2020 Conservation Outlook Assessment
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Details of multiple regression models results for the relationships between NRE, PRE, NRE:PRE and environmental factors (Latitude (LAT, o), mean annual precipitation (MAT, oC) and mean annual precipitation (MAP, mm)), respectively. Equations and R2 and P values describe the explanatory power of each model. Group Equation R2 P NRE All data y=1.56091+0.0036Lat 0.063 <0.0001 y=1.741650.0047MAT 0.039 <0.0001 y=1.747110.0000609MAP 0.054 <0.0001 y=1.7205+0.283461Lat0.038019MAT0.002754MAP 0.106 <0.0001 Graminoids y=1.63377+0.00225Lat 0.052 0.037 y=1.777880.00776MAT 0.073 <0.0001 y=1.776790.0000865MAP 0.038 0.002 y=1.525405+0.025707Lat0.569069MAT0.00372MAP 0.059 0.004 Forbs y=1.53428+0.00401Lat 0.088 <0.0001 y=1.714940.00297MAT 0.017 0.014 y=1.728780.0000519MAP 0.055 <0.0001 y=1.881503+0.547313Lat+0.455467MAT0.00249MAP 0.145 <0.0001 Monocots y=1.52058+0.00431Lat 0.069 <0.0001 y=1.708340.0015MAT 0.002 0.337 y=1.735440.0000621MAP 0.048 <0.0001 y=1.923174+0.090165Lat0.612721MAT0.000192MAP 0.102 <0.0001 Eudicots y=1.58939+0.00319Lat 0.058 <0.0001 y=1.772760.0071MAT 0.105 <0.0001 y=1.761330.0000623MAP 0.060 <0.0001 y=1.039314+0.514526Lat+0.47502MAT0.00428MAP 0.133 <0.0001 PRE All data y=1.67742+0.00278Lat 0.076 <0.0001 y=1.82743-0.00434MAT 0.059 <0.0001 y=1.82165-0.0000405MAP 0.055 <0.0001 y=1.463987+0.256038Lat0.152148MAT0.000796MAP 0.189 <0.0001 Graminoids y=1.71335+0.00248Lat 0.062 0.001 y=1.86398-0.00611MAT 0.119 <0.0001 y=1.85218-0.0000485MAP 0.041 0.007 y=1.716721+0.150796Lat0.743164MAT+0.001219MAP 0.134 <0.0001 Forbs y=1.67729+0.00234Lat 0.049 -
Confirmed Soc Reports List 2015-2016
Confirmed State of Conservation Reports for natural and mixed World Heritage sites 2015 - 2016 Nr Region Country Site Natural or Additional information mixed site 1 LAC Argentina Iguazu National Park Natural 2 APA Australia Tasmanian Wilderness Mixed 3 EURNA Belarus / Poland Bialowieza Forest Natural 4 LAC Belize Belize Barrier Reef Reserve System Natural World Heritage in Danger 5 AFR Botswana Okavango Delta Natural 6 LAC Brazil Iguaçu National Park Natural 7 LAC Brazil Cerrado Protected Areas: Chapada dos Veadeiros and Natural Emas National Parks 8 EURNA Bulgaria Pirin National Park Natural 9 AFR Cameroon Dja Faunal Reserve Natural 10 EURNA Canada Gros Morne National Park Natural 11 AFR Central African Republic Manovo-Gounda St Floris National Park Natural World Heritage in Danger 12 LAC Costa Rica / Panama Talamanca Range-La Amistad Reserves / La Amistad Natural National Park 13 AFR Côte d'Ivoire Comoé National Park Natural World Heritage in Danger 14 AFR Côte d'Ivoire / Guinea Mount Nimba Strict Nature Reserve Natural World Heritage in Danger 15 AFR Democratic Republic of the Congo Garamba National Park Natural World Heritage in Danger 16 AFR Democratic Republic of the Congo Kahuzi-Biega National Park Natural World Heritage in Danger 17 AFR Democratic Republic of the Congo Okapi Wildlife Reserve Natural World Heritage in Danger 18 AFR Democratic Republic of the Congo Salonga National Park Natural World Heritage in Danger 19 AFR Democratic Republic of the Congo Virunga National Park Natural World Heritage in Danger 20 AFR Democratic -
View Map of the Entire Serial Property
IUCN World Heritage Outlook: https://worldheritageoutlook.iucn.org/ Volcanoes of Kamchatka - 2017 Conservation Outlook Assessment (archived) IUCN Conservation Outlook Assessment 2017 (archived) Finalised on 09 November 2017 Please note: this is an archived Conservation Outlook Assessment for Volcanoes of Kamchatka. To access the most up-to-date Conservation Outlook Assessment for this site, please visit https://www.worldheritageoutlook.iucn.org. Volcanoes of Kamchatka عقوملا تامولعم Country: Russian Federation Inscribed in: 1996 Criteria: (vii) (viii) (ix) (x) This is one of the most outstanding volcanic regions in the world, with a high density of active volcanoes, a variety of types, and a wide range of related features. The six sites included in the serial designation group together the majority of volcanic features of the Kamchatka peninsula. The interplay of active volcanoes and glaciers forms a dynamic landscape of great beauty. The sites contain great species