Palaeoenvironment of the Cenomanian-Turonian transition at Eastbourne, England

Keyphrases

• Faunal Turnover 100%
• Marl 100%
• Cenomanian-Turonian Transition 100%
• Dwellers 75%
• Planktonic Foraminifera 50%
• Oxygen Minimum Zone 50%
• Oxygen Tolerance 50%
• Low Oxygen 50%
• Sea-level Fluctuations 50%
• Marine Transgression 50%
• Tunisia 25%
• High-resolution 25%
• Planktic 25%
• Upwelling 25%
• Thermocline 25%
• Bioturbation 25%
• Stable Isotopes 25%
• Climate Cooling 25%
• Italy 25%
• Upper Part 25%
• Lithology 25%
• Increased Productivity 25%
• Primary Productivity 25%
• Climate Warming 25%
• Erosion Surface 25%
• Oceanographic Conditions 25%
• Biostratigraphic Correlation 25%
• Lithological Variations 25%
• Organic Facies 25%
• Marine Regression 25%
• South East England 25%
• Bonarelli Level 25%
• Bahloul Formation 25%
• Long-term Expansion 25%
• Positive Shift 25%
• Oceanic Anoxic Events 25%
• Changing Climatic Conditions 25%
• Individual Foraminifera Analysis 25%

Earth and Planetary Sciences

• Sea Level 100%
• Turonian 100%
• Cenomanian 100%
• Paleoenvironment 100%
• England 100%
• Foraminifera 66%
• Tunisia 33%
• Thermocline 33%
• Bioturbation 33%
• Trough 33%
• Italy 33%
• Upwelling Water 33%
• Stable Isotope 33%
• Petrology 33%