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XI. International Conference on Permafrost, Book of Abstracts
XI. INTERNATIONAL CONFERENCE ON PERMAFROST | 20.-24. JUNE 2016 Landscapes and thermokarst lake area changes in Yedoma regions under modern climate conditions, Kolyma lowland tundra Aleksandra Veremeeva1, Nagezhda Glushkova2, Frank Günther3, Ingmar Nitze3, & Guido Grosse3 1Institute of Physical, Chemical and Biological Problems in Soil Science, Russian Academy of Sciences, Pushchino, Russia 2Institute of Geology and Mineralogy SB RAS, Novosibirsk, Russia 3Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Potsdam, Germany Recent landscape changes in the Yedoma region period. This map shows the magnitude and direction are particularly pronounced in varying thermokarst of changes for each multi-spectral index, which are lake areas reflecting the reaction of the land surface used as proxies for different land-surface properties. on modern climate changes. However, although ther- For single locations, the entire time-series can be fur- mokarst lake change detection is essential for the ther analyzed in more detail. For the period from quantification of water body expansion and drainage 1999 till 2005 air temperatures and precipitation have within a region, remote sensing-derived surface reflec- been analysed for several weather stations that existed tion trends additionally provide valuable information in the region. The Landsat time series analysis for about the general landscape development. The aim of the last 15 years shows that the northern part of the this research is to reveal the regularities of landscape region became wetter over the last 5 – 6 years. The and thermokarst lakes area changes in the Kolyma alases are particularly affected by the wetting trend. lowland tundra in comparison with meteorological The analysis of the meteo-data shows a trend of in- data and geological and geomorphological features. -
K. Fujita1, E. E. Dretzka2 and A. Grantz3 This Report Is Preliminary and Has Not Been Reviewed for Conformity with U. S. Geologi
UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY BIBLIOGRAPHY OF NORTHEAST SIBERIAN GEOLOGY AND GEOPHYSICS (SECOND EDITION) K. Fujita1, E. E. Dretzka2 and A. Grantz3 OPEN FILE REPORT 82-616 This report is preliminary and has not been reviewed for conformity with U. S. Geological Survey editorial standards. Menlo Park, California July 1982 1. Department of Geology, Michigan State University, East Lansing MI 48824 2. Department of Geological Sciences, Northwestern University, Evanston IL 60201; now at: Department of Computer Sciences, Stanford University, Stanford CA 94305. 3. U. S. Geological Survey, Menlo Park, CA 94025 INTRODUCTION This bibliography is a compendium of literature available in English, either in its original form or in translation, on the geology and geophysics of northeast Siberia and adjacent seas and shelves. It is an expanded version of Fujita and Dretzka (1978-) and has been updated to include publications released through early 1982. The area! coverage extends from the edge of the Siberian platform (just east of the Lena River) on the east to the U. S. - Russia Convention Line of 1867 on the west. The East Siberian and Chukchi Seas are included as the northern limit while the Sea if Okhotsk and Kamchatka represent the southern limits. Sakhalin has been excluded and some, but not all, references to the Kuril Islands have been included. A sketch map of the area is shown in figure 1. It is hoped that this listing is nearly exhaustive for works on this area with some exceptions. Neither the Paleontological Journal nor Petroleum Geology have been indexed in this edition and, in addition, articles on Recent seismicity and volcanic activity in the Kuril-Kamchatka arc have been omitted. -
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 -
The Brunhes-Matuyama Boundary in Western Beringia: a Review
Quaternary Science Reviews 30 (2011) 2054e2068 Contents lists available at ScienceDirect Quaternary Science Reviews journal homepage: www.elsevier.com/locate/quascirev The Brunhes-Matuyama boundary in Western Beringia: a review Pavel S. Minyuk*, Yury Yu. Ivanov 1 North-East Interdisciplinary Scientific Research Institute, Far East Branch Russian Academy of Science, 16 Portovaya St., Magadan 685000, Russia article info abstract Article history: Early-Middle Pleistocene deposits have been studied in Central and Northern Yakutia, the Magadan Received 24 September 2009 region, and Chukotka. The Brunhes-Matuyama boundary occurs in the Ozheleznenye Galechniki Received in revised form (¼Ferruginated pebblestones) beds of Central Yakutia that belong to the Talagay horizon of the Early- 31 May 