Siberian White Crane on Protected Territories of Yakutia (Russian Northeast)

Total Page:16

File Type:pdf, Size:1020Kb

Siberian White Crane on Protected Territories of Yakutia (Russian Northeast) Siberian White Crane on Protected Territories of Yakutia (Russian Northeast) N. I. Germogenov Abstract—The importance of existing protected territories of According to surveys of winter habitat in southeastern the Sakha Republic (Yakutia) to the conservation of the rare China, the current size of the white crane eastern popula- Siberian white crane is evaluated based on range structure and tion ranges from 2,610 to 3,000 individuals (Asia-Pacific new estimates of the white crane’s eastern population in northeast- Migratory Waterbird Conservation Strategy: 1996-2000; ern Russia. The protection of the Siberian crane’s population is Harris and others 1994). mostly carried out within 13 territories, occupying 8,934.5 km2 or 2.6 percent of the Sakha Republic’s area. Three of these territories are the Kytalyk Resource Reserve (16,080 km2), the Chaygurino Estimating Population Size in (23,756 km2), and the Khroma (1,130 km2). Reservations are the Northeast Yakutia _______________ sites of nesting and summering of more than 720 birds, or 37 to 43.7 percent of the eastern population. Various aspects of practical During the last 40 years, volumes of material describing and research activity related to the development and optimization the Siberian crane’s population in northeastern Yakutia of the population are examined. have been collected by various investigators during special and passing aircraft surveys (table 1). The data collected are characterized by significant variation in population size and habitat size estimation. In all cases, the extrapolation of Conservation of the white crane (Grus leucogeranus), a survey data was made without use of any necessary correc- globally imperiled species, is determined principally by the tion for methodical errors that can be introduced by conflict condition of its eastern population. The breeding area and between aircraft and ground survey results. main summer habitat of this population are subarctic tun- The cartographic registration of birds (scale 1:100,000) dra, forest tundra, and northern taiga in a vast system of during aircraft and ground observations in 1993 to 1997 lake depressions in northeastern Yakutia. To various de- 2 (following banding in 1990 to 1992) within the 1,314 km grees, the birds are found in the northern part of the control site in the Indigirsky population resulted in the territory, in the area between the Yana and Omoloy Rivers, identification of 86 individuals: 38 couples, four single birds, to the Kolyma River’s left bank—and in the southern part, 2 and two groups of three birds each (6.54 birds per 100 km ). in the Indigirka and Kolyma River basins up to the Momsky Forty of these birds, including 17 couples, were found in the Range’s northern spurs. The basic habitat area in Yakutia 2 course of a ground survey on July 5 to 10, 1995, in an area makes up between 220,000 to 300,000 km . The main part of 2 of 502 km (38 percent of the control site). The local density the nesting population is concentrated in the northern half of birds was 7.97 individuals per 100 km2 (Germogenov and of this area—in tundra and in forest tundra, which makes up others 1996). A similar population density was observed 130,000 km2 (Flint and Kisshchinsky 1975). According to during a ground survey dated August 5 to 10, 1995, in the recent investigations, the area of the population’s regu- 2 territory adjacent to the control site—7.34 individuals per lar habitat (no more than 82,000 km ) is composed of 2 2 100 km (26 birds per 354 km ). Of the 38 couples recorded three isolated centers of increased bird density: Khromsky, 2 2 in the control site, 14 were observed during one season, nine 10,300 km ; Indigirsky, 7,900 to 9,700 km ; and Alazeysky, during two seasons, six during three seasons, five during 1,950 to 4,380 km2 (Degtyaryov and Labutin 1991). four seasons, three during five seasons, and one during six Some (probably nonbreeding) birds spend the summer seasons (1990 to 1997). This observation reflects the diffi- beyond the bounds of the observed region—in the Lena River culty of yearly bird tracking, but suggests a strong attach- basin (the Linde and Khoruongka River basins) west of the ment for the territory. Accounting for annual variability in Zhigansk settlement (Degtyaryov and Labutin 1991). territorial fidelity and return rates, a population density from the control site of 5.4 birds per 100 km2, was indicated. Comparing this density with the estimates of Degtyaryov and Labutin (1991) for the same area (for example, 2.5 birds per 100 km2 in 1985; 1.7 per 100 km2 in 1987; and 2.63 per 100 km2 in 1989) suggests a correction factor (K + 2.46) In: Watson, Alan E.; Aplet, Greg H.; Hendee, John C., comps. 