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  • 2010-2014  (99,645)
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  • 1
    Call number: AWI G6-22-94848
    Description / Table of Contents: Появившиеся в последние десятилетия новые данные (множественные радиометрические определения возраста памятников, в том числе их ряды, для памятников голоценового каменного века Северо-Восточной Азии), а также новые геоархеологические объекты (например, палеолитическая Янская стоянка - самый северный памятник раннего верхнего палеолита мира), позволяют обратиться к рассмотрению проблем хронометрии последовательностей культурноисторического развития Северо-Востока Азии в позднем неоплейстоцене и голоцене, в эпохи, предшествовавшие формированию современной этнической карты этих территорий. Наибольшее внимание в предлагаемой работе уделено проблемам радиоуглеродной хронологии и хроностратиграфии памятников верхнего палеолита, документирующих на настоящий момент древнейшие достоверные этапы расселения человека на Северо-Востоке Азии. Для археологов, специалистов в области четвертичной геологии, геоморфологов, палеогеографов.
    Type of Medium: Monograph available for loan
    Pages: 263 Seiten , Illustrationen , 25 cm
    ISBN: 9785020255203
    Language: Russian
    Note: CONTENTS Preface lnroduction Chapter I. Radiocarbon chronology and chronostratigraphy of the Paleolith of NE Asia: Statement of a Question Chapter II. Paleolithic sites of the Aidan River Valley Features of geology and geomorphology of Aldan valley Age and validity of archaeological sites in Aldan valley "Tectonic hypothesis" Chronostratigraphy of the Late Pleistocene and Holocene sites in Aldan valley Chapter III. Archaeological sites of the Yana-Indighirka Lowland The Yana site It's discovery and history of research General description of the site area Deposits of the second terrace of Yana River and position of the cultural layer of the Yana site Radiocarbon age of the cultura layer Archaeological finds Fauna remains The Berelekh site History of research Geological profile and radiocarbon chronology of Berelekh geocomplex Archaeological component of Berelekh geocomplex Fauna remains Chapter IV. Radiocarbon dated Paleolithic site of NE Asia beyond the Aidan valley and Coastal (Yana-Kolyma) lowland Geoarchaeological objects of Upper and Middle Lena River Archaeological sites of Kolyma River basin and Sea of Okhotsk and Kolyma River watershed Ushki sites in Kamchatka Peninsula Concluding remarks for the Fourth Chapter Chapter V. Basic elements of radiocarbon chronology of the Holocene Stone Age of NE Asia Chapter VI. Radiocarbon chronology, archaeological periodization and peculiarities of cultural development of the Late Pleistocene and Holocene of NE Asia Conclusions Summary References List of abbreviations Radiocarbon laboratory's codes List of illustrations List of tables Appendices Table 1. Radiocarbon dates of archaeological site of NE Asia Table 8. A synopsis for geomorphology of 14C dated Late Pleistocene and Early Holocene archaeological sites of NE Asia , СОДЕРЖАНИЕ Предисловие Введение Глава I. Радиоуглеродная хронология и хроностратиrрафия палеолита Северо- Востока Азии: постановка проблемы Глава II. Памятники палеолита в долине р. Алдан Особенности строения долины р. Алдан Возраст и валидность археологических памятников Алдана «Тектоническая гипотеза» Хроностратиграфия памятников позднего неоплейстоцена и голоцена Алдана Глава III. Памятники Яно-Индиrирской низменности Янская стоянка История открытия и изучения Общая характеристика района стоянки Отложения разреза второй надпойменной террасы р. Яны и положение культурного слоя Янской стоянки Радиоуглеродный возраст культурного слоя Археологическая составляющая Фаунистическая характеристика Стоянка Берелёх История изучения Характеристика разреза и хронология Берелёхского комплекса Археологическая составляющая Берелёхского комплекса Комплекс фаунистических находок Глава IV. Датированные памятники палеолита Северо-Восточной Азии вне пределов долины Алдана и Приморской (Я но-Колымской) низменности Геоархеологические объекты Верхней и Средней Лены Памятники Колымской системы и Охотска-Колымского водораздела Комплекс Ушковских стоянок (Камчатский полуостров) Заключительные замечания к разделу Глава V. Основные черты радиоуглеродной хронологии rолоценовых памятников