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  • 1
    Monograph available for loan
    Monograph available for loan
    Harlow, England : Pearson
    Call number: AWI G10-21-94627
    Type of Medium: Monograph available for loan
    Pages: xxv, 810 Seiten , Illustrationen, Karten , 28 cm
    Edition: Fourth edition
    ISBN: 9781292083575
    Language: English
    Note: Contents Preface to the fourth edition Contributors Editor's acknowledgements Acknowledgements Part I: The role of physical geography 1 Approaching physical geography 1.1 Introduction 1.2 Historical development of physical geography 1.2.1 Physical geography before 1800 1.2.2 Physical geography between 1800 and 1950 1.2.3 Physical geography since 1950 1.3 Scientific methods 1.3.1 The positivist method 1.3.2 Critique of the positivist method 1.3.3 Realism as an alternative positivist approach 1.3.4 Benefits of multiple scientific methods in physical geography 1.4 The field, the laboratory and the model 1.4.1 Approaching data collection from the environment 1.4.2 Approaching laboratory work 1.4.3 Approaching numerical modelling 1.5 Using physical geography for managing the environment 1.6 Summary Further reading Part II: Continents and oceans 2 Earth geology and tectonics 2.1 Introduction 2.2 The Earth's structure 2.2.1 The interior of the Earth 2.2.2 The outer layers of the Earth 2.3 Rock type and formation 2.3.1 Igneous rock 2.3.2 Sedimentary rock 2.3.3 Metamorphic rock 2.3.4 The rock cycle 2.4 History of plate tectonics 2.4.1 Early ideas of global tectonics 2.4.2 Evidence that led directly to plate tectonic theory 2.5 The theory of plate tectonics 2.5.1 Lithospheric plates 2.5.2 Rates of plate movement 2.6 Structural features related directly to motion of the plates 2.6.1 Divergent plate boundaries 2.6.2 Transform faults 2.6.3 Convergent plate boundaries 2.6.4 Hot spots 2.7 The history of the continents 2.8 Summary Further reading 3 Oceans 3.1 Introduction 3.2 The ocean basins 3.2.1 The scale of the oceans 3.2.2 Geological structure of the ocean basins 3.2.3 The depth and shape of the ocean basins 3.3 Physical properties of the ocean 3.3.1 Salinity 3.3.2 Temperature structure of the oceans 3.4 Ocean circulation 3.4.1 Surface currents 3.4.2 The deep currents of the oceans 3.4.3 The weather of the ocean 3.5 Sediments in the ocean 3.6 Biological productivity 3.6.1 Photosynthesis in the ocean 3.6.2 Importance of nutrient supply to primary productivity 3.6.3 Animals of the sea 3.6.4 Pollution 3.7 Effect of global climate change on the oceans 3.8 Summary Further reading Part III: Past, present and future climate and weather 4 The Pleistocene 4.1 Introduction 4.2 Long-term cycles, astronomical forcing and feedback mechanisms 4.2.1 Orbital forcing theory 4.2.2 Evidence that orbital forcing causes climate change 4.2.3 Problems with orbital forcing theory 4.2.4 Internal feedback mechanisms 4.3 Short-term cycles 4.3.1 Glacial instability 4.3.2 The Younger Dryas 4.4 Further evidence for environmental change 4.4.1 Landforms 4.4.2 Plants 4.4.3 Insects 4.4.4 Other animal remains 4.5 Dating methods 4.5.1 Age estimation techniques 4.5.2 Age equivalent labels 4.5.3 Relative chronology 4.6 Pleistocene stratigraphy and correlation 4.7 Palaeodimate modelling 4.8 Summary Further reading 5 The Holocene 5.1 Introduction 5.2 Holocene climatic change 5.2.1 How the Holocene began 5.2.2 Drivers of climate change during the Holocene 5.2.3 The Little Ice Age 5.3 Holocene geomorphological change 5.3.1 Retreating ice sheets 5.3.2 Rising seas 5.4 Holocene ecosystem change 5.4.1 Responses of ecosystems to the end of the last glacial 5.4.2 Tropical Africa and the Sahara 5.4.3 European ecosystems 5.4.4 Island ecosystems 5.5 The rise of civilizations 5.5.1 Humans at the end of the last glacial 5.5.2 The beginnings of agriculture 5.5.3 Social and environmental consequences of agriculture 5.6 Human interaction with physical geography 5.6.1 Out of Eden? 5.6.2 Deforestation 5.6.3 Soil erosion and impoverishment 5.6.4 Irrigation and drainage 5.7 Summary Further reading 6 Atmospheric processes 6.1 Introduction 6.2 The basics of climate 6.3 The global atmospheric circulation 