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...
Main Authors: | , |
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Format: | Other/Unknown Material |
Language: | English |
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PANGAEA
1990
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.754364 https://doi.org/10.1594/PANGAEA.754364 |