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  • 1
    Online-Ressource
    Online-Ressource
    Princeton, NJ : Princeton University Press
    Schlagwort(e): Geochemistry ; Marine sediments ; SCIENCE / Earth Sciences / Oceanography
    Beschreibung / Inhaltsverzeichnis: Frontmatter -- Contents -- Preface -- Common Abbreviations and Symbols -- CHAPTER ONE Introduction -- CHAPTER TWO The Components of Marine Sediments -- CHAPTER THREE Isotope Geochemistry -- CHAPTER FOUR Physical Properties of Sediments -- CHAPTER FIVE An Introduction to Transport Processes in Sediments -- CHAPTER SIX Models of Sediment Diagenesis -- CHAPTER SEVEN Biogeochemical Processes in Sediments -- CHAPTER EIGHT Quantifying Carbon and Nutrient Remineralization in Sediments -- CHAPTER NINE An Introduction to the Organic Geochemistry of Marine Sediments -- CHAPTER TEN Dissolved Organic Matter in Marine Sediments -- CHAPTER ELEVEN Linking Sediment Organic Geochemistry and Sediment Diagenesis -- CHAPTER TWELVE Processes at the Sediment-Water Interface -- CHAPTER THIRTEEN Biogeochemical Processes in Pelagic (Deep-Sea) Sediments -- CHAPTER FOURTEEN Nonsteady-State Processes in Marine Sediments -- CHAPTER FIFTEEN The Controls on Organic Carbon Preservation in Marine Sediments -- CHAPTER SIXTEEN Biogeochemical Processes in Continental Margin Sediments -- CHAPTER SEVENTEEN Biogeochemical Processes in Continental Margin Sediments -- CHAPTER EIGHTEEN Linking Sediment Processes to Global Elemental Cycles: Authigenic Clay Mineral Formation and Reverse Weathering -- Appendix Some of the Field Sites Discussed in the Text -- References -- Index
    Materialart: Online-Ressource
    Seiten: 1 Online-Ressource (624 p) , 33 halftones. 75 line illus. 33 tables
    Ausgabe: 1. Auflage
    ISBN: 9780691216096
    Sprache: Englisch
    Anmerkung: Mode of access: Internet via World Wide Web. , In English
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 2
    Buch
    Buch
    Princeton : Princeton University Press
    Schlagwort(e): Marine sediments ; Geochemistry ; Lehrbuch ; Geochemie ; Meeressediment ; Geochemie ; Meeressediment ; Biogeochemie ; Hydrogeochemie ; Isotopengeochemie ; Organische Geochemie ; Meeresgeologie
    Materialart: Buch
    Seiten: xviii, 609 Seiten , Diagramme
    ISBN: 069109506X , 9780691095066
    DDC: 551.4686
    RVK:
    RVK:
    Sprache: Englisch
    Anmerkung: Literaturverzeichnis: Seiten 521-592
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 3
    ISSN: 1573-515X
    Schlagwort(e): amino acids ; ammonium production ; coastal marine sediments ; anoxic ; sulfate reduction
    Quelle: Springer Online Journal Archives 1860-2000
    Thema: Chemie und Pharmazie , Geologie und Paläontologie
    Notizen: Abstract In sediment slurry experiments with anoxic marine sediments collected in Cape Lookout Bight, NC, and a site in mid-Chesapeake Bay, the rates of sulfate reduction and ammonium production decrease with increasing dilution of sediment with oxygen-free sea-water. The effect of sediment dilution on the rates of these processes can be described by a simple mathematical relationship, and when these rates are corrected for sediment dilution they yield values which agree well with direct measurements of these processes. In sediment slurry studies of amino acid utilization in Cape Lookout Bight sediments, the fermentative decarboxylation of glutamic acid (to γ-aminobutyric acid) or aspartic acid (to alanine or β-alanine) did not occur when either of these amino acids were added to Cape Lookout Bight slurries. The addition of glutamic acid did however lead to a small (∼1) transient build-up of β-aminoglutaric acid. Measured rates of glutamic acid uptake in these slurries also decreased with increasing sediment dilution. Molybdate inhibition experiments demonstrated that dissolved free amino acids represent 1–3% of the carbon sources/electron donors used for sulfate reduction in Cape Lookout Bight sediments. The direct oxidation of amino acids by sulfate reducing bacteria also accounts for 13–20% of the total ammonium produced. Glutamic acid, alanine, β-aminoglutaric acid, aspartic acid and asparagine are the major amino acids oxidized by sulfate reducing bacteria in Cape Lookout Bight sediments.
    Materialart: Digitale Medien
    Standort Signatur Einschränkungen Verfügbarkeit
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