Late Paleogene paleotopographic evolution of the northern Cordilleran orogenic front: Implications for demise of the orogen

Carbonate stable and clumped isotopic evidence for late Eocene moderate to high elevation of the east-central Tibetan Plateau and its geodynamic implications

Terrestrial cooling and changes in hydroclimate in the continental interior of the United States across the Eocene-Oligocene boundary

Terrestrial paleoenvironmental reconstructions indicate transient peak warming during the early Eocene climatic optimum

Widespread basement erosion during the late Paleocene–early Eocene in the Laramide Rocky Mountains inferred from 87 Sr/ 86 Sr ratios of freshwater bivalve fossils

Sedimentology, detrital zircon geochronology, and stable isotope geochemistry of the lower Eocene strata in the Wind River Basin, central Wyoming