(Eocene epoch)
The transition from Sevier- to Laramide-style tectonics combined with the warmest temperatures of the last ~80 Ma and with short, rapid ‘hyperthermal’ climatic events all resulted in a unique set of geological conditions. How did plants, animals, climate and topography interact during this time period? Specific topics of study include:
1. The relation between the Paleocene-Eocene hyperthemal event (PETM) and changes in basin sedimentation.
2. The impact of non-PETM hyperthermals on terrestrial ecosystems and on basin sedimentation.
3. Interbasinal comparisons of climatic conditions, hydrology, vegetation type and forest structure.
4. Paleoelevation of the eastern side of the Rocky Mountain region during the Eocene and the impact elevation on climate.
5. Mammal behavior and climatic conditions of high-latitude regions during the Eocene ‘hothouse’. See Eberle et al (2009); Eberle et al (2010).
6. Methane production in polar regions during hothouse time periods and its impact on climate.
