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  • 1
    Online Resource
    Online Resource
    San Diego :Elsevier Science & Technology,
    Keywords: Biogeochemistry. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (689 pages)
    Edition: 3rd ed.
    ISBN: 9780123858757
    DDC: 577.14
    Language: English
    Note: Front Cover -- Biogeochemistry: An Analysis of Global Change -- Copyright -- Dedication -- Contents -- Preface -- Acknowledgments -- Biogeochemistry -- Part I: Processes and Reactions -- Chapter 1: Introduction -- What is biogeochemistry? -- Understanding the earth as a chemical system -- Scales of endeavor -- Thermodynamics -- Stoichiometry -- Large-Scale Experiments -- Models -- Lovelock's gaia -- Recommended Readings -- Chapter 2: Origins -- Introduction -- Origins of the Elements -- Origin of the solar system and the solid earth -- Origin of the atmosphere and the oceans -- Origin of life -- Evolution of metabolic pathways -- Photosynthesis: The Origin of Oxygen on Earth -- Chemoautotrophy -- Anaerobic Respiration -- Comparative planetary history: earth, mars, and venus -- Summary -- Recommended Readings -- Chapter 3: The Atmosphere -- Introduction -- Structure and Circulation -- Atmospheric Composition -- Gases -- Aerosols -- Biogeochemical Reactions in the Troposphere -- Major Constituents-Nitrogen and Oxygen -- Carbon Dioxide -- Trace Biogenic Gases -- Atmospheric Deposition -- Processes -- Regional Patterns and Trends -- Biogeochemical Reactions in the Stratosphere -- Ozone -- Stratospheric Sulfur Compounds -- Models of the Atmosphere and Global Climate -- Summary -- Recommended Readings -- Chapter 4: The Lithosphere -- Introduction -- Rock weathering -- Chemical Weathering -- Secondary Minerals -- Soil chemical reactions -- Cation Exchange Capacity -- Soil Buffering -- Anion Adsorption Capacity -- Phosphorus Minerals -- Soil development -- Forests -- Grasslands -- Deserts -- Models of Soil Development -- Weathering rates -- Chemical Weathering Rates -- Mechanical Weathering -- Total Denudation Rates -- Summary -- Recommended Readings -- Chapter 5: The Biosphere -- Introduction -- Photosynthesis -- Water-Use Efficiency. , Nutrient-Use Efficiency -- Respiration -- Net Primary Production -- Measurement and Allocation of NPP -- Net Ecosystem Production and Eddy-Covariance Studies -- The Fate of Net Primary Production -- Remote Sensing of Primary Production and Biomass -- Global Estimates of Net Primary Production and Biomass -- Net Primary Production and Global Change -- Detritus -- The Decomposition Process -- Humus Formation and Soil Organic Matter -- Turnover -- Soil Organic Matter and Global Change -- Summary -- Recommended Readings -- Chapter 6: The Biosphere -- Introduction -- Biogeochemical cycling in land plants -- Nutrient Uptake -- Nutrient Balance -- Nitrogen Assimilation -- Nitrogen Fixation -- Mycorrhizal Fungi -- Nutrient allocations and cycling in land vegetation -- The Annual Intrasystem Cycle -- Litterfall -- Mass Balance of the Intrasystem Cycle -- Nutrient Use Efficiency -- Biogeochemical cycling in the soil -- Soil Microbial Biomass and the Decomposition Process -- Nitrogen Cycling -- Emission of Nitrogen Gases from Soils -- Soil Phosphorus Cycling -- Sulfur Cycling -- Transformations in Fire -- The Role of Animals -- Calculating landscape mass balance -- Human impacts on terrestrial biogeochemistry -- Acid Rain -- Nitrogen Saturation -- Rising CO2 and Global Warming -- Summary -- Recommended Readings -- Chapter 7: Wetland Ecosystems -- Introduction -- Types of wetlands -- Wetland Hydrology -- Wetland Soils -- Wetland Vegetation -- Productivity in wetland ecosystems -- Organic matter storage in wetlands -- Microbial metabolism in saturated sediments -- Free Energy Calculation -- Measuring the Redox Potential of the Environment -- Anaerobic metabolic pathways -- Fermentation -- Dissimilatory Nitrate Reduction -- Iron and Manganese Reduction -- Sulfate Reduction -- Methanogenesis -- Aerobic Oxidation of CH4 -- Anaerobic Oxidation of CH4. , Microbial Consortia -- Wetlands and water quality -- Wetlands and global change -- Global Wetland Loss -- Sea Level Rise and Saltwater Intrusion -- Rising Temperatures -- Elevated CO2 -- Summary -- Recommended Readings -- Chapter 8: Inland Waters -- Introduction -- Special Properties of Water -- Gas Diffusion and Solubility -- Terrestrial-Aquatic Linkages -- Hydrologic Flowpaths -- Ion Chemistry -- Organic Subsidies -- Unique Features of Aquatic Food Webs -- Lakes -- Lake Water Budgets and Mixing -- Trophic Status of Lakes -- Carbon Cycling in Lakes -- Primary Production in Lakes -- Measuring Primary Productivity -- Nutrient Limitation of Lake NPP -- Micronutrient Limitation -- Light Limitation of NPP -- Herbivore Control of NPP -- The Fate of Organic Carbon in Lakes -- Carbon Export from Lakes -- Nutrient Cycling in Lakes -- Nitrogen Cycling in Lakes -- Lake Phosphorus Cycling -- Sulfur Cycling in Lakes -- Rivers -- River Water Budgets and Mixing -- Carbon Cycling in Rivers -- New Inputs of C-Primary Productivity in Rivers -- Limits to Autochthonous Production in Flowing Waters -- Carbon Budgets for Rivers -- Nutrient Spiraling in Rivers -- River Nitrogen Cycling -- River Phosphorus Cycling -- Estuaries -- Estuarine Water Budgets and Mixing -- Carbon Cycling in Estuaries -- Primary Production in Estuaries -- Nutrient Cycling in Estuaries -- Estuarine Phosphorus Cycling -- Anaerobic Metabolism in Estuarine Sediments -- Human impacts on inland waters -- Water Infrastructure -- Eutrophication -- Global Climate Change -- Summary -- Recommended Readings -- Chapter 9: The Oceans -- Introduction -- Ocean circulation -- Global Patterns -- El Niño -- The composition of seawater -- Major Ions -- Net primary production -- Measurement -- Global Patterns and Estimates -- Dissolved Organic Matter -- Fate of Marine Net Primary Production -- Sediment diagenesis. , Organic Diagenesis -- Biogenic Carbonates -- The biological pump: a model of carbon cycling in the ocean -- Nutrient cycling in the ocean -- Internal Cycles -- Air-Sea Exchange of Nitrogen -- External Inputs -- Gaseous Losses of Nitrogen from the Sea -- A Global Budget for Nitrogen in the Oceans -- Phosphorus -- Human Perturbations of Marine Nutrient Cycling -- Silicon, Iron, and Trace Metals -- Biogeochemistry of hydrothermal vent communities -- The marine sulfur cycle -- The sedimentary record of biogeochemistry -- Summary -- Recommended Readings -- Part II: Global Cycles -- Chapter 10: The Global Water Cycle -- Introduction -- The global water cycle -- Models of the hydrologic cycle -- The history of the water cycle -- The water cycle and climate change -- Rise in Sea Level -- Sea Ice -- Terrestrial Water Balance -- Summary -- Recommended Readings -- Chapter 11: The Global Carbon Cycle -- Introduction -- The modern carbon cycle -- Temporal perspectives on the carbon cycle -- Atmospheric methane -- Carbon monoxide -- Synthesis: linking the carbon and oxygen cycles -- Summary -- Recommended Readings -- Chapter 12: The Global Cycles of Nitrogen and Phosphorus -- Introduction -- The global nitrogen cycle -- Land -- Sea -- Temporal variations in the global nitrogen cycle -- Nitrous oxide -- The global phosphorus cycle -- Linking global biogeochemical cycles -- Summary -- Recommended Readings -- Chapter 13: The Global Cycles of Sulfur and Mercury -- Introduction -- The global sulfur cycle -- Temporal Perspectives on the Global Sulfur Cycle -- The Atmospheric Budget of Carbonyl Sulfide -- The global mercury cycle -- Summary -- Recommended Reading -- Chapter 14: Perspectives -- Recommended Reading -- Reference -- Index.