diversity, including the world's largest known variety of salmonoid fish and exceptional concentrations of sea otter, brown bear and Stellar's sea eagle. © UNESCO صخلملا 2017 Conservation Outlook Significant concern Conservation outlook for the geological values and also for the scenic values of the site is good as these are very robust against human activities, and because such activities are still relatively localized within the property. Conservation outlook is worse for the rich biodiversity values, which are protected by the size, remoteness, relative inaccessibility and pristine state of the site. Unsustainable use of natural resources (legal and illegal hunting and fishing) have started to erode these values along the additional threats posed by existing roads and the trend towards infrastructure development and associated with it increasing accessibility which will further increase the threats for biodiversity values. -
Central Sikhote-Alin
WHC Nomination Documentation File Name: 766rev.pdf UNESCO Region: EUROPE AND THE NORTH AMERICA __________________________________________________________________________________________________ SITE NAME: Central Sikhote-Alin DATE OF INSCRIPTION: 16th December 2001 STATE PARTY: RUSSIAN FEDERATION CRITERIA: N (iv) DECISION OF THE WORLD HERITAGE COMMITTEE: Excerpt from the Report of the 25th Session of the World Heritage Committee The Committee inscribed Central Sikhote-Alin on the World Heritage List under criterion (iv): Criterion (iv): The nominated area is representative of one of the world's most distinctive natural regions. The combination of glacial history, climate and relief has allowed the development of the richest and most unusual temperate forests in the world. Compared to other temperate ecosystems, the level of endemic plants and invertebrates present in the region is extraordinarily high which has resulted in unusual assemblages of plants and animals. For example, subtropical species such as tiger and Himalayan bear share the same habitat with species typical of northern taiga such as brown bear and reindeer. The site is also important for the survival of endangered species such as the scaly-sided (Chinese) merganser, Blakiston's fish-owl and the Amur tiger. This serial nomination consists of two protected areas in the Sikhote- Alin mountain range in the extreme southeast of the Russian Federation: NAME LOCATION AREA Sikhote-Alin Nature Preserve Terney District 401,428 ha Goralij Zoological Preserve Coastal zone on the Sea of Japan, N of Terney 4,749 ha The Committee encouraged the State Party to improve management of the Bikin River protected areas (Bikin Territory of Traditional Nature Use and Verkhnebikinski zakaznik) before nominating it as an extension. -
RCN #33 21/8/03 13:57 Page 1
RCN #33 21/8/03 13:57 Page 1 No. 33 Summer 2003 Special issue: The Transformation of Protected Areas in Russia A Ten-Year Review PROMOTING BIODIVERSITY CONSERVATION IN RUSSIA AND THROUGHOUT NORTHERN EURASIA RCN #33 21/8/03 13:57 Page 2 CONTENTS CONTENTS Voice from the Wild (Letter from the Editors)......................................1 Ten Years of Teaching and Learning in Bolshaya Kokshaga Zapovednik ...............................................................24 BY WAY OF AN INTRODUCTION The Formation of Regional Associations A Brief History of Modern Russian Nature Reserves..........................2 of Protected Areas........................................................................................................27 A Glossary of Russian Protected Areas...........................................................3 The Growth of Regional Nature Protection: A Case Study from the Orlovskaya Oblast ..............................................29 THE PAST TEN YEARS: Making Friends beyond Boundaries.............................................................30 TRENDS AND CASE STUDIES A Spotlight on Kerzhensky Zapovednik...................................................32 Geographic Development ........................................................................................5 Ecotourism in Protected Areas: Problems and Possibilities......34 Legal Developments in Nature Protection.................................................7 A LOOK TO THE FUTURE Financing Zapovedniks ...........................................................................................10 -
