Tepee Buttes are low conical hills which occur in scattered clusters along the strike of the Late Cretaceous Pierre Shale near Pueblo, Colorado, and around the Black Hills of South Dakota, Montana, and Wyoming. These erosional landforms develop around resistant columnar limestone masses thought to have been deposited by warm, methane-rich, submarine springs within relatively homogeneous, less resistant claystones. Origin of the Tepee Buttes is attributed to dewatering of underlying claystones. The submarine springs provided a unique habitat on the Western Interior Cretaceous sea bottom for growth of large populations of the lucinid bivalve, Nymphalucina occidentalis, often preserved in living position in reef-like masses encircling the spring vents. Concentration of abundant biomass immediately around the spring vents formed the basis of communities preserved as the Nymphalucina Assemblage dominated by N. occidentalis, but including ammonoid cephalopods, other bivalved mollusks, gastropods, foraminiferans, and a few decapod crustaceans. Fragments of grounded fossilized gymnosperm and angiosperm wood riddled with Teredo borings are also found on the vent cores. Twenty specimens of decapod crustaceans representing three new species of crabs were collected from Tepee Buttes near Oelrichs and Newell, South Dakota, and collecting near Pueblo, Colorado, yielded specimens belonging to three new species, as well as one specimen of Hoplitocarcinus punctatus. The new taxa include Heus foersteri, new genus and species, Raninella manningi, new species (family Raninidae), and Plagiophthalmus bjorki, new species (family Prosopidae ). Descriptions, illustrations, and comparisons of new taxa with previously described members of the family are given.