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    American Association for the Advancement of Science (AAAS)
    In: Science
    Publication Date: 2018-03-23
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Geosciences , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 5
    Publication Date: 2018-11-15
    Description: Limiting climate warming to 〈2°C requires increased mitigation efforts, including land stewardship, whose potential in the United States is poorly understood. We quantified the potential of natural climate solutions (NCS)—21 conservation, restoration, and improved land management interventions on natural and agricultural lands—to increase carbon storage and avoid greenhouse gas emissions in the United States. We found a maximum potential of 1.2 (0.9 to 1.6) Pg CO 2 e year –1 , the equivalent of 21% of current net annual emissions of the United States. At current carbon market prices (USD 10 per Mg CO 2 e), 299 Tg CO 2 e year –1 could be achieved. NCS would also provide air and water filtration, flood control, soil health, wildlife habitat, and climate resilience benefits.
    Electronic ISSN: 2375-2548
    Topics: Natural Sciences in General
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  • 6
    Publication Date: 2013-02-06
    Description: Human mobilization and use of reactive nitrogen (Nr) has been one of the major aspects of global change over the past century. Nowhere has that change been more dramatic than in China, where annual net Nr creation increased from 9.2 to 56 Tg from 1910 to 2010. Since 1956, anthropogenic...
    Print ISSN: 0027-8424
    Electronic ISSN: 1091-6490
    Topics: Biology , Medicine , Natural Sciences in General
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  • 7
    Electronic Resource
    Electronic Resource
    Palo Alto, Calif. : Annual Reviews
    Annual Review of Ecology, Evolution, and Systematics 8 (1977), S. 51-81 
    ISSN: 0066-4162
    Source: Annual Reviews Electronic Back Volume Collection 1932-2001ff
    Topics: Biology
    Type of Medium: Electronic Resource
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  • 8
    ISSN: 1432-1939
    Keywords: Biomass allocation ; Climate change CO2 enhancement ; Photosynthesis ; Relative growth rate
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract Increases in the concentration of atmospheric carbon dioxide may have a fertilizing effect on plant growth by increasing photosynthetic rates and therefore may offset potential growth decreases caused by the stress associated with higher temperatures and lower precipitation. However, plant growth is determined both by rates of net photosynthesis and by proportional allocation of fixed carbon to autotrophic tissue and heterotrophic tissue. Although CO2 fertilization may enhance growth by increasing leaf-level assimilation rates, reallocation of biomass from leaves to stems and roots in response to higher concentrations of CO2 and higher temperatures may reduce whole-plant assimilation and offset photosynthetic gains. We measured growth parameters, photosynthesis, respiration, and biomass allocation of Pinus ponderosa seedlings grown for 2 months in 2×2 factorial treatments of 350 or 650μ bar CO2 and 10/25° C or 15/30° C night/day temperatures. After 1 month in treatment conditions, total seedling biomass was higher in elevated CO2, and temperature significantly enhanced the positive CO2 effect. However, after 2 months the effect of CO2 on total biomass decreased and relative growth rates did not differ among CO2 and temperature treatments over the 2-month growth period even though photosynthetic rates increased ≈7% in high CO2 treatments and decreased ≈10% in high temperature treatments. Additionally, CO2 enhancement decreased root respiration and high temperatures increased shoot respiration. Based on CO2 exchange rates, CO2 fertilization should have increased relative growth rates (RGR) and high temperatures should have decreased RGR. Higher photosynthetic rates caused by CO2 fertilization appear to have been mitigated during the second month of exposure to treatment conditions by a ≈3% decrease in allocation of biomass to leaves and a ≈9% increase in root:shoot ratio. It was not clear why diminished photosynthetic rates and increased respiration rates at high temperatures did not result in lower RGR. Significant diametrical and potentially compensatory responses of CO2 exchange and biomass allocation and the lack of differences in RGR of ponderosa pine after 2 months of exposure of high CO2 indicate that the effects of CO2 fertilization and temperature on whole-plant growth are determined by complex shifts in biomass allocation and gas exchange that may, for some species, maintain constant growth rates as climate and atmospheric CO2 concentrations change. These complex responses must be considered together to predict plant growth reactions to global atmospheric change, and the potential of forest ecosystems to sequester larger amounts of carbon in the future.
