Controls on pyrite sulfur isotopes during early diagenesis in marine sediments of the South China Sea

Keyphrases

• AMS 14C 25%
• Carbon Content 25%
• Carbon-nitrogen 25%
• Carbon-sulfur 25%
• Deposition Conditions 25%
• Depositional Environment 25%
• Early Diagenesis 100%
• Environmental Reconstruction 25%
• Global Sulfur Cycle 25%
• Grain Size 25%
• Gravity Cores 25%
• Great Depth 25%
• High Organic Content 25%
• High Sedimentation Rate 25%
• Low Sulphur 25%
• Marine Sediments 100%
• Marine Sulfur Cycle 25%
• Nitrogen Content 25%
• Northern Continental Slope 25%
• Organic Matter Supply 25%
• Planktonic Foraminifera 25%
• Pore Water 25%
• Pyrite 100%
• Pyrite Sulfur Isotope 100%
• Shallow Depth 50%
• South China Sea 100%
• Sulfur Content 25%
• Sulfur Isotope Fractionation 25%
• Sulfur Isotopes 50%
• Sulfur Stable Isotopes 25%
• Syndepositional 25%
• Terrigenous Sediments 25%

Earth and Planetary Sciences

• China 100%
• Continental Slope 33%
• Depositional Environment 33%
• Diagenesis 100%
• Fractionation 33%
• Grain Size 33%
• Isotopic Composition 33%
• Marine Sediment 100%
• Organic Matter 33%
• Planktonic foraminifera 33%
• Porewater 33%
• Sedimentation Rate 33%
• Stable Isotope 33%
• Sulfur Cycle 66%
• Sulfur Isotope 100%