Disruption of the terrestrial plant ecosystem at the Cretaceous-Tertiary boundary, western interior
Science
By: R.H. Tschudy, C. L. Pillmore, C. J. Orth, J. S. Gilmore, and J.D. Knight
Links
- More information: Publisher Index Page (via DOI)
- Download citation as: RIS | Dublin Core
Abstract
The palynologically defined Cretaceous-Tertiary boundary in the western interior of North America occurs at the top of an iridium-rich clay layer. The boundary is characterized by the abrupt disappearance of certain pollen species, immediately followed by a pronounced, geologically brief change in the ratio of fern spores to angiosperm pollen. The occurrence of these changes at two widely separated sites implies continentwide disruption of the terrestrial ecosystem, probably caused by a major catastrophic event at the end of the period.
Suggested Citation
Tschudy, R., Pillmore, C.L., Orth, C.J., Gilmore, J.S., Knight, J., 1984, Disruption of the terrestrial plant ecosystem at the Cretaceous-Tertiary boundary, western interior: Science, v. 225, no. 4666, p. 1030-1032, https://doi.org/10.1126/science.225.4666.1030.
Study Area
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Disruption of the terrestrial plant ecosystem at the Cretaceous-Tertiary boundary, western interior |
| Series title | Science |
| DOI | 10.1126/science.225.4666.1030 |
| Volume | 225 |
| Issue | 4666 |
| Year Published | 1984 |
| Language | English |
| Publisher | American Association for the Advancement of Science |
| Description | 3 p. |
| First page | 1030 |
| Last page | 1032 |
| Country | Canada, United States |
| Other Geospatial | North America western interior |