каменноrо века Северо-Восточной Азии Глава VI. Радиоуглеродная хронология, археологическая периодизация и особенности культурно-исторических процессов позднего неоплейстоцена и rолоцена Северо-Восточной Азии Заключение Summary Литература Список сокращений Список иллюстраций Список табличного материала Список индексов лабораторий, проводящих радиоуглеродное датирование Приложения Таблица 1. Список радиоуглеродных дат археологических объектов Северо-Востока Азии Таблица 8. Краткий конспект геоморфологического положения датированных поздненеоплейстоценовых и раннеrолоценовых археологических памятников Северо-Востока Азии , Zusammenfassung in englischer Sprache , In kyrillischer Schrift
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  • 2
    Description / Table of Contents: The Oman Mountains contain one of the world's best- exposed and best-understood fold–thrust belts and the largest, best-exposed and most intensively studied ophiolite complex on Earth. This volume presents new international research from authors currently active in the field focusing on the geology of the Oman Mountains, the foreland region, the carbonate platforms of Northern and Central Oman and the underlying basement complex. In addition there is a particular focus on geoconservation in the region. The volume is divided into three main sections that discuss the tectonics of the Arabian plate using insights from geophysics, petrology, structural geology, geochronology and palaeontology; the petrology and geochemistry of the Oman Ophiolite and the sedimentary and hydrocarbon systems of Oman, drawing on the geophysics, structure and sedimentology of these systems. The volume is enhanced by numerous colour images provided courtesy of Petroleum Development Oman.
    Pages: Online-Ressource (VII, 471 Seiten)
    ISBN: 9781862393783
    Language: English
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  • 3
    Call number: S 90.0002(1727)
    In: Professional paper
    Type of Medium: Series available for loan
    Pages: VIII, 115 S. : Ill., graph. Darst. + 4 Kt.-Beil.
    ISBN: 9781411323681
    Series Statement: U.S. Geological Survey professional paper 1727
    Classification:
    Historical Geology
    Location: Lower compact magazine
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  • 4
    Call number: MOP 19538/1d-6d
    Type of Medium: Monograph available for loan
    Pages: 111 S.
    ISSN: 0486-2287
    Language: Russian
    Note: In kyrill. Schr.
    Location: MOP - must be ordered
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  • 5
    Call number: AWI G3-19-92416
    Description / Table of Contents: The book contains proceedings of the Second International School on paleopedology for young scholars «Paleosoils as a source of information about past environments». Abstracts of main lectures, description of region where the School was carried out and papers of young scientists are published in the book. Proceedings of the School are of interest for researchers of soil science, paleogeography, Quaternary geology and ecology.
    Type of Medium: Monograph available for loan
    Pages: 145 Seiten , Illustrationen
    ISBN: 978-5-8406-0430-4
    Language: Russian , English
    Note: CONTENT Preface / M. Dergacheva, A. Makeev Description of study area and paleosol / M. Dergacheva, N. Mironycheva-Tokareva, S. Ponomarev, D. Gavrilov LECTURES Essentials of the paleopedology and a review of Quaternary paleosols of the Northern Hemisphere: main items, presented in the lectures / A. Makeev Paleosols in geologic history of the Earth / A. Makeev Possibilites and limits of pedohumus method used at investigations types and environment of ancient pedogenesis / M. Dergacheva Classification system of paleosols / I. Fedeneva Indicating function of pedogenic carbonates in paleoclimatic reconstruction of Holocene and Pleistocene / O. Khokhlova Miromorphological capacities for reseaching of palaeosoils / M. Lebedeva (Verba) Three-dimensional morphology of soil / A. V. Zakharchenko Paleomagnetic method for studing Pliocene and Quaternary deposits of Siberia (current status, problems, prospects) / Z. N. Gnibidenko Specific chemical state anthropogenic transformed soil of the ancient settlements / O. Yakimenko Geochemical peculiarities of soils as an indicator of specific of their formation and anthropogenic transformation / L. Rikhvanov REPORTS Problem of paleosols weed / A. Blagodatnova Spatial distribution of mobile phosphates in Kamennyi Ambar settlement (Chelyabinsk region) / K. Bojtsova Review of literature data for the study of humus horizon chernozem rate formation / E. Burnatova Pedogenic features in paleosols of Samara Volga region archaeological sites / D. Vassilieva Paleosols of Early Iron Age double kurgan of burial ground Kuigenzhar (Northern Kazakhstan) / D. Gavrilov, R. Ishmuratov, A. Toguzbaev Salt soils of Central-Tuva depression / Ch. Danchai-ool Humus composition of Zaural' e forest-steppe and steppe zones on example of archaeological sites / T. Zhdanova Properties variation of the upper part of the modern soils and surface paleosols of key site Volodarka (Barnaul Priobye) / H. Zhaharova Chernozems morphological properties of key area «Volodarka» / O. Kazachenok Comparative characteristics of the modern turf-podzolic soil and the soil buried under centenary dump (Sysert' District, Middle Urals) / L. Kirilyuk Paleopedology: objects and article of researches (review of publications in a «Soil Science» magazine for 2008-2010) / M. Komarova Soils with a buried humus horizon / B. Mongush Paleogeography formation conditions of Tuva sandy landscapes / Ch. Mongush, S. Kurbatskaya The comparative characteristic of 700-year-old and background soil near Sovetskiy city (middle taiga) / O. Nekrasova Humus soil memory: the conditions and time limits for the conservation of steppe / A. Nikiforov Study Holocene evolution of Central Tuva soil and soil formation / K. Ochur Estimation of restoration rate of damaged soils (on materials of studying archaeological objects of the foreststeppe zone) / E. Politova, V. Valdayskih Some polygenetic chernozem characteristics of the Ob Plateau Eastern edge (for example, the key area "Volodarka") / S. Ponomarev Vertical zonality soils in the Sayan mountains in Tuva / V. Sanchaiban Soil physical properties as a soil memory flash / E. Surkova Peculiarities of soddy-alluvial soil of the river Sysert' water-meadow (The Middle Urals) / A. Uchaev Aqueous extract composition of anthropogenically disturbed soils of Kamennyi Am bar settlement / D. Filimonova Environmental conditions of steppe soils for example near the village of Volodarka / H. Cherepanova New investigations at Tokaj-Csorgukut II. Loess section, Northeast Hungary / D. G. Páll, G. Persaits, P. Sümegi P Preliminary results on the phytoliths of the dutch neolithic site Swifterbant as seen from samples retrieved from soils, pig droppings and molars / G. Persaits, D. C. M. Raemaekers , In kyrillischer Schrift , Beiträge teilweise in englischer, teilweise in russischer Sprache
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  • 6
    Monograph available for loan
    Monograph available for loan
    New York, NY [u.a.] : Norton
    Call number: PIK B 160-21-94413
    Type of Medium: Monograph available for loan
    Pages: XIV, 306 S. , graph. Darst.
    Edition: 3. ed.
    ISBN: 9780393919172 (hardcover)
    Language: English
    Note: Preface -- Introduction : the facts of economic growth -- The Solow model -- Empirical applications of neoclassical growth models -- The economics of ideas -- The engine of growth -- A simple model of growth and development -- Social infrastructure and long-run economic performance -- Population and the origin of sustained economic growth -- Alternative theories of endogenous growth -- Natural resources and economic growth -- Understanding economic growth -- Appendix A: Mathematical review -- Appendix B: Readings of interest -- Appendix C: Data on economic growth -- Bibliography -- Index..
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  • 7
    Call number: IASS 11.0018
    In: Interdisziplinäre Stoffstromforschung
    Type of Medium: Monograph available for loan
    Pages: 288 S. : graph. Darst
    ISBN: 9783895188244
    Series Statement: Interdisziplinäre Stoffstromforschung
    Branch Library: IASS
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  • 8
    Series available for loan
    Series available for loan
    Stuttgart : Schweizerbart
    Associated volumes
    Call number: S 00.0063(75)
    In: Stratigraphie von Deutschland
    In: Schriftenreihe der Deutschen Gesellschaft für Geowissenschaften
    Type of Medium: Series available for loan
    Pages: 461 S.
