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Thaynes Formation
Marine Early Triassic Actinopterygii from Elko County (Nevada, USA): implications for the Smithian equatorial vertebrate eclipse
Chemostratigraphy indicates a relatively complete Late Permian to Early Triassic sequence in the western United States
Gastropod evidence against the Early Triassic Lilliput effect
Three-dimensional structural model of the Painter and East Painter reservoir structures, Wyoming fold and thrust belt
Ecological Signature of Lower Triassic Shell Beds of the Western United States
Silt injection as a mode of fossilization; a Triassic example
Late Early Triassic foraminifers from possible dysaerobic to anaerobic paleoenvironments of the Thaynes Formation, Southeast Idaho
Stellahexaformis and Morozoviella; two new genera of Bryozoa from the Gerster Formation, northeastern Nevada
Parautochthonous Core-Thrusted Kink Folds and Chronologic Sequence of Thrusting, La Barge Platform, Sublette County, Wyoming: ABSTRACT
Source of Triassic Thaynes Hydrocarbons in Idaho-Wyoming-Utah Thrust Belt
Conodont paleoecology and biofacies analysis of the Lower Triassic Thaynes Formation in the Cordilleran Miogeocline
The Lower Triassic (Smithian) Thaynes Formation represents a broad spectrum of paleoenvironments. Samples collected along a depth-related gradient from tidal flats to a relatively deep, commonly dysaerobic, basin yielded an abundant conodont fauna. Simple chi-square tests and multivariate analyses using six conodont entities indicate the presence of three distinctive biofacies related to the general environmental gradient. The restricted inner shelf is characterized by Parachirognathus . The outer shelf is distinguished by a diverse conodont fauna including Furnishius . Basinward, the low diversity conodont fauna is dominated by species of Neogondolella. Some Early Triassic conodonts such as Neospathodus are ubiquitous and provide the best foundation for inter-basinal conodont zonation. Correlation of assemblages with corresponding position along an environmental gradient defined on lithologic criteria indicates that quantitative measures of conodont faunas are potentially useful in the analysis of paleogeography and changes in relative position of sea level.