Assessing environmental change associated with early Eocene hyperthermals in the Atlantic Coastal Plain, USA

Keyphrases

• Environmental Change 100%
• Eocene Hyperthermals 100%
• Atlantic Coastal Plain 100%
• ETM2 100%
• Paleocene-Eocene Thermal Maximum 80%
• Carbon Isotope Excursion 60%
• Hyperthermal 40%
• Clay Mineralogy 40%
• Biogenic Calcite 40%
• Salisbury Embayment 40%
• Climate Change 20%
• Arctic Ocean 20%
• Stable Carbon Isotopes 20%
• Illite 20%
• Global Warming Events 20%
• Transient Global 20%
• Dinoflagellate Cyst Assemblages 20%
• Surface Water 20%
• Magnetostratigraphy 20%
• Thermal Maximum 20%
• TEX86 20%
• Climatic Response 20%
• Calcareous Nannofossils 20%
• Temperature Variation 20%
• Biostratigraphy 20%
• Paleothermometry 20%
• Smectite 20%
• Tight 20%
• Large Fluctuations 20%
• Greenhouse Gas Forcing 20%
• Partial Pressure of CO2 (pCO2) 20%
• Nonlinear Response 20%
• Bottom Water Temperature 20%
• Paleotemperature Proxy 20%
• Nutrient Supply 20%
• Organic-walled Dinoflagellate Cysts 20%
• Hydroclimate 20%
• Shallow Marine Sediments 20%
• Maryland 20%
• Marine Palynology 20%
• Local Hydrology 20%
• Water Temperature Change 20%
• Absence of Evidence 20%
• Strong Perturbation 20%
• Calcareous Dinocysts 20%
• Hydroclimatic Changes 20%

Earth and Planetary Sciences

• Eocene 100%
• Environmental Change 100%
• Coastal Plain 100%
• United States of America 100%
• Paleocene 50%
• Carbon 14 37%
• Calcite 25%
• Mineralogy 25%
• Salinity 12%
• Global Warming 12%
• Climate Change 12%
• Arctic Ocean 12%
• Marine Sediment 12%
• Dinoflagellate Cyst 12%
• Water Temperature 12%
• Surface Water 12%
• Magnetostratigraphy 12%
• Nannofossil 12%
• Biostratigraphy 12%
• Dinocyst 12%
• Paleotemperature 12%
• Montmorillonite 12%
• Bottom Water 12%
• Palynology 12%
• Maryland 12%
• Illite 12%