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- Publications
- Influence
A Jurassic ceratosaur from China helps clarify avian digital homologies
Theropods have traditionally been assumed to have lost manual digits from the lateral side inward, which differs from the bilateral reduction pattern seen in other tetrapod groups. This unusual… Expand
Djadokhta Formation correlative strata in Chinese Inner Mongolia: an overview of the stratigraphy, sedimentary geology, and paleontology and comparisons with the type locality in the pre-Altai Gobi
- T. Jerzykiewicz, P. J. Currie, D. Eberth, P. Johnston, E. Koster, J. Zheng
- Geology
- 1 October 1993
Because the Bayan Mandahu redbeds of Inner Mongolia share similar sedimentary facies and fossil assemblages with the Djadokhta Formation of pre-Altai Gobi, the two units are interpreted as… Expand
Tectonic, stratigraphic, and sedimentologic significance of a regional discontinuity in the upper Judith River Group (Belly River wedge) of southern Alberta, Saskatchewan, and northern Montana
- D. Eberth, A. P. Hamblin
- Geology
- 1993
The lithostratigraphic interval between the Taber and Lethbridge coal zones in the upper portion of the nonmarine Judith River Group of southeastern Alberta is divisible into two lithostratigraphic… Expand
A basal tyrannosauroid dinosaur from the Late Jurassic of China
The tyrannosauroid fossil record is mainly restricted to Cretaceous sediments of Laurasia, although some very fragmentary Jurassic specimens have been referred to this group. Here we report a new… Expand
Feathered Non-Avian Dinosaurs from North America Provide Insight into Wing Origins
- Darla K. Zelenitsky, François Therrien, +4 authors Frank Hadfield
- Biology, Medicine
- Science
- 26 October 2012
Fancy Feathers In the past few decades, an increasing number of dinosaurs have been shown to have possessed feathers. While it seems likely that feathers themselves may have evolved for… Expand
A revised stratigraphy and depositional history for the Horseshoe Canyon Formation (Upper Cretaceous), southern Alberta plains
- D. Eberth, D. R. Braman
- Geology
- 1 September 2012
The Upper Cretaceous paralic to nonmarine Horseshoe Canyon Formation (HCFm) of southern Alberta is divided into seven mappable members: Strathmore, Drumheller, Horsethief, Morrin, Tolman, Carbon, and… Expand
The Taphonomy of a Centrosaurus (Ornithischia: Certopsidae) Bone Bed from the Dinosaur Park Formation (Upper Campanian), Alberta, Canada, with Comments on Cranial Ontogeny
- M. J. Ryan, A. P. Russell, D. Eberth, P. J. Currie
- Geology
- 1 October 2001
Abstract Bone bed 43 is one of at least eight paucispecific Centrosaurus bone beds located in the Dinosaur Park Formation (Upper Campanian) in Dinosaur Provincial Park, Alberta, Canada. It long has… Expand
Dinosaur biostratigraphy of the Edmonton Group (Upper Cretaceous), Alberta, Canada: evidence for climate influence
- D. Eberth, D. C. Evans, D. Brinkman, François Therrien, D. Tanke, L. S. Russell
- Geology
- 4 March 2013
A high-resolution biostratigraphic analysis of 287 dinosaurian macrofossils and 138 bonebeds in the Edmonton Group (Upper Cretaceous) of southern Alberta provides evidence for at least three… Expand
Dalton Wells: Geology and significance of debris-flow-hosted dinosaur bonebeds in the Cedar Mountain Formation (Lower Cretaceous) of eastern Utah, USA
- D. Eberth, Brooks B Britt, Rod D. Scheetz, Kenneth L. Stadtman, D. Brinkman
- Geology
- 27 June 2006
The Lower Cretaceous Dalton Wells dinosaur locality, north of Moab, Utah, consists of a 2 m thick, stacked succession of four fossil-rich bonebeds with an estimated collective lateral extent of more… Expand
Sequence stratigraphy, paleoclimate patterns, and vertebrate fossil preservation in JurassicCretaceous strata of the Junggar Basin, Xinjiang Autonomous Region, People's Republic of China
- D. Eberth, D. Brinkman, +4 authors Xian-Shen Cheng
- Geology
- 1 December 2001
Multi-kilometre-thick JurassicCretaceous-age sedimentary successions exposed in the southern, northwestern, and northeastern regions of the Junggar Basin display a consistent and correlative… Expand