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  • 1
    Monograph available for loan
    Monograph available for loan
    Boca Raton, Florida : CRC Press
    Call number: AWI G6-94-0192
    Description / Table of Contents: T ABLE OF CONTENTS: Chapter 1Introduction. - I. A Historical Overview of Nitrogen Study in the Sea. - A. Determination of Nitrogenaus Compounds in the Sea. - B. Biological Transformation of Nitrogen. - C. Stoichiometric Model of Organic Matter Mineralization. - D. Natural 15N Abundance. - lI. The Nitrogen Cycle. - Chapter 2 Physicochemical Properties of Nitrogen. - I. Properties of the Nitrogen Atom and Bonding. - lI. Thermodynamic Functions of Nitrogen. - III. Biogeochemical Sketch of Nitrogen. - Chapter 3 Nitrogen Isotopes. - I. Genesis of Isotopes of Light Elements. - II. Isotope Abundance and Fractionation. - III. Isotopic Exchange Reactions. - IV. Kinetic Isotope Effects. - V. Overall Isotopic Fractionation. - A. One-Step Reaction. - B. Unidirectional Two-Step Reaction at a Steady State. - C. Two-Step Reaction with a Reversible First Step at a Steady State. - D. Three-Step Reactions. - E. Multistep Reactions. - VI. Isotopic Exchange Equilibria of Nitrogen. - VII. Nitrogen Kinetic Isotope Effects During Nitrate Reduction. - A. Chemical Systems. - B. Biological Systems. - VIII. Isotope Fractionation in Branched Reactions and its Ecological Significance. - IX. Isotope Mass Balance in Marine Ecosystems. - A. Two-Source Model. - B. Three-Source Model. - Chapter 4 Components, Systems, and Processes. - I. Nitrogenous Compounds in the Sea: Abundance, Sources, and Sink. - lI. Physical Factors. - A. Water Movement and Mixing of Water. - B. Solar Radiation. - C. Effects of Temperature and Pressure on Chemical and Biochemical Reactions. - 1. Case 1: k2〉〉k3. - 2. Case 2: k3〉〉k2. - D. Nitrogen Supply by River Runoff and Precipitation. - III. Chemical Factors. - A. Chemical Behavior of Nitrogenaus Compounds in the Sea. - B. Hydrogen Ion Concentration. - C. Oxidation-Reduction Potential. - IV. Biochemical Processes. - A. Nitrogen Uptake and Assimilation. - B. Mineralization. - C. Nitrification. - D. Nitrate Respiration and Denitrification. - E. N2 Fixation. - Chapter 5 Abundance and Distribution of Nitrogen in the Sea and Their Physical, Chemical, and Biochemical Regulation. - I. Roles of the Ocean in the Global Nitrogen Cycle. - A. The Buildup of the Biogeochemical Cycle. - B. Nitrogen Inventories. - C. Nitrogen Budgets. - lI. Dissolved Nitrogen Gas. - A. Atmospheric Pressure. - B. Occlusion of Air Bubbles. - C. Effect of Mixing of Different Water Masses. - D. Biological Effects. - III. Ammonium, Nitrite, and Nitrate. - A. Distribution of Ammonium. - B. Distribution of Nitrite. - C. Distribution of Nitrate. - IV. Nitrous Oxide. - V. Urea. - VI. Other Nitrogenous Compounds in a Water Column. - VII. Nitrogen Uptake by Phytoplankton. - VIII. Mechanism of Formation of the Primary Nitrite Maximum. - A. Nitrification in the Sea. - B. Nitrite Production from Nitrate by Microalgae. - C. Nitrite Assimilation. - D. Formation of the Primary Nitrite Maximum. - Chapter 6 Nitrogen Dynamics in Various Oceanic Systems. - I. High Latitudinal Areas Rich in Nitrate. - II. Oligotrophic Areas. - A. Kuroshio Area. - B. Anticyclonic Gyre Off Shikoku. - Ill. Subtropical and Tropical Areas with Supply of Nitrate. - A. Upwelling Region. - B. Regional Upwelling. - l. The Frontal Margin of Oceanic Currents. - 2. Oceanic Eddy. - 3. Vortex Motion Around Islands. - IV. Sea Areas Where Nitrogen Fixation Occurs. - A. Trichodesmium Ecosystems. - B. Local Ecosystems Characterized by N2 Fixation. - 1. Coral Reefs. - 2. Seagrass Meadows and Salt Marshes. - V. Subsurface Ecosystems. - A. Decomposition of Organic Matter in the Subsurface Water. - B. Nitrogen Diagenesis in Sediments. - VI. Sea Areas Where Denitrification