Mapping Siberian Arctic Mountain Permafrost Landscapes by Machine Learning Multi-Sensors Remote Sensing: Example of Adycha River Valley
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1 Reply to Editor's Co E Ts Dear Denis-Didier, We Much Appreciate Your Effort and Your Helpful Comments. Our Replies Are Given
Reply to editor’s coets Dear Denis-Didier, we much appreciate your effort and your helpful comments. Our replies are given below in blue. Please note: All page and line numbers refer to the revised manuscript with track changes after completing the revision based on comments of three referees. P3, L6 What is the elevation of the site? You never indiacte such parameter to the study sites, please do so Thank you for this suggestion! We added the elevation for both study sites. P4, L14 give the coordinates of this site Thank you for this suggestion! We added coordinates for our Adycha sampling site. P4, L26 I guess these bags were prepared before to prevent any pollution. Can you precise this point please? We used freshly opened standard Whirl-Pak bags to store and melt the samples without any additional preparation. We added some information to the text. P5, L11 How was it extracted? We picked organic remains from our ice-wedge as well as host sediment samples at the ice-wedge sampling sites. We added this to the manuscript. P7, L22 add "bs" that you use later Changed accordingly. P7, L26 can you be more precise than unidentified plant? Were they leaves, piece of wood, roots? Same thing about the beetle remains. We added more details to the text (Plants: bract fragments and roots, Beetle remains: complete pieces and fragments of elytron). P7, L29 idem We added more details to the text (twigs, roots and florets). P8, L16 can you check as it seems to be rather Empetrum nigrum? add also the common name "crowberry" Thank you for correcting our mistake! Changed accordingly. -
Description of Map Units Northeast Asia Geodynamics Map
DESCRIPTION OF MAP UNITS NORTHEAST ASIA GEODYNAMICS MAP OVERLAP ASSEMBLAGES (Arranged alphabetically by map symbol) ad Adycha intermountain sedimentary basin (Miocene and Pliocene) (Yakutia) Basin forms a discontinuous chain along the foot of southwestern slope of Chersky Range in the Yana and Adycha Rivers basins. Contain Miocene and Pliocene sandstone, pebble gravel conglomerate, claystone, and minor boulder gravel conglomerate that range up to 400 m thick. REFERENCES: Grinenko and others, 1998. ag Agul (Rybinsk) molasse basin (Middle Devonian to Early Carboniferous) (Eastern Sayan) Consists of Middle Devonian through Early Carboniferous aerial and lacustrine sand-silt-mudstone, conglomerate, marl, and limestone with fauna and flora. Tuff, tuffite, and tuffaceous rock occur in Early Carboniferous sedimentary rocks. Ranges up to 2,000 m thick in southwestern margin of basin. Unconformably overlaps Early Devonian rocks of South Siberian volcanic-plutonic belt and Precambrian and early Paleozoic rocks of the Siberian Platform and surrounding fold belts. REFERENCES: Yanov, 1956; Graizer, Borovskaya, 1964. ags Argun sedimentary basin (Early Paleozoic) (Northeastern China) Occurs east of the Argun River in a discontinuously exposed, northeast-trending belt and consists of Cambrian and Ordovician marine, terrigenous detrital, and carbonate rocks. Cambrian units are composed of of feldspar- quartz sandstone, siltstone, shale and limestone and contain abundant Afaciacyathus sp., Bensocyathus sp., Robustocyathus yavorskii, Archaeocyathus yavorskii(Vologalin), Ethomophyllum hinganense Gu,o and other fossils. Ordovicain units consist of feldspar-quartz sandstone, siltstone, fine-grained sandstone and phylitic siltstone, and interlayered metamorphosed muddy siltstone and fine-grained sandstone with brachiopods, corals, and trilobites. Total thickness ranges up to 4,370 m. Basin unconformably overlies the Argunsky metamorphic terrane. -
Geotectonic Setting of the Tertiary Uyandina and Indigirka-Zyryanka Basins, Republic Sakha (Yakutia), Northeast Russia, Using Coal Rank Data
