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  • 1
    Call number: AWI Bio-24-95736
    Description / Table of Contents: Moss-microbe associations are often characterised by syntrophic interactions between the microorganisms and their hosts, but the structure of the microbial consortia and their role in peatland development remain unknown. In order to study microbial communities of dominant peatland mosses, Sphagnum and brown mosses, and the respective environmental drivers, four study sites representing different successional stages of natural northern peatlands were chosen on a large geographical scale: two brown moss-dominated, circumneutral peatlands from the Arctic and two Sphagnum-dominated, acidic peat bogs from subarctic and temperate zones. The family Acetobacteraceae represented the dominant bacterial taxon of Sphagnum mosses from various geographical origins and displayed an integral part of the moss core community. This core community was shared among all investigated bryophytes and consisted of few but highly abundant prokaryotes, of which many appear as endophytes of Sphagnum mosses. Moreover, brown mosses and Sphagnum mosses represent habitats for archaea which were not studied in association with peatland mosses so far. Euryarchaeota that are capable of methane production (methanogens) displayed the majority of the moss-associated archaeal communities. Moss-associated methanogenesis was detected for the first time, but it was mostly negligible under laboratory conditions. Contrarily, substantial moss-associated methane oxidation was measured on both, brown mosses and Sphagnum mosses, supporting that methanotrophic bacteria as part of the moss microbiome may contribute to the reduction of methane emissions from pristine and rewetted peatlands of the northern hemisphere. Among the investigated abiotic and biotic environmental parameters, the peatland type and the host moss taxon were identified to have a major impact on the structure of moss-associated bacterial communities, contrarily to archaeal communities whose structures were similar among the investigated bryophytes. For the first time it was shown that different bog development stages harbour distinct bacterial communities, while at the same time a small core community is shared among all investigated bryophytes independent of geography and peatland type. The present thesis displays the first large-scale, systematic assessment of bacterial and archaeal communities associated both with brown mosses and Sphagnum mosses. It suggests that some host-specific moss taxa have the potential to play a key role in host moss establishment and peatland development.
    Description / Table of Contents: Während die Beziehungen zwischen Moosen und den mit ihnen assoziierten Mikroorganismen oft durch syntrophische Wechselwirkungen charakterisiert sind, ist die Struktur der Moos-assoziierten mikrobiellen Gemeinschaften sowie deren Rolle bei der Entstehung von Mooren weitgehend unbekannt. Die vorliegende Arbeit befasst sich mit mikrobiellen Gemeinschaften, die mit Moosen nördlicher, naturnaher Moore assoziiert sind, sowie mit den Umweltfaktoren, die sie beeinflussen. Entlang eines groß angelegten geographischen Gradienten, der von der Hocharktis bis zur gemäßigten Klimazone reicht, wurden vier naturbelassene Moore als Probenstandorte ausgesucht, die stellvertretend für verschiedene Stadien der Moorentwicklung stehen: zwei Braunmoos-dominierte Niedermoore mit nahezu neutralem pH-Wert sowie zwei Sphagnum-dominierte Torfmoore mit saurem pH-Wert. Die Ergebnisse der vorliegenden Arbeit machen deutlich, dass die zu den Bakterien zählenden Acetobacteraceae das vorherrschende mikrobielle Taxon der Sphagnum-Moose gleich welchen geographischen Ursprungs darstellen und insbesondere innerhalb des Wirtsmoosgewebes dominieren. Gleichzeitig gehörten die Acetobacteraceae zum wesentlichen Bestandteil der mikrobiellen Kerngemeinschaft aller untersuchten Moose, die sich aus einigen wenigen Arten, dafür zahlreich vorkommenden Prokaryoten zusammensetzt. Die vorliegende Arbeit zeigt zudem erstmals, dass sowohl Braunmoose als auch Torfmoose ein Habitat für Archaeen darstellen. Die Mehrheit der Moos-assoziierten Archaeen gehörte dabei zu den methanbildenden Gruppen, wenngleich die metabolischen Aktivitätsraten unter Laborbedingungen meistens kaum messbar waren. Im Gegensatz hierzu konnte die Bakterien-vermittelte Methanoxidation sowohl an Braunmoosen als auch an Sphagnum-Moosen gemessen werden. Dies zeigt eindrucksvoll, dass Moos-assoziierte Bakterien potenziell zur Minderung von Methanemissionen aus nördlichen, aber auch wiedervernässten Mooren beitragen können. Ein weiteres wichtiges Resultat der vorliegenden Arbeit ist die Bedeutung des Moortyps (Niedermoor oder Torfmoor), aber auch der Wirtsmoosart selbst für die Struktur der Moos-assoziierten Bakteriengemeinschaften, während die archaeellen Gemeinschaftsstrukturen weder vom Moortyp noch von der Wirtsmoosart beeinflusst wurden und sich insgesamt deutlich ähnlicher waren als die der Bakterien. Darüber hinaus konnte erstmalig gezeigt werden, dass sich die bakteriellen Gemeinschaften innerhalb der unterschiedlichen Moorsukzessionsstadien zwar ganz erheblich voneinander unterscheiden, ein kleiner Teil der Bakterien dennoch Kerngemeinschaften bilden, die mit allen untersuchten Moosarten assoziiert waren. Bei der hier präsentierten Arbeit handelt es sich um die erste systematische Studie, die sich auf einer großen geographischen Skala mit den bakteriellen und archaeellen Gemeinschaften von Braunmoosen und Torfmoosen aus naturbelassenen nördlichen Mooren befasst. Die vorliegenden Ergebnisse machen deutlich, dass die untersuchten Moose ein ganz spezifisches mikrobielles Konsortium beherbergen, welches mutmaßlich eine Schlüsselrolle bei der Etablierung der Wirtspflanzen am Anfang der Moorentwicklung spielt und darüber hinaus das Potential hat, die charakteristischen Eigenschaften von Mooren sowie deren weitere Entwicklung zu prägen.
