Late Cretaceous to early Paleocene climate and sea-level fluctuations: The Tunisian record

Keyphrases

• Late Cretaceous 100%
• Early Paleocene 100%
• Sea-level Fluctuations 100%
• K/T Boundary 80%
• Tunisia 40%
• Early Danian 40%
• Late Maastrichtian 40%
• Humidity 40%
• Sea-level Lowstand 40%
• Tethys 40%
• Cretaceous-Tertiary 20%
• Foraminiferans 20%
• Bolide Impact 20%
• Middle Latitude 20%
• Environmental Stress 20%
• Clay 20%
• Deccan Volcanism 20%
• Incidental 20%
• Lithology 20%
• Clay Minerals 20%
• Long-term Trends 20%
• Rising Seas 20%
• Humid Climate 20%
• Biostratigraphy 20%
• Terrestrial Organic Matter 20%
• Short-term Effects 20%
• Bulk Rock 20%
• Clay Mineralogy 20%
• Rock Mineralogy 20%
• Greenhouse Conditions 20%
• Late Campanian 20%
• Packstone 20%
• Mineral Variation 20%
• Non-deposition 20%
• Climatic Trends 20%
• High Latitude 20%
• Neritic Habitat 20%
• Short-term Changes 20%
• Flooding Surface 20%

Earth and Planetary Sciences

• Late Cretaceous 100%
• Paleocene 100%
• Sea Level 100%
• Cretaceous-Tertiary Boundary 57%
• Maastrichtian 42%
• Tunisia 28%
• Hiatus 28%
• Danian 28%
• Tethys 28%
• Environmental Stress 14%
• Volcanism 14%
• Organic Matter 14%
• Biostratigraphy 14%
• Mineralogy 14%
• Long-Term Trend 14%
• Rising Sea Level 14%
• Campanian 14%
• Subtidal Environment 14%
• Clay Mineral 14%
• Petrology 14%