1998. to convert aerial survey numbers to estimates of the true Personal, societal, and ecological values of wilderness: Sixth World Wil- population size. derness Congress proceedings on research, management, and allocation, Applying this correction factor to white crane numbers volume I; 1997 October; Bangalore, India. Proc. RMRS-P-4. Ogden, UT: U.S. Department of Agriculture, Forest Service, Rocky Mountain Research in northeastern Yakutia (670 to 790 birds) estimated by Station. aircraft survey (Degtyaryov and Labutin 1991) yields an N. I. Germogenov is Professor at the Yakutsk Institute of Biology, estimated population size of 1,650 to 1,950 birds in this Russian Academy of Sciences, Lenin Avenue, 41, 677891, Yakutsk. E-mail: [email protected]. territory. USDA Forest Service Proceedings RMRS-P-4. 1998 55 Table 1—Information on white crane habitat and numbers in the Northeast of Yakutia. Area of main habitat (centres of increased Number of birds in main habitat Information source Period population density) (centres of increased population density) km2 Vorobyov 1963 1957-1960 — 200-250 couples or 400-500 specimens Uspenski and others 1962 1960 2,500-3,000 500-700 couples or 1,000-1,400 specimens Yegorov 1965 1963 20,000 900 specimens Yegorov 1971 1963-1964, 1966 32,000 1,500 specimens Flint and Kisshchinsky 1975 1971 130,000 (30,000) 300 specimens Flint and Sorokin 1982a,b 1977-1980 — 250-300 specimens Perfilyev 1965 1960-1962 — 300-350 couples or 600-700 specimens Perfilyev and Polakov 1979 1975, 1977 130,000 (30,000) 700 specimens Vshivtsev and others 1979 1978 >130,000 (51,000) 325 (301) specimens Labutin and others 1982 1980 65,560a 433 specimens Degtyaryov and Labutin 1991 1978-1989 82,000b (21,530c) 670-790 (572) specimens aTotal area of the population’s main distribution. bThe population’s regular breeding area. cTotal area of the three centres of increased density of the population. Particularly Protected Natural North East Asian Crane Site Network in 1997. Of the 13 protected territories in table 2, seven are included on the Territories______________________ preliminary “List of Important Bird Areas” or I.B.A. (1996). The Kytalyk Resource Reserve and the Chaygurino (two Preliminary population estimates are essential to evalu- 2 sites) and Khroma Reserves total 38,275 km or 12.8 percent ate the potential of the Particularly Protected Natural of the main range and 46.7 percent of the Yakutian Territories system being developed in the Sakha Republic population’s regular habitat area. These three reserves (Yakutia) to help conserve the white crane. carry most of the basic load of protection of breeding area Historically, indigenous Sakha people both revered the and summer habitat. According to population estimates, white crane as an image of purity and femininity, and relied 712 birds (37 to 43.7 percent of the population) nest or spend on it for meat and eggs (Andreyev 1974, 1987; Beme and summers within these territories. Within these reserves Priklonsky 1976; Ergis 1960; Maak 1886; Mikhel 1935; are several “centres” of markedly increased population den- Vorobyov 1963). In the last century, legal measures for sity. The Khromsky population centre accounts for 14 per- white crane protection in Yakutia were established (Hunt- 2 cent of the territory (or 1,477 km ), the Indigirsky centre ing Regulations of 1962) that forbade the hunting of this 2 makes up 33 to 40.6 percent (3,204 km ), and the Alazeysky species. The first Particularly Protected Natural Territory, 2 centre (up to 1989) up to 90 percent (2,430 km ). Thus, the which directly addressed conservation of the white cranes’ 2 total protected area comprises 7,111 km or 29.2 to 35.3 eastern population, was established in the early 1980’s. percent of the areas of increased population density and The long-term plan for the Particularly Protected Natu- the habitat of 422 birds (21.6 to 25.6 percent of the total ral Territory system was established by Sakha Republic population). President M. E. Nikolayev’s Decree, “On Measures of Beyond this main range of the population, white cranes Particularly Protected Natural Territories Development.” are sometimes found within territories and vicinities of According to the federal-regional legislative base currently the Ust-Lensky State Sanctuary situated in the Bulunsky in force, Particularly Protected Natural Territories are placed Ulus (Labutin and others 1982; Perfilyev and Polyakov under the federal (State Sanctuaries and Reserves), regional 1979), the Ust-Viluysky State Reserve in the Kobyaisky (National Parks, Resource Reserves), and local (Reserve Ter- Ulus (Report Cadastre of white crane in the Sakha Republic ritories) authority. Particularly Protected Natural Territo- (Yakutia) 1991), and the Ungra State Reserve in the ries of regional and local significance are developed without Neryungrinsky Ulus (Perfilyev 1965). In addition, signifi- their withdrawal from economic turnover, generally charac- cant newly established Reserve Territories are situated in terized by traditional nature use.
