Impact of Late Pennsylvanian (early Kasimovian) global warming was greater on wetland than dryland tropical floras; Geological Society of America, 2010 annual meeting

Keyphrases

• Global Warming 100%
• Wetlands 100%
• Drylands 100%
• Late Pennsylvanian 100%
• Kasimovian 100%
• Tropical Flora 100%
• Central Pangaea 66%
• Xeromorphic 66%
• Desmoinesian 66%
• Missourian 66%
• Western Pangea 66%
• Cyclic Changes 33%
• North America 33%
• Drying Conditions 33%
• Tropics 33%
• Physical Habitat 33%
• Climatic Constraints 33%
• New Mexico 33%
• Mineral Soil 33%
• Species Composition 33%
• Seed Plants 33%
• Diverse Habitat 33%
• Ice Age 33%
• Coastal Plain 33%
• Dry Regions 33%
• Wetland Environment 33%
• Coal Bed 33%
• Glacial-interglacial Cycles 33%
• Age Control 33%
• Wetland Vegetation 33%
• Compositional Diversity 33%
• Diversity Patterns 33%
• Non-marine 33%
• Seasonally Dry 33%
• Habitat Requirements 33%
• Species Dominance 33%
• Moscovian 33%
• Conodonts 33%
• Gzhelian 33%
• Callipterids 33%
• Euramerica 33%
• Seed Fern 33%
• Paleoflora 33%
• Coastal Floodplain 33%
• Floristic Turnover 33%
• Internal Responses 33%
• Seasonally Dry Climate 33%
• Dominance-diversity 33%
• Conifer Seeds 33%

Earth and Planetary Sciences

• Global Warming 100%
• Pennsylvanian 100%
• Pangaea 100%
• Vegetation 66%
• Biome 66%
• Floristics 33%
• New Mexico 33%
• Flood Plain 33%
• Arid Region 33%
• Glacial-Interglacial Cycle 33%
• Coastal Plain 33%
• Pleistocene Rewilding 33%
• Moscovian 33%
• Conodont 33%