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Spencer G. Lucas (2026)
Confusion, contradiction, consensus and controversy-Middle-Upper Jurassic stratigraphy on the Southern Colorado Plateau
In: Foster et al., 2026, New Developments in the Paleontology and Geology of the Upper Jurassic Morrison Formation. New Mexico Museum of Natural History and Science Bulletin 102: 73-93
https://www.researchgate.net/publication/399959000_CONFUSION_CONTRADICTION_CONSENSUS_AND_CONTROVERSY-MIDDLE-UPPER_JURASSIC_STRATIGRAPHY_ON_THE_SOUTHERN_COLORADO_PLATEAUMiddle-Upper Jurassic strata on the southern Colorado Plateau assigned to the San Rafael Group and overlying Morrison Formation have been studied for nearly 175 years. Early studies resulted in much confusion and uncertainty about the identification and correlation of the Jurassic stratigraphic units. The monograph by Baker, Dane and Reeside published by the U. S. Geological Survey in 1936 was a turning point in understanding that both resolved some of the confusion and produced more. It began a period of contradiction that culminated in a consensus in the 1950s, which was the Jurassic stratigraphy advocated by the U. S. Geological Survey. In the 1980s-1990s research by Anderson and Lucas called into question much of that consensus and thus began a wide-ranging controversy, particularly about the overall stratigraphic architecture, correlation and relationship to regional unconformities of the Middle-Upper Jurassic strata. These controversies have not been fully resolved. Recent publications have introduced new understanding and new problems, particularly with regard to lithostratigraphy, unconformities, sequence stratigraphy, distributive fluvial systems and magnetostratigraphy.
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Adrian P. Hunt, Spencer G. Lucas and John R. Foster (2026)
The ichnological record of vertebrate consumption from the Upper Jurassic Morrison Formation of western North America with description of a new dentalite and revision of the ichnogenus Machichnus
In: Foster et al., 2026, New Developments in the Paleontology and Geology of the Upper Jurassic Morrison Formation. New Mexico Museum of Natural History and Science Bulletin 102: 359-373
https://www.researchgate.net/publication/399959000_CONFUSION_CONTRADICTION_CONSENSUS_AND_CONTROVERSY-MIDDLE-UPPER_JURASSIC_STRATIGRAPHY_ON_THE_SOUTHERN_COLORADO_PLATEAUThe Upper Jurassic Morrison Formation is famous for its vertebrate fauna, notably dinosaurs, but it yields a relatively depauperate vertebrate ichnofauna, except for tracks. The track ichnofauna is quite extensive, but traces related to consumption are uncommon. Dentalites are known from several Morrison sauropods but only from a few theropods and other non-sauropod herbivorous dinosaurs. We restrict the dentalite ichnogenus Machichnus to include only the ichnospecies M. regularis, M. multilineatus and Machichnus inrosus, which represent rodent gnawing. Morsichnus igen. nov. is introduced to include the raking traces Morsichnus (Machichnus) bohemicus, Morsichnus (Machichnus) fatimae and Morsichnus (Machichnus) dimorphodon. Morsichnus deinodentatus igen. et isp. nov. represents the traces of the biting of large theropods. We coin the term Seeker Effect (Seeker Fieldwork Effect, Seeker Collections Effect) to recognize the importance in the fossil record of fossils being found when sought. Recent work suggests that the Seeker Collection Effect may reveal many more Morrison dentalites when existing collections are re-examined, and the same is true for molalites. Regurgitalites, consumulites and coprolites are very uncommon due to taphonomic megabiases. Pabulites and digestilites are recent concepts that have not been applied to the Morrison Formation trace-fossil record. Micturalites are absent or rare in the Morrison Formation, as they are elsewhere. Claims of Morrison dinosaur gastroliths are largely based on polished siliceous clasts that lack a skeletal association, so these are doubtful records of gastroliths. Theropod tracks from two large dinosaur quarries (Howe Quarry, Something Interesting Quarry) may represent scavenging by carnivores.
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