Stephan Mueller Spec. Publ. Ser., 4, 85–96, 2009 www.stephan-mueller-spec-publ-ser.net/4/85/2009/ Special © Author(s) 2009. This work is distributed under Publication the Creative Commons Attribution 3.0 License. Series Geotectonic setting of the Tertiary Uyandina and Indigirka-Zyryanka basins, Republic Sakha (Yakutia), Northeast Russia, using coal rank data H.-J. Paech Federal Institute for Geosciences and Natural Resources, Hannover, Germany now retired Abstract. Outcrops along the Inach River in the Uyandina of these studies was to determine whether Tertiary struc- basin and those along the Myatis’ River in the Indigirka- tures previously described by such authors as Imaev and Gri- Zyryanka basin were studied in detail and sampled for coal nenko (1989), Imaev et al. (1990, 1994, 1998) and Smetan- rank determinations. The Uyandina basin is an intramon- nikova et al. (1989) within the Circum-Arctic region of the tane pull-apart basin characterized by extensional structures Asian Continent are compressional or extensional in origin. within the Moma rift system. The coal rank is below 0.3% Preliminary results of the CASE-3 expedition are given in vitrinite reflectance (Rr ), which indicates shallow, imma- Paech et al. (1998). This contribution provides more detailed ture conditions of basin formation and very low subsidence. field observations and improved coal rank determinations. The Myatis’ River coal-bearing outcrops in the Indigirka- Zyryanka basin reveal compression induced by continent col- lision. The compressive deformation includes also lower- most Pliocene strata. Due to the position in the Verkhoyansk- 2 Study methods Chersky fold belt adjacent to the Kolyma-Omolon microcon- tinent the Indigirka-Zyryanka basin has much in common Logistic restrictions limited our investigations to a few areas: with a foredeep, i.e. -
Inventory and Distribution of Rock Glaciers in Northeastern Yakutia
land Article Inventory and Distribution of Rock Glaciers in Northeastern Yakutia Vasylii Lytkin Melnikov Permafrost Institute, Siberian Branch of the Russian Academy of Sciences, Yakutsk 677010, Russia; [email protected] Received: 2 September 2020; Accepted: 8 October 2020; Published: 10 October 2020 Abstract: Rock glaciers are common forms of relief of the periglacial belt of many mountain structures in the world. They are potential sources of water in arid and semi-arid regions, and therefore their analysis is important in assessing water reserves. Mountain structures in the north-east of Yakutia have optimal conditions for the formation of rock glaciers, but they have not yet been studied in this regard. In this article, for the first time, we present a detailed list of rock glaciers in this region. Based on geoinformation mapping using remote sensing data and field studies within the Chersky, Verkhoyansk, Momsky and Suntar-Khayata ranges, 4503 rock glaciers with a total area of 224.6 km2 were discovered. They are located within absolute altitudes, from 503 to 2496 m. Their average minimum altitude was at 1456 m above sea level, and the maximum at 1527 m. Most of these formations are located on the sides of the trough valleys, and form extended sloping types of rock glaciers. An assessment of the exposure of the slopes where the rock glaciers are located showed that most of the rock glaciers are facing north and south. Keywords: rock glacier; permafrost; inventory; northeastern Yakutia; remote sensing 1. Introduction The geography of distribution of rock glaciers is quite extensive. They are found in many mountainous regions of Europe, North and South America and Asia, including some circumpolar regions [1–18]. -
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. -
Mountain Glaciers of NE Asia in the Near Future: a Projection Based on Climate-Glacier Systems’ Interaction M
Mountain glaciers of NE Asia in the near future: a projection based on climate-glacier systems’ interaction M. D. Ananicheva, A. N. Krenke, E. Hanna To cite this version: M. D. Ananicheva, A. N. Krenke, E. Hanna. Mountain glaciers of NE Asia in the near future: a projection based on climate-glacier systems’ interaction. The Cryosphere Discussions, Copernicus, 2008, 2 (1), pp.1-21. hal-00298533 HAL Id: hal-00298533 https://hal.archives-ouvertes.fr/hal-00298533 Submitted on 7 Jan 2008 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. The Cryosphere Discuss., 2, 1–21, 2008 The Cryosphere www.the-cryosphere-discuss.net/2/1/2008/ Discussions TCD © Author(s) 2008. This work is licensed 2, 1–21, 2008 under a Creative Commons License. The Cryosphere Discussions is the access reviewed discussion forum of The Cryosphere Mountain glaciers of NE Asia M. D. Ananicheva et al. Title Page Mountain glaciers of NE Asia in the near Abstract Introduction future: a projection based on Conclusions References climate-glacier systems’ interaction Tables Figures ◭ ◮ M. D. Ananicheva1, A. N. Krenke1, and E. Hanna2 ◭ ◮ 1Institute of Geography, Russian Academy of Sciences, Moscow, Russia 2Department of Geography, University of Sheffield, UK Back Close Received: 22 November 2007 – Accepted: 26 November 2007 – Published: 7 January 2008 Full Screen / Esc Correspondence to: E. -