2010 Middle Pleistocene. These layers include classic Aldan mammal fauna. In Eastern Yakutia sediments of Accepted 3 June 2010 Early-Middle Pleistocene belong to the Akan horizon, and the Early Pleistocene sediments are from the Available online 22 July 2010 Chukochya horizon. These sediments which belong to the Olyor Formation and its age-equivalents yielded numerous mammal remains, termed the Olyor faunal complex. The Brunhes-Matuyama boundary is located in Akan horizon. In the upper reaches of the Kolyma River, the Brunhes-Matuyama boundary occurs in sediments of the Middle Pleistocene Belichan horizon. The boundary of the Brunhes- Matuyama is characteristic within the Elhkakvun and Enmakay formations of Chukotka. In Kamchatka, the boundary of Matuyama and Brunhes is evident in volcanic sequences. In the eastern part of the peninsula, this boundary is located in the Tumrok or Iult volcanic complex and in Central Kamchatka in the Kreruk volcanic complex. -
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). -
Tectonic Evolution of the Mesozoic South Anyui Suture Zone, GEOSPHERE; V
Research Paper GEOSPHERE Tectonic evolution of the Mesozoic South Anyui suture zone, GEOSPHERE; v. 11, no. 5 eastern Russia: A critical component of paleogeographic doi:10.1130/GES01165.1 reconstructions of the Arctic region 18 figures; 5 tables; 2 supplemental files; 1 animation Jeffrey M. Amato1, Jaime Toro2, Vyacheslav V. Akinin3, Brian A. Hampton1, Alexander S. Salnikov4, and Marianna I. Tuchkova5 1Department of Geological Sciences, New Mexico State University, MSC 3AB, P.O. Box 30001, Las Cruces, New Mexico 88003, USA CORRESPONDENCE: [email protected] 2Department of Geology and Geography, West Virginia University, 330 Brooks Hall, P.O. Box 6300, Morgantown, West Virginia 26506, USA 3North-East Interdisciplinary Scientific Research Institute, Far East Branch, Russian Academy of Sciences, Magadan, Portovaya Street, 16, 685000, Russia CITATION: Amato, J.M., Toro, J., Akinin, V.V., Hamp- 4Siberian Research Institute of Geology, Geophysics, and Mineral Resources, 67 Krasny Prospekt, Novosibirsk, 630091, Russia ton, B.A., Salnikov, A.S., and Tuchkova, M.I., 2015, 5Geological Institute, Russian Academy of Sciences, Pyzhevskii per. 7, Moscow, 119017, Russia Tectonic evolution of the Mesozoic South Anyui su- ture zone, eastern Russia: A critical component of paleogeographic reconstructions of the Arctic region: ABSTRACT INTRODUCTION Geosphere, v. 11 no. 5, p. 1530–1564, doi: 10 .1130 /GES01165.1. The South Anyui suture zone consists of late Paleozoic–Jurassic ultra- The South Anyui suture zone (Fig. 1) is a remnant of a Mesozoic ocean Received 19 December 2014 mafic rocks and Jurassic–Cretaceous pre-, syn-, and postcollisional sedimen- basin that separated the Arctic Alaska–Chukotka microplate from Siberia Revision received 2 July 2015 tary rocks. -
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. -
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 -
VI. Republic of Sakha (Yakutia) Overview of the Region Josh
Saving Russia's Far Eastern Taiga : Deforestation, Protected Areas, and Forests 'Hotspots' VI. Republic of Sakha (Yakutia) Overview of the Region Josh Newell Location The Republic of Yakutia (Sakha), situated in northeastern Siberia, stretches to the Henrietta Islands (77 N) in the far north and is washed by the Arctic Ocean (Laptev and Eastern Siberian Seas). These waters, the coldest and iciest of all seas in the northern hemisphere, are covered by ice for 9 to 10 months of the year. The Stanovoy Ridge (55 D. 30 D. N) borders Yakutia in the south, the upper reaches of the Olenyok River form the western border, and Chukotka forms the eastern border (165 E). Size Almost one-fifth of the territory of the Russian Federation (3,103,200 sq. km.) and greater than the combined areas of France, Austria, Germany, Italy, Sweden, England, Greece, and Finland. Climate Winter is prolonged and severe, with average January temperatures about -40C. Summer is short but warm; the average in July is 13C and temperatures have reached 39C in Yakutsk. In the northeast, the town of Verekhoyansk reaches -70C (-83F) and is considered the coldest inhabited place on Earth. There is little precipitation - from 150-200 mm. in Central Yakutia to 500-700 mm. in the mountains of eastern and southern Yakutia. Geography and Ecology Forty percent of Yakutia lies within the Arctic Circle and all of it is covered by eternally frozen ground- permafrost - which greatly influences the region's ecology and limits forests to the southern region. Yakutia can be divided into three great vegetation belts. -
Wetlands in Russia