6.4 Radiative and energy systems 6.4.1 The nature of energy 6.4.2 Distinguishing between temperature and heat 6.4.3 Radiation 6.4.4 Thermal inertia 6.4.5 The atmospheric energy balance 6.5 Moisture circulation systems 6.5.1 Moisture in the atmosphere and the hydrological cycle 6.5.2 Global distribution of precipitation and evaporation 6.5.3 The influence of vegetation on evaporation 6.5.4 Drought 6.6 Motion in the atmosphere 6.6.1 Convective overturning 6.6.2 The Earth's rotation and the winds 6.6.3 Long waves. Planetary Waves and Rossby Waves 6.6.4 Jet streams 6.7 The influence of oceans and ice on atmospheric processes 6.8 The Walker circulation 6.8.1 El Niño Southern Oscillation 6.8.2 North Atlantic Oscillation 6.9 Interactions between radiation, atmospheric trace gases and clouds 6.9.1 The greenhouse effect 6.9.2 A simple climate model of the enhanced greenhouse effect 6.9.3 Radiative interactions with clouds and sulfate aerosols 6.10 Ceoengineering 6.11 Summary Further reading 7 Contemporary climate change 7.1 Introduction 7.2 Climate change 7.2.1 Long-term change 7.2.2 Recent climate change and its causes 7.2.3 Predictions from global climate models (GCMs) 7.2.4 Critical evaluation of the state-of-the-art in GCMs 7.3 The carbon cycle: interaction with the climate system 7.4 Mitigation 7.5 Destruction of the ozone layer by chlorofluorocarbons (CFCs) 7.6 The future 7.7 Summary Further reading 8 Global climate and weather 8.1 Introduction 8.2 General controls of global climates 8.3 The tropics and subtropics 8.3.1 Equatorial regions 8.3.2 The Sahel and desert margins 8.3.3 Subtropical deserts 8.3.4 Humid subtropics 8.4 Mid and high-latitude climates 8.4.1 Depressions, fronts and anticyclones 8.4.2 Mid-latitude western continental margins 8.4.3 Mid-latitude east continental margins and continental interiors 8.5 Polar climates 8.6 A global overview 8.7 Summary Further reading 9 Regional and local climates 9.1 Introduction 9.2 Altitude and topography 9.2.1 Pressure 9.2.2 Temperature 9.2.3 Wind 9.2.4 Precipitation 9.2.5 Frost hollows 9.3 Influence of water bodies 9.4 Human influences 9.4.1 Shelter belts 9.4.2 Urban climates 9.4.3 Atmospheric pollution and haze 9.5 Summary Further reading Part IV: Biogeography and ecology 10 The biosphere 10.1 Introduction 10.2 Biological concepts 10.2.1 What is a species? 10.2.2 The naming of species 10.2.3 Levels of organization 10.2.4 Biodiversity 10.3 Patterns of distribution 10.3.1 Potential species distributions 10.3.2 Actual species distributions 10.3.3 Spatial patterns in biodiversity 10.4 Terrestrial biomes 10.4.1 Equatorial and tropical forests 10.4.2 Savanna 10.4.3 Hot Desert 10.4.4 Mediterranean-type biome 10.4.5 Temperate grassland 10.4.6 Temperate broadleaf forest 10.4.7 Taiga 10.4.8 Tundra 10.5 Aquatic biomes 10.5.1 Marine regions 10.5.2 Freshwater regions 10.6 Summary Further reading 11 Ecosystem processes 11.1 Introduction 11.2 The flow of energy and resources 11.2.1 Energy entering an ecosystem 11.2.2 Ecological thermodynamics 11.2.3 Trophic levels and food webs 11.2.4 Biogeochemical cycles 11.3 Biotic interactions 11.3.1 Mutualism 11.3.2 Herbivory, prédation and parasitism 11.3.3 Commensalism 11.3.4 Amensalism 11.3.5 Competition 11.4 Temporal change in ecosystems 11.4.1 Short-term changes 11.4.2 Disturbance and resilience 11.4.3 Succession 11.5 Human impact 11.5.1 Degrading ecosystems 11.5.2 Urban ecology 11.5.3 Conservation 11.6 Summary Further reading 12 Freshwater ecosystems 12.1 Introduction 12.2 Running waters: rivers and streams 12.2.1 River ecosystem geomorphological units 12.2.2 Spatial variability of river ecosystems 12.2.3 Temporal variability of river ecosystems 12.2.4 Human alterations to river ecosystems 12.3 Still waters: lakes and ponds 12.3.1 Classification of lake ecosystems 12.3.2 Spatial variability of lake ecosystems 12.3.3 Human influences on lake ecosystems 12.4 Summary Further reading 13 Vegetation and env
    Location: AWI Reading room
    Branch Library: AWI Library
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  • 2
    Electronic Resource
    Electronic Resource
    s.l. : American Chemical Society
    Biochemistry 29 (1990), S. 2127-2134 