Recommended publications
  • Download Download
    Journal of History Culture and Art Research (ISSN: 2147-0626) Tarih Kültür ve Sanat Araştırmaları Dergisi Vol. 7, No. 3, September 2018 Revue des Recherches en Histoire Culture et Art Copyright © Karabuk University http://kutaksam.karabuk.edu.tr ﻣﺠﻠﺔ اﻟﺒﺤﻮث اﻟﺘﺎرﯾﺨﯿﺔ واﻟﺜﻘﺎﻓﯿﺔ واﻟﻔﻨﯿﺔ DOI: 10.7596/taksad.v7i3.1738 Citation: Charina, O. (2018). Dynasties of Russian Storytellers in Yakutia and the Features of Their Repertoire (Bylinas and Historical Songs as a Case-Study). Journal of History Culture and Art Research, 7(3), 353-362. doi:http://dx.doi.org/10.7596/taksad.v7i3.1738 Dynasties of Russian Storytellers in Yakutia and the Features of Their Repertoire (Bylinas and Historical Songs as a Case-Study) Olga Iosifovna Charina1 Abstract The article studies the traditional family features of Russian folklore in Yakutia of the Russian people living in an area near the mouth of the Kolyma River, the Indigirka River and the midstream of the Lena River. Within the scope of research on the general outline of Russian folklore distribution in Yakutia during its period of flourishment, we also overview the local features which were established in the course of an extended time-period; a number of example will be presented from epic texts created in the following areas: Biryuk of the Olyokminsky region, Pohodsk and Russkoye Ustye located on the shore of the Arctic Ocean. Written records by V.G. Bogoraz compiled at the end of the 19th century, the written records compiled by S.I. Bolo, N.A. Gabyshev at the early 1940s, and written records created by Y.I.
