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  • 1
    Keywords: Global environmental change--Congresses. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (220 pages)
    Edition: 1st ed.
    ISBN: 9783642190162
    Series Statement: Global Change - the IGBP Series
    DDC: 363.738/74
    Language: English
    Note: Global Change - The IGBP Series -- Challenges of a Changing Earth -- Copyright -- Preface -- Contents -- Contributors -- Part I Opening -- Chapter 1 Opening Address -- Chapter 2 Challenges of a Changing Earth -- Part II Achievements and Challenges -- Part IIa Food, Land, Water, and Oceans -- Chapter 3 Toward Integrated Land-Change Science: Advances in 1.5 Decades of Sustained International Research on Land-Use and Land-Cover Change -- Chapter 4 Climate Variability and Ocean Ecosystem Dynamics: Implications for Sustainability -- Chapter 5 Food in the 21st Century: Global Climate of Disparities -- Chapter 6 Equity Dimensions of Dam-Based Water Resources Development: Winners and Losers -- Part IIb Out of Breath: Air Quality in the 21st Century -- Chapter 7 Atmospheric Chemistry in the "Anthropocene -- Chapter 8 Fires, Haze and Acid Rain: The Social and Political Framework of Air Pollution in ASEAN and Asia -- Part IIc Managing Planetary Metabolism? The Global Carbon Cycle -- Chapter 9 Carbon and the Science-Policy Nexus: The Kyoto Challenge -- Chapter 10 Industry Response to the CO2 Challenge -- Part IId Summary: Global Change and the Challenge for the Future -- Chapter 11 Global Change and the Challenge for the Future -- Part III Advances in Understanding -- Part IIIa Global Biogeochemistry: Understanding the Metabolic System of the Planet -- Chapter 12 Ocean Biogeochemistry: A Sea of Change -- Chapter 13 The Past, Present and Future of Carbon on Land -- Chapter 14 Can New Institutions Solve Atmospheric Problems? Confronting Acid Rain, Ozone Depletion and Climate Change -- Part IIIb Land-Ocean Interactions: Regional-Global Linkages -- Chapter 15 Emissions from the Oceans to the Atmosphere, Deposition from the Atmosphere to the Oceans and the Interactions Between Them -- Chapter 16 The Impact of Dams on Fisheries: Case of the Three Gorges Dam. , Chapter 17 Global Change in the Coastal Zone: The Case of Southeast Asia -- Part IIIc The Climate System: Prediction, Change and Variability -- Chapter 18 Climate Change Fore and Aft: Where on Earth Are We Going? -- Chapter 19 Climate Change - Past, Present and Future: A Personal Perspective -- Chapter 20 The Changing Cryosphere: Impacts of Global Warming in the High Latitudes -- Chapter 21 The Coupled Climate System: Variability and Predictability -- Part IIId Hot Spots of Land-Use Change and the Climate System: A Regional or Global Concern? -- Chapter 22 Hot Spots of Land-Use Change and the Climate System: A Regional or Global Concern? -- Chapter 23 Africa: Greening of the Sahara -- Chapter 24 The Role of Large-Scale Vegetation and Land Use in the Water Cycle and Climate in Monsoon Asia -- Chapter 25 Can Human-Induced Land-Cover Change Modify the Monsoon System? -- Chapter 26 The Amazon Basin and Land-Cover Change: A Future in the Balance? -- Part IV Looking to the Future -- Part IVa Simulating and Observing the Earth System -- Chapter 27 Virtual Realities of the Past, Present and Future -- Chapter 28 Coping with Earth System Complexity and Irregularity -- Chapter 29 Simulating and Observing the Earth System: Summary -- Part IVb Does the Earth System Need Biodiversity? -- Chapter 30 Marine Biodiversity: Why We Need It in Earth System Science -- Chapter 31 Does Biodiversity Matter to Terrestrial Ecosystem Processes and Services? -- Chapter 32 Biodiversity Loss and the Maintenance of Our Life-Support System -- Part IVc Can Technology Spare the Planet? -- Chapter 33 Maglevs and the Vision of St. Hubert - Or the Great Restoration of Nature: Why and How -- Chapter 34 Industrial Transformation: Exploring System Change in Production and Consumption -- Chapter 35 Will Technology Spare the Planet? -- Part IVd Towards Global Sustainability. , Chapter 36 Challenges and Road Blocks for Local and Global Sustainability -- Chapter 37 Research Systems for a Transition Toward Sustainability -- Chapter 38 Summary: Towards Global Sustainability -- Part IVe Closing Session -- Chapter 39 Closing Address -- Chapter 40 The Amsterdam Declaration on Global Change -- Index.