    Type of Medium: Dissertations
    Pages: XX, 139, liv Seiten , Illustrationen, Diagramme
    Language: English
    Note: Dissertation, Universität Potsdam, 2024 , Content Preface Acknowledgements Summary Zusammenfassung Abbreviations 1. Introduction 1.1. Peatlands 1.1.1. Peatland development and peat bog succession 1.1.2. Characteristic peatlands of the northern hemisphere 1.1.3. Anthropogenic threats of northern peatlands 1.1.4. Peat bog restoration 1.2. Peatland bryophytes 1.2.1. Brown mosses 1.2.2. Sphagnum mosses 1.3. Moss microbiota 1.3.1. Moss-associated bacteria 1.3.2. Moss-associated archaea 1.3.3. Endophytic prokaryotic communities 1.4. Biotic and abiotic influences on moss-associated microorganisms 1.5. Objectives 1.6. Study sites 1.6.1. High Arctic peatlands of Svalbard (SV) 1.6.2. Polygonal Tundra of Samoylov (SA) 1.6.3. Palsa Bogs of Neiden (NEI) 1.6.4. Kettle Bog Peatlands of Mueritz National Park (MUE) 2. Material and Methods 2.1. Sampling scheme overview 2.2. Sampling of pore water 2.3. Sampling of moss plantlets 2.4. Analysis of pore water chemistry 2.5. Cell wall analysis 2.5.1. Cation exchange capacity (CEC) 2.5.2. Holocellulose (HC) 2.5.3. Lignin and Lignin-like polymers (LLP) 2.5.4. Bulk moss litter analysis 2.6. Moss surface sterilisation and separation of putative epiphytic and endophytic microbial communities 2.7. DNA extraction and sequencing 2.8. Sequence analyses and bioinformatics 2.9. Statistical analyses 2.10. Potential methane production and oxidation assays 2.10.1. Surface sterilisation prior to activity tests 2.10.2. Methane production 2.10.3. Methane oxidation 3. Results 3.1. Peatland bulk and pore water characteristics 3.2. Diversity and structure of natural peatland microbial communities 3.3. Environmental drivers of moss-associated microbial communities 3.4. Microbial taxa associated with brown mosses and Sphagnum mosses 3.4.1. Moss-associated bacteria 3.4.2. Moss-associated archaea 3.4.3. Bacterial and archaeal core communities 3.4.4. Acetobacteraceae as dominant taxon of the bacterial core community 3.5. Sphagnum bacteriomes of disturbed, rewetted and pristine temperate kettle bog 3.6. Potential moss-associated methane production and methane oxidation rates 3.6.1. Moss-associated methane production 3.6.2. Moss-associated methane oxidation 4. Discussion 4.1. Environmental influences on moss-associated bacterial communities 4.2. Moss-associated archaeal communities and their environmental drivers 4.3. Distinct patterns of endophytic bacteria 4.4. The core microbiota and their possible role for peatland succession 4.5. The potential role of Acetobacteraceae for Sphagnum host mosses and bog ecosystems 4.6. Moss-associated microbial communities of the methane cycle and their potential metabolic activity 4.7. Diversity and structure of Sphagnum bacteriomes from pristine, disturbed and rewetted kettle bogs 5. Conclusion 6. Critical remarks and outlook 6.1. Critical remarks 6.2. Outlook Bibliography Supplementary
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  • 2
    Call number: AWI G3-24-95728
    Description / Table of Contents: This atlas is an attempt to translate and consolidate the available knowledge on permafrost. It is a timely book suffused with the compelling enthusiasm of its authors and contributors. Close to a hundred individuals participated in its making, and it does a magnificent job at describing permafrost with maps, words, art, and stories. Far from being an academic product in the traditional sense, it gathers the knowledge from the voices of scientists, Indigenous Peoples, northern residents, and local practitioners to provide a holistic and inclusive view of today’s challenges in the “country of permafrost”.
    Type of Medium: Monograph available for loan
    Pages: 174 Seiten , Illustrationen
    Language: English
    Note: Contents Foreword Prologue Earth’s Freezer: Introduction to Permafrost Frozen grounds: Permafrost in the Arctic Permafrost in profile: Landscape features Frozen in time: The history of permafrost An icy balance: Arctic permafrost physiography What lies within: Organic carbon in permafrost When ice grows up: Pingo Canadian Landmark Drilling down: Learning the secrets of permafrost Portrait: Annett Bartsch Un/settled: Life on frozen ground Frozen States I: Russian Federation Portrait: Vyacheslav Shadrin Frozen States II: North America Portrait: Jessi Pascal Frozen States III: Nordic region Portrait: Palle Jeremiassen Awakening Giant: Permafrost and Climate Change Warming up, warming down: Increasing ground temperatures The chill is gone: Thickening of the active layer Disappearing act: Declining permafrost extent Microorganisms, macro effects: Permafrost carbon cycle Faster, deeper, stronger I: Speed of thaw in North America Faster, deeper, stronger II: Speed of thaw in Scandinavia and the Russian Federation Crossing the threshold: Future scenarios of carbon release Portrait: Dmitry Streletskiy Moving Grounds: Permafrost Changes Frost and flora: The role of vegetation in permafrost landscapes Fire on ice: Peat, permafrost, and fire State of matter: Water, snow, and permafrost The rivers run through it: Arctic rivers, deltas and hydrology Along the edge of the world: Arctic coastal classification Wear and tear: Erosion of Arctic permafrost coasts Eating into the landscape: Retrogressive thaw slumps Portrait: Angus Alunik Losing ground: Projected rates of Arctic coastal erosion Beneath the waves: Changes in subsea permafrost Arctic Ripples: Impacts of Permafrost Thaw Feeling the heat: Permafrost thaw impacts on infrastructure Risky business I: North American Arctic and Kalaallit Nunaat (Greenland) Risky business II: The Russian Federation and Scandinavian Arctic Terra infirma I: Coastal infrastructure in Yamalo-Nenets Portrait: Susanna Gartler Terra infirma II: Reinforcing runways in Paulatuk Terra infirma III: Keeping cold food cold in Alaska Terra infirma IV: Urban planning in Ilulissat Nothing in isolation: Health and wellness and permafrost Portrait: Gwen Healey Akearok Toxic grounds: Contaminants and environmental health Coming back to life: Reemerging pathogens Frozen assets I: The formal economy Frozen assets II: Traditional and subsistence activities Cultural homeland: Alaas landscapes in Yakutia Holding Tight: Adaptation to Permafrost Thaw Bumpy road ahead: Transportation infrastructure and permafrost Undermined: Mining infrastructure and permafrost Keeping the light on: Energy infrastructure and permafrost No time to waste: Waste management and permafrost Modern history: Preserving Svalbard’s cultural heritage Portrait: Ingrid Rekkavik Going South: Permafrost in Other Areas A planetary perspective: Permafrost outside the Arctic Frozen giants: Permafrost in the mountains The view from the top: The Qinghai-Tibetan Plateau, Hindu Kush Himalaya, and Andes Europe’s frozen heart: Permafrost in the Alps The ends of the Earth I: Permafrost in Antarctica The ends of the Earth II: Antarctic Peninsula The ends of the Earth III: Queen Maud Land, Victoria Land, and the McMurdo Dry Valleys Over the Horizon Authors and contributors Acknowledgments Artist spotlight: Olga Borjon-Privé (Oluko) Artist spotlight: Katie Orlinsky Glossary Acronyms References
