The South Fork detachment fault, Park County, Wyoming; discussion and reply

South Fork detachment fault, Park County, Wyoming; geometry, extent, source

Oregon Basin oil and gas field, Park County, Wyoming

Oregon Basin Field, Park County, Wyoming

Paleozoic Formations Near Cody, Park County, Wyoming

Campanian Paleoseismites of the Elk Basin Anticline, Northern Bighorn Basin, U.S.A.: A Record of Initial Laramide Deformation

Calcardea junnei Gingerich, 1987 from the late Paleocene of North America is not a heron, but resembles the early Eocene Indian taxon Vastanavis Mayr et al., 2007

The Blacktail thrust-fold, Crandall Conglomerate, and Heart Mountain detachment fault, northwestern Wyoming

Deformation of Mesozoic Shales at Hamilton Dome, Bighorn Basin, Wyoming

Floral response to rapid warming in the earliest Eocene and implications for concurrent faunal change

Dissolved gases in hydrothermal (phreatic) and geyser eruptions at Yellowstone National Park, USA

MANGANESE-BEARING RHIZOCRETIONS IN THE WILLWOOD FORMATION, WYOMING, U.S.A.: IMPLICATIONS FOR PALEOCLIMATE DURING THE PALEOCENE–EOCENE THERMAL MAXIMUM

Revision of Piceoerpeton Meszoely (Caudata: Scapherpetontidae) and description of a new species from the late Maastrichtian and ?early Paleocene of western North America

INFLUENCE OF GAS PRODUCTION AND FILAMENT ORIENTATION ON STROMATOLITE MICROFABRIC

MICROBIAL BIOSIGNATURES IN IRON-MINERALIZED PHOTOTROPHIC MATS AT CHOCOLATE POTS HOT SPRINGS, YELLOWSTONE NATIONAL PARK, UNITED STATES

SILICIFICATION OF HIGHER PLANTS IN GEOTHERMALLY INFLUENCED WETLANDS: YELLOWSTONE AS A LOWER DEVONIAN RHYNIE ANALOG

Relationship of Floodplain Ichnocoenoses to Paleopedology, Paleohydrology, and Paleoclimate in the Willwood Formation, Wyoming, During the Paleocene–eocene Thermal Maximum

Astronomical climate control on paleosol stacking patterns in the upper Paleocene–lower Eocene Willwood Formation, Bighorn Basin, Wyoming

Downslope Fossil Contamination: Mammal-Bearing Fluvial Conglomerates and the Paleocene–Eocene Faunal Transition (Willwood Formation, Bighorn Basin, Wyoming)

Paleoclimatic Implications of Crayfish-Mediated Prismatic Structures in Paleosols of the Paleogene Willwood Formation, Bighorn Basin, Wyoming, U.S.A.