    ISBN: 9783510492237
    Series Statement: Schriftenreihe der Deutschen Gesellschaft für Geowissenschaften 75
    Classification:
    Stratigraphy
    Location: Lower compact magazine
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  • 9
    Monograph available for loan
    Monograph available for loan
    London : Hodder Education
    Call number: AWI G7-11-0061
    Description / Table of Contents: Glaciers & Glaciation is the classic textbook for all students of glaciation. Stimulating and accessible, it has established a reputation as a comprehensive and essential resource. In this new edition, the text, references and illustrations have been thoroughly updated to provide a state-of-the-art overview of the nature, origin and behaviour of glaciers and the geological and geomorphological evidence for their past history on earth. The first part of the book investigates the processes involved in forming glacier ice, the natureof glacier-climate relationships, the mechanisms of glacier flow and the interactions of glaciers with other natural systems such as rivers, lakes and oceans. In the second part, the emphasis moves to landforms and sediment, the interpretation of the earth's glacial legacy and the reconstruction of glacial depositional environments and palaeoglaciology.
    Type of Medium: Monograph available for loan
    Pages: XIV, 802 Seiten , Illustrationen
    Edition: Second edition
    ISBN: 9780340905791
    Language: English
    Note: CONTENTS PREFACE PREFACE TO THE SECOND EDITION ACKNOWLEDGEMENTS PART ONE GLACIERS 1 INTRODUCTION 1.1 Glacier systems 1.1.1 Mass balance 1.1.2 Meltwater 1.1.3 Glacier motion 1.1.4 Glaciers and sea-level change 1.1.5 Erosion and debris transport 1.1.6 Glacial sediments, landforms and landscapes 1.2 Glacier morphology 1.2.1 Ice sheets and ice caps 1.2.2 Glaciers constrained by topography 1.2.3 Ice shelves 1.3 Present distribution of glaciers 1.3.1 Influence of latitude and altitude 1.3.2 Influence of aspect, relief and distance from a moisture source 1.4 Past distribution of glaciers 1.4.1 'Icehouse' and 'greenhouse' worlds 1.4.2 Cenozoic glaciation 2 SNOW, ICE AND CLIMATE 2.1 Introduction 2.2 Surface energy balance 2.2.1 Changes of state and temperature 2.2.2 Shortwave radiation 2.2.3 Longwave radiation 2.2.4 Sensible and latent heat: turbulent fluxes 2.2.5 Energy supplied by rain 2.2.6 Why is glacier ice blue? 2.3 Ice temperature 2.3.1 The melting point of ice 2.3.2 Controls on ice temperature 2.3.3 Thermal structure of glaciers and ice sheets 2.4 Processes of accumulation and ablation 2.4.1 Snow and ice accumulation 2.4.2 Transformation of snow to ice 2.4.3 Melting of snow and ice 2.4.4 Sublimation and evaporation 2.4.5 The influence of debris cover 2.5 Mass balance 2.5.1 Definitions 2.5.2 Measurement of mass balance 2.5.3 Annual mass balance cycles 2.5.4 Mass balance gradients 2.5.5 The equilibrium line 2.5.6 Glaciation levels or glaciation thresholds 2.5.7 Glacier sensitivity to climate change 2.6 Glacier-climate interactions 2.6.1 Effects of glaciers and ice sheets on the atmosphere 2.7 Ice cores 2.7.1 Ice coring programmes 2.7.2 Stable isotopes 2.7.3 Ancient atmospheres: the gas content of glacier ice 2.7.4 Solutes and particulates 3 GLACIER HYDROLOGY 3.1 Introduction 3.2 Basic concepts 3.2.1 Water sources and routing 3.2.2 Hydraulic potential 3.2.3 Resistance to flow 3.2.4 Channel wall processes: melting, freezing and ice deformation 3.3 Supraglacial and englacial drainage 3.3.1 Supraglacial water storage and drainage 3.3.2 Englacial drainage 3.4 Subglacial drainage 3.4.1 Subglacial channels 3.4.2 Water films 3.4.3 Linked cavity systems 3.4.4 Groundwater flow 3.4.5 Water at the ice-sediment interface 3.5 Glacial hydrological systems 3.5.1 Temperate glaciers 3.5.2 Polythermal glaciers 3.5.3 Modelling glacial hydrological systems 3.6 Proglacial runoff 3.6.1 Seasonal and