    Type of Medium: Electronic Resource
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  • 9
    ISSN: 1432-1939
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Summary The effects of irradiance during growth on biomass allocation, growth rates, leaf chlorophyll and protein contents, and on gas exchange responses to irradiance and CO2 partial pressures of the evergreen, sclerophyllous, chaparral shrub, Ceanothus megacarpus were determined. Plants were grown at 4 irradiances for the growth experiments, 8, 17, 25, 41 nE cm-2 sec-1, and at 2 irradiances, 9 and 50 nE cm-2 sec-1, for the other comparisons. At higher irradiances root/shoot ratios were somewhat greater and specific leaf weights were much greater, while leaf area ratios were much lower and leaf weight ratios were slightly lower than at lower irradiances. Relative growth rates increased with increasing irradiance up to 25 nE cm-2 sec-1 and then leveled off, while unit leaf area rates increased steeply and unit leaf weight rates increased more gradually up to the highest growth irradiance. Leaves grown at 9 nE cm-2 sec-1 had less total chlorophyll per unit leaf area and more per unit leaf weight than those grown at 50 nE cm-2 sec-1. In a reverse of what is commonly found, low irradiance grown leaves had significantly higher chlorophyll a/b than high irradiance grown leaves. High irradiance grown leaves had much more total soluble protein per unit leaf area and per unit dry weight, and they had much higher soluble protein/chlorophyll than low irradiance grown leaves. High irradiance grown leaves had higher rates of respiration in very dim light, required higher irradiances for photosynthetic saturation and had higher irradiance saturated rates of photosynthesis than low irradiance grown leaves. CO2 compensation irradiances for leaves of both treatments were very low, 〈5 nE cm-2 sec-1. Leaves grown under low and those grown under high irradiances reached 95% of their saturated photosynthetic rates at 65 and 85 nE cm-2 sec-1, respectively. Irradiance saturated rates of photosynthesis were high compared to other chaparral shrubs, 1.3 for low and 1.9 nmol CO2 cm-2 sec-1 for high irradiance grown leaves. A very unusual finding was that leaf conductances to H2O were significantly lower in the high irradiance grown leaves than in the low irradiance grown leaves. This, plus the differences in photosynthetic rates, resulted in higher water use efficiencies by the high irradiance grown leaves. High irradiance grown leaves had higher rates of photosynthesis at any particular intercellular CO2 partial pressure and also responded more steeply to increasing CO2 partial pressure than did low irradiance grown leaves. Leaves from both treatments showed reduced photosynthetic capability after being subjected to low CO2 partial pressures (≃100 μbars) under high irradiances. This treatment was more detrimental to leaves grown under low irradiances. The ecological implications of these findings are discussed in terms of chaparral shrub community structure. We suggest that light availability may be an important determinant of chaparral community structure through its effects on water use efficiencies rather than on net carbon gain.
    Type of Medium: Electronic Resource
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