Occurs. - A. Denitrification in the Subsurface Water. - 1. Eastern Tropical North Pacific. - B. Marine Sediments. - 1. Coastal Sediments. - 2. Pelagic Sediment. - VII. Near Shore and Estuarine Systems. - A. Flooded Soil Ecosystems. - B. Tokyo Bay. - Chapter 7 Variation of 15N/14N in Nitrogen Cycling and Its Significance in Marine Environments. - I. Isotope Fractionation in the Nitrogen Cycle. - A. Isotope Exchange Reactions. - B. Fractionation in Biological Metabolic Processes. - II. Distribution of 15N in Nature. - A. General Patterns of 15N Distribution. - B. 15N in Antarctica. - C. 15N Abundance and the Biogeochemical Cycle. - D. [Delta]15N of Plants and Their Nitrogen Sources. - 1. Exchange-Reaction-Controlled Ecosystems. - 2. Enzyme-Controlled Ecosystems. - 3. Kinetically Controlled Ecosystems. - 4. Substrate-Controlled Ecosystems. - III. Integrated Nitrogen Isotope Fractionation in Ecosystems. - A. Enrichment of 15N in a Feeding Process. - B. [Delta]15N-[Delta]13C Relationships. - IV. Marine Ecosystems. - A. Phytoplankton and Particulate Organic Matter. - 1. Regional Characteristics of 15N Abundance of Phytoplankton. - 2. A Case Study in the Boreal Area. - 3. Geographical Variation of 15N Abundance in POM. - B. The Area Characterized by N2 Fixation. - C. Isotope Biogeochemistry of the Antarctic Ecosystem. - D. Denitrification in the Marine Aquatic System as lnvestigated Based on 15N Abundance Data. - E. 15N and 13C Abundance in River, Estuarine, and Coastal Areas. - 1. 15N and 13C Distribution in the Otsuchi River Watershed. - 2. Origin of Organic Matter in Bay Sediments. - F. Seabird Rockeries. - G. The Deep-Sea World. - H. Animal Behavior. - Chapter 8 Future Studies on Nitrogen Dynamics. - I. Human Impingement on the Nitrogen Cycle in Marine Systems. - A. Long-Term Effects. - B. Short-Term Effects. - II. A New Paradigm. - A. Isotope Biogeochemistry. - B. From Components to Systems. - References.
    Type of Medium: Monograph available for loan
    Pages: 208 S. : graph. Darst. ; 25 cm
    ISBN: 0849362733
    Branch Library: AWI Library
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  • 2
    Electronic Resource
    Electronic Resource
    s.l. : American Chemical Society
    Biochemistry 4 (1965), S. 1213-1225 
    ISSN: 1520-4995
    Source: ACS Legacy Archives
    Topics: Biology , Chemistry and Pharmacology
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    s.l. : American Chemical Society
    Biochemistry 4 (1965), S. 1225-1238 
    ISSN: 1520-4995
    Source: ACS Legacy Archives
    Topics: Biology , Chemistry and Pharmacology
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 307 (1984), S. 442-444 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Fig. 1 The device used for extraction and collection of dissolved N2O from seawater samples. Approximately 1001 of sea water was introduced into a stainless steel tank (T, 150 1 in volume), which had been filled with Ar. The gas above the sample water was circulated by the aid of a pump (P) ...
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 283 (1980), S. 752-754 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Williams and Gordon4 have investigated 13C abundances in suspended particulate organic carbon (POC) collected from the eastern North Pacific, between 10 and 2,940 m, the 513C values fell in the narrow range -22.0 to -24.3 They suggested that most of the suspended POC is biologically refractory. A ...
    Type of Medium: Electronic Resource
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  • 6
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] During a cruise (August-September 1983) of the RV Hakuho Mam in the western North Pacific Ocean we collected seawater samples at depths ranging from the surface to 4,800 m at Station C (45°09'N, 160° 18'E) and from the surface to 4,000m at Station E (28° 06' N, ...
