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Science 16 March 1984: Vol. 223. no. 4641, pp. 1183 - 1186 DOI: 10.1126/science.223.4641.1183
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Articles
The End of the Cretaceous: Sharp Boundary or Gradual Transition?
W. ALVAREZ 1,
L. W. ALVAREZ 2,
F. ASARO 2, and
H. V. MICHEL 2
1 Department of Geology and Geophysics, University of California, Berkeley 94720
2 Lawrence Berkeley Laboratory, University of California, Berkeley
Evidence indicates that the Cretaceous-Tertiary boundary is very sharp, and, within the limits of resolution, it is apparently synchronous at the various boundary localities. Arguments to the contrary, particularly those of Officer and Darke, are shown to invalid.
Submitted on July 14, 1983
Accepted on December 21, 1983
THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
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- A. HOFFMAN (1989)
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146, 21-35
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237, 1025-1029
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- Shocked Quartz in the Cretaceous-Tertiary Boundary Clays: Evidence for a Global Distribution.
- B. F. Bohor, B. F. BOHOR, P. J. MODRESKI, and E. E. FOORD (1987)
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236, 705-709
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- Response: Cretaceous Extinctions and Wildfires.
- E. ANDERS, W. S. WOLBACH, and R. S. LEWIS (1986)
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- Cretaceous-Tertiary Extinctions: Alternative Models.
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- Cretaceous-Tertiary Extinctions: Alternative Models.
- C. B. OFFICER and C. L. DRAKE (1985)
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230, 1294-1295
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- Terminal Cretaceous Environmental Events.
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