An iridium abundance anomaly at the palynological Cretaceous-Tertiary boundary in northern New Mexico

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Abstract

An iridium abundance anomaly, with concentrations up to 5000 parts per trillion over a background level of 4 to 20 parts per trillion, has been located in sedimentary rocks laid down under freshwater swamp conditions in the Raton Basin of northeastern New Mexico. The anomaly occurs at the base of a coal bed, at the same stratigraphic position at which several well-known species of Cretaceous-age pollen became extinct. 

Suggested Citation

Orth, C.J., Gilmore, J.S., Knight, J., Pillmore, C.L., Tschudy, R., and Fassett, J., 1981, An iridium abundance anomaly at the palynological Cretaceous-Tertiary boundary in northern New Mexico: Science, v. 214, no. 4527, p. 1341-1343, https://doi.org/10.1126/science.214.4527.1341.

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Publication type Article
Publication Subtype Journal Article
Title An iridium abundance anomaly at the palynological Cretaceous-Tertiary boundary in northern New Mexico
Series title Science
DOI 10.1126/science.214.4527.1341
Volume 214
Issue 4527
Year Published 1981
Language English
Publisher American Association for the Advancement of Science
Description 3 p.
First page 1341
Last page 1343
Country United States
State New Mexico
Other Geospatial northern New Mexico
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