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, -
Geodynamic Emplacement Setting of Late Jurassic Dikes of the Yana–Kolyma Gold Belt, NE Folded Framing of the Siberian Craton
minerals Article Geodynamic Emplacement Setting of Late Jurassic Dikes of the Yana–Kolyma Gold Belt, NE Folded Framing of the Siberian Craton: Geochemical, Petrologic, and U–Pb Zircon Data Valery Yu. Fridovsky 1,*, Kyunney Yu. Yakovleva 1, Antonina E. Vernikovskaya 1,2,3, Valery A. Vernikovsky 2,3 , Nikolay Yu. Matushkin 2,3 , Pavel I. Kadilnikov 2,3 and Nickolay V. Rodionov 1,4 1 Diamond and Precious Metal Geology Institute, Siberian Branch, Russian Academy of Sciences, 677000 Yakutsk, Russia; [email protected] (K.Y.Y.); [email protected] (A.E.V.); [email protected] (N.V.R.) 2 A.A. Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch, Russian Academy of Sciences, 630090 Novosibirsk, Russia; [email protected] (V.A.V.); [email protected] (N.Y.M.); [email protected] (P.I.K.) 3 Department of Geology and Geophysics, Novosibirsk State University, 630090 Novosibirsk, Russia 4 A.P. Karpinsky Russian Geological Research Institute, 199106 St. Petersburg, Russia * Correspondence: [email protected]; Tel.: +7-4112-33-58-72 Received: 30 September 2020; Accepted: 8 November 2020; Published: 11 November 2020 Abstract: We present the results of geostructural, mineralogic–petrographic, geochemical, and U–Pb geochronological investigations of mafic, intermediate, and felsic igneous rocks from dikes in the Yana–Kolyma gold belt of the Verkhoyansk–Kolyma folded area (northeastern Asia). The dikes of the Vyun deposit and the Shumniy occurrence intruding Mesozoic terrigenous rocks of the Kular–Nera and Polousniy–Debin terranes were examined in detail. The dikes had diverse mineralogical and petrographic compositions including trachybasalts, andesites, trachyandesites, dacites, and granodiorites. -
Mapping Siberian Arctic Mountain Permafrost
Mapping Siberian Arctic Mountain Permafrost Landscapes by Machine Learning Multi-Sensors Remote Sensing: Example of Adycha River Valley Moisei Zakharov, Sébastien Gadal, Yuri Danilov, Jūratė Kamičaitytė To cite this version: Moisei Zakharov, Sébastien Gadal, Yuri Danilov, Jūratė Kamičaitytė. Mapping Siberian Arctic Moun- tain Permafrost Landscapes by Machine Learning Multi-Sensors Remote Sensing: Example of Adycha River Valley. 7th International Conference on Geographical Information Systems Theory, Applica- tions and Management (GISTAM 2021), INSTICC, Apr 2021, Online streaming, Czech Republic. pp.125-133. hal-03207301 HAL Id: hal-03207301 https://hal.archives-ouvertes.fr/hal-03207301 Submitted on 24 Apr 2021 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Distributed under a Creative Commons Attribution - NonCommercial - NoDerivatives| 4.0 International License Mapping Siberian Arctic Mountain Permafrost Landscapes by Machine Learning Multi-Sensors Remote Sensing: Example of Adycha River Valley Moisei Zakharov1,2 a, Sébastien Gadal1,2 b Yuri Danilov2 c and Jūratė Kamičaitytė3 d 1Aix-Marseille Univ., CNRS, ESPACE UMR 7300, Univ., Nice Sophia Antipolis, Avignon Univ., 13545 Aix-en-Provence, France 2North-Eastern Federal University, 670000 Yakutsk, Republic of Sakha, Russian Federation, 3 Kaunas University of Technology, Kaunas, Lithuania [email protected], [email protected], [email protected], [email protected] Keywords: Permafrost landscape, remote sensing modeling, landscape mapping, terrain, Landsat, ASTER GDEM, Yakutia. -
Article Processing Charges for This Open-Access Ice Complex
Clim. Past, 15, 1443–1461, 2019 https://doi.org/10.5194/cp-15-1443-2019 © Author(s) 2019. This work is distributed under the Creative Commons Attribution 4.0 License. Past climate and continentality inferred from ice wedges at Batagay megaslump in the Northern Hemisphere’s most continental region, Yana Highlands, interior Yakutia Thomas Opel1,2, Julian B. Murton1, Sebastian Wetterich2, Hanno Meyer2, Kseniia Ashastina3, Frank Günther4,5,2, Hendrik Grotheer6, Gesine Mollenhauer6, Petr P. Danilov7, Vasily Boeskorov7, Grigoriy N. Savvinov7, and Lutz Schirrmeister2 1Permafrost Laboratory, Department of Geography, University of Sussex, Brighton, BN1 9RH, UK 2Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Telegrafenberg A45, 14473 Potsdam, Germany 3Senckenberg Research Institute and Natural History Museum, Research Station of Quaternary Palaeontology, 99423 Weimar, Germany 