Marine geochemistry [Libro electrónico] / editores: Horst D. Schulz, Matthias Zabel
Schulz, Horst D [editor] | Zabel, Matthias [editor/a].
Tipo de material: Libro en línea Editor: New York, New York, United States: Springer, c2000Descripción: xx, 455 páginas : ilustraciones mapas ; 28 centímetros.ISBN: 354066453X; 9783662042441 (Print); 9783662042427 (Online).Tema(s): Chemical oceanography | Marine sediments | GeochemistryNota de acceso: Disponible para usuarios de ECOSUR con su clave de acceso Nota de bibliografía: Incluye bibliografía e índice: páginas 443-455 Número de sistema: 56470Contenidos:Mostrar Resumen:Tipo de ítem | Biblioteca actual | Colección | Signatura | Estado | Fecha de vencimiento | Código de barras |
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Libros | Biblioteca Electrónica Recursos en línea (RE) | Acervo General | Recurso digital | ECO400564707337 |
Incluye bibliografía e índice: páginas 443-455
1. The solid phase of marine sediments.. 2. Geophysical properties in marine sediments.. 3. Quantification of early diagenesis: dissolved constituents in marine pore water.. 4. Organic matter: the driving force for early diagenesis.. 5. Bacteria and marine biogeochemistry.. 6. Early diagenesis at the benthic boundary layer: oxygen and nitrate in marine sediments.. 7. The reactivity of iron.. 8. Sulfate reduction in marine sediments.. 9. Marine carbonates: their formation and destruction.. 10. Influence of geochemical processes on stable isotope distribution in marine sediments.. 11. Manganese: predominant role of nodules and crusts.. 12. Back to the ocean cycles: benthic fluxes and their distribution patterns.. 13. Input from the deep: hot vents and cold seeps.. 14. Conceptual models and computer models.. Index
Disponible para usuarios de ECOSUR con su clave de acceso
Since 1980 a considerable amount of scientific research dealing with geochemical processes in marine sediments has been carried out. This textbook summarizes the state of the art in this field of research. The topics comprise the examination of sedimentological and physical properties of the sedimentary solid phase, of pore water and pore water constituents, organic matter as the driving force of most microbiological processes, biotic and abiotic redox reactions, carbonates and stable isotopes as proxies for paleoclimate reconstruction, metal enrichments in ferromanganese nodules and crusts as well as in hot vents and cold seeps on the seafloor. A new chapter describes properties, occurrence and formation of gas hydrates in marine sediments. The textbook ends with a chapter on model conceptions and computer models to quantify processes of early diagenesis. eng
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