Helicopter Tour to Kuril Lake-Caldera of Volcano Ksudach-Khodutkinskye Hot Springs (Tour 2)
HELICOPTER TOUR TO VALLEY OF GEYSERS-CALDERA OF VOLCANO UZON-NALYCHEVO VALLEY (TOUR 1) Period – all the year Transportation – helicopter Tour time – 6 hours Flight time – approximately 2 hours 15 minutes The famous Valley of Geysers is a canyon which has one of the biggest geyser area in the world. It is hidden in a hard access gorge of the Kronotsky Nature Reserve. It is unrivalled in beauty, landscape grandeur and number of springs throwing out fountains of hot water and steam. Gushing geysers, raging mud cauldrons, a turquoise lake, hot water and steam jets flowing down the slopes together with the lush greenery of grass and trees create a really fantastic sight. Not far from the Valley of Geysers there is one more unique and impressive place - Uzon caldera. It is a giant cavity with the dimensions 9×12 km, resulting from destruction of the ancient volcano, having an intensive hydrothermal activity on the bottom. There are a lot of boiling and raging craters, numerous mud cauldrons and small volcanoes, yellow fumaroles areas, steamy grounds where the steam and hot water come out from the earth. The peculiarity of this place is the crater-like holes 25-40 m deep and in diameter 25-150 m, in which hot lakes of odd colours are situated. ROUTE 11.00-12.00 - Flight from heliport of Yelizovo city to the Valley of Geysers. Flying around Karymskiy and Malyi Semyachik active volcanoes. 12.00-13.30 - Excursion to the Valley of Geysers. 13.30-13.40 - Flying to the Uzon caldera. 13.40-14.30 - Excursion in the caldera of Uzon volcano. -
Pskov from Wikipedia, the Free Encyclopedia Coordinates: 57°49′N 28°20′E
Create account Log in Article Talk Read Edit View history Pskov From Wikipedia, the free encyclopedia Coordinates: 57°49′N 28°20′E Pskov (Russian: Псков; IPA: [pskof] ( listen), ancient Russian spelling "Плѣсковъ", Pleskov) is Navigation Pskov (English) a city and the administrative center of Pskov Oblast, Russia, located about 20 kilometers Псков (Russian) Main page (12 mi) east from the Estonian border, on the Velikaya River. Population: 203,279 (2010 [1] Contents Census);[3] 202,780 (2002 Census);[5] 203,789 (1989 Census).[6] - City - Featured content Current events Contents Random article 1 History Donate to Wikipedia 1.1 Early history 1.2 Pskov Republic 1.3 Modern history Interaction 2 Administrative and municipal status Help 3 Landmarks and sights About Wikipedia 4 Climate Community portal 5 Economy Recent changes 6 Notable people Krom (or Kremlin) in Pskov Contact Wikipedia 7 International relations 7.1 Twin towns and sister cities Toolbox 8 References 8.1 Notes What links here 8.2 Sources Related changes 9 External links Upload file Special pages History [edit] Location of Pskov Oblast in Russia Permanent link Page information Data item Early history [edit] Cite this page The name of the city, originally spelled "Pleskov", may be loosely translated as "[the town] of purling waters". Its earliest mention comes in 903, which records that Igor of Kiev married a [citation needed] Print/export local lady, St. Olga. Pskovians sometimes take this year as the city's foundation date, and in 2003 a great jubilee took place to celebrate Pskov's 1,100th anniversary. Create a book Pskov The first prince of Pskov was Vladimir the Great's younger son Sudislav. -
Global Survey of Ex Situ Betulaceae Collections Global Survey of Ex Situ Betulaceae Collections
Global Survey of Ex situ Betulaceae Collections Global Survey of Ex situ Betulaceae Collections By Emily Beech, Kirsty Shaw and Meirion Jones June 2015 Recommended citation: Beech, E., Shaw, K., & Jones, M. 2015. Global Survey of Ex situ Betulaceae Collections. BGCI. Acknowledgements BGCI gratefully acknowledges the many botanic gardens around the world that have contributed data to this survey (a full list of contributing gardens is provided in Annex 2). BGCI would also like to acknowledge the assistance of the following organisations in the promotion of the survey and the collection of data, including the Royal Botanic Gardens Edinburgh, Yorkshire