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Stable Isotopes, Ir Anomaly and Other Elemental Markers Near the Palaeocene - Eocene Transition: Evidence from the Western Tethys
1998
Mineralogical magazine
Preserved Fulltext
The geological history of the Earth is characterized by several global events recording dramatic climatic, oceanographic and biotic changes. One of them is a short-term Palaeocene-Eocene (P/E) deep sea benthic foraminiferal extinction event (BEE), also marked by distinct negative 813C and 81So anomalies, recorded
doi:10.1180/minmag.1998.62a.1.211
fatcat:7noge4t2arexziylwbkuvhdsi4