Diagenesis and iron paleo-redox proxies: New perspectives from magnetic and iron speciation analyses in the Santa Barbara Basin

Keyphrases

• Biogenic Magnetite 20%
• Bivalve Shells 20%
• Bottom Water 80%
• Centennial Timescale 20%
• Depositional Events 20%
• Diagenesis 100%
• Dissolved O2 20%
• Dissolved Oxygen Concentration 20%
• Fe Speciation 20%
• Ferric Hydroxide 20%
• Flood Layer 20%
• Geochemical Methods 20%
• High Sedimentation Rate 20%
• Hypoxia 20%
• In Situ 20%
• Intolerant 20%
• Iron Mineralogy 20%
• Iron Speciation 100%
• Low Oxygen 20%
• Magnetic Analysis 20%
• Magnetic Techniques 20%
• Metal Enrichment 20%
• MoEF 20%
• Non-steady State 20%
• Oxygen Dissolved 20%
• Paleoredox Conditions 20%
• Paleoredox Proxy 100%
• Pore Water 100%
• Pyrite 60%
• Reaction Kinetics 20%
• Reactive Fe 20%
• Redox Geochemistry 20%
• Redox Proxies 20%
• Redox-active Metals 20%
• Santa Barbara Basin 100%
• Sediment Redox 20%
• Sediment-water Interface 20%
• Speciation Analysis 100%
• Sulfide 20%
• Sulfidic 60%
• Turbidites 40%
• Water Column 20%
• Water Environment 20%

Earth and Planetary Sciences

• Bottom Water 80%
• Diagenesis 100%
• Dissolved Oxygen 40%
• Geochemistry 20%
• Iron 100%
• Mineralogy 20%
• Porewater 100%
• Redox Condition 20%
• Sediment-Water Interface 20%
• Sedimentation Rate 20%
• Sulfide 20%
• Turbidite 40%
• Water Column 20%
• Water Environment 20%