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    Springer
    Archives of microbiology 117 (1978), S. 17-20 
    ISSN: 1432-072X
    Keywords: Blue-green algae ; ATP pool ; Glutamine synthesis ; Ammonia assimilation
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract When N2-grown cells ofAnabaena cylindrica were exposed to ammonia (50 μM to 5 mM) in the dark, the size of the ATP pool was reduced by 40% within 1 min, but restored after 5 or 6 min. The decrease in ATP was accompanied by increases in ADP and AMP, while the total adenylate content remained unaltered. The ammonia-induced change in the ATP pool was completely eliminated when algal cells were treated withl-methionine-dl-sulfoximine, an inhibitor of glutamine synthesis. These results suggest that ammonia is rapidly assimilated through the pathway mediated by glutamine synthetase accompanied by reduction of the ATP pool.
    Type of Medium: Electronic Resource
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  • 8
    ISSN: 1573-868X
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Water plumes, 20 km long or less, identified by low temperature, high salinity and high nutrient concentrations, were observed on the eastern side of Izu Islands where the Kuroshio Current or its branch flowed eastward. The T-S diagrams and the vertical profiles of oceanographic variables indicated that the water plumes resulted from the upwelling of subsurface water. A newly formed plume, characterized by a sharp temperature front and high nutrient concentrations, contained less chlorophyll than did old plumes. It is suggested that the upwelling plumes are maintained for a period long enough to allow luxuriant growth of phytoplankton.
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    Springer
    Journal of oceanography 42 (1986), S. 241-254 
    ISSN: 1573-868X
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Phosphorus dynamics in Tokyo Bay waters were investigated along with other oceanographic variables. Seasonal variations of dissolved inorganic phosphorus (DIP) and particulate phosphorus (PP) are inversely correlated with each other, and reflect variation in biological activity. A high concentration of PP in summer surface waters is caused by high primary production. The PP settled in the deeper layer is decomposed, and orthophosphate is regenerated within the water column and in sediments. Even during summer stratification period, the regenerated orthophosphate is occasionally advected upward by wind-induced water mixing and contributes to phytoplankton growth in the upper layer. Some dissolved organic phosphorus is producedin situ from PP, but it may be rapidly decomposed in the water column. The ratios of C∶chlorophylla and C∶N in particulate matter suggest that phytoplankton in the summer surface waters of Tokyo Bay are limited neither by nitrogen nor by phosphorus. The P∶N ratio in particulate matter varies substantially but it is positively correlated with the ambient concentration of DIP. Phytoplankton take up and store phosphorus within their cells when ambient DIP exceeds their demand. An abundance of total phosphorus in the summer water column can be attributed to increased discharge of river waters, although enhanced release of orthophosphate from anoxic sediments cannot be discounted.
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  • 10
    ISSN: 1573-868X
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract A simple procedure for fractionation of phosphorus components in natural populations of phytoplankton has been developed. By a combination of a trichloroacetic acid (TCA) extraction, a hot dilute acid treatment, a charcoal treatment and an organic solvent extraction, cellular phosphorus was divided into orthophosphate, nucleotide phosphorus, sugar phosphates, acid-soluble polyphosphates, lipid phosphorus, nucleic acid phosphorus, acid-insoluble polyphosphates, and residual phosphorus. The recovery of phosphorus was 94±5%. This technique was applied to natural populations of phytoplankton in summer surface waters of Tokyo Bay. Nucleic acid phosphorus and orthophosphate were most abundant, and accounted for 30 to 50% of total phytoplankton phosphorus. The nucleic acid phosphorus was proportional to the biomass of phytoplankton, irrespective of ambient nutrient concentrations. The orthophosphate showed the largest change in association with the change in cellular phosphorus content as well as in ambient phosphate. The orthophosphate serves as a phosphorus reserve in the natural populations of phytoplankton in summer surface waters of Tokyo Bay whereSkeletonema costatum was dominant. Acid-insoluble polyphosphates tended to increase when ambient concentration of phosphate was high, but their amounts were almost one order of magnitude lower than that of orthophosphate.
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