Stable carbon and oxygen isotope record of planktonic foraminifera across the Paleocene-Eocene boundary

The early Cenozoic marine carbon isotopic record is marked by a long-term shift from high d13C values in the late Paleocene to values that are 2 to 3 lower in the early Eocene. The shift is recorded in fossil carbonates from each ocean basin and represents a large change in the distribution of 12C b...

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Bibliographic Details
Main Authors: Stott, Lowell D, Sinha, Ashish, Thiry, Medard, Aubry, Marie-Pierre, Berggren, William A
Format: Dataset
Language:English
Published: PANGAEA 1996
Subjects:
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.770078
https://doi.org/10.1594/PANGAEA.770078