Volcanic and orbitally forced carbon release during the Middle Eocene Climatic Optimum

Reconstructing source-to-sink systems from detrital zircon core and rim ages

Mississippian southern Laurentia tuffs came from a northern Gondwana arc

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

ERRATUM: Late Paleogene emergence of a North American loess plateau

Late Paleogene emergence of a North American loess plateau

Late Paleozoic subsidence and burial history of the Fort Worth basin: Reply

Jurassic sedimentation in the south-central Qiangtang terrane reveals successive terrane collisions in central Tibet

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

Erratum: Paleozoic sediment dispersal before and during the collision between Laurentia and Gondwana in the Fort Worth Basin, USA

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

Paleozoic sediment dispersal before and during the collision between Laurentia and Gondwana in the Fort Worth Basin, USA

Late Paleozoic subsidence and burial history of the Fort Worth basin

Middle Cenozoic diachronous shift to eolian deposition in the central Rocky Mountains: Timing, provenance, and significance for paleoclimate, tectonics, and paleogeography

Provenance and Depositional Ages of Late Paleogene Fluvial Sedimentary Rocks In the Central Rocky Mountains, U.S.A.

Middle Cenozoic uplift and concomitant drying in the central Rocky Mountains and adjacent Great Plains

Reservoir stratigraphic heterogeneity within the Lower Cretaceous Muddy Sandstone in the Powder River Basin, northeast Wyoming, U.S.A.: Implications for carbon dioxide sequestration

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