    [Show full text]
  • Supplementary Information
    Supplementary Information Table S1. List of samples that yielded DNA in this study (EE2-EE26), followed by successfully amplified samples of cave lion from the study by Barnett et al. 2009. ALA=Alaska, EUR=Europe, SIB=Siberia, NC=not calibrated as out of range. The asterisk (*) denotes the approximate age as reported in Barnett et al. 2009. Sample CR haplotype/ Uncalibrated Calendar years Site and geographic region ID Genbank nr. 14C date before present EE2 D/ DQ899903 Schusterlucke cave (EUR) 15400 ± 130 18521 ± 1844 EE4 - Tyung, C Siberia (SIB) 46700±1300 48181 ± 6747 EE3 Y3 Tain cave, Urals (EUR) >49600 NC EE6 Y1 Elovka, Baikal (SIB) 18350 ± 75 21634 ± 1504 EE7 Y1 Volchika, C Siberia (SIB) 20085 ± 80 23266 ± 576 EE13 J/ DQ899909 New Siberian Islands (SIB) 47700 ± 800 48970 ± 6009 EE14 Y4 Yakutia, NE Siberia (SIB) >55400 NC EE15 B/ DQ899901 Yakutia, NE Siberia (SIB) 27720 ± 140 30880 ± 1543 EE16 Y2 Irkutsk, Baikal (SIB) 17910 ± 75 21024 ± 1041 EE17 B/ DQ899901 Khroma river, Yakutia (SIB) 19755 ± 80 20006 ± 404 EE19 - New Siberian Islands (SIB) 52000±1500 54373 ± 6396 EE20 J/ DQ899909 Yakutia, NE Siberia (SIB) >62400 NC EE21 G/ DQ899906 Nizhnyaya, C Siberia (SIB) 50500 ± 290 52785 ± 10541 EE26 Y5 (partial) Kyttyk Peninsula (SIB) 36550 ± 290 41025 ± 970 IB133 A/ DQ899900 Gold Run Creek, Yukon (ALA) 12640 ± 75 15016 ± 1463 RB112 A Caribou Creek, Yukon (ALA) n/a - RB74 A Fairbanks Creek, Alaska (ALA) n/a - RB75 A Ester Creek, Alaska (ALA) 12090 ± 80 13822 ± 341 IB134 B/ DQ899901 Gold Hill, Alaska (ALA) 18240 ± 90 21533 ± 1335 IB136 B Hunker
    [Show full text]
  • Le Canada : Une Culture De Métissage/Transcultural Canada
    LE CANADA : UNE CULTURE DE MÉTISSAGE/ TRANSCULTURAL CANADA LE CANADA : UNE CULTURE DE MÉTISSAGE/ TRANSCULTURAL CANADA Sous la direction de PAUL D. MORRIS Nous remercions le Conseil des arts du Canada de son soutien. L’an dernier, le Conseil a investi 153 millions de dollars pour mettre de l’art dans la vie des Canadiennes et des Canadiens de tout le pays. We acknowledge the support of the Canada Council for the Arts, which last year invested $153 million to bring the arts to Canadians throughout the country. Les Presses de l’Université Laval reçoivent chaque année du Conseil des Arts du Canada et de la Société de développement des entreprises culturelles du Québec une aide financière pour l’ensemble de leur programme de publication. Maquette de couverture : Laurie Patry Mise en pages : Danielle Motard ISBN papier : 978-2-7637-4269-4 ISBN pdf : 9782763742700 © Les Presses de l’Université Laval Tous droits réservés. Imprimé au Canada Dépôt légal 1er trimestre 2019 Les Presses de l’Université Laval www.pulaval.com Toute reproduction ou diffusion en tout ou en partie de ce livre par quelque moyen que ce soit est interdite sans l’autorisation écrite des Presses de l’Université Laval. … pour ma propre petite famille, métissée по-своему TABLE DES MATIÈRES REMERCIEMENTS XI INTRODUCTION 1 Paul D. Morris PREMIÈRE PARTIE INTERROGATIONS THÉORIQUES ET CRITIQUES 1 Six Theses on Transculturality: A View from the New World 19 Afef Benessaieh 2 À la recherche du Canadien : l’idée de métissage culturel, un aboutissement identitaire ? 39 Franck Chignier-Riboulon
    [Show full text]
  • Gialens 2017 Volume 11, No
    GIALens 2017 Volume 11, No. 2 GIALens volume 11 | number 2 A festschrift for Vasilii Vasilievich Illarionov GIALens 2017 Volume 11, No. 2 The Graduate Institute of Applied Linguistics (GIAL) is accredited by the Southern Association of Colleges and Schools Commission on Colleges (SACSCOC) to award Baccalaureate and Masters degrees. Contact the Commission on Colleges at 1866 Southern Lane, Decatur, Georgia 30033-4097 or call 404-679-4500 for questions about the accreditation of the Graduate Institute of Applied Linguistics. Please send editorial correspondence to the editor: [email protected] Graduate Institute of Applied Linguistics 7500 W. Camp Wisdom Road Dallas, TX 75236 U.S.A Editorial Board Dr. Doug Tiffin, President Dr. Michael Boutin, Chair, Applied Linguistics Department Dr. Steve Walter, Chair, Applied Anthropology Department GIALens 2017 Volume 11, No. 2 GIALens Volume 11 Number 2 Note to the reader: This issue of GIALens celebrates the 70th anniversary of Vasilii Illarionov’s birth and highlights his contribution to Sakha folkloristics and in particular the study of the Sakha epic tradition of olonkho. The articles featured in this issue have been written by some of his colleagues and friends in Yakutsk, Republic of Sakha (Yakutia), Russian Federation, and translated and edited by a team at GIAL’s Center for Excellence in World Arts, where the Sakha arts, among other forms of expressive arts, are studied at the graduate and undergraduate levels. Disclaimer: The views expressed in documents served by this site do not necessarily reflect the views of the Graduate Institute of Applied Linguistics nor any departments contained therein. Views are the sole property of the respective authors.