WETLANDS IN RUSSIA Volume 4 Wetlands in Northeastern Russia Compiled by A.V.Andreev Moscow 2004 © Wetlands International, 2004 All rights reserved. Apart from any fair dealing for the purpose of private study, research, criticism, or review (as permitted under the Copyright Designs and Patents Act 1988) no part of this publication may be reproduced, stored in a retrieval system or transmitted in any form or by any means, electronic, electrical, chemical, mechanical, optical, photocopying, recording or otherwise, without prior permission of the copyright holder. The production of this publication has been generously supported by the Ministry of Agriculture, Nature and Food Quality, The Netherlands Citation: Andreev, A.V. 2004. Wetlands in Russia, Volume 4: Wetlands in Northeastern Russia. Wetlands International–Russia Programme.198 pp. ISBN 90-5882-024-6 Editorial Board: V.O.Avdanin, V.G.Vinogradov, V.Yu. Iliashenko, I.E.Kamennova, V.G.Krivenko, V.A.Orlov, V.S.Ostapenko, V.E.Flint Translation: Yu.V.Morozov Editing of English text: D. Engelbrecht Layout: M.A.Kiryushkin Cover photograph: A.V.Andreev Designed and produced by KMK Scientific Press Available from: Wetlands International-Russia Programme Nikoloyamskaya Ulitsa, 19, stroeniye 3 Moscow 109240, Russia Fax: + 7 095 7270938; E-mail: [email protected] The presentation of material in this publication and the geographical designations employed do not imply the expression of any opinion whatsoever on the part of Wetlands International, concerning the legal status of any territory or area, -
Russian Cartography to Ca. 1700 L
62 • Russian Cartography to ca. 1700 L. A. Goldenberg the Sources of the Cartography of Russia,” Imago Mundi 16 (1962): The perception of a “foreign beginning” to Russian car- 33– 48. 1 tography is deeply rooted. It has been fostered by the 2. In al-Idrı¯sı¯’s large world map, Eastern Europe is placed on eight irretrievable loss of indigenous Russian maps of pre- sheets (nos. 54 –57, 64 –67), which show the Caspian lands, Bashkiria, seventeenth-century date, along with the unfamiliarity Volga Bulgaria, the upper reaches of the Severny (Severskiy) Donets, the with other sources. Thus the traditional cartographic im- Black Sea area, the lower Dniester area, the upper Dnieper area, the Carpathians, the Danube area, and the Baltic area, whereas the north- age of Russia was that provided by the Western European ern Caucasus and the lower Volga area are more distorted. In al-Idrı¯sı¯’s mapmakers. The name “Russia” first appeared in this map, sources for the ancient centers of ninth-century Rus are combined foreign cartographic record in the twelfth century. For ex- with more precise data on the well-traveled trade routes of the twelfth ample, on the Henry of Mainz mappamundi (ca. 1110), century. For al-Idrı¯sı¯ and the map of 1154, see S. Maqbul Ahmad, “Car- it is placed north of the mouth of the Danube; on the map tography of al-Sharı¯f al-Idı¯sı¯,” in HC 2.1:156 –74; Konrad Miller, Map- 2 pae arabicae: Arabische Welt- und Länderkarten des 9.–13. Jahrhun- of the cartographer al-Idrı¯sı¯ (1154), interesting geo- derts, 6 vols. -
Chronology of the Key Historical Events on the Eastern Seas of the Russian Arctic (The Laptev Sea, the East Siberian Sea, the Chukchi Sea)
Chronology of the Key Historical Events on the Eastern Seas of the Russian Arctic (the Laptev Sea, the East Siberian Sea, the Chukchi Sea) Seventeenth century 1629 At the Yenisei Voivodes’ House “The Inventory of the Lena, the Great River” was compiled and it reads that “the Lena River flows into the sea with its mouth.” 1633 The armed forces of Yenisei Cossacks, headed by Postnik, Ivanov, Gubar, and M. Stadukhin, arrived at the lower reaches of the Lena River. The Tobolsk Cossack, Ivan Rebrov, was the first to reach the mouth of Lena, departing from Yakutsk. He discovered the Olenekskiy Zaliv. 1638 The first Russian march toward the Pacific Ocean from the upper reaches of the Aldan River with the departure from the Butalskiy stockade fort was headed by Ivan Yuriev Moskvitin, a Cossack from Tomsk. Ivan Rebrov discovered the Yana Bay. He Departed from the Yana River, reached the Indigirka River by sea, and built two stockade forts there. 1641 The Cossack foreman, Mikhail Stadukhin, was sent to the Kolyma River. 1642 The Krasnoyarsk Cossack, Ivan Erastov, went down the Indigirka River up to its mouth and by sea reached the mouth of the Alazeya River, being the first one at this river and the first one to deliver the information about the Chukchi. 1643 Cossacks F. Chukichev, T. Alekseev, I. Erastov, and others accomplished the sea crossing from the mouth of the Alazeya River to the Lena. M. Stadukhin and D. Yarila (Zyryan) arrived at the Kolyma River and founded the Nizhnekolymskiy stockade fort on its bank.