Arboretum, University of Liverpool Ness Botanic Gardens, and Stone Lane Gardens & Arboretum (U.K.), and the Morton Arboretum (U.S.A). We would also like to thank contributors to The Red List of Betulaceae, which was a precursor to this ex situ survey. BOTANIC GARDENS CONSERVATION INTERNATIONAL (BGCI) BGCI is a membership organization linking botanic gardens is over 100 countries in a shared commitment to biodiversity conservation, sustainable use and environmental education. BGCI aims to mobilize botanic gardens and work with partners to secure plant diversity for the well-being of people and the planet. BGCI provides the Secretariat for the IUCN/SSC Global Tree Specialist Group. www.bgci.org FAUNA & FLORA INTERNATIONAL (FFI) FFI, founded in 1903 and the world’s oldest international conservation organization, acts to conserve threatened species and ecosystems worldwide, choosing solutions that are sustainable, based on sound science and take account of human needs. www.fauna-flora.org GLOBAL TREES CAMPAIGN (GTC) GTC is undertaken through a partnership between BGCI and FFI, working with a wide range of other organisations around the world, to save the world’s most threated trees and the habitats which they grow through the provision of information, delivery of conservation action and support for sustainable use. -
Volcanic Arc of Kamchatka: a Province with High-␦18O Magma Sources and Large-Scale 18O/16O Depletion of the Upper Crust
Geochimica et Cosmochimica Acta, Vol. 68, No. 4, pp. 841–865, 2004 Copyright © 2004 Elsevier Ltd Pergamon Printed in the USA. All rights reserved 0016-7037/04 $30.00 ϩ .00 doi:10.1016/j.gca.2003.07.009 Volcanic arc of Kamchatka: a province with high-␦18O magma sources and large-scale 18O/16O depletion of the upper crust 1, 2 3 1 ILYA N. BINDEMAN, *VERA V. PONOMAREVA, JOHN C. BAILEY, and JOHN W. VALLEY 1Department of Geology and Geophysics, University of Wisconsin, Madison, WI, USA 2Institute of Volcanic Geology and Geochemistry, Petropavlovsk-Kamchatsky, Russia 3Geologisk Institut, University of Copenhagen, Copenhagen, Denmark (Received March 20, 2003; accepted in revised form July 16, 2003) Abstract—We present the results of a regional study of oxygen and Sr-Nd-Pb isotopes of Pleistocene to Recent arc volcanism in the Kamchatka Peninsula and the Kuriles, with emphasis on the largest caldera- forming centers. The ␦18O values of phenocrysts, in combination with numerical crystallization modeling (MELTS) and experimental fractionation factors, are used to derive best estimates of primary values for ␦18O(magma). Magmatic ␦18O values span 3.5‰ and are correlated with whole-rock Sr-Nd-Pb isotopes and major elements. Our data show that Kamchatka is a region of isotopic diversity with high-␦18O basaltic magmas (sampling mantle to lower crustal high-␦18O sources), and low-␦18O silicic volcanism (sampling low-␦18O upper crust). Among one hundred Holocene and Late Pleistocene eruptive units from 23 volcanic centers, one half represents low-␦18O magmas (ϩ4 to 5‰). Most low-␦ 18O magmas are voluminous silicic ignimbrites related to large Ͼ10 km3 caldera-forming eruptions and subsequent intracaldera lavas and domes: Holocene multi-caldera Ksudach volcano, Karymsky and Kurile Lake-Iliinsky calderas, and Late Pleistocene Maly Semyachik, Akademy Nauk, and Uzon calderas. -
From Sacred Cow to Cash Cow Muller, Martin
From sacred cow to cash cow Muller, Martin License: Creative Commons: Attribution-NoDerivs (CC BY-ND) Document Version Publisher's PDF, also known as Version of record Citation for published version (Harvard): Müller, M 2014, 'From sacred cow to cash cow: the shifting political ecologies of protected areas in Russia', Zeitschrift für Wirtschaftsgeographie, vol. 58, no. 2-3, pp. 127-143. Link to publication on Research at Birmingham portal General rights Unless a licence is specified above, all rights (including copyright and moral rights) in this document are retained by the authors and/or the copyright holders. The express permission of the copyright holder must be obtained for any use of this material other than for purposes permitted by law. •Users may freely distribute the URL that is used to identify this publication. •Users may download and/or print one copy of the publication