassing the area of around 5 Million tected Areas in 1998. With this approval, the hectares that accounted for 5.3% of the coun- goals are established to develop a protected try’s territory. With WWF’s direct involve- area network to secure ecological balance and ment, the size of PAs enlarges with establish- ensure effective management to an international ment of Gobi Gurvan Saikhan, Gorkhi-Terelj, level. The National Programme is one of the Khangai Mountain Range and Khar-Us Lake few national programmes adopted by the Par- National parks. liament. The total size of the PA network for the entire • Due to WWF’s assistance to the Government country is doubled in less than 6 years. for raising the funds to support PA network, • With direct involvement of WWF, the draft the German Government ensures long-term Law on Protected Areas and Law on Buffer financial commitment for nature conservation zone of Protected Area are developed and within bilateral agreement. adopted, through an internal zoning system • In 1997, the WWF Mongolia Project Office is which is adopted as a basis for sound PA upgraded to a Country Office and officially networks and its functionality.