Stable isotopic composition and carbonate concentrations of sediments of the Cretaceous/Paleogene boundary in the Antarctic

Stable isotopic records across the Cretaceous/Paleogene (K/P) boundary in Maud Rise Holes 689B and 690C indicate that significant climatic changes occurred during the latest Cretaceous, beginning approximately 500 k.y. prior to the mass extinction event and the enrichment of iridium at the K/P bound...

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Bibliographic Details
Main Authors: Stott, Lowell D, Kennett, James P
Format: Other/Unknown Material
Language:English
Published: PANGAEA 1990
Subjects:
ODP
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.754364
https://doi.org/10.1594/PANGAEA.754364