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  • 3
    Call number: AWI A7-24-95703
    Description / Table of Contents: The icosahedral non-hydrostatic large eddy model (ICON-LEM) was applied around the drift track of the Multidisciplinary Observatory Study of the Arctic (MOSAiC) in 2019 and 2020. The model was set up with horizontal grid-scales between 100m and 800m on areas with radii of 17.5km and 140 km. At its lateral boundaries, the model was driven by analysis data from the German Weather Service (DWD), downscaled by ICON in limited area mode (ICON-LAM) with horizontal grid-scale of 3 km. The aim of this thesis was the investigation of the atmospheric boundary layer near the surface in the central Arctic during polar winter with a high-resolution mesoscale model. The default settings in ICON-LEM prevent the model from representing the exchange processes in the Arctic boundary layer in accordance to the MOSAiC observations. The implemented sea-ice scheme in ICON does not include a snow layer on sea-ice, which causes a too slow response of the sea-ice surface temperature to atmospheric changes. To allow the sea-ice surface to respond faster to changes in the atmosphere, the implemented sea-ice parameterization in ICON was extended with an adapted heat capacity term. The adapted sea-ice parameterization resulted in better agreement with the MOSAiC observations. However, the sea-ice surface temperature in the model is generally lower than observed due to biases in the downwelling long-wave radiation and the lack of complex surface structures, like leads. The large eddy resolving turbulence closure yielded a better representation of the lower boundary layer under strongly stable stratification than the non-eddy-resolving turbulence closure. Furthermore, the integration of leads into the sea-ice surface reduced the overestimation of the sensible heat flux for different weather conditions. The results of this work help to better understand boundary layer processes in the central Arctic during the polar night. High-resolving mesoscale simulations are able to represent temporally and spatially small interactions and help to further develop parameterizations also for the application in regional and global models.
    Type of Medium: Dissertations
    Pages: xii, 110 Seiten , Illustrationen, Diagramme
    Language: English
    Note: Dissertation, Universität Potsdam, 2023 , Contents 1. Introduction 2. Boundary Layers Types of the Atmosphere 2.1. The Convective Boundary Layer (CBL) 2.2. The Neutral Boundary Layer (NBL) 2.3. The Stable Boundary Layer (SBL) 3. The Closure problem 4. Model description 4.1. Applied model versions 4.2. Governing equations 4.3. Horizontal grid 4.4. Vertical grid 4.5. Lateral boundaries 4.6. Parametrizations 4.6.1. Radiation scheme 4.6.2. Microphysics 4.6.3. Mellor-Yamada scheme 4.6.4. Smagorinsky scheme 4.6.5. Sea ice scheme 4.7. Difference to classical LES Models 5. Experimental Setup 6. MOSAiC Measurements 6.1. ARM Meteorological tower 6.2. Radiosondes 7. Model evaluation for the central Arctic 7.1. Impact of the horizontal resolution 7.1.1. Under cold, light wind conditions 7.1.2. Under stormy conditions 7.2. Impact of the sea-ice scheme 7.3. Impact of the lower boundary conditions 7.4. Impact of the parametrization schemes under cold, light wind conditions 7.4.1. Near-surface variables 7.4.2. Vertical profiles 7.4.3. Surface fluxes 7.4.4. Boundary Layer Height 7.5. Impact of the parametrization schemes under stormy conditions 7.5.1. Near-surface variables 7.5.2. Vertical profiles 7.5.3. Surface fluxes 7.5.4. Boundary Layer height 8. Discussion and Summary Acknowledgements Appendix
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  • 4
    Call number: 21/M 20.94120 ; AWI S6-24-91420
    Type of Medium: Monograph available for loan
    Pages: 288 Seiten , Illustrationen, Karten
    Language: English
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  • 5
    Call number: AWI G3-24-95700
    Description / Table of Contents: With Arctic ground as a huge and temperature-sensitive carbon reservoir, maintaining low ground temperatures and frozen conditions to prevent further carbon emissions that contrib-ute to global climate warming is a key element in humankind’s fight to maintain habitable con-ditions on earth. Former studies showed that during the late Pleistocene, Arctic ground condi-tions were generally colder and more stable as the result of an ecosystem dominated by large herbivorous mammals and vast extents of graminoid vegetation – the mammoth steppe. Characterised by high plant productivity (grassland) and low ground insulation due to animal-caused compression and removal of snow, this ecosystem enabled deep permafrost aggrad-ation. Now, with tundra and shrub vegetation common in the terrestrial Arctic, these effects are not in place anymore. However, it appears to be possible to recreate this ecosystem local-ly by artificially increasing animal numbers, and hence keep Arctic ground cold to reduce or-ganic matter decomposition and carbon release into the atmosphere. By measuring thaw depth, total organic carbon and total nitrogen content, stable carbon iso-tope ratio, radiocarbon age, n-alkane and alcohol characteristics and assessing dominant vegetation types along grazing intensity transects in two contrasting Arctic areas, it was found that recreating conditions locally, similar to the mammoth steppe, seems to be possible. For permafrost-affected soil, it was shown that intensive grazing in direct comparison to non-grazed areas reduces active layer depth and leads to higher TOC contents in the active layer soil. For soil only frozen on top in winter, an increase of TOC with grazing intensity could not be found, most likely because of confounding factors such as vertical water and carbon movement, which is not possible with an impermeable layer in permafrost. In both areas, high animal activity led to a vegetation transformation towards species-poor graminoid-dominated landscapes with less shrubs. Lipid biomarker analysis revealed that, even though the available organic material is different between the study areas, in both permafrost-affected and sea-sonally frozen soils the organic material in sites affected by high animal activity was less de-composed than under less intensive grazing pressure. In conclusion, high animal activity af-fects decomposition processes in Arctic soils and the ground thermal regime, visible from reduced active layer depth in permafrost areas. Therefore, grazing management might be utilised to locally stabilise permafrost and reduce Arctic carbon emissions in the future, but is likely not scalable to the entire permafrost region.