    [Show full text]
  • Laptev Sea System
    Russian-German Cooperation: Laptev Sea System Edited by Heidemarie Kassens, Dieter Piepenburg, Jör Thiede, Leonid Timokhov, Hans-Wolfgang Hubberten and Sergey M. Priamikov Ber. Polarforsch. 176 (1995) ISSN 01 76 - 5027 Russian-German Cooperation: Laptev Sea System Edited by Heidemarie Kassens GEOMAR Research Center for Marine Geosciences, Kiel, Germany Dieter Piepenburg Institute for Polar Ecology, Kiel, Germany Jör Thiede GEOMAR Research Center for Marine Geosciences, Kiel. Germany Leonid Timokhov Arctic and Antarctic Research Institute, St. Petersburg, Russia Hans-Woifgang Hubberten Alfred-Wegener-Institute for Polar and Marine Research, Potsdam, Germany and Sergey M. Priamikov Arctic and Antarctic Research Institute, St. Petersburg, Russia TABLE OF CONTENTS Preface ....................................................................................................................................i Liste of Authors and Participants ..............................................................................V Modern Environment of the Laptev Sea .................................................................1 J. Afanasyeva, M. Larnakin and V. Tirnachev Investigations of Air-Sea Interactions Carried out During the Transdrift II Expedition ............................................................................................................3 V.P. Shevchenko , A.P. Lisitzin, V.M. Kuptzov, G./. Ivanov, V.N. Lukashin, J.M. Martin, V.Yu. ßusakovS.A. Safarova, V. V. Serova, ßvan Grieken and H. van Malderen The Composition of Aerosols
    [Show full text]
  • Quaternary International Xxx (2010) 1E23
    ARTICLE IN PRESS Quaternary International xxx (2010) 1e23 Contents lists available at ScienceDirect Quaternary International journal homepage: www.elsevier.com/locate/quaint Sedimentary characteristics and origin of the Late Pleistocene Ice Complex on north-east Siberian Arctic coastal lowlands and islands e A review L. Schirrmeister a,*, V. Kunitsky b, G. Grosse c, S. Wetterich a, H. Meyer a, G. Schwamborn a, O. Babiy b, A. Derevyagin d, C. Siegert a a Alfred Wegener Institute for Polar and Marine Research, Periglacial Research, Telegrafenberg A 43, 14471 Potsdam, Germany b Melnikov Permafrost Institute RAS SB, Merslotnaya Street, Yakutsk, Republic of Sakha, (Yakutia), 677010 Russia c Geophysical Institute, University of Alaska Fairbanks (UAF), 903 Koyukuk Drive, Fairbanks, AK 99775, USA d Moscow State University (MSU), Faculty of Geology Russia, Moscow 119899, Vorobievy Gory article info abstract Article history: The origin of Late Pleistocene ice-rich, fine-grained permafrost sequences (Ice Complex deposits) in arctic Available online xxx and subarctic Siberia has been in dispute for a long time. Corresponding permafrost sequences are frequently exposed along seacoasts and river banks in Yedoma hills, which are considered to be erosional remnants of Late Pleistocene accumulation plains. Detailed cryolithological, sedimentological, geochro- nological, and stratigraphical results from 14 study sites along the Laptev and East Siberian seacoasts were summarized for the first time in order to compare and correlate the local datasets on a large regional scale. The sediments of the Ice Complex are characterized by poorly-sorted silt to fine-sand, buried cryosols, TOC contents of 1.2e4.8 wt%, and very high ground ice content (40e60 wt% absolute).