shorter-term cycles 3.6.2 Runoff and climate change 3.7 Glacial lakes and outburst floods 3.7.1 Introduction 3.7.2 Moraine-dammed lakes 3.7.3 Ice-dammed lakes 3.7.4 Icelandic subglacial lakes 3.7.5 Estimating GLOF magnitudes 3.8 Life in glaciers 3.8.1 Supraglacial ecosystems 3.8.2 Subglacial ecosystems 3.9 Glacier hydrochemistry 3.9.1 Overview 3.9.2 Snow chemistry 3.9.3 Chemical weathering processes 3.9.4 Subglacial chemical weathering 3.9.5 Proglacial environments 3.9.6 Rates of chemical erosion 4 PROCESSES OF GLACIER MOTION 4.1 Introduction 4.2 Stress and strain 4.2.1 Stress 4.2.2 Strain 4.2.3 Rheology: stress-strain relationships 4.2.4 Force balance in glaciers 4.3 Deformation of ice 4.3.1 Glen's Flow Law 4.3.2 Crystal fabric, impurities and water content 4.3.3 Ice creep velocities 4.4 Sliding 4.4.1 Frozen beds 4.4.2 Sliding of wet-based ice 4.4.3 Glacier-bed friction 4.4.4 The role of water 4.5 Deformable beds 4.5.1 The Boulton-Hindmarsh model 4.5.2 Laboratory testing of subglacial tills 4.5.3 Direct observations of deformable glacier beds 4.5.4 Rheology of subglacial till 4.6 Rates of basal motion 4.6.1 'Sliding laws' 4.6.2 Local and non-local controls on ice velocity 4.7 Crevasses and other structures: strain made visible 4.7.1 Crevasses 4.7.2 Crevasse patterns 4.7.3 Layering, foliation and related structures 5 GLACIER DYNAMICS 5.1 Introduction 5.2 Understanding glacier dynamics 5.2.1 Balance velocities 5.2.2 Deviations from the balance velocity 5.2.3 Changes in ice thickness: continuity 5.2.4 Thermodynamics 5.3 Glacier models 5.3.1 Overview 5.3.2 Equilibrium glacier profiles 5.3.3 Time-evolving glacier models 5.4 Dynamics of valley glaciers 5.4.1 Intra-annual velocity variations 5.4.2 Multi-annual variations 5.5 Calving glaciers 5.5.1 Flow of calving glaciers 5.5.2 Calving processes 5.5.3 'Calving laws' 5.5.4 Advance and retreat of calving glaciers 5.6 Ice shelves 5.6.1 Mass balance of k e shelves 5.6.2 Flow of ice shelves 5.6.3 Ice shelf break-up 5.7 Glacier surges 5.7.1 Overview 5.7.2 Distribution of surging glaciers 5.7.3 Temperate glacier surges 5.7.4 Polythermal surging glaciers 5.7.5 Surge mechanisms 6 THE GREENLAND AND ANTARCTIC ICE SHEETS 6.1 Introduction 6.2 The Greenland Ice Sheet 6.2.1 Overview 6.2.2 Climate and surface mass balance 6.2.3 Ice sheet flow 6.2.4 Ice streams and outlet glaciers 6.3 The Antarctic Ice Sheet 6.3.1 Overview 6.3.2 Climate and mass balance 6.3.3 Flow of inland ice 6.3.4 Ice streams 6.3.5 Hydrology and subglacial lakes 6.3.6 Ice stream stagnation and reactivation 6.3.7 Stability of the West Antarctic Ice Sheet 7 GLACIERS AND SEA LEVEL CHANGE 7.1 Introduction 7.2 Causes of sea-level change 7.2.1 Overview 7.2.2 Glacio-eustasy and global ice volume 7.2.3 Glacio-isostasy and ice sheet loading 7.3 Sea-level change over glacial-interglacial cycles 7.3.1 Ice sheet fluctuations and eustatic sea-level change 7.3.2 Sea-level histories in glaciated regions 7.4 Glaciers and recent sea-level change 7.4.1 Recorded sea-level change 7.4.2 Global glacier mass balance 7.5 Future sea-level change 7.5.1 IPCC climate and sea-level projections 7.5.2 Predicting the glacial contribution to sea-level change PART TWO GLACIATION 8 EROSIONAL PROCESSES, FORMS AND LANDSCAPES 8.1 Introduction 8.2 Subglacial erosion 8.2.1 Rock fracture: general principles 8.2.2 Abrasion 8.2,3 Quarrying 8.2.4 Erosion beneath cold ice 8.2.5 Erosion of soft beds 8.3 Small-scale erosional forms 8.3.1 Striae and polished surfaces 8.3.2 Rat tails 8.3.3 Chattermarks, gouges and fractures 8.3.4 P-forms 8.4 Intermediate-scale erosional forms 8.4.1 Roches moutonnees 8.4.2 Whalebacks and rock drumlins 8.4.3 Crag and tails 8.4.4 Channels 8.5 Large-scale erosional landforms 8.5.1 Rock basins and overdeepenings 8.5.2 Basins and overdeepenings in soft sediments 8.5.3 Troughs and fjords 8.5.4 Cirques 8.5.5 Strandflats 8.6 Landscapes of glacial erosion 8.6.1 