Oceanic anoxic events and plankton evolution: Biotic response to tectonic forcing during the mid-Cretaceous

Keyphrases

• Accumulation Points 20%
• Albian 20%
• Barremian 20%
• Biotic Responses 100%
• Black Shale 60%
• Carbon Isotope Excursion 40%
• Carbonate 20%
• Cenomanian-Turonian Boundary 20%
• Climate System 40%
• Deep Sea 20%
• Dissolved Iron 20%
• Early Aptian 20%
• Early Turonian 20%
• Geographic Distribution 20%
• Global Warming 20%
• Hydrothermal Activity 20%
• Isotopic Evidence 20%
• Late Albian 20%
• Late Cretaceous 20%
• Lower Aptian 20%
• Marine Productivity 40%
• Marl 20%
• Mexico 20%
• Mid-Cretaceous 100%
• Nutrient Partitioning 20%
• Ocean Circulation 20%
• Ocean Climate 40%
• Oceanic Anoxic Event 100%
• Oceanic Crust 20%
• Organic Carbon Burial 20%
• Organic-rich Shale 20%
• Pelagic Carbonates 20%
• Plankton 60%
• Production Activities 20%
• Rate of Spread 20%
• Speciation 20%
• Strontium 20%
• Submarine Volcanism 20%
• Tectonic Forcing 100%
• Tethys 20%
• Trace Metals 20%
• Turonian 20%
• Volcanism 20%
• Water Column Stratification 20%
• Widespread Distribution 20%

Earth and Planetary Sciences

• Albian 100%
• Aptian 100%
• Barremian 33%
• Black Shale 100%
• Cenomanian-Turonian Boundary 33%
• Deep Sea 33%
• Geographic Distribution 33%
• Global Warming 33%
• Hydrothermal Activity 33%
• Late Cretaceous 33%
• Mexico 33%
• Ocean Circulation 33%
• Ocean Crust 33%
• Organic Carbon 33%
• Sea Level 33%
• Tectonics 100%
• Tethys 66%
• Trace Metal 33%
• Turonian 66%
• Volcanism 66%
• Water Column 33%