03 Dec 2021
Research article | 03 Dec 2021
Climate and ecology in the Rocky Mountain interior after the early Eocene Climatic Optimum
Rebekah A. Stein et al.
Related subject area
Subject: Continental Surface Processes | Archive: Terrestrial Archives | Timescale: CenozoicMammal faunal change in the zone of the Paleogene hyperthermals ETM2 and H2
Clim. Past, 11, 1223–1237,2015
Allen, S. E.: Fossil palm flowers from the Eocene of the Rocky Mountain region with affinities to Phoenix L. (Arecaceae: Coryphoideae), Int. J. Plant Sci., 176, 586–596, 2015.
Allen, S. E.: Reconstructing the local vegetation and seasonality of the Lower Eocene Blue Rim site of southwestern Wyoming using fossil wood, Int. J. Plant Sci., 17, 689–714, 2017a.
Allen, S. E.: The Uppermost Lower Eocene Blue Rim Flora from the Bridger Formation of Southwestern Wyoming: Floristic Composition, Paleoclimate, and Paleoecology, Doctoral Dissertation, University of Florida, 2017b.
Allen, S. E., Stull, G. W., and Manchester, S. R.: Icacinaceae from the Eocene of western North America, Am. J. Bot., 102, 725–744, 2015.
Anagnostou, E., John, E. H., Edgar, K. M., Foster, G. L., Ridgwell, A., Inglis, G. N., Pancost, R. D., Lunt, D. J., and Pearson, P. N.: Changing atmospheric CO2 concentration was the primary driver of early Cenozoic climate, Nature, 533, 380–384, 2016.