    Type of Medium: Dissertations
    Pages: X, 104, A-57 Seiten , Illustrationen, Diagramme
    Language: English
    Note: Dissertation, Universität Potsdam, 2024 , Table of contents ABSTRACT ZUSAMMENFASSUNG ABBREVIATIONS AND NOMENCLATURE CHAPTER 1: INTRODUCTION 1.1 SCIENTIFIC BACKGROUND 1.1.1 ARCTIC GROUND 1.1.2 THE PHENOMENON OF PERMAFROST 1.1.3 ARCTIC NON - PERMAFROST AREAS 1.1.4 HYPOTHESIS 1.2 AIMS AND OBJECTIVES 1.3 METHODS 1.3.1 FIELD METHODS AND SAMPLING APPROACH 1.3.2 STUDY AREA SELECTION 1.3.3 LABORATORY METHODS 1.4 THESIS ORGANISATION CHAPTER 2: LARGE HERBIVORES ON PERMAFROST – A PILOT STUDY OF GRAZING IMPACTS ON PERMAFROST SOIL CARBON STORAGE IN NORTHEASTERN SIBERIA 2.1 ABSTRACT 2.2 I NTRODUCTION 2.3 STUDY AREA 2.4 METHODS 2.4.1 FIELD SAMPLING APPROACH 2.4.2 LABORATORY WORK 2.4.3 DATA ANALYSIS AND EXTERNAL DATA 2.5 RESULTS 2.5.1 VEGETATION ASSESSMENT 2.5.2 SEASONAL THAW DEPTH 2.5.3 CARBON PARAMETERS (TOC, TOC/TN RATIOS , AND Δ13 C RATIOS ) 2.5.4 GRAIN SIZE DISTRIBUTION AND WATER CONTENT 2.5.5 STATISTICS AND CORRELATION ANALYSIS 2.6 DISCUSSION 2.6.1 EFFECTS OF GRAZING ON VEGETATION STRUCTURE AND PERMAFROST THAW 2.6.2 CARBON ACCUMULATION UNDER GRAZING IMPACT 2.6.3 METHODOLOGICAL LIMITATIONS OF THE PILOT STUDY 2.7 CONCLUSION 2.8 DATA AVAILABILITY STATEMENT 2.9 AUTHOR CONTRIBUTIONS 2.10 FUNDING 2.11 ACKNOWLEDGEMENTS 2.12 CONFLICT OF INTERESTS CHAPTER 3: IMPACTS OF REINDEER ON SOIL CARBON STORAGE IN THE SEASONALLY FROZEN GROUND OF NORTHERN FINLAND: A PILOT STUDY 3.1 ABSTRACT 3.2 I NTRODUCTION 3.3 STUDY AREA 3.4 METHODS 3.4.1 FIELD WORK 3.4.2 LABORATORY ANALYSIS 3.4.3 DATA ANALYSIS AND CALCULATIONS 3.5 RESULTS 3.5.1 CORE DESCRIPTIONS 3.5.2 VEGETATION 3.5.3 CARBON PARAMETERS 3.5.6 COMPARATIVE DATA ANALYSIS 3.6 DISCUSSION 3.6.1 REINDEER IMPACT ON SOIL CARBON STORAGE 3.6.2 REINDEER IMPACT ON VEGETATION 3.6.3 REINDEER IMPACT ON GROUND CHARACTERISTICS 3.6.4 SOC DENSITY AND STOCKS ACROSS THE KUTUHARJU STATION AREA 3.6.5 METHODOLOGICAL LIMITATIONS OF THE PILOT STUDY DESIGN 3.6.6 IMPLICATIONS OF THE PILOT STUDY FOR FUTURE RESEARCH 3.7 CONCLUSION 3.8 DATA AVAILABILITY 3.9 AUTHOR CONTRIBUTION 3.10 COMPETING INTERESTS 3.11 ACKNOWLEDGEMENTS 3.12 FUNDING TABLE 3-1 TABLE 3-2 TABLE 3-3 CHAPTER 4: LIPID BIOMARKER SCREENING TO TRACE RECENT LARGE HERBIVORE INFLUENCE ON SOIL CARBON IN PERMAFROST AND SEASONALLY FROZEN ARCTIC GROUND 4.1 ABSTRACT 4.2 I NTRODUCTION 4.3 STUDY AREA 4.4 METHODS 4.4.1 SAMPLING APPROACH 4.4.2 LABORATORY ANALYSIS 4.4.3 LIPID BIOMARKER INDICES 4.4.4 STATISTICS 4.5 RESULTS 4.5.1 TOC 4.5.2 C/N RATIO 4.5.3 STABLE CARBON ISOTOPE RATIO 4.5.4 ABSOLUTE N- ALKANE CONCENTRATION 4.5.5 AVERAGE CHAIN LENGTH 4.5.6 CARBON PREFERENCE INDEX 4.5.7 HIGHER - PLANT ALCOHOL INDEX 4.5.8 STATISTICAL RESULTS 4.6 DISCUSSION 4.6.1 EFFECTS OF GRAZING INTENSITY ON BIOMARKER SIGNALS 4.6.2 EFFECTS OF GROUND THERMAL REGIME ON SOIL OM DEGRADATION 4.6.3 I MPACT OF HERBIVORY ON PERMAFROST OM STORAGE 4.7 CONCLUSION 4.8 ACKNOWLEDGEMENTS 4.9 COMPETING INTERESTS 4.10 AUTHOR CONTRIBUTION 4.11 FUNDING 4.12 DATA AVAILABILITY CHAPTER 5: SYNTHESIS 5.1 ECOSYSTEM CHANGES UNDER THE IMPACT OF LARGE HERBIVORES 5.2 GRAZING EFFECTS ON SOIL ORGANIC MATTER DECOMPOSITION 5.3 F EASIBILITY OF UTILISING HERBIVORY IN THE ARCTIC 5.4 RESEARCH IMPLICATIONS FOR SUCCESSFUL PLANNING AND USE OF ARCTIC HERBIVORY REFERENCES 93 FINANCIAL AND TECHNICAL SUPPORT APPENDIX 1 APPENDIX I ORGANIC CARBON CHARACTERISTICS IN ICE - RICH PERMAFROST IN ALAS AND YEDOMA DEPOSITS , CENTRAL YAKUTIA, SIBERIA APPENDIX II WHAT ARE THE EFFECTS OF HERBIVORE DIVERSITY ON TUNDRA ECOSYSTEMS ? A SYSTEMATIC REVIEW (ABSTRACT) APPENDIX III SUPPLEMENTARY MATERIAL TO CHAPTER 2: LARGE HERBIVORES ON PERMAFROST – A PILOT STUDY OF GRAZING IMPACTS ON PERMAFROST SOIL CARBON STORAGE IN NORTHEASTERN SIBERIA APPENDIX IV SUPPLEMENTARY MATERIAL TO CHAPTER 3: IMPACTS OF REINDEER ON SOIL CARBON STORAGE IN THE SEASONALLY FROZEN GROUND OF NORTHERN FINLAND : A PILOT STUDY APPENDIX V SUPPLEMENTARY MATERIAL TO CHAPTER 4: A PILOT STUDY OF LIPID BIOMARKERS TO TRACE RECENT LARGE HERBIVORE INFLUENCE ON SOIL CARBON IN PERMAFROST AND SEASONALLY ROZEN ARCTIC GROUND APPENDIX VI SUPPLEMENTARY MATERIAL TO APPENDIX IV: ORGANIC CARBON CHARACTERISTICS IN ICE - RICH PERMAFROST IN ALAS AND YEDOMA DEPOSITS , CENTRAL YAKUTIA, SIBERIA ACKNOWLEDGEMENTS - DANKSAGUNG
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  • 6
    Monograph available for loan
    Monograph available for loan
    New York, NY : Humana Press
    Call number: AWI Bio-24-95664
    Description / Table of Contents: This volume provides detailed protocols for the isolation, enumeration, characterization of diverse bacteriophages, including both small to jumbo bacteriophages, from soil, fecal, municipal wastewater, and from food niche samples. Chapters highlight the diversity of bacteriophages in different environments, quantifications using culture, molecular techniques, protocols for isolate, interaction of bacteriophage proteins with host cells, and how to use bacteriophages to transfer foreign genetic elements to bacterial strains. In addition to the above, chapters feature the application of bacteriophages/bacteriophage-derived products. Written in the highly successful Methods in Molecular Biology series format, chapters include introductions to their respective topics, lists of necessary materials and reagents, step-by-step, readily reproducible laboratory protocols, and tips (in the Notes section) on troubleshooting and avoiding known pitfalls. Authoritative and cutting-edge, Bacteriophages: Methods and Protocols aims to ensure successful results in further study of this vital field.