    [Show full text]
  • Wild Reindeer of Yakutia
    The Sixth North American Caribou Workshop, Prince George, British Columbia, Canada, 1-4 March, 1994. Brief communication Wild reindeer of Yakutia V. M. Safronov Institute of Applied Ecology of the North, Siberian Division, Russian Academy of Sciences, Yakutsk, Russia. Abstract: Three major herds of wild reindeer (Rangifer tarandus tarandus L.), totaling over 200,000 animals, occur in the tundra and taiga of northern Yakutia. These herds have been expanding since the late 1950s and now occupy most of their historic range. In addition, several thousand wild reindeer occupy the New Siberian Islands and adjacent coastal mainland tundra, and there are about 60,000 largely sedentary forest reindeer in mountainous areas of the southern two- thirds of the province. Wild reindeer are commercially hunted throughout the mainland, and the production of wild meat is an important part of the economy of the province and of individual reindeer enterprises which produce both wild and domestic meat. Key words: commercial harvest, density, economic importance, industrial development, Lena-Olenek, movements, Russia, Sundrun, Yana-Indigirka Rangifer, Special Issue No. 9, 387-390 Introduction population dynamics, economic importance, and Three major herds of wild reindeer {Rangifer taran• conservation. dus) occur on the continental tundras of the autonomous province of Yakutia. These herds are Yana-Indigirka herd the Yana-Indigirka, Sundrun (Indigirka-Kolyma) Movements and distribution and Lena-Olenek (Bulun) (Fig. 1; Table 1). A sepa• The current range of the Yana-Indigirka herd covers rate herd also inhabits the New Siberian Islands in about 400,000 km2 (Fig. 1) and is similar to the range summer but winters extensively on the adjacent of this herd at the turn of the century (Mikhel, 1938).
    [Show full text]
  • 304 Isaev Layout 1
    CHANGE IN PTARMIGAN NUMBERS IN YAKUTIA ARKADY P. ISAEV Institute for Biological Problems of the Cryolithozone, Siberian Branch of the Russian Academy of Sciences, pr. Lewina 41, Yakutsk 677007, Russia. E-mail: [email protected] ABSTRACT.—Counts of Willow Ptarmigan (Lagopus lagopus) and Rock Ptarmigan (L. muta) have been conducted for as long as 25 years in some areas of the Russian Republic of Yakutia in tundra, taiga, and along the ecotone of these landscapes. The largest counts of Willow Ptarmigan occur in the tundra and forest-tundra. Willow Ptarmigan numbers fluctuate, and the length of the “cycles” vary among areas in Yakutia. Fluctuations in ptarmigan numbers are greater in the tundra and forest-tundra than in the northern taiga. Rock Ptarmigan are common in the mountain areas and tundra of Yakutia, and their numbers also fluctuate. Factors affecting ptarmigan populations are weather shifts in early spring and unfavorable weather during hatching. A decrease in the num- ber of Willow Ptarmigan in the taiga belt of Yakutia is most likely explained by a greater anthro- pogenic load. Current Willow and Rock Ptarmigan populations in Yakutia appear stable, except for central and southern areas. Received 1 February 2011, accepted 31 May 2011. ISAEV, A. P. 2011. Change in ptarmigan number in Yakutia. Pages 259–266 in R. T. Watson, T. J. Cade, M. Fuller, G. Hunt, and E. Potapov (Eds.). Gyrfalcons and Ptarmigan in a Changing World, Volume II. The Peregrine Fund, Boise, Idaho, USA. http://dx.doi.org/10.4080/gpcw.2011.0304 Key words: Willow Ptarmigan, Rock Ptarmigan, Yakutia, Russia, count changes.
