
Hydrothermal Circulation and Seawater Chemistry
Links and Feedbacks
- English
- ePUB (mobile friendly)
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Hydrothermal Circulation and Seawater Chemistry
Links and Feedbacks
About this book
GEOPHYSICAL MONOGRAPH SERIES
Hydrothermal Circulation and Seawater Chemistry
Links and Feedbacks
The chemical exchange between seawater and the underlying ocean crust occurs at temperatures ranging from about 2°C on the seafloor to more than 500°C deep in the crust. These hydrothermal reactions strongly influence the chemical composition of seawater and, in turn, seawater chemistry impacts hydrothermal exchange; these feedbacks play a crucial role in the Earth system.
Hydrothermal Circulation and Seawater Chemistry: Links and Feedbacks explores on- and off-axis hydrothermal systems and their effects on ocean chemistry and the Earth system.
Volume highlights include:
- Hydrothermal fluxes dependent on boundary conditions such as climate and sedimentation history
- Low-temperature, off-axis systems that have large fluxes of elements
- Observational and experimental perspectives of on-axis hydrothermal processes
- Methods for tracking hydrothermal and oceanic processes using sediments or isotope proxies
- The role of oceanic hydrothermal systems in planetary-scale cycles on Earth and beyond
The American Geophysical Union promotes discovery in Earth and space science for the benefit of humanity. Its publications disseminate scientific knowledge and provide resources for researchers, students, and professionals.
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Information
Table of contents
- COVER
- TABLE OF CONTENTS
- GEOPHYSICAL MONOGRAPH SERIES
- TITLE PAGE
- COPYRIGHT
- LIST OF CONTRIBUTORS
- PREFACE
- 1 A Brief Introduction to Potential Links and Feedbacks Between Hydrothermal Processes and Seawater Chemistry
- 2 Geochemical Controls on the Composition of Hydrothermal Vent Fluids at Mid-Ocean Ridges
- 3 Experimental Geochemistry Techniques Applied to the Interpretation of High-Temperature Inorganic Geochemistry of Mid-Ocean Ridge Hydrothermal Systems
- 4 The Influence of Seawater Mixing on the Element Budgets in Basalt-Hosted Mid-Ocean Ridge Hydrothermal Systems
- 5 A Review of MacrobiologyâMicrobiology Interactions at Mid-Ocean Ridge Hydrothermal Systems and Their Role in Mediating Element Fluxes into the Ocean
- 6 Instruments and Observations Needed for Better Understanding of Hydrothermal Fluxes Across the Seafloor
- 7 The Marine Sediment Archive of Hydrothermal Activity
- 8 The Effect of Seawater Sr Concentration on the Hydrothermal Alteration of Oceanic Crust: Sr Isotopes in Dikes of the Early Paleozoic Bay of Islands Ophiolite
- 9 Low-Temperature Ridge Flank Heat and Fluid Fluxes, Contributions to Global Biogeochemical Cycles, and Archives of Changing Global Conditions
- 10 The Effect of Off-Axis Hydrothermal Systems on the Oceanic Mg Budget as Revealed by Mg Isotopes: A Review
- 11 Seafloor Weathering: Lessons from Studies of the Critical Zone
- 12 A Historical Perspective on Long-Term Global Biogeochemical Box Models
- 13 Extreme Supercontinental Climate Control: Punctuated Mantle Thermal Mixing and a Sustained Snowball Earth?
- 14 Geochemical and Geophysical Controls on Hydrothermal Fluxes on Habitable Worlds
- 15 The Role of Hydrothermal Processes in the Evolution of Early Earth and Aquaplanets
- INDEX
- END USER LICENSE AGREEMENT