4Institute of Geosciences, University of Potsdam, Karl-Liebknecht-Str. 24–25, 14476 Potsdam, Germany 5Laboratory Geoecology of the North, Faculty of Geography, Lomonosov Moscow State University, Leninskie Gory 1, Moscow 119991, Russia 6Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Am Handelshafen 12, 27570 Bremerhaven, Germany 7Science Research Institute of Applied Ecology of the North, North-East Federal University, 43 Lenin Avenue, Yakutsk 677007, Russia Correspondence: Thomas Opel ([email protected], [email protected]) Received: 23 October 2018 – Discussion started: 30 October 2018 Revised: 1 July 2019 – Accepted: 9 July 2019 – Published: 2 August 2019 Abstract. Ice wedges in the Yana Highlands of interior (mean δ18O about −33 ‰) and of the MIS 3–2 upper sand Yakutia – the most continental region of the Northern Hemi- unit (mean δ18O from about −33 ‰ to −30 ‰) are less dis- sphere – were investigated to elucidate changes in winter cli- tinctive regionally. -
Moss Flora of the Yana-Adycha Plateau (North-East Yakutia) Флора Мхов Яно-Адычанского Плоскогорья (Северо-Восточная Якутия) V.G
Arctoa (2010) 19: 175-182 MOSS FLORA OF THE YANA-ADYCHA PLATEAU (NORTH-EAST YAKUTIA) ФЛОРА МХОВ ЯНО-АДЫЧАНСКОГО ПЛОСКОГОРЬЯ (СЕВЕРО-ВОСТОЧНАЯ ЯКУТИЯ) V.G. ISAKOVA1 В.Г. ИСАКОВА1 Abstract An annotated list of mosses of the Yana-Adycha Plateau (north-east Yakutia) is presented, including 173 species and 3 varieties of mosses from 83 genera and 34 families. The flora includes many rare xerophytic shecies: Hilpertia velenovskyi, Pterygoneurum kozlovii, Syntrichia caninervis, Fabronia ciliaris, Coscinodon cribrosus, C. hartzii. Orthotrichum сupulatum is a new addition to Yakutian flora. Резюме Представленный аннотированный список мхов Яно-Адычанского плос- когорья (Северо-Восточная Якутия) насчитывает 173 вида и 3 разновидности из 83 родов и 34 семейств. Среди них много редких ксерофитов: Hilpertia velenovskyi, Pterygoneurum kozlovii, Syntrichia caninervis, Fabronia ciliaris, Coscinodon cribrosus, C. hartzii. Orthotrichum сupulatum приводится впервые для Якутии. KEYWORDS: mosses, North-east Yakutia, the Yana-Adycha Plateau This paper provides data for the Yana River is +3°С (at nights –2°С, at daytime +8°С), while region, one of the least explored in Yakutia which tmin = –25°С and tmax = +27°С. is itself poorly studied for bryophytes. The study According to the geobotanical classification, area is situated within the Yana-Adycha Plateau the region belongs to the northern taiga subzone (Fig. 1) with relatively low (400-600 m) to medi- (Andreev et al., 1987; Kuznetsova, 2005). um-high (up to 1726 m) elevations. The moun- The dominant tree in the Yana-Adycha Pla- tains in the studied region are generally flat with teau is Larix cajanderi Mayr. Larch forests reach some peaks with steep slopes. -
Large Mammals of the Anthropogene of Yakutia
Large Mammals of the Anthropogene of Yakutia Peter A. Lazarev Large mammals (phylogeny, taxonomy, paleoecology, faunal complexes, taphonomy, remains) Anthropogene Yakutia 03.00.08 Zoology ABSTRACT Dissertation for the Degree of Doctor of Biological Sciences, Yakutsk 2005 Work performed at the Institute of Applied Ecology of the North Academy of Sciences of the Republic of Sakha (Yakutia) Scientific consultant: Sc.D., Professor N.K.Vereshchagin Officials: Member of RAS, Doctor of Biology, Professor N.G. Solomonov, Sc.D. M.A.Erbaeva, Sc.D. Y.N .Litvinov Lead organization: Zoological Institute Defense of the thesis will be held in May 2005, at a meeting of the Dissertation Council D 003,033 01.po award of the Degree of Doctor of Science at the Institute of Systematics and Ecology of Animals at: 630091, Russia, Novosibirsk, ul. Frunze 11. , For further reviews of author's information, please contact: 630091, Russia, Novosibirsk, ul. Frunze 11 The thesis can be found in the library of the Institute of Systematics and Ecology of Animals Autoabstract sent in March 2005 Scientific Secretary of the Dissertation Council Sc.D., Professor C / A.Yu.Haritonov Introduction GENERAL DESCRIPTION OF WORK Relevance of the topic: High abundance and diversity of anthropogenic mammals and the large number of localities of remains imply most promising research possibilities for cryozoological paleotheriology are in North Asia. In the permafrost the unique burial of corpses and skeletons of extinct animals have safely survived the mass extinction of animals in general and the excavation and study of such findings lead to the understanding of the causes of their death and burial taphonomic features.