    [Show full text]
  • OYMYAKON RING STRUCTURE in the NORTH-EASTERN SIBERIA: ONE MORE TERRESTRIAL COUNTERPART of Coronm on VENUS; G.A
    LPS XXVT 189 OYMYAKON RING STRUCTURE IN THE NORTH-EASTERN SIBERIA: ONE MORE TERRESTRIAL COUNTERPART OF CORONm ON VENUS; G.A. Burba, Vernadsky Institute, Moscow 117975, Russia The highest area of the vast mountain country in the NE Siberia consists of the mountain ranges arranged as a 380-km-diameter ring structure. It is located between 62 and 66 N latitude, 139 and 148 E longitude, centering at 64 N, 143.5 E. The general topographic shape of this ring structure - a higher mountain ring (up to 3000 m) with a lower, but still topographically high (1000-1200 m), plateau inside, and lowland plains outside - resembles typical topography of the large circular features on Venus termed Corona (pl. - Coronae). The ring structure under consideration will be referred further as Oymyakon Ring Structure (OyRS) after Oymyakon Highland (Oymyakonskoye Nagorye) which occupies the considerable area within this ring structure, as well as after Oymyakon settlement located close to the structure's center. This settlement is well known as the Earth's Northern hemisphere "pole of cold". The topographically most prominent parts of the OyRS rim are Chersky Range (Khrebet Cherskogo) as NE segment, and Suntar-Khayata Range as SW segment. The following description is tracing the rim crest position from the South part of the rim to West, North, East, and back to South. SW segment of OyRS rim goes from Druza Mt. (2745 m) westward along Suntar- Khayata Range to 2933 m Mount, then to Mus-Khaya Mt. (2959 m), then to 2409 m Mount. NW segment of OyRS rim goes from 2409 m Mount (Western Suntar-Khayata Range) northward to 2041 m Mount at western edge of Oymyakon Highland, then to 1872 m Mount at southern part of Elgin Plateau (Elginskoye Ploskogorye), then some 50 km east of Vershina-Tuoydakh Mt.
    [Show full text]
  • Detailed Species Accounts from the Threatened Birds Of
    Threatened Birds of Asia: The BirdLife International Red Data Book Editors N. J. COLLAR (Editor-in-chief), A. V. ANDREEV, S. CHAN, M. J. CROSBY, S. SUBRAMANYA and J. A. TOBIAS Maps by RUDYANTO and M. J. CROSBY Principal compilers and data contributors ■ BANGLADESH P. Thompson ■ BHUTAN R. Pradhan; C. Inskipp, T. Inskipp ■ CAMBODIA Sun Hean; C. M. Poole ■ CHINA ■ MAINLAND CHINA Zheng Guangmei; Ding Changqing, Gao Wei, Gao Yuren, Li Fulai, Liu Naifa, Ma Zhijun, the late Tan Yaokuang, Wang Qishan, Xu Weishu, Yang Lan, Yu Zhiwei, Zhang Zhengwang. ■ HONG KONG Hong Kong Bird Watching Society (BirdLife Affiliate); H. F. Cheung; F. N. Y. Lock, C. K. W. Ma, Y. T. Yu. ■ TAIWAN Wild Bird Federation of Taiwan (BirdLife Partner); L. Liu Severinghaus; Chang Chin-lung, Chiang Ming-liang, Fang Woei-horng, Ho Yi-hsian, Hwang Kwang-yin, Lin Wei-yuan, Lin Wen-horn, Lo Hung-ren, Sha Chian-chung, Yau Cheng-teh. ■ INDIA Bombay Natural History Society (BirdLife Partner Designate) and Sálim Ali Centre for Ornithology and Natural History; L. Vijayan and V. S. Vijayan; S. Balachandran, R. Bhargava, P. C. Bhattacharjee, S. Bhupathy, A. Chaudhury, P. Gole, S. A. Hussain, R. Kaul, U. Lachungpa, R. Naroji, S. Pandey, A. Pittie, V. Prakash, A. Rahmani, P. Saikia, R. Sankaran, P. Singh, R. Sugathan, Zafar-ul Islam ■ INDONESIA BirdLife International Indonesia Country Programme; Ria Saryanthi; D. Agista, S. van Balen, Y. Cahyadin, R. F. A. Grimmett, F. R. Lambert, M. Poulsen, Rudyanto, I. Setiawan, C. Trainor ■ JAPAN Wild Bird Society of Japan (BirdLife Partner); Y. Fujimaki; Y. Kanai, H.