    ISSN: 1520-4995
    Source: ACS Legacy Archives
    Topics: Biology , Chemistry and Pharmacology
    Type of Medium: Electronic Resource
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  • 3
    ISSN: 1573-4978
    Keywords: bone ; intermediate filament ; nuclear matrix ; osteoblast ; osteosarcoma ; tissue matrix
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract Treatment for osteosarcoma is problematic because there are no prognostic markers. Diagnosis is primarily limited to cytologic grading. Oncogenesis alters cell structure therefore osteoblast tissue matrix proteins (extracellular matrix, cytoskeletal, intermediate filament, and nuclear matrix proteins), components of the cell substructure, are candidates for osteosarcoma markers. Structural proteins of the extracellular matrix, e.g. the collagens, are useful for diagnosis but not for tumors that produce little osteoid. To identify principal cellular tissue matrix proteins that distinguish normal from transformed human osteoblasts, their expression in normal osteoblasts, two osteosarcoma cell lines, and three primary osteosarcoma tumors were compared. The tumors were graded as (i) intermediate, (ii) high, and (iii) high grade recurrent. The 1-D SDS/PAGE profiles of the major components of the nuclear matrix and intermediate filament fractions from normal osteoblasts did not vary with biopsy site, age, or sex of patients. These profiles included known cytoskeletal proteins and OB250, a ∼250 kD protein(s) observed in the intermediate filament fraction. A loss of protein bands, including OB250, was observed in the osteosarcoma cell lines and tumors. The intermediate and high grade tumors exhibited nearly identical protein profiles including potential tumor-specific proteins and collagen, consistent with the presence of intracellular collagen fibers in osteosarcoma. A microsequence was obtained for OT25, a novel low molecular weight protein observed in osteosarcoma cell lines. Fibrinogen γ-chain, a protein that mediates cell adhesion was recovered from the high grade recurrent tumor.
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    New York, N.Y. : Wiley-Blackwell
    Journal of Cellular Biochemistry 67 (1997), S. 451-465 
    ISSN: 0730-2312
    Keywords: bone ; differentiation ; nuclear matrix ; osteoblast ; topoisomerase II ; Life and Medical Sciences ; Cell & Developmental Biology
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Biology , Chemistry and Pharmacology , Medicine
    Notes: The molecular mechanisms that mediate the transition from an osteoprogenitor cell to a differentiated osteoblast are unknown. We propose that topoisomerase II (topo II) enzymes, nuclear proteins that mediate DNA topology, contribute to coordinating the loss of osteoprogenitor proliferative capacity with the onset of differentiation. The isoforms topo II-α and -β, are differentially expressed in nonosseous tissues. Topo II-α expression is cell cycle-dependent and upregulated during mitogenesis. Topo II-β is expressed throughout the cell cycle and upregulated when cells have plateaued in growth. To determine whether topo II-α and -β are expressed in normal bone, we analyzed rat lumbar vertebrae using immunohistochemical staining. In the tissue sections, topo II-α was expressed in the marrow cavity of the primary spongiosa. Mature osteoblasts along the trabecular surfaces did not express topo II-α, but were immunopositive for topo II-β, as were cells of the marrow cavity. Confocal laser scanning microscopy was used to determine the nuclear distribution of topo II in rat osteoblasts isolated from the metaphyseal distal femur and the rat osteosarcoma cells, ROS 17/2.8. Topo II-α exhibited a punctate nuclear distribution in the bone cells. Topo II-β was dispersed throughout the interior of the nucleus but concentrated at the nuclear envelope. Serum starvation of the cells attenuated topo II-α expression but did not modulate expression of the β-isoform. These results indicate that the loss of osteogenic proliferation correlates with the downregulation of topo II-α expression. J. Cell. Biochem. 67:451-465, 1997. © 1997 Wiley-Liss, Inc.