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    Journal of industrial microbiology and biotechnology 6 (1990), S. 1-18 
    ISSN: 1476-5535
    Keywords: Microbody ; Glyoxysome ; Peroxisome ; Catalase ; Hydrocarbon ; Enzyme ; Fungal microbody ; Fungus
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Process Engineering, Biotechnology, Nutrition Technology
    Notes: Summary Microbodies are ubiquitous organelles in fungal cells, occurring in both vegetative hyphae and spores. They are bounded by a single membrane and may contain a crystalloid inclusion with subunits spaced at regular intervals. Typically, they contain catalase which reacts with the cytochemical stain 3,3′-diaminobenzidine to yield an electron-opaque product, urate oxidase,l-α-hydroxy acid oxidase andd-amino acid oxidase. Their fragility and the necessity to disrupt the tough fungal cell wall before isolating them make them difficult to isolate. Analysis of enzymes in purified or partially purified microbodies from fungi indicates that they participate in fatty acid degradation, the glyoxylate cycle, purine metabolism, methanol oxidation, assimilation of nitrogenous compounds, amine metabolism and oxalate synthesis. In organisms where microbodies are known to contain enzymes of the glyoxylate cycle, they are known as glyoxysomes; where they are known to contain peroxidatic activity, they are known as peroxisomes. In some cases microbodies contain enzymes for only a portion of a pathway or cycle. Thus, they must be involved in metabolic cooperation with other organelles, particularly mitochondria. The number, size and shape of microbodies in cells, their buoyant density and their enzyme contents may vary with the composition of the medium; their proliferation in cells is regulated by the growth environment. The isolation from the same organism of microbodies with different buoyant densities and different enzymes suggests strongly that more than one type of microbody can be formed by fungi.
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    Springer
    Journal of industrial microbiology and biotechnology 3 (1988), S. 111-117 
    ISSN: 1476-5535
    Keywords: Cladosporium resinae ; Microbody ; Catalase ; Spheroplast ; Hydrocarbon
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Process Engineering, Biotechnology, Nutrition Technology
    Notes: Summary Cells ofCladosporium resinae form greater numbers of microbodies when grown onn-alkanes than when grown on glucose. To facilitate isolation of microbodies, hydrocarbon-grown cells were spheroplasted. Of four spheroplasting agents and five osmotic supports examined, best results were obtained after a 4-h incubation with Novozym 234 plus chitinase and with 0.8 M sorbitol as osmotic support. Equal numbers of spheroplasts were obtained at pH 5.8 and at pH 7.0. Catalase was used as a marker for microbodies and cytochrome-c oxidase as a marker for mitochondria. Urate oxidase, a second marker for microbodies, was not detected in cell extracts. Microbodies were extremely fragile; of eight spheroplast disruption techniques attempted, the best yield of microbodies was obtained using a Teflon homogenizer for 5 min. Microbodies were partially purified by differential and density gradient centrifugation. Best results were obtained with discontinuous Percoll gradients which yielded a fraction enriched in microbodies and one enriched in mitochondria.
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    Springer
    Child psychiatry & human development 16 (1985), S. 67-76 
    ISSN: 1573-3327
    Source: Springer Online Journal Archives 1860-2000
    Topics: Medicine
    Notes: Abstract Twelve children between the ages of 14 and 23 months were observed in play group interactions during three different periods of the day. The results suggest that the dimension of time is an important factor in determining individual differences in the behavior of young children.
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    Springer
    Child psychiatry & human development 17 (1986), S. 88-94 
    ISSN: 1573-3327
    Source: Springer Online Journal Archives 1860-2000
    Topics: Medicine
    Notes: Abstract The relationship between maternal and caregiver assessments of temperament and measures of social initiative and solitary behavior was examined in a playgroup of twelve children between 14 and 23 months. Caregiver and maternal ratings of sociability failed to differentiate between those infants who were observed to be high or low in initiative. Instead caregiver ratings of sociability were most strongly related to the absence of social interaction, i.e., solitary behavior. Maternal ratings were more closely related to age and how the infant responded to others' initiations.
    Type of Medium: Electronic Resource
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  • 6
    Publication Date: 2020-12-02
    Description: At Integrated Ocean Drilling Program (IODP) Expedition 317 Site U1352, east of the South Island New Zealand, we continuously cored a 1927-m-thick Holocene-to-Eocene section where we can uniquely document downhole changes in induration and lithification in siliciclastic to calcareous fine-grained sediment using a wide range of petrological, physical-property, and geochemical data sets. Porosity decreases from around 50% at the surface to 5–10% at the base of the deepest hole, with a corresponding increase in density from ∼ 2 to ∼ 2.5 g cm3. There are progressive bulk mineral changes with depth, including an increase in carbonate and decrease in quartz and clay content. Grain compaction is first seen in thin section at 347 m below sea floor and intensifies downhole. Pressure solution (chemical compaction) begins at 380 m and is common below 1440 m, with stylolite development below 1600 m, and sediment injection features below 1680 m. Porewater geochemistry and petrographic observations document two active zones of cementation, one shallow (eogenetic) down to ∼ 50 m, as evidenced by micritic nodules and pore-water geochemistry driven by methane oxidation by sulfate, and another burial-related cementation zone (mesogenetic) starting at ∼ 300 m. A transitional zone occurs between 50 and 300 m. Our results quantify downhole diagenetic changes and verify depth estimates for these processes inferred from outcrop studies, and provide an actualistic example of cementation and compaction trends in a slope setting.
    Description: Published
    Description: 272–287
    Description: 5A. Paleoclima e ricerche polari
    Description: JCR Journal
    Keywords: 04.04. Geology
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 7
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