    [Show full text]
  • Crustal Architecture of the East Siberian Arctic Shelf and Adjacent Arctic Ocean Constrained by Seismic Data and Gravity Modeling Results
    This is a repository copy of Crustal architecture of the East Siberian Arctic Shelf and adjacent Arctic Ocean constrained by seismic data and gravity modeling results. White Rose Research Online URL for this paper: http://eprints.whiterose.ac.uk/129730/ Version: Accepted Version Article: Drachev, SS, Mazur, S, Campbell, S et al. (2 more authors) (2018) Crustal architecture of the East Siberian Arctic Shelf and adjacent Arctic Ocean constrained by seismic data and gravity modeling results. Journal of Geodynamics, 119. pp. 123-148. ISSN 0264-3707 https://doi.org/10.1016/j.jog.2018.03.005 Crown Copyright © 2018 Published by Elsevier Ltd. This is an author produced version of a paper published in Journal of Geodynamics. Uploaded in accordance with the publisher's self-archiving policy. This manuscript version is made available under the Creative Commons CC-BY-NC-ND 4.0 license http://creativecommons.org/licenses/by-nc-nd/4.0/. Reuse This article is distributed under the terms of the Creative Commons Attribution-NonCommercial-NoDerivs (CC BY-NC-ND) licence. This licence only allows you to download this work and share it with others as long as you credit the authors, but you can’t change the article in any way or use it commercially. More information and the full terms of the licence here: https://creativecommons.org/licenses/ Takedown If you consider content in White Rose Research Online to be in breach of UK law, please notify us by emailing [email protected] including the URL of the record and the reason for the withdrawal request.
    [Show full text]
  • Tracing Silicate Weathering Processes in the Permafrost-Dominated Lena River Watershed Using Lithium Isotopes
    Available online at www.sciencedirect.com ScienceDirect Geochimica et Cosmochimica Acta 245 (2019) 154–171 www.elsevier.com/locate/gca Tracing silicate weathering processes in the permafrost-dominated Lena River watershed using lithium isotopes Melissa J. Murphy a,⇑, Don Porcelli a, Philip A.E. Pogge von Strandmann b, Catherine A. Hirst c,d, Liselott Kutscher c,e, Joachim A. Katchinoff f, Carl-Magnus Mo¨rth e, Trofim Maximov g, Per S. Andersson c a Department of Earth Sciences, University of Oxford, South Parks Road, Oxford OX1 3AN, UK b London Geochemistry and Isotope Centre (LOGIC), Institute of Earth and Planetary Sciences, University College London and Birkbeck College, Gower Street, London WC1E 6BT, UK c Department of Geosciences, Swedish Museum of Natural History, Box 50007, SE-104 05 Stockholm, Sweden d Earth and Life Institute, Universite´ catholique de Louvain, Croix du Sud, L7.05.10, B-1348 Louvain-la-Neuve, Belgium e Department of Geological Sciences, Stockholm University, SE-10691 Stockholm, Sweden f Department of Geology & Geophysics, Yale University, USA g Institute for Biological Problems of the Cryolithozone, Siberian Branch, Russian Academy of Science, Russia Received 25 March 2018; accepted in revised form 19 October 2018; Available online 31 October 2018 Abstract Increasing global temperatures are causing widespread changes in the Arctic, including permafrost thawing and altered freshwater inputs and trace metal and carbon fluxes into the ocean and atmosphere. Changes in the permafrost active layer thickness can affect subsurface water flow-paths and water-rock interaction times, and hence weathering processes. Riverine lithium isotope ratios (reported as d7Li) are tracers of silicate weathering that are unaffected by biological uptake, redox, car- bonate weathering and primary lithology.
    [Show full text]