Late Eocene to early Oligocene oxygen and carbon isotope records and biogenic barium accumulation rates in Maud Rise, Kerguelen Plateau and Agulhas Ridge
The late Eocene through early Oligocene (40-33 Ma) represents a transition from a warm-house to icehouse climate mode, with the expansion of Antarctic glaciation shortly after the Eocene/Oligocene (E/O) boundary. Identifying the driving mechanisms for this climatic event remains controversial and de...
Main Authors: | , , , , , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.959619 |