    Type of Medium: Monograph available for loan
    Pages: XVI, 431 Seiten , Illustrationen
    ISBN: 978-1-0716-3548-3 , 9781071635483
    ISSN: 1064-3745 , 1940-6029
    Series Statement: Methods in Molecular Biology 2738
    Language: English
    Note: Contents Preface Contributors PART I AN OVERVIEW OF THE DIVERSITY OF BACTERIOPHAGES 1 Structural and Genomic Diversity of Bacteriophages / Bert Ely, Jacob Lenski, and Tannaz Mohammadi 2 The Diversity of Bacteriophages in the Human Gut / Amanda Carroll-Portillo, Derek M. Lin, and Henry C. Lin 3 Breaking the Ice: A Review of Phages in Polar Ecosystems / Mara Elena Heinrichs, Gonçalo J. Piedade, Ovidiu Popa, Pacifica Sommers, Gareth Trubl, Julia Weissenbach, and Janina Rahlff 4 The Diversity of Bacteriophages in Hot Springs / Timothy J. Marks and Isabella R. Rowland PART II ISOLATION OF BACTERIOPHAGES 5 Isolation of Bacteriophages from Soil Samples in a Poorly Equipped Field Laboratory in Kruger National Park / Ayesha Hassim and Kgaugelo Edward Lekota 6 Purification and Up-Concentration of Bacteriophages and Viruses from Fecal Samples / Frej Larsen, Rasmus Riemer Jakobsen, Xiaotian Mao, Josue Castro-Mejia, Ling Deng, and Dennis S. Nielsen 7 Isolation of Enterococcus Bacteriophages from Municipal Wastewater Samples Using an Enrichment Step / Cory Schwarz and Jacques Mathieu 8 Phage DNA Extraction, Genome Assembly, and Genome Closure / Justin Boeckman, Mei Liu, Jolene Ramsey, and Jason Gill PART III ENUMERATION OF BACTERIOPHAGES 9 Enumeration of Bacteriophages by Plaque Assay / Diana Elizabeth Waturangi 10 Detection and Quantification of Bacteriophages in Wastewater Samples by Culture and Molecular Methods/ Laura Sala-Comorera, Maite Muniesa, and Lorena Rodríguez-Rubio 11 Flow Virometry: A Fluorescence-Based Approach to Enumerate Bacteriophages in Liquid Samples / Elena A. Dlusskaya and Rafik Dey 12 A Metagenomics Approach to Enumerate Bacteriophages in a Food Niche / Kelsey White, Giovanni Eraclio, Gabriele Andrea Lugli, Marco Ventura, Jennifer Mahony, Fabio Dal Bello, and Douwe van Sinderen PART IV CHARACTERIZATION OF BACTERIOPHAGES 13 Bioinformatic Analysis of Staphylococcus Phages: A Key Step for Safe Cocktail Development / Soledad Telma Carrasco and He´ctor Ricardo Morbidoni 14 Use of Localized Reconstruction to Visualize the Shigella Phage Sf6 Tail Apparatus / Chun-Feng David Hou, Fenglin Li, Stephano Iglesias, and Gino Cingolani 15 Bacteriophage–Host Interactions and Coevolution / Diana M. Álvarez-Espejo, Dácil Rivera, and Andrea I. Moreno-Switt 16 Unraveling Physical Interactions of Clostridioides difficile with Phage and Phage-Derived Proteins Using In Vitro and Whole-Cell Assays / Wichuda Phothichaisri, Tanaporn Phetruen, Surang Chankhamhaengdecha, Tavan Janvilisri, Puey Ounjai, Robert P. Fagan, and Sittinan Chanarat 17 Phage Transduction of Staphylococcus aureus / Melissa-Jane Chu Yuan Kee and John Chen PART V APPLICATION OF BACTERIOPHAGES AND BACTERIOPHAGE-DERIVED COMPONENTS 18 The Next Generation of Drug Delivery: Harnessing the Power of Bacteriophages / Alaa A. A. Aljabali, Mohammad B. M. Aljbaly, Mohammad A. Obeid, Seyed Hossein Shahcheraghi, and Murtaza M. Tambuwala 19 Construction of Nonnatural Cysteine-Cross-Linked Phage Libraries / Brittney Chau, Kristi Liivak, and Jianmin Gao 20 Application of Deep Sequencing in Phage Display / Vincent Van Deuren, Sander Plessers, Rob Lavigne, and Johan Robben 21 The Application of Bacteriophage and Photoacoustic Flow Cytometry in Bacterial Identification / Robert H. Edgar, Anie-Pier Samson, and John A. Viator 22 Propagation, Purification, and Characterization of Bacteriophages for Phage Therapy / Katarzyna Kosznik-Kwaśnicka, Gracja Topka, Jagoda Mantej, Łukasz Grabowski, Agnieszka Necel, Grzegorz Węgrzyn, and Alicja Węgrzyn 23 Overcoming Bacteriophage Resistance in Phage Therapy / Elina Laanto 24 Bacteriophage Virus-Like Particles: Platforms for Vaccine Design / Ebenezer Tumban Index
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  • 7
    Call number: AWI G5-24-95642
    In: Developments in paleoenvironmental research, 21
    In: Tracking environmental change using lake sediments, 6
    Description / Table of Contents: This book, entitled Tracking Environmental Change Using Lake Sediments: Volume 6 – Sedimentary DNA, provides an overview of the applications of sedimentary DNA-based approaches to paleolimnological studies. These approaches have shown considerable potential in providing information about the long-term changes of overall biodiversity in lakes and their watersheds in response to natural and anthropogenic changes, as well as tracking human migrations over the last thousands of years. Although the first studies investigating the preservation of these molecular proxies in sediments originate from the late-1990s, the number of scientific publications on this topic has increased greatly over the last five years. Alongside numerous ecological findings, several sedimentary DNA studies have been dedicated to understanding the reliability of this approach to reconstruct past ecosystem changes. Despite the major surge of interest, a comprehensive compilation of sedimentary DNA approaches and applications has yet to be attempted. The overall aim of this DPER volume is to fill this knowledge gap.
