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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Africa
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North Africa
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Morocco (1)
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Asia
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Commonwealth of Independent States
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North America
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United States
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oxygen
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fossils
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geologic age
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Primary terms
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Africa
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North Africa
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Asia
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Cenozoic
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lower Paleocene
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Chordata
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Tetrapoda
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Amphibia
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Lissamphibia
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Caudata (1)
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Aves (1)
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Mammalia
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Multituberculata (1)
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Theria
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Reptilia
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Diapsida
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Archosauria
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dinosaurs
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Ornithischia
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Ceratopsia
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Triceratops (2)
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Ornithopoda
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Hadrosauridae (3)
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Saurischia
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Carnosauria (20)
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Coelurosauria
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Eosuchia (1)
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coprolites (1)
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diagenesis (1)
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Europe
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Western Europe
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United Kingdom
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Hebrides
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Inner Hebrides
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geochemistry (1)
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ichnofossils (5)
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Invertebrata
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isotopes
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maps (1)
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Mesozoic
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Cretaceous
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Lower Cretaceous (1)
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Upper Cretaceous
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Blufftown Formation (1)
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Campanian
-
Dinosaur Park Formation (1)
-
upper Campanian (1)
-
-
Fruitland Formation (1)
-
Hell Creek Formation (4)
-
Horseshoe Canyon Formation (12)
-
Judith River Formation (1)
-
Kirtland Shale (2)
-
K-T boundary (1)
-
Lance Formation (1)
-
Laramie Formation (1)
-
Maestrichtian
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lower Maestrichtian (2)
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Niobrara Formation (1)
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Oldman Formation (1)
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Senonian (11)
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Two Medicine Formation (1)
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Jurassic
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oxygen
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sedimentary rocks
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Tyrannosauridae
TYRANNOSAUR CANNIBALISM: A CASE OF A TOOTH-TRACED TYRANNOSAURID BONE IN THE LANCE FORMATION (MAASTRICHTIAN), WYOMING
PRELIMINARY INVESTIGATION OF SEASONAL PATTERNS RECORDED IN THE OXYGEN ISOTOPE COMPOSITIONS OF THEROPOD DINOSAUR TOOTH ENAMEL
Theropod dinosaurs from the Middle Jurassic (Bajocian–Bathonian) of Skye, Scotland
The significance of the theropod collections of the Royal Tyrrell Museum of Palaeontology to our understanding of Late Cretaceous theropod diversity
Albertosaurus (Dinosauria: Theropoda) material from an Edmontosaurus bonebed (Horseshoe Canyon Formation) near Edmonton: clarification of palaeogeographic distribution
Enhancing bonebed mapping with GIS technology using the Danek Bonebed (Upper Cretaceous Horseshoe Canyon Formation, Edmonton, Alberta, Canada) as a case study
Multivariate analysis of isolated tyrannosaurid teeth from the Danek Bonebed, Horseshoe Canyon Formation, Alberta, Canada
From Tyrannosaurus rex to asteroid impact: Early studies (1901–1980) of the Hell Creek Formation in its type area
Over a century has passed since 1901 when W.T. Hornaday showed a fragment of a horn of Triceratops found in the valley of Hell Creek to H.F. Osborn at the American Museum of Natural History. The following year Osborn's assistant, Barnum Brown, was dispatched to eastern Montana and began investigations of its geology and paleontology. By 1929, Brown had published a geological analysis of the rocks exposed in the southern tributaries of the Missouri River, named the Hell Creek Formation, and published studies of some of the dinosaurs discovered there. Parts of his collections of fossil mollusks, plants, and vertebrates contributed to research by others, particularly members of the U.S. Geological Survey. From 1930 to 1959, fieldwork was slowed by the Great Depression and World War II, but both the continuing search for coal, oil, and gas as well as collections of fossils made during construction of Fort Peck Dam set the stage for later research. Field parties from several museums collected dinosaurian skeletons in the area between 1960 and 1971. In 1962, concentrations of microvertebrates were rediscovered in McCone County by field parties from the University of Minnesota. Ten years later, field parties from the University of California Museum of Paleontology began collecting microvertebrates from exposures in the valley of Hell Creek and its tributaries. The research based on this field research provided detailed geological and paleontological analyses of the Hell Creek Formation and its biota. In turn, these contributed to studies of evolutionary patterns and the processes that produced the changes in the terrestrial biota across the Cretaceous-Paleogene boundary.