Related Content
Search Google Scholar for:
|
|
Science 2 May 1986: Vol. 232. no. 4750, pp. 629 - 633 DOI: 10.1126/science.232.4750.629
|
|
Articles
Gradual Dinosaur Extinction and Simultaneous Ungulate Radiation in the Hell Creek Formation
ROBERT E. SLOAN 1,
J. KEITH RIGBY JR. 2,
LEIGH M. VAN VALEN 3, and
DIANE GABRIEL 4
1 Department of Geology and Geophysics, University of Minnesota, Minneapolis, MN 55455.
2 Department of Earth Sciences, University of Notre Dame, Notre Dame, IN 46556.
3 Biology Department, University of Chicago, Chicago, IL 60637.
4 Department of Vertebrate Paleontology, Milwaukee Public Museum, Milwaukee, WI 53233.
Dinosaur extinction in Montana, Alberta, and Wyoming was a gradual process that began 7 million years before the end of the Cretaceous and accelerated rapidly in the final 0.3 million years of the Cretaceous, during the interval of apparent competition from rapidly evolving immigrating ungulates. This interval involves rapid reduction in both diversity and population density of dinosaurs. The last dinosaurs known are from a channel that contains teeth of Mantuan mammals, seven species of dinosaurs, and Paleocene pollen. The top of this channel is 1.3 meters above the likely position of the iridium anomaly, the Cretaceous/Tertiary boundary.
Submitted on July 8, 1985
Accepted on January 28, 1986
THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
- Dinosaurs and the Cretaceous Terrestrial Revolution.
- G. T Lloyd, K. E Davis, D. Pisani, J. E Tarver, M. Ruta, M. Sakamoto, D. W.E Hone, R. Jennings, and M. J Benton (2008)
Proc R Soc B
275, 2483-2490
| Abstract »
| Full Text »
| PDF »
- Estimating the diversity of dinosaurs.
- S. C. Wang and P. Dodson (2006)
PNAS
103, 13601-13605
| Abstract »
| Full Text »
| PDF »
- Stratigraphy, sedimentology and palaeoecology of the dinosaur-bearing Kundur section (Zeya-Bureya Basin, Amur Region, Far Eastern Russia).
- J. VAN ITTERBEECK, Y. BOLOTSKY, P. BULTYNCK, and P. GODEFROIT (2005)
Geological Magazine
142, 735-750
| Abstract »
| Full Text »
| PDF »
- Rumen metabolites serve ticks to exploit large mammals.
- G. Donze, C. McMahon, and P. M. Guerin (2004)
J. Exp. Biol.
207, 4283-4289
| Abstract »
| Full Text »
| PDF »
- The high oxygen atmosphere toward the end-Cretaceous; a possible contributing factor to the K/T boundary extinctions and to the emergence of C4 species.
- J. Gale, S. Rachmilevitch, J. Reuveni, and M. Volokita (2001)
J. Exp. Bot.
52, 801-809
| Abstract »
| Full Text »
| PDF »
- The Maastrichtian record at Blake Nose (western North Atlantic) and implications for global palaeoceanographic and biotic changes.
- K. G. MacLeod and B. T. Huber (2001)
Geological Society, London, Special Publications
183, 111-130
| Abstract »
| PDF »
- A new important record of earliest Cenozoic mammalian history: Eutheria and paleogeographic/biostratigraphic summaries.
- J. J. Eberle and J. A. Lillegraven (1998)
Rocky Mountain Geology
33, 49-117
| Abstract »
| Full Text »
| PDF »
- The Cretaceous-Tertiary biotic transition.
- N. Macleod, N. MACLEOD, P. F. RAWSON, P. L. FOREY, F. T. BANNER, M. K. BOUDAGHER-FADEL, P. R. BOWN, J. A. BURNETT, P. CHAMBERS, S. CULVER, et al. (1997)
Journal of the Geological Society
154, 265-292
| Abstract »
| PDF »
- Sudden extinction of the dinosaurs: latest Cretaceous, upper Great Plains, USA.
- P. Sheehan, D. Fastovsky, R. Hoffmann, C. Berghaus, and D. Gabriel (1991)
Science
254, 835-839
| Abstract »
| PDF »
- Barriers Against Interdisciplinarity: Implications for Studies of Science, Technology, and Society (STS.
- H. H. Bauer (1990)
Science Technology Human Values
15, 105-119
| Abstract »
| PDF »
- Mass extinctions: the view of a sceptic.
- A. HOFFMAN (1989)
Journal of the Geological Society
146, 21-35
| Abstract »
| PDF »
- End-Cretaceous Mass Extinction Event: Argument for Terrestrial Causation.
- A. Hallam and A. HALLAM (1987)
Science
238, 1237-1242
| Abstract »
| PDF »
- Cretaceous-Tertiary Dinosaur Extinction.
- G. J. Retallack, G. RETALLACK, and G. D. LEAHY (1986)
Science
234, 1170-1171
| PDF »
|
|