from the University of Birmingham research portal for the purpose of private study or non-commercial research. •User may use extracts from the document in line with the concept of ‘fair dealing’ under the Copyright, Designs and Patents Act 1988 (?) •Users may not further distribute the material nor use it for the purposes of commercial gain. Where a licence is displayed above, please note the terms and conditions of the licence govern your use of this document. When citing, please reference the published version. Take down policy While the University of Birmingham exercises care and attention in making items available there are rare occasions when an item has been uploaded in error or has been deemed to be commercially or otherwise sensitive. -
Dr. Duke's Phytochemical and Ethnobotanical Databases List of Plants for Lyme Disease (Chronic)
Dr. Duke's Phytochemical and Ethnobotanical Databases List of Plants for Lyme Disease (Chronic) Plant Chemical Count Activity Count Garcinia xanthochymus 1 1 Nicotiana rustica 1 1 Acacia modesta 1 1 Galanthus nivalis 1 1 Dryopteris marginalis 2 1 Premna integrifolia 1 1 Senecio alpinus 1 1 Cephalotaxus harringtonii 1 1 Comptonia peregrina 1 1 Diospyros rotundifolia 1 1 Alnus crispa 1 1 Haplophyton cimicidum 1 1 Diospyros undulata 1 1 Roylea elegans 1 1 Bruguiera gymnorrhiza 1 1 Gmelina arborea 1 1 Orthosphenia mexicana 1 1 Lumnitzera racemosa 1 1 Melilotus alba 2 1 Duboisia leichhardtii 1 1 Erythroxylum zambesiacum 1 1 Salvia beckeri 1 1 Cephalotaxus spp 1 1 Taxus cuspidata 3 1 Suaeda maritima 1 1 Rhizophora mucronata 1 1 Streblus asper 1 1 Plant Chemical Count Activity Count Dianthus sp. 1 1 Glechoma hirsuta 1 1 Phyllanthus flexuosus 1 1 Euphorbia broteri 1 1 Hyssopus ferganensis 1 1 Lemaireocereus thurberi 1 1 Holacantha emoryi 1 1 Casearia arborea 1 1 Fagonia cretica 1 1 Cephalotaxus wilsoniana 1 1 Hydnocarpus anthelminticus 2 1 Taxus sp 2 1 Zataria multiflora 1 1 Acinos thymoides 1 1 Ambrosia artemisiifolia 1 1 Rhododendron schotense 1 1 Sweetia panamensis 1 1 Thymelaea hirsuta 1 1 Argyreia nervosa 1 1 Carapa guianensis 1 1 Parthenium hysterophorus 1 1 Rhododendron anthopogon 1 1 Strobilanthes cusia 1 1 Dianthus superbus 1 1 Pyropolyporus fomentarius 1 1 Euphorbia hermentiana 1 1 Porteresia coarctata 1 1 2 Plant Chemical Count Activity Count Aerva lanata 1 1 Rivea corymbosa 1 1 Solanum mammosum 1 1 Juniperus horizontalis 1 1 Maytenus -
Weathering of Volcanic Ash in the Cryogenic Zone of Kamchatka, Eastern Russia
Clay Minerals, (2014) 49, 195–212 OPEN ACCESS Weathering of volcanic ash in the cryogenic zone of Kamchatka, eastern Russia 1, 2 E. KUZNETSOVA * AND R. MOTENKO 1 SINTEF Building and Infrastructure, Trondheim, NO-7465, Norway, and 2 Lomonosov Moscow State University, Moscow, 119991, Russia (Received 8 August 2012; revised 28 August 2013; Editor: Harry Shaw) ABSTRACT: The nature of the alteration of basaltic, andesitic and rhyolitic glass of Holocene and Pleistocene age and their physical and chemical environments have been investigated in the ash layers within the cryogenic soils associated with the volcanoes in the central depression of Kamchatka. One of the main factors controlling the alteration of the volcanic glass is their initial chemistry with those of andesitic (SiO2 =53À65 wt.%) and basaltic (SiO2 < 53 wt.%) compositions being characterized by the presence of allophane, whereas volcanic glass of rhyolitic composition (SiO2>65 wt.%) are characterized by opal. Variations in the age of eruption of individual ashes, the amount and nature of the soil water, the depth of the active annual freeze-thawing layer, the thermal conductivity of the weathering soils, do not play a controlling role in the type of weathering products of the ashes but may affect their rates of alteration. KEYWORDS: volcanic ash, allophane, opal, unfrozen water, thermal conductivity, permafrost, Kamchatka. The highly active volcanic area of Kamchatka in local and remote eruptions and from the secondary eastern Russia is part of the circum-Pacific belt of re-deposition of ash (Bazanova et al., 2005). andesitic volcanism. It is situated north of the 49th Considerable research has been carried out on the parallel of latitude and is characterized by a weathering of volcanic glass.