    Additional Material: 6 Ill.
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  • 5
    Electronic Resource
    Electronic Resource
    New York, N.Y. : Wiley-Blackwell
    Journal of Cellular Biochemistry 63 (1996), S. 374-383 
    ISSN: 0730-2312
    Keywords: tissue matrix ; primary spongiosa ; PTH-induced downregulation ; topoisomerase ; NuMA ; Life and Medical Sciences ; Cell & Developmental Biology
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Biology , Chemistry and Pharmacology , Medicine
    Notes: Parathyroid hormone (PTH) alters osteoblast morphology. How these changes in cell shape modify nuclear structure and ultimately gene expression is not known. Chronic exposure to rat PTH (1-34) [10 nM] attenuated the expression of 200, 190, and 160 kD proteins in the nuclear matrix-intermediate filament subfraction of the rat osteosarcoma cells, ROS 17/2.8 [Bidwell et al. (1994b): Endocrinology 134:1738-1744]. Here, we determined that these same PTH-responsive proteins were expressed in rat metaphyseal osteoblasts. We identified the 200 kD protein as a non-muscle myosin. Although the molecular weights, subcellular distribution, and half-lives of the 190 and 160 kD proteins were similar to topoisomerase II-α and -β, nuclear matrix enzymes that mediate DNA topology, the 190 and 160 kD proteins did not interact with topoisomerase antibodies. Nevertheless, the expression of topoisomerase II-α, and NuMA, a component of the nuclear core filaments, was also regulated by PTH in the osteosarcoma cells. The 190 kD protein was selectively expressed in bone cells as it was not observed in OK opossum kidney cells, H4 hepatoma cells, or NIH3T3 cells. PTH attenuated mRNA expression of the PTH receptor in our cell preparations. These results demonstrate that PTH selectively alters the expression of osteoblast membrane, cytoskeletal, and nucleoskeletal proteins. Topoisomerase II-α, NuMA, and the 190 and 160 kD proteins may direct the nuclear PTH signalling pathways to the target genes and play a structural role in osteoblast gene expression. © 1996 Wiley-Liss, Inc.
    Additional Material: 7 Ill.
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  • 6
    Publication Date: 2017-04-13
    Print ISSN: 0923-4861
    Electronic ISSN: 1572-9834
    Topics: Biology
    Published by Springer
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  • 7
    Publication Date: 2017-04-22
    Print ISSN: 0094-8276
    Electronic ISSN: 1944-8007
    Topics: Geosciences , Physics
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  • 8
    Publication Date: 2013-07-26
    Description: Measurements were made of the hydraulic conductivity ( K ) of peat around a natural soil pipe in a blanket bog. This is the first investigation of decimetre-scale variability in both vertical K and horizontal K in blanket peats, which were found to be higher than indicated by previous research. This information suggests that it may be appropriate to reconsider (I) the spatial sampling strategies employed to investigate sub-surface flow in blanket peatlands, and (II) how field data are used to parameterise flow models. Critically, there was spatial structure in the heterogeneity, with a wedge of high- K peat directly above the pipe forming a hydrological conduit between near-surface peat and the perennially-flowing pipe. There was also significantly greater horizontal K parallel to the pipe's orientation compared with horizontal K perpendicular to the pipe. Determinations of the triaxial anisotropy of K , undertaken for the first time in peat soils, revealed substantial directional variations in K . The K around the pipe-peat interface was investigated; however, sample length dependency of K for peat samples precluded the investigation of a hypothesised low- K skin around the pipe.
    Print ISSN: 0043-1397
    Electronic ISSN: 1944-7973
    Topics: Architecture, Civil Engineering, Surveying , Geography
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 9
  • 10
    Publication Date: 2019-02-08
    Print ISSN: 0960-3115
    Electronic ISSN: 1572-9710
    Topics: Biology
    Published by Springer
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