    Type of Medium: Monograph available for loan
    Pages: xxiii, 437 Seiten , Illustrationen
    ISBN: 9783031437991 , 978-3-031-43798-4 , 9783031437984
    Series Statement: Developments in paleoenvironmental research 21
    Language: English
    Note: Contents 1 Using Lake Sedimentary DNA to Reconstruct Biodiversity Changes / Eric Capo, Cécilia Barouillet, and John P. Smol 2 The Sources and Fates of Lake Sedimentary DNA / Charline Giguet-Covex, Stanislav Jelavić, Anthony Foucher, Marina A. Morlock, Susanna A. Wood, Femke Augustijns, Isabelle Domaizon, Ludovic Gielly, and Eric Capo 3 The Sedimentary Ancient DNA Workflow / Peter D. Heintzman, Kevin Nota, Alexandra Rouillard, Youri Lammers, Tyler J. Murchie, Linda Armbrecht, Sandra Garcés-Pastor, and Benjamin Vernot 4 Bacterial and Archaeal DNA from Lake Sediments / Aurèle Vuillemin, Marco J. L. Coolen, Jens Kallmeyer, Susanne Liebner, and Stefan Bertilsson 5 Cyanobacterial DNA from Lake Sediments / Marie-Eve Monchamp and Frances R. Pick 6 Protist DNA from Lake Sediments / Cécilia Barouillet, Isabelle Domaizon, and Eric Capo 7 Diatom DNA from Lake Sediments / Katharina Dulias, Laura S. Epp, and Kathleen R. Stoof-Leichsenring 8 Aquatic Vegetation DNA from Lake Sediments / Aloïs Revéret, Inger G. Alsos, and Peter D. Heintzman 9 Aquatic Animal DNA from Lake Sediments / Irene Gregory-Eaves, Marie-Eve Monchamp, and Zofia E. Taranu 10 Terrestrial Plant DNA from Lake Sediments / Sandra Garcés-Pastor, Kevin Nota, Dilli P. Rijal, Sisi Liu, Weihan Jia, Maria Leunda, Christoph Schwörer, Sarah E. Crump, Laura Parducci, and Inger G. Alsos 11 Terrestrial Fauna and Hominin DNA from Sedimentary Archives / Tyler J. Murchie, Charline Giguet-Covex, Peter D. Heintzman, Viviane Slon, and Yucheng Wang 12 An Overview of Biodiversity and Network Modeling Approaches: Applications to Sedimentary DNA Records / Zofia E. Taranu, Irene Gregory-Eaves, and Marie-Eve Monchamp 13 Perspectives and Future Developments Within Sedimentary DNA Research / Luke E. Holman, Yi Wang, Rikai Sawafuji, Laura S. Epp, Kristine Bohmann, and Mikkel Winther Pedersen Glossary, Acronyms and Abbreviations Index
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  • 8
    Monograph available for loan
    Monograph available for loan
    [Marburg] : H4O - Heroes for the Ocean
    Call number: AWI G2-24-95628
    Type of Medium: Monograph available for loan
    Pages: 200 Seiten , Illustrationen , 24.5 cm x 19.5 cm, 850 g
    Edition: 1. Auflage
    ISBN: 9783000752018 , 978-3-00-075201-8
    Series Statement: Edition 1 - Ostsee - Nordsee, Nordatlantik
    Language: German
    Note: INHALT Vorwort ERSTER TEIL Faszination Ozean Im Reich der Tiefe Astronaut auf Erden Die Stimme der Meere ZWEITER TEIL Am Abgrund der Meere Der Schatz von Helgoland Geisterjagd vor Rügen Am Limit DRITTER TEIL Der Weg nach vorn Unscheinbarer Superheld Grundreinigung Mut zur Hoffnung Dein Leben für den Ozean DANKSAGUNG DIE AUTOREN IMPRESSUM BILDNACHWEIS
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  • 9
    Call number: AWI G2-23-95540
    In: World ocean review, 8
    Type of Medium: Series available for loan
    Pages: 243 Seiten , Illustrationen
    ISBN: 978-3-86648-733-8 , 9783866487338
    Series Statement: World ocean review 8
    Language: English
    Note: Inhaltsverzeichnis Vorwort Kapitel 1 Dringlichst gesucht – Wege aus der Klimakrise Alarmstufe Rot für Mensch und Natur Lösungen für das Treibhausgas-Problem? CONCLUSIO: Die Klimakrise kennt nur eine Lösung: Treibhausgasneutralität Kapitel 2 Die Rolle des Ozeans im Kohlenstoffkreislauf der Erde Wie der Ozean Kohlendioxid aufnimmt CONCLUSIO: Kohlenstoffspeicher Ozean: Riesig, effizient und in Gefahr 67 Kapitel 3 Das ungenutzte Klimaschutzpotenzial der Ökosysteme an Land Wälder, Wiesen und Böden als Kohlenstoffspeicher CONCLUSIO: Lösungen, die viel zu selten umgesetzt werden Kapitel 4 Marine CDR-Verfahren: Forschung unter Zeit- und Erwartungsdruck Ein Ozean der Möglichkeiten oder gefährlicher Hype? Kapitel 5 Mehr Kohlenstoffeinlagerung in Wiesen und Wäldern des Meeres? Blue Carbon: Ein Lösungsansatz mit doppeltem Nutzen CONCLUSIO: Küstenökosysteme: Marine Kohlenstoffsenke mit unverzichtbaren Zusatzleistungen Kapitel 6 Künstlicher Auftrieb: Die Idee von der Begrünung des Ozeans Eine Anschubhilfe für die biologische Kohlenstoffpumpe CONCLUSIO: Künstlicher Auftrieb – Prädikat: „nur bedingt nützlich“ Kapitel 7 Gezielte Eingriffe in die Meereschemie Alkalinitätserhöhung: Verfahren in den Kinderschuhen CONCLUSIO: Alkalinitätserhöhung – theoretisch verstanden, im Feld jedoch kaum getestet Kapitel 8 Kohlendioxid verpressen tief unter dem Meer Gasspeicherung in Sandsteinschichten und Basaltgestein CONCLUSIO: Kohlendioxidspeicherung unter dem Meer: Ein umstrittenes Verfahren im Aufwind Kapitel 9 Leitprinzipien und Regeln für einen Einsatz mariner CDR-Verfahren Wie regelt man eine verstärkte CO2-Aufnahme des Meeres? CONCLUSIO: Regulierung möglicher CDR-Einsätze: Gebraucht werden klare Strategien und Vorschriften Gesamt-Conclusio Abkürzungen Quellenverzeichnis Mitwirkende Index Partner und Danksagung Abbildungsverzeichnis Impressum .
