Multiple sulfur-isotopic evidence for a shallowly stratified ocean following the Triassic-Jurassic boundary mass extinction

Keyphrases

• Sulfur 100%
• Pyrite 100%
• Triassic-Jurassic Boundary 100%
• Mass Extinction 100%
• Stratified Ocean 100%
• Isotopic Evidence 100%
• Triassic-Jurassic 66%
• Jurassic-Cretaceous Transition 66%
• Epicontinental Seaway 66%
• Organic Carbon 33%
• Carbon Isotopes 33%
• Carbonate 33%
• Black Shale 33%
• Chemocline 33%
• Phanerozoic 33%
• Rhaetian 33%
• Early Jurassic 33%
• Biotic Crisis 33%
• Euxinia 33%
• Suboxic 33%
• Oxic 33%
• Sulfur Isotopes 33%
• Ocean Redox 33%
• Hettangian 33%
• Marine Ecosystems 33%
• Depositional Environment 33%
• Positive Shifts 33%
• Local Development 33%
• Euxinic Conditions 33%
• Bacterial Biomarkers 33%
• Shallow Depth 33%
• Multiple Sulfur Isotopes 33%
• Redox Variations 33%
• Storm Wave Base 33%
• Seawater Sulfate 33%
• Water Depth Gradient 33%
• Ocean Stratification 33%
• Boundary Crisis 33%
• Marine Anoxia 33%
• Isotope Records 33%
• Anoxic Events 33%
• Mass-dependent 33%

Earth and Planetary Sciences

• Mass Extinction 100%
• Black Shale 33%
• Water Depth 33%
• Phanerozoic 33%
• Early Jurassic 33%
• Rhaetian 33%
• Sulfur Isotopes 33%
• Hettangian 33%
• Depositional Environment 33%
• Local Development 33%
• Aquatic Environment 33%
• Organic Carbon 33%
• Storm 33%