Areal scouring 8.6.2 Selective linear erosion 8.6.3 Landscapes of little or no glacial erosion 8.6.4 Alpine landscapes 8.6.5 Cirque landscapes 8.6.6 Continent-scale patterns of erosion 9 DEBRIS ENTRAPMENT AND TRANSPORT 9.1 Introduction 9.2 Approaches to the study of glacial sediments 9.2.1 The glacial debris cascade 9.2.2 Spatial hierarchies of sediments and landforms 9.3 Glacial debris entrainment 9.3.1 Supraglacial debris entrainment 9.3.2 Incorporation of debris into basal ice 9.4 Debris transport and release 9.4.1 Subglacial transport 9.4.2 High-level debris transport 9.4.3 Glacifluvial transport 9.5 Effects of transport on debris 9.5.1 Granulometry 9.5.2 Clast morphology 9.5.3 Particle micromorphology 10 GLACIGENIC SEDIMENTS AND DEPOSITIONAL PROCESSES 10.1 Introduction 10.2 Sediment description and classification 10.2.1 Sediment description 10.2.2 Deformation structures 10.2.3 Primary and secondary deposits 10.3 Primary glacigenic deposits (till) 10.3.1 Overview 10.3.2 Processes of subglacial till formation 10.3.3 Glacitectonite 10.3.4 Subglacial traction till 10.4 Glacifluvial deposits 10.4.1 Terminology and classification of glacifluvial sediments 10.4.2 Plane bed deposits 10.4.3 Ripple cross-laminated facies 10.4.4 Dunes 10.4.5 Antidunes 10.4.6 Scour and minor channel fills 10.4.7 Gravel sheets 10.4.8 Silt and mud drapes 10.4.9 Hyperconcentrated flow deposits 10.5 Gravitational mass movement deposits and syn-sedimentary deformation structures 10.5.1 Overview 10.5.2 Fall deposits 10.5.3 Slide and slump deposits 10.5.4 Debris (sediment-gravity) flow deposits 10.5.5
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  • 10
    Call number: AWI Bio-11-0074
    Description / Table of Contents: Outside Russia very little is known about the terrestrial ecology, vegetation, biogeographical patterns, and biodiversity of the enormously extensive ecosystems of Yakutia, Siberia. These systems are very special in that they function on top of huge layers of permafrost and are exposed to very severe and extreme weather conditions, the range between winter and summer temperatures being more than 100 degrees C. The soils are generally poor, and human use of the vegetation is usually extensive. Main vegetation zones are taiga and tundra, but Yakutia also supports a special land and vegetation form, caused by permafrost, the alas: more or less extensive grasslands around roundish lakes in taiga. All these vegetation types will be described and their ecology and ecophysiological characteristics will be dealt with. Because of the size of Yakutia, covering several climatic zones, and its extreme position on ecological gradients, Yakutia contains very interesting biogeographical patterns, which also will be described. Our analyses are drawn from many years of research in Yakutia and from a vast body of ecological and other literature in Russian publications and in unpublished local reports. The anthropogenic influence on the ecosystems will be dealt with. This includes the main activities of human interference with nature: forestry, extensive reindeer herding, cattle and horse grazing, etc. Also fire and other prominent ecological factors are dealt with. A very important point is also the very high degree of naturalness that is still extant in Yakutia`s main vegetation zones.
    Type of Medium: Monograph available for loan
    Pages: XV, 390 S. : Ill., graph. Darst., Kt.
    ISBN: 9789048137732
    Series Statement: Plant and vegetation 3
    Note: Contents: 1 Natural conditions. - 2 Flora of Yakutia: composition and ecological structure. - 3 Vegetation of Yakutia: Elements of ecology and plant sociology. - 4 Vegetation and human activity. - 5 Insect impact on vegetation. - 6 Structural and functional pecularities of the plants of Yakutia. - 7 Nature conservation status and its prospects.
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