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  • 10
    Call number: AWI P1-20-94200 ; M 23.94200
    Description / Table of Contents: Die Hochgebirge haben eine große Bedeutung für das globale Klima, die Wasserversorgung und die Biosphäre. So ist die besonders starke Ausprägung des Amazonas-Regenwalds den Anden zu verdanken. Sie verhindern den Durchzug der aus dem Atlantik mit viel Luftfeuchtigkeit kommenden Wolken. Dadurch erhält das Amazonas-Gebiet im Jahresdurchschnitt über 2.000 mm Regen, was die Grundlage für die intensive Bewaldung ist. Obwohl die Gebirge global nur ca. 12% der Landfläche bedecken, beherbergen Hochgebirge rund die Hälfte aller Säugetierarten und 74% aller endemischen Vogelarten (ohne Inselarten). 21 der 34 globalen Biodiversitätshotspots befinden sich in Hochgebirgen. In den Gebirgen entstehen aufgrund von höheren Niederschlägen wichtige Wasserressourcen auch für die angrenzenden Tiefländer. Trotz der für den Menschen oft erschwerten Zugänglichkeit sind Hochgebirge und Hoch-Plateaus, besonders in tropischen Regionen, Orte dichter Besiedlung und sogar von Hochkulturen. Die Folgen des Klimawandels sind in den Hochgebirgen besonders deutlich. So war die Erwärmung in den vergangenen Jahrzehnten dort höher als in den Flachländern. Die Gletscher schrumpfen in fast allen Gebirgen, insbesondere in den letzten Jahrzehnten. Auf den jetzt eisfreien Flächen siedeln sich schon nach wenigen Jahren neue Pflanzengemeinschaften an. In den Alpen hat das Eisvolumen seit 1850 schon um mehr als zwei Drittel abgenommen. Das entspricht allein seit 1997 einem Süßwasserverlust von etwa dem 14fachen Volumen des Bodensees. Insgesamt sind die Klimaänderungen in den Gebirgsregionen gravierender als im Flachland. Mit der Zunahme der Starkregen und dem Rückgang des Permafrosts nimmt die Gefahr von Erdrutschen zu, und manche Gletscher wurden instabil. Im Mittel haben sich die Temperaturen im Gebirgspermafrost in einem Jahrzehnt von 2007 bis 2016 um etwa 0,2°C erhöht. Die Schneedeckendauer nahm in den letzten Jahrzehnten kontinuierlich ab; die Herausforderungen für den Wintertourismus werden zusehends größer.
    Type of Medium: Monograph available for loan
    Pages: 384 Seiten , Illustrationen, Diagramme, Karten
    ISBN: 9783982006734
    Language: German
    Note: Inhaltsverzeichnis Vorwort Liste der Autoren/Autorinnen und der Gutachter Hochgebirge: Definition, Bedeutung, Veränderungen und Gefahren / (José L. Lozán,Siegmar-W. Breckle, Heidi Escher-Vetter, Hartmut Graßl & Dieter Kasang) 1 Bedeutung der Hochgebirge 1.1 Der Einfluss von Hochgebirgen auf die Zirkulation der Atmosphäre / (Jürgen Böhner & Jörg Bendix) 1.2 Die Entstehung der Hochgebirge / (Martin Meschede) 1.3 Übersicht über die wichtigsten Gebirge der Erde / (José L.Lozán, Siegmar-W. Breckle, Dieter Kasang & Heidi Escher-Vetter) 1.4 Berge und Gebirge im Meer / (Bernd Christiansen) 1.5 Hochgebirge: Wassertürme für eine wachsende Weltbevölkerung / (Carmen de Jong) 1.6 Erdoberflächenprozesse im Hochgebirge – Der Einfluss des Klimawandels / (Lothar Schrott & Jan Blöthe) 1.7 Hochgebirge: Hotspots der Biodiversität / (Severin Irl & Andreas H. Schweiger) 1.8 Hochgebirge als Ressourcenräume für Tiefländer / (Matthias Winiger) 1.9 Bevölkerung und Siedlungsstrukturen im Hochgebirge / (Christoph Stadel & Axel Borsdorf) 1.10 Lokale Anpassungsstrategien für Landnutzung in Hochgebirgen / (Hermann Kreutzmann) 2 Paläoökologische Veränderungen in Hochgebirgen 2.1 Globale Klima- und Gletscherveränderungen im Pleistozän und Holozän / (Heinz Veit & Alexander Groos) 2.2 Welche Umweltinformationen können aus Jahrringen abgeleitet werden? / (Achim Bräuning & Jussi Grießinger) 2.3 Holozäne Klimaänderungen und Waldgrenzschwankungen in den Alpen / (Conradin A. Burga) 2.4 Anthropogene Einflüsse auf die Hochgebirgsumwelt im Holozän: Einblicke aus einer alpinen