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...
Main Authors: | , , , , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
1996
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.770078 https://doi.org/10.1594/PANGAEA.770078 |