Bergbaulandschaft / (Kerstin Kowarik & Hans Reschreiter) 3 Veränderungen der Kryosphäre in Hochgebirgen 3.1 Gletscherbeobachtung und globale Trends / (Frank Paul & Martin Hoelzle) 3.2 Die Gletscher Hochasiens im Klimawandel / (Tobias Bolch, Atanu Bhattacharya & Owen King) 3.3 Die Karakorum-Anomalie / (Christoph Mayer, Astrid Lambrecht & Alexander Groos) 3.4 Wenn Gletscher abrutschen / (Andreas Kääb) 3.5 Tropische Gletscher: Ostafrika / (Rainer Prinz & Thomas Mölg) 3.6 Die Gletscher der Anden im Klimawandel / (Thorsten Seehaus) 3.7 Gletscher und Schnee in Hochgebirgen Nordamerikas / (Dieter Kasang & José L. Lozán) 3.8 Gletscherschmelze unter Schuttbedeckung: Verbreitung, Prozesse und Messmethoden / (Pascal Buri, Simone Schauwecker & Jakob Steiner) 3.9 Permafrost in den Alpen – Langzeitbeobachtung und Entwicklung über zwei Jahrzehnte (Jeannette Nötzli) 3.10 Globale Klimaänderung und die Gletscher auf Neuseeland / (Stefan Winkler) 3.11 Einfluss des Klimawandels auf die Schneebedeckung / (Kay Helfricht & Marc Olefs) 4 Hydrologische Veränderungen in Hochgebirgen 4.1 Hochgebirgsgewässer im Wandel / (Heike Zimmermann-Timm, Deep Narayan Shah & Ram Devi Tachamo Shah) 4.2 Einfluss des globalen Wandels auf die Bodenstabilität des alpinen Graslandes / (Christine Alewell, Lauren Zweifel & Katrin Meusburger 4.3 Sozio-Hydrologie des Trans-Himalaya – Schmelzwasserverfügbarkeit und Bewässerungslandwirtschaft / (Marcus Nüsser, Juliane Dame & Susanne Schmidt) 4.4 Hochgebirge und Wasserressourcen in Peru und Kalifornien / (Dieter Kasang) 4.5 Hydrologische Veränderungen in vergletscherten Einzugsgebieten / (Regine Hoch) 5 Biodiversität der Hochgebirge im Klimawandel 5.1 Klimawandel und Vegetationsdynamik im Hochgebirge / (Harald Pauli) 5.2 Phänologische Veränderungen in Hochgebirgen / (Christian Rixen) 5.3 Klimawandel und Gebirgswälder: Bedrohung der Multifunktionalität? / (Georg Gratzer) 5.4 Alpine Waldgrenzen im Klimawandel – Wie sind die heterogenen Reaktionsmuster zu erklären? / (Udo Schickhoff, Maria Bobrowski & Niels Schwab) 5.5 Vegetation und Klimawandel an der Ostkordillere von Ecuador am Beispiel des Páramo de Papallacta / (M. Daud Rafiqpoor & Siegmar-W. Breckle) 5.6 Auswirkungen des Klimawandels auf das Wachstum von Zwergsträuchern in Hochgebirgen / (Stef Weijers & Jörg Löffler) 5.7 Pflanzen besiedeln neue Lebensräume: Primärsukzession auf Gletschervorfeldern / (Brigitta Erschbamer & Conradin A. Burga) 5.8 Klimawandel und biologische Invasionen im Hochgebirge /(Anna Schertler, Franz Essl & Bernd Lenzner) 5.9 Die Tierwelt der Alpen im Klimawandel / (Peter Huemer, Hermann Sonntag, Friederike Barkmann & André Stadler) 5.10 Ökologische Folgen des Landnutzungswandels in den Alpen / (Erich Tasser & Ulrike Tappeiner) 6 Sozioökonomische Veränderungen in Hochgebirgen 6.1 Ökonomische Bewertung von Biodiversität und Ökosystemleistungen in den Alpen / (Andreas Bartel & Barbara Färber) 6.2 Der sozioökonomische Strukturwandel in den Alpen / (Oliver Bender & Andreas Haller) 6.3 Klimawandel und Wintersporttourismus: Wahrnehmung und Reaktion der Touristen / (Jürgen Schmude & Maximilian Witting) 6.4 Mensch-Umwelt-Interaktionen im Äthiopischen Hochland / (Simon Strobelt & Michèle von Kocemba) 7 Naturgefahren in Hochgebirgen 7.1 Klimawandel, Morphodynamik und gravitative Massenbewegungen / (Thomas Glade) 7.2 Einfluss der Permafrostdegradation auf Hangstabilität / (Friederike Günzel & Wilfried Haeberli) 7.3 Warnsignal Klima - Die Lawinengefahr im Klimawandel / (Benjamin Reuter, Christoph Mitterer & Sascha Bellaire) 7.4 Gefahren aus vergletscherten Vulkanen: Das Beispiel Nevado del Ruiz / (Simon Allen, Christian Huggel & Frank Paul) 7.5 Bedrohung durch Erdbeben im Himalaya / (Birger-G. Lühr) 7.6 Risiken durch Gletscherseen im Klimawandel / (Holger Frey & Wilfried Haeberli) 7.7 Bergstürze, Seeausbrüche und Muren im Pamir / (Siegmar-W. Breckle & Martin Mergili) 8 Maßnahmen zum Klimaschutz und zur Anpassung 8.1 Klimawandel und Naturschutz im Gebirge: Neue Herausforderungen / (Mario F. Broggi) 8.2 Klimawandel und Anpassungsstrategien im Alpentourismus / (Ulrike Pröbstl-Haider) 8.3 Klimawandel in den Lebenswelten und Handlungslogiken ländlicher Bevölkerung im Hochgebirge: Perspektiven aus dem Callejón de Huaylas, Peru / (Martina Neuburger) 8.4 Hochland-Tiefland Beziehungen in ihrer Bedeutung für eine nachhaltige Entwicklung in Gebirgsräumen / (Paul Messerli, Susanne Wymann von Dach & Thomas Kohler) 9 Sachregister
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